{"id":39812,"date":"2013-02-19T08:48:00","date_gmt":"2013-02-19T08:48:00","guid":{"rendered":"tag:blogger.com,1999:blog-3194836150491826912.post-5494874277530509669"},"modified":"2013-02-19T09:05:15","modified_gmt":"2013-02-19T09:05:15","slug":"unidad-03-las-formas-de-la-tierra","status":"publish","type":"post","link":"https:\/\/blogsaverroes.juntadeandalucia.es\/geohistoria\/2013\/02\/19\/unidad-03-las-formas-de-la-tierra\/","title":{"rendered":"Unidad 03. Las formas de la Tierra"},"content":{"rendered":"<h3 class=\"post-title entry-title\" itemprop=\"name\"><b><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><span class=\"Apple-style-span\" style=\"font-weight: normal;\"><b><span class=\"Apple-style-span\" style=\"color: yellow;\"><span class=\"Apple-style-span\" style=\"font-size: medium;\">TALLER 1. LA LISTOSFERA<\/span><\/span><\/b><\/span><\/span><\/b><\/h3>\n<div class=\"post-header\"><\/div>\n<div style=\"text-align: justify;\"><b><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">1.1. LA ESTRUCTURA DE LA TIERRA.<\/span><\/b><\/div>\n<div style=\"text-align: justify;\">\n<div style=\"margin: 0px;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">&nbsp;&nbsp;  &nbsp;En nuestro planeta las tierras se hallan repartidas en diversos  continentes o grandes masas de tierra que emergen o sobresalen de los  oc\u00e9anos y mares.<\/span><\/div>\n<\/div>\n<div style=\"text-align: justify;\">\n<div style=\"margin: 0px;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">&nbsp;&nbsp;  &nbsp;A pesar de que existen 5 grandes masas contientales (\u00c1frica, Am\u00e9rica,  Eurasia, Ocean\u00eda y Antartida), habitualmente dividimos la Tierra en 6  continentes:&nbsp;\u00c1frica, Am\u00e9rica, Asia, Euorpa, Ocean\u00eda y Antartida.<\/span><\/div>\n<\/div>\n<ul>\n<li style=\"text-align: justify;\"><span style=\"font-weight: normal;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">La superficie de los continentes presenta relieves muy variados como&nbsp;<\/span><\/span><span style=\"font-weight: normal;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">llanuras<\/span><\/span><span style=\"font-weight: normal;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">,&nbsp;<\/span><\/span><span style=\"font-weight: normal;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">mesetas<\/span><\/span><span style=\"font-weight: normal;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">,&nbsp;<\/span><\/span><span style=\"font-weight: normal;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">cordilleras<\/span><\/span><span style=\"font-weight: normal;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">,&nbsp;<\/span><\/span><span style=\"font-weight: normal;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">valles<\/span><\/span><span style=\"font-weight: normal;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">&nbsp;y&nbsp;<\/span><\/span><span style=\"font-weight: normal;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">depresiones<\/span><\/span><span style=\"font-weight: normal;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">.<\/span><\/span><\/li>\n<li style=\"text-align: justify;\"><span style=\"font-weight: normal;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">Los oc<\/span><\/span><span style=\"font-weight: normal;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">\u00e9anos ba\u00f1an los continentes modelando sus costas, con acantilados, playas\u2026<\/span><\/span><\/li>\n<li style=\"text-align: justify;\"><span style=\"font-weight: normal;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">En medio de estas grandes masas de agua surgen los&nbsp;<\/span><\/span><span style=\"font-weight: normal;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">archipi\u00e9lagos<\/span><\/span><span style=\"font-weight: normal;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">&nbsp;con sus&nbsp;<\/span><\/span><span style=\"font-weight: normal;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">isla<\/span><\/span><\/li>\n<\/ul>\n<div style=\"text-align: justify;\">\n<div style=\"margin: 0px;\"><span style=\"font-weight: normal;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">La&nbsp;<\/span><\/span><span style=\"font-weight: normal;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">Tierra<\/span><\/span><span style=\"font-weight: normal;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">&nbsp;es una gran&nbsp;<\/span><\/span><span style=\"font-weight: normal;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">esfera<\/span><\/span><span style=\"font-weight: normal;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">&nbsp;ligeramente achatada por los polos que se divide en tres grandes zonas conc\u00e9ntricas.<\/span><\/span><\/div>\n<\/div>\n<div style=\"text-align: justify;\">\n<div style=\"margin: 0px;\"><span style=\"font-weight: normal;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><br \/><\/span><\/span><\/div>\n<\/div>\n<div class=\"separator\" style=\"clear: both; margin: 0px; text-align: center;\"><a href=\"http:\/\/1.bp.blogspot.com\/__iXhFNsMosg\/TM7aUBtKkXI\/AAAAAAAAADY\/43Q1IWrCcYo\/s1600\/composicion_interna.jpg\" style=\"clear: right; float: right; margin-bottom: 1em; margin-left: 1em; text-align: justify;\"><img loading=\"lazy\" decoding=\"async\" border=\"0\" height=\"320\" src=\"http:\/\/1.bp.blogspot.com\/__iXhFNsMosg\/TM7aUBtKkXI\/AAAAAAAAADY\/43Q1IWrCcYo\/s320\/composicion_interna.jpg\" style=\"cursor: move;\" width=\"211\" \/><\/a><\/div>\n<div style=\"margin-left: 1em; margin-right: 1em; text-align: justify;\">\n<div style=\"margin: 0px;\"><a href=\"http:\/\/2.bp.blogspot.com\/__iXhFNsMosg\/TM2r6IP16FI\/AAAAAAAAABc\/ODS1GzLXi08\/s1600\/Las+capas+de+la+Tierra.jpg\" style=\"margin-left: 1em; margin-right: 1em;\"><span class=\"Apple-style-span\" style=\"color: black;\"><\/span><\/a><a href=\"http:\/\/2.bp.blogspot.com\/__iXhFNsMosg\/TM2r6IP16FI\/AAAAAAAAABc\/ODS1GzLXi08\/s1600\/Las+capas+de+la+Tierra.jpg\" style=\"margin-left: 1em; margin-right: 1em;\"><img loading=\"lazy\" decoding=\"async\" border=\"0\" height=\"216\" src=\"http:\/\/2.bp.blogspot.com\/__iXhFNsMosg\/TM2r6IP16FI\/AAAAAAAAABc\/ODS1GzLXi08\/s320\/Las+capas+de+la+Tierra.jpg\" style=\"cursor: move;\" width=\"320\" \/><\/a><\/div>\n<\/div>\n<div style=\"margin: 0px;\"><\/div>\n<div class=\"separator\" style=\"clear: both; margin: 0px; text-align: center;\"><span