World Library  
Flag as Inappropriate
Email this Article

Lituya Bay

Article Id: WHEBN0000496455
Reproduction Date:

Title: Lituya Bay  
Author: World Heritage Encyclopedia
Language: English
Subject: Megatsunami, 1958 Lituya Bay megatsunami, Lituya Glacier, MV Lituya, Gulf of Alaska
Collection: Bays of Alaska, Landforms of Hoonah–angoon Census Area, Alaska
Publisher: World Heritage Encyclopedia

Lituya Bay

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.
Location North Pacific Ocean
River sources Lituya Glacier
Cascade Glacier
Crillion Glacier
Basin countries United States
Max. length 14.5 km (9.01 mi)
Max. width 3.2 km (1.99 mi)

Lituya Bay (; 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 1
  • 1958 megatsunami 2
  • See also 3
  • References 4
  • External links 5


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 four recorded tsunamis, in 1854, 1899, 1936, and 1958.[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]

See also


  • Guinness World Records Ltd. (2005). Guinness World Records 2006: 84.
  • Mega-tsunami: Wave of Destruction. Horizon. BBC Two 12 October 2000
  1. ^  . 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". Retrieved 2013-12-03. 
  4. ^ Casey, Susan. The Wave. Doubleday, 2010, pp. 153-158

External links

  • E. W. Eickelberg, Lituya Bay, Gulf of Alaska. U.S. Coast and Geodetic Survey FIELD ENGINEERS BULLETIN no. 10, December 1936
  • World's Biggest Tsunami: The largest recorded tsunami with a wave 1,720 feet (520 m) tall in Lituya Bay, Alaska
  • Photos of damage from the 1958 tsunami

Eyewitness reports of the tsunami

  • History of Lituya Bay, Tsunami and Laperouse (in French)
  • Giant Waves in Lituya Bay, Alaska; USGS PP 354-C
This article was sourced from Creative Commons Attribution-ShareAlike License; additional terms may apply. World Heritage Encyclopedia content is assembled from numerous content providers, Open Access Publishing, and in compliance with The Fair Access to Science and Technology Research Act (FASTR), Wikimedia Foundation, Inc., Public Library of Science, The Encyclopedia of Life, Open Book Publishers (OBP), PubMed, U.S. National Library of Medicine, National Center for Biotechnology Information, U.S. National Library of Medicine, National Institutes of Health (NIH), U.S. Department of Health & Human Services, and, which sources content from all federal, state, local, tribal, and territorial government publication portals (.gov, .mil, .edu). Funding for and content contributors is made possible from the U.S. Congress, E-Government Act of 2002.
Crowd sourced content that is contributed to World Heritage Encyclopedia is peer reviewed and edited by our editorial staff to ensure quality scholarly research articles.
By using this site, you agree to the Terms of Use and Privacy Policy. World Heritage Encyclopedia™ is a registered trademark of the World Public Library Association, a non-profit organization.

Copyright © World Library Foundation. All rights reserved. eBooks from Project Gutenberg are sponsored by the World Library Foundation,
a 501c(4) Member's Support Non-Profit Organization, and is NOT affiliated with any governmental agency or department.