 {"id":17798,"date":"2018-07-31T08:00:03","date_gmt":"2018-07-31T11:00:03","guid":{"rendered":"https:\/\/www.glaciareschilenos.org\/?p=17798"},"modified":"2025-02-06T18:38:01","modified_gmt":"2025-02-06T21:38:01","slug":"glaciers-of-torres-del-paine-national-park-pingo-glacier","status":"publish","type":"post","link":"https:\/\/www.glaciareschilenos.org\/en\/places\/glaciers-of-torres-del-paine-national-park-pingo-glacier\/","title":{"rendered":"Glaciers of Torres del Paine National Park: Pingo Glacier"},"content":{"rendered":"<p style=\"text-align: left;\"><span style=\"font-weight: 400;\">The protagonist of this article is part of the southern Patagonian ice field. It doesn\u2019t have the volume or the extension of its neighbors Grey or Tyndall. It exhibits two main arms, which separated by a <\/span><i><span style=\"font-weight: 400;\">nunatak<\/span><\/i><span style=\"font-weight: 400;\"> (rock island or mountain peak) give the characteristic shape to this glacier. A beautiful and wide lake is born from it, while a river emerges meandering for several kilometers until it enters a valley and ends its course in the Grey river<\/span>.<\/p>\n<p style=\"text-align: left;\"><span style=\"font-weight: 400;\">Did you guess which glacier I&#8217;m talking about? That&#8217;s right, the <\/span><b>Pingo glacier<\/b><span style=\"font-weight: 400;\">.<\/span><\/p>\n<div id=\"attachment_887\" style=\"width: 1642px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-887\" class=\"wp-image-887 size-full\" src=\"https:\/\/glaciareschilenoss3.s3.us-west-1.amazonaws.com\/wp-content\/uploads\/2018\/07\/10050931\/fgh.jpg\" alt=\"\" width=\"1632\" height=\"918\" \/><p id=\"caption-attachment-887\" class=\"wp-caption-text\"><span style=\"font-weight: 400;\">Lagoon and glacier Pingo.<\/span><\/p><\/div>\n<p><span style=\"font-weight: 400;\">The consequences of climate change haven\u2019t made an exception for this glacier. It has experienced a significant retreat, since it\u2019s a glacier located at a low altitude (its front is about 300 m.a.s.l.) and its extension is declining every year. This can be seen in the following image, obtained from the glaciological laboratory of Chile<\/span>:<\/p>\n<div id=\"attachment_891\" style=\"width: 587px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-891\" class=\"wp-image-891 size-full\" src=\"https:\/\/glaciareschilenoss3.s3.us-west-1.amazonaws.com\/wp-content\/uploads\/2018\/07\/10053049\/retroceso-pingo.jpg\" alt=\"\" width=\"577\" height=\"399\" \/><p id=\"caption-attachment-891\" class=\"wp-caption-text\"><span style=\"font-weight: 400;\">Image obtained from the glaciology laboratory website, used for informational and didactic purposes only.<\/span><\/p><\/div>\n<p>&nbsp;<\/p>\n<h2>Acceso al mirador del glaciar Pingo para excursionistas<\/h2>\n<p><b>Summary of the excursion:<\/b><\/p>\n<table style=\"height: 435px;\" border=\"1\" width=\"478\">\n<tbody>\n<tr>\n<td width=\"75\">\n<p style=\"text-align: center;\"><span style=\"font-weight: 400;\">Country<\/span><\/p>\n<\/td>\n<td width=\"132\">\n<p style=\"text-align: center;\">Chile<\/p>\n<\/td>\n<\/tr>\n<tr>\n<td style=\"text-align: center;\" width=\"75\"><span style=\"font-weight: 400;\">Area<\/span><\/td>\n<td style=\"text-align: center;\" width=\"132\">\n<p style=\"text-align: center;\"><span style=\"font-weight: 400;\">Torres del Paine National Park<\/span><\/p>\n<\/td>\n<\/tr>\n<tr>\n<td style=\"text-align: center;\" width=\"75\"><span style=\"font-weight: 400;\">N\u00b0 of days<\/span><\/td>\n<td width=\"132\">\n<p style=\"text-align: center;\">2 days<\/p>\n<\/td>\n<\/tr>\n<tr>\n<td width=\"75\">\n<p style=\"text-align: center;\"><span style=\"font-weight: 400;\">Distance<\/span><\/p>\n<\/td>\n<td width=\"132\">\n<p style=\"text-align: center;\"><span style=\"font-weight: 400;\">40km (round trip)<\/span><\/p>\n<\/td>\n<\/tr>\n<tr>\n<td width=\"75\">\n<p style=\"text-align: center;\"><span style=\"font-weight: 400;\">Difficulty<\/span><\/p>\n<\/td>\n<td width=\"132\">\n<p style=\"text-align: center;\"><span style=\"font-weight: 400;\">Medium(*)<\/span><\/p>\n<\/td>\n<\/tr>\n<tr>\n<td width=\"75\">\n<p style=\"text-align: center;\"><span style=\"font-weight: 400;\">Path<\/span><\/p>\n<\/td>\n<td style=\"text-align: center;\" width=\"132\"><span style=\"font-weight: 