class=\"Apple-style-span\" style=\"clear: right; float: right; font-family: Arial, Helvetica, sans-serif; margin-bottom: 1em; margin-left: 1em;\"><\/span><\/div>\n<ul>\n<li style=\"text-align: justify;\"><span style=\"font-weight: normal;\"><span style=\"font-weight: normal;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">La capa externa es la&nbsp;<\/span><\/span><b><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">corteza<\/span><\/b><span style=\"font-weight: normal;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">, que apenas representa el 1% del total del planeta<\/span><\/span><span style=\"font-weight: normal;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">. La corteza, junto con la parte superior del manto, recibe el nombre de&nbsp;<\/span><\/span><span style=\"font-weight: normal;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">litosfera<\/span><\/span><span style=\"font-weight: normal;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">.<\/span><\/span><\/span><\/li>\n<li style=\"text-align: justify;\"><span style=\"font-weight: normal;\"><span style=\"font-weight: normal;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">A su alrededor est\u00e1 el&nbsp;<\/span><\/span><b><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">manto<\/span><\/b><span style=\"font-weight: normal;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">, que<\/span><\/span><span style=\"font-weight: normal;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">&nbsp;representa un 84% del volumen de la Tierra<\/span><\/span><span style=\"font-weight: normal;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">.<\/span><\/span><\/span><\/li>\n<li style=\"text-align: justify;\"><span style=\"font-weight: normal;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><span style=\"font-weight: normal;\"><\/span>La parte m\u00e1s interna es el&nbsp;<\/span><\/span><b><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">n<\/span><\/b><b><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">\u00fa<\/span><\/b><b><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">cleo<\/span><\/b><b><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">&nbsp;<\/span><\/b><span style=\"font-weight: normal;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">y supone un 15% del volumen total del planeta<\/span><\/span><span style=\"font-weight: normal;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">.<\/span><\/span><\/li>\n<\/ul>\n<div style=\"text-align: center;\">\n<div style=\"text-align: center;\">\n<div style=\"text-align: center;\">\n<div style=\"margin: 0px;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><\/span><\/div>\n<\/div>\n<\/div>\n<div style=\"text-align: justify;\">\n<div style=\"margin: 0px;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><br \/><\/span><\/div>\n<div style=\"margin: 0px;\"><b><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">1.2. LA CORTEZA TERRESTRE.<\/span><\/b><\/div>\n<div style=\"margin: 0px;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">La corteza terrestre tiene una anchura muy desigual.<\/span><\/div>\n<div>\n<ul>\n<li style=\"text-align: justify;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">La corteza terrestre no es lisa, sino que forma&nbsp;<i>monta\u00f1as<\/i>,&nbsp;<i>valles<\/i>,&nbsp;<i>depresiones&nbsp;<\/i>y&nbsp;<i>llanuras<\/i>&nbsp;que configuran el relieve de la tierra<\/span><\/li>\n<li style=\"text-align: justify;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">El relieve de la Tierra, aunque parece estable, cambia debido a la acci\u00f3n de los agentes internos y externos<\/span><\/li>\n<li style=\"text-align: justify;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">Los relieves se transforman lentamente por la acci\u00f3n del agua, del viento y de la acci\u00f3n humana (erosi\u00f3n).<\/span><\/li>\n<\/ul>\n<\/div>\n<div style=\"margin: 0px;\"><\/div>\n<\/div>\n<div style=\"text-align: justify;\">\n<div style=\"margin: 0px;\"><b><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">1.3. LA DERIVA DE LOS CONTINENTES.<\/span><\/b><\/div>\n<div style=\"margin: 0px;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">&nbsp;&nbsp; &nbsp;Seg\u00fan la teor\u00eda de la deriva de los continentes, la corteza de la Tierra estaba formada por un \u00fanico continente, denominado&nbsp;<span class=\"Apple-style-span\" style=\"color: red;\"><b>Pangea<\/b><\/span>, que flotaba sobre el manto.&nbsp;<\/span><\/div>\n<div>\n<div class=\"separator\" style=\"clear: both; margin: 0px; text-align: center;\"><a href=\"http:\/\/1.bp.blogspot.com\/__iXhFNsMosg\/TM2td7crvNI\/AAAAAAAAABg\/0mNiM5Tldyg\/s1600\/Pangea.jpg\" style=\"margin-left: 1em; margin-right: 1em;\"><img loading=\"lazy\" decoding=\"async\" border=\"0\" height=\"177\" src=\"http:\/\/1.bp.blogspot.com\/__iXhFNsMosg\/TM2td7crvNI\/AAAAAAAAABg\/0mNiM5Tldyg\/s320\/Pangea.jpg\" style=\"cursor: move;\" width=\"320\" \/><\/a><\/div>\n<div style=\"text-align: justify;\">\n<div style=\"margin: 0px;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><br \/><\/span><\/div>\n<\/div>\n<div style=\"margin: 0px;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><\/span><\/div>\n<div style=\"text-align: justify;\">\n<div style=\"margin: 0px;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">&nbsp;&nbsp; &nbsp;El movimiento de rotaci\u00f3n de la Tierra rompi\u00f3 este \u00fanico continente dando lugar a las llamadas placas tect\u00f3nicas.&nbsp;<\/span><\/div>\n<\/div>\n<div class=\"separator\" style=\"clear: both; margin: 0px; text-align: center;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><a href=\"http:\/\/2.bp.blogspot.com\/__iXhFNsMosg\/TM2udoPw7cI\/AAAAAAAAABk\/PSQteAZPVpQ\/s1600\/Deriva+de+los+continentes.jpg\" style=\"margin-left: 1em; margin-right: 1em;\"><img loading=\"lazy\" decoding=\"async\" border=\"0\" height=\"138\" src=\"http:\/\/2.bp.blogspot.com\/__iXhFNsMosg\/TM2udoPw7cI\/AAAAAAAAABk\/PSQteAZPVpQ\/s400\/Deriva+de+los+continentes.jpg\" style=\"cursor: move;\" width=\"400\" \/><\/a><\/span><\/div>\n<div class=\"separator\" style=\"clear: both; margin: 0px; text-align: justify;\"><\/div>\n<div class=\"separator\" style=\"clear: both; margin: 0px; text-align: justify;\"><\/div>\n<div style=\"text-align: justify;\">\n<div style=\"margin: 0px;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">&nbsp;&nbsp;&nbsp;<\/span><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">A  pesar de los lentos movimientos, cuando dos placas chocan una de ellas  puede elevarse formando grandes cordilleras, mientras la otra se hunde  hasta crear profundas fosas marinas.