| Ice Peak | |
|---|---|
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| Highest point | |
| Elevation | 2,526 m (8,287 ft) |
| Prominence | 56 m (184 ft) |
| Parent peak | Mount Edziza |
| Coordinates | 57°41′26″N 130°38′08″W / 57.69056°N 130.63556°WCoordinates: 57°41′26″N 130°38′08″W / 57.69056°N 130.63556°W |
| Geography | |
| Location | British Columbia, Canada |
| Parent range | Tahltan Highland |
| Topo map | NTS 104G/10 |
| Geology | |
| Age of rock | |
| Mountain type | Stratovolcano |
| Volcanic belt | Northern Cordilleran Volcanic Province |
| Last eruption | Holocene |
Ice Peak is a stratovolcano, located 39 km (24 mi) west of Tatogga and 3 km (2 mi) south of Mount Edziza, British Columbia, Canada. It overlaps the 7.5-million-year-old Armadillo Peak. It lies on a large volcanic plateau, which is made of basaltic lava flows from the massive Mount Edziza volcanic complex. Ice Peak last erupted during the Holocene.
The summit of Ice Peak is a remnant of the western rim of a small summit caldera, which has been nearly destroyed by alpine glaciation.
Ice Peak gets name because it is almost completely surrounded by glaciers.