400;\">Noticeable<\/span><\/td>\n<\/tr>\n<tr>\n<td style=\"text-align: center;\" width=\"75\"><span style=\"font-weight: 400;\">Coordinate<\/span><\/td>\n<td width=\"132\">\n<p style=\"text-align: center;\">Lat: \u2013 51.010003 ; Long: -73.339646<\/p>\n<\/td>\n<\/tr>\n<\/tbody>\n<\/table>\n<p><span style=\"font-weight: 400;\">This beautiful glacier is located on the western side of the Torres del Paine, an area of the park that is little frequented and of high scientific interest (which we will discuss in detail in another article). These lands are under the care of Walter Ferrier (a pioneer in the area). In order to access it, you must first request authorization from Conaf [<\/span><i><span style=\"font-weight: 400;\">The National Forestry Corporation]<\/span><\/i><span style=\"font-weight: 400;\">, and only accredited guides are allowed to go there.<\/span><\/p>\n<p><span style=\"font-weight: 400;\">After registering your visit and number of days of stay (considering that at least 1 night of camping is required to see the glacier), you start the hike along a clearly marked trail with very little slope. After 4 km, you arrive at a refuge near the shore of the <\/span><i><span style=\"font-weight: 400;\">Pingo<\/span><\/i><span style=\"font-weight: 400;\"> river, which has only a campsite without basic services. Passing it you\u2019ll find a sign indicating a 12 km distance to the Zapata camp. On the way to this camp, you\u2019ll have the opportunity to contemplate 2 beautiful waterfalls: <\/span><i><span style=\"font-weight: 400;\">Chorrillo de los Salmones<\/span><\/i><span style=\"font-weight: 400;\"> waterfall and <\/span><i><span style=\"font-weight: 400;\">Pingo<\/span><\/i><span style=\"font-weight: 400;\"> waterfall, while a beautiful forest of <\/span><i><span style=\"font-weight: 400;\">coig\u00fces [oak]<\/span><\/i><span style=\"font-weight: 400;\"> and l<\/span><i><span style=\"font-weight: 400;\">engas<\/span><\/i><span style=\"font-weight: 400;\"> [white oak] shelters you with its shadows. If you are (very) lucky, you might find some <\/span><i><span style=\"font-weight: 400;\">huemul<\/span><\/i><span style=\"font-weight: 400;\"> along the way, or maybe a <\/span><i><span style=\"font-weight: 400;\">bagual<\/span><\/i><span style=\"font-weight: 400;\"> [wild horse] grazing near the camp (they usually cross the river from one side to the other looking for food). After 16 km, you\u2019ll have reached the Zapata camp, which is ideal to set up your shelter (from here you are 4 km from the viewpoint of the Pingo and Zapata glacier).<\/span><\/p>\n<p><span style=\"font-weight: 400;\">On the second day, leaving the camp and following the well-marked trail, you\u2019ll find a sign indicating that the viewpoint is approximately 1 hour (4 km) away. At times, there are heaps of stones indicating the direction to follow, which will lead you to cross a small stream and begin a low-difficulty ascent. After overcoming a marshy area, you\u2019ll see the viewpoint, and if the day is clear you will be delighted with the lake and glacier Pingo, as well as the lagoon that rises from the waterfall of the Zapata glacier. The return is by the same route as the outward journey.<\/span><\/p>\n<p><span style=\"font-weight: 400;\">(*) Regarding the weighting of the difficulty, \u201cMedium\u201d is understood as a physical activity that requires some experience on trails with slopes and muddy areas, or areas with abundant vegetation, in addition to relatively long distances carrying a backpack. It\u2019s recommended to take the necessary considerations.<\/span><\/p>\n<p>&nbsp;<\/p>\n<h2 style=\"text-align: center;\"><span style=\"font-weight: 400;\">Gallery of <\/span><i><span style=\"font-weight: 400;\">Pingo<\/span><\/i><span style=\"font-weight: 400;\"> glacier.<\/span><\/h2>\n<p><span style=\"font-weight: 400;\">Finally, here you have a selection of the best pictures I\u2019ve been able to capture of this glacier from different angles and perspectives. I hope these postcards will inspire you and that you will book this beautiful excursion!