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Segula volcano

Stratovolcano 1160 m / 3,806 ft
United States, Aleutian Islands, 52.02°N / 178.14°E
Current status: dormant (1 out of 5) | Reports
Segula volcano books
Typical eruption style: unspecified
Segula volcano eruptions: unknown, no recent eruptions
TimeMag. / DepthDistanceLocation
Wed, 31 Jan
Wed, 31 Jan 00:57 UTCM 2.2 / 3 km5 km- 6km NE of Little Sitkin Island, Alaska
Mon, 22 Jan
Mon, 22 Jan 04:47 UTCM 3.2 / 71.7 km38 km- 37km S of Kiska Volcano, Alaska
Sat, 20 Jan
Sat, 20 Jan 19:43 UTCM 4.7 / 131.1 km13 km- 13km SSE of Little Sitkin Island, Alaska
Sat, 13 Jan
Sat, 13 Jan 01:35 UTCM 5.2 / 75.5 km102 km- 37km WSW of Little Sitkin Island, Alaska
View all recent quakes

Background:

The 6 x 7 km island of Segula east of Kiska volcano consists of a conical stratovolcano cut by a prominent NNW-SSE-trending fissure that extends to sea level at both ends of the island. The northern end of the fissure is flooded by the sea to produce a long, narrow cove. Segula was constructed above a 100-m-deep submarine platform that extends eastward to Khvostof and Davidof islands. A submarine debris-avalanche deposit extends up to 18 km offshore to the north. The summit of Segula contains a small, poorly defined caldera that is partly overtopped on the south by a cinder cone that forms the 1153 m high point of the island and on the north by extensive lava flows that reach the NE coast along a broad front. Another lava field on the SE coast originated from a cinder cone at 300 m altitude on the SE flank. No historical eruptions are known from Segula, but Nelson (1959) considered fresh lava flows on the north flank to possibly be only a few hundred years old.
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Smithsonian / GVP volcano information


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