{"id":3883,"date":"2025-12-16T11:56:48","date_gmt":"2025-12-16T11:56:48","guid":{"rendered":"https:\/\/sismoiberica.org\/?post_type=glossary&#038;p=3883"},"modified":"2025-12-16T11:56:48","modified_gmt":"2025-12-16T11:56:48","slug":"escarpament-de-falla","status":"publish","type":"glossary","link":"https:\/\/sismoiberica.org\/es\/glossary\/escarpament-de-falla\/","title":{"rendered":"Escarpament de falla"},"content":{"rendered":"\n<p class=\"wp-block-paragraph\">Ressalt o esgla\u00f3 en la topografia generat pel moviment d&#8217;una falla que trenca i despla\u00e7a la superf\u00edcie del terreny. Els escarpaments de falla tendeixen a observar-se com a lineacions relativament rectil\u00ednies damunt del terreny. Es poden generar escarpaments de falla a partir de falles normals, falles inverses i falles direccionals.<\/p>\n\n\n\n<figure class=\"wp-block-image size-full\"><img fetchpriority=\"high\" decoding=\"async\" width=\"186\" height=\"414\" src=\"https:\/\/sismoiberica.org\/wp-content\/uploads\/2025\/12\/image-1.png\" alt=\"\" class=\"wp-image-3884\" srcset=\"https:\/\/sismoiberica.org\/wp-content\/uploads\/2025\/12\/image-1.png 186w, https:\/\/sismoiberica.org\/wp-content\/uploads\/2025\/12\/image-1-135x300.png 135w\" sizes=\"(max-width: 186px) 100vw, 186px\" \/><\/figure>\n\n\n\n<p class=\"wp-block-paragraph\">Extret de Stewart and Hancock.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">Episodes, Vol 13, 4, 256-263<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Ressalt o esgla\u00f3 en la topografia generat pel moviment d&#8217;una falla que trenca i despla\u00e7a la superf\u00edcie del terreny. Els escarpaments de falla tendeixen a observar-se com a lineacions relativament rectil\u00ednies damunt del terreny. Es poden generar escarpaments de falla a partir de falles normals, falles inverses i falles direccionals. Extret de Stewart and Hancock. [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":0,"parent":0,"template":"","glossary-cat":[],"class_list":["post-3883","glossary","type-glossary","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/sismoiberica.org\/es\/wp-json\/wp\/v2\/glossary\/3883","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/sismoiberica.org\/es\/wp-json\/wp\/v2\/glossary"}],"about":[{"href":"https:\/\/sismoiberica.org\/es\/wp-json\/wp\/v2\/types\/glossary"}],"author":[{"embeddable":true,"href":"https:\/\/sismoiberica.org\/es\/wp-json\/wp\/v2\/users\/1"}],"version-history":[{"count":0,"href":"https:\/\/sismoiberica.org\/es\/wp-json\/wp\/v2\/glossary\/3883\/revisions"}],"wp:attachment":[{"href":"https:\/\/sismoiberica.org\/es\/wp-json\/wp\/v2\/media?parent=3883"}],"wp:term":[{"taxonomy":"glossary-cat","embeddable":true,"href":"https:\/\/sismoiberica.org\/es\/wp-json\/wp\/v2\/glossary-cat?post=3883"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}