tag:blogger.com,1999:blog-62381521186882239342024-03-19T10:54:48.309+01:00Eira de PedraConozco una “eira” de piedra eterna y gris, rodeada de hórreos. Allí han quedado guardados recuerdos de mi niñez y adolescencia. En aquel lugar mágico he compartido momentos inolvidables. Os invito a que esta Eira de piedra virtual sea, al igual que aquella, lugar de encuentro, entretenimiento y aprendizaje sobre el mundo que nos rodea y su cultura.Sonia María García Garcíahttp://www.blogger.com/profile/13489949561200644676noreply@blogger.comBlogger109125tag:blogger.com,1999:blog-6238152118688223934.post-45130369285559067712022-08-02T20:47:00.005+02:002022-08-02T20:48:32.120+02:00" CASTAÑILANDIA", mi nueva obra sobre O Courel<p> <a href="https://soniamariagarciagarcia.blogspot.com/2022/05/castanilandia.html" target="_blank">LEE TODO SOBRE "CASTAÑILANDIA" PINCHANDO EN ESTE ENLACE</a></p><p><br /></p><div class="separator" style="clear: both; text-align: center;"><a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgfpg6h3dml5Bd8QY8DxrUlxPNwjJ3ua4FeuJrpExfCG-KT1mOkkK1PaAG-zEO_2Oi0qJRdpoGTSgeHQPWbPHjT_iAl4-Syyvf9OljqhTyOCz63bVuJ29SBCM5fUUFFWAkvcxiC3hdig1JtwD2GKD3banaF0O2Wl6_V-MGAFXD058tgKnVU4j19f2-P/s2472/Portada%2001.jpg" imageanchor="1" style="margin-left: 1em; margin-right: 1em;"><img border="0" data-original-height="2468" data-original-width="2472" height="638" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgfpg6h3dml5Bd8QY8DxrUlxPNwjJ3ua4FeuJrpExfCG-KT1mOkkK1PaAG-zEO_2Oi0qJRdpoGTSgeHQPWbPHjT_iAl4-Syyvf9OljqhTyOCz63bVuJ29SBCM5fUUFFWAkvcxiC3hdig1JtwD2GKD3banaF0O2Wl6_V-MGAFXD058tgKnVU4j19f2-P/w640-h638/Portada%2001.jpg" width="640" /></a></div><br /><p><br /></p>Sonia María García Garcíahttp://www.blogger.com/profile/13489949561200644676noreply@blogger.com0tag:blogger.com,1999:blog-6238152118688223934.post-36804951679929190942021-08-26T00:46:00.002+02:002021-08-26T00:47:21.243+02:00TODAS MIS NOVEDADES BIBLIOGRÁFICAS<p><span style="font-size: medium;">Podéis consultar todas las novedades con respecto a mis libros:</span></p><p><span style="font-size: medium;">O LIBRO DO COUREL</span></p><p><span style="font-size: medium;">TOCA, EL ORO DE LA GALLAECIA</span></p><p><span style="font-size: medium;">UN ANO NO CARBALLAL. DENDE A VIDA TRADICIONAL AOS NOVOS TEMPOS NO COUREL.</span></p><p><span style="font-size: medium;">RELATOS DE CANDIL</span></p><p><span style="font-size: medium;">En mi blog: <a href="https://soniamariagarciagarcia.blogspot.com">SONIA MARÍA GARCÍA GARCÍA- ESCRITORA</a></span></p><p><br /></p><div class="separator" style="clear: both; text-align: center;"><a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEjHhE36_ntrVoskwGdxA0iXqA7KigjOC4PIJcKYEslNWPM0Jhb5V-67wSRZEDlIpXZz7VWyD42Br4FayrDv9ZP2eBN-igzHes9R2m-I3Af56vxNcWBFd7FOvHuloCXPvPZKTmOQOkiyv40/s520/7e.jpg" style="margin-left: 1em; margin-right: 1em;"><img border="0" data-original-height="520" data-original-width="520" height="400" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEjHhE36_ntrVoskwGdxA0iXqA7KigjOC4PIJcKYEslNWPM0Jhb5V-67wSRZEDlIpXZz7VWyD42Br4FayrDv9ZP2eBN-igzHes9R2m-I3Af56vxNcWBFd7FOvHuloCXPvPZKTmOQOkiyv40/w400-h400/7e.jpg" width="400" /></a></div><br /><div class="separator" style="clear: both; text-align: center;"><a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEjGpZQ6ZNGMNWGTbtxtpKYMxn7QueyxNrjdQwo2CxRmim3MfH5yh-zwZggEypU8OwaIvX1FJBAzdlqTfoN0dvodn5YzQ2IAbF1pigXHaOQQF8SSP-Zm4fn3qjAtu1Db8D_utockGWclvzk/s591/18698307_789659624536419_186906023585886694_n.jpg" style="margin-left: 1em; margin-right: 1em;"><img border="0" data-original-height="591" data-original-width="394" height="400" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEjGpZQ6ZNGMNWGTbtxtpKYMxn7QueyxNrjdQwo2CxRmim3MfH5yh-zwZggEypU8OwaIvX1FJBAzdlqTfoN0dvodn5YzQ2IAbF1pigXHaOQQF8SSP-Zm4fn3qjAtu1Db8D_utockGWclvzk/w266-h400/18698307_789659624536419_186906023585886694_n.jpg" width="266" /></a></div><br /><div class="separator" style="clear: both; text-align: center;"><a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhqaVm3mIpOAheCoImAOK5OI6zgYnWZkvRePvBKBypV5mT8koKhzJJ3CxU9TyRqaJk8wJWw7UuN4KH1VrOtVRLAyXtsAQXVnbop6kmMSr3euDeG7fNkVY6ckEFMN0KfJ43lRtQV_5qv5Mg/s2000/Libro+virtual.jpg" style="margin-left: 1em; margin-right: 1em;"><img border="0" data-original-height="1334" data-original-width="2000" height="426" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhqaVm3mIpOAheCoImAOK5OI6zgYnWZkvRePvBKBypV5mT8koKhzJJ3CxU9TyRqaJk8wJWw7UuN4KH1VrOtVRLAyXtsAQXVnbop6kmMSr3euDeG7fNkVY6ckEFMN0KfJ43lRtQV_5qv5Mg/w640-h426/Libro+virtual.jpg" width="640" /></a></div><br /><div class="separator" style="clear: both; text-align: center;"><a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhXup5g0u9qx4MqHRjimfKH3S0oaUlHnUt1PUkeBRyR5vXmBry0wJ4CaVxsvzhiGCe43qOPkFCiMpgtxEvcADz44heQBx2InY_pRyltj27I1YqI6-duKW7TOLtyu254Do6ey9kuP56zibs/s2048/IMG_20210722_190247.jpg" style="margin-left: 1em; margin-right: 1em;"><img border="0" data-original-height="2048" data-original-width="2048" height="400" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhXup5g0u9qx4MqHRjimfKH3S0oaUlHnUt1PUkeBRyR5vXmBry0wJ4CaVxsvzhiGCe43qOPkFCiMpgtxEvcADz44heQBx2InY_pRyltj27I1YqI6-duKW7TOLtyu254Do6ey9kuP56zibs/w400-h400/IMG_20210722_190247.jpg" width="400" /></a></div><br /><p><br /></p><p><br /></p><p><br /></p><p><br /></p><p><br /></p><p><br /></p>Sonia María García Garcíahttp://www.blogger.com/profile/13489949561200644676noreply@blogger.com0tag:blogger.com,1999:blog-6238152118688223934.post-76932342182986941332021-08-05T01:47:00.005+02:002021-08-05T01:47:54.623+02:00PRESENTACIÓN DE "UN ANO NO CARBALLAL" NA FEIRA DO LIBRO DA CORUÑA<p> <b style="font-size: large; text-align: justify;">"UN ANO NO CARBALLAL. DA VIDA TRADICIONAL AOS NOVOS TEMPOS NO COUREL"</b><span style="font-size: large; text-align: justify;">, xa está inmerso na viaxe dos libros dende o seu autor aos lectores, e sempre hai un momento especial que é a súa presentación. Estas son algunhas instantáneas da 50 Feira do Libro da Coruña, onde tivemos sensacións moi especiais. </span></p><p style="text-align: justify;"><span style="font-size: medium;">Voa alto e lonxe, meu filliño...</span></p><p style="text-align: justify;"><span style="font-size: medium;"><br /></span></p><p style="text-align: justify;"></p><div class="separator" style="clear: both; text-align: center;"><a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEiulpUXv-B5iKRHv8qn4D8hu2PaIsOzGsgT4D8LL0c1w1-7Sy0W7Mm_fnR7Dm4kdMTTrWBMKMh19k9RURtZI-0C5Si4Jo2cyTzilqyda8xV_9giFH7SCTG39U5LPepXJWHeL2O0YDlaNX8/s1000/IMG_20210803_194242.jpg" imageanchor="1" style="margin-left: 1em; margin-right: 1em;"><img border="0" data-original-height="1000" data-original-width="1000" height="640" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEiulpUXv-B5iKRHv8qn4D8hu2PaIsOzGsgT4D8LL0c1w1-7Sy0W7Mm_fnR7Dm4kdMTTrWBMKMh19k9RURtZI-0C5Si4Jo2cyTzilqyda8xV_9giFH7SCTG39U5LPepXJWHeL2O0YDlaNX8/w640-h640/IMG_20210803_194242.jpg" width="640" /></a></div><br /><div class="separator" style="clear: both; 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text-align: center;"><a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEj-LEQUc5Ou_hPZg4XQjVY4oAirOodknaKP1ywU1TDfbo252UmjjJqItjEPIp2671iPaeIqR6dem_LsF7jbJ1sJ4IBZGwdr_V0AkWNHzla9gcRRVtrZuGis7EzmppKq_ekWtSJzvrIltwI/s1000/IMG_20210803_205028.jpg" imageanchor="1" style="margin-left: 1em; margin-right: 1em;"><img border="0" data-original-height="1000" data-original-width="1000" height="640" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEj-LEQUc5Ou_hPZg4XQjVY4oAirOodknaKP1ywU1TDfbo252UmjjJqItjEPIp2671iPaeIqR6dem_LsF7jbJ1sJ4IBZGwdr_V0AkWNHzla9gcRRVtrZuGis7EzmppKq_ekWtSJzvrIltwI/w640-h640/IMG_20210803_205028.jpg" width="640" /></a></div><br /><div class="separator" style="clear: both; text-align: center;"><a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhiLi0SqF-kNbn8BBENVNejGd0-vqdV47pft0ouolUe0uwXDYa0pH9hc-ql-Vl3t2Biddro4GU_y6b06tIwG_TTYPVfu0Blp82kOPJFWAfvSTLG7Tch5wnK36AaheI499MGNXVakTACDlM/s1000/IMG_20210803_205126.jpg" imageanchor="1" style="margin-left: 1em; margin-right: 1em;"><img border="0" data-original-height="918" data-original-width="1000" height="588" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhiLi0SqF-kNbn8BBENVNejGd0-vqdV47pft0ouolUe0uwXDYa0pH9hc-ql-Vl3t2Biddro4GU_y6b06tIwG_TTYPVfu0Blp82kOPJFWAfvSTLG7Tch5wnK36AaheI499MGNXVakTACDlM/w640-h588/IMG_20210803_205126.jpg" width="640" /></a></div><br /><div class="separator" style="clear: both; text-align: center;"><a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEirOkVrbCEiNATyyMX5AF_Gmn7R9BimOe-nQiPORv4HUIYe1hYvykHDOsf7IOJuyRqzPKx9eKDpF1Hr3J4mdnVml2muikBRvRxoI7jw9-qheTvIq4yBL3KZ_3ePVt3gqJ0lH7nCEsOrroQ/s1000/IMG_20210803_205149.jpg" imageanchor="1" style="margin-left: 1em; margin-right: 1em;"><img border="0" data-original-height="912" data-original-width="1000" height="584" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEirOkVrbCEiNATyyMX5AF_Gmn7R9BimOe-nQiPORv4HUIYe1hYvykHDOsf7IOJuyRqzPKx9eKDpF1Hr3J4mdnVml2muikBRvRxoI7jw9-qheTvIq4yBL3KZ_3ePVt3gqJ0lH7nCEsOrroQ/w640-h584/IMG_20210803_205149.jpg" width="640" /></a></div><br /><div class="separator" style="clear: both; text-align: center;"><a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgxINyZ9YEypNtj7HVuR1x5RSroWlmvKMZPnqltq7S5yZQoyVUNthdeGY81g3k-XQFGLoRn6sAXNO-jyMA5DSGt-OaWl9sg39Ww0COlwkjArBZfv-QSADDmSJ6LxQ6i_AWcgQue2FsXnCA/s1000/IMG_20210803_203821.jpg" imageanchor="1" style="margin-left: 1em; margin-right: 1em;"><img border="0" data-original-height="1000" data-original-width="1000" height="640" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgxINyZ9YEypNtj7HVuR1x5RSroWlmvKMZPnqltq7S5yZQoyVUNthdeGY81g3k-XQFGLoRn6sAXNO-jyMA5DSGt-OaWl9sg39Ww0COlwkjArBZfv-QSADDmSJ6LxQ6i_AWcgQue2FsXnCA/w640-h640/IMG_20210803_203821.jpg" width="640" /></a></div><br /><span style="font-size: medium;"><br /></span><p></p>Sonia María García Garcíahttp://www.blogger.com/profile/13489949561200644676noreply@blogger.com0tag:blogger.com,1999:blog-6238152118688223934.post-80494118644449901462021-08-05T01:40:00.001+02:002021-08-05T01:41:28.657+02:00RELATOS DE CANDIL<p></p><div class="separator" style="clear: both; text-align: center;"><a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgfUVbrDOSJ7dat92fVr_8H0OcuYYLW1HHb_lHk_kB8epS44KnCa8QqIL6AnEKgnIT6lFLw10U4Afj9s8H_PQt7nle-nYpCyH9aYqS2ww1ziyNDUpZe775yp_sCtN7zTUqbzoFFn-kbiqc/s640/IMG_20210722_190247.jpg" imageanchor="1" style="margin-left: 1em; margin-right: 1em;"><img border="0" data-original-height="640" data-original-width="640" height="640" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgfUVbrDOSJ7dat92fVr_8H0OcuYYLW1HHb_lHk_kB8epS44KnCa8QqIL6AnEKgnIT6lFLw10U4Afj9s8H_PQt7nle-nYpCyH9aYqS2ww1ziyNDUpZe775yp_sCtN7zTUqbzoFFn-kbiqc/w640-h640/IMG_20210722_190247.jpg" width="640" /></a></div><br /> <p></p><p></p><p style="font-style: normal; font-variant: normal; font-weight: normal; letter-spacing: normal; orphans: 2; widows: 2;">
<span style="font-family: arial;"><span style="color: #cccccc; font-size: medium;">Os
presento mi segunda obra literaria: <b>RELATOS DE CANDIL.</b></span></span></p>
<p style="font-style: normal; font-variant: normal; font-weight: normal; letter-spacing: normal; orphans: 2; widows: 2;">
<span style="font-family: arial;"><span style="color: #cccccc; font-size: medium;"><i>Relatos
de candil </i>es una recopilación de historias llenas de misterio y
suspense, escritas a partir de leyendas gallegas. Algunas de ellas se
basan, además, en hechos reales. El extraordinario dominio de la
narración, los diálogos precisos, las descripciones detalladas y
los personajes poliédricos atraparán al lector, recorriendo
distintas épocas de Galicia y lugares tan variados como el Camino de
Santiago, A Ribeira Sacra, A Mariña lucense, A Coruña antigua o A
Costa da Morte entre otros.</span></span></p>
<p style="font-style: normal; font-variant: normal; font-weight: normal; letter-spacing: normal; orphans: 2; widows: 2;">
<span style="font-family: arial;"><span style="color: #cccccc; font-size: medium;">Leed
y soñad iluminados por la tenue luz del candil que los une…</span></span></p><br /><p></p><div class="separator" style="clear: both; text-align: center;"><a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhdjYqifm4YMWTh7m_UewsxsU2yuq-3SNf-57GW5GLYK4905UvhYpeggX2j1sOKSsdeuy9olWLYXns2gvme5FTF4HESjloT3mcp0sczQVK7QO4QPmOluzjAxn4s2PFWHxWP2yChP-g0QHY/s639/IMG_20210722_180052.jpg" imageanchor="1" style="margin-left: 1em; margin-right: 1em;"><img border="0" data-original-height="552" data-original-width="639" height="552" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhdjYqifm4YMWTh7m_UewsxsU2yuq-3SNf-57GW5GLYK4905UvhYpeggX2j1sOKSsdeuy9olWLYXns2gvme5FTF4HESjloT3mcp0sczQVK7QO4QPmOluzjAxn4s2PFWHxWP2yChP-g0QHY/w640-h552/IMG_20210722_180052.jpg" width="640" /></a></div><br /><div class="separator" style="clear: both; text-align: center;"><br /></div><p style="font-variant-east-asian: normal; font-variant-numeric: normal;">
<span style="font-family: arial;"><span style="color: #cccccc; font-size: 14pt;"><b>TÍTULO:
</b><i>Relatos de candil</i></span></span></p>
<p align="left" style="font-variant-east-asian: normal; font-variant-numeric: normal;">
<span style="font-family: arial;"><span style="color: #cccccc; font-size: 14pt;"><b>AUTORA:
</b>Sonia María García García</span></span></p>
<p align="left" style="font-variant-east-asian: normal; font-variant-numeric: normal;">
<span style="font-family: arial;"><span style="color: #cccccc; font-size: 14pt;"><b>FORMATO:
</b>Tapa blanda con solapas</span></span></p>
<p align="left" style="font-variant-east-asian: normal; font-variant-numeric: normal;">
<span style="font-family: arial;"><span style="color: #cccccc; font-size: 14pt;"><b>TAMAÑO:
</b>15 x 21 cms</span></span></p>
<p align="left" style="font-variant-east-asian: normal; font-variant-numeric: normal;">
<span style="font-family: arial;"><span style="color: #cccccc; font-size: 14pt;"><b>PÁGINAS:
</b>214</span></span></p>
<p align="left" style="font-variant-east-asian: normal; font-variant-numeric: normal;">
<span style="font-family: arial;"><span style="color: #cccccc; font-size: 14pt;"><b>EDITORIAL:
</b>Círculo Rojo</span></span></p>
<p style="font-variant-east-asian: normal; font-variant-numeric: normal;">
<span style="font-family: arial;"><span style="color: #cccccc; font-size: 14pt;"><b>PRECIO:
16 Euros</b></span></span></p>
<p align="left" style="font-variant-east-asian: normal; font-variant-numeric: normal;">
<span style="font-family: Times New Roman;"><span style="font-size: 14pt;"><span style="color: #cccccc; font-family: arial;">(GASTOS
DE ENVÍO INCLUIDOS PARA TODO EL TERRITORIO ESPAÑOL. CONSULTAR PARA
OTROS DESTINOS)</span></span></span></p>
<p align="left" style="font-variant-east-asian: normal; font-variant-numeric: normal;">
<span style="font-family: Times New Roman;"><span style="color: #cccccc; font-size: 14pt;"><span style="font-family: arial;"><b>FORMA
DE PAGO: </b></span><span style="font-family: arial;">PayPal, Bizum </span><span style="font-family: arial;"><span style="font-size: 18pt;">(PAGO
100% SEGURO), consultar otras posibilidades.</span></span></span></span></p>
<p align="left" style="font-variant-east-asian: normal; font-variant-numeric: normal;">
<span style="font-family: Times New Roman;"><span style="font-size: 14pt;"><span style="font-family: arial;"><span style="color: #cccccc; font-size: 18pt;"><b>CONSULTAS
Y PEDIDOS PERSONALIZADOS EN:sonjamar@hotmail.com</b></span></span></span></span></p>
<p align="left" style="font-variant-east-asian: normal; font-variant-numeric: normal;">
<span style="font-family: arial;"><span style="color: #cccccc; font-size: 14pt;"><b>¡Os
atenderé encantada!</b></span></span></p><p align="left" style="font-variant-east-asian: normal; font-variant-numeric: normal;"><span style="color: black;"><span style="font-family: arial;"><span style="font-size: 14pt;"><b><br /></b></span></span></span></p><p align="left" style="font-variant-east-asian: normal; font-variant-numeric: normal;"><span style="color: black;"><span style="font-family: arial;"><span style="font-size: 14pt;"></span></span></span></p><div class="separator" style="clear: both; text-align: center;"><span style="color: black;"><span style="font-family: arial;"><span style="font-size: 14pt;"><a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgys8IhYwT4bF7teOXJLBWC3lJrOMklS0tbbnXOHnJ5lqD8KDxfTCzi8uahZqUn4J74iZJcvxkbTW3HJBF7dUtHWKghWb-U8Ikt-d_B0szBmTHm18CiZR-2eIyEme5EKepobo1T2nbdsAo/s640/IMG_20210722_190819.jpg" imageanchor="1" style="margin-left: 1em; margin-right: 1em;"><img border="0" data-original-height="596" data-original-width="640" height="596" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgys8IhYwT4bF7teOXJLBWC3lJrOMklS0tbbnXOHnJ5lqD8KDxfTCzi8uahZqUn4J74iZJcvxkbTW3HJBF7dUtHWKghWb-U8Ikt-d_B0szBmTHm18CiZR-2eIyEme5EKepobo1T2nbdsAo/w640-h596/IMG_20210722_190819.jpg" width="640" /></a></span></span></span></div><span style="color: black;"><span style="font-family: arial;"><span style="font-size: 14pt;"><br /><b><br /></b></span></span></span><p></p><p></p><p align="left" style="line-height: 100%; margin-bottom: 0cm; orphans: 2; widows: 2;">
<span style="font-variant: normal;"><span style="font-family: arial;"><span style="color: #cccccc; font-size: medium;"><span style="letter-spacing: normal;"><span style="font-style: normal;"><span style="font-weight: normal;">También
podéis adquirirlo en los siguientes enlaces:</span></span></span></span></span></span>
</p><p align="left" style="line-height: 100%; margin-bottom: 0cm; orphans: 2; widows: 2;"><span style="font-variant: normal;"><span style="color: black;"><span style="font-family: arial;"><span style="font-size: medium;"><span style="letter-spacing: normal;"><span style="font-style: normal;"><span style="font-weight: normal;"><br /></span></span></span></span></span></span></span></p><p align="left" style="line-height: 100%; margin-bottom: 0cm; orphans: 2; widows: 2;"><span style="font-variant: normal;"><span style="color: black;"><span style="font-family: arial;"><span style="font-size: medium;"><span style="letter-spacing: normal;"><span style="font-style: normal;"><span style="font-weight: normal;"><a href="https://editorialcirculorojo.com/133737/" target="_blank">COMPRAR EN EDITORIAL CÍRCULO ROJO</a><br /></span></span></span></span></span></span></span></p><p align="left" style="line-height: 100%; margin-bottom: 0cm; orphans: 2; widows: 2;"><span style="font-variant: normal;"><span style="color: black;"><span style="font-family: arial;"><span style="font-size: medium;"><span style="letter-spacing: normal;"><span style="font-style: normal;"><a href="https://www.amazon.es/Relatos-candil-Sonia-Mar%C3%ADa-Garc%C3%ADa/dp/8411048306/ref=sr_1_1?__mk_es_ES=%C3%85M%C3%85%C5%BD%C3%95%C3%91&dchild=1&keywords=RELATOS+DE+CANDIL&qid=1628117983&sr=8-1" target="_blank">COMPRAR EN AMAZON.ES</a><br /></span></span></span></span></span></span></p><p align="left" style="line-height: 100%; margin-bottom: 0cm; orphans: 2; widows: 2;"><span style="font-variant: normal;"><span style="color: black;"><span style="font-family: arial;"><span style="font-size: medium;"><span style="letter-spacing: normal;"><span style="font-style: normal;"><br /></span></span></span></span></span></span></p><br /><p></p>Sonia María García Garcíahttp://www.blogger.com/profile/13489949561200644676noreply@blogger.com0tag:blogger.com,1999:blog-6238152118688223934.post-31584884427363621992021-07-02T10:40:00.001+02:002021-07-02T10:40:46.950+02:00"UN ANO NO CARBALLAL. DENDE A VIDA TRADICIONAL AOS NOVOS TEMPOS NO COUREL"<p><span style="text-align: justify;">En breve, publicaré mi nueva obra "UN ANO NO CARBALLAL. DENDE A VIDA TRADICIONAL AOS NOVOS TEMPOS NO COUREL", un análisis pormenorizado de la vida en esta comarca gallega de montaña y de toda la Galicia interior, a partir de los testimonios de sus propios vecinos. </span></p><p style="text-align: justify;">Si os interesa la etnografía, la antropología, la historia de Galicia, la riqueza de la lengua gallega y la realidad de nuestros ancestros, os invito a pasear por este libro ilustrado con unas fotografías espectaculares y complementado por dos mapas en una edición de calidad excepcional. </p><p style="text-align: justify;">Esta es la vista virtual de la obra que pronto estará en nuestras librerías y en la página de la Editorial Canela.</p><p style="text-align: justify;">Seguiré informando, muchas gracias.</p><p style="text-align: justify;"><br /></p><div class="separator" style="clear: both; text-align: center;"><a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEjUnB6pjqh7auWzY5WNm3PAw3DMLJAclgibn9Ako6hCylDPG1eHSttdd677TCCHc0b9wVXVAVi7pvuqviFy64zrCjuSMYwuCu_NgxYeSMsku1xHbhA8lHp66gO0xORi-0jvVrvUIRW-1K4/s2000/Libro+virtual.jpg" imageanchor="1" style="margin-left: 1em; margin-right: 1em;"><img border="0" data-original-height="1334" data-original-width="2000" height="426" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEjUnB6pjqh7auWzY5WNm3PAw3DMLJAclgibn9Ako6hCylDPG1eHSttdd677TCCHc0b9wVXVAVi7pvuqviFy64zrCjuSMYwuCu_NgxYeSMsku1xHbhA8lHp66gO0xORi-0jvVrvUIRW-1K4/w640-h426/Libro+virtual.jpg" width="640" /></a></div><br /><p style="text-align: justify;"><br /></p>Sonia María García Garcíahttp://www.blogger.com/profile/13489949561200644676noreply@blogger.com0tag:blogger.com,1999:blog-6238152118688223934.post-71573863713401692962020-07-07T23:29:00.003+02:002020-07-08T00:04:19.939+02:00POSTALES DE AQUÍ Y DE ALLÁ: Barcia<div style="text-align: justify;">
<br /></div>
<div style="text-align: justify;">
Barcia es una localidad del concejo asturiano de Santa Eulalia de Oscos. Se encuentra a 710 metros de altitud por lo que cuenta con muestras de una arquitectura tradicional de media montaña, como este precioso corredor de madera con una baranda de motivos populares. </div>
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<div class="separator" style="clear: both; text-align: center;">
<a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEiIGTFBcl6TXikUxQYTb3IPHHF9kfYCor6DNFUbiTM6JwErqczyHe0teXlbra5c7D7grNxlRR6HzJFTYNCBAlaQRbkQwUg6u1juYLehHvLSvMXOiGVSPLMScfCWBQfcnDlEV8jv_6xRn8g/s1600/DSCN0138.JPG" style="margin-left: 1em; margin-right: 1em;"><img border="0" data-original-height="1003" data-original-width="1280" height="500" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEiIGTFBcl6TXikUxQYTb3IPHHF9kfYCor6DNFUbiTM6JwErqczyHe0teXlbra5c7D7grNxlRR6HzJFTYNCBAlaQRbkQwUg6u1juYLehHvLSvMXOiGVSPLMScfCWBQfcnDlEV8jv_6xRn8g/s640/DSCN0138.JPG" width="640" /></a></div>
<div style="text-align: justify;"><br /></div>Sonia María García Garcíahttp://www.blogger.com/profile/13489949561200644676noreply@blogger.com0tag:blogger.com,1999:blog-6238152118688223934.post-17232300976286900272020-07-07T00:36:00.005+02:002020-07-07T01:15:18.341+02:00POSTALES DE AQUÍ Y DE ALLÁ: Nuestra Señora de Las Vegas de Requijada<div style="color: #1c1e21; font-family: helvetica, arial, sans-serif; font-size: 14px; margin-bottom: 6px; text-align: justify;">
<span style="background-color: black; color: white; font-family: inherit;">Como durante un tiempo va a ser imposible viajar y hasta a mis lugares podré ir con cuentagotas, me trasladaré de aquí para allá a través de fotografías del pasado a lugares en los que ya he estado. Hay que consolarse y también es bonito revivir y compartir.</span></div>
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<span style="color: white;"><span style="background-color: black;">Empiezo con esta asombrosa portada románica del siglo XI, de Nuestra señora de Las Vegas de Requijada en Santiuste de Pedraza (Segovia, Castilla- León, España). La iglesia se construyó en varias fases entre los siglos XI y XIV sobre los restos de un templo romano y de una basílica paleocristiana. La portada se encuentra bajo una galería porticada que la protege y que permitió que llegase a nosotros algo tan poco usual del románico para nuestra vista contemporánea como es la policromía.</span></span></div>
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<span style="color: white;"><span style="background-color: black;">La foto es del año 2009.</span></span></div>
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<a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEjpuZYhyphenhyphen8FwH4bP2rxZUU1_5ldmW9_ValGS68thPnX4tgyqDZQxUYileN8mZG9lc_EooD-BvIMfkIp4uDjUMM7asCdzP_17YiBD5jyWayz1ZKa_WzOTKVSZ2LnkYzwniFUXfVaqGayew9I/s1600/IMGP0247+Nuestra+Se%25C3%25B1ora+de+Las+Vegas-Requijada.JPG" style="margin-left: 1em; margin-right: 1em;"><img border="0" data-original-height="986" data-original-width="1320" height="478" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEjpuZYhyphenhyphen8FwH4bP2rxZUU1_5ldmW9_ValGS68thPnX4tgyqDZQxUYileN8mZG9lc_EooD-BvIMfkIp4uDjUMM7asCdzP_17YiBD5jyWayz1ZKa_WzOTKVSZ2LnkYzwniFUXfVaqGayew9I/s640/IMGP0247+Nuestra+Se%25C3%25B1ora+de+Las+Vegas-Requijada.JPG" width="640" /></a></div>
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Sonia María García Garcíahttp://www.blogger.com/profile/13489949561200644676noreply@blogger.com0tag:blogger.com,1999:blog-6238152118688223934.post-12472540711902126382020-05-08T18:34:00.002+02:002020-05-08T18:34:55.537+02:00LA GALICIA INTERIOR<br />
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<span data-original-attrs="{"style":"font-family: \"Times New Roman\"; mso-ansi-language: ES; mso-bidi-language: AR-SA; mso-fareast-font-family: \"Times New Roman\"; mso-fareast-language: ES;"}"><span data-original-attrs="{"style":"font-family: \"Trebuchet MS\", sans-serif;"}"><span style="font-family: Times, Times New Roman, serif;">Empezaré este apartado con el área interior de la provincia de La Coruña. Es ésta una<span data-original-attrs="{"style":"mso-spacerun: yes;"}"> </span>plataforma muy degradada y desfigurada por la erosión y el encajamiento de los ríos siguiendo la dirección de las fallas. Se extiende entre Bergantiños- Finisterre y la Dorsal. Se incluyen las cuencas de los ríos Tambre y Ulla, el valle de la Barcala (Negreira), del Dubra, las tierras de Órdenes (Tambre), el valle de la Mahía, Padrón, A Estrada ( Ulla)...</span></span></span></div>
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<span data-original-attrs="{"style":"mso-bookmark: OLE_LINK1;"}"><span data-original-attrs="{"style":"font-family: \"Trebuchet MS\", sans-serif;"}"><span style="font-family: Times, Times New Roman, serif;">En la comarca de As Mariñas (al S del río Lambre), se extiende un nivel aplanado a 600m. que nos lleva hacia las tierras de Curtis. Por debajo de este nivel existe otra área aplanada y a altitudes inferiores hay restos de otras superficies aplanadas más o menos degradadas por los ríos. En Abegondo y Mabegondo se suceden oteros residuales y pequeñas superficies planas rotas por el río Mero. Hacia el SE, horizontalidad. Son las tierras de Mesía (a un nivel de unos 500m.), o de Mesón de Vento (sobre los 400m.). La morfología en este sector está en relación con la litología, con la red fluvial y con el modelado en el Cuaternario antiguo que ha suavizado las vertientes. Hacia el S, entre As Mariñas y el río Tambre, el relieve apenas varía. Eso sí, las superficies son más amplias y la horizontalidad más acusada. Los ríos que se encajan en distinto grado en esta área son el Anllóns, el Baio, el Xallas y el Tambre.</span></span></span></div>
