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Geological Formation

Mueller Glacier

Glaciers and Ice Formations

Mueller Glacier is a 13-kilometer glacier in Aoraki/Mount Cook National Park on New Zealand's South Island, within the Southern Alps. It originates near Mount Montgomerie, flows northwest and curves around the Sealy Range, fed along the way by the Frind and Huddleston glaciers, before ending at a small unnamed terminal lake also fed by the nearby Hooker Glacier. That lake is the source of the Hooker River, which flows on to Lake Pukaki via the Tasman River. The glacier is named for the botanist and explorer Ferdinand von Mueller, reached its Little Ice Age maximum extent between about 1725 and 1730 according to lichen dating, and is currently retreating. 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: Mueller 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: Mueller Glacier
In the Other Atlases
Sources
1. Mueller Glacier (Wikipedia)
Entity description, protection designation
Quote, Entity description, protection designation
Mueller Glacier is a 13-kilometer glacier in Aoraki/Mount Cook National Park on New Zealand's South Island, within the Southern Alps. It originates near Mount Montgomerie, f
View the Source
Wikidata: Mueller Glacier
Wikidata Q3866899, class allow-list match (w-wdresolver-0926)View the Source
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