<?xml version='1.0' encoding='UTF-8'?><?xml-stylesheet href="http://www.blogger.com/styles/atom.css" type="text/css"?><feed xmlns='http://www.w3.org/2005/Atom' xmlns:openSearch='http://a9.com/-/spec/opensearchrss/1.0/' xmlns:georss='http://www.georss.org/georss' xmlns:gd='http://schemas.google.com/g/2005' xmlns:thr='http://purl.org/syndication/thread/1.0'><id>tag:blogger.com,1999:blog-1365774083631955253</id><updated>2011-04-21T12:40:34.421-07:00</updated><category term='Xeografía Física'/><title type='text'>Xeografia de Galicia</title><subtitle type='html'></subtitle><link rel='http://schemas.google.com/g/2005#feed' type='application/atom+xml' href='http://xeografiasebas.blogspot.com/feeds/posts/default'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/1365774083631955253/posts/default?max-results=100'/><link rel='alternate' type='text/html' href='http://xeografiasebas.blogspot.com/'/><link rel='hub' href='http://pubsubhubbub.appspot.com/'/><author><name>Sebas</name><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='32' height='24' src='http://2.bp.blogspot.com/_Bmn4Bys6ZPo/SO-Aott-wbI/AAAAAAAAABc/CQttoXOlux4/S220/25112006123.jpg'/></author><generator version='7.00' uri='http://www.blogger.com'>Blogger</generator><openSearch:totalResults>7</openSearch:totalResults><openSearch:startIndex>1</openSearch:startIndex><openSearch:itemsPerPage>100</openSearch:itemsPerPage><entry><id>tag:blogger.com,1999:blog-1365774083631955253.post-472325837077328379</id><published>2008-11-27T11:08:00.000-08:00</published><updated>2008-12-01T10:32:53.638-08:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='Xeografía Física'/><title type='text'>A Vexetación de Galicia</title><content type='html'>&lt;ul&gt;&lt;li&gt;&lt;div align="justify"&gt;&lt;a href="http://4.bp.blogspot.com/_Bmn4Bys6ZPo/STLW8BR3ngI/AAAAAAAAAEs/BW8xvAdS-kU/s1600-h/carballo.jpg"&gt;&lt;img id="BLOGGER_PHOTO_ID_5274514440228150786" style="FLOAT: left; MARGIN: 0px 10px 10px 0px; WIDTH: 202px; CURSOR: hand; HEIGHT: 320px" alt="" src="http://4.bp.blogspot.com/_Bmn4Bys6ZPo/STLW8BR3ngI/AAAAAAAAAEs/BW8xvAdS-kU/s320/carballo.jpg" border="0" /&gt;&lt;/a&gt; A vexetación en Galicia depende de tres factores fundamentais, o chan, o clima e a acción antrópica.&lt;br /&gt;&lt;br /&gt;O chan depende da naturaza da roca, en Galicia e maioritario o granito. Nas rexións que aflora o granito teñen o chan pobre, sin embargo nas depresións o chan e bo para a agricultura, que poden ser chan areosos ou arcillosos.&lt;br /&gt;&lt;/div&gt;&lt;/li&gt;&lt;li&gt;&lt;div align="justify"&gt;O &lt;a href="http://pt.wikipedia.org/wiki/Granito"&gt;granito&lt;/a&gt; abunda nas rexións montañosas donde suele ser habitual nas ladeiras abancadas para o aproveitamento agrícola. Unha explotación de granito preto do noso entorno é &lt;a href="http://webs.uvigo.es/smgminas/images/fotos/2007-2008/canteras_porrino/canteras_porrino_17.jpg"&gt;As canterias de granito de O Porriño.&lt;/a&gt;&lt;/div&gt;&lt;/li&gt;&lt;/ul&gt;&lt;div align="justify"&gt;O clima é chuvioso e templado, que é bo para as especies típicas do bosque caducifolio.&lt;br /&gt;&lt;/div&gt;&lt;div align="justify"&gt;A causa do transformación da vexetación e a &lt;a href="http://club.telepolis.com/geografo/geomorfologia/acctantro.htm"&gt;acción antrópica&lt;/a&gt;. &lt;/div&gt;&lt;div align="justify"&gt;&lt;/div&gt;&lt;div align="justify"&gt;As de árbores que predominan en Galicia son: o pino que é autóctono, o eucalipto, o robre que é especie dominante, &lt;a href="http://www.galespa.com.ar/carballo.htm"&gt;o carballo&lt;/a&gt;, entre outras.&lt;a href="http://1.bp.blogspot.com/_Bmn4Bys6ZPo/STLWB4vdHGI/AAAAAAAAAEk/o3lel8OzJGQ/s1600-h/pino_maritimo.jpg"&gt;&lt;img id="BLOGGER_PHOTO_ID_5274513441503911010" style="FLOAT: left; MARGIN: 0px 10px 10px 0px; WIDTH: 306px; CURSOR: hand; HEIGHT: 205px" alt="" src="http://1.bp.blogspot.com/_Bmn4Bys6ZPo/STLWB4vdHGI/AAAAAAAAAEk/o3lel8OzJGQ/s320/pino_maritimo.jpg" border="0" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div align="justify"&gt;&lt;/div&gt;&lt;div align="justify"&gt;&lt;/div&gt;&lt;div align="justify"&gt;&lt;/div&gt;&lt;div align="justify"&gt;Sin embargo, máis da cuarta parte do espazo galego esta ocupado por matorrais, debido a degradación do bosque. Nela predominan o &lt;a href="http://gl.wikipedia.org/wiki/Toxo"&gt;toxo&lt;/a&gt;, as silvas entre outros.