VIDEO MAPS Pictures Aftershock The main shock was followed by an earthquake of magnitude 7.6.

Five Pictures Plate boundary Extra Info Subduction of the Pacific Plate beneath the North American Plate ---- Alaska-Aleutian Mega thrust On Adak Island, cracks occurred in prefabricated wood buildings; on Shemya Island, cracks were observed in an asphalt runway. Earthquake frequency of occurrence in time and magnitude are given. Studies of earthquake aftershocks as a function of space, time, and rate of energy release (magnitude) afford new evidence of earth structure. A magnitude 7.9 earthquake occurred on Monday, June 23 at 12:53 pm AKDT (20:53 UTC) in the Rat Islands region (large red star on the map). Journal of Geophysical Research: Solid Earth. The 1965 Rat Islands earthquake occurred at 05:01 UTC, on 4 February (19:01, 3 February local time). The sharp boundary conditions of the epicenter locations suggest block faulting about the Rat Islands as a subsystem of the Aleutian Islands arc structure. The rupture process and tectonic implications of the great 1964 Prince William Sound earthquake. Magnitude Range ≥ 4.0 ANSS Comcat ; Tectonic Summary. Plate Boundary Between the Pacific and North American Crustal Plates. The earthquake was associated with a 600 km long rupture along the plate boundary, based on the distribution of aftershocks. Nearly 2 months later, that triggered a tsunami. The November 17, 2003, M 7.8 Rat Islands earthquake occurred as the result of shallow thrust faulting on or near the plate interface between the overriding North America plate and the subducting Pacific plate, along the subduction zone defining the Aleutian Arc of Alaska. 1906-08-17 00:11:10 UTC 8.3 magnitude, 110 km depth Rat Islands, Aleutian Islands 8.3 magnitude earthquake 1906-08-17 00:11:10 UTC at 00:11 August 17, 1906 UTC 2020-09-17 03:29:26 UTC 4.2 magnitude, 153 km depth Rat Islands, Aleutian Islands 4.2 magnitude earthquake 2020-09-17 03:29:26 UTC at 03:29 September 17, 2020 UTC The Rat Island earthquake of February 4, 1965 (origin time 05h 01m 21.8s, h = 40 km), is one of the largest earthquakes recorded in recent years. The 1965 Rat Islands earthquake share common features with the 1963 Kuril Islands earthquake and the 1964 Alaska earthquake.. Earthquake.
Shallow Subduction Zones: Seismicity, Mechanics and Seismic Potential. The earthquake had a moment magnitude of 8.8 and triggered a destructive tsunami that caused at least 500 casualties on the coast of Colombia. It occurred at a depth of 118 km (73 miles) and was located 25 km (15 miles) WNW of Amchitka, 325 km (203 miles) W of Adak and 334 km (209 miles) ESE of Shemya. The great Rat Islands underthrusting earthquake (M w = 8.7), of February 4, 1965, represents subduction of the Pacific plate beneath the North American plate along a 600‐km segment of the western end of the Aleutian Islands.Body wave inversion techniques are used to determine the spatial and temporal heterogeneities associated with the Rat Islands earthquake. The pattern of energy release suggest the presence of three asperities along the plate interface, each causing a pulse of moment release. This earthquake occurred at the Rat Island on February 4, 1965 just a year after the tragedy of the 1964 earthquake. 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