 {"id":21488,"date":"2023-10-12T08:29:21","date_gmt":"2023-10-12T11:29:21","guid":{"rendered":"https:\/\/www.glaciareschilenos.org\/?p=21488"},"modified":"2026-06-09T21:54:32","modified_gmt":"2026-06-10T00:54:32","slug":"chilean-glaciers-in-evolution-analysis-of-the-2022-public-glacier-inventory-ipg","status":"publish","type":"post","link":"https:\/\/www.glaciareschilenos.org\/en\/report\/chilean-glaciers-in-evolution-analysis-of-the-2022-public-glacier-inventory-ipg\/","title":{"rendered":"Chilean glaciers in evolution: Analysis of the 2022 Public Glacier Inventory (IPG)"},"content":{"rendered":"<p><span style=\"font-weight: 400;\">In May 2022, the Ministry of Public Works, through its General Water Authority (DGA), published the <\/span><b><i>Inventario P\u00fablico de Glaciares 2022<\/i><\/b><b> [2022 Public Glacier Inventory]. <\/b><span style=\"font-weight: 400;\">In this report, <\/span><b>26,169 glaciers in Chile <\/b><span style=\"font-weight: 400;\">were recorded, covering an area of <\/span><b>21,009.79 km\u00b2, <\/b><span style=\"font-weight: 400;\">which represents approximately <\/span><b>2.8% of the national territory <\/b><span style=\"font-weight: 400;\">(excluding the Chilean Antarctic). These glaciers contained an estimated <\/span><b>2,710.7 km\u00b3 of ice, equivalent to 2,301.5 km\u00b3 of water.<\/b><\/p>\n<p><span style=\"font-weight: 400;\">This latest iteration of the inventory, developed between 2019 and 2022, stands out for its <\/span><b>refined methodological approach<\/b><span style=\"font-weight: 400;\">. A major advancement was the use of higher-resolution satellite imagery, a factor that allowed researchers to identify hundreds of glaciers missed in previous studies and to rectify the classification of snow patches that were formerly mistaken for glaciers in the first survey. \u00a0 <\/span><\/p>\n<p><b>Fundaci\u00f3n Glaciares Chilenos <\/b><span style=\"font-weight: 400;\">had the opportunity to interview <\/span><b>Alexis Segovia Rocha<\/b><span style=\"font-weight: 400;\">\u2014a professional from the Division of Hydrology, Glaciology, and Snow at the General Water Authority (DGA) of the Ministry of Public Works and a professor at the University of Chile. During this interview, he addressed essential questions to better understand<\/span><b> the impact of the Public Glacier Inventory (IPG)<\/b><span style=\"font-weight: 400;\">, covering topics such as the process of creating this survey, its importance for decision-making by authorities, environmental protection, and scientific research.<\/span><\/p>\n<p><span style=\"font-weight: 400;\">To fully grasp the significance of the Public Glacier Inventory (IPG), it\u2019s essential to explore <\/span><b>its fundamental definition, its primary objective, and its evolution over time. <\/b><\/p>\n<p><b><i>\u201c<\/i><\/b><i><span style=\"font-weight: 400;\">The Public Glacier Inventory (IPG) is an effort to record as much of the ice in the country as possible<\/span><\/i><span style=\"font-weight: 400;\">\u2014<\/span><i><span style=\"font-weight: 400;\">both in terms of number and glacial surface area<\/span><\/i><span style=\"font-weight: 400;\">\u2014<\/span><i><span style=\"font-weight: 400;\">and to generate highly relevant information about the Chilean cryosphere, so that we can conduct studies and see the relevance of these ice bodies and examine the characteristics of the country\u2019s different macro-regions,\u201d <\/span><\/i><span style=\"font-weight: 400;\">explains Alexis Segovia. <\/span><\/p>\n<p><i><span style=\"font-weight: 400;\">\u201cThe first national glacier inventory was conducted between 2008 and 2014 by the General Water Authority (DGA), (&#8230;) and this effort was repeated in 2019 and completed in 2022, marking the second National Glacier Inventory.