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Río Anllóns a su paso por Verdes (Coristanco- A Coruña)</div>
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Río Tambre en el lugar de Chaián (Trazo- A Coruña)</div>
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El río Ulla encaja aguas arriba de Pontecesures, en Ponte Ulla, atraviesa la Depresión Meridiana y abre su valle de nuevo hasta la desembocadura aunque sigue siendo un valle profundo. En el camino de este río encontramos un potente dique de cuarzo que ha resistido los ataques de los distintos agentes morfogenéticos: el Pico Sacro.</div>
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<span style="text-align: justify;"> A Ulloa</span></div>
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<span style="text-align: left;">Santiago y Pico Sacro al fondo</span></div>
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<span style="text-align: left;">Río Ulla en O Xirimbao (Reis-Teo- A Coruña)</span></div>
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Al sur del Ulla, el prelitoral se estrecha entre el mar y las sierras centro-occidentales. Existen una serie de escalones a distintas altitudes y encontramos la Depresión Meridiana que se alarga entre Padrón y Caldas de Reis y desde aquí hasta Pontevedra. </div>
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Los encajamientos de los valles fluviales son frecuentes, destacando el río Deza por Carboeiro, o el del río Toxa cerca de Merza donde se precipita sobre el Deza.</div>
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Fervenza del Toxa (Silleda- Pontevedra)</div>
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En la provincia de Lugo es obligado hablar de A Terra Chá. Se extiende entre las sierras septentrionales, las centro-occidentales, la Serra de Meira al E y el valle del Miño. Podemos distinguir tres niveles:</div>
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- Un nivel aplanado a 600 m. (Xermade, Guitiriz, Vilalba, Begonte, Muimenta y Lugo)</div>
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- Un área depresionaria ( Rábade, Cospeito, Castro de Rei, Outeiro de Rei)</div>
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- Un nivel aplanado superior a 700 m. por Meira y Rebordaos, Antas de Ulla, Palas de Rei y Monterroso hasta Chantada.</div>
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Es una superficie de erosión poco alterada aunque con relieves residuales. Entre esto y el tipo de materiales aparecen encharcamientos.</div>
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Baamonde (Lugo)</div>
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Outeiro de Rei (Lugo)</div>
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Finalmente, dentro de la Galicia interior me resta citar los dos grandes valles fluviales gallegos:</div>
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El Valle Medio del Miño, sector en el que el Miño se encaja profundamente en las superficies de erosión circundantes por erosión fluvial y tectónica. Sus afluentes más importantes en este sector son el Avia que baja desde la dorsal y el Arnoia<span data-original-attrs="{"style":"mso-spacerun: yes;"}"> </span>que provoca un relieve muy accidentado.</div>
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<span style="text-align: left;">Río Arnoia a su paso por Allariz (Ourense)</span></div>
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Río Miño en el lugar llamado Cabo do Mundo (O Saviñao- Lugo)</div>
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<span style="text-align: left;"> Embalse de Belesar en el Miño (Lugo)</span></div>
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Terrazas para el cultivo del vino en las laderas del Miño</div>
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<span style="text-align: left;">Encajamiento del Miño en la Depresión Meridiana poco antes de su desembocadura en el Atlántico</span></div>
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El Valle del Sil, es un valle muy encajado y pronunciado, profundo y estrecho debido a la erosión fluvial y, sobre todo, a la tectónica (juego de levantamientos y hundimientos tectónicos desde mediados del Terciario hasta principios del Cuaternario).Las laderas son muy inclinadas con pendientes de hasta el 70 por ciento. El hombre ha intervenido construyendo bancales, terrazas o "socalcos" en las vertientes que permiten su aprovechamiento y evitan la erosión el suelo.</div>
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<span style="text-align: left;">Cañón del Sil </span></div>
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Con este recorrido por el relieve gallego tenemos una visión global de nuestra tierra. En próximos artículos abordaremos lugares concretos de importancia especial que nos permitirán conocerla más en detalle.</div>
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BIBLIOGRAFÍA:<br /><br /><br /><div data-original-attrs="{"style":"margin: 0cm 12pt 0pt; text-align: justify;"}" style="margin: 0cm 12pt 0pt;">
<span data-original-attrs="{"style":"font-family: \"Book Antiqua\"; mso-bidi-font-size: 18.0pt;"}" style="font-family: "book antiqua";"><span data-original-attrs="{"style":"font-size: x-small;"}" style="font-size: xx-small;">- PÉREZ ALBERTI, A.: <u>Xeografía de Galicia, Tomo I : O</u></span></span></div>
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<span data-original-attrs="{"style":"font-family: \"Book Antiqua\"; mso-bidi-font-size: 18.0pt;"}" style="font-family: "book antiqua";"><span data-original-attrs="{"style":"font-size: x-small;"}" style="font-size: xx-small;">Ed. Sálvora, La Coruña, 1982</span></span></div>
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<span data-original-attrs="{"style":"font-family: \"Book Antiqua\"; mso-bidi-font-size: 18.0pt;"}" style="font-family: "book antiqua";"></span></div>
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<span data-original-attrs="{"style":"font-family: \"Book Antiqua\"; mso-bidi-font-size: 18.0pt;"}" style="font-family: "book antiqua";"><span data-original-attrs="{"style":"font-size: x-small;"}" style="font-size: xx-small;">- V.V.A.A.: <u>Geografía de Galicia, Tomo I</u></span></span></div>
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<span data-original-attrs="{"style":"font-family: \"Book Antiqua\"; mso-bidi-font-size: 18.0pt;"}" style="font-family: "book antiqua";"><span data-original-attrs="{"style":"font-size: x-small;"}" style="font-size: xx-small;">La Opinión, La Coruña, 2000</span></span></div>
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Sonia María García Garcíahttp://www.blogger.com/profile/13489949561200644676noreply@blogger.com0tag:blogger.com,1999:blog-6238152118688223934.post-39787147999824447072020-05-08T18:20:00.004+02:002023-04-05T18:03:43.812+02:00LAS DEPRESIONES DE GALICIA<br />
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Al borde de algunas sierras y entre las grandes extensiones interiores aparecen una serie de depresiones como la de As Pontes explotada por sus lignitos y que está en relación con otra más pequeña: la Depresión de Roupar. Del mismo estilo es <span style="mso-spacerun: yes;"> </span>la Depresión de Meirama con la misma explotación que la de As Pontes.</div>
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En la provincia de Pontevedra encontramos las depresiones de O Porriño-Tui, Tea y Oleiros. Tienen en común sus bordes escarpados y rocosos y un fondo plano en el que es posible encontrar varios niveles de <b style="mso-bidi-font-weight: normal;">glacis, abanicos aluviales y terrazas fluviales</b>. En la primera destacan además, las Gándaras de Budiño, área lacustre originada por el remansamiento del río Louro debido al fondo plano de la depresión y la abundancia de materiales arcillosos. Desgraciadamente, están degradadas en parte siempre debido a la mano del hombre.</div>
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La Depresión Central de A Terra Cha, ya en la provincia de Lugo, está limitada por fallas desde el N al O. El límite oriental es menos nítido. Es un depósito que se ha degenerado en <b style="mso-bidi-font-weight: normal;">condiciones palustres o lacustres</b> como en As Pontes, Meirama o la Depresión Meridiana. Por encima de él encontramos <b style="mso-bidi-font-weight: normal;">glacis y abanicos aluviales</b> como en Outeiro de Rei o en Rábade. La acción fluvial del Miño y afluentes ha originado un relieve ondulado con pequeños oteros.<br /> </div>
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Lagunas de Riocaldo (Begonte-Lugo)</div>
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Laguna de Cospeito (Cospeito-Lugo)</div>
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Laguna do Rei (Rábade- Lugo)</div>
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En la misma provincia encontramos la Depresión Sarria- Lemos de morfología plana y la Depresión de Quiroga formada por el mismo tipo de depósitos que la anterior. Está abierta a favor de una fractura que aprovechan el río Quiroga y el Sil.<br /> </div>
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Río Cabe circulando por la depresión de Monforte de Lemos (Lugo)</div>
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Depresión de Quiroga por la que discurre el río Sil</div>
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Ya en la provincia de Orense, se extiende un área con <b style="mso-bidi-font-weight: normal;">depresiones tectónicas</b> separadas por bloques levantados. Aparece así la Depresión de Valdeorras y la Depresión de Maceda en la que la <b style="mso-bidi-font-weight: normal;">morfogénesis fluvial</b> reciente ha labrado un relieve suavemente ondulado con áreas aplanadas, cerros y pequeños valles. Al Sur, la Depresión de A Limia con lignitos a unos 90 m. de profundidad y de gran horizontalidad. La Depresión de Monterrei está separada de las depresiones de Maceda y a Limia por un bloque levantado hasta los 900m. Su fondo plano y la riqueza en sedimentos es semejante a las anteriores. El contacto con las tierras de su entorno es brusco. Además, y dada la existencia de fracturas N-S la depresión es rica en fuentes termales. Por último, mencionar la Depresión de O Bolo que aprovecha una fractura N-S para abrirse. Más que un área hundida se trata de un sector abierto por el Bibei y el Camba aprovechando la existencia de la fractura.</div>
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Pero la depresión más curiosa de Galicia es la Depresión Meridiana que se extiende de N a S desde Carballo hasta Tui.</div>
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Depresión meridiana entre O Porriño y Tui que el río Miño aprovecha para encajar su curso</div><div class="separator" style="clear: both; text-align: center;"><br /></div><div class="separator" style="clear: both; text-align: left;">Para saber más, podéis consultar la bibliografía recomendada. </div>
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<b style="mso-bidi-font-weight: normal;"><span style="font-size: 16pt;">GLOSARIO<span data-original-tag="O:P"></span></span></b></div>
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<b style="mso-bidi-font-weight: normal;">GLACIS: </b>suave pendiente formada por deposición de<span style="mso-spacerun: yes;"> </span>partículas finas</div>
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<strong>ABANICO ALUVIAL:</strong> acumulación de material, especialmente arenas y gravas finas, en forma de abanico o cono, depositados por una coriente de agua en el punto donde abandona un valle angosto que atraviesa un macizo montañoso y se abre a una llanura o valle principal.<br /><strong></strong> </div>
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<b style="mso-bidi-font-weight: normal;">TERRAZA FLUVIAL: </b>pequeña plataforma construida en un valle fluvial por los propios sediemntos del río que se depositan a los ladosdel cauce en los lugares en los que la pendiente del mismo se hace menor.<b style="mso-bidi-font-weight: normal;"><span data-original-tag="O:P"></span></b></div>
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<b style="mso-bidi-font-weight: normal;">ZONA PALUSTRE</b>: lugar de escasa profundidad de agua que permite la instalación de<span style="mso-spacerun: yes;"> </span>vegetación.<b style="mso-bidi-font-weight: normal;"><span data-original-tag="O:P"></span></b></div>
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<b style="mso-bidi-font-weight: normal;">DEPRESIÓN TECTÓNICA: </b>es una fosa limitada en ambos lados por fallas entre las cuales el terreno se ha hundido por efecto de fuerzas internas<b style="mso-bidi-font-weight: normal;"><span data-original-tag="O:P"></span></b></div>
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<b style="mso-bidi-font-weight: normal;">MORFOGÉNESIS FLUVIAL: </b>acción de los ríos sobre las formas del relieve.<br /><br /><br /><br /><span data-original-tag="O:P"><div style="margin: 0cm 12pt 0pt;">
<strong>Bibliografía:</strong><br /> </div>
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<span style="font-family: "book antiqua";"><span style="font-size: xx-small;">- DERRUAU: <u>Geomorfología</u></span></span></div>
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<span style="font-size: xx-small;"><span style="font-family: "book antiqua";">Editorial Ariel, 1991</span></span></div>
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<span style="font-family: "book antiqua";"><span style="font-size: xx-small;">- PÉREZ ALBERTI, A.: <u>Xeografía de Galicia, Tomo I : O</u></span></span></div>
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<span style="font-family: "book antiqua";"><span style="font-size: xx-small;">Ed. Sálvora, La Coruña, 1982</span></span></div>
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<span style="font-family: "book antiqua";"><span style="font-size: xx-small;">- V.V.A.A.: <u>Geografía de Galicia, Tomo I</u></span></span></div>
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<span style="font-family: "book antiqua";"><span style="font-size: xx-small;">La Opinión, La Coruña, 2000</span></span></div>
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Sonia María García Garcíahttp://www.blogger.com/profile/13489949561200644676noreply@blogger.com1tag:blogger.com,1999:blog-6238152118688223934.post-78221930662389385152020-05-08T18:11:00.001+02:002020-05-08T18:11:53.477+02:00LAS SIERRAS DE GALICIA<br />
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Una vez recorrida la costa en nuestro primer viaje por Galicia a través de estas páginas, empezaremos nuestro viaje por las <b data-original-attrs="{"style":"mso-bidi-font-weight: normal;"}">Sierras Septentrionales</b>. Son éstas superficies aplanadas levantadas por la tectónica que en este sector ha actuado con fuerza. La acción fluvial y los cambios climáticos han sido elementos con un papel fundamental en su aspecto actual. Es importante, además, la variada litología existente que ha favorecido el modelado de un relieve contrastado. El Monte Guriscado, los Montes do Xistral, el Cordal de Neda.... son parte de estas sierras.</div>
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<b data-original-attrs="{"style":"mso-bidi-font-weight: normal;"}">Las Sierras Centro-occidentales o Dorsal Gallega</b> se extienden de N a S, desde la Serra Faladoira hasta Faro de Avión, aumentando su altitud cuanto más hacia el S. Están formadas por:</div>
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La Serra Faladoira que presenta un relieve apalachense hacia el O. Se trata de una alternancia entre valles profundos y abiertos con crestas suaves con resaltes de cuarzo y cuarcita. La Serra da Loba y el Cordal de Montouto, con una máxima cota de 742 m. y morfología aplanada. La Serra de A Cova da Serpe y O Careón. Es una sierra suave basculada hacia el E. Dominan los esquistos, granitos y " <b data-original-attrs="{"style":"mso-bidi-font-weight: normal;"}">ollo de sapo</b>". La máxima altura es el Pico Cova de 841m. La Serra do Farelo formada por una serie de escalones aplanados desde los 800 m. a los 500 m., sin grandes desniveles. La Serra do Faro que divide las comarcas del Deza y Asneiro de las de Chantada. Está formada también, como la anterior, por varios escalones a distintas altitudes. Su máxima cota está en el Pico Faro de 1187 m.</div>
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Hacia el S el relieve es más movido. Se alteran bloques levantados con bloques hundidos. Las sierras se ramifican y adquieren mayor volumen: Montes do Testeiro con morfología aplanada en las cumbres, Serra do Suido y Serra do Cando (suaves pero llegan a los 1000 m.), Serra do Faro de Avión, formada por varios niveles aplanados entre los 1000 m. y los 600 m. con laderas<span data-original-attrs="{"style":"mso-spacerun: yes;"}"> </span>empinadas y valles encajados.</div>
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Al S se extiende un área muy degradada por la <b data-original-attrs="{"style":"mso-bidi-font-weight: normal;"}">morfogénesis fluvial</b> de los afluentes del Miño. El relieve se descompone en sectores aplanados cortados por valles fluviales. El Valle del Miño, entre O Ribeiro y As Neves presenta una morfología cerrada. Las fracturas han favorecido un juego de bloques y han engendrado un valle tectónico con frecuentes cambios de dirección. Además, y por el mismo motivo, las fuentes termales jalonan el valle entre Orense y Tui. </div>
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<b data-original-attrs="{"style":"mso-bidi-font-weight: normal;"}">Las Sierras Orientales y Sudorientales</b> se elevan ya hasta los 2000 m. de altitud. El tránsito entre la Galicia interior y estas sierras se hace a través de altas tierras o pequeñas sierras y <b data-original-attrs="{"style":"mso-bidi-font-weight: normal;"}">depresiones tectónicas.<span data-original-tag="O:P"></span></b></div>
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Las Sierras entre el Eo y el Sil se han engendrado sobre materiales pizarrosos, cuarcitas y calizas. Destacan: O Pozo, Portelo, Pedruñales, Foncuberta, Calamouco, Ancares, Piornal, Rañadoiro, Caurel y Serra dos Cabalos. Son una sucesión de crestas y valles. En muchos casos son <strong>interfluvios</strong> coronados por crestones de cuarcita. La acción de los ríos ha sido fundamental en ellas, junto con los movimientos tectónicos y el <b data-original-attrs="{"style":"mso-bidi-font-weight: normal;"}">modelado glaciar y periglaciar</b>.</div>
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Valle del Eo en su nacimiento</div>
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Cascada de Vilarxubín (A Fonsagrada). La más alta de Galicia con más de 50 metros de caída. El río Porteliña no puede salvar la cresta de cuarcitas que forman una falla y salta al vacío. </div>
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Montañas de A Fonsagrada en el valle del río Suarna, al fondo, las sierras asturianas de Ibias</div>
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Cresta cuarcítica en A Pena do Inferno (A Fonsagrada)</div>
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Morrena glaciar</div>
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Detalle<br />
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Detalle</div>
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A Serra de Ancares es de las más importantes del sector. Sus cotas máximas son el Pico Cuíña (1987 m.), el Mustallar (1924 m.) y el Miravalles (1969 m.) . Está formada por una sucesión de valles en paralelo labrados por los afluentes de los ríos Navia y Sil y crestas alomadas, con barras cuarcíticas resaltando en ocasiones. Sus valles son muy profundos y hay huellas de glaciarismo de cumbre, pequeños circos y valles en U (típicos tras la excavación por parte de un glaciar). Pueden verse también <b data-original-attrs="{"style":"mso-bidi-font-weight: normal;"}">morrenas</b>. En las vertientes, existen restos de <b data-original-attrs="{"style":"mso-bidi-font-weight: normal;"}">modelado periglaciar</b>: derrubios estratificados, coladas de bloques<span data-original-attrs="{"style":"color: purple;"}" style="color: purple;">...</span></div>
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<span style="text-align: left;">Las tres fotografías anteriores son de los Ancares vistos desde A Fonsagrada</span></div>
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Valle del Ser<br />
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Miravalles (1969 m.)<br />
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Valle del Balouta<br />
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<a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEjOVSW8RD4XtaqINlZKPiEUGlCkpf7a2forhk-sMNwKvtfi_NlVBU6q1bQzX82Ns_TxxCYHQXNTWCn5NTUThULpvQ-DJLMeuSOekpJYxUNJUarG3sE_qIBREW-j55gF76ZLEZghH8an56A/s1600/14.JPG" imageanchor="1" style="margin-left: 1em; margin-right: 1em;"><img border="0" data-original-height="1600" data-original-width="1271" height="320" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEjOVSW8RD4XtaqINlZKPiEUGlCkpf7a2forhk-sMNwKvtfi_NlVBU6q1bQzX82Ns_TxxCYHQXNTWCn5NTUThULpvQ-DJLMeuSOekpJYxUNJUarG3sE_qIBREW-j55gF76ZLEZghH8an56A/s320/14.JPG" width="254" /></a></div>
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Derrubios<br />
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Detalle de cresta de cuarcita<br />
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Valle glaciar en U<br />
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Cresta cuarcítica en Rao<br />
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Morrena glaciar cercana a Piornedo (Cervantes)<br />
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Sierras ancaresas<br />
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Tres Bispos (1798m.) y Os Penedois (1787m)<br />
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Los bosques de frondosas tienen en Ancares grandes representantes<br />
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Ancares al fondo nevado desde O Cebreiro (Pedrafita) . En primer plano valle del Navia.</div>
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La Serra do Caurel es muy similar a la anterior. En este caso recorrida por los afluentes del Sil (Lor, Soldón y Quiroga). El relieve es movido, los valles muy encajados y sus alturas máximas son el Formigueiros (1643 m.) y el Piapaxaro (1610 m.). Existen también huellas glaciares y periglaciares. </div>
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A Devesa da Rogueira se ha instalado sobre un antiguo circo glaciar<br />
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Valle del Lor. En la parte media izquierda observamos el hayedo de Sisto<br />
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<a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEiQ2hXXrrMmxzZRBNSv08xZRRl0WxOkeuXVvz1pew_f0SfAMMErcotdQRMoOC_MINwpeaRxY4BzcVUxPuuPLmOGpiFaeTynTxLWWjajfJ-a3CNgo2xP4jY0JS5zTlmQBRQ9PVtAIIyR7D4/s1600/26.JPG" imageanchor="1" style="margin-left: 1em; margin-right: 1em;"><img border="0" data-original-height="1200" data-original-width="1600" height="240" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEiQ2hXXrrMmxzZRBNSv08xZRRl0WxOkeuXVvz1pew_f0SfAMMErcotdQRMoOC_MINwpeaRxY4BzcVUxPuuPLmOGpiFaeTynTxLWWjajfJ-a3CNgo2xP4jY0JS5zTlmQBRQ9PVtAIIyR7D4/s320/26.JPG" width="320" /></a></div>
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Donde los ríos no pueden encajarse se forman cascadas como la de Vieiros (Quiroga)<br />
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En O Caurel, es frecuente encontrarse formaciones kársticas como estas estalactitas o el sifón de la foto siguiente, por afloramientos de rocas calcáreas. En este caso las fotos han sido tomadas en O Val Das Mouras (O Caurel).</div>
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<span style="text-align: justify;">En O Pozo das Mulas (las "mulas" son las enormes rocas que vemos en la fotografía) es posible ver enormes morrenas que el hielo arrastró hasta aquí en épocas mucho más frías. (O Caurel)</span><br />
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Valle del Lor hacia el norte<br />
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<a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEjz2QwJTBavO-7Zr2OmQDxVd3m3O6azXtDk95HJhKLV9w27D6Vq_7-fIa8IRzafZDnhbgV_gRSiTUNXGGvGN8UK7nLID7VjUuYbFqicOREQEfHq0GjYekmpkACxtDf-MUo8DDeU4cztskw/s1600/31.JPG" imageanchor="1" style="margin-left: 1em; margin-right: 1em;"><img border="0" data-original-height="670" data-original-width="1592" height="134" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEjz2QwJTBavO-7Zr2OmQDxVd3m3O6azXtDk95HJhKLV9w27D6Vq_7-fIa8IRzafZDnhbgV_gRSiTUNXGGvGN8UK7nLID7VjUuYbFqicOREQEfHq0GjYekmpkACxtDf-MUo8DDeU4cztskw/s320/31.JPG" width="320" /></a></div>
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Cordal de O Courel<br />
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<a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgafDsKGEFFzZsZDH15zgRpv_IrDa7CjXDGGQSuebX8IngezDjvTJWXATNoC_Esvn8KmwS6pW3spEzR5qJp6_2_teo3kLL4F53fG3PkdoHBpAHUsTR3j_8FBX1d_Wrkj6DRTWTc_6_GiuU/s1600/32.JPG" imageanchor="1" style="margin-left: 1em; margin-right: 1em;"><img border="0" data-original-height="1071" data-original-width="1600" height="214" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgafDsKGEFFzZsZDH15zgRpv_IrDa7CjXDGGQSuebX8IngezDjvTJWXATNoC_Esvn8KmwS6pW3spEzR5qJp6_2_teo3kLL4F53fG3PkdoHBpAHUsTR3j_8FBX1d_Wrkj6DRTWTc_6_GiuU/s320/32.JPG" width="320" /></a></div>
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Hacia el Formigueiros (1643m. )<br />
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<a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgkGSl_gXXI_aNTdLBzPTztWf6d3A91Gq4W8u3twV-K7MfxO5OJZvhXXADhkW4-DXt1OMg-t0IIOg82Q313EzKMk-e61BJUyKNt4SEtzyYgsPLu1KZl1NKK3veOOzN7ICcC1gkGR4IHfeY/s1600/34.jpg" imageanchor="1" style="margin-left: 1em; margin-right: 1em;"><img border="0" data-original-height="774" data-original-width="1175" height="210" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgkGSl_gXXI_aNTdLBzPTztWf6d3A91Gq4W8u3twV-K7MfxO5OJZvhXXADhkW4-DXt1OMg-t0IIOg82Q313EzKMk-e61BJUyKNt4SEtzyYgsPLu1KZl1NKK3veOOzN7ICcC1gkGR4IHfeY/s320/34.jpg" width="320" /></a></div>
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Piapáxaro (1610 m.)<br />
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<a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhPO8KAUn0OBg6h4pW07fDN4SeUGdv3SYHRoYeK6Yfa6JW_biTaBRGkiFuazshwJS4Whowsufvq9lIsDZWkxazVnBVMgPT0E8h7TDDmsaO3KHFz7zUPjwvoyN6JNBW7Aq3YsllRYqoS-as/s1600/35.jpg" imageanchor="1" style="margin-left: 1em; margin-right: 1em;"><img border="0" data-original-height="565" data-original-width="1176" height="153" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhPO8KAUn0OBg6h4pW07fDN4SeUGdv3SYHRoYeK6Yfa6JW_biTaBRGkiFuazshwJS4Whowsufvq9lIsDZWkxazVnBVMgPT0E8h7TDDmsaO3KHFz7zUPjwvoyN6JNBW7Aq3YsllRYqoS-as/s320/35.jpg" width="320" /></a></div>