&lt;/div&gt;&lt;p&gt;&lt;/p&gt;&lt;p&gt;&lt;/p&gt;&lt;p&gt;&lt;/p&gt;&lt;p&gt;&lt;br /&gt;&lt;/p&gt;&lt;p&gt;&lt;/p&gt;&lt;p&gt;&lt;/p&gt;&lt;p&gt;&lt;br /&gt;&lt;/p&gt;&lt;div align="justify"&gt;&lt;/div&gt;&lt;div align="justify"&gt;&lt;/div&gt;&lt;div align="justify"&gt;&lt;/div&gt;&lt;div align="justify"&gt;&lt;/div&gt;&lt;div align="justify"&gt;&lt;/div&gt;&lt;div align="justify"&gt;&lt;/div&gt;&lt;div align="justify"&gt;&lt;/div&gt;&lt;div align="justify"&gt;&lt;/div&gt;&lt;div align="justify"&gt;&lt;/div&gt;&lt;div align="justify"&gt;&lt;/div&gt;&lt;div align="justify"&gt;&lt;/div&gt;&lt;div align="justify"&gt;&lt;/div&gt;&lt;div align="justify"&gt;&lt;/div&gt;&lt;div align="justify"&gt;&lt;/div&gt;&lt;div align="justify"&gt;FONTES:&lt;/div&gt;&lt;span style="color:#ff0000;"&gt;&lt;p&gt;&lt;br /&gt;Internet:&lt;/span&gt;&lt;br /&gt;&lt;/p&gt;&lt;ol&gt;&lt;li&gt;&lt;div align="justify"&gt;&lt;span style="color:#000000;"&gt;&lt;a href="http://gl.wikipedia.org/wiki/Portada"&gt;Wikipedia&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;/li&gt;&lt;li&gt;&lt;a href="http://www.galespa.com.ar/carballo.htm"&gt;galiciaespallada&lt;/a&gt; &lt;/li&gt;&lt;li&gt;&lt;a href="http://www.galespa.com.ar/carballo.htm"&gt;club.telepolis&lt;/a&gt;&lt;/li&gt;&lt;/ol&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/1365774083631955253-472325837077328379?l=xeografiasebas.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://xeografiasebas.blogspot.com/feeds/472325837077328379/comments/default' title='Enviar comentarios'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=1365774083631955253&amp;postID=472325837077328379' title='0 comentarios'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/1365774083631955253/posts/default/472325837077328379'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/1365774083631955253/posts/default/472325837077328379'/><link rel='alternate' type='text/html' href='http://xeografiasebas.blogspot.com/2008/11/vexetacin-en-galicia-depende-de-tres.html' title='A Vexetación de Galicia'/><author><name>Sebas</name><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='32' height='24' src='http://2.bp.blogspot.com/_Bmn4Bys6ZPo/SO-Aott-wbI/AAAAAAAAABc/CQttoXOlux4/S220/25112006123.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://4.bp.blogspot.com/_Bmn4Bys6ZPo/STLW8BR3ngI/AAAAAAAAAEs/BW8xvAdS-kU/s72-c/carballo.jpg' height='72' width='72'/><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-1365774083631955253.post-8865264747173778825</id><published>2008-11-19T09:54:00.000-08:00</published><updated>2008-12-01T10:51:25.034-08:00</updated><title type='text'>O clima Oceánico de Galicia</title><content type='html'>&lt;div align="justify"&gt;&lt;a href="http://1.bp.blogspot.com/_Bmn4Bys6ZPo/STQuHynT2PI/AAAAAAAAAE0/ZsTko5ID3r8/s1600-h/adveccion+do+oeste1.bmp"&gt;&lt;img id="BLOGGER_PHOTO_ID_5274891774938306802" style="FLOAT: left; MARGIN: 0px 10px 10px 0px; WIDTH: 293px; CURSOR: hand; HEIGHT: 267px" alt="" src="http://1.bp.blogspot.com/_Bmn4Bys6ZPo/STQuHynT2PI/AAAAAAAAAE0/ZsTko5ID3r8/s320/adveccion+do+oeste1.bmp" border="0" /&gt;&lt;/a&gt;O &lt;a href="http://gl.wikipedia.org/wiki/Clima_oce%C3%A1nico"&gt;&lt;strong&gt;clima oceánico ou Atlántico&lt;/strong&gt;&lt;/a&gt; caracterízase por temperaturas suaves e fortes chuvias a causa da proximidade do océano, é propio das zonas templadas con dinamimo de correntes mariñas e ventos. As precipitacións son abundantes e están ben distribuídas aínda que cun máximo hibernal&lt;br /&gt;&lt;br /&gt;&lt;/div&gt;&lt;div align="justify"&gt;Os invernos non son moi fríos nin os veran moi calurosos.&lt;/div&gt;&lt;br /&gt;&lt;br /&gt;&lt;div align="justify"&gt;Tamén teñen clima oceánico outras comunidades autónomas como son, &lt;a href="http://gl.wikipedia.org/wiki/Asturias"&gt;Asturias&lt;/a&gt;, Cantabria, País Vasco, asi mesmo como Fracia e países do noroeste europeo.