| Crypt Peak | |
| Elevation Ft: | 8579 |
| Elevation Ref: | [1] |
| Prominence Ft: | 1021 |
| Isolation Mi: | 1.59 |
| Range: | Lewis Range Rocky Mountains |
| Parent Peak: | Miche Wabun Peak (8,861 ft) |
| Location: | Glacier National Park Glacier County, Montana, U.S. |
| Map: | USA Montana#USA |
| Label Position: | bottom |
| Coordinates: | 48.998°N -113.8251°W |
| Topo: | USGS Mount Cleveland |
| Rock: | Sedimentary rock |
| Age: | Precambrian |
Crypt Peak is an 85790NaN0 mountain summit located in Glacier National Park, in Glacier County of the U.S. state of Montana. It is situated along the Canada–United States border, above Crypt Lake, and is partially within Waterton Lakes National Park. Crypt Peak is part of the Lewis Range, and is approximately three miles east of Waterton Lake. Topographic relief is significant as Crypt Peak rises over 2100abbr=offNaNabbr=off above Crypt Lake in approximately one-half mile (1.6 km), and 4400-1NaN-1 above Waterton Lake in 3miles. Precipitation runoff from the mountain drains west to Waterton Lake, and east to Belly River. This geographical feature's name has not yet been officially adopted by the United States Board on Geographic Names.
Based on the Köppen climate classification, Crypt Peak is located in an alpine subarctic climate zone characterized by long, usually very cold winters, and short, cool to mild summers.[2] Temperatures can drop below −10 °F with wind chill factors below −30 °F.
Like the mountains in Glacier National Park, Crypt Peak 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 31NaN1 thick, 50miles wide and 160miles long over younger rock of the cretaceous period.[3] The reddish rock at the top of Crypt Peak is argillite.[4]