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Martin volcano

Stratovolcano 1863 m / 6,112 ft
United States, Alaska Peninsula, 58.17°N / -155.36°W
Current status: dormant (1 out of 5)
Martin volcano books
Typical eruption style: unspecified
Martin volcano eruptions: 1953 
TimeMag. / DepthDistanceLocation
Sun, 7 Jan
Sun, 7 Jan 15:30 UTCM 2.4 / 98.1 km28 km- 107km SSE of King Salmon, Alaska
Sun, 7 Jan 12:03 UTCM 2.02 km- 92km WNW of Larsen Bay, Alaska
Wed, 3 Jan
Wed, 3 Jan 23:20 UTCM 1.8 / 0.3 km3 km- 91km SE of King Salmon, Alaska
Wed, 3 Jan 18:40 UTCM 1.5 / 0.7 km3 km- 91km SE of King Salmon, Alaska
Wed, 3 Jan 16:17 UTCM 3.2 / 4.8 km23 km- 109km SSE of King Salmon, Alaska
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Background:

The mostly ice-covered Mount Martin stratovolcano lies at the SW end of the Katmai volcano cluster in Katmai National Park. The volcano was named for George C. Martin, the first person to visit and describe the Katmai area after the 1912 eruption. Mount Martin is capped by a 300-m-wide summit crater, which is ice-free because of an almost-constant steam plume and contains a shallow acidic lake. The edifice of Martin volcano overlies glaciated lava flows of the adjacent mid- to late-Pleistocene Alagoshak volcano on the WSW and was constructed entirely during the Holocene. Mount Martin consists of a small fragmental cone that was the source of ten thick overlapping blocky dacitic lava flows, largely uneroded by glaciers, that descend 10 km to the NW, cover 31 sq km, and form about 95% of the eruptive volume of the volcano. Two reports of historical eruptions that originated from uncertain sources were attributed by Muller et al. (1954) to Martin.
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Smithsonian / GVP volcano information

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