&lt;br /&gt;&lt;a href="http://4.bp.blogspot.com/_Bmn4Bys6ZPo/STQuWeQwGKI/AAAAAAAAAE8/r1kJ8Y_sqqE/s1600-h/Veran+fundamental.jpg"&gt;&lt;img id="BLOGGER_PHOTO_ID_5274892027173017762" style="FLOAT: right; MARGIN: 0px 0px 10px 10px; WIDTH: 649px; CURSOR: hand; HEIGHT: 211px" alt="" src="http://4.bp.blogspot.com/_Bmn4Bys6ZPo/STQuWeQwGKI/AAAAAAAAAE8/r1kJ8Y_sqqE/s320/Veran+fundamental.jpg" border="0" /&gt;&lt;/a&gt;&lt;/div&gt;&lt;div align="justify"&gt;&lt;/div&gt;&lt;div align="justify"&gt;&lt;/div&gt;&lt;div align="justify"&gt;&lt;/div&gt;&lt;div align="justify"&gt;&lt;/div&gt;&lt;div align="justify"&gt;&lt;/div&gt;&lt;div align="justify"&gt;&lt;/div&gt;&lt;div align="justify"&gt;&lt;/div&gt;&lt;div align="justify"&gt;&lt;/div&gt;&lt;div align="justify"&gt;&lt;/div&gt;&lt;div align="justify"&gt;&lt;/div&gt;&lt;div align="justify"&gt;&lt;/div&gt;&lt;div align="justify"&gt;&lt;/div&gt;&lt;div align="justify"&gt;Nesta imaxe pódese apreciar que o &lt;a href="http://gl.wikipedia.org/wiki/Anticicl%C3%B3n"&gt;&lt;strong&gt;anticiclon das azores&lt;/strong&gt; (anticiclón dinámico)&lt;/a&gt; fai que o clima de verán en galicia sea seco, soleado e caluroso. Excepcionalmente tamén pode exercer a súa influencia no outono e na primavera e incluso no inverno.&lt;/div&gt;&lt;div align="justify"&gt;&lt;/div&gt;&lt;div align="justify"&gt;FONTES:&lt;/div&gt;&lt;div align="justify"&gt;&lt;/div&gt;&lt;ul&gt;&lt;li&gt;&lt;div align="justify"&gt;&lt;span style="color:#cc0000;"&gt;Internet:&lt;/span&gt;&lt;/div&gt;&lt;/li&gt;&lt;/ul&gt;&lt;ol&gt;&lt;li&gt;&lt;div align="justify"&gt;&lt;a href="http://gl.wikipedia.org/wiki/Portada"&gt;galipedia&lt;/a&gt;&lt;/div&gt;&lt;/li&gt;&lt;/ol&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/1365774083631955253-8865264747173778825?l=xeografiasebas.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://xeografiasebas.blogspot.com/feeds/8865264747173778825/comments/default' title='Enviar comentarios'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=1365774083631955253&amp;postID=8865264747173778825' title='0 comentarios'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/1365774083631955253/posts/default/8865264747173778825'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/1365774083631955253/posts/default/8865264747173778825'/><link rel='alternate' type='text/html' href='http://xeografiasebas.blogspot.com/2008/11/o-clima-ocenico-de-galicia.html' title='O clima Oceánico de Galicia'/><author><name>Sebas</name><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='32' height='24' src='http://2.bp.blogspot.com/_Bmn4Bys6ZPo/SO-Aott-wbI/AAAAAAAAABc/CQttoXOlux4/S220/25112006123.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://1.bp.blogspot.com/_Bmn4Bys6ZPo/STQuHynT2PI/AAAAAAAAAE0/ZsTko5ID3r8/s72-c/adveccion+do+oeste1.bmp' height='72' width='72'/><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-1365774083631955253.post-7179619068590942496</id><published>2008-11-12T09:59:00.000-08:00</published><updated>2008-12-10T09:47:08.129-08:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='Xeografía Física'/><title type='text'>Encoro de As Eiras</title><content type='html'>&lt;div align="justify"&gt;&lt;a href="http://4.bp.blogspot.com/_Bmn4Bys6ZPo/STQ1ZsAPAWI/AAAAAAAAAFk/JJZTGaPlTjI/s1600-h/eiras+2.jpg"&gt;&lt;img id="BLOGGER_PHOTO_ID_5274899778982838626" style="FLOAT: left; MARGIN: 0px 10px 10px 0px; WIDTH: 270px; CURSOR: hand; HEIGHT: 414px" alt="" src="http://4.bp.blogspot.com/_Bmn4Bys6ZPo/STQ1ZsAPAWI/AAAAAAAAAFk/JJZTGaPlTjI/s320/eiras+2.jpg" border="0" /&gt;&lt;/a&gt; Tras o sequía do pasado outono, o embalse de Eiras,(O nome Eiras ven dun pobo que quedou baixo as augas do encoro) situado no concello de Fornelos de Montes leva dous meses e medio o 100% da súa capacidade, segundo indican os partes publicados por augas de Galicia. Concretamente, dende mediados do pasado mes de marzo o encoro atópase o límite da súa capacidade, sendo o último boletín do pasado 2 de xuño, no que se confirmaba esta situación. Al últimas choivas de maio deixaron unhas imaxes curiosas, xa que debido a gran cantidade de auga a presa veuse obrigada a abrir as comportas superiores, prodúcindo unhas cataratas espectaculares, e soltando unha gran cantidade de auga o río Oitavén o seu paso polo concello de Soutomaior. non hai moitos meses nos que o nivel do encoro era preocupante, no pasado outono e durante o mes de decembro cando o encoro rondaba a metade da súa capacidade, e