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Martin volcano

Stratovolcano 1863 m / 6,112 ft
United States, Alaska Peninsula, 58.17°N / -155.36°W
Current status: normal or dormant (1 out of 5) | Reports
Martin volcano books
Typical eruption style: unspecified
Martin volcano eruptions: 1953 
TimeMag. / DepthDistanceLocation
Thu, 15 Aug 2019
Thu, 15 Aug 15:48 UTCM 1.75 km90km SE of King Salmon, Alaska (USA)
Tue, 13 Aug 2019
Tue, 13 Aug 18:10 UTCM 1.15 km90km SE of King Salmon, Alaska (USA)
Thu, 8 Aug 2019
Thu, 8 Aug 12:49 UTCM 1.6 / 0.4 km3 km93km SE of King Salmon, Alaska (USA)
Wed, 7 Aug 2019
Wed, 7 Aug 10:01 UTCM 0.3 / 1.1 km1 km95km SE of King Salmon, Alaska (USA)
Thu, 1 Aug 2019
Thu, 1 Aug 15:48 UTCM 1.5 / 1.6 km1 km95km SE of King Salmon, Alaska (USA)
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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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