{"id":8395,"date":"2011-12-27T00:05:33","date_gmt":"2011-12-26T23:05:33","guid":{"rendered":"http:\/\/blog.laveredadepuebla.com\/?p=8395"},"modified":"2023-02-10T12:30:54","modified_gmt":"2023-02-10T12:30:54","slug":"dolinas-en-el-karst-de-tamajon","status":"publish","type":"post","link":"https:\/\/blog.sierranortedeguadalajara.com\/?p=8395","title":{"rendered":"Dolinas en el karst de Tamaj\u00f3n"},"content":{"rendered":"<p><a href=\"http:\/\/laveredadepuebla.files.wordpress.com\/2011\/12\/111227-dolinas-3.jpg\"><img loading=\"lazy\" decoding=\"async\" class=\"alignright  wp-image-8396\" title=\"111227 dolinas 3\" src=\"https:\/\/blog.sierranortedeguadalajara.com\/wp-content\/uploads\/2023\/02\/111227-dolinas-3.jpg\" alt=\"\" width=\"210\" height=\"158\" \/><\/a>Aunque<strong><em> <a href=\"http:\/\/platea.pntic.mec.es\/~cmarti3\/GEO\/mod\/karst.htm\">las dolinas <\/a><\/em><\/strong>\u00a0tienen el mismo origen que<a href=\"http:\/\/blog.laveredadepuebla.com\/2010\/04\/08\/%c2%bfcarcava-o-torca\/\"> <strong><em>las torcas<\/em><\/strong><\/a>, estas tiene las paredes m\u00e1s altas y agrestes. Se<strong><em> <\/em><\/strong>forman por el hundimiento de cuevas internas en los karsts.<\/p>\n<p><a href=\"http:\/\/laveredadepuebla.files.wordpress.com\/2011\/12\/111227-dolinas-1.jpg\"><img loading=\"lazy\" decoding=\"async\" class=\"alignleft size-thumbnail wp-image-8397\" title=\"111227 Dolinas 1\" src=\"https:\/\/blog.sierranortedeguadalajara.com\/wp-content\/uploads\/2023\/02\/111227-dolinas-1.jpg\" alt=\"\" width=\"150\" height=\"112\" \/><\/a>La disoluci\u00f3n de calizas provoca que la superficie se hunda hacia el interior y se crean se depresiones circulares con paredes verticales de escasa altura y poco escarpadas.\u00a0 El fondo est\u00e1 relleno de arcillas de descalcificaci\u00f3n, lo que las hace muy f\u00e9rtiles y a veces son utilizadas como tierra de pastos y\/o de labor.<\/p>\n<p><a href=\"http:\/\/laveredadepuebla.files.wordpress.com\/2011\/12\/111227-dolinas-2.jpg\"><img loading=\"lazy\" decoding=\"async\" class=\"alignleft  wp-image-8398\" title=\"111227 dolinas 2\" src=\"https:\/\/blog.sierranortedeguadalajara.com\/wp-content\/uploads\/2023\/02\/111227-dolinas-2.jpg\" alt=\"\" width=\"210\" height=\"158\" \/><\/a>En el <strong><em><a href=\"http:\/\/blog.laveredadepuebla.com\/2011\/12\/19\/el-karst-de-tamajon\/\">karst de Tamaj\u00f3n<\/a> <\/em><\/strong>tenemos de los dos tipos. Sean estas las dolinas m\u00e1s vistosas; las torcas est\u00e1n en el<strong><em> <a href=\"http:\/\/laveredadepuebla.com\/rutasypueblos\/almiruete.pdf\">sabinar<\/a><\/em><\/strong>. Un argumento m\u00e1s para recorrer la <a href=\"http:\/\/laveredadepuebla.com\/rutasypueblos\/enebrales.pdf\"><strong><em>ciudad encantada<\/em><\/strong>.<\/a><\/p>\n<p><strong><em>Lar-ami<\/em><\/strong><\/p>\n","protected":false},"excerpt":{"rendered":"<p>Aunque las dolinas \u00a0tienen el mismo origen que las torcas, estas tiene las paredes m\u00e1s altas y agrestes. Se forman por el hundimiento de cuevas internas en los karsts. La disoluci\u00f3n de calizas provoca que la superficie se hunda hacia el interior y se crean se depresiones circulares con paredes verticales de escasa altura y &hellip; <\/p>\n<p class=\"link-more\"><a href=\"https:\/\/blog.sierranortedeguadalajara.com\/?p=8395\" class=\"more-link\">Seguir leyendo<span class=\"screen-reader-text\"> \u00abDolinas en el karst de Tamaj\u00f3n\u00bb<\/span><\/a><\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[12,17,9],"tags":[70,7,21],"class_list":["post-8395","post","type-post","status-publish","format-standard","hentry","category-actualidad","category-paisajes-y-lugares-de-la-sierra-norte","category-rincones-de-la-sierra-norte","tag-almiruete","tag-naturaleza","tag-tamajon","entry"],"_links":{"self":[{"href":"https:\/\/blog.sierranortedeguadalajara.com\/index.php?rest_route=\/wp\/v2\/posts\/8395","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/blog.sierranortedeguadalajara.com\/index.php?rest_route=\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/blog.sierranortedeguadalajara.com\/index.php?rest_route=\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/blog.sierranortedeguadalajara.com\/index.php?rest_route=\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/blog.sierranortedeguadalajara.com\/index.php?rest_route=%2Fwp%2Fv2%2Fcomments&post=8395"}],"version-history":[{"count":1,"href":"https:\/\/blog.sierranortedeguadalajara.com\/index.php?rest_route=\/wp\/v2\/posts\/8395\/revisions"}],"predecessor-version":[{"id":30851,"href":"https:\/\/blog.sierranortedeguadalajara.com\/index.php?rest_route=\/wp\/v2\/posts\/8395\/revisions\/30851"}],"wp:attachment":[{"href":"https:\/\/blog.sierranortedeguadalajara.com\/index.php?rest_route=%2Fwp%2Fv2%2Fmedia&parent=8395"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/blog.sierranortedeguadalajara.com\/index.php?rest_route=%2Fwp%2Fv2%2Fcategories&post=8395"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/blog.sierranortedeguadalajara.com\/index.php?rest_route=%2Fwp%2Fv2%2Ftags&post=8395"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}