incluso se chegou a&lt;a href="http://3.bp.blogspot.com/_Bmn4Bys6ZPo/STQynZSzQpI/AAAAAAAAAFM/e-yJsPNkI7Q/s1600-h/800px-Embalse_de_Eiras_-_Fornelos_de_Montes_-_Pontevedra.jpg"&gt;&lt;/a&gt; plantexar a posibilidade de comenzar con determinadas restriccións de auga, fundamentalmente na cidade de Vigo e nalgunhas poboacións do seu arredor, que dependen directamente do abastecemento de auga procedente deste encoro. &lt;/div&gt;&lt;div align="justify"&gt;&lt;br /&gt;&lt;/div&gt;&lt;div align="justify"&gt;Actualmente abastece de auga potable a Vigo e maior parte da súa metrópole, Cangas, O Porriño, Redondela, Mos, Baiona entre outros.&lt;br /&gt;&lt;br /&gt;FONTES:&lt;/div&gt;&lt;br /&gt;&lt;ol&gt;&lt;li&gt;&lt;span style="color:#ff0000;"&gt;Internet:&lt;/span&gt; &lt;/li&gt;&lt;li&gt;&lt;div align="left"&gt;&lt;a href="http://www.embalses.net/pantano-1236-eiras.html"&gt;embalse&lt;/a&gt;&lt;/div&gt;&lt;/li&gt;&lt;li&gt;&lt;div align="left"&gt;&lt;span style="font-size:130%;"&gt;&lt;span style="font-size:100%;"&gt;&lt;a href="http://www.fornelos.com/"&gt;fornelos&lt;/a&gt;&lt;/span&gt;&lt;/span&gt;&lt;/div&gt;&lt;/li&gt;&lt;li&gt;&lt;div align="left"&gt;&lt;a href="http://www.vigometropolitano.com/news/177/"&gt;vigometropolitano&lt;/a&gt;&lt;/div&gt;&lt;/li&gt;&lt;br /&gt;&lt;div align="left"&gt;&lt;span style="font-size:100%;"&gt;&lt;/span&gt;&lt;/div&gt;&lt;/ol&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/1365774083631955253-7179619068590942496?l=xeografiasebas.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://xeografiasebas.blogspot.com/feeds/7179619068590942496/comments/default' title='Enviar comentarios'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=1365774083631955253&amp;postID=7179619068590942496' title='0 comentarios'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/1365774083631955253/posts/default/7179619068590942496'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/1365774083631955253/posts/default/7179619068590942496'/><link rel='alternate' type='text/html' href='http://xeografiasebas.blogspot.com/2008/11/encoro-de-as-eiras.html' title='Encoro de As Eiras'/><author><name>Sebas</name><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='32' height='24' src='http://2.bp.blogspot.com/_Bmn4Bys6ZPo/SO-Aott-wbI/AAAAAAAAABc/CQttoXOlux4/S220/25112006123.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://4.bp.blogspot.com/_Bmn4Bys6ZPo/STQ1ZsAPAWI/AAAAAAAAAFk/JJZTGaPlTjI/s72-c/eiras+2.jpg' height='72' width='72'/><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-1365774083631955253.post-2473367597166537750</id><published>2008-10-27T12:05:00.001-07:00</published><updated>2008-11-13T11:06:45.345-08:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='Xeografía Física'/><title type='text'>Concello de Fornelos de Montes</title><content type='html'>&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://4.bp.blogspot.com/_Bmn4Bys6ZPo/SRHjQeqPMyI/AAAAAAAAADM/P-t94TrZ-_o/s1600-h/mappon%5B1%5D.jpg"&gt;&lt;img id="BLOGGER_PHOTO_ID_5265239311620453154" style="DISPLAY: block; MARGIN: 0px auto 10px; WIDTH: 234px; CURSOR: pointer; HEIGHT: 292px; TEXT-ALIGN: center" alt="" src="http://4.bp.blogspot.com/_Bmn4Bys6ZPo/SRHjQeqPMyI/AAAAAAAAADM/P-t94TrZ-_o/s400/mappon%5B1%5D.jpg" border="0" /&gt;&lt;/a&gt;&lt;br /&gt;O concello de &lt;a href="http://www.fornelos.com/"&gt;&lt;span style="FONT-WEIGHT: bold"&gt;Fornelos de Montes&lt;/span&gt;&lt;/a&gt; está situado na provincia de Pontevedra. &lt;div align="justify"&gt;&lt;/div&gt;&lt;div align="justify"&gt;Limita polo norte cos concellos de &lt;a href="http://www.pontecaldelas.org/index_gal.htm"&gt;Pontecaldelas&lt;/a&gt; e &lt;a href="http://www.alama.es/"&gt;A lama&lt;/a&gt;, ao sur con Mondariz e Covelo, ao leste con Leiro ( provincia de Ourense) e ao oeste con Soutomaior e Pazos de Borbén.