Red Mountain (Glacier County, Montana)
Mountain in the state of Montana From Wikipedia, the free encyclopedia
Red Mountain (9,382 feet (2,860 m)) is located in the Lewis Range, Glacier National Park in the U.S. state of Montana. Red Mountain is 2.75 miles (4.43 km) north of Rising Wolf Mountain.[3]
| Red Mountain | |
|---|---|
 Southwest aspect | |
| Highest point | |
| Elevation | 9,382 ft (2,860 m)[1] |
| Prominence | 1,937 ft (590 m)[1] |
| Parent peak | Rising Wolf Mountain[1] |
| Listing | Mountains in Glacier County, Montana |
| Coordinates | 48°32′08″N 113°25′27″W[2] |
| Geography | |
  Red Mountain Location in Montana  Red Mountain Location in the United States | |
| Location | Glacier County, Montana, U.S. |
| Parent range | Lewis Range |
| Topo map(s) | USGS Cut Bank Pass, MT |
Based on the Köppen climate classification, it is located in an alpine subarctic climate zone with long, cold, snowy winters, and cool to warm summers.[4] Winter temperatures can drop below −10 °F with wind chill factors below −30 °F.
| Climate data for Red Mountain, Glacier County (MT) 48.5341 N, 113.4066 W, Elevation: 8,717 ft (2,657 m) (1991–2020 normals) | |||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Month | Jan | Feb | Mar | Apr | May | Jun | Jul | Aug | Sep | Oct | Nov | Dec | Year |
| Mean daily maximum °F (°C) | 22.9 (−5.1) |
23.6 (−4.7) |
29.1 (−1.6) |
33.2 (0.7) |
42.5 (5.8) |
50.4 (10.2) |
61.5 (16.4) |
61.8 (16.6) |
52.8 (11.6) |
39.0 (3.9) |
27.2 (−2.7) |
21.7 (−5.7) |
38.8 (3.8) |
| Daily mean °F (°C) | 16.6 (−8.6) |
15.9 (−8.9) |
20.3 (−6.5) |
24.7 (−4.1) |
33.3 (0.7) |
40.7 (4.8) |
50.4 (10.2) |
50.5 (10.3) |
42.3 (5.7) |
30.9 (−0.6) |
21.0 (−6.1) |
15.6 (−9.1) |
30.2 (−1.0) |
| Mean daily minimum °F (°C) | 10.3 (−12.1) |
8.2 (−13.2) |
11.4 (−11.4) |
16.2 (−8.8) |
24.2 (−4.3) |
31.0 (−0.6) |
39.4 (4.1) |
39.2 (4.0) |
31.7 (−0.2) |
22.9 (−5.1) |
14.9 (−9.5) |
9.5 (−12.5) |
21.6 (−5.8) |
| Average precipitation inches (mm) | 8.30 (211) |
6.00 (152) |
7.32 (186) |
5.80 (147) |
5.35 (136) |
6.32 (161) |
2.08 (53) |
2.26 (57) |
3.92 (100) |
5.73 (146) |
7.86 (200) |
7.63 (194) |
68.57 (1,743) |
| Source: PRISM Climate Group[5] | |||||||||||||
Like other mountains in Glacier National Park, it 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.[6]
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