Glacier King
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Glacier King is a mountain
summit A summit is a point on a surface that is higher in elevation than all points immediately adjacent to it. The topography, topographic terms acme, apex, peak (mountain peak), and zenith are synonymous. The term (mountain top) is generally used ...
in Alaska, United States.


Description

Glacier King is located in the
Boundary Ranges The Boundary Ranges, also known in the singular and as the Alaska Boundary Range, are the largest and most northerly subrange of the Coast Mountains. They begin at the Nass River, near the southern end of the Alaska Panhandle in the Canadian p ...
of the
Coast Mountains The Coast Mountains (french: La chaîne Côtière) are a major mountain range in the Pacific Coast Ranges of western North America, extending from southwestern Yukon through the Alaska Panhandle and virtually all of the Coast of British Columbia ...
and set on land managed by Tongass National Forest. The remote peak is east-southeast of
The Tusk The Tusk () is a sharply pointed peak of white marble, about 460 m high, in the east part of Mayer Crags. It stands 1.5 nautical miles (2.8 km) south of Mount Henson at the west side of the terminus of Liv Glacier Liv Glacier is a steep vall ...
and north of
Juneau The City and Borough of Juneau, more commonly known simply as Juneau ( ; tli, Dzánti K'ihéeni ), is the capital city of the state of Alaska. Located in the Gastineau Channel and the Alaskan panhandle, it is a unified municipality and the se ...
on the western margin of the Juneau Icefield. Precipitation runoff and glacial meltwater from the mountain's north slope drains to
Berners Bay Berners Bay (Lingít: ''Dax̱anáak'' or ''Wóoshde X̱’al.át Yé'') is a waterway in the U.S. state of Alaska, approximately north of Juneau. It is a large and deep indentation, about wide at the entrance, which is formed by Point Bridget and ...
and Lynn Canal via the Gilkey River, whereas the south slope is surrounded by the Taku Glacier. Topographic relief is significant as the north face rises 4,500 feet (1,370 m) in . The mountain's descriptive name was applied by members of the Juneau Icefield Research Project in 1964 and the toponym was officially adopted in 1965 by the
United States Board on Geographic Names The United States Board on Geographic Names (BGN) is a federal body operating under the United States Secretary of the Interior. The purpose of the board is to establish and maintain uniform usage of geographic names throughout the federal governm ...
.


Climate

Based on the Köppen climate classification, Glacier King is located in a tundra climate zone with long, cold, snowy winters, and cool summers. Weather systems coming off the Gulf of Alaska are forced upwards by the Coast Mountains ( orographic lift), causing heavy precipitation in the form of rainfall and snowfall. Winter temperatures can drop to 0 °F with wind chill factors below −10 °F. This climate supports the Taku Glacier south of the peak, the Juneau Icefield east of the peak, and unnamed glaciers on the north slope.


See also

* Geospatial summary of the High Peaks/Summits of the Juneau Icefield * Geography of Alaska


References


External links

* Glacier King
weather forecast
{{Portal bar, Mountains, Geography, Alaska Mountains of Alaska Mountains of Juneau, Alaska North American 1000 m summits Boundary Ranges Coast Mountains Tongass National Forest