<\/span><\/p>\n<p>&nbsp;<\/p>\n<div id=\"attachment_889\" style=\"width: 960px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-889\" class=\"wp-image-889 size-full\" src=\"https:\/\/glaciareschilenoss3.s3.us-west-1.amazonaws.com\/wp-content\/uploads\/2018\/07\/10052338\/at-pingo.jpg\" alt=\"\" width=\"950\" height=\"534\" \/><p id=\"caption-attachment-889\" class=\"wp-caption-text\"><span style=\"font-weight: 400;\">Sunset on the <\/span><i><span style=\"font-weight: 400;\">Pingo<\/span><\/i><span style=\"font-weight: 400;\"> glacier.<\/span><\/p><\/div>\n<p>&nbsp;<\/p>\n<div id=\"attachment_885\" style=\"width: 1343px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-885\" class=\"wp-image-885 size-full\" src=\"https:\/\/glaciareschilenoss3.s3.us-west-1.amazonaws.com\/wp-content\/uploads\/2018\/07\/10050742\/8.jpg\" alt=\"\" width=\"1333\" height=\"750\" \/><p id=\"caption-attachment-885\" class=\"wp-caption-text\"><i><span style=\"font-weight: 400;\">Pingo<\/span><\/i><span style=\"font-weight: 400;\"> glacier from the peak of <\/span><i><span style=\"font-weight: 400;\">Zapata<\/span><\/i><span style=\"font-weight: 400;\"> Hill<\/span><\/p><\/div>\n<p>&nbsp;<\/p>\n<div id=\"attachment_888\" style=\"width: 960px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-888\" class=\"wp-image-888 size-full\" src=\"https:\/\/glaciareschilenoss3.s3.us-west-1.amazonaws.com\/wp-content\/uploads\/2018\/07\/10051051\/L1030512.jpg\" alt=\"\" width=\"950\" height=\"534\" \/><p id=\"caption-attachment-888\" class=\"wp-caption-text\"><i><span style=\"font-weight: 400;\">Pingo<\/span><\/i><span style=\"font-weight: 400;\"> glacier cavern<\/span><\/p><\/div>\n<p>&nbsp;<\/p>\n<div id=\"attachment_886\" style=\"width: 1343px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-886\" class=\"wp-image-886 size-full\" src=\"https:\/\/glaciareschilenoss3.s3.us-west-1.amazonaws.com\/wp-content\/uploads\/2018\/07\/10050752\/22-2.jpg\" alt=\"\" width=\"1333\" height=\"750\" \/><p id=\"caption-attachment-886\" class=\"wp-caption-text\"><span style=\"font-weight: 400;\">Lagoon and <\/span><i><span style=\"font-weight: 400;\">Pingo<\/span><\/i><span style=\"font-weight: 400;\"> glacier<\/span><\/p><\/div>\n","protected":false},"excerpt":{"rendered":"<p>The protagonist of this article is part of the southern Patagonian ice field. It doesn\u2019t have the volume or the extension of its neighbors Grey or Tyndall. It exhibits two main arms, which separated by a nunatak (rock island or mountain peak) give the characteristic shape to this glacier. A beautiful and wide lake is [&hellip;]<\/p>\n","protected":false},"author":8,"featured_media":17799,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"googlesitekit_rrm_CAow57LVCw:productID":"","_et_pb_use_builder":"","_et_pb_old_content":"","_et_gb_content_width":"","footnotes":""},"categories":[2871],"tags":[2735,2635,2636,2825,2689,2681,2742,1473,2828],"coauthors":[3344],"class_list":["post-17798","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-places","tag-adventure","tag-chile","tag-climate-change","tag-conaf-en-2","tag-cryosphere","tag-glacier-en-2","tag-glaciers","tag-parque-nacional-torres-del-paine","tag-torres-del-paine-en-2"],"_links":{"self":[{"href":"https:\/\/www.glaciareschilenos.org\/en\/wp-json\/wp\/v2\/posts\/17798","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.glaciareschilenos.org\/en\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.glaciareschilenos.org\/en\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.glaciareschilenos.org\/en\/wp-json\/wp\/v2\/users\/8"}],"replies":[{"embeddable":true,"href":"https:\/\/www.glaciareschilenos.org\/en\/wp-json\/wp\/v2\/comments?post=17798"}],"version-history":[{"count":2,"href":"https:\/\/www.glaciareschilenos.org\/en\/wp-json\/wp\/v2\/posts\/17798\/revisions"}],"predecessor-version":[{"id":17802,"href":"https:\/\/www.glaciareschilenos.org\/en\/wp-json\/wp\/v2\/posts\/17798\/revisions\/17802"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/www.glaciareschilenos.org\/en\/wp-json\/wp\/v2\/media\/17799"}],"wp:attachment":[{"href":"https:\/\/www.glaciareschilenos.org\/en\/wp-json\/wp\/v2\/media?parent=17798"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.glaciareschilenos.org\/en\/wp-json\/wp\/v2\/categories?post=17798"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.glaciareschilenos.org\/en\/wp-json\/wp\/v2\/tags?post=17798"},{"taxonomy":"author","embeddable":true,"href":"https:\/\/www.glaciareschilenos.org\/en\/wp-json\/wp\/v2\/coauthors?post=17798"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}