&nbsp;<\/span><\/div>\n<\/div>\n<div class=\"separator\" style=\"clear: both; margin: 0px; text-align: center;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><span class=\"Apple-style-span\" style=\"font-family: 'Times New Roman';\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><a href=\"http:\/\/3.bp.blogspot.com\/__iXhFNsMosg\/TM2u--prNaI\/AAAAAAAAABo\/oqyIr0OfsNk\/s1600\/subduccion.jpg\" style=\"margin-left: 1em; margin-right: 1em;\"><img loading=\"lazy\" decoding=\"async\" border=\"0\" height=\"147\" src=\"http:\/\/3.bp.blogspot.com\/__iXhFNsMosg\/TM2u--prNaI\/AAAAAAAAABo\/oqyIr0OfsNk\/s200\/subduccion.jpg\" style=\"cursor: move;\" width=\"200\" \/><\/a><\/span><\/span><span class=\"Apple-style-span\" style=\"font-family: 'Times New Roman';\"><\/span>&nbsp;<\/span><\/div>\n<div class=\"separator\" style=\"clear: both; margin: 0px; text-align: center;\"><\/div>\n<div class=\"separator\" style=\"clear: both; margin: 0px; text-align: justify;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">&nbsp;&nbsp;&nbsp;<\/span><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">Los puntos de contacto entre dos placas son \u00e1reas de gran inestabilidad, que se manifiestan en forma de terremotos y volcanes.<\/span><\/div>\n<div style=\"text-align: justify;\">\n<div>\n<div style=\"margin: 0px;\"><\/div>\n<div style=\"text-align: justify;\">\n<div style=\"margin: 0px;\">\n<div style=\"text-align: center;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><b><span class=\"Apple-style-span\" style=\"color: yellow;\"><span class=\"Apple-style-span\" style=\"font-size: medium;\">TALLER 2. LOS AGENTES DE FORMACI\u00d3N DEL RELIEVE<\/span><\/span><\/b><\/span><\/div>\n<p><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><b>2. LOS AGENTES DE FORMACI\u00d3N DEL RELIEVE.<\/b><\/span><\/div>\n<\/div>\n<div style=\"margin: 0px;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><\/span><\/div>\n<div style=\"text-align: justify;\">\n<div style=\"margin: 0px;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><b><span class=\"Apple-style-span\" style=\"font-weight: normal;\"><b>2.1. LOS AGENTES INTERNOS.<\/b><\/span><\/b><\/span><\/div>\n<\/div>\n<div style=\"margin: 0px;\"><\/div>\n<div style=\"text-align: justify;\">\n<div style=\"margin: 0px;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">&nbsp;&nbsp;  &nbsp;Se ha comprobado que debajo de la corteza terrestre se encuentran  gases y otros materiales muy comprimidos que la presionan hasta  agrietarla y deformarla.<\/span><\/div>\n<\/div>\n<div style=\"margin: 0px;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><\/span><\/div>\n<\/div>\n<div style=\"margin: 0px;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">&nbsp;&nbsp; &nbsp;Las fuerzas internas de la Tierra, o agentes internos, provocan los&nbsp;<b>terremotos&nbsp;<\/b>y los&nbsp;<b>volcanes<\/b>.<\/span><\/div>\n<div class=\"separator\" style=\"clear: both; margin: 0px; text-align: justify;\"><\/div>\n<div>\n<div style=\"margin: 0px;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><\/span><\/div>\n<div style=\"text-align: justify;\">\n<div style=\"margin: 0px;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><b>A. Los terremotos<\/b><\/span><\/div>\n<\/div>\n<div style=\"text-align: justify;\">\n<div style=\"margin: 0px;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">&nbsp;&nbsp; &nbsp;El movimiento se propaga en todas direcciones en forma de&nbsp;<\/span><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><i>ondas s\u00edsmicas<\/i><\/span><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">, parecidas a las que se forman, por ejemplo, cuando lanzamos una piedra a un lago.&nbsp;<\/span><\/div>\n<\/div>\n<div style=\"text-align: justify;\">\n<div style=\"margin: 0px;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">&nbsp;&nbsp; &nbsp;En un terremoto se distinguen 2 zonas:<\/span><\/div>\n<\/div>\n<div style=\"text-align: center;\">\n<div class=\"separator\" style=\"clear: both; margin: 0px; text-align: justify;\"><\/div>\n<div style=\"text-align: center;\">\n<div style=\"margin: 0px;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><span class=\"Apple-style-span\" style=\"font-family: 'Times New Roman';\"><a href=\"http:\/\/1.bp.blogspot.com\/__iXhFNsMosg\/TM3IN8rwBYI\/AAAAAAAAACk\/wlfqx5ssOPU\/s1600\/terremoto.jpg\" style=\"margin-left: 1em; margin-right: 1em;\"><img loading=\"lazy\" decoding=\"async\" border=\"0\" height=\"440\" src=\"http:\/\/1.bp.blogspot.com\/__iXhFNsMosg\/TM3IN8rwBYI\/AAAAAAAAACk\/wlfqx5ssOPU\/s640\/terremoto.jpg\" style=\"cursor: move;\" width=\"640\" \/><\/a><\/span><\/span><\/div>\n<\/div>\n<\/div>\n<div style=\"text-align: justify;\">\n<div style=\"margin: 0px;\">&nbsp;&nbsp; &nbsp;<span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">Los terremotos se producen como consecuencia del movimiento de placas que configuran la corteza terrestre.<\/span><\/div>\n<\/div>\n<div style=\"text-align: justify;\">\n<div style=\"margin: 0px;\">&nbsp;&nbsp; &nbsp;<span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">Mientras  dura el terremoto, normalmente unos pocos segundos, el suelo tiembla y  se producen unos efectos que pueden ser devastadores.<\/span><\/div>\n<\/div>\n<div style=\"text-align: justify;\">\n<div style=\"margin: 0px;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><br \/><\/span><\/div>\n<\/div>\n<div class=\"separator\" style=\"clear: both; margin: 0px; text-align: center;\"><a href=\"http:\/\/1.bp.blogspot.com\/__iXhFNsMosg\/TM3I5IKnnpI\/AAAAAAAAACs\/TiU8sGKcf_Y\/s1600\/An%C3%B3nimo.jpg\" style=\"clear: left; float: left; margin-bottom: 1em; margin-right: 1em; text-align: justify;\"><img decoding=\"async\" border=\"0\" src=\"http:\/\/1.bp.blogspot.com\/__iXhFNsMosg\/TM3I5IKnnpI\/AAAAAAAAACs\/TiU8sGKcf_Y\/s1600\/An%C3%B3nimo.jpg\" style=\"cursor: move;\" \/><\/a><\/div>\n<div style=\"text-align: justify;\">\n<div style=\"text-align: left;\">\n<div style=\"text-align: justify;\">\n<div style=\"margin: 0px;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><b><span class=\"Apple-style-span\" style=\"font-size: x-small;\">Puedes ver los efectos de un terremoto en la simulaci\u00f3n que aparece en el siguiente enlace. Debes pulsar \u00abSimulaci\u00f3n\u00bb.