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Morrenas<br />
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Pliegues de Froxán<br />
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<a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEiYnUeVNsKBw1GFK05yBR7OQwhFwiw_CyPgWqRqBmqKCfgQtZOWBX2YRuj3VganZT_VBl0hx5bkOm-tN8tKpIumDT3TGnxFppXBgWq5WgQ13YcHtfGLh4TUbU4sXjQ90ttlOmxtf78cJug/s1600/37.JPG" imageanchor="1" style="margin-left: 1em; margin-right: 1em;"><img border="0" data-original-height="853" data-original-width="1600" height="170" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEiYnUeVNsKBw1GFK05yBR7OQwhFwiw_CyPgWqRqBmqKCfgQtZOWBX2YRuj3VganZT_VBl0hx5bkOm-tN8tKpIumDT3TGnxFppXBgWq5WgQ13YcHtfGLh4TUbU4sXjQ90ttlOmxtf78cJug/s320/37.JPG" width="320" /></a></div>
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Valle del Lóuzara<br />
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<a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgQGTupnD0B4tzAKO0RoRua8MUvEsqlw9QO6NWhHBE-zB2oeeSDkPoU0MkjF_C0AxR6GfBUKe8ohtmXCJlR8mye0Dst9izisH4ZhelI454Cld5D-qez_0YiEJq2fSGGFQFIKe5jWHuZ8es/s1600/38.JPG" imageanchor="1" style="margin-left: 1em; margin-right: 1em;"><img border="0" data-original-height="1057" data-original-width="1589" height="212" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgQGTupnD0B4tzAKO0RoRua8MUvEsqlw9QO6NWhHBE-zB2oeeSDkPoU0MkjF_C0AxR6GfBUKe8ohtmXCJlR8mye0Dst9izisH4ZhelI454Cld5D-qez_0YiEJq2fSGGFQFIKe5jWHuZ8es/s320/38.JPG" width="320" /></a></div>
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Sierra de Cereixido (Quiroga)</div>
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Al Sur del Sil encontramos el Macizo de Manzaneda que está compuesto por las Sierras de Queixa, San Mamede, O Burgo, As Corzas y los Montes do Invernadeiro. Predominan en todas ellas los granitos y las pelitas. La Serra de Queixa presenta una monotonía en las cumbres pero gran vivacidad en los valles que la bordean. Aparecen cascadas. Es nítida la huella de los circos glaciares que han suavizado las formas del centro y arrastrado materiales hacia los bordes (por encima de los 800 m.). Por debajo, en las vertientes actuó el periglaciarismo. En la Serra de San Mamede encontramos de nuevo un relieve de valles y crestas consecuencia de los materiales que la conforman: esquistos con capas de cuarzo y cuarcita que quedan en resalte. En el caso de los Montes do Invernadeiro son las pizarras las que se alternan con las cuarcitas creándose valles paralelos y crestas. Aparecen también <b data-original-attrs="{"style":"mso-bidi-font-weight: normal;"}">valles disimétricos</b> y huellas de glaciarismo y periglaciarismo. El Macizo de Trevinca está formado por la Serra do Eixe y de A Carba. Su morfología es alomada pero con encajamiento de los ríos Bibei y Casaio. Glaciarismo en las cumbres y modelado glaciar también en los valles. Se repiten las características en la Serra Segundeira. Las sierras de Larouco, Xurés o Santa Eufemia están modeladas en granitos y basculadas por la tectónica y disecadas por la acción de los cauces de agua. Glaciarismo y periglaciarismo. Acabamos este apartado de las sierras con las de Leboreiro y los Montes do Quinxo.</div>
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Xurés<br />
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Corga de Fecha (Xurés)</div>
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Xurés, erosión del granito<br />
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Valle del Río Caldo (Xurés)<br />
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Xurés<br />
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Río Caldo con marmitas de gigante por la erosión del granito</div>
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<b data-original-attrs="{"style":"mso-bidi-font-weight: normal;"}"><span data-original-attrs="{"style":"font-size: 22pt;"}" style="font-size: 22pt;">GLOSARIO<span data-original-tag="O:P"></span></span></b></div>
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<b data-original-attrs="{"style":"mso-bidi-font-weight: normal;"}">SEPTENTRIONAL: </b>al norte<b data-original-attrs="{"style":"mso-bidi-font-weight: normal;"}"><span data-original-tag="O:P"></span></b></div>
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<b data-original-attrs="{"style":"mso-bidi-font-weight: normal;"}">OLLO DE SAPO: </b>Gneis con incrustaciones de cuarzo con aspecto de “ollo de sapo”.</div>
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<b data-original-attrs="{"style":"mso-bidi-font-weight: normal;"}">MORFOGÉNESIS FLUVIAL: </b>acción de los ríos sobre las formas del relieve.<b data-original-attrs="{"style":"mso-bidi-font-weight: normal;"}"><span data-original-tag="O:P"></span></b></div>
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<b data-original-attrs="{"style":"mso-bidi-font-weight: normal;"}">DEPRESIÓN TECTÓNICA: </b>es una fosa limitada en ambos lados por fallas entre las cuales el terreno se ha hundido por efecto de fuerzas internas<b data-original-attrs="{"style":"mso-bidi-font-weight: normal;"}"><span data-original-tag="O:P"></span></b></div>
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<b data-original-attrs="{"style":"mso-bidi-font-weight: normal;"}">INTERFLUVIO: </b>espacio<b data-original-attrs="{"style":"mso-bidi-font-weight: normal;"}"> </b>entre dos ríos.<b data-original-attrs="{"style":"mso-bidi-font-weight: normal;"}"><span data-original-tag="O:P"></span></b></div>
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<b data-original-attrs="{"style":"mso-bidi-font-weight: normal;"}">MODELADO GLACIAR: </b>Es el relieve efecto de una <span data-original-attrs="{"style":"mso-bidi-font-weight: bold;"}">glaciación</span>, <span data-original-attrs="{"style":"mso-bidi-font-weight: bold;"}">edad de hielo</span> o <span data-original-attrs="{"style":"mso-bidi-font-weight: bold;"}">periodo glacial</span> que es un periodo de larga duración en el cual baja la temperatura global del clima de la Tierra, dando como resultado una expansión del hielo continental, los casquetes polares y los glaciares.</div>
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<b data-original-attrs="{"style":"mso-bidi-font-weight: normal;"}">MODELADO PERIGLACIAR: </b>es el efecto en el relieve en zonas con condiciones climáticas frías, próximas al medio glaciar, en el espacio o en el tiempo, en las que la acción de la helada es el proceso dominante.<b data-original-attrs="{"style":"mso-bidi-font-weight: normal;"}"><span data-original-tag="O:P"></span></b></div>
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<strong>MORRENA:</strong> Montón de rocas y barro acumuladas por un glaciar.</div>
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<b data-original-attrs="{"style":"mso-bidi-font-weight: normal;"}">VALLE DISIMÉTRICO</b>: valle en el que las laderas no tienen la misma pendiente.</div>
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<b data-original-attrs="{"style":"mso-bidi-font-weight: normal;"}">GLACIS: </b>suave pendiente formada por deposición de<span data-original-attrs="{"style":"mso-spacerun: yes;"}"> </span>partículas finas.<b data-original-attrs="{"style":"mso-bidi-font-weight: normal;"}"><span data-original-tag="O:P"></span></b></div>
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<span data-original-attrs="{"style":"color: #333333;"}" style="color: #333333;"></span><span data-original-tag="O:P"><strong>ABANICO ALUVIAL: </strong>acumulación de material, especialmente arenas y gravas finas, en forma de abanico o cono, depositados por una corriente de agua en el punto donde abandona un valle angosto que atraviesa un macizo montañoso y se abre a una llanura o valle principal.</span></div>
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Bibliografía<strong>:</strong></div>
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<span data-original-attrs="{"style":"font-family: \"Book Antiqua\"; mso-bidi-font-size: 18.0pt;"}" style="font-family: "book antiqua";"><span data-original-attrs="{"style":"font-size: x-small;"}" style="font-size: xx-small;">- DERRUAU: <u>Geomorfología</u></span></span></div>
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<span data-original-attrs="{"style":"font-size: x-small;"}" style="font-size: xx-small;"><span data-original-attrs="{"style":"font-family: \"Book Antiqua\"; mso-bidi-font-size: 18.0pt;"}" style="font-family: "book antiqua";">Editorial Ariel, 1991</span></span></div>
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<span data-original-attrs="{"style":"font-family: \"Book Antiqua\"; mso-bidi-font-size: 18.0pt;"}" style="font-family: "book antiqua";"><span data-original-attrs="{"style":"font-size: x-small;"}" style="font-size: xx-small;">- PÉREZ ALBERTI, A.: <u>Xeografía de Galicia, Tomo I : O</u></span></span></div>
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<span data-original-attrs="{"style":"font-family: \"Book Antiqua\"; mso-bidi-font-size: 18.0pt;"}" style="font-family: "book antiqua";"><span data-original-attrs="{"style":"font-size: x-small;"}" style="font-size: xx-small;">Ed. Sálvora, La Coruña, 1982</span></span></div>
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<span data-original-attrs="{"style":"font-family: \"Book Antiqua\"; mso-bidi-font-size: 18.0pt;"}" style="font-family: "book antiqua";"></span></div>
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<span data-original-attrs="{"style":"font-family: \"Book Antiqua\"; mso-bidi-font-size: 18.0pt;"}" style="font-family: "book antiqua";"><span data-original-attrs="{"style":"font-size: x-small;"}" style="font-size: xx-small;">- V.V.A.A.: <u>Geografía de Galicia, Tomo I</u></span></span></div>
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<span data-original-attrs="{"style":"font-family: \"Book Antiqua\"; mso-bidi-font-size: 18.0pt;"}" style="font-family: "book antiqua";"><span data-original-attrs="{"style":"font-size: x-small;"}" style="font-size: xx-small;">La Opinión, La Coruña, 2000</span></span></div>
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Sonia María García Garcíahttp://www.blogger.com/profile/13489949561200644676noreply@blogger.com0tag:blogger.com,1999:blog-6238152118688223934.post-51628175605601208322020-05-08T16:24:00.001+02:002020-05-08T16:24:31.633+02:00LA RASA CANTÁBRICA<br />
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De todos es conocido que el paisaje que disfrutamos en la actualidad es un instante en la evolución geológica y geomorfológica que empezó hace millones de años y que continuará hasta que la vida del planeta Tierra toque a su fin. Lo que para nosotros es toda una vida, en el tiempo geológico es apenas un suspiro, por lo que para explicar<span data-original-attrs="{"style":"mso-spacerun: yes;"}"> </span>cualquier tipo de paisaje debemos tener esto muy en cuenta. La Rasa Cantábrica que se extiende desde el cabo Peñas hasta Burela y desde Ribadeo hasta Burela en su parte gallega, es producto de una evolución larga que tampoco ha terminado.</div>
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Se trata de una superficie aplanada, con inclinación hacia el Oeste, que se nota en su pérdida de altitud desde los 110 metros en su extremo oriental<span data-original-attrs="{"style":"mso-spacerun: yes;"}"> </span>a los 18-20 metros entre Foz y Burela, donde termina al encontrarse con la masa granítica de San Ciprián. Tiene unos 2 kilómetros de anchura, aunque no de modo uniforme,<span data-original-attrs="{"style":"mso-spacerun: yes;"}"> </span>y está formada por esquistos y pizarras. Ambas rocas son metamórficas, formadas por cambios de temperatura o presión<span data-original-attrs="{"style":"mso-spacerun: yes;"}"> </span>a partir de materiales arcillosos por lo que su origen está en aportes desde el continente, eólicos (traídos por el viento)<span data-original-attrs="{"style":"mso-spacerun: yes;"}"> </span>y marinos según la ocasión, que se transformaron en estas rocas. Ambas, esquistos y pizarras, tienen una estructura en láminas con minerales planos y alargados que le dan a la Rasa su forma característica en capas paralelas. Su composición es rica en mica, cuarzo, clorita, talco, hornblenda, grafito...y, a veces, su coloración es rojiza o incluso negra por estar los minerales cementados con óxidos de hierro y manganeso.</div>
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Esta plataforma sufrió un levantamiento tectónico en la era Terciaria, aproximadamente hace unos 40-38 millones de años que terminó en el Mioceno (entre 23-5 millones de años) con los últimos momentos de la orogenia alpina. Quiere esto decir que Iberia y Eurasia tendían a<span data-original-attrs="{"style":"mso-spacerun: yes;"}"> </span>juntarse siendo la franja litoral cantábrica el punto que sufrió las tensiones. Como consecuencia del choque, la placa euroasiática se deslizó bajo la placa ibérica , elevó la Rasa y provocó el plegamiento de la cordillera Cantábrica formada por materiales más plásticos que tienden más a doblarse<span data-original-attrs="{"style":"mso-spacerun: yes;"}"> </span>que a romperse. Desde entonces, aunque de un modo más lento, la Rasa siguió ascendiendo hasta el Cuaternario, hace unos 1.8 millones de años lo que ha originado distintos niveles de rasa porque los movimientos no eran continuos.</div>
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Esta plataforma elevada, durante el Cuaternario hubo de sufrir más cambios y estos fueron ocasionados por las distintas etapas climáticas que se sucedieron en esta era, en la que todavía nos encontramos.<span data-original-attrs="{"style":"mso-spacerun: yes;"}"> </span>Durante este tiempo, se sucedieron etapas más frías (glaciares) con etapas más cálidas (interglaciares) e inclusive llegamos a tener momentos de clima más parecido al tropical de hoy en día. Por ello, el mar sufrió elevaciones y transgresiones (retrocesos) según la capacidad de los glaciares para retener el agua. La<span data-original-attrs="{"style":"mso-spacerun: yes;"}"> </span>Rasa fue todavía más aplanada dándole su aspecto actual. Llegó a estar 120 metros por debajo del nivel del mar y a entre 2 y 6 metros por encima en el último período interglaciar hace de unos seis a cinco mil años. Hubo tiempo en todos estos cambios a que actuaran sobre ella el mar, el viento, la lluvia...según las circunstancias.</div>
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<a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEh-djBytSa2Wk4KFCd4ZYZ5D53MvCns91GlmMbIsbmh-7hzI6fu7hFeRjqr7ABrlXc6QEj5WjfavRqc5kMp9YPfSxD7w9UN6qGJHmMVHZRQrFnA6uuI2UwMc4YrSGvq4fJQ1ylF7gJSzwo/s1600/6.jpg" imageanchor="1" style="margin-left: 1em; margin-right: 1em;"><img border="0" data-original-height="213" data-original-width="320" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEh-djBytSa2Wk4KFCd4ZYZ5D53MvCns91GlmMbIsbmh-7hzI6fu7hFeRjqr7ABrlXc6QEj5WjfavRqc5kMp9YPfSxD7w9UN6qGJHmMVHZRQrFnA6uuI2UwMc4YrSGvq4fJQ1ylF7gJSzwo/s1600/6.jpg" /></a></div>
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<span style="text-align: justify;">Tal como está hoy en día, sufre una intensa erosión ejercida por el mar sobre sus acantilados. Por los materiales que la conforman, ya citados, y por sus grandes fracturas, se forman</span><span data-original-attrs="{"style":"mso-spacerun: yes;"}" style="text-align: justify;"> </span><span style="text-align: justify;">cuevas ("furnas"), bufadores o bufones, arcos e islotes. La evolución es la siguiente: en primer lugar la acción del mar excava la parte baja de los acantilados y a la vez que</span><span data-original-attrs="{"style":"mso-spacerun: yes;"}" style="text-align: justify;"> </span><span style="text-align: justify;">los materiales arrancados y desgastados por la acción marina y del viento, forman playas, se van formando cuevas. Una vez que la profundidad es suficiente, el techo de la cueva, simplemente por su peso, se desmorona. Si la abertura superior es pequeña pueden formarse bufadores o bufones, si el techo se desmorona completamente, se forman arcos. Pero el mar, el viento, la lluvia.... siguen ejerciendo su erosión y el techo que une el arco con la tierra se acaba hundiendo igualmente y aparecen entonces los islotes.</span></div>
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<span style="text-align: justify;">Así pues, lugares tan visitados como la Playa de las Catedrales en la Mariña lucense, islotes y las distintas formaciones que hoy vemos, tienen este interesante origen.</span></div>
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<strong style="text-transform: uppercase;">LAS FOTOGRAFÍAS QUE ACOMPAÑAN A ESTA ENTRADA SON CORTESÍA DE GABRIEL LÓPEZ PÉREZ</strong></div>
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Bibliografía: <span data-original-tag="O:P"></span></div>
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<span data-original-attrs="{"style":"font-family: \"Book Antiqua\"; mso-bidi-font-size: 18.0pt;"}" style="font-family: "book antiqua";">- V.V.A.A.: <u>Geografía de Galicia, Tomo I</u></span></div>
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La Opinión, La Coruña, 2000</div>
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Sonia María García Garcíahttp://www.blogger.com/profile/13489949561200644676noreply@blogger.com0tag:blogger.com,1999:blog-6238152118688223934.post-410733284614265392020-05-08T16:16:00.001+02:002020-05-08T16:16:08.467+02:00LA COSTA DE GALICIA<br />
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La costa gallega posee una morfología variada ya que encontramos playas, acantilados... y, además, un elemento muy particular: las rías. A través de ellas el mar penetra hacia el interior de la tierra.</div>
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<tr><td class="tr-caption" style="text-align: center;"><span style="font-size: small;">Ría de A Coruña</span><br /><br /><br /><div style="text-align: left;">
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<span style="font-size: small; text-align: justify;">Existen varias hipótesis que intentan explicar su formación. Unas se inclinan por identificarlas con un valle fluvial hundido e invadido por el mar (lo que no se cumple en las </span><b data-original-attrs="{"style":"mso-bidi-font-weight: normal;"}" style="font-size: medium; text-align: justify;">meridionales</b><span style="font-size: small; text-align: justify;">). Otras, apuntan a los materiales como factor que favorece la excavación del mar tierra adentro... Pero la teoría más aceptada y difundida es la que divide las rías en cuatro tipos (tres propiamente dichos y uno mixto).</span></div>
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<span style="font-size: small; text-align: justify;">El primer tipo son las RÍAS EN EMBUDO. Es la forma más simple con equilibrio entre la importancia del río y la ría. Son de este tipo la mayoría de las Rías Altas.</span></div>
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<span style="font-size: small; text-align: justify;">El segundo grupo es el formado por las</span><span data-original-attrs="{"style":"mso-spacerun: yes;"}" style="font-size: small; text-align: justify;"> </span><span style="font-size: small; text-align: justify;">RÍAS </span><span data-original-attrs="{"style":"mso-bidi-font-weight: normal;"}" style="font-size: small; text-align: justify;"><b>TECTÓNICAS</b></span><span style="font-size: small; text-align: justify;">. Son rías amplias debidas a un sistema de </span><b data-original-attrs="{"style":"mso-bidi-font-weight: normal;"}" style="font-size: medium; text-align: justify;">fracturas</b><span style="font-size: small; text-align: justify;">. Ejemplos de ellas son las de Muros y Noia, Pontevedra o la de Vigo.</span></div>
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<span style="font-size: small; text-align: justify;">El tercer tipo recibe el nombre de RÍAS EN ALVEOLO. Son </span><b data-original-attrs="{"style":"mso-bidi-font-weight: normal;"}" style="font-size: medium; text-align: justify;">cubetas de alteración</b><span style="font-size: small; text-align: justify;"> terciaria cuyo origen está en el proceso de erosión que se desarrolló bajo condiciones climáticas distintas a las actuales (en un ambiente más tropical). Son las rías que tienen un contorno más irregular: Arousa, A Coruña...</span></div>
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<span style="font-size: small; text-align: justify;">Son ejemplo de RÍAS DE CARÁCTER MIXTO las de Ribadeo, Betanzos, Camariñas... (rías en embudo e influenciadas por la tectónica).</span></div>
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<span style="font-size: small; text-align: justify;">Las de Ortigueira, Viveiro y Cedeira son mixtas en embudo y alveolo.</span></div>
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<span style="font-size: small; text-align: justify;">Pero nuestro litoral es algo más que rías. Es un conjunto de rías, playas, acantilados e islas desde el Cantábrico hasta el punto más meridional de Galicia en el Atlántico.</span></div>
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<span style="font-size: small;">En primer término playa de Lira, en segundo término, playa de Carnota y Monte Pindo</span></div>
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<span style="font-size: small;">Playa mixta de cantos y arena (A Coruña)</span></div>
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<span style="font-size: small;">Acantilados en Malpica</span></div>
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<span style="font-size: small;">Playa de cantos (A Coruña)</span></div>
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<span style="font-size: small;">Desde la Ría de Ribadeo hasta Burela existe un relieve suave que se materializa en la </span><strong style="font-size: medium;">Rasa,</strong><span style="font-size: small;"> de la que hablaremos con detenimiento en la próxima entrada del blog. Esta es un </span><b data-original-attrs="{"style":"mso-bidi-font-weight: normal;"}" style="font-size: medium;">nivel de aplanamiento</b><span style="font-size: small;"> situado por debajo de los 100 metros y de unos 2 kilómetros de anchura que labraron las aguas marinas.</span></div>
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<span style="font-size: small;">Rasa (Fotografía cortesía de Gabriel López)</span></div>
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<span style="font-size: small;">Detalle de la Rasa</span></div>
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<span style="font-size: small;">La red fluvial de este sector ha excavado sólo pequeños valles y desembocan formando </span><b data-original-attrs="{"style":"mso-bidi-font-weight: normal;"}" style="font-size: medium;">ensenadas</b><span style="font-size: small;">. La ría de Foz completa este sector.</span></div>
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<span style="font-size: small;">El segundo tramo discurre entre la Ría de Viveiro y la de Ortigueira (entre ambas está la Ría do Barqueiro). En este sector de costa encontramos más entrantes y salientes. Las zonas arenosas tienen menor desarrollo que en la zona de Rasa y dominan los acantilados. Las sierras llegan hasta más cerca del mar y desaparece la </span><b data-original-attrs="{"style":"mso-bidi-font-weight: normal;"}" style="font-size: medium;">plataforma costera</b><span style="font-size: small;">. La acción fluvial ha provocado la aparición de zonas fangosas poco profundas que se inundan durante la marea alta o sólo en las grandes mareas, y que suelen estar ocupadas por vegetación. </span></div>
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<span style="font-size: small;">Ría do Barqueiro</span></div>
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<span style="font-size: small;">Punta de Estaca de Bares que separa el mar Cantábrico del océano Atlántico y es el punto más septentrional de la Península Ibérica.</span></div>
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<span style="font-size: small; text-align: justify;">Entramos a partir de aquí en un continuo acantilado debido a la Serra da Capelada. Llega a los 600 metros de altitud con pendientes muy fuertes y conformando uno de los acantilados más altos de Europa. Está </span><b data-original-attrs="{"style":"mso-bidi-font-weight: normal;"}" style="font-size: medium; text-align: justify;">basculada </b><span style="font-size: small; text-align: justify;">hacia la Ría de Ortigueira por lo que las aguas de sus ríos desembocan aquí y no en el océano.</span></div>
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<span style="font-size: small; text-align: justify;">Hacia el sur aparece la Ría de Cedeira con formaciones arenosas y dunas. La costa se vuelve rectilínea y aparecen lagunas costeras y zonas palustres. Tenemos valiosos ejemplos en la Lagoa da Rega (Pantín), la Lagoa da Frouxeira (Valdoviño) o la Lagoa de Doniños.</span></div>
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<span style="font-size: small;">Frouxeira</span></div>
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<span style="font-size: small;">Llegamos así a la Ría de Ferrol. Su boca es estrecha (ha tenido que hacerse paso entre granitos), su parte central ancha (esquistos) y su fondo vuelve a ser estrecho. Además de la diferencia </span><b data-original-attrs="{"style":"mso-bidi-font-weight: normal;"}" style="font-size: medium;">litológica</b><span style="font-size: small;"> existe una diferencia en la altitud de las laderas que influye en la red fluvial a veces de morfología suave (Belelle, Río Grande de Xubia...) y, a veces, más brusca en donde los ríos son incapaces de romper la roca y aparecen cascadas.</span></div>
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<span style="font-size: small;">Fervenza do Belelle</span></div>
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<span style="font-size: small; text-align: justify;">También los esquistos favorecen una morfología abierta en la Ría de Ares y Betanzos. Los ríos Eume, Lambre, Mandeo y Mendo conforman un relieve suave.</span></div>
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<span style="font-size: small; text-align: justify;">En Miño y la Ría de Betanzos es muy importante el proceso de </span><b data-original-attrs="{"style":"mso-bidi-font-weight: normal;"}" style="font-size: medium; text-align: justify;">terrestrificación.</b><span style="font-size: small; text-align: justify;"> Además, en Miño encontramos un banco arenoso que ha frenado la acción marina y fluvial hasta el punto de </span><b data-original-attrs="{"style":"mso-bidi-font-weight: normal;"}" style="font-size: medium; text-align: justify;">colmatar </b><span style="font-size: small; text-align: justify;"> la desembocadura del río Baxoi.</span></div>
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<span style="font-size: small; text-align: justify;">El relieve sigue siendo suave y de poca altitud</span><span data-original-attrs="{"style":"mso-spacerun: yes;"}" style="font-size: small; text-align: justify;"> </span><span style="font-size: small; text-align: justify;">hasta la Ría de La Coruña . Es ésta una media luna abierta al océano con zonas cerradas por formaciones arenosas como en Santa Cristina (flecha arenosa). Hacia el interior existen ya escalones a distintas altitudes.</span></div>