&lt;/div&gt;&lt;div align="justify"&gt;&lt;/div&gt;&lt;div align="justify"&gt;&lt;/div&gt;&lt;div align="justify"&gt;&lt;/div&gt;&lt;div align="justify"&gt;&lt;/div&gt;&lt;div align="justify"&gt;As coordenadas xeográficas 42º 22´ 25´´ Norte, 42º 17´ 07´´ Sur, 8º 19´ 00´´ Leste e 8º 31´ 20´´ Oeste. &lt;/div&gt;&lt;div align="justify"&gt;&lt;/div&gt;&lt;div align="justify"&gt;É o concello situado máis ao interior da Área Metropolitana viguesa, presentando altitudes que oscilan entre un mínimo de 90 metros no Oeste, na parroquia de Calvos ao pe do curso do río Oitavén, e os 1.059 metros. &lt;/div&gt;&lt;span style="COLOR: rgb(204,102,0)"&gt;&lt;span style="font-size:180%;"&gt;&lt;span style="FONT-WEIGHT: bold"&gt;&lt;div align="center"&gt;&lt;span style="font-size:100%;color:#cc6600;"&gt;Fontes:&lt;/span&gt;&lt;/div&gt;&lt;div style="TEXT-ALIGN: center" align="justify"&gt;&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/div&gt;&lt;ol&gt;&lt;li&gt;&lt;div style="TEXT-ALIGN: left"&gt;&lt;span style="COLOR: rgb(204,102,0)"&gt;&lt;span style="COLOR: rgb(0,0,0)"&gt;&lt;span style="color:#ff0000;"&gt;Internet:&lt;/span&gt;&lt;/span&gt;&lt;/span&gt;&lt;/div&gt;&lt;/li&gt;&lt;/ol&gt;&lt;ul&gt;&lt;li&gt;&lt;div style="TEXT-ALIGN: left"&gt;&lt;span style="COLOR: rgb(204,102,0)"&gt;&lt;span style="COLOR: rgb(0,0,0)"&gt;&lt;a href="http://www.gl.wikipedia.org/wiki/Fornelos_de_Montes"&gt;Fornelos_de_Montes&lt;/a&gt; &lt;/span&gt;&lt;/span&gt;&lt;/div&gt;&lt;/li&gt;&lt;/ul&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/1365774083631955253-2473367597166537750?l=xeografiasebas.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://xeografiasebas.blogspot.com/feeds/2473367597166537750/comments/default' title='Enviar comentarios'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=1365774083631955253&amp;postID=2473367597166537750' title='0 comentarios'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/1365774083631955253/posts/default/2473367597166537750'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/1365774083631955253/posts/default/2473367597166537750'/><link rel='alternate' type='text/html' href='http://xeografiasebas.blogspot.com/2008/10/concello-de-fornelos-de-montes.html' title='Concello de Fornelos de Montes'/><author><name>Sebas</name><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='32' height='24' src='http://2.bp.blogspot.com/_Bmn4Bys6ZPo/SO-Aott-wbI/AAAAAAAAABc/CQttoXOlux4/S220/25112006123.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://4.bp.blogspot.com/_Bmn4Bys6ZPo/SRHjQeqPMyI/AAAAAAAAADM/P-t94TrZ-_o/s72-c/mappon%5B1%5D.jpg' height='72' width='72'/><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-1365774083631955253.post-1868907041932536273</id><published>2008-10-11T10:36:00.000-07:00</published><updated>2008-11-07T08:55:55.212-08:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='Xeografía Física'/><title type='text'>As RIAS de Galicia</title><content type='html'>&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://4.bp.blogspot.com/_Bmn4Bys6ZPo/SPzGayc2S3I/AAAAAAAAACs/PR6qkAuKY0w/s1600-h/ria_de_vigo.jpeg"&gt;&lt;img id="BLOGGER_PHOTO_ID_5259296628383566706" style="FLOAT: left; MARGIN: 0pt 10px 10px 0pt; CURSOR: pointer" alt="" src="http://4.bp.blogspot.com/_Bmn4Bys6ZPo/SPzGayc2S3I/AAAAAAAAACs/PR6qkAuKY0w/s200/ria_de_vigo.jpeg" border="0" /&gt;&lt;/a&gt;&lt;br /&gt;&lt;div style="TEXT-ALIGN: justify"&gt;A &lt;b&gt;ría&lt;/b&gt; é un dos posibeis &lt;a title="Accidente xeográfico" href="http://gl.wikipedia.org/wiki/Accidente_xeogr%C3%A1fico"&gt;accidentes xeográficos&lt;/a&gt; que forma a desembocadura dun &lt;span style="TEXT-DECORATION: underline"&gt;río&lt;/span&gt; no &lt;span style="TEXT-DECORATION: underline"&gt;mar&lt;/span&gt; ou &lt;span style="TEXT-DECORATION: underline"&gt;océano&lt;/span&gt;. É un grande &lt;a title="Estuario" href="http://gl.wikipedia.org/wiki/Estuario"&gt;estuario&lt;/a&gt; formado a partir dun vale costeiro mergullado; este vale no que se atopa non ten orixe glaciar, o que basicamente diferencia a ría do &lt;a title="Fiorde" href="http://gl.wikipedia.org/wiki/Fiorde"&gt;fiorde.&lt;/a&gt;&lt;br /&gt;&lt;/div&gt;&lt;br /&gt;&lt;div style="TEXT-ALIGN: justify"&gt;En Galicia exiten: A Rías Baixas, Rías Medias e as Rías Altas.