&nbsp;<\/span><\/b><\/span><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><b><span class=\"Apple-style-span\" style=\"font-size: x-small;\">ENLACE:&nbsp;<a href=\"http:\/\/www.ucoerm.net\/public\/terremoto.swf\">http:\/\/www.ucoerm.net\/public\/terremoto.swf<\/a><\/span><\/b><\/span><\/div>\n<\/div>\n<\/div>\n<\/div>\n<div style=\"text-align: justify;\">\n<div style=\"margin: 0px;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><br \/><\/span><\/div>\n<\/div>\n<div class=\"separator\" style=\"clear: both; margin: 0px; text-align: justify;\"><b><span class=\"Apple-style-span\" style=\"font-family: 'Times New Roman'; font-weight: normal;\">&nbsp;<\/span><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><span class=\"Apple-style-span\" style=\"font-size: x-small;\"><span class=\"Apple-style-span\" style=\"color: blue;\">Puedes o\u00edr un documental sobre las cat\u00e1strofes que puede provocar un terremoto.<\/span><\/span><\/span><\/b><\/div>\n<div class=\"separator\" style=\"clear: both; margin: 0px; text-align: justify;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><b><span class=\"Apple-style-span\" style=\"font-family: 'Times New Roman'; font-weight: normal;\"><br \/><\/span><\/b><\/span><\/div>\n<div class=\"separator\" style=\"clear: both; margin: 0px; text-align: justify;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><b>B. Los volcanes<\/b><\/span><\/div>\n<div style=\"text-align: justify;\">\n<div style=\"margin: 0px;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">&nbsp;&nbsp; &nbsp;<\/span><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">&nbsp;&nbsp; &nbsp;Cuando alguna de las grietas de la corteza terrestre es tan profunda que alcanza las zonas donde hay&nbsp;<i>magma<\/i>, \u00e9ste asciende por ella como una&nbsp;<i>chimenea&nbsp;<\/i>y, a trav\u00e9s del&nbsp;<i>cr\u00e1ter<\/i>, puede salir al exterior en forma de&nbsp;<i>erupci\u00f3n volc\u00e1nica<\/i>.<\/span><\/div>\n<div class=\"separator\" style=\"clear: both; margin: 0px; text-align: center;\"><a href=\"http:\/\/4.bp.blogspot.com\/__iXhFNsMosg\/TM3LB1EX6-I\/AAAAAAAAAC0\/YTBUrqI_K5U\/s1600\/volcan.jpg\" style=\"margin-left: 1em; margin-right: 1em;\"><img loading=\"lazy\" decoding=\"async\" border=\"0\" height=\"532\" src=\"http:\/\/4.bp.blogspot.com\/__iXhFNsMosg\/TM3LB1EX6-I\/AAAAAAAAAC0\/YTBUrqI_K5U\/s640\/volcan.jpg\" style=\"cursor: move;\" width=\"640\" \/><\/a><\/div>\n<div style=\"margin: 0px;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><br \/><\/span><\/div>\n<\/div>\n<div style=\"text-align: justify;\">\n<div style=\"text-align: center;\">\n<div style=\"text-align: justify;\">\n<div style=\"margin: 0px;\">&nbsp;&nbsp; &nbsp;<span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">En  las erupciones volc\u00e1nicas se expulsan gases, cenizas, piedras y lava  incandescente. En contacto con el aire, estos materiales se enfr\u00edan, se  depositan y forman&nbsp;<i>conos volc\u00e1nicos<\/i>.<\/span><\/div>\n<\/div>\n<\/div>\n<div style=\"text-align: center;\">\n<div style=\"text-align: justify;\">\n<div style=\"margin: 0px;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><br \/><\/span><\/div>\n<\/div>\n<\/div>\n<div style=\"margin: 0px;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><\/span><\/div>\n<div style=\"font-family: 'Times New Roman'; margin: 0px; text-align: center;\">\n<div style=\"text-align: center;\">\n<div style=\"margin: 0px;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><\/span><\/div>\n<\/div>\n<\/div>\n<\/div>\n<div style=\"text-align: justify;\">\n<div style=\"margin: 0px;\"><span class=\"Apple-style-span\" style=\"font-family: 'Times New Roman';\">&nbsp;<\/span><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><span class=\"Apple-style-span\" style=\"font-size: x-small;\"><span class=\"Apple-style-span\" style=\"color: blue;\"><b>Puedes o\u00edr un documental sobre las cat\u00e1strofes que puede provocar un Volc\u00e1n.<\/b><\/span><\/span><\/span><\/div>\n<div style=\"margin: 0px;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><br \/><\/span><\/div>\n<\/div>\n<div style=\"text-align: justify;\">\n<div style=\"margin: 0px;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><b>2.2. LOS AGENTES INTERNOS.<\/b><\/span><\/div>\n<\/div>\n<div style=\"text-align: justify;\">\n<div style=\"margin: 0px;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">&nbsp;&nbsp; &nbsp;Las formas del relieve tambi\u00e9n son el resultado de los agentes externos: agua, viento, vegetaci\u00f3n\u2026&nbsp;<\/span><\/div>\n<div style=\"margin: 0px;\"><\/div>\n<ul>\n<li><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">El&nbsp;<\/span><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><b>agua<\/b><\/span><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">,  principal agente modelador del paisaje, puede actuar intensamente y de  diversas maneras: el agua de lluvia, el agua helada, las olas, las  corrientes marinas&#8230;<\/span><\/li>\n<\/ul>\n<\/div>\n<div style=\"font-family: Arial,Helvetica,sans-serif; text-align: center;\">\n<div style=\"text-align: center;\">\n<div style=\"margin: 0px;\"><span class=\"Apple-style-span\" style=\"font-family: 'Times New Roman';\"><a href=\"http:\/\/1.bp.blogspot.com\/__iXhFNsMosg\/TM3NEnxnEmI\/AAAAAAAAADE\/BKV56gwXiyQ\/s1600\/erosion+agua.jpg\" style=\"margin-left: 1em; margin-right: 1em;\"><img loading=\"lazy\" decoding=\"async\" border=\"0\" height=\"210\" src=\"http:\/\/1.bp.blogspot.com\/__iXhFNsMosg\/TM3NEnxnEmI\/AAAAAAAAADE\/BKV56gwXiyQ\/s320\/erosion+agua.jpg\" width=\"320\" \/><\/a>&nbsp;<\/span><span class=\"Apple-style-span\" style=\"font-family: 'Times New Roman';\"><\/span><\/div>\n<\/div>\n<\/div>\n<ul>\n<li style=\"text-align: justify;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">El&nbsp;<\/span><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><b>viento&nbsp;<\/b><\/span><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">desgasta las rocas y las erosiona.