| Gable Peaks | |
| Elevation Ft: | 7700. |
| Elevation Ref: | [1] |
| Prominence Ft: | 480. |
| Isolation Mi: | 3.34 |
| Parent Peak: | Trilobite Peak (8,245 ft) |
| Location: | Flathead County, Montana, U.S. |
| Map: | Montana#USA |
| Relief: | 1 |
| Label Position: | right |
| Range: | Rocky Mountains Flathead Range Trilobite Range |
| Coordinates: | 48.04°N -113.1755°W |
| Topo: | USGS Gable Peaks |
| Rock: | Sedimentary rock |
| Age: | Precambrian |
Gable Peaks is a remote 7700abbr=offNaNabbr=off double summit mountain located in Flathead County of the U.S. state of Montana.[2]
Gable Peaks is located at the north end of the Trilobite Range, which is a subset of the Flathead Range. It is situated on the common boundary shared by Great Bear Wilderness and the Bob Marshall Wilderness, on land managed by Flathead National Forest. The 7,700-foot north peak and 7,698-foot south peak are 0.35 mile apart.[3] Precipitation runoff from the mountain drains north to the Middle Fork Flathead River, and topographic relief is significant as the summit rises over 2700abbr=offNaNabbr=off above the river in approximately 1.5 mile. The nearest higher neighbor is Cruiser Mountain, 3.5miles to the south-southeast.
Based on the Köppen climate classification, Gable Peaks is located in a subarctic climate zone characterized by long, usually very cold winters, and short, cool to mild summers.[4] Winter temperatures can drop below −10 °F with wind chill factors below −30 °F.
Gable Peaks 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.[5]