Upsala Glacier is a large valley glacier on the eastern side of the Southern Patagonian Ice Field, with its higher reaches lying in territory disputed between Chile and Argentina. It flows generally north to south with three lesser, east-flowing tributary glaciers, Bertacchi, Cono and Murallon, and its terminus lies at the Upsala channel of Lago Argentino within Los Glaciares National Park. Upsala Glacier is one of the region's most visited features despite being overshadowed in popularity by the nearby Perito Moreno glacier, and it is well known for a rapid retreat that has continued since it was first documented in 1810, with an especially fast retreat beginning in 2008 that was reported as roughly ten times faster than the preceding eight years. This description is adapted from Wikipedia contributors under CC BY-SA 4.0; changes were made. https://creativecommons.org/licenses/by-sa/4.0/
Facts
Classification
Protected StatusNational Park or Reserve 1 Connections
Caused By
Wikidata P31 formation-type mapped to formative process Glaciation via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.
Source Wikidata: Upsala Glacier
In Discipline
Wikidata P31 formation-type mapped to discipline Glaciology via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.
Source Wikidata: Upsala Glacier
In the Other Atlases
- Also in Geography Atlas: Argentina, found in there.
- Also in Geography Atlas: Chile, found in there.
Sources
1. Upsala Glacier (Wikipedia)
Lead section
The Upsala Glacier is a large valley glacier on the eastern side of the Southern Patagonian Ice Field.
Entity description, protection designation
its terminus lies at the Upsala channel of Lago Argentino within Los Glaciares National Park. Upsala Glacier is one of the region's most visited features despite being over
View the SourceWikidata: Upsala Glacier
Wikidata Q962630, class allow-list match (w-wdresolver-0926)View the Source Reader Challenges (0)
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