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)
Segula volcano books
United States, Aleutian Islands, 52.02°N / 178.14°E
Current status: dormant (1 out of 5)
Segula volcano books
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Typical eruption style: unspecified
Segula volcano eruptions: unknown, no recent eruptions
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Segula volcano eruptions: unknown, no recent eruptions
| Time | Mag. / Depth | Distance | Location |
| Wed, 14 Jun | |||
| Wed, 14 Jun 08:53 UTC | M 2.7 / 102.1 km | 16 km | - 14km SSW of Little Sitkin Island, Alaska |
| Sat, 3 Jun | |||
| Sat, 3 Jun 19:14 UTC | M 3.8 / 119.1 km | 15 km | - 30km SSW of Little Sitkin Island, Alaska |
| Sat, 3 Jun 13:34 UTC | M 3.0 / 103 km | 19 km | - 18km SSW of Little Sitkin Island, Alaska |
| Thu, 1 Jun | |||
| Thu, 1 Jun 03:15 UTC | M 3.1 / 111.2 km | 8 km | - 6km SSW of Little Sitkin Island, Alaska |
| Tue, 30 May | |||
| Tue, 30 May 16:30 UTC | M 2.0 / 18.4 km | 26 km | - 33km NNW of Little Sitkin Island, Alaska |
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.---
Smithsonian / GVP volcano information
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