\u201d<\/span><\/i><\/p>\n<p><span style=\"font-weight: 400;\">Below, some of the most relevant data from the 2022 Public Glacier Inventory will be presented.<\/span><\/p>\n<p><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter wp-image-13220 size-full\" src=\"https:\/\/glaciareschilenoss3.s3.us-west-1.amazonaws.com\/wp-content\/uploads\/2023\/08\/11203430\/Diseno-sin-titulo-22.png\" alt=\"\" width=\"1080\" height=\"1080\" srcset=\"https:\/\/glaciareschilenoss3.s3.us-west-1.amazonaws.com\/wp-content\/uploads\/2023\/08\/11203430\/Diseno-sin-titulo-22.png 1080w, https:\/\/glaciareschilenoss3.s3.us-west-1.amazonaws.com\/wp-content\/uploads\/2023\/08\/11203430\/Diseno-sin-titulo-22-980x980.png 980w, https:\/\/glaciareschilenoss3.s3.us-west-1.amazonaws.com\/wp-content\/uploads\/2023\/08\/11203430\/Diseno-sin-titulo-22-480x480.png 480w\" sizes=\"(min-width: 0px) and (max-width: 480px) 480px, (min-width: 481px) and (max-width: 980px) 980px, (min-width: 981px) 1080px, 100vw\" \/><\/p>\n<div id=\"attachment_13222\" style=\"width: 1090px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-13222\" class=\"wp-image-13222 size-full\" src=\"https:\/\/glaciareschilenoss3.s3.us-west-1.amazonaws.com\/wp-content\/uploads\/2023\/08\/11203513\/Diseno-sin-titulo-23.png\" alt=\"\" width=\"1080\" height=\"1080\" srcset=\"https:\/\/glaciareschilenoss3.s3.us-west-1.amazonaws.com\/wp-content\/uploads\/2023\/08\/11203513\/Diseno-sin-titulo-23.png 1080w, https:\/\/glaciareschilenoss3.s3.us-west-1.amazonaws.com\/wp-content\/uploads\/2023\/08\/11203513\/Diseno-sin-titulo-23-980x980.png 980w, https:\/\/glaciareschilenoss3.s3.us-west-1.amazonaws.com\/wp-content\/uploads\/2023\/08\/11203513\/Diseno-sin-titulo-23-480x480.png 480w\" sizes=\"(min-width: 0px) and (max-width: 480px) 480px, (min-width: 481px) and (max-width: 980px) 980px, (min-width: 981px) 1080px, 100vw\" \/><p id=\"caption-attachment-13222\" class=\"wp-caption-text\">Distribution of glacier surface area (km\u00b2) by region according to the 2022 Public Glacier Inventory (IPG). The chart illustrates that the Magallanes and Ays\u00e9n regions account for the vast majority of the country\u2019s glaciated territory in terms of total area.<\/p><\/div>\n<p><span style=\"font-weight: 400;\">Segovia points out that <\/span><i><span style=\"font-weight: 400;\">\u201cBoth inventories were developed nearly <\/span><\/i><b><i>100% using satellite imagery <\/i><\/b><i><span style=\"font-weight: 400;\">(&#8230;) with 96% comprising Landsat 8 imagery at 15 meters and Sentinel 2 imagery at 10 meters. Regarding rock glaciers, imagery ranging from Google Earth to the PlanetScope satellite\u2014which offers 3-meter resolution\u2014was utilized. (&#8230;) These images must meet certain criteria; specifically, they must be cloud-free, otherwise the glaciers cannot be seen, and secondly, they should ideally be from the end of the summer season (&#8230;) in this inventory, it\u2019s evident that many glaciers are larger than in the previous one because <\/span><\/i><b><i>the improved imagery (2022) allowed for the mapping and recording of debris-covered zones with higher resolution, which weren\u2019t considered in the previous inventory.\u201d<\/i><\/b><\/p>\n<div id=\"attachment_13097\" style=\"width: 1147px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-13097\" class=\"wp-image-13097 size-full\" src=\"https:\/\/glaciareschilenoss3.s3.us-west-1.amazonaws.com\/wp-content\/uploads\/2023\/08\/06192649\/Glaciar-Tapado.jpg\" alt=\"\" width=\"1137\" height=\"964\" srcset=\"https:\/\/glaciareschilenoss3.s3.us-west-1.amazonaws.com\/wp-content\/uploads\/2023\/08\/06192649\/Glaciar-Tapado.jpg 1137w, https:\/\/glaciareschilenoss3.s3.us-west-1.amazonaws.com\/wp-content\/uploads\/2023\/08\/06192649\/Glaciar-Tapado-980x831.jpg 980w, https:\/\/glaciareschilenoss3.s3.us-west-1.amazonaws.com\/wp-content\/uploads\/2023\/08\/06192649\/Glaciar-Tapado-480x407.jpg 480w\" sizes=\"(min-width: 0px) and (max-width: 480px) 480px, (min-width: 481px) and (max-width: 980px) 980px, (min-width: 981px) 1137px, 100vw\" \/><p id=\"caption-attachment-13097\" class=\"wp-caption-text\">Alexis Segovia, glaciologist at the General Water Authority of the Ministry of Public Works, and professor at the University of Chile. Photo taken at the El Tapado glacier, Coquimbo Region. Photo by Daniela Carri\u00f3n.