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Canada · Volcanic field

Fort Selkirk volcanic field

Fort Selkirk

Type
Volcanic field
Elevation
1239m
Last eruption
Unknown
Volcano Mountain is a cone within the Fort Selkirk volcanic field in the central Yukon Territory, near the junction of the Yukon and Pelly rivers, and is Canada's northernmost Holocene volcano. Volcano Mountain comprises a scoria cone and a series of lava flows that traveled to the NE and SW.
Volcano Mountain is a cone within the Fort Selkirk volcanic field in the central Yukon Territory, near the junction of the Yukon and Pelly rivers, and is Canada's northernmost Holocene volcano. Volcano Mountain comprises a scoria cone and a series of lava flows that traveled to the NE and SW. · Photo: Photo by Lionel Jackson (Geological Survey of Canada).
Type
Volcanic field
Country
Canada
Region
North America / Northern Cordilleran Volcanic Province
Elevation
1239m
Coordinates
62.930, -137.380
Last eruption
Unknown
Tectonic setting
Intraplate / Continental crust (> 25 km)
Landform
Cluster
Major rock type
Trachybasalt / Tephrite basanite

Geological summary

The Fort Selkirk volcanic field near the junction of the Yukon and Pelly rivers in central Yukon is the northernmost Holocene volcanic field in Canada.

Excerpt from the Global Volcanism Program, Smithsonian Institution · Read the full summary on GVP →

From Wikipedia

The Fort Selkirk volcanic field is a monogenetic volcanic field in the Northern Cordilleran Volcanic Province, Yukon Territory, Canada. It is the northernmost Holocene age volcanic field in Canada, located close to the connection of the Yukon and Pelly rivers. The youngest eruptions within the field are unknown. However, the youngest volcano Volcano Mountain produced lava flows that appear to be only a few hundred years old.

Wikipedia · CC BY-SA · Read full article →

Eruption history

Glossary

Detailed timeline

No eruption records available.

Nearby volcanoes

External links

⚠ For reference only. Not for emergency response.