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Lituya Bay

Coordinates: 58°38′13″N 137°34′23″W / 58.63694°N 137.57306°W / 58.63694; -137.57306 (Hudson Bay)
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Lituya Bay
Oblique aerial photograph of Lituya Bay in the Summer of 1958. Damage from the 1958 megatsunami appears as the lighter-colored areas on the shores where trees have been stripped away.
LocationNorth Pacific Ocean
Coordinates58°38′13″N 137°34′23″W / 58.63694°N 137.57306°W / 58.63694; -137.57306 (Hudson Bay)
River sourcesLituya Glacier
Cascade Glacier
Crillion Glacier
Basin countriesUnited States
Max. length14.5 km (9.01 mi)
Max. width3.2 km (1.99 mi)

Lituya Bay (/l[invalid input: 'ɪ-']ˈtjjə/; Tlingit: Ltu.aa,[1] meaning "No Lake Within") is a fjord located on the coast of the Southeast part of the U.S. state of Alaska. It is 14.5 km (9.0 mi) long and 3.2 km (2.0 mi) wide at its widest point. The bay was noted in 1786 by Jean-François de La Pérouse, who named it Port des Français. Twenty-one of his men perished in the tidal current in the bay.

Description

The smaller Cascade Glacier and Crillon Glacier 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.[2]

The bay is known for its high tides, which have a range of approximately 3 m (9.8 ft). Tidal currents in the entrance reach 9.4 km/h (5.1 kn). The entrance is considered dangerous to navigation, especially when the tidal currents are running, but the interior of the bay provides good protection to anchored ships.[2]

Lituya Bay is also famous for hosting four recorded tsunamis over 100 feet: in 1854 (395 feet high), 1899 (200 feet), 1936 (490 feet), and 1958 (1720 feet).[3][4]

1958 megatsunami

Spruce tree shattered by the force of the water.

The same topography that leads to the heavy tidal currents also created the highest wave from a tsunami in recorded history. On July 9, 1958, an earthquake caused a landslide in the Gilbert Inlet at the head of the bay, generating a massive megatsunami measuring between 100 ft (30 m) and 300 ft (91 m). The wave possessed sufficient power to snap off all the trees up to 1,720 feet (520 m) high on the slope directly opposite the landslide. There were three fishing boats anchored near the entrance of Lituya Bay on the day the giant wave occurred. One boat sank and the two people on board were killed. The other two boats were able to ride the waves. Among the survivors were William A. Swanson and Howard G. Ulrich, who provided accounts of what they observed. Based on Swanson's description of the length of time it took the wave to reach his boat after overtopping Cenotaph Island near the bay's entrance, the wave may have been traveling 120 mph. When it reached the open sea, however, it dissipated quickly. This incident was the first direct evidence and eyewitness report of the existence of megatsunamis.[3]

The initial wave and the subsequent up to 20 feet high secondary waves along the main body of the bay were caused primarily by an enormous subaerial rockfall into Gilbert Inlet at the head of Lituya Bay, triggered by dynamic earthquake ground motions. The large mass of rock and ice, acting as a monolith, impacted the bottom of the inlet with great force. The impact created a crater which displaced and folded recent and Tertiary deposits and sedimentary layers. The displaced water and the folding of sediments broke and uplifted 1,300 feet (400 m) of ice along the entire front of the Lituya Glacier. Also, the impact resulted in water-splashing action that reached the 1,720-foot (520 m) elevation on the other side of the narrow inlet.

Mathematical modeling studies conducted by Dr. Charles Mader, support this mechanism as there is a sufficient volume and an adequately deep layer of water in the Lituya Bay inlet to account for the giant wave runup and subsequent inundation[citation needed]. Because of the similarity to asteroid generated tsunami waves, full Navier-Stokes modeling, as suggested by Dr. Mader, could further verify this impulsive rockfall mechanism[citation needed].

See also

References

  • Guinness World Records Ltd. (2005). Guinness World Records 2006: 84.
  • Mega-tsunami: Wave of Destruction. Horizon. BBC Two 12 October 2000
  1. ^ Teben'kov, M.D.; Translated by R.A. Pierce (1981) [1852], Atlas of the Northwest Coasts of America: From Bering Strait to Cape Corrientes and the Aleutian Islands with Several Sheets on the Northeast Coast of Asia, Kingston, Ontario: Limestone Press, p. 27, ISBN 0-919642-55-1 {{citation}}: Cite has empty unknown parameters: |chapterurl= and |month= (help). Spelled L'tua in translation of Tebenkov's log.
  2. ^ a b United States Coast Pilot 9. p. 130.
  3. ^ a b Don J. Miller, Giant Waves in Lituya Bay, Alaska
  4. ^ Casey, Susan. The Wave. Doubleday, 2010, pp. 153-158