<\/p><\/div>\n<p>&nbsp;<\/p>\n<div id=\"attachment_13224\" style=\"width: 587px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-13224\" class=\"wp-image-13224\" src=\"https:\/\/glaciareschilenoss3.s3.us-west-1.amazonaws.com\/wp-content\/uploads\/2023\/08\/11203835\/3-4.png\" alt=\"\" width=\"577\" height=\"320\" srcset=\"https:\/\/glaciareschilenoss3.s3.us-west-1.amazonaws.com\/wp-content\/uploads\/2023\/08\/11203835\/3-4.png 577w, https:\/\/glaciareschilenoss3.s3.us-west-1.amazonaws.com\/wp-content\/uploads\/2023\/08\/11203835\/3-4-480x266.png 480w\" sizes=\"(min-width: 0px) and (max-width: 480px) 480px, (min-width: 481px) 577px, 100vw\" \/><p id=\"caption-attachment-13224\" class=\"wp-caption-text\">*The Ays\u00e9n Region has the largest number of glaciers in the country, but it doesn\u2019t have the largest total glacier area; that distinction belongs to the Magallanes and Chilean Antarctic Region.<\/p><\/div>\n<p><span style=\"font-weight: 400;\">A common question is: <\/span><b>What is the significance of the Public Glacier Inventory?<\/b><span style=\"font-weight: 400;\"> Alexis explains: \u201c<\/span><i><span style=\"font-weight: 400;\">Knowing<\/span><\/i> <i><span style=\"font-weight: 400;\">the quantity of glaciers and the ice surface area <\/span><\/i><b><i>allows us to estimate the volume of ice stored in the mountains, and this volume can be translated into the equivalent amount of water stored there<\/i><\/b><i><span style=\"font-weight: 400;\"> (&#8230;) therefore, knowing the volume of water stored in the mountains is crucial information regarding the water crisis. Additionally, knowing the percentage of glaciation within certain basins allows us to estimate the true contribution of the glacier to those basins based on total water levels. (&#8230;) From an ecosystem perspective, it helps us conduct estimates within protected wild areas, which harbor a significant number of glaciers. It is estimated that between 83% and 86% of the ice surface area is within the National System of Protected Wild Areas (SNASPE).\u201d<\/span><\/i><\/p>\n<div id=\"attachment_13226\" style=\"width: 560px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-13226\" class=\"wp-image-13226\" src=\"https:\/\/glaciareschilenoss3.s3.us-west-1.amazonaws.com\/wp-content\/uploads\/2023\/08\/11203905\/4-4.png\" alt=\"\" width=\"550\" height=\"360\" srcset=\"https:\/\/glaciareschilenoss3.s3.us-west-1.amazonaws.com\/wp-content\/uploads\/2023\/08\/11203905\/4-4.png 550w, https:\/\/glaciareschilenoss3.s3.us-west-1.amazonaws.com\/wp-content\/uploads\/2023\/08\/11203905\/4-4-480x314.png 480w\" sizes=\"(min-width: 0px) and (max-width: 480px) 480px, (min-width: 481px) 550px, 100vw\" \/><p id=\"caption-attachment-13226\" class=\"wp-caption-text\">*It should be noted that the largest glacier in Chile is the P\u00edo XI glacier; however, the IPG2022 doesn\u2019t include the surface area within the zone pending demarcation, as established by the &#8220;Agreement between the Republic of Chile and the Argentine Republic to specify the boundary line from Mount Fitz Roy to Mount Daudet\u201d of December 1998.