The 1983, Sea of Japan earthquake or often referred to as the Nihonkai-Chubu earthquake occurred on May 26, at 11:59 JST about 100 km west of the coast of Noshiro in Akita Prefecture, Japan. Many Japanese mobile phones get alerts when an earthquake is just about to happen. The Mid-Sea of Japan Earthquake of May 16, 1983 and Numerical Analysis of the Tsunami Masanori Hamada and Miehihiro Kitahara Faculty of Marine Science and Technology, Tokai University, Shimizu, Shizuoka 424, Japan Katsuya Nakagawa and Tomoaki Ando Fuyo Data Processing and Systems Development, Inc., 4-7-14 Akasaka, Tokyo 107, Japan To clarify the general characteristics of the 1983 Mid-Sea … The focal mechanisms of the 1940, 1964, and 1983 earthquakes are all consistent with the Sea of Japan thrusting beneath Honshu and Hokkaido. This gives you a few precious seconds to turn off gas, get under a … The damage caused by subsoil liquefaction as well as the tsunami data such as wave height, run-up height on land, arrival time, etc., were examined. Out of the 107 fatalities, all but four were killed by the resulting tsunami, which struck communities along the coast, especially Aomori and Akita Prefectures and the east coast of Noto Peninsula. To clarify the general characteristics of the 1983 Mid-Sea of Japan Earthquake and its induced tsunami, site investigation was carried out. In Japan, the shindo scale is commonly used to measure earthquakes by seismic intensity instead of magnitude. The earthquake had a magnitude of 7.7 on the Richter scale, as measured by the Japan Meteorological Agency (JMA). This is similar to the Modified Mercalli intensity scale used in the United States or the Liedu scale used in China, meaning that the scale measures the intensity of an earthquake at a given location instead of measuring the energy an earthquake … On May 26, 1983 at 11:59:57 local time, a magnitude-7.7 earthquake occurred in the Sea of Japan, about 100 km west of the coast of Noshiro in Akita Prefecture, Japan. Seismic reflection surveys and sediment cores reveal that mass-failure deposits, which are distributed on the continental … 1983 Sea of Japan earthquake (Wikipedia) More info; Keitai notification. A few seconds after noon on May 26, 1983, a major earthquake occurred in the Japan Sea about 100 km off the coast of Akita Prefecture, which is located in the northeast Honshu, Japan. This basin is semi-enclosed with no active conduits for the entrance of coarse detrital sediments. Earthquake measurement. 1983 earthquakes (Figure 1). Moderate mag. 5.0 earthquake - Eastern Sea of Japan on Friday, 18 March 1983 at 00:18 (GMT) 1983 Sea of Japan earthquake. On May 26, 1983 at 11:59:57 local time, a magnitude-7.7 earthquake occurred in the Sea of Japan, about 100 km west of the coast of Noshiro in Akita Prefecture, Japan. earthquakes is high. Both mass failure deposits and turbidites are widely distributed in the epicentral area of the 1983 earthquake (Mw 7.9) in the eastern margin of the Japan Sea. Sinc e ther is no deep Wa dati-Benioff zone associated with the under thrusting of the Sea of Japan, one simple interpretation of the tectonics is that a new The Event • May 26, 1983 at 12:00 pm • 7.7 magnitude earthquake occurs of the west coast on Honshu (40.46 N, 139.10 E) • Earthquake a direct result of reverse faulting • Abruptly changed bathymetry in Sea of Japan which generated destructive Tsunami along the coasts of S. Korea, Japan, and USSR.
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