Gareloi Island
Anangusix̂, Île Gareloi
51°47′N 178°48′W
Gareloi (Russian: Горелый) or Anangusook (Aleut: Anangusix̂) is a volcanic island in the Delarof Islands of the Aleutian Islands of Alaska. It is located between the Tanaga Pass and the Amchitka Pass.

Terrain
51°47′N 178°48′W
Overview
Gareloi (Russian: Горелый) or Anangusook (Aleut: Anangusix̂) is a volcanic island in the Delarof Islands of the Aleutian Islands of Alaska. It is located between the Tanaga Pass and the Amchitka Pass. The island is 6 miles (9.7 km) in length and 5 miles (8.0 km) wide. Its land area is 25.95 square miles (67.2 km2), making Gareloi the largest island in the Delarof group. Gareloi Volcano, a stratovolcano, is situated in the center of the island which reaches a height of 5,161 feet (1,573 m). On the other side of a small saddle lies another peak of the island however it does not equal the height of Mount Gareloi. The island is uninhabited. Coastal cliffs provide nesting habitat for more than 600,000 seabirds, mostly for crevice nesting auklets. Least Auklets account for 62% of the colony, Crested Auklets for 30%, and Parakeet Auklets for 6%. Each of these species is present on the island in numbers exceeding 1% of their global populations. The island consists of lava rock, black lava, eroded lava, and ashes; the lower slopes and valleys are covered with grass and tundra in many places. The shores have steep cliffs with rocks and boulders at the base; boulders, pinnacles, and rocks awash extend around the shoreline. Heavy kelp surrounds most of the island, and extends offshore to 10 fathoms (18 m). Depths of 10 fathoms or more are within 0.5 miles (800 m) of the island. A trapper's hut is on the beach above the N shore of Gareloi Island. Gareloi's northern, slightly higher peak is on the southern rim of a crater about 330 yards (300 m) across, which contains several active fumaroles. Thirteen younger craters, from 87 yards (80 m) to 1 mile (1,600 m) in diameter, are aligned along a south-southeast trending fissure that extends from strandline to the southern summit. These craters formed during a major explosive eruption in 1929 that also produced four blocky lava flows, and a blanket of grassy andesitic tuff that covers an area roughly 1.5 by 3 miles (2.4 by 4.8 km) on the volcano's southeast flank. Gareloi Volcano had four confirmed eruptions in the 1980s and one unconfirmed eruption in 1996. All but one of them were considered explosive eruptions. In Spring and Summer 2007 there was a period of increased seismic activity on Gareloi Island, sometimes reaching 40 earthquakes per day.
From Wikipedia, CC BY-SA 4.0
Chart
Nearest islands
- Ogliuga Island24 km
- 24 km
- Kavalga Island26 km
- Skagul Island26 km
- Unalga Island29 km
- Ulak Island48 km
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34.2 km²▲ 566 m
Major islands
Ulak Island
31.3 km²▲ 164 m
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13.7 km²▲ 92 m
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Ogliuga Island
9.7 km²▲ 19 m
Minor islands
Skagul Island
4.4 km²▲ 25 m
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2.3 km²▲ 71 m
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1.5 km²▲ 55 m
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0.29 km²▲ 39 m
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716 km²▲ 1,196 m
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508 km²▲ 1,804 m
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886 km²▲ 898 m
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Adak Island
716 km²▲ 1,196 m
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Tanaga Island
508 km²▲ 1,804 m
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Minor islands

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Photographs

View of Gareloi Island in the Aleutian Islands from the west.
Gareloi Island, Aleutian Islands

Gareloi Volcano, elevation 1573 m, in the westeren Aleutian Islands, Alaska. Levied lava flows from a 1980s eruption drape the south flank of the southern summit crater. The white zone on the crater headwall is an extensive fumarole field.
Sources
Facts
Photographs
- Gareloi 01. Michelle L. Coombs, USGS AVO / Public domain
- Gareloi-Island. NASA / Public domain
- Gareloi. USGS - McGimsey R.G. / Public domain