<\/p><\/div>\n<p>&nbsp;<\/p>\n<div id=\"attachment_13148\" style=\"width: 1090px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-13148\" class=\"wp-image-13148 size-full\" src=\"https:\/\/glaciareschilenoss3.s3.us-west-1.amazonaws.com\/wp-content\/uploads\/2023\/08\/11132757\/79534785_135980871192781_1042599961815036220_n.jpg\" alt=\"\" width=\"1080\" height=\"1080\" srcset=\"https:\/\/glaciareschilenoss3.s3.us-west-1.amazonaws.com\/wp-content\/uploads\/2023\/08\/11132757\/79534785_135980871192781_1042599961815036220_n.jpg 1080w, https:\/\/glaciareschilenoss3.s3.us-west-1.amazonaws.com\/wp-content\/uploads\/2023\/08\/11132757\/79534785_135980871192781_1042599961815036220_n-980x980.jpg 980w, https:\/\/glaciareschilenoss3.s3.us-west-1.amazonaws.com\/wp-content\/uploads\/2023\/08\/11132757\/79534785_135980871192781_1042599961815036220_n-480x480.jpg 480w\" sizes=\"(min-width: 0px) and (max-width: 480px) 480px, (min-width: 481px) and (max-width: 980px) 980px, (min-width: 981px) 1080px, 100vw\" \/><p id=\"caption-attachment-13148\" class=\"wp-caption-text\">P\u00edo XI glacier, Magallanes Region, Chile. Photo: Adam Spencer.<\/p><\/div>\n<p><span style=\"font-weight: 400;\">Within the context of the importance of the Public Glacier Inventory (IPG) of Chile, it\u2019s fundamental to understand <\/span><b>how the data they provide is used and how various institutions<\/b><b><i>\u2014<\/i><\/b><b>both national and international<\/b><b><i>\u2014<\/i><\/b><b>are involved in its development and implementation. <\/b><\/p>\n<p><span style=\"font-weight: 400;\">The data provided by the inventory is used primarily by <\/span><i><span style=\"font-weight: 400;\">\u201cresearch centers, universities, companies involved in environmental consulting, the Ministry of the Environment, and law projects that have been discussed in some time. All of these use the data of the Public Glacier Inventory.\u201d<\/span><\/i><\/p>\n<p><span style=\"font-weight: 400;\">The DGA bases its glacier inventory methodology on the <\/span><b><i>UNESCO <\/i><\/b><i><span style=\"font-weight: 400;\">standard regarding glacier mapping (&#8230;) as well as glacier classification standards\u2014whether it\u2019s a mountain glacier, a valley glacier, a glacieret, a rock glacier, and so on. We also take into consideration other institutions, such as the <\/span><\/i><b><i>IPA <\/i><\/b><i><span style=\"font-weight: 400;\">(International Permafrost Association), whose guidelines we follow for the mapping of rock glaciers.\u201d<\/span><\/i><\/p>\n<p><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter wp-image-13215 \" src=\"https:\/\/glaciareschilenoss3.s3.us-west-1.amazonaws.com\/wp-content\/uploads\/2023\/08\/11202441\/4-3.png\" alt=\"\" width=\"514\" height=\"335\" srcset=\"https:\/\/glaciareschilenoss3.s3.us-west-1.amazonaws.com\/wp-content\/uploads\/2023\/08\/11202441\/4-3.png 514w, https:\/\/glaciareschilenoss3.s3.us-west-1.amazonaws.com\/wp-content\/uploads\/2023\/08\/11202441\/4-3-480x313.png 480w\" sizes=\"(min-width: 0px) and (max-width: 480px) 480px, (min-width: 481px) 514px, 100vw\" \/><\/p>\n<p><b>Comparison with the 2014 Inventory<\/b><\/p>\n<p><span style=\"font-weight: 400;\">The survey reports an increase of 2,055 glaciers (about 8%) compared to the first inventory in 2014; this is mainly because, over the past 15 years, many have fragmented into smaller ice bodies. On the other hand, there has been an approximate 8% loss in ice surface area due to glacial melting. <\/span><\/p>\n<p>&nbsp;<\/p>\n<p><img loading=\"lazy\" decoding=\"async\" class=\"aligncenter wp-image-13230 \" src=\"https:\/\/glaciareschilenoss3.s3.us-west-1.amazonaws.com\/wp-content\/uploads\/2023\/08\/11204129\/Diseno-sin-titulo-22-1.png\" alt=\"\" width=\"463\" height=\"413\" \/><\/p>\n<p><span style=\"font-weight: 400;\">Alexis adds:\u00a0<\/span><i><span style=\"font-weight: 400;\">\u201cWhile it\u2019s true that, given the inexperience we had in 2014, certain methodologies have since been improved\u2014thanks to technology and better imagery\u2014so the two glacier inventories are not strictly comparable.