| Atlin Volcanic Field | |
|---|---|
  Atlin Volcanic Field | |
| Highest point | |
| Elevation | 1,880 m (6,170 ft)[1] |
| Listing | Northern Cordilleran volcanoes |
| Coordinates | 59°41′N 133°19′W / 59.68°N 133.32°W[1] |
| Geography | |
| Location | British Columbia, Canada |
| Parent range | Teslin Plateau (southern Yukon Plateau) |
| Geology | |
| Rock age | Holocene |
| Mountain type | Cinder cones |
| Volcanic arc/belt | Northern Cordilleran Volcanic Province |
| Last eruption | Unknown, possible eruptions in 1898.[1] |
The Atlin Volcanic Field, also called the Llangorse Volcanic Field and the Surprise Lake Volcanic Field, is a group of late-Pleistocene to Holocene cinder cones that lies on the Teslin Plateau east of Atlin Lake, Canada. The largest volcanic feature is the 1880-m-high Ruby Mountain which has been partially dissected by Pleistocene and post-Wisconsin glaciation. Two basaltic cinder cones at the heads of Cracker Creek and Volcanic Creek lie within glacially dissected U-shaped valleys and may be of postglacial age.