Helmet Peak is a monogenetic cinder cone of the Milbanke Sound Group in British Columbia, Canada. The basaltic tuff breccias on Lake Island and Lady Douglas Island originated from Helmet Peak on Lady Island.
| Helmet Peak | |
|---|---|
  Helmet Peak | |
| Highest point | |
| Elevation | 318 m (1,043 ft)[1] |
| Prominence | 318 m (1,043 ft)[1] |
| Listing | |
| Coordinates | 52°21′16″N 128°21′01″W / 52.35444°N 128.35028°W[2] |
| Geography | |
| Country | Canada |
| Province | British Columbia |
| Parent range | Kitimat Ranges |
| Topo map | NTS 103A8 Spiller Channel |
| Geology | |
| Age of rock | Holocene[citation needed] |
| Mountain type | Monogenetic cinder cone |
| Volcanic arc/belt | Milbanke Sound Group |
| Last eruption | Unknown |
See also edit
References edit
- ^ a b "Helmet Peak". Bivouac.com. Retrieved 2023-05-08.
- ^ "Helmet Peak (British Columbia)". BC Geographical Names. Retrieved 2023-05-08.
External links edit
- "Topographic map of Helmet Peak". opentopomap.org. Retrieved 2023-05-08.
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