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Icy Bay (
Tlingit The Tlingit ( or ; also spelled Tlinkit) are indigenous peoples of the Pacific Northwest Coast of North America. Their language is the Tlingit language (natively , pronounced ),
: ''Lig̲aasi Áa'') is a body of water in the borough of Yakutat,
Alaska Alaska ( ; russian: Аляска, Alyaska; ale, Alax̂sxax̂; ; ems, Alas'kaaq; Yup'ik: ''Alaskaq''; tli, Anáaski) is a state located in the Western United States on the northwest extremity of North America. A semi-exclave of the U.S., ...
, formed in the last 100 years by the rapid retreat of the
Guyot In marine geology, a guyot (pronounced ), also known as a tablemount, is an isolated underwater volcanic mountain ( seamount) with a flat top more than below the surface of the sea. The diameters of these flat summits can exceed .Yahtse, and
Tyndall Tyndall (the original spelling, also Tyndale, "Tindol", Tyndal, Tindoll, Tindall, Tindal, Tindale, Tindle, Tindell, Tindill, and Tindel) is the name of an English family taken from the land they held as tenants in chief of the Kings of Engla ...
Glacier A glacier (; ) is a persistent body of dense ice that is constantly moving under its own weight. A glacier forms where the accumulation of snow exceeds its Ablation#Glaciology, ablation over many years, often Century, centuries. It acquires dis ...
s. It is part of the Wrangell-Saint Elias Wilderness. At the beginning of the 20th century, the bay entrance was permanently blocked by a giant
tidewater glacier The tidewater glacier cycle is the typically centuries-long behavior of tidewater glaciers that consists of recurring periods of advance alternating with rapid retreat and punctuated by periods of stability. During portions of its cycle, a tidewate ...
face that calved
iceberg An iceberg is a piece of freshwater ice more than 15 m long that has broken off a glacier or an ice shelf and is floating freely in open (salt) water. Smaller chunks of floating glacially-derived ice are called "growlers" or "bergy bits". The ...
s directly into the
Gulf of Alaska The Gulf of Alaska (Tlingit: ''Yéil T'ooch’'') is an arm of the Pacific Ocean defined by the curve of the southern coast of Alaska, stretching from the Alaska Peninsula and Kodiak Island in the west to the Alexander Archipelago in the east, ...
. A century-long
glacial retreat The retreat of glaciers since 1850 affects the availability of fresh water for irrigation and domestic use, mountain recreation, animals and plants that depend on glacier-melt, and, in the longer term, the level of the oceans. Deglaciation occu ...
has opened a multi-armed bay more than long. Icy Bay is a popular destination for
sea kayak A sea kayak or touring kayak is a kayak developed for the sport of paddling on open waters of lakes, bays, and the ocean. Sea kayaks are seaworthy small boats with a covered deck and the ability to incorporate a spray deck. They trade off the man ...
ers, and is reachable by
bush plane A bush airplane is a general aviation aircraft used to provide both scheduled and unscheduled passenger and flight services to remote, undeveloped areas, such as the Canadian north or bush, Alaskan tundra, the African bush, or savanna, Amazon ra ...
from Yakutat,
Alaska Alaska ( ; russian: Аляска, Alyaska; ale, Alax̂sxax̂; ; ems, Alas'kaaq; Yup'ik: ''Alaskaq''; tli, Anáaski) is a state located in the Western United States on the northwest extremity of North America. A semi-exclave of the U.S., ...
.