\u201d<\/span><\/i><\/p>\n<p><b>Final conclusions<\/b><\/p>\n<p><span style=\"font-weight: 400;\">The relevance of the Public Glacier Inventory in Chile is essential for understanding and addressing the environmental challenges we face. This detailed survey provides specific information about the quantity, location, and characteristics of the glaciers<\/span><i><span style=\"font-weight: 400;\">, <\/span><\/i><span style=\"font-weight: 400;\">which is fundamental for the sustainable management of our water resources and for adapting to climate change.<\/span><\/p>\n<p><span style=\"font-weight: 400;\">As Alexis says: <\/span><i><span style=\"font-weight: 400;\">\u201cThe main conclusions of this inventory are that<\/span><\/i><b><i> there has been a retreat or loss of glacier area in the country,<\/i><\/b><i><span style=\"font-weight: 400;\"> and that many glaciers that were single bodies 15 years ago have fragmented\u2014a global trend (&#8230;) it must be noted that <\/span><\/i><b><i>the fact that we have more glaciers doesn\u2019t mean that new glaciers have formed over the last 15 years<\/i><\/b><i><span style=\"font-weight: 400;\">; instead, it\u2019s a result of the shrinkage of these ice bodies as they fragment.\u201d <\/span><\/i><\/p>\n<p><span style=\"font-weight: 400;\">The inventory has become an invaluable tool for political decision-making, environmental planning, and scientific research related to the Chilean cryosphere. Furthermore, it allows us to understand the impact of the glacier retreat and its relation to the water shortage in the country. <\/span><\/p>\n<p><b>This inventory represents a significant advancement compared to the 2014 edition<\/b><span style=\"font-weight: 400;\">; for instance: <\/span><i><span style=\"font-weight: 400;\">\u201cThe debris-covered portions of glaciers that were previously unmapped were included, representing a greater effort to incorporate both these sections and entirely new glaciers (&#8230;) in fact, over 1,200 rock glaciers were detected that hadn\u2019t been mapped in 2014, as the technology at the time made it extremely difficult.\u201d<\/span><\/i><\/p>\n<p><span style=\"font-weight: 400;\">Alexis highlights an important detail: <\/span><i><span style=\"font-weight: 400;\">\u201cThis new inventory underwent <\/span><\/i><b><i>a peer review process<\/i><\/b><i><span style=\"font-weight: 400;\">; that is, when the 2022 inventory was nearly finalized, it was sent to 60 individuals and organizations\u2014including institutions, foundations, NGOs, and universities\u2014with expertise in glaciology for comments and observations. These contributions make this inventory far more robust than the 2014 version, as it had the opportunity to be reviewed by subject matter experts. We evaluated and corrected every observation received and subsequently followed up with the person or institution that provided the feedback.\u201d<\/span><\/i><\/p>\n<p><span style=\"font-weight: 400;\">As <\/span><b>Fundaci\u00f3n Glaciares Chilenos,<\/b><span style=\"font-weight: 400;\"> we believe that glacier conservation and environmental protection are urgent tasks that cannot be postponed. It\u2019s everyone\u2019s responsibility to unite in the defense of our natural resources and take effective action to preserve them for future generations.\u00a0<\/span><\/p>\n<div id=\"attachment_13159\" style=\"width: 2570px\" class=\"wp-caption aligncenter\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-13159\" class=\"wp-image-13159 size-full\" src=\"https:\/\/glaciareschilenoss3.s3.us-west-1.amazonaws.com\/wp-content\/uploads\/2023\/08\/11135521\/Glaciar-Ohiggins-region-de-Aysen-scaled.jpg\" alt=\"\" width=\"2560\" height=\"1710\" srcset=\"https:\/\/glaciareschilenoss3.s3.us-west-1.amazonaws.com\/wp-content\/uploads\/2023\/08\/11135521\/Glaciar-Ohiggins-region-de-Aysen-scaled.jpg 2560w, https:\/\/glaciareschilenoss3.s3.us-west-1.amazonaws.com\/wp-content\/uploads\/2023\/08\/11135521\/Glaciar-Ohiggins-region-de-Aysen-1280x855.jpg 