PhotosLocation


Mount_Parker_(Alaska) Latitude and Longitude:

58°51′45″N 136°53′10″W / 58.8625421°N 136.8862367°W / 58.8625421; -136.8862367
From Wikipedia, the free encyclopedia
Mount Parker
Northwest aspect, above Lamplugh Glacier
Highest point
Elevation3,170 ft (966 m) [1]
Prominence220 ft (67 m) [2]
Isolation1.65 mi (2.66 km) [2]
Coordinates 58°51′45″N 136°53′10″W / 58.8625421°N 136.8862367°W / 58.8625421; -136.8862367 [3]
Naming
EtymologyAbraham L. Parker [4]
Geography
Mount Parker is located in Alaska
Mount Parker
Mount Parker
Location in Alaska
CountryUnited States
State Alaska
Census Area Hoonah–Angoon
Protected area Glacier Bay National Park
Parent range Saint Elias Mountains
Fairweather Range [1]
Topo map USGS Mount Fairweather D-3
Geology
Age of rock Cretaceous [5]
Type of rock Granodiorite [5]

Mount Parker is a 3,170-foot (966 m) mountain summit in the US state of Alaska.

Description

Mount Parker is located in the Fairweather Range of the Saint Elias Mountains. It is set within Glacier Bay National Park and Preserve and is situated 3.4 miles (5.5 km) east of Mount Cooper. [1] Although modest in elevation, topographic relief is significant as the summit rises from tidewater of Glacier Bay in 1.7 miles (2.7 km) and the west face rises 2,000 feet (610 m) above the Lamplugh Glacier in 0.5 mi (0.80 km). The mountain's toponym has been officially adopted by the U.S. Board on Geographic Names. [3]

Climate

Based on the Köppen climate classification, Mount Parker is located in a marine subpolar climate zone, with long, cold, snowy winters, and cool summers. [6] Weather systems coming off the Gulf of Alaska are forced upwards by the Saint Elias Mountains ( orographic lift), causing heavy precipitation in the form of rainfall and snowfall. Winter temperatures can drop below 0 °F with wind chill factors below −10 °F. This climate supports the Reid and Lamplugh glaciers on opposite sides of this peak.

Geology

The dominant rock of the Mount Parker area between Lamplugh Glacier and Reid Glacier is granodiorite and quartz diorite which contains quartz vein gold lodes. The gold was processed by six mines of the Reid Inlet gold area. The LeRoy Mine was the largest mine, discovered in 1938 by Gustavus founder and resident, Abraham L. Parker (1866–1941), and his son, Leslie F. Parker. [5] [7]

See also

References

  1. ^ a b c "Mount Parker, Alaska". Peakbagger.com. Retrieved 2024-02-10.
  2. ^ a b "Parker, Mount - 3,170' Alaska". listsofjohn.com. Retrieved 2024-02-10.
  3. ^ a b "Mount Parker". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved 2024-02-10.
  4. ^ United States Congress House Committee on Interior and Insular Affairs, 1962, US Government Printing Office, p. 829.
  5. ^ a b c Rossman, Darwin (1959). Geology and Ore Deposits in the Reid Inlet Area, Glacier Bay, Alaska, USGS Bulletin 1058-B. Washington: US Government Printing Office. pp. 38–41.
  6. ^ Peel, M. C.; Finlayson, B. L.; McMahon, T. A. (2007). "Updated world map of the Köppen−Geiger climate classification". Hydrol. Earth Syst. Sci. 11 (5): 1633. Bibcode: 2007HESS...11.1633P. doi: 10.5194/hess-11-1633-2007. ISSN  1027-5606.
  7. ^ A History of Administration and Visitor Use in Glacier Bay National Park and Preserve, Chapter VII: Private Interests and a Second Boundary Adjustment, nps.gov, Retrieved 2024-02-10.

External links