&nbsp;<\/span><\/li>\n<\/ul>\n<div style=\"font-family: Arial,Helvetica,sans-serif; text-align: center;\">\n<div style=\"text-align: center;\">\n<div style=\"margin: 0px;\"><span class=\"Apple-style-span\" style=\"font-family: 'Times New Roman';\"><a href=\"http:\/\/3.bp.blogspot.com\/__iXhFNsMosg\/TM3M0zkNM3I\/AAAAAAAAADA\/2QwQDTh9zks\/s1600\/Erosion+viento.jpg\" style=\"margin-left: 1em; margin-right: 1em;\"><img loading=\"lazy\" decoding=\"async\" border=\"0\" height=\"212\" src=\"http:\/\/3.bp.blogspot.com\/__iXhFNsMosg\/TM3M0zkNM3I\/AAAAAAAAADA\/2QwQDTh9zks\/s320\/Erosion+viento.jpg\" width=\"320\" \/><\/a>&nbsp;<\/span><span class=\"Apple-style-span\" style=\"font-family: 'Times New Roman';\"><\/span><\/div>\n<\/div>\n<\/div>\n<ul>\n<li style=\"text-align: justify;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">La&nbsp;<b>vegetaci\u00f3n&nbsp;<\/b>tambi\u00e9n contribuye a la formaci\u00f3n del relieve terrestre.&nbsp;<\/span><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">Las ra\u00edces de plantas y \u00e1rboles pueden ayudar a romper las rocas, pero tambi\u00e9n a fijar el suelo de la ladera de las monta\u00f1as.<\/span><\/li>\n<\/ul>\n<div style=\"margin-left: 1em; margin-right: 1em; text-align: center;\">\n<div style=\"text-align: center;\">\n<div style=\"margin: 0px;\"><a href=\"http:\/\/2.bp.blogspot.com\/__iXhFNsMosg\/TM3MZfxwoLI\/AAAAAAAAAC4\/IzC69qX12PY\/s1600\/Erosion+vegetacion.gif\" style=\"margin-left: 1em; margin-right: 1em;\"><img loading=\"lazy\" decoding=\"async\" border=\"0\" height=\"317\" src=\"http:\/\/2.bp.blogspot.com\/__iXhFNsMosg\/TM3MZfxwoLI\/AAAAAAAAAC4\/IzC69qX12PY\/s320\/Erosion+vegetacion.gif\" style=\"cursor: move;\" width=\"320\" \/><\/a>&nbsp;<\/div>\n<\/div>\n<\/div>\n<\/div>\n<\/div>\n<\/div>\n<\/div>\n<\/div>\n<div>\n<div style=\"text-align: center;\">\n<div style=\"margin: 0px;\">\n<div style=\"text-align: justify;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><b><span class=\"Apple-style-span\" style=\"color: blue;\">RESUMEN:  Puedes ver un cuadro resumen en la siguiente presentaci\u00f3n. Lo primero  que tienes que hacer es pinchar en \u00abVIEW FULL SIZE\u00bb: y luego s\u00f3lo debes  pinchar y dejar pulsado sobre las im\u00e1gines el bot\u00f3n del rat\u00f3n para que  se ampl\u00eden.<\/span><\/b><\/span><\/div>\n<\/div>\n<\/div>\n<\/div>\n<div style=\"text-align: center;\">\n<div style=\"text-align: justify;\">\n<div style=\"text-align: center;\">\n<div style=\"text-align: justify;\">\n<div style=\"margin: 0px;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><span class=\"Apple-style-span\" style=\"font-size: x-small;\"><b><span class=\"Apple-style-span\" style=\"color: blue;\"><br \/><\/span><\/b><\/span><\/span><\/div>\n<\/div>\n<\/div>\n<\/div>\n<\/div>\n<div style=\"text-align: center;\">\n<div style=\"text-align: justify;\">\n<div style=\"margin: 0px;\"><\/div>\n<\/div>\n<\/div>\n<div style=\"text-align: center;\">\n<div style=\"text-align: center;\">\n<div style=\"margin: 0px;\"><img loading=\"lazy\" decoding=\"async\" border=\"0\" height=\"0\" src=\"http:\/\/counters.gigya.com\/wildfire\/IMP\/CXNID=2000002.0NXC\/bT*xJmx*PTEyODg2MzM2OTAzMDUmcHQ9MTI4ODYzMzY5MzE2NCZwPTIyMTYzMSZkPSZnPTImbz*1MDJlOTExYzczNDI*MTA3Yjhk\/YTVkYWViNmM3NWU2NCZvZj*w.gif\" style=\"cursor: move; height: 0px; visibility: hidden; width: 0px;\" width=\"0\" \/><\/div>\n<\/div>\n<div style=\"text-align: center;\">\n<div style=\"margin: 0px;\"><\/div>\n<\/div>\n<div style=\"text-align: center;\">\n<div style=\"margin: 0px;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><b><span class=\"Apple-style-span\" style=\"color: yellow;\"><span class=\"Apple-style-span\" style=\"font-size: medium;\">TALLER 3. LAS FORMAS DE RELIEVE<\/span><\/span><\/b><\/span><\/div>\n<\/div>\n<div style=\"text-align: justify;\">\n<div style=\"margin: 0px;\">\n<div style=\"margin: 0px;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><b>3. LAS FORMAS DEL RELIEVE.<\/b><\/span><\/div>\n<\/div>\n<\/div>\n<div style=\"text-align: justify;\">\n<div style=\"margin: 0px;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">&nbsp;&nbsp;  &nbsp;La acci\u00f3n combinada de los agentes internos (terremotos y volcanes) y  externos (agua, viento, vegetaci\u00f3n y el ser humano) del modelado  terrestre crea distintas formas del relieve.<\/span><\/div>\n<\/div>\n<div class=\"separator\" style=\"clear: both; margin: 0px; text-align: justify;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">&nbsp;&nbsp;  &nbsp;Adem\u00e1s de las monta\u00f1as y cordilleras hay otras muchas formas del  modelado de la superficie terrestre y del fondo de los oc\u00e9anos.<\/span><\/div>\n<div>\n<div style=\"text-align: justify;\">\n<div style=\"margin: 0px;\"><\/div>\n<\/div>\n<div class=\"separator\" style=\"clear: both; margin: 0px; text-align: center;\"><a href=\"http:\/\/3.bp.blogspot.com\/__iXhFNsMosg\/TNaFiE5Ub5I\/AAAAAAAAADs\/TwL53e-mDMg\/s1600\/formas+de+la+Tierra.jpg\" style=\"margin-left: 1em; margin-right: 1em;\"><img loading=\"lazy\" decoding=\"async\" border=\"0\" height=\"221\" src=\"http:\/\/3.bp.blogspot.com\/__iXhFNsMosg\/TNaFiE5Ub5I\/AAAAAAAAADs\/TwL53e-mDMg\/s400\/formas+de+la+Tierra.jpg\" style=\"cursor: move;\" width=\"400\" \/><\/a><\/div>\n<ul>\n<li style=\"font-family: Arial,Helvetica,sans-serif; text-align: justify;\"><b>Monta\u00f1a<\/b>. Elevaci\u00f3n natural del terreno de m\u00e1s de 700 metros. Se agrupan formando grandes&nbsp;<i style=\"font-weight: bold;\">cordilleras&nbsp;<\/i>o<i style=\"font-weight: bold;\">&nbsp;sierras<\/i>, como los Andes o Sierra Morena.<\/li>\n<\/ul>\n<div class=\"separator\" style=\"clear: both; margin: 0px; text-align: center;\"><a href=\"http:\/\/3.bp.blogspot.com\/__iXhFNsMosg\/TNaJw_nVyEI\/AAAAAAAAADw\/SF4BLSRraSM\/s1600\/Aconcagua.jpg\" style=\"margin-left: 1em; margin-right: 1em;\"><img loading=\"lazy\" decoding=\"async\" border=\"0\" height=\"200\" src=\"http:\/\/3.bp.blogspot.com\/__iXhFNsMosg\/TNaJw_nVyEI\/AAAAAAAAADw\/SF4BLSRraSM\/s200\/Aconcagua.jpg\" style=\"cursor: move;\" width=\"134\" \/><\/a>&nbsp;<a href=\"http:\/\/2.bp.blogspot.com\/__iXhFNsMosg\/TNaJ_8JBGLI\/AAAAAAAAAD0\/5kxbgcrjPus\/s1600\/k2.jpg\" style=\"margin-left: 1em; margin-right: 1em;\"><img loading=\"lazy\" decoding=\"async\" border=\"0\" height=\"128\" src=\"http:\/\/2.bp.blogspot.com\/__iXhFNsMosg\/TNaJ_8JBGLI\/AAAAAAAAAD0\/5kxbgcrjPus\/s200\/k2.jpg\" style=\"cursor: move;\" width=\"200\" \/><\/a>&nbsp;<\/div>\n<ul>\n<li style=\"font-family: Arial,Helvetica,sans-serif; text-align: justify;\"><b>Llanuras<\/b>. Es una espacio con poca o ninguna variaci\u00f3n en la altura de la superficie, como la Gran Llanura Europea.