Exile Hill | |
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Exile Peak | |
![]() Geological cross section of Exile Hill | |
Highest point | |
Elevation | 1,890 m (6,200 ft)[1] |
Coordinates | 57°22′41″N 130°49′29″W / 57.37806°N 130.82472°W[2] |
Geography | |
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Location in Mount Edziza Provincial Park | |
Country | Canada[3] |
Province | British Columbia[3] |
District | Cassiar Land District[2] |
Protected area | Mount Edziza Provincial Park[2] |
Parent range | Tahltan Highland[3] |
Topo map | NTS 104G7 Mess Lake[2] |
Geology | |
Formed by | Volcanism[4] |
Mountain type(s) | Cinder cone, plug dome[5][6] |
Rock type(s) | Basalt, trachyte[7] |
Last eruption | Pliocene age[5] |
Exile Hill, sometimes referred to as Exile Peak, is an isolated hill in Cassiar Land District of northwestern British Columbia, Canada. It has an elevation of 1,890 metres (6,200 feet) and is part of the Arctic Lake Plateau or the neighbouring Spectrum Range, which are within the limits of the Tahltan Highland. Exile Hill is about 60 kilometres (37 miles) southeast of the community of Telegraph Creek in Mount Edziza Provincial Park. Access to Exile Hill is via aircraft which are permitted to land on Mess Lake and Little Arctic Lake to the northwest and southeast, respectively.
Exile Hill is part of the Mount Edziza volcanic complex, which consists of diverse landforms such as shield volcanoes, stratovolcanoes, lava domes and cinder cones. The volcanic rocks comprising the hill are of Pliocene age and are subdivided into two geological formations that were deposited during the second magmatic cycle of the Mount Edziza volcanic complex. Basalt comprises the Nido Formation whereas the younger Spectrum Formation consists of trachyte. Nearby volcanic features include Outcast Hill, Tadekho Hill, Kuno Peak, Nahta Cone and Wetalth Ridge.
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