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<span style="font-size: small; text-align: justify;">A partir de aquí la costa cambia. Predominan los granitos y los acantilados se encadenan con grandes arenales con formaciones dunares de gran desarrollo. Un buen ejemplo de todo ello, añadiendo además su laguna, es el conjunto de Baldaio.</span></div>
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<span style="font-size: small;">Baldaio</span></div>
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<span style="font-size: small; text-align: justify;">En este sector aparecen de Norte a Sur la Ría de Corme y Laxe, la Ría de Camariñas y la Ría de Cee y Corcubión. Destaca en ésta última el Monte Pindo en el que se incrusta la pequeña Ría de Ézaro. El río Xallas es incapaz de excavar su cauce y se despeña hacia esta ría.</span></div>
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<span style="font-size: small;">Punta Nariga (erosión del granito)</span></div>
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<span style="font-size: small;">Ría de Corme y Laxe</span></div>
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<span style="font-size: small;">Plena Costa da Morte</span></div>
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<span style="font-size: small;">Ensenada do Trece, su complejo dunar y duna rampante al fondo</span></div>
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<span style="font-size: small;"> Fisterra bajo el sol poniente</span></div>
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<span style="font-size: small; text-align: justify;">La Ría de Muros y Noia es de transición entre las Rías Altas y las Rías Bajas. Está situada entre la Sierra de Outes al Norte y la del Barbanza al Sur. Estas sierras quedaron como restos de la superficie de erosión fundamental de Galicia y alcanzan los 700 m. de altitud en el Barbanza. Las aguas de esta ría son las del río Tambre. En cualquier caso, el frente litoral es suave y abundan los arenales y dunas como en Corrubedo. Existe aquí la única duna viva de Galicia que aún sigue moviéndose.</span></div>
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<span style="font-size: small;">La Ría de Arousa es una ría tectónica. Se trata de una gran depresión terciaria rellena de </span><b data-original-attrs="{"style":"mso-bidi-font-weight: normal;"}" style="font-size: medium;">sedimentos </b><span style="font-size: small;">e inundada por el océano. Al Norte la delimita la Sierra del Barbanza y al Sur una serie de promontorios como el Xiabre, el Castrove... con gran contraste entre las llanuras costeras y estas sierras. En ella desemboca el río Ulla. </span></div>
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<span style="font-size: small;">Existen huellas de distintos niveles marinos en la Isla de Arousa, el Salnés o en la ensenada de A Toxa donde también se observan áreas fangosas. En el arenal de La Lanzada aparecen dunas y restos de playas antiguas. </span></div>
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<span style="font-size: small;">La Ría de Pontevedra está en relación con una fractura SO- NE con tramos movidos y otros más abiertos pero siempre de morfología suave. Las playas son menos numerosas que en otros tramos pero siempre están presentes. En ella desemboca el río Lérez.</span></div>
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<span style="font-size: small;">A su entrada encontramos las Islas de Ons. Son unas islas graníticas con playas y acantilados. Su valor ecológico es muy grande y recientemente han sido nombradas Parque Nacional junto con las Islas Cíes y la Isla de Sálvora</span><span data-original-attrs="{"style":"color: purple;"}" style="color: purple; font-size: small;">.</span></div>
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<span data-original-attrs="{"style":"color: purple;"}" style="font-size: small;"><span style="color: white;">Ría de Arousa</span></span></div>
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<span data-original-attrs="{"style":"color: purple;"}" style="font-size: small;"><span style="color: white;">Islas de Ons </span></span></div>
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<span data-original-attrs="{"style":"color: purple;"}" style="color: purple; font-size: small;"><span style="color: black;">La Ría de Vigo es similar a la anterior pero más amplia. Al Norte la delimita la península do Morrazo desgajada por la Depresión Meridiana que la rompe por Redondela. También aparecen playas y dunas muy degradadas por el hombre. En su boca hallamos las Islas Cíes ( Parque Nacional) de extraordinaria riqueza ecológica.</span></span></div>
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Islas Cíes</div>
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<span style="font-size: small; text-align: justify;">Al sur, los Montes da Groba la separan del valle del Miño. Es éste un medio abierto que favorece la introducción de los ambientes marinos hacia el interior. En este sector destaca la gran fracturación del granito.</span></div>
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<b data-original-attrs="{"style":"mso-bidi-font-weight: normal;"}"><span data-original-attrs="{"style":"font-size: 22pt;"}" style="font-size: 22pt;">GLOSARIO<span data-original-tag="O:P"></span></span></b></div>
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<b data-original-attrs="{"style":"mso-bidi-font-weight: normal;"}">SEPTENTRIONAL</b>: al Norte.</div>
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<b data-original-attrs="{"style":"mso-bidi-font-weight: normal;"}">MERIDIONAL</b>: al Sur.</div>
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<b data-original-attrs="{"style":"mso-bidi-font-weight: normal;"}">FRACTURA</b>: ruptura en las rocas.</div>
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<b data-original-attrs="{"style":"mso-bidi-font-weight: normal;"}">TECTÓNICA</b>: es la especialidad de la geología que estudia las estructuras geológicas producidas por deformación de la corteza terrestre, las que las rocas adquieren después de haberse formado, así como los procesos que las originan.</div>
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<b data-original-attrs="{"style":"mso-bidi-font-weight: normal;"}">CUBETA DE ALTERACIÓN</b>: depresión en la que se depositan materiales que sufren algún tipo de cambio.</div>
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<b data-original-attrs="{"style":"mso-bidi-font-weight: normal;"}">RASA</b>: plataforma de erosión marina o terraza emergida durante el Terciario.</div>
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<b data-original-attrs="{"style":"mso-bidi-font-weight: normal;"}">NIVEL DE APLANAMIENTO</b>: superficie plana.</div>
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<b data-original-attrs="{"style":"mso-bidi-font-weight: normal;"}">ENSENADA</b>: entrada de agua circular o redondeada con una boca estrecha</div>
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<b data-original-attrs="{"style":"mso-bidi-font-weight: normal;"}">PLATAFORMA COSTERA</b>: Terraza en el litoral.</div>
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<b data-original-attrs="{"style":"mso-bidi-font-weight: normal;"}">BASCULADA</b>: inclinada.</div>
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<b data-original-attrs="{"style":"mso-bidi-font-weight: normal;"}">ZONA PALUSTRE</b>: lugar de escasa profundidad de agua que permite la instalación de<span data-original-attrs="{"style":"mso-spacerun: yes;"}"> </span>vegetación.</div>
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<b data-original-attrs="{"style":"mso-bidi-font-weight: normal;"}">LITOLOGÍA</b>: parte de la geología que nos habla de las rocas.</div>
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<b data-original-attrs="{"style":"mso-bidi-font-weight: normal;"}">TERRESTRIFICACIÓN</b>: relleno de lugares por aporte de sólidos<span data-original-attrs="{"style":"mso-spacerun: yes;"}"> </span>que da lugar a zonas fangosas.</div>
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<b data-original-attrs="{"style":"mso-bidi-font-weight: normal;"}">COLMATAR</b>: rellenar.</div>
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<b data-original-attrs="{"style":"mso-bidi-font-weight: normal;"}">SEDIMENTO</b>: material sólido, transportado por una corriente de agua, el viento o la gravedad que se deposita en lugares de menor altitud o en los fondos fluviales o marinos.</div>
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<span data-original-attrs="{"style":"font-family: \"Book Antiqua\"; mso-bidi-font-size: 18.0pt;"}" style="font-family: "book antiqua";"><span data-original-attrs="{"style":"font-size: x-small;"}" style="font-size: xx-small;">- PÉREZ ALBERTI, A.: <u>Xeografía de Galicia, Tomo I : O</u></span></span></div>
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<span data-original-attrs="{"style":"font-family: \"Book Antiqua\"; mso-bidi-font-size: 18.0pt;"}" style="font-family: "book antiqua";"><span data-original-attrs="{"style":"font-size: x-small;"}" style="font-size: xx-small;">Ed. Sálvora, La Coruña, 1982</span></span></div>
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<span data-original-attrs="{"style":"font-family: \"Book Antiqua\"; mso-bidi-font-size: 18.0pt;"}" style="font-family: "book antiqua";"></span></div>
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<span data-original-attrs="{"style":"font-family: \"Book Antiqua\"; mso-bidi-font-size: 18.0pt;"}" style="font-family: "book antiqua";"><span data-original-attrs="{"style":"font-size: x-small;"}" style="font-size: xx-small;">- V.V.A.A.: <u>Geografía de Galicia, Tomo I</u></span></span></div>
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<span data-original-attrs="{"style":"font-family: \"Book Antiqua\"; mso-bidi-font-size: 18.0pt;"}" style="font-family: "book antiqua";"><span data-original-attrs="{"style":"font-size: x-small;"}" style="font-size: xx-small;">La Opinión, La Coruña, 2000</span></span></div>
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Sonia María García Garcíahttp://www.blogger.com/profile/13489949561200644676noreply@blogger.com0tag:blogger.com,1999:blog-6238152118688223934.post-20349875940946774992020-05-08T15:31:00.002+02:002020-05-08T15:31:42.551+02:00EL RELIEVE DE GALICIA<br />
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El territorio gallego no es uniforme. Siempre ha sido comentario popular la dificultad de la <b data-original-attrs="{"style":"mso-bidi-font-weight: normal;"}">orografía</b> gallega a la hora de planificar carreteras, líneas de ferrocarril, túneles, viaductos…O, simplemente y sin ponernos tan técnicos, al movernos en coche por ella o al hacer una ruta de senderismo. ¿Quién no ha sufrido nuestras curvas o nuestras cuestas?</div>
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En Galicia no hay montañas demasiado elevadas. Desde los 0 metros de altitud a nivel del mar podemos llegar a los 2124 metros de Pena Trevinca como máxima altura. Lo que ocurre es que el territorio está muy compartimentado y ese paso de unas superficies a otras es el que origina la complicación del mismo con las repercusiones correspondientes en el clima, población, comunicaciones, etc.<br /> </div>
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Para facilitar la descripción del relieve gallego dividiré el mismo en varios sectores que analizaré poco a poco.</div>
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<span data-original-attrs="{"style":"mso-bidi-font-weight: bold;"}">En primer lugar la parte<span data-original-attrs="{"style":"mso-spacerun: yes;"}"> </span>litoral.</span></div>
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<tr><td style="text-align: center;"><a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEg5sCd3q0-3a_KonLL_VwUe9YP14kLAta3cl3i1UtRsJwmFVYIeF44RT-TmZ5jklYP2F6bPzVWrdR49jojJ8dp3NqTjkYVAMCvfBpwcsnGzS1Cb7XM1Ui-XAIo8ioJ-dgDW4NDeI9txpss/s1600/DSC_0067dream.JPG" imageanchor="1" style="margin-left: auto; margin-right: auto;"><img border="0" data-original-height="191" data-original-width="400" height="152" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEg5sCd3q0-3a_KonLL_VwUe9YP14kLAta3cl3i1UtRsJwmFVYIeF44RT-TmZ5jklYP2F6bPzVWrdR49jojJ8dp3NqTjkYVAMCvfBpwcsnGzS1Cb7XM1Ui-XAIo8ioJ-dgDW4NDeI9txpss/s320/DSC_0067dream.JPG" width="320" /></a></td></tr>
<tr><td class="tr-caption" style="text-align: center;"><span style="font-size: small;">Costa de Arteixo (A Coruña)</span></td></tr>
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<span data-original-attrs="{"style":"mso-bidi-font-weight: bold;"}">Un segundo sector, levantado y conformado por las sierras orientales </span>(Ancares, Caurel, Eixe, Segundeira, Queixa, Xurés, Larouco...), las montañas <strong>septentrionales</strong><span data-original-attrs="{"style":"mso-spacerun: yes;"}"> </span>(Faladoira, Capelada...) y<span data-original-attrs="{"style":"mso-spacerun: yes;"}"> </span>las centro- occidentales o Dorsal gallega (Loba, Cova da Serpe, Faro, Testeiro, Suido, Faro de Avión ...).</div>
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<tr><td style="text-align: center;"><a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEjNwtkMX9YsFRHSYXx8chl31HDkLZ_UTXs157Uq2Shx8cz1jTOjn-HntTmWdZkBzjflPOMWWvdzDw_w32xqg1llM4QREmThUzIsLmJGFLJsafIChRZuZeT-o3Nss_c5xwIrFuYMeNpzJjc/s1600/DSC_0346pic.jpg" imageanchor="1" style="margin-left: auto; margin-right: auto;"><img border="0" data-original-height="251" data-original-width="400" height="200" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEjNwtkMX9YsFRHSYXx8chl31HDkLZ_UTXs157Uq2Shx8cz1jTOjn-HntTmWdZkBzjflPOMWWvdzDw_w32xqg1llM4QREmThUzIsLmJGFLJsafIChRZuZeT-o3Nss_c5xwIrFuYMeNpzJjc/s320/DSC_0346pic.jpg" width="320" /></a></td></tr>
<tr><td class="tr-caption" style="text-align: center;"><span style="font-size: small;">Ancares (Lugo)</span></td></tr>
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<span data-original-attrs="{"style":"mso-bidi-font-weight: bold;"}">Rodean estas sierras a las grandes extensiones en la Galicia interior: la meseta lucense, el NO de Orense, el O de la Dorsal y el<span data-original-attrs="{"style":"mso-spacerun: yes;"}"> </span>centro de la provincia de A Coruña.</span></div>
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<tr><td class="tr-caption" style="text-align: center;"><span style="font-size: small;">A Ulloa (Lugo)</span></td></tr>
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<span data-original-attrs="{"style":"mso-bidi-font-weight: bold;"}">Finalmente, encontramos también <b data-original-attrs="{"style":"mso-bidi-font-weight: normal;"}">fosas tectónicas o depresiones</b>: As Pontes, Sarria y Monforte, Valdeorras, Quiroga, Maceda, Xinzo, Verín....Y la más particular, la depresión Meridiana, de N a S, entre Carballo y Tui.</span></div>
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<tr><td class="tr-caption" style="text-align: center;"><span style="font-size: small;">Depresión meridiana Carballo- Tui desde O Monte Aloia (Tui-Pontevedra)</span></td></tr>
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<b data-original-attrs="{"style":"mso-bidi-font-weight: normal;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;">GLOSARIO:</span></b></div>
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<b data-original-attrs="{"style":"mso-bidi-font-weight: normal;"}">OROGRAFIA</b>: Conjunto de montes de una comarca.</div>
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<b data-original-attrs="{"style":"mso-bidi-font-weight: normal;"}">SEPTENTRIONAL</b>: al Norte.</div>
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<b data-original-attrs="{"style":"mso-bidi-font-weight: normal;"}">FOSA TECTÓNICA</b>: es una larga depresión limitada en ambos lados por fallas entre las cuales el terreno se ha hundido por efecto de fuerzas internas.</div>
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Bibliografía<strong>:</strong></div>
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<span data-original-attrs="{"style":"font-family: \"Book Antiqua\"; mso-bidi-font-size: 18.0pt;"}" style="font-family: "book antiqua";"><span data-original-attrs="{"style":"font-size: x-small;"}" style="font-size: xx-small;">- DERRUAU: <u>Geomorfología</u></span></span></div>
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<span data-original-attrs="{"style":"font-size: x-small;"}" style="font-size: xx-small;"><span data-original-attrs="{"style":"font-family: \"Book Antiqua\"; mso-bidi-font-size: 18.0pt;"}" style="font-family: "book antiqua";">Editorial Ariel, 1991</span> </span></div>
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<span data-original-attrs="{"style":"font-family: \"Book Antiqua\"; mso-bidi-font-size: 18.0pt;"}" style="font-family: "book antiqua";"><span data-original-attrs="{"style":"font-size: x-small;"}" style="font-size: xx-small;">- PÉREZ ALBERTI, A.: <u>Xeografía de Galicia, Tomo I : O</u></span></span></div>
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<span data-original-attrs="{"style":"font-family: \"Book Antiqua\"; mso-bidi-font-size: 18.0pt;"}" style="font-family: "book antiqua";"><span data-original-attrs="{"style":"font-size: x-small;"}" style="font-size: xx-small;">Ed. Sálvora, La Coruña, 1982 </span></span></div>
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<span data-original-attrs="{"style":"font-family: \"Book Antiqua\"; mso-bidi-font-size: 18.0pt;"}" style="font-family: "book antiqua";"><span data-original-attrs="{"style":"font-size: x-small;"}" style="font-size: xx-small;">- V.V.A.A.: <u>Geografía de Galicia, Tomo I</u></span></span></div>
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<span data-original-attrs="{"style":"font-family: \"Book Antiqua\"; mso-bidi-font-size: 18.0pt;"}" style="font-family: "book antiqua";"><span data-original-attrs="{"style":"font-size: x-small;"}" style="font-size: xx-small;">La Opinión, La Coruña, 2000</span></span></div>
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Sonia María García Garcíahttp://www.blogger.com/profile/13489949561200644676noreply@blogger.com0tag:blogger.com,1999:blog-6238152118688223934.post-25055240415843985032020-05-08T02:29:00.002+02:002020-05-08T02:29:58.722+02:00EVOLUCIÓN GEOMORFOLÓGICA DE GALICIA<br />
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<span data-original-attrs="{"style":"mso-bidi-font-size: 18.0pt;"}">Es inevitable hacer un rápido recorrido por la evolución del relieve gallego hasta llegar a ser el escenario de nuestras vidas para entender como Galicia se ha convertido en lo que ven nuestros ojos.</span><span data-original-tag="O:P"></span></div>
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<span data-original-attrs="{"style":"mso-bidi-font-size: 18.0pt;"}">Nuestro viaje comienza hace 2.000 millones de años, llega hasta la actualidad y continuará en el futuro. En aquella época tan lejana, el sector central del actual Macizo Gallego tiene a ambos lados dos surcos marinos no muy profundos que serán rellenados de materiales paleozoicos y antepaleozoicos a lo largo de toda la Era Primaria. Durante la orogenia Herciniana (hace unos 400 millones de años), esos materiales son elevados, plegados o fracturados, surgiendo en la superficie materiales metamórficosy también rocas plutónicas ( granitos ). El territorio gallego se fragmenta en numerosas parcelas siguiendo las fracturas que se producen en este momento. </span></div>
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<tr><td style="text-align: center;"><a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEjj6HU2fh5v17zP8ociXa23a0-3ztNkomBMG2gTJuI_hwarzqHskbYdWUz8E3HU9Aoxteas33C_vv-evI9DKALBFsa_xB4SlRRveVzAFNSnBgWtEUmXDA796Ai7cFIV1FZfxZbC6CYNvS8/s1600/IMGP0051.JPG" imageanchor="1" style="margin-left: auto; margin-right: auto;"><img border="0" data-original-height="346" data-original-width="400" height="345" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEjj6HU2fh5v17zP8ociXa23a0-3ztNkomBMG2gTJuI_hwarzqHskbYdWUz8E3HU9Aoxteas33C_vv-evI9DKALBFsa_xB4SlRRveVzAFNSnBgWtEUmXDA796Ai7cFIV1FZfxZbC6CYNvS8/s400/IMGP0051.JPG" width="400" /></a></td></tr>
<tr><td class="tr-caption" style="text-align: center;"><span style="font-size: small; text-align: left;"> Bolas de granito en Penas de Rodas (Outeiro de Rei- Lugo)</span><br /><br /><br /></td></tr>
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<span style="text-align: justify; text-indent: 20.3pt;">Durante el Secundario todo ello es reducido a llanura.</span><br />
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<span data-original-attrs="{"style":"mso-bidi-font-size: 18.0pt;"}" style="text-align: justify; text-indent: 27.0667px;">Ya en la Era Terciaria, a consecuencia del plegamiento alpino, esta llanura se fractura en todas direcciones. Los materiales situados en la parte oriental son más plásticos (calizas) y se pliegan más que fracturarse. Quedan así bloques escalonados a distintas altitudes. Son éstas mayores en el Este y descienden hacia el Oeste. Estos bloques también van a sufrir erosión y son desequilibrados de nuevo, más o menos al nivel de hoy, en la segunda mitad del Terciario. Aún las montañas más altas que tenemos en Galicia, tienen las cumbres arrasadas. La red fluvial, instalada previamente, irá cortando los bloques según éstos ascienden, mientras que apenas lo hace en los que van descendiendo.</span><br style="text-align: justify; text-indent: 27.0667px;" /><span style="text-align: justify; text-indent: 27.0667px;"> </span><div class="separator" style="clear: both; text-align: center;">
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<tr><td style="text-align: center;"><a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEiKG3AwBWQw0qg7UcLTAdgdlamkxeqXBYLWd2ss98zDT0t-lpM0db9wrou-RAW__dzc9yXspPRjtVee0ukDSD07imj1eaeyO5u7330KSIMqW99y6ch4efv-zUMpvPai-tQyghFl4BohSFs/s1600/DSC_0115.JPG" imageanchor="1" style="margin-left: auto; margin-right: auto;"><img border="0" data-original-height="309" data-original-width="320" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEiKG3AwBWQw0qg7UcLTAdgdlamkxeqXBYLWd2ss98zDT0t-lpM0db9wrou-RAW__dzc9yXspPRjtVee0ukDSD07imj1eaeyO5u7330KSIMqW99y6ch4efv-zUMpvPai-tQyghFl4BohSFs/s1600/DSC_0115.JPG" /></a></td></tr>
<tr><td class="tr-caption" style="text-align: center;"><span style="font-size: small; text-align: justify; text-indent: 27.0667px;">Caliza en O Val das Mouras (O Caurel- Lugo)<br /><br /><br /></span></td></tr>
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<tr><td style="text-align: center;"><img border="0" data-original-height="212" data-original-width="640" height="211" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEihPq7nVrb9WoDgtY5Ozt3_stkeUrj8gYmcJCLKfEp7VXPwdpLLoStr55Va7JtXT3S5yFnPkeFcFZf5paJA1V_nA1d6QwgdalFUAFl1Vf6zBgKIVzjeoYl1a2C9PL5sSJIy4GT5D8Fb01w/s640/DSC_0849.JPG" style="margin-left: auto; margin-right: auto;" width="640" /></td></tr>
<tr><td class="tr-caption" style="text-align: center;"><span style="font-size: small;">Pliegue en Campodola (Quiroga -Lugo)<br /><br /><br /></span></td></tr>
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<tr><td style="text-align: center;"><a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEggOamMLAcQO8qKceQOaR77IL5wPZ9nlkFQFjU45Y2vS5200uvnr35jw2h2mxX0lea4d6QQ8t04lqGgr8-jJ_65yO4t5r8zliJH_rCwZylVOLdnEbQpOOyi7E3y91q49qjozIG2TSNJEvA/s1600/IMGP0082.JPG" imageanchor="1" style="margin-left: auto; margin-right: auto;"><img border="0" data-original-height="266" data-original-width="400" height="212" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEggOamMLAcQO8qKceQOaR77IL5wPZ9nlkFQFjU45Y2vS5200uvnr35jw2h2mxX0lea4d6QQ8t04lqGgr8-jJ_65yO4t5r8zliJH_rCwZylVOLdnEbQpOOyi7E3y91q49qjozIG2TSNJEvA/s320/IMGP0082.JPG" width="320" /></a></td></tr>
<tr><td class="tr-caption" style="text-align: center;"><span style="font-size: small;">Pliegue de Campodola- Leixazós (Quiroga -Lugo)<br /><br /><br /><br /><br /></span></td></tr>
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<span data-original-attrs="{"style":"mso-bidi-font-size: 18.0pt;"}" style="text-align: center; text-indent: 0px;">Durante el Cuaternario se producen fuertes cambios climáticos. Existen períodos muy fríos (</span><span data-original-attrs="{"style":"mso-bidi-font-size: 18.0pt;"}" style="text-align: center; text-indent: 0px;">aparecen huellas de glaciarismo cuaternario sobre las partes más altas de Ancares, Serra Segundeira, Serra de Queixa, Xurés, Courel...), en que los ríos llevan poca agua y el nivel del mar desciende... Y otros períodos más benignos, interglaciares (de los que también hay restos incluso en la costa cantábrica de Galicia), en que se funden los hielos y el mar eleva su nivel. Como consecuencia de esta alternancia, hay momentos de excavación de los ríos y momentos de depósito de materiales. Se forman así terrazas fluviales que aparecen por buena parte de Galicia como testigo de la evolución.</span><span style="text-align: center; text-indent: 0px;"> </span><span data-original-attrs="{"style":"mso-bidi-font-size: 18.0pt;"}" style="text-align: center; text-indent: 0px;">Otras pruebas- testigo de la evolución de Galicia en este período son los campos de bloques ( fragmentados, levantados y movidos por el hielo), ríos de bloques, depósitos de ladera, y está probada la existencia de diversos tipos de glaciares.</span></div>
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<tr><td style="text-align: center;"><a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEjWvZXDvyMJ4UqONyHpKDGZO1IIgITgegn2Q_flm8gvPVz7XkcEAIXs8g8OS0tQPRnShOECITdOwlaoE4hXh_xxMAfTWRJIWX_WZYSimzjYHMdpudN_leZGre8n9X3qlLZUpluqDrU5xVg/s1600/IMGP0064.JPG" imageanchor="1" style="margin-left: auto; margin-right: auto;"><img border="0" data-original-height="256" data-original-width="320" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEjWvZXDvyMJ4UqONyHpKDGZO1IIgITgegn2Q_flm8gvPVz7XkcEAIXs8g8OS0tQPRnShOECITdOwlaoE4hXh_xxMAfTWRJIWX_WZYSimzjYHMdpudN_leZGre8n9X3qlLZUpluqDrU5xVg/s1600/IMGP0064.JPG" /></a></td></tr>
<tr><td class="tr-caption" style="text-align: center;"><span style="font-size: small;">A Devesa de A Rogueira (O Caurel- Lugo) se asienta sobre un antiguo circo glaciar.</span></td></tr>
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<tr><td style="text-align: center;"><a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhDc-UpKfG3Y8jwpPP98Hsjcgp-wclT2Fp1XIcH1K7SDIMcJqNbuGpqnHm-iB2tsXzXVvuJSjLc_8cCfxex5X0aIRzsBRfPkYQL5wzijyUIL8qFKEb3qwDdaWE3K2K5H9-C5CyR029VCRA/s1600/IMGP0105.JPG" imageanchor="1" style="margin-left: auto; margin-right: auto;"><img border="0" data-original-height="175" data-original-width="320" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhDc-UpKfG3Y8jwpPP98Hsjcgp-wclT2Fp1XIcH1K7SDIMcJqNbuGpqnHm-iB2tsXzXVvuJSjLc_8cCfxex5X0aIRzsBRfPkYQL5wzijyUIL8qFKEb3qwDdaWE3K2K5H9-C5CyR029VCRA/s1600/IMGP0105.JPG" /></a></td></tr>
<tr><td class="tr-caption" style="text-align: center;"><span style="font-size: small;">El campo de bloques donde nace el Miño (Meira- Lugo)<br /><br /><br /><br /><br /><br /><br /><br /></span></td></tr>
