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Mendenhall Glacier

 

Blue ice sheet, 12 mi (19 km) long, 1.5 mi (2.4 km) wide, and more than 100 ft (30 m) high. It flows from the southern half of the huge Juneau Icefield, which lies in the Boundary Ranges in southeastern Alaska, U.S. A relic of the Little Ice Age (16th century to the mid-19th century), it recedes about 100 – 150 ft (30 – 45 m) a year. The adjacent Mendenhall Lake began to form about 1900 and is now 1.5 mi (2.4 km) long and 1 mi (1.6 km) wide.

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WordNet: Mendenhall Glacier
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Note: click on a word meaning below to see its connections and related words.

The noun has one meaning:

Meaning #1: a glacier of the Piedmont type near Juneau in Alaska
  Synonym: Great Mendenhall Glacier


Wikipedia: Mendenhall Glacier
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Mendenhall Glacier and frozen Mendenhall Lake on a clear winter day.

Mendenhall Glacier is a glacier about 12 miles (19 km) long located in Mendenhall Valley, about 12 miles (19 km) from downtown Juneau in the southeast area of the U.S. state of Alaska.

Originally known as Sitaantaagu ("the Glacier Behind the Town") or Aak'wtaaksit ("the Glacier Behind the Little Lake") by the Tlingits, the glacier was named Auke (Auk) Glacier by naturalist John Muir for the Tlingit Auk Kwaan (or Aak'w Kwaan) band 1888. In 1899 it was renamed in honor of Thomas Corwin Mendenhall. It extends from the Juneau Icefield, its source, to Mendenhall Lake and ultimately the Mendenhall River.

The Juneau Icefield Research Program has monitored the outlet glaciers of the Juneau Icefield since 1942 , including Mendenhall Glacier. From 1951–1958 the terminus of the glacier, which flows into suburban Juneau, has retreated 1,900 feet (580 m). The glacier has also receded 1.75 miles (2.82 km) since 1958, when Mendenhall Lake was created, and over 2.5 miles (4.0 km) since 1500. The end of the glacier currently has limited crevassing a negative glacier mass balance and will continue to retreat in the foreseeable future.

Closer view of the glacier in the winter.

Given that average yearly temperatures are currently increasing, and the outlook is for this trend to continue, it is actually possible that the glacier might experience a period of stabilization or slight advance during its retreating march. This is because increasing amounts of warm, moist air will be carried up to the head of the icefield, where colder ambient temperatures will cause it to precipitate as snow. The increased amount of snow will feed the icefield, possibly enough to offset the continually increasing melting experienced at the glacier's terminus. However, this interesting phenomenon will fade away if temperatures continue to climb, since the head of the glacier will no longer have cold enough ambient temperatures to cause snow to precipitate.

A glacier cave under Mendenhall Glacier

The United States Forest Service administers the Mendenhall Glacier Visitor Center as part of Tongass National Forest. Forest interpreters offer conservation education programs throughout the year for children and adults.

Gallery

Mendenhall Lake and Glacier from the southeastern edge of the lake.
Mendenhall Lake and Glacier from the Visitor's Center.
Mendenhall Glacier from a footpath in August 2003.

See also

External links

Coordinates: 58°27′0″N 134°32′20″W / 58.45°N 134.53889°W / 58.45; -134.53889


 
 

 

Copyrights:

Britannica Concise Encyclopedia. Britannica Concise Encyclopedia. © 2006 Encyclopædia Britannica, Inc. All rights reserved.  Read more
WordNet. WordNet 1.7.1 Copyright © 2001 by Princeton University. All rights reserved.  Read more
Wikipedia. This article is licensed under the Creative Commons Attribution/Share-Alike License. It uses material from the Wikipedia article "Mendenhall Glacier" Read more