| Stanton Mountain | |
| Elevation Ft: | 7750 |
| Elevation Ref: | [1] |
| Prominence Ft: | 630 |
| Isolation Mi: | 1.66 |
| Isolation Ref: | [2] |
| Parent Peak: | Mount Vaught (8,854 ft) |
| Etymology: | Lottie Stanton |
| Location: | Flathead County, Montana, U.S. |
| Map: | Montana#USA |
| Relief: | 1 |
| Label Position: | bottom |
| Coordinates: | 48.6599°N -113.8942°W |
| Topo: | USGS Camas Ridge East |
| Easiest Route: | scrambling |
Stanton Mountain is a 7750feet mountain summit located in the Livingston Range, of Glacier National Park in the U.S. state of Montana.[3] Stanton Mountain rises more than 4500feet above the northern shore of Lake McDonald. The mountain's name refers to Mrs. Lottie Stanton who lived near the west side of the park in the late 1800s, and with her husband operated a livery stable in historic Demersville.[4] She was a pioneering woman who followed the construction camps during the railroad building days.[5] The mountain's name was officially adopted in 1929.[3] In the late 1800s it was known as Mt. Lottie Stanton.[6] The nearest higher peak is Mount Vaught, 1.38miles to the northeast.[1] Precipitation runoff from the mountain drains into tributaries of the Flathead River.
Based on the Köppen climate classification, Stanton Mountain is located in a 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.
Like other mountains in Glacier National Park, Stanton Mountain 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.[8]