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<span data-original-attrs="{"style":"mso-bidi-font-size: 18.0pt;"}"><span style="text-indent: 40px;">Es muy importante resaltar el papel de otro agente ajeno a la naturaleza pero igual de importante para la evolución del relieve y el medio: el hombre. La acción antrópica en Galicia es evidente desde hace unos 5.000 años, si no antes. Existe en este momento un retroceso del "quercus" ( roble/" carballo") asociado a un enfriamiento del clima y, además a una deforestación de tipo antrópico. Esta actividad deforestadora es más acusada a partir del Bronce inicial asociada a la roturación de nuevas tierras para el cultivo. Ya en épocas históricas este proceso ha continuado por razones variadas (cultivos, fabricación de papel, exportación de madera, etc....). Estas rozas afectan a las áreas de mayor pendiente porque una vez desprovistas de vegetación son más fáciles de atacar por los procesos morfogenéticos. Sin embargo, también el hombre se ha preocupado de paliar la situación construyendo terrazas, habituales en muchos valles meridionales, que sirven de freno a la evolución del relieve. Construidas de abajo- arriba de los valles, crean escalones artificiales que van deteniendo el descenso del agua por las vertientes y propician la aparición de nuevos suelos.</span></span></div>
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<tr><td style="text-align: center;"><a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEi_RcdK0buQOR_betrKc51chaneikV1oJt-qgBU5OhMrXEeTUCnpSK-6EaF38DjbRTIeP89AXmBuTlP4UXJCrM5xrbxNebhmUSyyU_B8s0-Kb3a6LqR-IehubEI2VBAD91XCStTZ0we0MY/s1600/Valle+del+Mi%25C3%25B1o+03.JPG" imageanchor="1" style="margin-left: auto; margin-right: auto;"><img border="0" data-original-height="220" data-original-width="320" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEi_RcdK0buQOR_betrKc51chaneikV1oJt-qgBU5OhMrXEeTUCnpSK-6EaF38DjbRTIeP89AXmBuTlP4UXJCrM5xrbxNebhmUSyyU_B8s0-Kb3a6LqR-IehubEI2VBAD91XCStTZ0we0MY/s1600/Valle+del+Mi%25C3%25B1o+03.JPG" /></a></td></tr>
<tr><td class="tr-caption" style="text-align: center;"><span style="font-size: small;">Terrazas en la ladera del río Miño<br /><br /><br /></span></td></tr>
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<span data-original-attrs="{"style":"mso-bidi-font-size: 18.0pt;"}"><span data-original-attrs="{"style":"mso-bidi-font-size: 18.0pt;"}" style="text-align: left; text-indent: 0px;">El excesivo pastoreo también influyó en ciertas áreas en que se fuese perdiendo el escaso manto de suelo. Sin embargo, cuando se cultivó el monte, se frenó la evolución del relieve.El cambio de especies autóctonas como el "carballo" (Quercus robur)por otras ajenas como el eucalipto, puede provocar, a largo plazo, la aceleración de los procesos al romper el ciclo biológico. También la construcción de embalses de agua origina una deceleración de la morfogénesis al frenar la excavación de los ríos. Sin embargo, sus riberas cambian muy rápidamente por los ascensos y descensos del nivel del agua.</span><br style="text-align: left; text-indent: 0px;" /><span data-original-attrs="{"style":"mso-bidi-font-size: 18.0pt;"}" style="text-align: left; text-indent: 0px;"></span><span data-original-tag="O:P" style="text-align: left; text-indent: 0px;"></span><br style="text-align: left; text-indent: 0px;" /><div data-original-attrs="{"style":"text-align: justify;"}" style="text-indent: 0px;">
<span data-original-attrs="{"style":"mso-bidi-font-size: 18.0pt;"}">Como vemos, el hombre es un agente a tener en cuenta en la evolución del relieve.</span><br /> </div>
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<span data-original-attrs="{"style":"mso-bidi-font-size: 18.0pt;"}">A modo de resumen de lo expuesto podemos dividir el relieve gallego, de modo general, en tres subunidades:</span><br /><span data-original-tag="O:P"></span> </div>
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<span data-original-attrs="{"style":"mso-bidi-font-size: 18.0pt;"}">- <u>Sectores levantados</u>, cuyo conjunto más importante es la <u>banda oriental</u> con niveles de cumbres entre los 1600- 2000 metros ( Ancares, Caurel, Eixe, Segundeira, Queixa, Xurés, Larouco...) . Las <u>montañas septentrionales </u>con mucha menos altura ( Faladoira, Capelada...) . Las <u>centro-occidentales o Dorsal gallega </u>( Loba, Cova da Serpe, Faro, Testeiro, Suido, Faro de Avión ...) entre los 700- 1.100 metros de altitud.</span><span data-original-tag="O:P"></span></div>
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<span data-original-attrs="{"style":"mso-bidi-font-size: 18.0pt;"}">- <u>Grandes extensiones en la Galicia interior</u>, entre los 400- 600 metros. Meseta lucense, NO de Orense, O de la Dorsal, centro de la provincia de la Coruña.</span><span data-original-tag="O:P"></span></div>
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<span data-original-attrs="{"style":"mso-bidi-font-size: 18.0pt;"}">- <u>Fosas tectónicas</u> : As Pontes, Sarria y Monforte, Valdeorras, Quiroga, Maceda, Xinzo, Verín.... La más particular es la depresión Meridiana, de N a S, entre Carballo y Tui.<span data-original-tag="O:P"></span></span></div>
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Bibliografía:<span data-original-tag="O:P"></span></div>
<span data-original-attrs="{"style":"font-size: x-small;"}" style="font-size: xx-small; text-align: left; text-indent: 0px;"></span><br style="text-align: left; text-indent: 0px;" /><div data-original-attrs="{"style":"margin: 0cm 12pt 0pt;"}" style="margin: 0cm 12pt 0pt; text-align: left; text-indent: 0px;">
<span data-original-attrs="{"style":"font-size: x-small;"}" style="font-size: xx-small;"><span data-original-attrs="{"style":"font-family: \"Book Antiqua\"; mso-bidi-font-size: 18.0pt;"}" style="font-family: "book antiqua";">- DERRUAU: <u>Geomorfología</u></span><span data-original-tag="O:P"></span></span></div>
<span data-original-attrs="{"style":"font-size: x-small;"}" style="font-size: xx-small; text-align: left; text-indent: 0px;"></span><br style="text-align: left; text-indent: 0px;" /><div data-original-attrs="{"style":"margin: 0cm 12pt 0pt; text-indent: 30pt;"}" style="margin: 0cm 12pt 0pt; text-align: left; text-indent: 30pt;">
<span data-original-attrs="{"style":"font-size: x-small;"}" style="font-size: xx-small;"><span data-original-attrs="{"style":"font-family: \"Book Antiqua\"; mso-bidi-font-size: 18.0pt;"}" style="font-family: "book antiqua";">Editorial Ariel, 1991</span></span></div>
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<span data-original-attrs="{"style":"font-size: x-small;"}" style="font-size: xx-small;"><span data-original-attrs="{"style":"font-family: \"Book Antiqua\"; mso-bidi-font-size: 18.0pt;"}" style="font-family: "book antiqua";">- PÉREZ ALBERTI, A.: <u>Xeografía de Galicia, Tomo I : O</u></span><span data-original-tag="O:P"></span></span></div>
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<span data-original-attrs="{"style":"font-size: x-small;"}" style="font-size: xx-small;"><span data-original-attrs="{"style":"font-family: \"Book Antiqua\"; mso-bidi-font-size: 18.0pt;"}" style="font-family: "book antiqua";">Ed. Sálvora, La Coruña, 1982</span><span data-original-tag="O:P"></span></span></div>
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<span data-original-attrs="{"style":"font-size: x-small;"}" style="font-size: xx-small;"><span data-original-attrs="{"style":"font-family: \"Book Antiqua\"; mso-bidi-font-size: 18.0pt;"}" style="font-family: "book antiqua";">- V.V.A.A.: <u>Geografía de Galicia, Tomo I</u></span><span data-original-tag="O:P"></span></span></div>
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<span data-original-attrs="{"style":"font-size: x-small;"}" style="font-size: xx-small;"><span data-original-attrs="{"style":"font-family: \"Book Antiqua\"; mso-bidi-font-size: 18.0pt;"}" style="font-family: "book antiqua";">La Opinión, La Coruña, 2000</span><span data-original-tag="O:P"></span></span></div>
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Sonia María García Garcíahttp://www.blogger.com/profile/13489949561200644676noreply@blogger.com0tag:blogger.com,1999:blog-6238152118688223934.post-5603238163794566992020-05-08T02:04:00.001+02:002020-05-08T02:04:44.944+02:00FACTORES CLIMÁTICOS DE GALICIA<br />
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<span data-original-attrs="{"style":"color: #eeeeee;"}" lang="es"><span style="color: white;">La localización de Galicia en el occidente de Europa y entre el medio templado y el subtropical le confieren una inestabilidad atmosférica particular.</span></span></div>
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<span data-original-attrs="{"style":"color: #eeeeee;"}"><span style="color: white;"><span lang="es">Está sometida a la influencia de la circulación general de las latitudes medias con una gran variabilidad de los estados de la atmósfera. </span><span data-original-attrs="{"style":"font-size: large;"}"><span lang="es"><span data-original-attrs="{"style":"font-size: small;"}">Esta influencia varía </span></span><span lang="es"><span data-original-attrs="{"style":"font-size: small;"}">debido a los factores geográficos regionales y locales.</span></span></span></span></span></div>
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<span data-original-attrs="{"style":"color: #eeeeee;"}"><span style="color: white;"><span lang="es">El relieve y los caracteres térmicos del océano crean nuevas estructuras en las capas bajas de la troposfera, acentuando o atenuando algunos elementos de variabilidad como la desviación de los flujos o las deformaciones de las superficies de continuidad. </span><span lang="es">La temperatura del océano influye en la transferencia de energía océano- atmósfera, creándose situaciones de inestabilidad. </span><span lang="es">El distinto comportamiento océano- continente determina un régimen de brisas marinas que pueden, en el verano, modificar incluso la dirección de los vientos dominantes de la circulación general. Con estas brisas se atenúa el contraste térmico océano- continente y tiende a aumentar la nubosidad.</span></span></span></div>
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<span style="color: white;"><span lang="es"></span><span data-original-attrs="{"style":"color: #eeeeee;"}" lang="es">La disposición meridiana (N- S) del relieve provoca una ralentización de los flujos del O, deformaciones de los frentes y desviaciones de las líneas de corriente. Por ello, las vertientes expuestas a las masas húmedas concentran las precipitaciones y la nubosidad, y las de abrigo y las depresiones interiores aparecen como enclaves alejados de la influencia atlántica.</span></span></div>
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<span style="color: white;"><span lang="es"></span><span data-original-attrs="{"style":"color: #eeeeee;"}"> </span></span></div>
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<span style="color: white;"><span data-original-attrs="{"style":"color: #eeeeee;"}" lang="es">Es tal la influencia de la orografía que Galicia se sitúa, por su relieve, entre las regiones más lluviosas de Europa occidental a pesar de su proximidad a la zona subtropical.</span><br /><span data-original-attrs="{"style":"color: #eeeeee;"}"></span><br /><span data-original-attrs="{"style":"color: #eeeeee;"}">En nuevas entradas del blog, iremos desgranando todos los matices del clima de Galicia.</span></span></div>
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<span data-original-attrs="{"style":"color: #eeeeee;"}" style="color: #eeeeee;">Bibliografía:</span></div>
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<span lang="es"></span><span data-original-attrs="{"style":"color: #eeeeee;"}" style="color: #eeeeee;"> </span><br /><div data-original-attrs="{"style":"margin: 0cm 12pt 0pt; text-align: justify;"}" style="margin: 0cm 12pt 0pt;">
<span data-original-attrs="{"style":"font-family: \"Book Antiqua\"; mso-bidi-font-size: 18.0pt;"}" style="font-family: "book antiqua";"><span data-original-attrs="{"style":"font-size: x-small;"}" style="font-size: xx-small;"><span data-original-attrs="{"style":"color: #eeeeee;"}" style="color: #eeeeee;">- V.V.A.A.: <u>Geografía de Galicia, Tomo I</u></span></span></span></div>
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<span data-original-attrs="{"style":"font-family: \"Book Antiqua\"; mso-bidi-font-size: 18.0pt;"}" style="font-family: "book antiqua";"><span data-original-attrs="{"style":"color: #eeeeee; font-size: x-small;"}" style="color: #eeeeee; font-size: xx-small;">La Opinión, A Coruña, 2000</span></span></div>
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Sonia María García Garcíahttp://www.blogger.com/profile/13489949561200644676noreply@blogger.com0tag:blogger.com,1999:blog-6238152118688223934.post-82235559773019964172020-05-08T01:56:00.000+02:002020-05-08T01:56:59.625+02:00PARQUE DA NATUREZA DO RÍO BAROSA<div class="separator" style="clear: both; text-align: center;">
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<span style="text-align: justify;">En el concello de Barro (Pontevedra), encontramos un conjunto etnográfico- natural de gran valor. Se trata de un conjunto de diecisiete molinos en cascada que aprovechan la fuerza de la caída del agua de las llamadas Fervenzas de Barosa o de Maquieira. Se trata de unos saltos del río Barosa , afluente del Chaín, que, a su vez, desemboca en el Umia. </span><br />
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Estos molinos pertenecieron al Monasterio de San Martiño Pinario de Santiago. Con la desamortización del siglo XIX pasaron a manos de particulares en unos casos, y a ser molinos de maquía en otros. </div>
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Sus "moas" molían maíz y centeno sobre todo, y un par de ellas, trigo. </div>
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El paseo por sus senderos comienza a la altura de la Illa de Barosa y del Muíño de Oubiña, un negocio hostelero que ha respetado la estructura del molino y que está regentado por personas que se preocupan por la conservación del conjunto y por la realización de actividades que dan a conocer el entorno y la utilidad de los molinos. </div>
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<tr><td class="tr-caption" style="text-align: center;"><span style="font-size: small;">Muíño de Oubiña<br /><br /></span></td></tr>
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<tr><td class="tr-caption" style="text-align: center;"><span style="font-size: small;">Muíño de Oubiña</span></td></tr>
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<tr><td class="tr-caption" style="text-align: center;"><span style="font-size: small;">Muíño de Oubiña</span></td></tr>
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<span style="text-align: justify;">En la parte final de la cascada hay una poza hasta la que cae el agua resbalando por grandes rocas planas, pero subiendo por el margen derecho del río, llegamos a otra poza y a una parte de la cascada más vertical de gran belleza. Hasta aquí, los molinos están en el margen izquierdo, después pasan al derecho. </span><br />
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<tr><td class="tr-caption" style="text-align: center;"><span style="font-size: small;">Illa de Barosa</span></td></tr>
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<tr><td class="tr-caption" style="text-align: center;"><span style="font-size: small;">Illa de Barosa</span></td></tr>
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<tr><td class="tr-caption" style="text-align: center;"><span style="font-size: small;">Illa de Barosa<br /></span></td></tr>
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<tr><td style="text-align: center;"><a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhmOnekC7xzr2yr4srRioez0JsB8aQT42PQiwK3P_8ReSEX-CcaZqd7Fr48QZ2zV7uXFkauwdETyP7ANv_Fu33vU7qOjAEnMrzU-O-w-7SFU6mf6UMnD9KiYJn57_NWfcbcKittVSBMXeE/s1600/DSC_0086.JPG" imageanchor="1" style="margin-left: auto; margin-right: auto;"><img border="0" data-original-height="428" data-original-width="640" height="428" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhmOnekC7xzr2yr4srRioez0JsB8aQT42PQiwK3P_8ReSEX-CcaZqd7Fr48QZ2zV7uXFkauwdETyP7ANv_Fu33vU7qOjAEnMrzU-O-w-7SFU6mf6UMnD9KiYJn57_NWfcbcKittVSBMXeE/s640/DSC_0086.JPG" width="640" /></a></td></tr>
<tr><td class="tr-caption" style="text-align: center;"><table align="center" cellpadding="0" cellspacing="0" class="tr-caption-container" data-original-attrs="{"style":"margin-left: auto; margin-right: auto; text-align: center;"}" style="margin-left: auto; margin-right: auto; text-align: center;"><tbody>
<tr><td class="tr-caption" data-original-attrs="{"style":"text-align: center;"}">Uno de esos bancos maravillosos que tiene Galicia<br /></td></tr>
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<tr><td class="tr-caption" style="text-align: center;"><span style="font-size: small;">Pías en las rocas</span></td></tr>
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<tr><td style="text-align: center;"><a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEiHVN3yqotyIxwiUbGDaLkaEspU8mQZyyplwnZnOandP3Fhmjv0FUo37JY8NN-5V7Qq4P_6wTnTJIRDSPbpftfFUS71gpAoH7m5_evC5AZaFU7WLmNw3DqM7hdhuxqc6UtSa5LXmSxiAig/s1600/DSC_0093.JPG" imageanchor="1" style="margin-left: auto; margin-right: auto;"><img border="0" data-original-height="640" data-original-width="428" height="640" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEiHVN3yqotyIxwiUbGDaLkaEspU8mQZyyplwnZnOandP3Fhmjv0FUo37JY8NN-5V7Qq4P_6wTnTJIRDSPbpftfFUS71gpAoH7m5_evC5AZaFU7WLmNw3DqM7hdhuxqc6UtSa5LXmSxiAig/s640/DSC_0093.JPG" width="428" /></a></td></tr>
<tr><td class="tr-caption" style="text-align: center;"><span style="font-size: small;">Aprovechamiento del agua de un molino para otro</span></td></tr>
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<span style="text-align: justify;"><br /></span>
<span style="text-align: justify;">Aguas arriba existe una presa lítica en la que incluso vemos cantidad de grabados, mayormente cruces, pero también de tipo lineal y cazoletas, lo que nos hace pensar en una reutilización de rocas con grabados primitivos, cristianizados con cruces de protección. </span><br />
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<span style="text-align: justify;">En la parte superior, el río va manso y existe allí otra área de esparcimiento. </span><br />
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Se puede bajar por el mismo lado o por el contrario hasta llegar de nuevo a la parte inferior de las cascadas. </div>
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Bien vale una visita con calzado cómodo y ganas de zambullirse en la naturaleza y la Historia. </div>
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Sonia María García Garcíahttp://www.blogger.com/profile/13489949561200644676noreply@blogger.com0tag:blogger.com,1999:blog-6238152118688223934.post-88175101483822456262020-05-08T01:25:00.002+02:002020-05-08T01:25:58.411+02:00LA BERENGUELA<span style="background-color: black; color: #f3f3f3; font-size: 14pt; text-align: justify;"><br /></span>
<span style="background-color: black; color: #f3f3f3; font-size: 14pt; text-align: justify;">Uno de los mayores placeres que se puede disfrutar con la piel de gallina y la emoción en el alma, es encontrarse una tarde- noche de invierno en la Plaza del Obradoiro de Santiago de Compostela, a los pies de la catedral, mientras las nubes descargan su orvallo sobre tí y la campana de la Torre del Reloj da las campanadas de la hora en punto. Cuantas más mejor. Conseguirá que repique también tu corazón.</span><br />
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<a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgDBm8x71AZvaEBC2IKIvbpeRjCgohTcd3icppjcwtg-cINRN-JliK-X5-1zjwel8Acrw3127RYTKsJdjvSLoz3jYX-hPpor38he_vYiAqDbjApbLaB7BpOtbptLDOWCS3IxAVgguBSPxM/s1600/Catedral+024.jpg" imageanchor="1" style="margin-left: 1em; margin-right: 1em;"><img border="0" data-original-height="640" data-original-width="480" height="640" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgDBm8x71AZvaEBC2IKIvbpeRjCgohTcd3icppjcwtg-cINRN-JliK-X5-1zjwel8Acrw3127RYTKsJdjvSLoz3jYX-hPpor38he_vYiAqDbjApbLaB7BpOtbptLDOWCS3IxAVgguBSPxM/s640/Catedral+024.jpg" width="480" /></a></div>
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<span style="color: white;"><span data-original-attrs="{"style":"font-size: 14pt; line-height: 16.8pt; text-align: justify;"}" style="font-size: 14pt; line-height: 16.8pt; text-align: justify;">La Torre del Reloj, también llamada de la Trinidad, o de la Berenguela, se encuentra en la intersección de la plaza de las Platerías y la plaza de la Quintana. Se inició su construcción en</span><span class="apple-converted-space" data-original-attrs="{"style":"font-size: 14pt; line-height: 16.8pt; text-align: justify;"}" style="font-size: 14pt; line-height: 16.8pt; text-align: justify;"> el año 1316 bajo mandato del arzobispo Rodrigo de Padrón </span><span data-original-attrs="{"style":"font-size: 14pt; line-height: 16.8pt; text-align: justify;"}" style="font-size: 14pt; line-height: 16.8pt; text-align: justify;">como torre defensiva y, tras su muerte, continuó la obra el arzobispo Berenguel de Landoira, a quien la Torre y su campana más famosa, deben su nombre.</span></span></div>
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<a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEiMcpEIox_hiZlDnS-G3sy1z269ICLutSXpnodbj0nlO87-jdvECup77CJOKuzriMQppOomm93KOW0B2hsBnUzh1Bx6W3X4aONpY5Qv5prX8BlnGdratnFxYWYvdu8hsL5ojVxGCDu075s/s1600/DSC_0031.JPG" imageanchor="1" style="margin-left: 1em; margin-right: 1em;"><img border="0" data-original-height="640" data-original-width="457" height="640" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEiMcpEIox_hiZlDnS-G3sy1z269ICLutSXpnodbj0nlO87-jdvECup77CJOKuzriMQppOomm93KOW0B2hsBnUzh1Bx6W3X4aONpY5Qv5prX8BlnGdratnFxYWYvdu8hsL5ojVxGCDu075s/s640/DSC_0031.JPG" width="456" /></a></div>
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<span data-original-attrs="{"style":"background-color: black; font-size: 14pt;"}" style="background-color: black; font-size: 14pt;"><span data-original-attrs="{"style":"color: #f3f3f3;"}" style="color: #f3f3f3;"><br /></span></span></div>
<div data-original-attrs="{"style":"background-attachment: initial; background-clip: initial; background-image: initial; background-origin: initial; background-position: initial; background-repeat: initial; background-size: initial; line-height: 16.8pt; margin: 15.6pt 0cm 6pt; text-align: justify;"}" style="line-height: 16.8pt; margin: 15.6pt 0cm 6pt; text-align: justify;">
<span data-original-attrs="{"style":"background-color: black; font-size: 14pt;"}" style="background-color: black; font-size: 14pt;"><span data-original-attrs="{"style":"color: #f3f3f3;"}" style="color: #f3f3f3;"><span data-original-attrs="{"style":"font-size: 14pt; line-height: 16.8pt; text-align: justify;"}" style="font-size: 14pt; line-height: 16.8pt;">Más de trescientos años después, durante el Barroco, el arquitecto Domingo de Andrade prosiguió su construcción, y entre 1676 y 1680, la elevó dos plantas más. Con la utilización de diversas estructuras consiguió un conjunto armonioso con ornamentos vegetales y alusivos a la tradición jacobea, con un coronamiento en forma piramidal y una linterna</span><span class="apple-converted-space" data-original-attrs="{"style":"font-size: 14pt; line-height: 16.8pt; text-align: justify;"}" style="font-size: 14pt; line-height: 16.8pt;"> </span><span data-original-attrs="{"style":"font-size: 14pt; line-height: 16.8pt; text-align: justify;"}" style="font-size: 14pt; line-height: 16.8pt;">como remate final, alcanzando los 72 metros de altura.</span></span></span></div>
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<span data-original-attrs="{"style":"background-color: black; font-size: 14pt;"}" style="background-color: black; font-size: 14pt;"><span data-original-attrs="{"style":"color: #f3f3f3;"}" style="color: #f3f3f3;"><span data-original-attrs="{"style":"font-size: 14pt; line-height: 16.8pt; text-align: justify;"}" style="font-size: 14pt; line-height: 16.8pt;"><br /></span></span></span></div>
<div data-original-attrs="{"style":"background-attachment: initial; background-clip: initial; background-image: initial; background-origin: initial; background-position: initial; background-repeat: initial; background-size: initial; line-height: 16.8pt; margin: 15.6pt 0cm 6pt; text-align: justify;"}" style="line-height: 16.8pt; margin: 15.6pt 0cm 6pt; text-align: justify;">
<span data-original-attrs="{"style":"background-color: black; color: #f3f3f3;"}" style="background-color: black; color: #f3f3f3;"><span data-original-attrs="{"style":"font-size: 14pt;"}" style="font-size: 14pt;">Desgraciadamente, las campanas que escuchamos hoy en día son réplicas de las originales. Con el paso del tiempo, tanto la Berenguela como la campana de los cuartos, sufrieron diversas grietas que afectaron al sonido, y fueron sustituidas en el año 1990 por otras fundidas por la casa </span><span data-original-attrs="{"style":"font-size: 14pt;"}" style="font-size: 14pt;">Eijsbouts en 1989, </span></span><span data-original-attrs="{"style":"font-size: 14pt;"}" style="background-color: black; font-size: 14pt;"><span data-original-attrs="{"style":"background-color: black; color: #f3f3f3;"}" style="color: #f3f3f3;">en sus talleres de Asten (Países Bajos). Quien quiera ver las originales, tendrá que acceder a los Museos de la Catedral, ya que se exponen en el Claustro.</span></span></div>
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<a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgePFPZfe-wR-5u9f-okgx9sqa0-XMh46mezLZsAyai3i1MbGzPaSApOTsKdUsPv0Ib93168XLDJTaBf6OsdDLOFNdNjHZzLMksFstOdY4e2aO5knxQrX7JXRLtEZVTtLX7xDTAVe_mVe4/s1600/berenguela+y+cuartos.jpg" imageanchor="1" style="margin-left: 1em; margin-right: 1em;"><img border="0" data-original-height="293" data-original-width="400" height="234" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgePFPZfe-wR-5u9f-okgx9sqa0-XMh46mezLZsAyai3i1MbGzPaSApOTsKdUsPv0Ib93168XLDJTaBf6OsdDLOFNdNjHZzLMksFstOdY4e2aO5knxQrX7JXRLtEZVTtLX7xDTAVe_mVe4/s320/berenguela+y+cuartos.jpg" width="320" /></a></div>
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<span data-original-attrs="{"style":"background-color: black; font-size: 14pt;"}" style="background-color: black; font-size: 14pt;"><span data-original-attrs="{"style":"color: #f3f3f3;"}" style="color: #f3f3f3;"><div class="MsoNormal" data-original-attrs="{"style":"background-attachment: initial; background-clip: initial; background-image: initial; background-origin: initial; background-position: initial; background-repeat: initial; background-size: initial; margin-bottom: 7.5pt;"}" style="color: black; font-size: medium; margin-bottom: 7.5pt; text-align: left;">