&lt;br /&gt;&lt;/div&gt;&lt;div style="TEXT-ALIGN: justify"&gt;&lt;br /&gt;&lt;/div&gt;&lt;div style="TEXT-ALIGN: center"&gt;&lt;ul style="TEXT-ALIGN: center"&gt;&lt;li&gt;&lt;span style="FONT-WEIGHT: bold"&gt;&lt;span style="FONT-STYLE: italic"&gt;RIAS BAIXAS:&lt;/span&gt;&lt;/span&gt;&lt;/li&gt;&lt;/ul&gt;&lt;div style="TEXT-ALIGN: justify"&gt;&lt;a href="http://gl.wikipedia.org/wiki/R%C3%ADa_de_Vigo"&gt;Ría de Vigo&lt;/a&gt;, &lt;a href="http://gl.wikipedia.org/wiki/R%C3%ADa_de_Pontevedra"&gt;Ría de Pontevedra&lt;/a&gt;, Ría de Arousa, Ría de Muros e Noia, Ría de Corcubión, Rías de Baiona e a Ría de Aldan. &lt;/div&gt;&lt;ul&gt;&lt;li&gt;&lt;span style="FONT-WEIGHT: bold"&gt;&lt;span style="FONT-STYLE: italic"&gt;RÍAS MEDIAS:&lt;/span&gt;&lt;/span&gt;&lt;/li&gt;&lt;/ul&gt;&lt;div style="TEXT-ALIGN: justify"&gt;Ría de Camariñas, Ría de Corme e Laxe, Ría do Burgo, Ría de Betanzos, Ría de Ares, &lt;a href="http://gl.wikipedia.org/wiki/R%C3%ADa_de_Ferrol"&gt;Ría de Ferrol&lt;/a&gt;, Ría de Cedeira e a Ría de Ortigueira.&lt;br /&gt;&lt;/div&gt;&lt;br /&gt;&lt;ul&gt;&lt;li&gt;&lt;span style="FONT-WEIGHT: bold"&gt;&lt;span style="FONT-STYLE: italic"&gt;RÍAS ALTAS:&lt;/span&gt;&lt;/span&gt;&lt;/li&gt;&lt;/ul&gt;&lt;div style="TEXT-ALIGN: justify"&gt;Ría de Barqueiro, Ría de Viveiro, Ría de Foz e a &lt;a href="http://gl.wikipedia.org/wiki/R%C3%ADa_de_Ribadeo"&gt;Ría de Ribadeo&lt;/a&gt;&lt;br /&gt;&lt;br /&gt;&lt;div style="TEXT-ALIGN: center"&gt;&lt;span style="FONT-WEIGHT: bold; COLOR: rgb(204,102,0)"&gt;FONTES:&lt;/span&gt;&lt;br /&gt;&lt;/div&gt;&lt;/div&gt;&lt;div style="TEXT-ALIGN: justify"&gt;&lt;/div&gt;&lt;div style="TEXT-ALIGN: justify"&gt;&lt;/div&gt;&lt;div style="TEXT-ALIGN: justify"&gt;BIBLIOGRAFÍA:&lt;/div&gt;&lt;div style="TEXT-ALIGN: justify"&gt;- Internet:&lt;/div&gt;&lt;div style="TEXT-ALIGN: justify"&gt;&lt;a href="http://gl.wikipedia.org/wiki/Portada"&gt;Wikipedia&lt;/a&gt; &lt;/div&gt;&lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/1365774083631955253-1868907041932536273?l=xeografiasebas.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://xeografiasebas.blogspot.com/feeds/1868907041932536273/comments/default' title='Enviar comentarios'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=1365774083631955253&amp;postID=1868907041932536273' title='0 comentarios'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/1365774083631955253/posts/default/1868907041932536273'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/1365774083631955253/posts/default/1868907041932536273'/><link rel='alternate' type='text/html' href='http://xeografiasebas.blogspot.com/2008/10/as-rias-de-galicia.html' title='As RIAS de Galicia'/><author><name>Sebas</name><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='32' height='24' src='http://2.bp.blogspot.com/_Bmn4Bys6ZPo/SO-Aott-wbI/AAAAAAAAABc/CQttoXOlux4/S220/25112006123.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://4.bp.blogspot.com/_Bmn4Bys6ZPo/SPzGayc2S3I/AAAAAAAAACs/PR6qkAuKY0w/s72-c/ria_de_vigo.jpeg' height='72' width='72'/><thr:total>0</thr:total></entry><entry><id>tag:blogger.com,1999:blog-1365774083631955253.post-2535236861526852086</id><published>2008-10-10T08:48:00.000-07:00</published><updated>2008-11-07T08:56:22.367-08:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='Xeografía Física'/><title type='text'>O Relevo de Galicia</title><content type='html'>&lt;a onblur="try {parent.deselectBloggerImageGracefully();} catch(e) {}" href="http://3.bp.blogspot.com/_Bmn4Bys6ZPo/SPCUql3ivWI/AAAAAAAAACM/FaeimkpOZs0/s1600-h/mapa+fisico+galicia+galego.jpg"&gt;&lt;img id="BLOGGER_PHOTO_ID_5255864224581860706" style="FLOAT: left; MARGIN: 0pt 10px 10px 0pt; WIDTH: 255px; CURSOR: pointer; HEIGHT: 257px" alt="" src="http://3.bp.blogspot.com/_Bmn4Bys6ZPo/SPCUql3ivWI/AAAAAAAAACM/FaeimkpOZs0/s400/mapa+fisico+galicia+galego.jpg" border="0" /&gt;&lt;/a&gt;&lt;br /&gt;&lt;div style="TEXT-ALIGN: justify"&gt;Ó relevo actual de Galicia é o resultado da actuación de diferentes elementos a través do tempo, cun relevo variado no que se combinan &lt;strong&gt;serras, chairas, costas acantiladas e &lt;/strong&gt;&lt;a href="http://gl.wikipedia.org/wiki/R%C3%ADas_Baixas"&gt;&lt;strong&gt;rías&lt;/strong&gt;&lt;/a&gt;.&lt;br /&gt;&lt;/div&gt;&lt;br /&gt;&lt;br /&gt;&lt;br /&gt;&lt;div style="TEXT-ALIGN: justify"&gt;A altura media do relevo de Galicia non é moi elevada (non supera os 500 metros de altitude media), aínda que abundan as montañas e os outeiros con relevos pouco vigorosos.