&nbsp;<\/li>\n<\/ul>\n<div class=\"separator\" style=\"clear: both; margin: 0px; text-align: center;\"><a href=\"http:\/\/2.bp.blogspot.com\/__iXhFNsMosg\/TNaLEGvLQTI\/AAAAAAAAAD4\/4phhCuscLXU\/s1600\/Llanura+2.jpg\" style=\"margin-left: 1em; margin-right: 1em;\"><img loading=\"lazy\" decoding=\"async\" border=\"0\" height=\"149\" src=\"http:\/\/2.bp.blogspot.com\/__iXhFNsMosg\/TNaLEGvLQTI\/AAAAAAAAAD4\/4phhCuscLXU\/s200\/Llanura+2.jpg\" style=\"cursor: move;\" width=\"200\" \/><\/a><a href=\"http:\/\/4.bp.blogspot.com\/__iXhFNsMosg\/TNaLE-P9qwI\/AAAAAAAAAD8\/Y2vZOtXlXbA\/s1600\/llanura.jpg\" style=\"margin-left: 1em; margin-right: 1em;\"><img loading=\"lazy\" decoding=\"async\" border=\"0\" height=\"150\" src=\"http:\/\/4.bp.blogspot.com\/__iXhFNsMosg\/TNaLE-P9qwI\/AAAAAAAAAD8\/Y2vZOtXlXbA\/s200\/llanura.jpg\" style=\"cursor: move;\" width=\"200\" \/><\/a><\/div>\n<ul>\n<li style=\"text-align: justify;\">&nbsp;<span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><b>Mesetas<\/b><\/span><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">. Su superficie tambi\u00e9n es plana, pero a diferencia de las llanuras su altitud es mayor, como la Meseta Castellana.<\/span><\/li>\n<\/ul>\n<div style=\"text-align: justify;\">\n<div style=\"margin: 0px;\"><\/div>\n<\/div>\n<div class=\"separator\" style=\"clear: both; margin: 0px; text-align: center;\"><a href=\"http:\/\/3.bp.blogspot.com\/__iXhFNsMosg\/TNaL45BPxkI\/AAAAAAAAAEA\/VSQguwCUsOc\/s1600\/meseta-rusia.jpg\" style=\"margin-left: 1em; margin-right: 1em;\"><img loading=\"lazy\" decoding=\"async\" border=\"0\" height=\"150\" src=\"http:\/\/3.bp.blogspot.com\/__iXhFNsMosg\/TNaL45BPxkI\/AAAAAAAAAEA\/VSQguwCUsOc\/s200\/meseta-rusia.jpg\" style=\"cursor: move;\" width=\"200\" \/><\/a><a href=\"http:\/\/3.bp.blogspot.com\/__iXhFNsMosg\/TNaL7N8z-0I\/AAAAAAAAAEE\/MS7PywnzHs0\/s1600\/meseta.jpg\" style=\"margin-left: 1em; margin-right: 1em;\"><img loading=\"lazy\" decoding=\"async\" border=\"0\" height=\"150\" src=\"http:\/\/3.bp.blogspot.com\/__iXhFNsMosg\/TNaL7N8z-0I\/AAAAAAAAAEE\/MS7PywnzHs0\/s200\/meseta.jpg\" style=\"cursor: move;\" width=\"200\" \/><\/a><\/div>\n<ul>\n<li>&nbsp;<span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><b>Valles<\/b><\/span><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">. En general, es una depresi\u00f3<\/span><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">n de la superficie terrestre &nbsp;entre dos vertientes, por donde discurre habitualmente un r\u00edo.<\/span><\/li>\n<\/ul>\n<div class=\"separator\" style=\"clear: both; margin: 0px; text-align: center;\"><a href=\"http:\/\/3.bp.blogspot.com\/__iXhFNsMosg\/TNaM9jVp8AI\/AAAAAAAAAEI\/Ofgc1xnTrH0\/s1600\/valle.jpg\" style=\"margin-left: 1em; margin-right: 1em;\"><img loading=\"lazy\" decoding=\"async\" border=\"0\" height=\"136\" src=\"http:\/\/3.bp.blogspot.com\/__iXhFNsMosg\/TNaM9jVp8AI\/AAAAAAAAAEI\/Ofgc1xnTrH0\/s200\/valle.jpg\" style=\"cursor: move;\" width=\"200\" \/><\/a><a href=\"http:\/\/3.bp.blogspot.com\/__iXhFNsMosg\/TNaM-FFMcgI\/AAAAAAAAAEM\/MK4X5TaCbbk\/s1600\/valle+2.jpg\" style=\"margin-left: 1em; margin-right: 1em;\"><img loading=\"lazy\" decoding=\"async\" border=\"0\" height=\"150\" src=\"http:\/\/3.bp.blogspot.com\/__iXhFNsMosg\/TNaM-FFMcgI\/AAAAAAAAAEM\/MK4X5TaCbbk\/s200\/valle+2.jpg\" style=\"cursor: move;\" width=\"200\" \/><\/a><\/div>\n<ul>\n<li style=\"text-align: justify;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><b>Islas<\/b><\/span><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">: emergen en el mar, pueden ser parte del relieve submarino o tener origen volc\u00e1nico o coralino.<\/span>&nbsp;<\/li>\n<\/ul>\n<div class=\"separator\" style=\"clear: both; margin: 0px; text-align: center;\"><a href=\"http:\/\/4.bp.blogspot.com\/__iXhFNsMosg\/TNaNj42CfDI\/AAAAAAAAAEQ\/8-BxIfSljAA\/s1600\/Isla+Coelleira+3.jpg\" style=\"margin-left: 1em; margin-right: 1em;\"><img loading=\"lazy\" decoding=\"async\" border=\"0\" height=\"135\" src=\"http:\/\/4.bp.blogspot.com\/__iXhFNsMosg\/TNaNj42CfDI\/AAAAAAAAAEQ\/8-BxIfSljAA\/s200\/Isla+Coelleira+3.jpg\" style=\"cursor: move;\" width=\"200\" \/><\/a><a href=\"http:\/\/3.bp.blogspot.com\/__iXhFNsMosg\/TNaNly1eVUI\/AAAAAAAAAEU\/6EryOM-x2UA\/s1600\/isla.jpeg\" style=\"margin-left: 1em; margin-right: 1em;\"><img loading=\"lazy\" decoding=\"async\" border=\"0\" height=\"112\" src=\"http:\/\/3.bp.blogspot.com\/__iXhFNsMosg\/TNaNly1eVUI\/AAAAAAAAAEU\/6EryOM-x2UA\/s200\/isla.jpeg\" style=\"cursor: move;\" width=\"200\" \/><\/a><\/div>\n<ul>\n<li style=\"text-align: justify;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><b>Archipi\u00e9lagos<\/b>: son grupos de islas.<\/span><\/li>\n<\/ul>\n<div class=\"separator\" style=\"clear: both; margin: 0px; text-align: center;\"><a href=\"http:\/\/2.bp.blogspot.com\/__iXhFNsMosg\/TNaOLiDxTvI\/AAAAAAAAAEY\/k7C2JJPpJ_s\/s1600\/archipelago.jpg\" style=\"margin-left: 1em; margin-right: 1em;\"><img loading=\"lazy\" decoding=\"async\" border=\"0\" height=\"138\" src=\"http:\/\/2.bp.blogspot.com\/__iXhFNsMosg\/TNaOLiDxTvI\/AAAAAAAAAEY\/k7C2JJPpJ_s\/s200\/archipelago.jpg\" style=\"cursor: move;\" width=\"200\" \/><\/a><a href=\"http:\/\/3.bp.blogspot.com\/__iXhFNsMosg\/TNaOL9wzumI\/AAAAAAAAAEc\/9jQAK-rCpn0\/s1600\/archipelago2.jpg\" style=\"margin-left: 1em; margin-right: 1em;\"><img loading=\"lazy\" decoding=\"async\" border=\"0\" height=\"139\" src=\"http:\/\/3.bp.blogspot.com\/__iXhFNsMosg\/TNaOL9wzumI\/AAAAAAAAAEc\/9jQAK-rCpn0\/s200\/archipelago2.jpg\" style=\"cursor: move;\" width=\"200\" \/><\/a><\/div>\n<ul>\n<li style=\"text-align: justify;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><b>Cabos:&nbsp;<\/b>Saliente de la tierra que se interna hacia el mar.<\/span><\/li>\n<\/ul>\n<div style=\"margin: 0px;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><\/span><\/div>\n<div style=\"text-align: center;\">\n<div style=\"text-align: center;\">\n<div style=\"margin: 0px;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><b>&nbsp;<\/b><a href=\"http:\/\/4.bp.blogspot.com\/__iXhFNsMosg\/TNaO2kUA3PI\/AAAAAAAAAEg\/e4_yo8ENb_M\/s1600\/cabo.jpg\" style=\"margin-left: 1em; margin-right: 1em;\"><img loading=\"lazy\" decoding=\"async\" border=\"0\" height=\"135\" src=\"http:\/\/4.bp.blogspot.com\/__iXhFNsMosg\/TNaO2kUA3PI\/AAAAAAAAAEg\/e4_yo8ENb_M\/s200\/cabo.jpg\" style=\"cursor: move;\" width=\"200\" \/><\/a>&nbsp;<a href=\"http:\/\/3.bp.blogspot.com\/__iXhFNsMosg\/TNaO22pK9JI\/AAAAAAAAAEk\/vyxeisyfJQM\/s1600\/Cabo2.jpg\" style=\"margin-left: 1em; margin-right: 1em;\"><img loading=\"lazy\" decoding=\"async\" border=\"0\" height=\"150\" src=\"http:\/\/3.bp.blogspot.com\/__iXhFNsMosg\/TNaO22pK9JI\/AAAAAAAAAEk\/vyxeisyfJQM\/s200\/Cabo2.jpg\" style=\"cursor: move;\" width=\"200\" \/><\/a><\/span><\/div>\n<\/div>\n<\/div>\n<ul>\n<li style=\"text-align: justify;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><b>Pen\u00ednsulas<\/b>: Es una extensi\u00f3n de tierra rodeada de mar por todas partes excepto por una que la une a un territorio m\u00e1s grande.