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Geological Formation

Margerie Glacier

Glaciers and Ice Formations

Margerie Glacier is a tidewater glacier about 21 miles long in Glacier Bay, Alaska, in the United States, within Glacier Bay National Park and Preserve. It originates on the southern slopes of Mount Root, at an elevation of 12,860 feet on the Alaska-Canada border, and flows southeast before turning northeast to reach its terminus at sea level in Tarr Inlet. About a mile wide with a 350-foot total height at its terminus, including 100 feet underwater, it is one of the park's most active and most visited glaciers and has remained stable in recent decades while most of the park's other tidewater glaciers have been receding. The glacier is named for the French geologist Emmanuel de Margerie, who visited the area in 1913. 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 Status
National Park or Reserve 1
Connections

Caused By

Glaciation, Processes

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: Margerie 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: Margerie Glacier
In the Other Atlases
Sources
1. Margerie Glacier (Wikipedia)
  • Lead section
    Margerie Glacier is a 21 mi (34 km) long tidewater glacier in Glacier Bay, Alaska, United States within the boundaries of Glacier Bay National Park and Preserve.
  • Entity description, protection designation
    21 miles long in Glacier Bay, Alaska, in the United States, within Glacier Bay National Park and Preserve. It originates on the southern slopes of Mount Root, at an elevati
View the Source
Wikidata: Margerie Glacier
Wikidata Q1895241, class allow-list match (w-wdresolver-0926)View the Source
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