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The undissected stratovolcano of Amukta volcano makes up most of nearly circular, 7.7-km-wide Amukta Island (Amuux̂tax̂[1] in Aleut). It is the westernmost of the Islands of Four Mountains chain. The cone, about 5.8 km in basal diameter and topped by a 0.4 km wide summit crater, appears on synthetic-aperture radar imagery to be built upon a 300+ meter high, east-west trending arcuate ridge. Extensions of that ridge on the southwest and east sides of the island indicate an older caldera approximately 6 km in diameter and open to the sea on the south side. No hot springs or fumaroles have been reported from Amukta. Sekora (1973, p. 29) reports the presence of a cinder cone near the northeastern shore of the island.

Mount Amukta
Mt. Amukta, June 1972
Highest point
Elevation3,497 ft (1,066 m)
Prominence1,066 m (3,497 ft) 
Coordinates52°30′N 171°15′W
Geography
LocationAmukta Island, Alaska, U.S.
Parent rangeAleutian Range
Topo mapUSGS Amukta C-4
Geology
Mountain typeStratovolcano
Volcanic arc/beltAleutian Arc
Last eruptionMarch 1997

Volcanic activity


Well documented reports of historical Amukta volcanism are sparse; activity was noted from 1786 to 1791, and again in 1876 (Coats, 1950). Petroff (1884, citing Grewingk, 1850) lists activity at Amukhton in 1770, presumably the same volcano; conversely, Dall (1870, citing Grewingk, 1850) describes a cessation of activity at Amukta in 1770. On February 13, 1963 an eruption occurred involving the central crater and one or more parasitic vents; both ash and lava were produced (Anchorage Times, February 11, 1963; Decker, 1967). Persistent low clouds obscured the exact source of the lava, but the flow was seen to extend from the west side of the cone southwest into the sea at Traders Cove (Bulletin of Volcanic Eruptions, 1963).

In late August and early September, 1987, a commercial pilot observed a 10.5 km high eruption plume rising through cloud cover near Amukta Island. On September 4, another pilot observed a small dark ash plume issuing from the summit of Amukta (Smithsonian Institution, 1987). On Sept. 18, yet another pilot reported a 300m-high ash plume.

In early July 1996, a passing ship reported a 1-km high plume of "ash and smoke" (Neal and McGimsey, 1997). On August 28 Mt. Cleveland, 100 km to the northeast, was also active and winds were blowing towards Amukta.

Map of Amutka Island.
Map of Amutka Island.

Composition


Igneous rocks produced by this volcano range from granite to monzonite, however the most common rock found in/around Mt. Amukta is basalt.


See also



Sources


by T.P. Miller, R.G. McGimsey, D.H. Richter, J.R. Riehle, C.J. Nye, M.E. Yount, and J.A. Dumoulin. U.S. GEOLOGICAL SURVEY Open-File Report 98-582, 104 pages, 102 figures. Alaska Volcano Observatory, Alaska, 1998.

  1. Bergsland, K. (1994). Aleut Dictionary. Fairbanks: Alaska Native Language Center.

На других языках


[de] Amukta Island

Die Insel Amukta liegt in den zentralen Aleuten, südwestlich der Insel Chagulak, und ist die westlichste der Islands of Four Mountains. Sie wird von dem symmetrischen Schichtvulkan Amukta mit einem Durchmesser von 7,7 Kilometern gebildet. Der Vulkan besitzt einen Krater mit einem Durchmesser von 400 Metern. An der Nordwestküste befindet sich ein Schlackenkegel.
- [en] Mount Amukta

[it] Vulcano Amukta

Il Vulcano Amukta è uno stratovulcano integro che costituisce quasi per intero l'omonima isola, nelle Aleutine.

[ru] Амукта (вулкан)

Амукта[2] (англ. Mount Amukta) — активный вулкан, расположенный на одноимённом острове, состоящий в архипелаге Алеутские острова, входящих в состав Штата Аляска, США. Амукта — стратовулкан, высотой 1066 метров. Последняя бурная активность проявлялась в 1997 году. Является самым западным вулканом в составе Четырёхсопочных островов. Главный конус вулкана расположен на северо-западе острова. Вулканические извержения происходили как из главного купола, так и из вулканических разломов ниже конуса вулкана. В период затишья вершина вулкана покрывается снегом.



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