{"id":1408,"date":"2021-08-22T13:02:27","date_gmt":"2021-08-22T11:02:27","guid":{"rendered":"https:\/\/guaracentral.com\/blog\/?p=1408"},"modified":"2021-08-22T13:09:12","modified_gmt":"2021-08-22T11:09:12","slug":"ripples-lagunies","status":"publish","type":"post","link":"https:\/\/guaracentral.com\/blog\/ripples-lagunies\/","title":{"rendered":"Ripples en Laguni\u00e9s (Patrimonio p\u00e9treo)"},"content":{"rendered":"<p>Los ripples, ripple marks o ripples\u00a0 (denominado de todas estas maneras) de corriente son estructuras sedimentarias las cuales encontramos a modo de ondulaciones. Se forman gracias a la acci\u00f3n de una corriente de agua o del viento sobre una superficie arenosa. Los <a href=\"https:\/\/aleph.org.mx\/que-es-una-cresta-y-un-valle\">valles y crestas<\/a> se disponen de manera perpendicular a la corriente y migran a favor de esta generando su laminaci\u00f3n interna.<\/p>\n<p>En uno de los lados del ripple, se est\u00e1 produciendo erosi\u00f3n y en el lado contrario se deposita el material desplazado que surge de esta. Por tanto, un cambio en las condiciones del entorno, sea cual sea, va a provocar\u00a0 que el equilibrio se modifique, pudi\u00e9ndose eliminar de esta manera por completo el ripple. Por ejemplo, si nos encontramos ante el caso\u00a0 de que\u00a0 la corriente aumente su velocidad hay dos opciones, o queda enterrado o preservado, si existe una mayor cantidad de sedimento disponible.<\/p>\n<figure id=\"attachment_1410\" aria-describedby=\"caption-attachment-1410\" style=\"width: 283px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" class=\"wp-image-1410 size-full\" src=\"https:\/\/guaracentral.com\/blog\/wp-content\/uploads\/2021\/08\/v-1.png\" alt=\"\" width=\"283\" height=\"210\" \/><figcaption id=\"caption-attachment-1410\" class=\"wp-caption-text\">Imagen del Ripple de Laguni\u00e9s<\/figcaption><\/figure>\n<p>La presencia de ripples fosilizados en este lugar, nos indica la existencia anterior de masas de agua dulce, seguramente de escasa profundidad.<\/p>\n<p>Este elemento geol\u00f3gico compuesto por fondos fluviales f\u00f3siles lo podemos observar mientras\u00a0 realizamos la ruta <a href=\"https:\/\/guaracentral.com\/ruta\/ruta-l3-guara-central-los-estaos\/26.html\">L3<\/a>. Esta ruta tiene como punto de partida y de finalizaci\u00f3n el pueblo de Labata. Tambi\u00e9n, a mitad de trayecto se pasa por los esta\u00f1os.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Los ripples, ripple marks o ripples\u00a0 (denominado de todas estas maneras) de corriente son estructuras sedimentarias las cuales encontramos a modo de ondulaciones. Se forman gracias a la acci\u00f3n de [&hellip;]<\/p>\n","protected":false},"author":2,"featured_media":1409,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":[],"categories":[8,17],"tags":[],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v16.8 - https:\/\/yoast.com\/wordpress\/plugins\/seo\/ -->\n<title>Ripples en Laguni\u00e9s (Patrimonio p\u00e9treo) - Guara Central - Geolog\u00eda<\/title>\n<meta name=\"description\" content=\"Los ripples de Laguni\u00e9s son estructuras sedimentarias que se forman por la acci\u00f3n de una corriente de agua o de viento sobre una superficie arenosa.\" \/>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"https:\/\/guaracentral.com\/blog\/ripples-lagunies\/\" \/>\n<meta property=\"og:locale\" content=\"es_ES\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Ripples en Laguni\u00e9s (Patrimonio p\u00e9treo) - 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