Mount Gould (9,557 ft (2,913 m)) is a peak on the Continental Divide in Glacier National Park, Montana, United States.[4] It is the highest point of the Garden Wall, a distinctive ridge of the Lewis Range. It is most notable for its huge, steep east face, which drops 4,000 ft (1,220 m) in only one-half mile (0.8 km). This face provides a backdrop to Grinnell Lake, and is often photographed.
| Mount Gould | |
|---|---|
 Mount Gould with eastern cliff face | |
| Highest point | |
| Elevation | 9,557 ft (2,913 m)[1] |
| Prominence | 1,953 ft (595 m)[1] |
| Parent peak | Mount Siyeh |
| Isolation | 3.13 mi (5.04 km)[2] |
| Listing | Mountains in Glacier County, Montana |
| Coordinates | 48°44′34″N 113°42′52″W / 48.74278°N 113.71444°W[3] |
| Geography | |
  Mount Gould | |
| Parent range | Lewis Range |
| Topo map | USGS Logan Pass |
| Geology | |
| Rock type | limestone, diorite |
| Climbing | |
| First ascent | 1920 by Frank B. Wynn, Harry R. Horn, Henry H. Goddard, and party |
| Easiest route | West Face (scramble/Class 3) |
Mount Gould was named in 1887 by George Bird Grinnell for his hunting companion, George H. Gould, and the name was officially adopted in 1929 by the United States Board on Geographic Names.[5]
The first recorded[6] ascent of Mount Gould was in 1920, by Frank B. Wynn, Harry R. Horn, Henry H. Goddard, and party. They used the West Face route, which is the easiest and most commonly used route today. It starts from the Highline Trail, which skirts the west side of the peak, and involves some rock scrambling but no technical climbing.
Climbing the sheer East Face of Mount Gould is theoretically possible; however the brittle, loose nature of the rock in Glacier National Park makes the ascent highly technical, unpleasant, and dangerous.[citation needed]
Climate
editBased on the Köppen climate classification, Mount Gould is located in an alpine subarctic climate zone characterized by long, usually very cold winters, and short, cool to mild summers.[7] Temperatures can drop below −10 °F with wind chill factors below −30 °F.
Geology
editLike the mountains in Glacier National Park, Mount Gould is composed of sedimentary rock laid down during the Precambrian to Jurassic periods. Formed in shallow seas, this sedimentary rock was initially uplifted beginning 170 million years ago when the Lewis Overthrust fault pushed an enormous slab of precambrian rocks 3 mi (4.8 km) thick, 50 miles (80 km) wide and 160 miles (260 km) long over younger rock of the cretaceous period.[8] The bulk of the peak is composed of limestone of the Siyeh Formation, and the conspicuous dark band on the east face is a diorite sill.[9]
See also
editNotes
edit- ^ a b "Mount Gould, Montana". Peakbagger.com. Retrieved June 12, 2018.
- ^ "Gould, Mount - 9,553' MT". listsofjohn.com. Retrieved 2021-08-10.
- ^ "Mount Gould". Geographic Names Information System. United States Geological Survey, United States Department of the Interior. Retrieved June 12, 2018.
- ^ Logan Pass, MT (Map). TopoQwest (United States Geological Survey Maps). Retrieved June 12, 2018.
- ^ Decisions of the United States Geographic Board, Place Names, Glacier National Park, Mont., US Government Printing Office, March 6, 1929, page 7.
- ^ Since access to the summit is nontechnical, an earlier ascent, and perhaps a much earlier Native American ascent, is possible.
- ^ 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): 1633–1644. Bibcode:2007HESS...11.1633P. doi:10.5194/hess-11-1633-2007. ISSN 1027-5606. S2CID 9654551.
- ^ Gadd, Ben (2008). "Geology of the Rocky Mountains and Columbias".
{{cite journal}}: Cite journal requires|journal=(help) - ^ James L. Dyson, The Geologic Story of Glacier National Park
Sources
edit- J. Gordon Edwards and Josephine Gould, A Climber's Guide to Glacier National Park, Falcon Press, 1991. ISBN 0-87842-177-7.
External links
edit
- Weather forecast: Mount Gould