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Mount Veniaminof

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|- | style="border-top:1px solid #999966; border-right:1px solid #999966" bgcolor=#e7dcc3 width=85 | Coordinates: | style="border-top:1px solid #999966" width=220 | [56°11′53″N, 159°23′27″W]Coordinates: |-

|- | style="border-top:1px solid #999966; border-right:1px solid #999966" bgcolor=#e7dcc3 width=85 | Topo map: | style="border-top:1px solid #999966" width=220 | USGS Chignik A-5 |-

|- | style="border-top:1px solid #999966; border-right:1px solid #999966" bgcolor=#e7dcc3 width=85 | Type: | style="border-top:1px solid #999966" width=220 | Stratovolcano |- | style="border-top:1px solid #999966; border-right:1px solid #999966" bgcolor=#e7dcc3 width=85 | Age of rock: | style="border-top:1px solid #999966" width=220 | |- | style="border-top:1px solid #999966; border-right:1px solid #999966" bgcolor=#e7dcc3 width=85 | Last eruption: | style="border-top:1px solid #999966" width=220 | 2005 |-

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Mount Veniaminof is a volcano located on the Alaska Peninsula. The mountain was named after Ioann (Ivan Popov) Veniaminov (1797-1879), a Russian Orthodox missionary priest whose writings on the Aleut language and ethnology are still standard references.

The volcano was the site of a colossal (VEI 6) eruption around 1750 BC. This eruption left a large caldera. In modern times the volcano has had numerous small eruptions (over ten of them since 1930); these are located at a cinder cone in the middle of the caldera.

Veniaminof has one of the highest elevations of Alaskan volcanoes. Partly for this reason, it is covered by a glacier that fills most of the caldera. Because of the glacier and the caldera walls, there is the possibility for a major flood from a glacier run at some point in the future.

Map showing volcanoes of Alaska Peninsula.
Enlarge
Map showing volcanoes of Alaska Peninsula.

Sources

 


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