1280w, https:\/\/glaciareschilenoss3.s3.us-west-1.amazonaws.com\/wp-content\/uploads\/2023\/08\/11135521\/Glaciar-Ohiggins-region-de-Aysen-980x655.jpg 980w, https:\/\/glaciareschilenoss3.s3.us-west-1.amazonaws.com\/wp-content\/uploads\/2023\/08\/11135521\/Glaciar-Ohiggins-region-de-Aysen-480x321.jpg 480w\" sizes=\"(min-width: 0px) and (max-width: 480px) 480px, (min-width: 481px) and (max-width: 980px) 980px, (min-width: 981px) and (max-width: 1280px) 1280px, (min-width: 1281px) 2560px, 100vw\" \/><p id=\"caption-attachment-13159\" class=\"wp-caption-text\">O\u2019Higgins glacier, Ays\u00e9n Region, Chile. Photo: Richard Bezzaza.<\/p><\/div>\n<p>&nbsp;<\/p>\n<p><b>Links of Interest\u00a0<\/b><\/p>\n<ul>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">2022 Public Glacier Inventory:\u00a0<\/span><a href=\"https:\/\/dga.mop.gob.cl\/Paginas\/InventarioGlaciares.aspx\" target=\"_blank\" rel=\"noopener\"><span style=\"font-weight: 400;\">Link<\/span><\/a><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Complete interview with Alexis Segovia Rocha:\u00a0<\/span><a href=\"https:\/\/glaciareschilenoss3.s3.us-west-1.amazonaws.com\/wp-content\/uploads\/2023\/08\/06161419\/Entrevista-Alexis-Segovia-DGA.pdf\" target=\"_blank\" rel=\"noopener\"><span style=\"font-weight: 400;\">Link<\/span><\/a><\/li>\n<li style=\"font-weight: 400;\" aria-level=\"1\"><span style=\"font-weight: 400;\">Types of glaciers:\u00a0<\/span><a href=\"https:\/\/www.glaciareschilenos.org\/que-tipos-de-glaciares-existen-en-chile\/\" target=\"_blank\" rel=\"noopener\"><span style=\"font-weight: 400;\">Link<\/span><\/a><\/li>\n<\/ul>\n<p><b>Featured Image:<\/b><\/p>\n<p><i><span style=\"font-weight: 400;\">San Quint\u00edn <\/span><\/i><span style=\"font-weight: 400;\">glacier, <\/span><i><span style=\"font-weight: 400;\">Magallanes <\/span><\/i><span style=\"font-weight: 400;\">Region, Chile \/ \u00a9NasaEarth<\/span><\/p>\n","protected":false},"excerpt":{"rendered":"<p>In May 2022, the Ministry of Public Works, through its General Water Authority (DGA), published the Inventario P\u00fablico de Glaciares 2022 [2022 Public Glacier Inventory]. In this report, 26,169 glaciers in Chile were recorded, covering an area of 21,009.79 km\u00b2, which represents approximately 2.8% of the national territory (excluding the Chilean Antarctic). These glaciers contained [&hellip;]<\/p>\n","protected":false},"author":33,"featured_media":13185,"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":[2797],"tags":[2959,3788],"coauthors":[3332],"class_list":["post-21488","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-report","tag-dga-en-2","tag-unesco"],"_links":{"self":[{"href":"https:\/\/www.glaciareschilenos.org\/en\/wp-json\/wp\/v2\/posts\/21488","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\/33"}],"replies":[{"embeddable":true,"href":"https:\/\/www.glaciareschilenos.org\/en\/wp-json\/wp\/v2\/comments?post=21488"}],"version-history":[{"count":4,"href":"https:\/\/www.glaciareschilenos.org\/en\/wp-json\/wp\/v2\/posts\/21488\/revisions"}],"predecessor-version":[{"id":21534,"href":"https:\/\/www.glaciareschilenos.org\/en\/wp-json\/wp\/v2\/posts\/21488\/revisions\/21534"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/www.glaciareschilenos.org\/en\/wp-json\/wp\/v2\/media\/13185"}],"wp:attachment":[{"href":"https:\/\/www.glaciareschilenos.org\/en\/wp-json\/wp\/v2\/media?parent=21488"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.glaciareschilenos.org\/en\/wp-json\/wp\/v2\/categories?post=21488"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.glaciareschilenos.org\/en\/wp-json\/wp\/v2\/tags?post=21488"},{"taxonomy":"author","embeddable":true,"href":"https:\/\/www.glaciareschilenos.org\/en\/wp-json\/wp\/v2\/coauthors?post=21488"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}