<span data-original-attrs="{"style":"background-color: black; color: #f3f3f3;"}" style="color: #f3f3f3;"><span data-original-attrs="{"style":"font-size: 14pt; line-height: 16.8pt; text-align: justify;"}" style="font-size: 14pt; line-height: 16.8pt; text-align: justify;">La Berenguela original fue fundida en el </span><span data-original-attrs="{"style":"font-size: 14pt; line-height: 16.8pt; text-align: justify;"}" style="font-size: 14pt; line-height: 16.8pt; text-align: justify;">año <span class="apple-converted-space"> </span>1729<span class="apple-converted-space"> </span>por Güemes Sampedro, un famoso fundidor de la época. Pesa casi<span class="apple-converted-space"> </span>diez toneladas, su diámetro es de 256 cm. y la altura de<span class="apple-converted-space"> </span>216 cm. Su afinación es en "Do".</span></span></div>
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<span data-original-attrs="{"style":"background-color: black; color: #f3f3f3;"}" style="color: #f3f3f3;"><span data-original-attrs="{"style":"font-size: 14pt; line-height: 16.8pt; text-align: justify;"}" style="font-size: 14pt; line-height: 16.8pt; text-align: justify;"><br /></span></span></div>
<div class="MsoNormal" data-original-attrs="{"style":"background-attachment: initial; background-clip: initial; background-image: initial; background-origin: initial; background-position: initial; background-repeat: initial; background-size: initial; margin-bottom: 7.5pt; text-align: justify;"}" style="color: black; font-size: medium; margin-bottom: 7.5pt;">
<span data-original-attrs="{"style":"background-color: black; font-size: 14pt;"}" style="font-size: 14pt;"><span data-original-attrs="{"style":"color: #f3f3f3;"}" style="color: #f3f3f3;">Está decorada con una cruz patriarcal con el calvario de Jesucristo, un cuadro sobre la batalla de Clavijo (la famosa en la que se atribuye la participación del “Santiago Matamoros”), una representación del sepulcro de Santiago con siete velas encima, una concha de vieira (símbolo de los peregrinos) y otros motivos.<span data-original-tag="O:P"></span></span></span></div>
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<span data-original-attrs="{"style":"background-color: black; font-size: 14pt;"}" style="font-size: 14pt;"><span data-original-attrs="{"style":"color: #f3f3f3;"}" style="color: #f3f3f3;"><br /></span></span></div>
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<div class="MsoNormal" data-original-attrs="{"style":"background-attachment: initial; background-clip: initial; background-image: initial; background-origin: initial; background-position: initial; background-repeat: initial; background-size: initial; margin-bottom: 7.5pt; text-align: justify;"}" style="color: black; font-size: medium; margin-bottom: 7.5pt;">
<span data-original-attrs="{"style":"background-color: black; font-size: 14pt;"}" style="font-size: 14pt;"><span data-original-attrs="{"style":"color: #f3f3f3;"}" style="color: #f3f3f3;">La campana original que tocaba los cuartos fue fundida por el mismo artesano que la Berenguela y en el mismo año. En su caso pesa casi dos toneladas, su diámetro, al igual que la altura están en torno a los 150 centímetros. Está afinada en "Sol".</span></span></div>
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<a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhGetP6mdFvI14YDeRKx5VgwKknHKRVsDL9r3PiPBqrOKMBxM63jSBBnhcBK1eLJa-FWyUb9BT9Vq7mHk7bsPN27e7nrV4KoeZgd27RD8QEBoNC93exUC9_WffP5Dv6K6v5ZuwntJ41Ab0/s1600/DSC_0086.JPG" imageanchor="1" style="margin-left: 1em; margin-right: 1em;"><img border="0" data-original-height="640" data-original-width="428" height="640" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhGetP6mdFvI14YDeRKx5VgwKknHKRVsDL9r3PiPBqrOKMBxM63jSBBnhcBK1eLJa-FWyUb9BT9Vq7mHk7bsPN27e7nrV4KoeZgd27RD8QEBoNC93exUC9_WffP5Dv6K6v5ZuwntJ41Ab0/s640/DSC_0086.JPG" width="428" /></a></div>
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<span data-original-attrs="{"style":"background-color: black; font-size: 14pt;"}" style="background-color: black; font-size: 14pt;"><span data-original-attrs="{"style":"color: #f3f3f3;"}" style="color: #f3f3f3;"><span style="font-size: 18.6667px;">El reloj fue construido en</span><span class="apple-converted-space" style="font-size: 18.6667px;"> </span><span style="font-size: 18.6667px;">1831</span><span class="apple-converted-space" style="font-size: 18.6667px;"> en Ferrol por Andrés Antelo, </span><span style="font-size: 18.6667px;">por encargo del Arzobispo Rafael Vélez. Consta de cuatro esferas, que van orientadas según los puntos cardinales, en cada cara de la Torre. Una de las mayores peculiaridades del reloj, es que</span><span class="apple-converted-space" style="font-size: 18.6667px;"> </span><span style="font-size: 18.6667px;">cuenta con sólo una aguja. Las horas las da la campana Berenguela y los cuartos la otra más pequeña.</span></span></span></div>
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<a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEj5h6E7GdOib-8fl00QSLoZKpdKyOCBeyvucxO2-y79y1PDH7Bg9W7gU-HX6YtjNlfmOPourAcMHZ5nsP9a-cKoD6gRWy_GEdweiwjN4xAmn9HIJD2jPcnH039yeKJe5sGm7d7uOhiQLjo/s1600/DSC_0092+%25282%2529.JPG" imageanchor="1" style="margin-left: 1em; margin-right: 1em;"><img border="0" data-original-height="640" data-original-width="428" height="640" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEj5h6E7GdOib-8fl00QSLoZKpdKyOCBeyvucxO2-y79y1PDH7Bg9W7gU-HX6YtjNlfmOPourAcMHZ5nsP9a-cKoD6gRWy_GEdweiwjN4xAmn9HIJD2jPcnH039yeKJe5sGm7d7uOhiQLjo/s640/DSC_0092+%25282%2529.JPG" width="428" /></a></div>
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<div data-original-attrs="{"style":"background-attachment: initial; background-clip: initial; background-image: initial; background-origin: initial; background-position: initial; background-repeat: initial; background-size: initial; line-height: 16.8pt; margin: 15.6pt 0cm 6pt; text-align: justify;"}" style="line-height: 16.8pt; margin: 15.6pt 0cm 6pt; text-align: justify;">
<span data-original-attrs="{"style":"font-size: 14pt; line-height: 16.8pt;"}" style="background-color: black; color: #f3f3f3; font-size: 14pt; line-height: 16.8pt;">Cuenta la leyenda</span><span data-original-attrs="{"style":"font-size: 14pt; line-height: 16.8pt;"}" style="background-color: black; color: #f3f3f3; font-size: 14pt; line-height: 16.8pt;"> </span><span data-original-attrs="{"style":"font-size: 14pt; line-height: 16.8pt;"}" style="background-color: black; color: #f3f3f3; font-size: 14pt; line-height: 16.8pt;">que si alguna medianoche en vez de tocar doce campanadas la Berenguela toca trece, el demonio gozará de una hora mágica para andar suelto por toda la ciudad…</span></div>
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Sonia María García Garcíahttp://www.blogger.com/profile/13489949561200644676noreply@blogger.com0tag:blogger.com,1999:blog-6238152118688223934.post-57174928230487023512020-05-08T01:15:00.000+02:002020-05-08T01:15:16.175+02:00BALEIRA Y FRAGA DA MARRONDA<div class="separator" style="clear: both; text-align: center;">
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<span style="text-align: justify;">Baleira es un concello de 168.15 kilómetros cuadrados situado en el sector oriental de la provincia de Lugo. Tiene doce parroquias y una de las densidades de población más bajas de Galicia. Su relieve es montañoso con grandes contrastes entre sierras y valles. Además, nacen en él dos ríos que vierten a distintas cuencas: el Eo (vertiente cantábrica) y el Neira (afluente del Miño). La temperatura media es baja y la oscilación térmica elevada pero no es un lugar muy lluvioso, más menos 1000 mm. , en invierno en forma de nieve.</span><br />
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La base económica del municipio es el sector primario tanto en su faceta agrícola como, sobre todo, en la ganadería bovina. Otra fuente de ingresos es la explotación forestal de pino. Sólo en O Cádabo hay un cierto sector terciario por concentrarse allí, como capital, todos los servicios.</div>
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Pero la gran riqueza biológica del municipio se concentra en la Fraga da Marronda (parte de ella se encuentra también en el municipio aledaño de A Fonsagrada).</div>
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<a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhmzyVfAK0es7_pqB6BIT2LKicGgo_faPho2_PKkLJWYIsQ1PWHv2FBEUozDbbupG6-6KoNtyLSznv46z2VnGGkTH-XE5SV-Izx1pJWPniYeTXYiIWYQmyor2RKVhPQkjHGF_hkT42SM1U/s1600/DSC_0350.JPG" imageanchor="1" style="margin-left: 1em; margin-right: 1em;"><img border="0" data-original-height="320" data-original-width="218" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhmzyVfAK0es7_pqB6BIT2LKicGgo_faPho2_PKkLJWYIsQ1PWHv2FBEUozDbbupG6-6KoNtyLSznv46z2VnGGkTH-XE5SV-Izx1pJWPniYeTXYiIWYQmyor2RKVhPQkjHGF_hkT42SM1U/s1600/DSC_0350.JPG" /></a></div>
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El bosque de A Marronda es una gran extensión de frondosas en un excepcional estado de conservación que alcanza una superficie de 1.221, 97 ha., y cuenta con la especial y excepcional presencia de hayas.</div>
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<tr><td class="tr-caption" style="text-align: center;"><span style="font-size: small;">Serbal de cazadores (<i>Sorbus aucuparia</i>)</span></td></tr>
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Hayas (<i>Fagus sylvatica</i>) en su límite suroccidental de Europa.</div>
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<tr><td class="tr-caption" style="text-align: center;"><span style="font-size: small;">Acebo (<i>Ilex aquifolium)</i></span></td></tr>
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<span style="text-align: justify;">Y muchas más especies como robles, avellanos, abedules, manzanos y perales bravos, castaños, arces, uces, arándanos, hiedras, silvas, piornos, helechos y un gran etcétera.</span></div>
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<span style="text-align: justify;">También es muy importante su fauna con ejemplares de: salamandras, sapos, ranas, lagartijas, serpientes...Aves rapaces como el azor, gavilán, águila caudal, halcones... Nocturnas como el cárabo. O pequeños pajarillos como herrerillos, pimpín, petirrojo real, verderolo...o no tan pequeños como el cuervo o la urraca...También multitud de mamíferos como ardillas, lirón careto, ratones de campo, marta, garduña, zorro, gato montés, entre otros. Incluso, de vez en cuando, se pasea por ella el oso.</span></div>
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<tr><td class="tr-caption" style="text-align: center;"><span style="font-size: small;">Cuarcitas de A Lastra<br /><br /></span></td></tr>
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<tr><td class="tr-caption" style="text-align: center;"><span style="font-size: small;">Valle del nacimiento del río Eo<br /><br /></span><div data-original-attrs="{"style":"text-align: center;"}" style="font-size: medium;">
ESTA ENTRADA ESTÁ DEDICADA</div>
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A MI BUEN AMIGO NACIDO EN BALEIRA</div>
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MANUEL PIN (D.E.P.)</div>
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Sonia María García Garcíahttp://www.blogger.com/profile/13489949561200644676noreply@blogger.com0tag:blogger.com,1999:blog-6238152118688223934.post-58808982172371390112020-05-08T00:58:00.000+02:002020-05-08T00:58:42.048+02:00BARRIO MARINERO DE FONTÁN<div class="separator" style="clear: both; text-align: center;">
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<span style="text-align: justify;">Las antiguas casas marineras del barrio de Fontán (Sada- A Coruña), forman un conjunto singular. </span><br />
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Se trata de viviendas estrechas que destacan por el colorido y contrastes de sus fachadas, todas ellas sencillas pero encantadoras. </div>
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<tr><td class="tr-caption" style="text-align: center;">Artesanía marinera</td></tr>
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<tr><td class="tr-caption" style="text-align: center;">Hórreo<br /><br /><br /><br /><div style="text-align: left;">
<span style="font-size: small; text-align: center;">En una villa marinera no pueden faltar los gatos de los vecinos:</span></div>
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<span style="text-align: justify;">En la parte Norte del barrio existieron dos castillos. Hoy nos queda como recuerdo, la batería del Castillo de Fontán que se construyó en el siglo XVIII para proteger las industrias de la villa: salazones de sardina y la fábrica de textiles que surtía de telas y cordeles a la Armada Real, recibiendo grandes privilegios por parte del rey Carlos II. </span></div>
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A su lado queda un lugar cargado de leyendas de túneles y riquezas: a Cova D´anca, a los pies de la foto.</div>
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El barrio de Fontán merece un paseo detenido. Pasar sus calles peatonales, además de gozar de las vistas sobre el puerto y la ría, son un ejercicio de acercamiento a nuestro barrios gremiales tradicionales, a nuestra historia y un relax para nuestros, a veces, castigados sentidos.<br /></div>
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Sonia María García Garcíahttp://www.blogger.com/profile/13489949561200644676noreply@blogger.com0tag:blogger.com,1999:blog-6238152118688223934.post-25033133455043567872020-05-08T00:40:00.001+02:002020-05-08T00:40:35.270+02:00PONTE DO PORCO<br />
<span style="text-align: justify;">A Ponte do Porco (Miño- A Coruña), situada sobre el Río Lambre, guarda una leyenda que a continuación os contaré.</span><br />
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Don Nuno Freire de Andrade tenía un mozo, llamado Roxín por el color rojo de su cabello, que se enamoró de la hija de éste, Teresa, siendo correspondido. Dándose cuanta el padre de la relación entre ambos jóvenes y de la inconveniencia de ésta, entregó a Roxín una bolsa con una gran cantidad de monedas de oro y lo envió a recorrer el mundo.</div>
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Roxín le pidió a Don Nuno que le dejase quedar en el castillo de Pontedeume pero el señor se negó. Le pidió quedarse entonces en el castillo de A Nogueirosa, cerca de Pontedeume, cosa que sí aceptó Don Nuno. Quiso aprovechar el preocupado padre la marcha de Roxín para casar rápidamente a su hija con Enrique de Osorio a pesar de la oposición de la chica.</div>
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<span style="text-align: justify;">En aquellos tiempos, un gran jabalí asolaba los contornos y Don Nuno organizó una cacería para intentar capturarlo, cosa imposible hasta entonces. Invitó a Don Enrique y éste pidió a Teresa que lo acompañara. Ella no aceptó de buena gana pero ante su insistencia fue con él. El jabalí se hacía de rogar, no aparecía, y estando la pareja sobe el puente del río Lambre, vieron como el jabalí venía hacia ellos a gran velocidad. Enrique disparó una flecha al jabalí pero éste continuaba su carrera y amedrentado Don Enrique saltó del puente abajo dejando sola a Teresa, que murió por la embestida del animal, huyendo rápidamente a su vez.</span></div>
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<span style="text-align: center;">Días más tarde, encontraron un jabalí muerto en aquel puente con una daga clavada en la garganta.</span></div>
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<span style="text-align: justify;">Nuno Freire fue a verlo y se dio cuenta de que la daga era suya y que se la había regalado hacía tiempo a Roxín Roxal. Y pensó entonces, que el joven nunca jamás habría abandonado a su hija.</span></div>
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Una escultura en el lugar representa el jabalí de la casa de Andrade.</div>
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<span data-original-attrs="{"style":"font-size: x-small;"}" style="font-size: xx-small;">BIBLIOGRAFÍA:</span><br /><span data-original-attrs="{"style":"font-size: x-small;"}" style="font-size: xx-small;"></span><br /><span data-original-attrs="{"style":"font-size: x-small;"}" style="font-size: xx-small;">- VAQUEIRO, Vítor: Guía da Galiza Máxica</span><br /><span data-original-attrs="{"style":"font-size: x-small;"}" style="font-size: xx-small;"> Ed. Galaxia, Vigo, 1998</span></div>
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Sonia María García Garcíahttp://www.blogger.com/profile/13489949561200644676noreply@blogger.com0tag:blogger.com,1999:blog-6238152118688223934.post-52389093295668456652020-05-08T00:34:00.001+02:002020-05-08T00:34:23.860+02:00MOLINO DE XUVIA Y SUS AVES<br />
<span style="text-align: justify;">El río Xuvia nace en los Montes da Serra, a 460 metros de altitud cerca de Tafornelos en el concello de As Somozas. Recorre 31 kilómetros antes de desembocar entre Xuvia (Narón- A Coruña) y Santa Maria de Neda (Neda- A Coruña), en el fondo de la Ría de Ferrol y bajo el puente de los Andrade.</span><br />
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En sus aguas observamos, sólo en un pequeño paseo, diversidad de especies de aves, lo que nos deja bien claro la importancia de este ecosistema. Observamos gaviotas como la patiamarilla y la reidora:</div>
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<span style="text-align: left;">Azulones:</span></div>
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<span style="text-align: left;">Otros tipos de patos:</span></div>
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<span style="text-align: left;">O la preciosa garza real:</span></div>
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Pero, sin duda, la figura destacada es la del molino construido a finales del siglo XVIII por franceses dedicados a la fabricación de harina. En 1858 era el principal molino del país en capacidad de molienda. Recibía el grano en barcos del Báltico, de América y de Santander, a la vez que producía el pan para todos los barcos que salían desde Ferrol. Años más tarde, llegó a mover una fábrica de papel, una de tejidos y una de laminados de cobre.</div>
<br style="text-align: left;" /><span style="text-align: left;">Detalle del molino y su presa:</span></div>
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<span style="text-align: left;">Plano más general:</span></div>
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Sonia María García Garcíahttp://www.blogger.com/profile/13489949561200644676noreply@blogger.com0tag:blogger.com,1999:blog-6238152118688223934.post-62751212685204124692020-05-07T23:59:00.000+02:002020-05-07T23:59:42.785+02:00LA LÍRICA GALAICO- PORTUGUESA<br />
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<span style="color: white;"><span data-original-attrs="{"style":"color: #cccccc; font-family: Times, \"Times New Roman\", serif; font-size: large;"}" style="font-family: times, "times new roman", serif; font-size: medium;">El <b>gallego</b> nace como lengua romance entre los siglos IX- XII frente al latín (lengua de las élites y de la cultura escrita). Deriva del latín vulgar de uso popular y transmisión oral y se impone como lengua literaria en las cortes peninsulares a partir el siglo XII por su calidad lírica. Su máximo apogeo llega a mediados del siglo XIII en la corte de Alfonso X el Sabio.</span><br /><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-tag="O:P"></span></span><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif; font-size: large;"}" style="font-family: times, "times new roman", serif; font-size: medium;"> </span></span></div>
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<span style="color: white;"><span data-original-attrs="{"style":"color: #cccccc; font-family: Times, \"Times New Roman\", serif; font-size: large;"}" style="font-family: times, "times new roman", serif; font-size: medium;"></span></span></div>
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<span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><span style="color: white;">Existe en Galicia una tradición literaria oral y popular desde la época de los reyes suevos en que los juglares animan los convites con danzas y cantos (poco conocida por ser ágrafa), con temáticas rurales y marineras, gallegas. A ésta se unen las influencias provenzales que llegan a través del Camino de Santiago con temas más cortesanos. Con todo ello se forma una <b>lírica galaico - portuguesa</b> muy rica y variada de la que, lamentablemente, sólo nos ha llegado una pequeña parte en forma, principalmente, de <i>"Cancioneiros</i>". Los más importantes son los de <i>Ajuda</i>, <i>da Vaticana</i>, <i>de la Biblioteca</i> <i>Nacional</i> y <i>el de Berkeley</i>.</span></span></span></span></div>
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<span style="color: white;"><span style="font-family: times, "times new roman", serif; font-size: medium; text-align: justify;">Figuras como la del </span><i style="font-family: times, "times new roman", serif; font-size: large; text-align: justify;">trovador</i><span style="font-family: times, "times new roman", serif; font-size: medium; text-align: justify;"> (noble músico), el</span><i style="font-family: times, "times new roman", serif; font-size: large; text-align: justify;"> segrel</i><span style="font-family: times, "times new roman", serif; font-size: medium; text-align: justify;"> (escudero o hidalgo poeta- cantor),el </span><i style="font-family: times, "times new roman", serif; font-size: large; text-align: justify;">juglar</i><span style="font-family: times, "times new roman", serif; font-size: medium; text-align: justify;"> (villano cantor), el</span><i style="font-family: times, "times new roman", serif; font-size: large; text-align: justify;"> menestrel</i><span style="font-family: times, "times new roman", serif; font-size: medium; text-align: justify;"> o la</span><i style="font-family: times, "times new roman", serif; font-size: large; text-align: justify;"> soldadeira</i><span style="font-family: times, "times new roman", serif; font-size: medium; text-align: justify;"> ( mujeres que acompañan a los juglares), se encargan de transmitir esta literatura con su voz y su música a través de su forma por excelencia: </span><b style="font-family: times, "times new roman", serif; font-size: large; text-align: justify;">la cantiga.</b></span><br />
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<div data-original-attrs="{"style":"text-align: justify;"}" style="text-align: justify;">
<span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><span style="color: white;"><br /></span></span></span></span></div>
<div data-original-attrs="{"style":"text-align: justify;"}" style="text-align: justify;">
<span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><span style="color: white;">La <b>cantiga de amigo </b>es la adopción culta de una forma de carácter popular, antigua y autóctona en la que el papel protagonista lo tiene una mujer desgraciada en el amor que lamenta la partida de su enamorado. Se trata de un amor natural y espontáneo ambientado en el campo, la ciudad o al lado del mar. La mujer siente empatía con la naturaleza y dialoga con ella. Se trata de unas cantigas de gran musicalidad a base de paralelismos y leixaprén. Es el género cultivado por nuestros más grandes cantores: Martín Códax, Mendinho, Xoán de Cangas...</span></span></span></span></div>
<div data-original-attrs="{"style":"text-align: justify;"}" style="text-align: justify;">
<span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><span style="color: white;"><br /></span></span></span></span></div>
<div data-original-attrs="{"style":"text-align: justify;"}" style="text-align: justify;">
<span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><span style="color: white;"><br /></span></span></span></span></div>
<div data-original-attrs="{"style":"text-align: justify;"}" style="text-align: center;">
<span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><span style="color: white;"><div align="center" data-original-attrs="{"style":"text-align: center;"}" style="font-family: "Times New Roman"; font-size: medium;">
<span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><em><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;">Ondas do mar de Vigo,</span></span></em></span><br /><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><em><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><span data-original-tag="O:P"></span></span></span></em></span> </div>
<div class="separator" data-original-attrs="{"style":"clear: both; text-align: center;"}" style="clear: both; font-family: "Times New Roman"; font-size: medium;">
<span data-original-attrs="{"style":"color: #cccccc; font-family: Times, \"Times New Roman\", serif; font-size: large;"}" style="font-family: times, "times new roman", serif; font-size: medium;"><em></em></span><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><em><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;">Se vistes meu amigo</span></span></em></span></div>
<div class="separator" data-original-attrs="{"style":"clear: both; text-align: center;"}" style="clear: both; font-family: "Times New Roman"; font-size: medium;">
<span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><em><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><span data-original-tag="O:P"></span></span></span></em></span> </div>
<div class="separator" data-original-attrs="{"style":"clear: both; text-align: center;"}" style="clear: both; font-family: "Times New Roman"; font-size: medium;">
<span data-original-attrs="{"style":"color: #cccccc; font-family: Times, \"Times New Roman\", serif; font-size: large;"}" style="font-family: times, "times new roman", serif; font-size: medium;"><em></em></span><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><em><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;">e, ai Deus, se verrá cedo!</span></span></em></span></div>
<div class="separator" data-original-attrs="{"style":"clear: both; text-align: center;"}" style="clear: both; font-family: "Times New Roman"; font-size: medium;">
<span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><em><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><span data-original-tag="O:P"></span></span></span></em></span> </div>
<div class="separator" data-original-attrs="{"style":"clear: both; text-align: center;"}" style="clear: both; font-family: "Times New Roman"; font-size: medium;">
<span data-original-attrs="{"style":"color: #cccccc; font-family: Times, \"Times New Roman\", serif; font-size: large;"}" style="font-family: times, "times new roman", serif; font-size: medium;"><em></em></span><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><em><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;">Ondas do mar levado,</span></span></em></span></div>
<div class="separator" data-original-attrs="{"style":"clear: both; text-align: center;"}" style="clear: both; font-family: "Times New Roman"; font-size: medium;">
<span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><em><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><span data-original-tag="O:P"></span></span></span></em></span> </div>
