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Whitney Glacier information


Whitney
Map showing the location of Whitney
Map showing the location of Whitney
Whitney
Location in California
Map showing the location of Whitney
Map showing the location of Whitney
Whitney
Whitney (the United States)
TypeMountain glacier
LocationMount Shasta,
Siskiyou County, California, United States
Coordinates41°24′50″N 122°12′41″W / 41.41389°N 122.21139°W / 41.41389; -122.21139[1]
Area.5 sq mi (1.3 km2)
Length2 mi (3.2 km)
Thickness126 ft (38 m) in 1986
TerminusMoraine
StatusExpanding

The Whitney Glacier is a glacier situated on Mount Shasta, in the U.S. state of California.[2][3] The Whitney Glacier is the longest glacier and the only valley glacier in California. In area and volume, it ranks second in the state behind the nearby Hotlum Glacier. In 1986, the glacier was measured to be 126 ft (38 m) deep and over three km in length.[4] The glacier starts on Mount Shasta's Misery Hill at 13,700 ft (4,200 m) and flows northwestward down to the saddle between Mount Shasta and Shastina,[5] where uneven ground causes a major icefall at 11,800 ft (3,600 m).[5] It then flows down the valley between the two peaks, reaching its terminus at 9,500 to 9,800 ft (2,900 to 3,000 m).[5][6]

  1. ^ "Whitney Glacier". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved September 30, 2012.
  2. ^ "Existing Glaciers of Mount Shasta". College of the Siskiyous. Retrieved January 23, 2007.
  3. ^ "Glaciers of California". Glaciers of the American West. Glaciers Online. Archived from the original on September 3, 2006. Retrieved January 23, 2007.
  4. ^ Driedger, Carolyn L.; Kennard, Paul M. (1986). "Ice volumes on Cascade volcanoes; Mount Rainier, Mount Hood, Three Sisters, and Mount Shasta". U.S. Geological Survey Professional Paper 1365. Retrieved March 6, 2007.
  5. ^ a b c Google Earth elevation for GNIS coordinates.
  6. ^ "Whitney Glacier, USGS MOUNT SHASTA (CA) Topo Map". USGS Quad maps. TopoQuest.com. Retrieved July 5, 2008.

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