<\/span><\/li>\n<\/ul>\n<div class=\"separator\" style=\"clear: both; margin: 0px; text-align: center;\"><a href=\"http:\/\/4.bp.blogspot.com\/__iXhFNsMosg\/TNaPkVGJ4PI\/AAAAAAAAAEo\/_gnKDOduOeI\/s1600\/peninsula.jpg\" style=\"margin-left: 1em; margin-right: 1em;\"><img loading=\"lazy\" decoding=\"async\" border=\"0\" height=\"157\" src=\"http:\/\/4.bp.blogspot.com\/__iXhFNsMosg\/TNaPkVGJ4PI\/AAAAAAAAAEo\/_gnKDOduOeI\/s200\/peninsula.jpg\" style=\"cursor: move;\" width=\"200\" \/><\/a><a href=\"http:\/\/4.bp.blogspot.com\/__iXhFNsMosg\/TNaPnFDfSKI\/AAAAAAAAAEs\/CRvlbsjsk0I\/s1600\/peninsula2.jpg\" style=\"margin-left: 1em; margin-right: 1em;\"><img loading=\"lazy\" decoding=\"async\" border=\"0\" height=\"150\" src=\"http:\/\/4.bp.blogspot.com\/__iXhFNsMosg\/TNaPnFDfSKI\/AAAAAAAAAEs\/CRvlbsjsk0I\/s200\/peninsula2.jpg\" style=\"cursor: move;\" width=\"200\" \/><\/a><\/div>\n<ul>\n<li style=\"text-align: justify;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><b>Golfos, r\u00edas y fiordos<\/b><\/span><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">: son entrantes de agua en la tierra muy aptos para navegar.<\/span><\/li>\n<\/ul>\n<div style=\"text-align: justify;\">\n<div style=\"margin: 0px;\">\n<div style=\"text-align: center;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><b><span class=\"Apple-style-span\" style=\"color: yellow;\"><span class=\"Apple-style-span\" style=\"font-size: medium;\">TALLER 4. CONTINENTES Y OC\u00c9ANOS<\/span><\/span><\/b> <\/span><\/div>\n<\/div>\n<\/div>\n<div style=\"margin: 0px;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><\/span><\/div>\n<div style=\"text-align: justify;\">\n<div style=\"margin: 0px;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><b>4. LOS CONTINENTES Y OC\u00c9ANOS.<\/b><\/span><\/div>\n<div style=\"margin: 0px;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><b>4.1. CONTINENTES<\/b><\/span><\/div>\n<div style=\"margin: 0px;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><b>&nbsp;&nbsp; &nbsp;<\/b>Los continentes son grandes extensiones de tierras emergidas que separan los oc\u00e9anos.<\/span><\/div>\n<div>\n<ul>\n<li style=\"text-align: justify;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><b><span class=\"Apple-style-span\" style=\"color: white;\"><span class=\"Apple-style-span\" style=\"background-color: black;\">\u00c1frica<\/span><\/span><\/b><\/span><\/li>\n<\/ul>\n<\/div>\n<div>\n<div style=\"margin: 0px;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">&nbsp;&nbsp; &nbsp;\u00c1frica est\u00e1 separada de Europa por el Mediterr\u00e1neo, y de Asia por el mar Rojo. El canal de Suez une ambos mares.<\/span><\/div>\n<ul>\n<li style=\"text-align: justify;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><b><span class=\"Apple-style-span\" style=\"background-color: lime;\"><span class=\"Apple-style-span\" style=\"color: white;\">Am\u00e9rica<\/span><\/span><\/b><\/span><\/li>\n<p><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><\/span><\/ul>\n<div style=\"text-align: justify;\">\n<div style=\"margin: 0px;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">&nbsp;&nbsp;  &nbsp;Am\u00e9rica se extiende, a lo largo de 15000 km, por los dos hemisferios  de la Tierra. Separa los dos grandes oc\u00e9anos del planeta, el Atl\u00e1ntico y  el Pac\u00edfico.&nbsp;Habitualmente dividimos Am\u00e9rica en dos subcontinentes:  Am\u00e9rica del Norte y Am\u00e9rica del Sur. Estos dos subcontinentes est\u00e1n  unidos por el istmo de Am\u00e9rica Central.<b><br \/><\/b><\/span><\/div>\n<\/div>\n<\/div>\n<div>\n<ul>\n<li style=\"text-align: justify;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><b><span class=\"Apple-style-span\" style=\"background-color: yellow;\"><span class=\"Apple-style-span\" style=\"color: white;\">Asia<\/span><\/span><\/b><\/span><\/li>\n<\/ul>\n<div style=\"text-align: justify;\">\n<div style=\"margin: 0px;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">&nbsp;&nbsp; El continente asi\u00e1tico es una gran masa de tierra situada en la parte oriental de Eurasia.<\/span><\/div>\n<\/div>\n<ul>\n<li style=\"text-align: justify;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><b><span class=\"Apple-style-span\" style=\"background-color: blue;\"><span class=\"Apple-style-span\" style=\"color: white;\">Europa<\/span><\/span><\/b><\/span><\/li>\n<p><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><\/span><\/ul>\n<\/div>\n<div>\n<div style=\"text-align: justify;\">\n<div style=\"margin: 0px;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">&nbsp;&nbsp;  Europa est\u00e1 situada en la parte occidental de Eurasia.&nbsp;Las cordilleras  de los Urales y del C\u00e1ucaso, y los mares Caspio y Negro marcan los  l\u00edmites entre ambos continentes. El mar Mediterr\u00e1neo es el l\u00edmite entre  Europa y \u00c1frica.<b><br \/><\/b><\/span><\/div>\n<\/div>\n<\/div>\n<div>\n<ul>\n<li style=\"text-align: justify;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><b><span class=\"Apple-style-span\" style=\"background-color: red;\"><span class=\"Apple-style-span\" style=\"color: white;\">Ocean\u00eda<\/span><\/span><\/b><\/span><\/li>\n<\/ul>\n<div style=\"text-align: justify;\">\n<div style=\"margin: 0px;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">&nbsp;&nbsp;  &nbsp;M\u00e1s de 10000 islas repartidas por el oc\u00e9ano Pac\u00edfico forman Ocean\u00eda.  Habitualmente distinguimos cuatro grandes conjuntos: Australasia,  Melanesia, Micronesia y Polinesia.<b><br \/><\/b><\/span><\/div>\n<\/div>\n<\/div>\n<div>\n<ul>\n<li style=\"text-align: justify;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><b><span class=\"Apple-style-span\" style=\"background-color: cyan;\"><span class=\"Apple-style-span\" style=\"color: white;\">Ant\u00e1rtida<\/span><\/span><\/b><\/span><\/li>\n<\/ul>\n<div style=\"text-align: justify;\">\n<div style=\"margin: 0px;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">&nbsp;&nbsp;  &nbsp;Situada en el Polo Sur, la Ant\u00e1rtida est\u00e1 rodeada por los oc\u00e9anos  Pac\u00edfico, Atl\u00e1ntico e \u00cdndico. Las temperaturas extremas, de hasta \u201365\u00b0C,  y los fuertes vientos hacen que la vida all\u00ed resulte casi imposible.