&lt;/div&gt;&lt;br /&gt;&lt;div style="TEXT-ALIGN: justify"&gt;As cadeas montañosas son de pouca elevación; as máximas altitudes acádanse nas serras orientais (&lt;a href="http://www.ancares.info/web/"&gt;&lt;strong&gt;Os Ancares&lt;/strong&gt;&lt;/a&gt;&lt;strong&gt;, &lt;/strong&gt;&lt;a href="http://www.serradocourel.es/"&gt;&lt;strong&gt;O Courel&lt;/strong&gt;&lt;/a&gt;&lt;strong&gt;, &lt;/strong&gt;&lt;a href="http://www.manzaneda.com/"&gt;&lt;strong&gt;Manzaneda &lt;/strong&gt;&lt;/a&gt;&lt;strong&gt;ou &lt;/strong&gt;&lt;a href="http://www.concellodequeixa.org/"&gt;&lt;strong&gt;Queixa&lt;/strong&gt;&lt;/a&gt;), onde se atopa o cumio maior &lt;a href="http://www.xunta.es/conselle/cma/GL/CMA05e/CMA05eh/CMA05ehb/es30007.htm"&gt;&lt;strong&gt;Pena Trevinca&lt;/strong&gt;,&lt;/a&gt; Dende o punto xeolóxico, Galicia é un bloque de rochas precámbricas e paleozoicas .&lt;/div&gt;&lt;br /&gt;&lt;div style="TEXT-ALIGN: justify"&gt;Os materias que forman a base do relevo, as rochas, podénse agrupar en Galicia en diferentes grupos : &lt;a href="http://gl.wikipedia.org/wiki/Granito"&gt;&lt;strong&gt;Granitos&lt;/strong&gt;&lt;/a&gt;&lt;strong&gt;, Xistos, rochas básocas , gneis ollo de sapo, rochas sedimentarias e depósitos non consolidados.&lt;br /&gt;&lt;br /&gt;&lt;/strong&gt;&lt;/div&gt;&lt;div align="center"&gt;&lt;strong&gt;&lt;span style="COLOR: rgb(204,102,0)"&gt;FONTES:&lt;/span&gt;&lt;/strong&gt;&lt;/div&gt;&lt;div align="left"&gt;&lt;strong&gt;&lt;span style="COLOR: rgb(204,102,0);font-size:130%;" &gt;&lt;/span&gt;&lt;/strong&gt;&lt;/div&gt;&lt;div align="left"&gt;&lt;strong&gt;Bibliografía:&lt;/strong&gt;&lt;/div&gt;&lt;div style="TEXT-ALIGN: justify" align="left"&gt;- Xeografía de Galicia Lois Gonzalez, R ; e Martínez Gargamala, H ; Obradoiro Santillana, Vigo 1998.&lt;br /&gt;&lt;strong&gt;Internet:&lt;br /&gt;&lt;/strong&gt;- &lt;a href="http://gl.wikipedia.org/wiki/Portada"&gt;Wikipedia&lt;/a&gt;&lt;/div&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/1365774083631955253-2535236861526852086?l=xeografiasebas.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://xeografiasebas.blogspot.com/feeds/2535236861526852086/comments/default' title='Enviar comentarios'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=1365774083631955253&amp;postID=2535236861526852086' title='1 comentarios'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/1365774083631955253/posts/default/2535236861526852086'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/1365774083631955253/posts/default/2535236861526852086'/><link rel='alternate' type='text/html' href='http://xeografiasebas.blogspot.com/2008/10/o-relevo-de-galicia.html' title='O Relevo de Galicia'/><author><name>Sebas</name><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='32' height='24' src='http://2.bp.blogspot.com/_Bmn4Bys6ZPo/SO-Aott-wbI/AAAAAAAAABc/CQttoXOlux4/S220/25112006123.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://3.bp.blogspot.com/_Bmn4Bys6ZPo/SPCUql3ivWI/AAAAAAAAACM/FaeimkpOZs0/s72-c/mapa+fisico+galicia+galego.jpg' height='72' width='72'/><thr:total>1</thr:total></entry><entry><id>tag:blogger.com,1999:blog-1365774083631955253.post-7621002190649867230</id><published>2008-10-02T11:00:00.001-07:00</published><updated>2008-11-07T08:57:53.725-08:00</updated><category scheme='http://www.blogger.com/atom/ns#' term='Xeografía Física'/><title type='text'>ILLAS CÍES: Paraíso Natural</title><content type='html'>&lt;div align="justify"&gt;&lt;span style="font-family:georgia;"&gt;A illas cies son un dos principais atractivos da cidade olivica ( vigo).&lt;/span&gt;&lt;/div&gt;&lt;br /&gt;&lt;div align="justify"&gt;&lt;a href="http://1.bp.blogspot.com/_Bmn4Bys6ZPo/SOUMWJUJUYI/AAAAAAAAAAU/6wWgF-AO80Q/s1600-h/Illas+cÃ&amp;shy;es.bmp"&gt;&lt;span style="font-family:georgia;"&gt;&lt;img id="BLOGGER_PHOTO_ID_5252618114994622850" style="FLOAT: right; MARGIN: 0px 0px 10px 10px; CURSOR: hand" alt="" src="http://1.bp.blogspot.com/_Bmn4Bys6ZPo/SOUMWJUJUYI/AAAAAAAAAAU/6wWgF-AO80Q/s320/Illas+c%C3%ADes.bmp" border="0" /&gt;&lt;/span&gt;&lt;/a&gt;&lt;span style="font-family:georgia;"&gt; Conocidas como " Illas dos Douses", foron olvidades durante séculos. &lt;/span&gt;&lt;/div&gt;&lt;div align="justify"&gt;&lt;br /&gt;&lt;span style="font-family:georgia;"&gt;As tres illas que compoñen o pequeno archipélago das Cíes son: &lt;a href="http://www.egu.es/egu/adjuntos_comentarios/0/cies.jpg"&gt;Illa de Faro&lt;/a&gt;, &lt;a href="http://www.navymar.com/Faros/Islas%20Cies/Isla%20Norte/Playa%20de%20Rodas.jpg"&gt;Illa Norte&lt;/a&gt; e a &lt;a href="http://www.dondeviajar.es/files/2008/04/isla-sur-o-de-san-martino.jpg"&gt;Illa sur ou de san martiño.