<div class="separator" data-original-attrs="{"style":"clear: both; text-align: center;"}" style="clear: both; font-family: "Times New Roman"; font-size: medium;">
<span data-original-attrs="{"style":"color: #cccccc; font-family: Times, \"Times New Roman\", serif; font-size: large;"}" style="font-family: times, "times new roman", serif; font-size: medium;"><em></em></span><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><em><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;">Se vistes meu amado</span></span></em></span></div>
<div class="separator" data-original-attrs="{"style":"clear: both; text-align: center;"}" style="clear: both; font-family: "Times New Roman"; font-size: medium;">
<span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><em><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><span data-original-tag="O:P"></span></span></span></em></span> </div>
<div class="separator" data-original-attrs="{"style":"clear: both; text-align: center;"}" style="clear: both; font-family: "Times New Roman"; font-size: medium;">
<span data-original-attrs="{"style":"color: #cccccc; font-family: Times, \"Times New Roman\", serif; font-size: large;"}" style="font-family: times, "times new roman", serif; font-size: medium;"><em></em></span><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><em><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;">e, ai Deus, se verrá cedo!</span></span></em></span></div>
<div class="separator" data-original-attrs="{"style":"clear: both; text-align: center;"}" style="clear: both; font-family: "Times New Roman"; font-size: medium;">
<span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><em><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><span data-original-tag="O:P"></span></span></span></em></span> </div>
<div class="separator" data-original-attrs="{"style":"clear: both; text-align: center;"}" style="clear: both; font-family: "Times New Roman"; font-size: medium;">
<span data-original-attrs="{"style":"color: #cccccc; font-family: Times, \"Times New Roman\", serif; font-size: large;"}" style="font-family: times, "times new roman", serif; font-size: medium;"><em></em></span><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><em><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;">Se vistes meu amigo,</span></span></em></span></div>
<div class="separator" data-original-attrs="{"style":"clear: both; text-align: center;"}" style="clear: both; font-family: "Times New Roman"; font-size: medium;">
<span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><em><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><span data-original-tag="O:P"></span></span></span></em></span> </div>
<div class="separator" data-original-attrs="{"style":"clear: both; text-align: center;"}" style="clear: both; font-family: "Times New Roman"; font-size: medium;">
<span data-original-attrs="{"style":"color: #cccccc; font-family: Times, \"Times New Roman\", serif; font-size: large;"}" style="font-family: times, "times new roman", serif; font-size: medium;"><em></em></span><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><em><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;">o por que eu sospiro</span></span></em></span></div>
<div class="separator" data-original-attrs="{"style":"clear: both; text-align: center;"}" style="clear: both; font-family: "Times New Roman"; font-size: medium;">
<span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><em><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><span data-original-tag="O:P"></span></span></span></em></span> </div>
<div class="separator" data-original-attrs="{"style":"clear: both; text-align: center;"}" style="clear: both; font-family: "Times New Roman"; font-size: medium;">
<span data-original-attrs="{"style":"color: #cccccc; font-family: Times, \"Times New Roman\", serif; font-size: large;"}" style="font-family: times, "times new roman", serif; font-size: medium;"><em></em></span><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><em><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;">e, ai Deus, se verrá cedo!</span></span></em></span></div>
<div class="separator" data-original-attrs="{"style":"clear: both; text-align: center;"}" style="clear: both; font-family: "Times New Roman"; font-size: medium;">
<span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><em><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><span data-original-tag="O:P"></span></span></span></em></span> </div>
<div class="separator" data-original-attrs="{"style":"clear: both; text-align: center;"}" style="clear: both; font-family: "Times New Roman"; font-size: medium;">
<span data-original-attrs="{"style":"color: #cccccc; font-family: Times, \"Times New Roman\", serif; font-size: large;"}" style="font-family: times, "times new roman", serif; font-size: medium;"><em></em></span><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><em><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;">Se vistes meu amado,</span></span></em></span></div>
<div class="separator" data-original-attrs="{"style":"clear: both; text-align: center;"}" style="clear: both; font-family: "Times New Roman"; font-size: medium;">
<span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><em><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><span data-original-tag="O:P"></span></span></span></em></span> </div>
<div class="separator" data-original-attrs="{"style":"clear: both; text-align: center;"}" style="clear: both; font-family: "Times New Roman"; font-size: medium;">
<span data-original-attrs="{"style":"color: #cccccc; font-family: Times, \"Times New Roman\", serif; font-size: large;"}" style="font-family: times, "times new roman", serif; font-size: medium;"><em></em></span><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><em><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;">por que hei gram coidado</span></span></em></span></div>
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<span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><em><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><span data-original-tag="O:P"></span></span></span></em></span> </div>
<div class="separator" data-original-attrs="{"style":"clear: both; text-align: center;"}" style="clear: both; font-family: "Times New Roman"; font-size: medium;">
<span data-original-attrs="{"style":"color: #cccccc; font-family: Times, \"Times New Roman\", serif; font-size: large;"}" style="font-family: times, "times new roman", serif; font-size: medium;"><em></em></span><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><em><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;">e, ai Deus,se verrá cedo!</span></span></em></span></div>
<span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-size: small; text-align: left;"><em><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><span data-original-tag="O:P"></span></span></span></em></span><br style="font-family: "Times New Roman"; font-size: medium; text-align: left;" /><div class="separator" data-original-attrs="{"style":"clear: both; text-align: center;"}" style="clear: both; font-family: "Times New Roman"; font-size: medium;">
<span data-original-attrs="{"style":"color: #cccccc; font-family: Times, \"Times New Roman\", serif; font-size: large;"}" style="font-family: times, "times new roman", serif; font-size: medium;"><em></em></span></div>
<div align="center" data-original-attrs="{"style":"text-align: center;"}" style="font-family: "Times New Roman"; font-size: medium;">
<span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><em><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;">MARTÍN CÓDAX<span data-original-tag="O:P"></span></span></span></em></span></div>
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<span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><em><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><br /></span></span></em></span></div>
</span></span></span></span></div>
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<span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><span style="color: white;"><br /></span></span></span></span></div>
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<a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEiX-d3sH7fRt89-Pbhc-saWK9OpRB052Cb_XUderBUGSTAj4RqGgS46KnlesvnoSXZIvZ5yB-VFR3Twep0UGlyR6E3rPz2PWm_OCyyhVjis43EBtgl7PRr0EcBB6v5GAsCV90ZV2uD9s0A/s1600/4.JPG" imageanchor="1" style="margin-left: 1em; margin-right: 1em;"><span style="color: white;"><img border="0" data-original-height="240" data-original-width="320" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEiX-d3sH7fRt89-Pbhc-saWK9OpRB052Cb_XUderBUGSTAj4RqGgS46KnlesvnoSXZIvZ5yB-VFR3Twep0UGlyR6E3rPz2PWm_OCyyhVjis43EBtgl7PRr0EcBB6v5GAsCV90ZV2uD9s0A/s1600/4.JPG" /></span></a></div>
<div data-original-attrs="{"style":"text-align: justify;"}" style="text-align: justify;">
<span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><span style="color: white;"><br /></span></span></span></span></div>
<div data-original-attrs="{"style":"text-align: justify;"}" style="text-align: justify;">
<span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><span style="color: white;"><br /></span></span></span></span></div>
<div data-original-attrs="{"style":"text-align: justify;"}" style="text-align: justify;">
<span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><span style="color: white;">La <b>cantiga de amor </b>se desvía hacia las fórmulas de amor cortesano y cortés de influencia provenzal. El protagonista es un hombre que se dirige a la mujer idealizada o reflexiona sobre ella. Es un tipo de cantiga en la que predominan las ideas sobre la forma plasmándose en una métrica sin ligazón paralelística.</span></span></span></span></div>
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<span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><span style="color: white;"><br /></span></span></span></span></div>
<div data-original-attrs="{"style":"text-align: justify;"}" style="text-align: justify;">
<span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><span style="color: white;"><br /></span></span></span></span></div>
<div data-original-attrs="{"style":"text-align: justify;"}" style="text-align: center;">
<span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><span style="color: white;"><div align="center" data-original-attrs="{"style":"text-align: center;"}" style="font-family: "Times New Roman"; font-size: medium;">
<em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;">A dona que eu am´e tenho por senhor<span data-original-tag="O:P"></span></span></span></span></em></div>
<span data-original-attrs="{"style":"color: #cccccc; font-family: Times, \"Times New Roman\", serif; font-size: large;"}" style="text-align: left;"><em></em></span><br style="font-family: "Times New Roman"; font-size: medium; text-align: left;" /><div align="center" data-original-attrs="{"style":"text-align: center;"}" style="font-family: "Times New Roman"; font-size: medium;">
<em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;">amostrade-mi-a, Deus, se vos em pracer for<span data-original-tag="O:P"></span></span></span></span></em></div>
<span data-original-attrs="{"style":"color: #cccccc; font-family: Times, \"Times New Roman\", serif; font-size: large;"}" style="text-align: left;"><em></em></span><br style="font-family: "Times New Roman"; font-size: medium; text-align: left;" /><div align="center" data-original-attrs="{"style":"text-align: center;"}" style="font-family: "Times New Roman"; font-size: medium;">
<em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;">se nom dade-mi a morte.<span data-original-tag="O:P"></span></span></span></span></em></div>
<span data-original-attrs="{"style":"color: #cccccc; font-family: Times, \"Times New Roman\", serif; font-size: large;"}" style="text-align: left;"><em></em></span><br style="font-family: "Times New Roman"; font-size: medium; text-align: left;" /><div align="center" data-original-attrs="{"style":"text-align: center;"}" style="font-family: "Times New Roman"; font-size: medium;">
<em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;">A que tenh´eu por lume d´estes olhos meus<span data-original-tag="O:P"></span></span></span></span></em></div>
<span data-original-attrs="{"style":"color: #cccccc; font-family: Times, \"Times New Roman\", serif; font-size: large;"}" style="text-align: left;"><em></em></span><br style="font-family: "Times New Roman"; font-size: medium; text-align: left;" /><div align="center" data-original-attrs="{"style":"text-align: center;"}" style="font-family: "Times New Roman"; font-size: medium;">
<em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;">e por que choram sempr´, amostrade-mi-a, Deus,<span data-original-tag="O:P"></span></span></span></span></em></div>
<span data-original-attrs="{"style":"color: #cccccc; font-family: Times, \"Times New Roman\", serif; font-size: large;"}" style="text-align: left;"><em></em></span><br style="font-family: "Times New Roman"; font-size: medium; text-align: left;" /><div align="center" data-original-attrs="{"style":"text-align: center;"}" style="font-family: "Times New Roman"; font-size: medium;">
<em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;">se nom dade-mi a morte.<span data-original-tag="O:P"></span></span></span></span></em></div>
<span data-original-attrs="{"style":"color: #cccccc; font-family: Times, \"Times New Roman\", serif; font-size: large;"}" style="text-align: left;"><em></em></span><br style="font-family: "Times New Roman"; font-size: medium; text-align: left;" /><div align="center" data-original-attrs="{"style":"text-align: center;"}" style="font-family: "Times New Roman"; font-size: medium;">
<em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;">Essa que vós fezestes melhor parecer<span data-original-tag="O:P"></span></span></span></span></em></div>
<span data-original-attrs="{"style":"color: #cccccc; font-family: Times, \"Times New Roman\", serif; font-size: large;"}" style="text-align: left;"><em></em></span><br style="font-family: "Times New Roman"; font-size: medium; text-align: left;" /><div align="center" data-original-attrs="{"style":"text-align: center;"}" style="font-family: "Times New Roman"; font-size: medium;">
<em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;">de quantas sei, ai Deus!, fazede-mi-a veer,<span data-original-tag="O:P"></span></span></span></span></em></div>
<span data-original-attrs="{"style":"color: #cccccc; font-family: Times, \"Times New Roman\", serif; font-size: large;"}" style="text-align: left;"><em></em></span><br style="font-family: "Times New Roman"; font-size: medium; text-align: left;" /><div align="center" data-original-attrs="{"style":"text-align: center;"}" style="font-family: "Times New Roman"; font-size: medium;">
<em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;">se nom dade-mi a morte.<span data-original-tag="O:P"></span></span></span></span></em></div>
<span data-original-attrs="{"style":"color: #cccccc; font-family: Times, \"Times New Roman\", serif; font-size: large;"}" style="text-align: left;"><em></em></span><br style="font-family: "Times New Roman"; font-size: medium; text-align: left;" /><div align="center" data-original-attrs="{"style":"text-align: center;"}" style="font-family: "Times New Roman"; font-size: medium;">
<em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;">Ai deus !, que mi-a fezestes mais ca mim amar,<span data-original-tag="O:P"></span></span></span></span></em></div>
<span data-original-attrs="{"style":"color: #cccccc; font-family: Times, \"Times New Roman\", serif; font-size: large;"}" style="text-align: left;"><em></em></span><br style="font-family: "Times New Roman"; font-size: medium; text-align: left;" /><div align="center" data-original-attrs="{"style":"text-align: center;"}" style="font-family: "Times New Roman"; font-size: medium;">
<em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;">mostrade-mi-a u possa com ela falar,<span data-original-tag="O:P"></span></span></span></span></em></div>
<span data-original-attrs="{"style":"color: #cccccc; font-family: Times, \"Times New Roman\", serif; font-size: large;"}" style="text-align: left;"><em></em></span><br style="font-family: "Times New Roman"; font-size: medium; text-align: left;" /><div align="center" data-original-attrs="{"style":"text-align: center;"}" style="font-family: "Times New Roman"; font-size: medium;">
<em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;">se nom dade-mi a morte.</span></span></span></em><br /><em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><span data-original-tag="O:P"></span></span></span></span></em> </div>
<span data-original-attrs="{"style":"color: #cccccc; font-family: Times, \"Times New Roman\", serif; font-size: large;"}" style="text-align: left;"><em></em></span><br style="font-family: "Times New Roman"; font-size: medium; text-align: left;" /><div align="center" data-original-attrs="{"style":"text-align: center;"}" style="font-family: "Times New Roman"; font-size: medium;">
<em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;">BERNAL DE BONAVAL</span></span></span></em></div>
<div align="center" data-original-attrs="{"style":"text-align: center;"}" style="font-family: "Times New Roman"; font-size: medium;">
<em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><br /></span></span></span></em></div>
<div align="center" data-original-attrs="{"style":"text-align: center;"}" style="font-family: "Times New Roman"; font-size: medium;">
<em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><br /></span></span></span></em></div>
<div class="separator" style="clear: both; text-align: center;">
<a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgS60P2BXdfd3g5oOfKE3SlymVDqO9NFqGMDIpjSv5CNRhG_BGugB_-xzH5_1X3qa8kJ-TgsD3AIUlPJhm-5Yxq0mIghB4IccEmQRIvF7eENgd5N-RVsJQauQm4o1AePFsqd7nLjm6jwaY/s1600/5.JPG" imageanchor="1" style="margin-left: 1em; margin-right: 1em;"><img border="0" data-original-height="320" data-original-width="278" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgS60P2BXdfd3g5oOfKE3SlymVDqO9NFqGMDIpjSv5CNRhG_BGugB_-xzH5_1X3qa8kJ-TgsD3AIUlPJhm-5Yxq0mIghB4IccEmQRIvF7eENgd5N-RVsJQauQm4o1AePFsqd7nLjm6jwaY/s1600/5.JPG" /></a></div>
<div align="center" data-original-attrs="{"style":"text-align: center;"}" style="font-family: "Times New Roman"; font-size: medium;">
<em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><br /></span></span></span></em></div>
</span></span></span></span></div>
<div data-original-attrs="{"style":"text-align: justify;"}" style="text-align: justify;">
<span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><span style="color: white;"><br /></span></span></span></span></div>
<div data-original-attrs="{"style":"text-align: justify;"}" style="text-align: justify;">
<span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><span style="color: white;"><div data-original-attrs="{"style":"text-align: justify;"}" style="font-family: "Times New Roman"; font-size: medium;">
<span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;">Es tradicional la coexistencia de lo lírico y de lo humorístico en la literatura gallega y ello aparece así reflejado en las <b>cantigas de escarnio</b> y en las de <b>maldizer. </b>Su intención es burlesca y a través de un lenguaje expresivo, de la crudeza, la obscenidad, el doble sentido y la sátira tenemos una crónica de la sociedad y vida de la época.<span data-original-tag="O:P"></span></span></span></span></div>
<div data-original-attrs="{"style":"text-align: justify;"}" style="font-family: "Times New Roman"; font-size: medium;">
<span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><br /></span></span></span></div>
<div data-original-attrs="{"style":"text-align: justify;"}" style="font-family: "Times New Roman"; font-size: medium;">
<span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><br /></span></span></span></div>
<div data-original-attrs="{"style":"text-align: justify;"}" style="font-family: "Times New Roman"; font-size: medium; text-align: center;">
<span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><div align="center" data-original-attrs="{"style":"text-align: center;"}" style="font-family: "Times New Roman"; font-size: medium;">
<em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;">Porque no mundo minguou a verdade</span></span></span></em><br /><em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><span data-original-tag="O:P"></span></span></span></span></em> </div>
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<span data-original-attrs="{"style":"color: #cccccc; font-family: Times, \"Times New Roman\", serif; font-size: large;"}" style="font-family: times, "times new roman", serif; font-size: medium;"><em></em></span></div>
<div align="center" data-original-attrs="{"style":"text-align: center;"}" style="font-family: "Times New Roman"; font-size: medium;">
<em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;">punhei um dia de a ir buscar</span></span></span></em><br /><em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><span data-original-tag="O:P"></span></span></span></span></em> </div>
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<span data-original-attrs="{"style":"color: #cccccc; font-family: Times, \"Times New Roman\", serif; font-size: large;"}" style="font-family: times, "times new roman", serif; font-size: medium;"><em></em></span></div>
<div align="center" data-original-attrs="{"style":"text-align: center;"}" style="font-family: "Times New Roman"; font-size: medium;">
<em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;">e,u por ela fui preguntar,</span></span></span></em><br /><em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><span data-original-tag="O:P"></span></span></span></span></em> </div>
<div class="separator" data-original-attrs="{"style":"clear: both; text-align: center;"}" style="clear: both; font-family: "Times New Roman"; font-size: medium;">
<span data-original-attrs="{"style":"color: #cccccc; font-family: Times, \"Times New Roman\", serif; font-size: large;"}" style="font-family: times, "times new roman", serif; font-size: medium;"><em></em></span></div>
<div align="center" data-original-attrs="{"style":"text-align: center;"}" style="font-family: "Times New Roman"; font-size: medium;">
<em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;">dissérom todos: - Alhur la buscade,</span></span></span></em><br /><em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><span data-original-tag="O:P"></span></span></span></span></em> </div>
<div class="separator" data-original-attrs="{"style":"clear: both; text-align: center;"}" style="clear: both; font-family: "Times New Roman"; font-size: medium;">
<span data-original-attrs="{"style":"color: #cccccc; font-family: Times, \"Times New Roman\", serif; font-size: large;"}" style="font-family: times, "times new roman", serif; font-size: medium;"><em></em></span></div>
<div align="center" data-original-attrs="{"style":"text-align: center;"}" style="font-family: "Times New Roman"; font-size: medium;">
<em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;">ca de tal guisa se foi a perder,</span></span></span></em><br /><em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><span data-original-tag="O:P"></span></span></span></span></em> </div>
<div class="separator" data-original-attrs="{"style":"clear: both; text-align: center;"}" style="clear: both; font-family: "Times New Roman"; font-size: medium;">
<span data-original-attrs="{"style":"color: #cccccc; font-family: Times, \"Times New Roman\", serif; font-size: large;"}" style="font-family: times, "times new roman", serif; font-size: medium;"><em></em></span></div>
<div align="center" data-original-attrs="{"style":"text-align: center;"}" style="font-family: "Times New Roman"; font-size: medium;">
<em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;">que nom podemos em novas haver</span></span></span></em><br /><em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><span data-original-tag="O:P"></span></span></span></span></em> </div>
<div class="separator" data-original-attrs="{"style":"clear: both; text-align: center;"}" style="clear: both; font-family: "Times New Roman"; font-size: medium;">
<span data-original-attrs="{"style":"color: #cccccc; font-family: Times, \"Times New Roman\", serif; font-size: large;"}" style="font-family: times, "times new roman", serif; font-size: medium;"><em></em></span></div>
<div align="center" data-original-attrs="{"style":"text-align: center;"}" style="font-family: "Times New Roman"; font-size: medium;">
<em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;">nem ja nom anda na irmaidade.</span></span></span></em><br /><em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><span data-original-tag="O:P"></span></span></span></span></em> </div>
<div class="separator" data-original-attrs="{"style":"clear: both; text-align: center;"}" style="clear: both; font-family: "Times New Roman"; font-size: medium;">
<span data-original-attrs="{"style":"color: #cccccc; font-family: Times, \"Times New Roman\", serif; font-size: large;"}" style="font-family: times, "times new roman", serif; font-size: medium;"><em></em></span></div>
<div align="center" data-original-attrs="{"style":"text-align: center;"}" style="font-family: "Times New Roman"; font-size: medium;">
<em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;">Nos mosteiros dos frades regrados</span></span></span></em><br /><em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><span data-original-tag="O:P"></span></span></span></span></em> </div>
<div class="separator" data-original-attrs="{"style":"clear: both; text-align: center;"}" style="clear: both; font-family: "Times New Roman"; font-size: medium;">
<span data-original-attrs="{"style":"color: #cccccc; font-family: Times, \"Times New Roman\", serif; font-size: large;"}" style="font-family: times, "times new roman", serif; font-size: medium;"><em></em></span></div>
<div align="center" data-original-attrs="{"style":"text-align: center;"}" style="font-family: "Times New Roman"; font-size: medium;">
<em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;">a demandei, e dissérom- m´assi :</span></span></span></em><br /><em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><span data-original-tag="O:P"></span></span></span></span></em> </div>
<div class="separator" data-original-attrs="{"style":"clear: both; text-align: center;"}" style="clear: both; font-family: "Times New Roman"; font-size: medium;">
<span data-original-attrs="{"style":"color: #cccccc; font-family: Times, \"Times New Roman\", serif; font-size: large;"}" style="font-family: times, "times new roman", serif; font-size: medium;"><em></em></span></div>
<div align="center" data-original-attrs="{"style":"text-align: center;"}" style="font-family: "Times New Roman"; font-size: medium;">
<em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;">-Nom bsquedes ós a verdad´aquí,<span data-original-tag="O:P"></span></span></span></span></em></div>
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<span data-original-attrs="{"style":"color: #cccccc; font-family: Times, \"Times New Roman\", serif; font-size: large;"}" style="font-family: times, "times new roman", serif; font-size: medium;"><em></em></span></div>
