ⓘ Mount Amukta

                                     

ⓘ Mount Amukta

The undissected stratovolcano of Amukta volcano makes up most of nearly circular, 7.7-km-wide Amukta Island. 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 reports the presence of a cinder cone near the northeastern shore of the island.

                                     

1. 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 lists activity at Amukhton in 1770, presumably the same volcano; conversely, Dall 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. 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.