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After the earthquake it was observed that a subglacial lake, located northwest of the bend in the Lituya Glacier at the head of Lituya Bay, had dropped 100 ft (30 m). This proposed another possible cause to the production of the 100 ft (30 m) wave which caused destruction as high as 1,720 ft (520 m) above the surface of the bay as its momentum ...
On July 9, 1958, an earthquake along the Fairweather Fault loosened about 40 million cubic yards of rock above Lituya Bay. The impact of this enormous volume of rock falling from approximately 3,300 feet (1,000 m) produced locally the largest recorded tsunami (an estimated 1,700 feet (520 m) high) and devastated the entire bay. [3]
Cenotaph Island in Lituya Bay. The smaller Cascade and Crillon glaciers and the larger Lituya Glacier all spill into Lituya Bay, which is a part of Glacier Bay National Park and Preserve. Cenotaph Island is located roughly in the middle of the bay. The entrance of the bay is approximately 500 m (0.31 mi) wide, with a narrow navigable channel. [3]
Lituya Glacier is a tidewater glacier in the U.S. state of Alaska. Located at 58°43′25″N 137°29′33″W / 58.72361°N 137.49250°W / 58.72361; -137.49250 inside Glacier Bay National Park and Preserve , its source is in the Fairweather Range and it feeds into Lituya Bay on the gulf coast of Southeast Alaska
The megatsunami was the largest known marine tsunami worldwide since the Lituya Bay wave; [10] although the Taan Fiord landslide was larger than the one at Lituya Bay, the Lituya Bay wave was larger than the one in Taan Fiord because the landslide in Taan Fiord did not fall from as great a height and landed in shallower water. [4]
At least 20 aftershocks follows, with another major earthquake – measuring at least 7.5 magnitude – striking central Turkey hours later Map of Turkey shows where massive 7.8 magnitude ...
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It struck north of the city of Adiyama at around 11.30am, just over 24 hours after a 7.8 magnitude tremor wreaked havoc in the worst earthquake to hit the country in more than 20 years.