2015 landslide and megatsunami

At 8:19 p.m.
Alaska Daylight Time The Alaska Time Zone observes standard time by subtracting nine hours from Coordinated Universal Time ( UTC−09:00). During daylight saving time its time offset is eight hours ( UTC−08:00). The clock time in this zone is based on mean solar ...
on 17 October 2015, the side of a mountain collapsed on the western end of the head of Taan Fiord, a finger of Icy Bay formed by the retreat of Tyndall Glacier. The resulting
landslide Landslides, also known as landslips, are several forms of mass wasting that may include a wide range of ground movements, such as rockfalls, deep-seated grade (slope), slope failures, mudflows, and debris flows. Landslides occur in a variety of ...
generated a
megatsunami A megatsunami is a very large wave created by a large, sudden displacement of material into a body of water. Megatsunamis have quite different features from ordinary tsunamis. Ordinary tsunamis are caused by underwater tectonic activity (movemen ...
in Taan Fjord. The area is uninhabited and no one was visiting it at the time, and the event went undetected for several hours until its signature was noted as a 4.9
magnitude Magnitude may refer to: Mathematics *Euclidean vector, a quantity defined by both its magnitude and its direction *Magnitude (mathematics), the relative size of an object *Norm (mathematics), a term for the size or length of a vector *Order of ...
event on
seismogram A seismogram is a graph output by a seismograph. It is a record of the ground motion at a measuring station as a function of time. Seismograms typically record motions in three cartesian axes (x, y, and z), with the z axis perpendicular to the ...
s at
Columbia University Columbia University (also known as Columbia, and officially as Columbia University in the City of New York) is a private research university in New York City. Established in 1754 as King's College on the grounds of Trinity Church in Manhatt ...
in
New York City New York, often called New York City or NYC, is the List of United States cities by population, most populous city in the United States. With a 2020 population of 8,804,190 distributed over , New York City is also the L ...
. Scientists visited the
fjord In physical geography, a fjord or fiord () is a long, narrow inlet with steep sides or cliffs, created by a glacier. Fjords exist on the coasts of Alaska, Antarctica, British Columbia, Chile, Denmark, Germany, Greenland, the Faroe Islands, Ice ...
in the spring and summer of 2016 to gather data on the event. Their studies revealed that the landslide consisted of about of rock with a volume of and lasted 60 to 100 seconds, reaching a maximum speed of . Some of the landslide came to rest on the foot of Tyndall Glacier, but about of rock with a volume of about entered the fjord, where it dislodged another of material from the bottom of the fjord. Some of the landslide's debris traversed the deep water at the head of the fjord and then climbed to reach a final resting place at an elevation of about on the opposite shore. Altogether, the landslide debris covered . The landslide generated a megatsunami with an initial height of about that struck the opposite shore of the fjord, with a run-up height (i.e., the maximum height on land the megatsunami reached as it ran up the shore) of . At a speed of up to , the megatsunami then continued down the entire length of the fjord – about – and into Icy Bay. In the uppermost of the fjord, run-up exceeded along the shore, and run-up heights in the upper part of the fjord otherwise varied between on the southeast shore and on the northwest side. In the middle part of the fjord, run-up heights varied greatly, dropping to as low as in some places but reaching in others. In the lower fjord, run-up heights on both sides were , increasing to at the entrance to the fjord. Along its path, the wave inundated an overall area of and left a trim line at its run-up height, stripping away all vegetation, including
alder Alders are trees comprising the genus ''Alnus'' in the birch family Betulaceae. The genus comprises about 35 species of monoecious trees and shrubs, a few reaching a large size, distributed throughout the north temperate zone with a few sp ...
forests, and leaving behind barren beaches that reached elevations of . The wave may have been about tall when it entered Icy Bay itself about 12 minutes after the landslide, and it inundated the bay's coastline with run-up levels of as much as in some places, although the run-up diminished to below the normal high-tide level in Icy Bay at distances greater than from the mouth of Taan Fiord. When it reached the nearest
tide gauge A tide gauge is a device for measuring the change in sea level relative to a vertical datum. It its also known as mareograph, marigraph, sea-level recorder and limnimeter. When applied to freshwater continental water bodies, the instrument may ...
, located to the southeast of the landslide near Yakutat, Alaska, the wave had diminished to a height of . The Taan Fiord event bore a strong similarity to the July 1958 landslide and megatsunami in Alaska's
Lituya Bay Lituya Bay (; Tlingit: ''Ltu.aa'',. Spelled L'tua in translation of Tebenkov's log. meaning 'lake within the point') is a fjord located on the coast of the south-east part of the U.S. state of Alaska. It is long and wide at its widest point. ...
. The Taan Fiord landslide was the largest recorded in
North America North America is a continent in the Northern Hemisphere and almost entirely within the Western Hemisphere. It is bordered to the north by the Arctic Ocean, to the east by the Atlantic Ocean, to the southeast by South America and the Car ...
since the eruption of Mount St. Helens in May 1980, and the largest non-volcanic landslide in North America ever recorded. The megatsunami was the largest known marine tsunami worldwide since the Lituya Bay wave; 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. The Taan Fiord wave also was the fourth-largest megatsunami of any type over the previous 100 years, with the fourth-highest run-up ever recorded anywhere in the world. Scientists assessed the landslide occurred because the retreat of Tyndall Glacier between 1961 and 1991 had left the mountainside unsupported by what had once been about of glacial ice. They also noted that heavy rains may have weakened the mountainside further, and that seismic waves from a 4.1-magnitude
earthquake An earthquake (also known as a quake, tremor or temblor) is the shaking of the surface of the Earth resulting from a sudden release of energy in the Earth's lithosphere that creates seismic waves. Earthquakes can range in intensity, from ...
centered about away arrived two minutes before the landside began and may also have contributed to the event.


References

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External links


Sea Kayaking in Icy Bay
Fjords of Alaska Bodies of water of Yakutat City and Borough, Alaska Tourist attractions in Yakutat City and Borough, Alaska Megatsunamis