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Snowy Mountain volcano

Stratovolcanoes 2162 m / 7,093 ft
United States, Alaska Peninsula, 58.34°N / -154.68°W
Current status: dormant (1 out of 5)
Snowy Mountain volcano books
Typical eruption style: unspecified
Snowy Mountain volcano eruptions: 1710 ± 200 years
TimeMag. / DepthDistanceLocation
Sun, 16 Apr
Sun, 16 Apr 21:39 UTCM 1.9 / 0.1 km1 km- 99km ESE of King Salmon, Alaska
Thu, 13 Apr
Thu, 13 Apr 14:00 UTCM 1.8 / 101.5 km9 km- 90km NW of Larsen Bay, Alaska
Mon, 10 Apr
Mon, 10 Apr 14:02 UTCM 2.0 / 90.4 km29 km- 69km NNW of Larsen Bay, Alaska
Mon, 20 Mar
Mon, 20 Mar 15:36 UTCM 2.8 / 10.8 km2 km- 95km ESE of King Salmon, Alaska
View all recent quakes

Background:

Glacier-covered, 2161-m-high Snowy Mountain, located 15 km NE of Mount Katmai, is the SW-most of a chain of closely spaced volcanoes extending NE along the crest of the Alaska Range. More than 90% of the compound Snowy volcano is mantled by glacial ice, which prompted the naming of the volcano by members of the 1917 Katmai expedition. Two small andesitic-dacitic stratovolcanoes, SW Snowy and NE Snowy, originated about 200,000 years ago. Only NE Snowy has been active during the Holocene. Late-Holocene collapse of this volcano produced a large debris avalanche that traveled to the north and left a large breached crater inside which a blocky lava dome was constructed. Peat beneath an ash layer thought to be associated with the the lava dome was radiocarbon dated at about 250 +/- 70 years ago. No historical eruptive activity has been documented, but fumarolic activity has been observed at NE Snowy. A zone of persistent diffuse shallow seismicity is located on and NW of the volcano.
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Smithsonian / GVP volcano information


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