&lt;/a&gt;&lt;/span&gt;&lt;/div&gt;&lt;p align="justify"&gt;&lt;span style="font-family:georgia;"&gt;Pódense atopar numerosas aves, unha frondosa vexetación de tintes descoñecidos, unha impresionante serra que xorde de maneira abrupta e radical casi dende a mesma praia e un sin fin de maravillas se nos acercamos personalmente ata as illas.&lt;/span&gt;&lt;/p&gt;&lt;p&gt;&lt;span style="font-family:georgia;"&gt;&lt;/span&gt;&lt;/p&gt;&lt;p&gt;&lt;span style="font-family:georgia;"&gt;&lt;/span&gt;&lt;/p&gt;&lt;p&gt;&lt;span style="font-family:georgia;"&gt;&lt;/span&gt;&lt;/p&gt;&lt;p align="justify"&gt;&lt;/p&gt;&lt;p align="justify"&gt;&lt;a href="http://3.bp.blogspot.com/_Bmn4Bys6ZPo/SQC8Nvz2kVI/AAAAAAAAAC8/Myot7aMRA9g/s1600-h/1172155881Islas%2520Cies.jpg"&gt;&lt;span style="font-family:georgia;"&gt;&lt;img id="BLOGGER_PHOTO_ID_5260411309127012690" style="FLOAT: left; MARGIN: 0px 10px 10px 0px; WIDTH: 320px; CURSOR: hand; HEIGHT: 240px" alt="" src="http://3.bp.blogspot.com/_Bmn4Bys6ZPo/SQC8Nvz2kVI/AAAAAAAAAC8/Myot7aMRA9g/s320/1172155881Islas%2520Cies.jpg" border="0" /&gt;&lt;/span&gt;&lt;/a&gt;&lt;span style="font-family:georgia;"&gt;A &lt;strong&gt;praia das Rozas&lt;/strong&gt; foi considerada unha das &lt;em&gt;mellores de todo o mundo&lt;/em&gt;, publicada no periódico " the guardian ", tamén foi rexudio de piratas e na actualidade &lt;/span&gt;&lt;a href="http://gl.wikipedia.org/wiki/Parque_Nacional_das_Illas_Atl%C3%A1nticas"&gt;&lt;span style="font-family:georgia;color:#ff0000;"&gt;parque nacional&lt;/span&gt;&lt;/a&gt;&lt;span style="font-family:georgia;"&gt;, de augas cristalinas de &lt;span style="color:#33cc00;"&gt;&lt;span style="color:#000000;"&gt;color esmeralda&lt;/span&gt; &lt;/span&gt;&lt;span style="color:#000000;"&gt;e de &lt;/span&gt;area fina e moi branca fai delicias daqueles turistas e non turistas que a visitan.&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&lt;p align="justify"&gt;&lt;span style="font-family:georgia;"&gt;&lt;/span&gt;&lt;/p&gt;&lt;p align="justify"&gt;&lt;span style="font-family:georgia;"&gt;&lt;/span&gt;&lt;/p&gt;&lt;p align="center"&gt;&lt;span style="font-family:georgia;"&gt;&lt;span style="color:#cc6600;"&gt;&lt;strong&gt;FONTES:&lt;/strong&gt;&lt;/span&gt;&lt;/span&gt;&lt;/p&gt;&lt;p align="left"&gt;&lt;span style="font-family:georgia;"&gt;Internet: &lt;/span&gt;&lt;/p&gt;&lt;p align="left"&gt;&lt;span style="font-family:georgia;"&gt;&lt;/p&gt;&lt;/span&gt;&lt;div class="blogger-post-footer"&gt;&lt;img width='1' height='1' src='https://blogger.googleusercontent.com/tracker/1365774083631955253-7621002190649867230?l=xeografiasebas.blogspot.com' alt='' /&gt;&lt;/div&gt;</content><link rel='replies' type='application/atom+xml' href='http://xeografiasebas.blogspot.com/feeds/7621002190649867230/comments/default' title='Enviar comentarios'/><link rel='replies' type='text/html' href='http://www.blogger.com/comment.g?blogID=1365774083631955253&amp;postID=7621002190649867230' title='0 comentarios'/><link rel='edit' type='application/atom+xml' href='http://www.blogger.com/feeds/1365774083631955253/posts/default/7621002190649867230'/><link rel='self' type='application/atom+xml' href='http://www.blogger.com/feeds/1365774083631955253/posts/default/7621002190649867230'/><link rel='alternate' type='text/html' href='http://xeografiasebas.blogspot.com/2008/10/illas-cies-paraiso-natural.html' title='ILLAS CÍES: Paraíso Natural'/><author><name>Sebas</name><email>noreply@blogger.com</email><gd:image rel='http://schemas.google.com/g/2005#thumbnail' width='32' height='24' src='http://2.bp.blogspot.com/_Bmn4Bys6ZPo/SO-Aott-wbI/AAAAAAAAABc/CQttoXOlux4/S220/25112006123.jpg'/></author><media:thumbnail xmlns:media='http://search.yahoo.com/mrss/' url='http://1.bp.blogspot.com/_Bmn4Bys6ZPo/SOUMWJUJUYI/AAAAAAAAAAU/6wWgF-AO80Q/s72-c/Illas+c%C3%ADes.bmp' height='72' width='72'/><thr:total>0</thr:total></entry></feed>