<\/span><\/div>\n<\/div>\n<\/div>\n<div>\n<div style=\"text-align: justify;\">\n<div style=\"margin: 0px;\">\n<div style=\"text-align: center;\"><\/p>\n<ul>\n<li style=\"text-align: justify;\"><span class=\"Apple-style-span\" style=\"color: blue; font-family: Arial, Helvetica, sans-serif;\"><b>Para ver las&nbsp;<a href=\"http:\/\/maps.google.es\/maps\/ms?hl=es&amp;ie=UTF8&amp;msa=0&amp;msid=116054019322439831582.0004933159c881a8d1c93&amp;ll=25.165173,0.703125&amp;spn=150.68083,298.828125&amp;z=1&amp;source=embed\" style=\"text-align: left;\">Formas de relieve en el mundo<\/a>&nbsp;en un mapa m\u00e1s grande pincha en el enlace y en luego en cada uno de los iconos del mapa que se te abra.<\/b><\/span><\/li>\n<\/ul>\n<\/div>\n<p><span class=\"Apple-style-span\" style=\"color: blue;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><\/span><\/span><\/p>\n<div style=\"font-family: 'Times New Roman'; margin: 0px;\">\n<div style=\"margin: 0px; text-align: center;\"><span class=\"Apple-style-span\" style=\"font-size: x-small;\"><span class=\"Apple-style-span\" style=\"font-size: 13px;\"><br \/><\/span><\/span><\/div>\n<\/div>\n<p><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><b>4.2. LOS OC\u00c9ANOS.<\/b><\/span><\/div>\n<\/div>\n<\/div>\n<div>\n<div style=\"text-align: justify;\">\n<div style=\"margin: 0px;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">&nbsp;&nbsp; &nbsp;El 97,21% del agua del planeta es salada y est\u00e1 en:<\/span><\/div>\n<\/div>\n<\/div>\n<div>\n<ul style=\"font-family: Arial,Helvetica,sans-serif;\">\n<li style=\"text-align: justify;\"><b>Oc\u00e9anos<\/b>: grandes masas de agua que separan los continentes; en la Tierra hay cinco.<\/li>\n<li style=\"text-align: justify;\"><b>Mares<\/b>: prolongaci\u00f3n de los oc\u00e9anos en las zonas m\u00e1s cercanas a los continentes.<\/li>\n<\/ul>\n<div style=\"text-align: justify;\">\n<div style=\"margin: 0px;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\">&nbsp;&nbsp; &nbsp;Los oc\u00e9anos de la Tierra son cinco:<\/span><\/div>\n<\/div>\n<ul>\n<li style=\"text-align: justify;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><b>Pac\u00edfico<\/b>: cuenta con numerosas islas volc\u00e1nicas y coralinas, y con las fosas marinas m\u00e1s profundas.<\/span><\/li>\n<p><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><\/p>\n<li style=\"text-align: justify;\"><b>Atl\u00e1ntico<\/b>: es estrecho y alargado, y el menos profundo de todos; tiene muchos mares.<\/li>\n<li style=\"text-align: justify;\"><b>\u00cdndico<\/b>: se extiende entre \u00c1frica y Asia, tiene pocas islas y su profundidad es media.<\/li>\n<li style=\"text-align: justify;\"><b>Glacial \u00c1rtico<\/b>: Rodea el Polo Norte y sus aguas est\u00e1s siempre heladas.<\/li>\n<li style=\"text-align: justify;\"><b>Glacial Ant\u00e1rtico<\/b>: Rodea el Polo Sur y sus aguas est\u00e1n siempre heladas.<\/li>\n<p><\/span><\/ul>\n<div>\n<div style=\"text-align: justify;\">\n<div style=\"margin: 0px;\"><span class=\"Apple-style-span\" style=\"font-family: Arial, Helvetica, sans-serif;\"><b><span class=\"Apple-style-span\" style=\"font-size: x-small;\"><span class=\"Apple-style-span\" style=\"color: blue;\">Puedes aprender un poco m\u00e1s de las formas de relieve, continentes y oc\u00e9anos con los dos siguientes enlaces:<\/span><\/span><\/b><\/span><\/div>\n<\/div>\n<\/div>\n<div>\n<div style=\"text-align: center;\">\n<div style=\"text-align: justify;\">\n<ul>\n<li><span class=\"Apple-style-span\" style=\"color: blue; font-family: Arial, Helvetica, sans-serif;\"><b><a href=\"http:\/\/www.xtec.net\/%7Eealonso\/flash\/mmundi2e.html\">Mapa interactivo<\/a>&nbsp;(Juego)<\/b><\/span><\/li>\n<li><span class=\"Apple-style-span\" style=\"color: blue; font-family: Arial, Helvetica, sans-serif;\"><b><span class=\"Apple-style-span\" style=\"color: black; font-weight: normal;\"><b><span class=\"Apple-style-span\" style=\"color: blue;\">Para ver&nbsp;<a href=\"http:\/\/maps.google.es\/maps\/ms?hl=es&amp;ie=UTF8&amp;msa=0&amp;msid=111783334266156363873.000480c05e15c10441b8e&amp;ll=21.289374,-10.546875&amp;spn=151.485441,298.828125&amp;z=1&amp;source=embed\" style=\"text-align: left;\">Oc\u00e9anos de la Tierra<\/a>&nbsp;en un mapa m\u00e1s grande pincha en el enlace subrayado.<\/span><\/b><\/span><\/b><\/span><\/li>\n<\/ul>\n<\/div>\n<\/div>\n<\/div>\n<\/div>\n<\/div>\n<\/div>\n<\/div>\n","protected":false},"excerpt":{"rendered":"<p>TALLER 1. LA LISTOSFERA1.1. LA ESTRUCTURA DE LA TIERRA.&nbsp;&nbsp;  &nbsp;En nuestro planeta las tierras se hallan repartidas en diversos  continentes o grandes masas de tierra que emergen o sobresalen de los  oc\u00e9anos y mares.&nbsp;&nbsp;  &nbsp;A pe&#8230;<\/p>\n","protected":false},"author":1190,"featured_media":0,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"ngg_post_thumbnail":0,"footnotes":""},"categories":[1],"tags":[12044,1915,12052],"aioseo_notices":[],"_links":{"self":[{"href":"https:\/\/blogsaverroes.juntadeandalucia.es\/geohistoria\/wp-json\/wp\/v2\/posts\/39812"}],"collection":[{"href":"https:\/\/blogsaverroes.juntadeandalucia.es\/geohistoria\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/blogsaverroes.juntadeandalucia.es\/geohistoria\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/blogsaverroes.juntadeandalucia.es\/geohistoria\/wp-json\/wp\/v2\/users\/1190"}],"replies":[{"embeddable":true,"href":"https:\/\/blogsaverroes.juntadeandalucia.es\/geohistoria\/wp-json\/wp\/v2\/comments?post=39812"}],"version-history":[{"count":1,"href":"https:\/\/blogsaverroes.juntadeandalucia.es\/geohistoria\/wp-json\/wp\/v2\/posts\/39812\/revisions"}],"predecessor-version":[{"id":39815,"href":"https:\/\/blogsaverroes.juntadeandalucia.es\/geohistoria\/wp-json\/wp\/v2\/posts\/39812\/revisions\/39815"}],"wp:attachment":[{"href":"https:\/\/blogsaverroes.juntadeandalucia.es\/geohistoria\/wp-json\/wp\/v2\/media?parent=39812"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/blogsaverroes.juntadeandalucia.es\/geohistoria\/wp-json\/wp\/v2\/categories?post=39812"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/blogsaverroes.juntadeandalucia.es\/geohistoria\/wp-json\/wp\/v2\/tags?post=39812"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}