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<em><span data-original-attrs="{"style":"color: #cccccc; font-family: Times; font-size: large;"}" style="font-family: times; font-size: medium;"></span></em> </div>
<div align="center" data-original-attrs="{"style":"text-align: center;"}" style="font-family: "Times New Roman"; font-size: medium;">
<em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;">ca muitos anos havemos passados</span></span></span></em><br /><em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><span data-original-tag="O:P"></span></span></span></span></em> </div>
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<span data-original-attrs="{"style":"color: #cccccc; font-family: Times, \"Times New Roman\", serif; font-size: large;"}" style="font-family: times, "times new roman", serif; font-size: medium;"><em></em></span></div>
<div align="center" data-original-attrs="{"style":"text-align: center;"}" style="font-family: "Times New Roman"; font-size: medium;">
<span data-original-attrs="{"lang":"EN-GB","style":"mso-ansi-language: EN-GB;"}"><em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;">que nom morou nosco, per boa fe,</span></span></span></em></span><br /><span data-original-attrs="{"lang":"EN-GB","style":"mso-ansi-language: EN-GB;"}"><em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><span data-original-tag="O:P"></span></span></span></span></em></span> </div>
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<span data-original-attrs="{"style":"color: #cccccc; font-family: Times, \"Times New Roman\", serif; font-size: large;"}" style="font-family: times, "times new roman", serif; font-size: medium;"><em></em></span></div>
<div align="center" data-original-attrs="{"style":"text-align: center;"}" style="font-family: "Times New Roman"; font-size: medium;">
<em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;">nem sabemos u ela agora x´e</span></span></span></em><br /><em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><span data-original-tag="O:P"></span></span></span></span></em> </div>
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<span data-original-attrs="{"style":"color: #cccccc; font-family: Times, \"Times New Roman\", serif; font-size: large;"}" style="font-family: times, "times new roman", serif; font-size: medium;"><em></em></span></div>
<div align="center" data-original-attrs="{"style":"text-align: center;"}" style="font-family: "Times New Roman"; font-size: medium;">
<em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;">e d´al havemos mayores coidados.<span data-original-tag="O:P"></span></span></span></span></em></div>
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<span data-original-attrs="{"style":"color: #cccccc; font-family: Times, \"Times New Roman\", serif; font-size: large;"}" style="font-family: times, "times new roman", serif; font-size: medium;"><em></em></span></div>
<div align="center" data-original-attrs="{"style":"text-align: center;"}" style="font-family: "Times New Roman"; font-size: medium;">
<em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;">...<span data-original-tag="O:P"></span></span></span></span></em></div>
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<span data-original-attrs="{"style":"color: #cccccc; font-family: Times, \"Times New Roman\", serif; font-size: large;"}" style="font-family: times, "times new roman", serif; font-size: medium;"><em></em></span></div>
<div align="center" data-original-attrs="{"style":"text-align: center;"}" style="font-family: "Times New Roman"; font-size: medium;">
<em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;">AIRAS NUNES</span></span></span></em></div>
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<em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><br /></span></span></span></em></div>
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<em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><br /></span></span></span></em></div>
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<a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhNqVhocCjgizWmZDYjTmVZ4xm-y-RvqhSv7MOqfg_lbrCwfeDXrcGHOkaNOzK1zKjbrzrSD8IZQ8EJtmKx-VKg-CF85zX4mPkc2JnoDXuA9-EdQ9K_2JM7d2EEpjKk_3kOIliZfFK6PXk/s1600/6.JPG" imageanchor="1" style="margin-left: 1em; margin-right: 1em;"><img border="0" data-original-height="225" data-original-width="320" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhNqVhocCjgizWmZDYjTmVZ4xm-y-RvqhSv7MOqfg_lbrCwfeDXrcGHOkaNOzK1zKjbrzrSD8IZQ8EJtmKx-VKg-CF85zX4mPkc2JnoDXuA9-EdQ9K_2JM7d2EEpjKk_3kOIliZfFK6PXk/s1600/6.JPG" /></a></div>
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<em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><br /></span></span></span></em></div>
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<em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><br /></span></span></span></em></div>
<div data-original-attrs="{"style":"text-align: center;"}" style="font-family: "Times New Roman"; font-size: medium; text-align: left;">
<em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><br /></span></span></span></em></div>
</span></span></span></div>
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<span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><div data-original-attrs="{"style":"text-align: justify;"}" style="font-family: "Times New Roman"; font-size: medium;">
<span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;">Mención especial merecen las <b>Cantigas de Santa María</b> de Alfonso X El Sabio. Son 427 canciones líricas y narrativas de alabanza marial. Tienen la forma de una cantiga de amor en la que el rey será el enamorado de Santa María abandonando sus otros amores y exhortando a los trovadores a que las canten.<span data-original-tag="O:P"></span></span></span></span></div>
<div data-original-attrs="{"style":"text-align: justify;"}" style="font-family: "Times New Roman"; font-size: medium;">
<span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><br /></span></span></span></div>
<div data-original-attrs="{"style":"text-align: justify;"}" style="font-family: "Times New Roman"; font-size: medium;">
<span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><br /></span></span></span></div>
<div data-original-attrs="{"style":"text-align: justify;"}" style="font-family: "Times New Roman"; font-size: medium; text-align: center;">
<span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><br /></span></span></span></div>
<div>
<span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><div align="center" data-original-attrs="{"style":"text-align: center;"}" style="font-family: "Times New Roman"; font-size: medium; text-align: center;">
<em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;">Rosa das rosas e Fror das frores,<span data-original-tag="O:P"></span></span></span></span></em></div>
<span data-original-attrs="{"style":"color: #cccccc; font-family: Times, \"Times New Roman\", serif; font-size: large;"}" style="text-align: left;"><em></em></span><br style="font-family: "Times New Roman"; font-size: medium; text-align: left;" /><div align="center" data-original-attrs="{"style":"text-align: center;"}" style="font-family: "Times New Roman"; font-size: medium; text-align: center;">
<em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;">Dona das donas, Señor das senhores.<span data-original-tag="O:P"></span></span></span></span></em></div>
<span data-original-attrs="{"style":"color: #cccccc; font-family: Times, \"Times New Roman\", serif; font-size: large;"}" style="text-align: left;"><em></em></span><br style="font-family: "Times New Roman"; font-size: medium; text-align: left;" /><div align="center" data-original-attrs="{"style":"text-align: center;"}" style="font-family: "Times New Roman"; font-size: medium; text-align: center;">
<em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;">Rosa de beldad´e de parecer<span data-original-tag="O:P"></span></span></span></span></em></div>
<span data-original-attrs="{"style":"color: #cccccc; font-family: Times, \"Times New Roman\", serif; font-size: large;"}" style="text-align: left;"><em></em></span><br style="font-family: "Times New Roman"; font-size: medium; text-align: left;" /><div align="center" data-original-attrs="{"style":"text-align: center;"}" style="font-family: "Times New Roman"; font-size: medium; text-align: center;">
<em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;">e Fror d´a legria e de prazer,<span data-original-tag="O:P"></span></span></span></span></em></div>
<span data-original-attrs="{"style":"color: #cccccc; font-family: Times, \"Times New Roman\", serif; font-size: large;"}" style="text-align: left;"><em></em></span><br style="font-family: "Times New Roman"; font-size: medium; text-align: left;" /><div align="center" data-original-attrs="{"style":"text-align: center;"}" style="font-family: "Times New Roman"; font-size: medium; text-align: center;">
<em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;">Dona em mui piadosa seer,<span data-original-tag="O:P"></span></span></span></span></em></div>
<span data-original-attrs="{"style":"color: #cccccc; font-family: Times, \"Times New Roman\", serif; font-size: large;"}" style="text-align: left;"><em></em></span><br style="font-family: "Times New Roman"; font-size: medium; text-align: left;" /><div align="center" data-original-attrs="{"style":"text-align: center;"}" style="font-family: "Times New Roman"; font-size: medium; text-align: center;">
<em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;">Señor em tolher coitas e doores.<span data-original-tag="O:P"></span></span></span></span></em></div>
<span data-original-attrs="{"style":"color: #cccccc; font-family: Times, \"Times New Roman\", serif; font-size: large;"}" style="text-align: left;"><em></em></span><br style="font-family: "Times New Roman"; font-size: medium; text-align: left;" /><div align="center" data-original-attrs="{"style":"text-align: center;"}" style="font-family: "Times New Roman"; font-size: medium; text-align: center;">
<em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;">Rosa das rosas e Fror das frores,<span data-original-tag="O:P"></span></span></span></span></em></div>
<span data-original-attrs="{"style":"color: #cccccc; font-family: Times, \"Times New Roman\", serif; font-size: large;"}" style="text-align: left;"><em></em></span><br style="font-family: "Times New Roman"; font-size: medium; text-align: left;" /><div align="center" data-original-attrs="{"style":"text-align: center;"}" style="font-family: "Times New Roman"; font-size: medium; text-align: center;">
<em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;">Dona das donas, Señor das senhores.<span data-original-tag="O:P"></span></span></span></span></em></div>
<span data-original-attrs="{"style":"color: #cccccc; font-family: Times, \"Times New Roman\", serif; font-size: large;"}" style="text-align: left;"><em></em></span><br style="font-family: "Times New Roman"; font-size: medium; text-align: left;" /><div align="center" data-original-attrs="{"style":"text-align: center;"}" style="font-family: "Times New Roman"; font-size: medium; text-align: center;">
<em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;">...<span data-original-tag="O:P"></span></span></span></span></em></div>
<span data-original-attrs="{"style":"color: #cccccc; font-family: Times, \"Times New Roman\", serif; font-size: large;"}" style="text-align: left;"><em></em></span><br style="font-family: "Times New Roman"; font-size: medium; text-align: left;" /><div align="center" data-original-attrs="{"style":"text-align: center;"}" style="font-family: "Times New Roman"; font-size: medium; text-align: center;">
<em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;">ALFONSO X</span></span></span></em></div>
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<em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><br /></span></span></span></em></div>
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<em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><br /></span></span></span></em></div>
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<a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEiQ0LQjW2mUTVa-MoziRWTtgqsigSHOhJ9k5ql7l2_sodmht9hbRqa9CYqgTTfucraNNUrEGU1s-YUJVwoHrRdKbGGK0FO-lo1RGBucQul1iqILHHqc1F3PAXHMmFU3nw8aJ4XX4tpRmkk/s1600/8.JPG" imageanchor="1" style="margin-left: 1em; margin-right: 1em;"><img border="0" data-original-height="320" data-original-width="281" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEiQ0LQjW2mUTVa-MoziRWTtgqsigSHOhJ9k5ql7l2_sodmht9hbRqa9CYqgTTfucraNNUrEGU1s-YUJVwoHrRdKbGGK0FO-lo1RGBucQul1iqILHHqc1F3PAXHMmFU3nw8aJ4XX4tpRmkk/s1600/8.JPG" /></a></div>
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<em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><br /></span></span></span></em></div>
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<em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><br /></span></span></span></em></div>
<div align="center" data-original-attrs="{"style":"text-align: center;"}" style="font-family: "Times New Roman"; font-size: medium; text-align: center;">
<em><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><br /></span></span></span></em></div>
<div align="center" data-original-attrs="{"style":"text-align: center;"}" style="font-family: "Times New Roman"; font-size: medium; text-align: center;">
<div data-original-attrs="{"style":"text-align: justify;"}" style="text-align: justify;">
<span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;">Existen otras formas menores como las <i>cantigas de Lais</i>, de "<i>descordo</i>", de " <i>planto</i>" , el <i>serventesio</i>, o las <i>pastorelas.<span data-original-tag="O:P"></span></i></span></span></span></div>
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<span data-original-attrs="{"style":"color: #cccccc; font-family: Times, \"Times New Roman\", serif; font-size: large;"}" style="font-family: times, "times new roman", serif; font-size: medium;"></span></div>
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<span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;">La presión del castellano como lengua oficial, las pestes del siglo XIV, las luchas dinásticas, la Revolución Irmandiña, y el quebranto de las peregrinaciones a Santiago, entre otras causas, provocaron la decadencia de esta fértil y rica época para la lírica.</span></span></span></div>
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<span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"><span data-original-attrs="{"style":"color: #cccccc;"}"><span data-original-attrs="{"style":"font-size: large;"}" style="font-size: medium;"><span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-size: small; text-align: left;"><span data-original-attrs="{"style":"color: #cccccc;"}">BIBLIOGRAFÍA:<span data-original-tag="O:P"></span></span></span><br style="font-family: "Times New Roman"; font-size: medium; text-align: left;" /><div class="separator" data-original-attrs="{"style":"clear: both; text-align: center;"}" style="clear: both; font-family: "Times New Roman"; font-size: medium; text-align: center;">
<span data-original-attrs="{"style":"color: #cccccc; font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"></span></div>
<span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-size: small; text-align: left;"><span data-original-attrs="{"style":"color: #cccccc;"}">- Pérez Pascual, Ignacio; Reboleiro González, Amando: História da Língua; Vía Láctea, A Coruña, 1987<span data-original-tag="O:P"></span></span></span><br style="font-family: "Times New Roman"; font-size: medium; text-align: left;" /><div class="separator" data-original-attrs="{"style":"clear: both; text-align: center;"}" style="clear: both; font-family: "Times New Roman"; font-size: medium; text-align: center;">
<span data-original-attrs="{"style":"color: #cccccc; font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"></span></div>
<span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-size: small; text-align: left;"><span data-original-attrs="{"style":"color: #cccccc;"}">- V.V.A.A.<b>: </b>Literatura Galego- Portuguesa Medieval; Vía Láctea, A Coruña, 1987<span data-original-tag="O:P"></span></span></span><br style="font-family: "Times New Roman"; font-size: medium; text-align: left;" /><div class="separator" data-original-attrs="{"style":"clear: both; text-align: center;"}" style="clear: both; font-family: "Times New Roman"; font-size: medium; text-align: center;">
<span data-original-attrs="{"style":"color: #cccccc; font-family: Times, \"Times New Roman\", serif;"}" style="font-family: times, "times new roman", serif;"></span></div>
<span data-original-attrs="{"style":"font-family: Times, \"Times New Roman\", serif;"}" style="font-size: small; text-align: left;"><span data-original-attrs="{"style":"color: #cccccc;"}">- V.V.A.A.: Historia de Galicia. Tomo 2; Faro de Vigo, Vigo, 1991<span data-original-tag="O:P"></span></span></span></span></span></span></div>
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Sonia María García Garcíahttp://www.blogger.com/profile/13489949561200644676noreply@blogger.com0tag:blogger.com,1999:blog-6238152118688223934.post-47033675805689385202020-05-07T23:30:00.001+02:002020-05-07T23:30:18.215+02:00FERVENZA DO BELELLE<div class="separator" style="clear: both; text-align: center;">
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En O Roxal, parroquia de Anca, concello de Neda (A Coruña), el río Belelle salta un desnivel de rocas graníticas de unos 45 metros de altura. Además de la fervenza, la fraga de sus alrededores es muy interesante con especies propias de bosque atlántico y de bosque de ribera. </div>
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Tras las fuertes lluvias de este comienzo de año 2016, la fervenza luce espectacular. A continuación, os dejo una serie de fotos y un vídeo que espero os transmita, de algún modo, la maravillosa naturaleza que tenemos. No olvidéis encender los altavoces para escuchar la música del agua y el viento de la cascada. </div>
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Si pincháis en las fotos podréis verlas a mayor tamaño. </div>
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<tr><td class="tr-caption" style="text-align: center;">Muíño da Barcia</td></tr>
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<tr><td class="tr-caption" style="text-align: center;">Río Belelle</td></tr>
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<tr><td class="tr-caption" style="text-align: center;"><span style="font-size: 12.8px;">Muíño da Barcia</span><br /><br /><br /><div style="text-align: left;">
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<span style="text-align: center;">La senda de la derecha nos lleva a la fervenza, la izquierda a un pequeño salto.</span></div>
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<span style="text-align: center;">Y aquí el mundo se convierte en agua.</span></div>
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La fraga que rodea la fervenza y acompaña al río desde mucho más arriba es una joya con especies como los laureles, robles, cerezos bravos, avellanos, musgos y helechos...De esos bosques que decimos "encantados" cuando no sabemos ponerles ya mejores calificativos.</div>
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Las temperaturas anormalmente altas de esta temporada hace que nos encontremos en flor plantas que tendrían que florecer mucho más adelante como las "xestas", tojos o también prímulas. </div>
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<span style="text-align: center;">Pincha en este enlace para ver el vídeo: <a href="https://www.youtube.com/watch?v=s-lXUbB3u-c">VÍDEO FERVENZA DO BELELLE</a></span></div>
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Sonia María García Garcíahttp://www.blogger.com/profile/13489949561200644676noreply@blogger.com0tag:blogger.com,1999:blog-6238152118688223934.post-90590281742218407232020-05-07T19:34:00.000+02:002020-05-07T19:34:03.420+02:00CAPILLA Y CRUCEIRO DE BRAVOS<br />
<span style="text-align: justify;">El lugar de Bravos pertenece a la Parroquia de Vicinte, situada en el Concello de Outeiro de Rei (Lugo). Hasta 1890 fue parroquia y a partir de ese año, la construcción de la que hoy hablamos dejó de ser iglesia para convertirse en Capilla de la Cofradía de la Virgen del Rosario (fundada en 1704).</span><br />
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Las medidas se corresponden con una iglesia románica rural y quedan varios elementos de aquella época (siglo XII), aunque sufrió varias remodelaciones.<br />
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<span style="text-align: justify;">Está construida con sillares de granito y consta de una nave y un ábside rectangular. La portada se abre con un arco apuntado en el exterior (de medio punto en el interior).</span><br />
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En el tímpano hay una cruz con entrelazos, abarcada por una circunferencia.<br />
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<a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhNpgIVLqrcd_Si9yx1Jwuw9YeJ3MawkPvwIVh-ikPjQrAzbY64h-V0GF1U3uCbGWCSqWBLbZP6LkX7ga3hooheKkH1rMBnairIwYWz0GsMMkA67M3gzZfAul0bW4V8HMd2a36IkMH_Wjo/s1600/DSC_0230.JPG" imageanchor="1" style="margin-left: 1em; margin-right: 1em;"><img border="0" data-original-height="430" data-original-width="640" height="430" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEhNpgIVLqrcd_Si9yx1Jwuw9YeJ3MawkPvwIVh-ikPjQrAzbY64h-V0GF1U3uCbGWCSqWBLbZP6LkX7ga3hooheKkH1rMBnairIwYWz0GsMMkA67M3gzZfAul0bW4V8HMd2a36IkMH_Wjo/s640/DSC_0230.JPG" width="640" /></a></div>
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En el lado Sur hay una parte de un arco de medio punto, algunos canecillos y ménsulas, además de un arco apuntado cuyo tímpano está decorado por tres torres dentro de un disco.<br />
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Al lado del disco, escrito con letras monacales, hay una inscripción que dice: "Me hizo el arcediano Juan...en el año del Señor 1412".<br />
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En un cruce de caminos a un lado de la Capilla, se encuentra el Cruceiro de Bravos.<br />
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<a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEiglzd0G-vaMuwWKPCQfC1w9mOpD7Hg7w4ZwPDZ5ZYj_QiVqfebG4TA5V0u5dNRr04tvW1Nl3JGoz1KV3ljv5BNuoEZfPaEeRY8jDUSicmiljHTL1oJUT3mFZw-LKCD-rf7GmLjx4bbYMo/s1600/DSC_0242.JPG" imageanchor="1" style="margin-left: 1em; margin-right: 1em;"><img border="0" data-original-height="640" data-original-width="476" height="640" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEiglzd0G-vaMuwWKPCQfC1w9mOpD7Hg7w4ZwPDZ5ZYj_QiVqfebG4TA5V0u5dNRr04tvW1Nl3JGoz1KV3ljv5BNuoEZfPaEeRY8jDUSicmiljHTL1oJUT3mFZw-LKCD-rf7GmLjx4bbYMo/s640/DSC_0242.JPG" width="476" /></a></div>
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<span style="text-align: justify;"> Y dominando el conjunto, un gran roble centenario.</span><br />
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<span style="text-align: justify;"><br /></span>Sonia María García Garcíahttp://www.blogger.com/profile/13489949561200644676noreply@blogger.com0tag:blogger.com,1999:blog-6238152118688223934.post-82356858595119392552020-05-07T19:24:00.000+02:002020-05-07T19:38:06.563+02:00ÁNGELES EN EL CEMENTERIO DE SAN AMARO<br />
<span style="text-align: justify;">A Coruña vive mirando al mar y no podía ser menos que lo hicieran también sus difuntos.</span><br />
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<a href="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEiDWOHtHAU0kRx3wMT8BMnOjdre-m-Gn09GsRG4Mh4Awup_LIGKmVsIsJtyt7pLLuUpom0wmkqcHDUKAe_DctEIg-GWbY0cz5pXmtEwkS9DxrN_Tp4L6OODlf59ugLRcSruFtR_nK4kZos/s1600/1.JPG" imageanchor="1" style="margin-left: 1em; margin-right: 1em;"><img border="0" data-original-height="1348" data-original-width="1422" height="378" src="https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEiDWOHtHAU0kRx3wMT8BMnOjdre-m-Gn09GsRG4Mh4Awup_LIGKmVsIsJtyt7pLLuUpom0wmkqcHDUKAe_DctEIg-GWbY0cz5pXmtEwkS9DxrN_Tp4L6OODlf59ugLRcSruFtR_nK4kZos/s400/1.JPG" width="400" /></a></div>
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Tiene la fama de ser uno de los más bellos cementerios atlánticos, donde reposan los restos de personas de muy diversos pensamientos, profesiones, ideas políticas, épocas, estatus social, conocidos y anónimos... bajo la desnudez de la tierra o en el más bello panteón. Construido en terraza, observa el mar ya sin prisas, recibiendo su aroma y salitre, disfrutando de la placidez de una mañana de primavera o resistiendo los vientos y lluvias atlánticas invernales.</div>
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Cuando fue construido, allá a principios del siglo XIX, fue consagrado a San Amaro que se asocia con el "Más Allá". Un santo peregrino que llega a Galicia por barco pero cuando llega a Compostela no puede entrar en la catedral por la multitud. Regresa al puerto para volver a su casa y se encuentra con otra multitud de gente que peregrina a otro templo. Pregunta y le dicen que son devotos de un santo que peregrinó a Santiago pero no pudo entrar en la catedral...hace 300 años... Intemporalidad, búsqueda del Paraíso siguiendo al sol...</div>
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La capilla neoclásica que preside su entrada tiene un sugestivo rótulo que en parte dice: "El término del cuerpo es el que veis; el del alma será según obréis". ¿...?</div>
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Durante los siglos de su existencia, el cementerio ha crecido en proporciones, ha pasado por distintas épocas constructivas y decorativas como el Neoclásico, el Eclecticismo historicista, el Modernismo, el Regionalismo....y pasear por sus "calles" y "distritos" es un ejercicio de memoria, arte y sensibilidad. Existen muchos aspectos en los que detenernos, pero yo hoy lo he hecho en un elemento especial: esculturas de ángeles y figuras en mármol. </div>
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Muchos marmolistas han trabajado y trabajan todavía para el cementerio, algunos anónimos, otros de renombre como Molina. Losas de nichos, panteones, de las más sencillas cruces a cruces celtas o revestidas de vegetales, esculturas con diferentes significados, alegorías de la muerte o del dolor que produce, plañideras... y ángeles, muchos ángeles con tubas o trompetas, pensativos, alicaídos, mirando al cielo en busca de esperanza, pensativos o incluso inquisidores que con la mirada y el gesto te preguntan si lo estás haciendo todo bien...</div>
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A continuación veréis fotografías de algunos ejemplos pero quedan más y muchísimos elementos que recoger, aunque eso, será ya otro día y en otro paseo por esta otra parte de La Coruña.</div>
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Sonia María García Garcíahttp://www.blogger.com/profile/13489949561200644676noreply@blogger.com0