Physics:Megatsunami

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Short description: Very large wave created by a large, sudden displacement of material into a body of water
Diagram of the 1958 Lituya Bay megatsunami, which proved the existence of megatsunamis

A megatsunami is a very large wave created by a large, sudden displacement of material into a body of water.

Megatsunamis have different features from ordinary tsunamis. Ordinary tsunamis are caused by underwater tectonic activity (movement of the earth's plates) and therefore occur along plate boundaries and as a result of earthquakes and the subsequent rise or fall in the sea floor that displaces a volume of water. Ordinary tsunamis exhibit shallow waves in the deep waters of the open ocean that increase dramatically in height upon approaching land to a maximum run-up height of around 30 metres (100 ft) in the cases of the most powerful earthquakes.[1] By contrast, megatsunamis occur when a large amount of material suddenly falls into water or anywhere near water (such as via a landslide, meteor impact, or volcanic eruption). They can have extremely large initial wave heights in the hundreds of metres, far beyond the height of any ordinary tsunami. These giant wave heights occur because the water is "splashed" upwards and outwards by the displacement.

Examples of modern megatsunamis include the one associated with the 1883 eruption of Krakatoa (volcanic eruption), the 1958 Lituya Bay megatsunami (a landslide which caused an initial wave of 524 metres (1,719 ft)), and the Vajont Dam landslide (caused by human activity destabilizing sides of valley). Prehistoric examples include the Storegga Slide (landslide), and the Chicxulub, Chesapeake Bay, and Eltanin meteor impacts.

Overview

A megatsunami is a tsunami with an initial wave amplitude (height) measured in many tens or hundreds of metres. A megatsunami is a separate class of event from an ordinary tsunami and is caused by different physical mechanisms.

Normal tsunamis result from displacement of the sea floor due to plate tectonics. Powerful earthquakes may cause the sea floor to displace vertically on the order of tens of metres, which in turn displaces the water column above and leads to the formation of a tsunami. Ordinary tsunamis have a small wave height offshore and generally pass unnoticed at sea, forming only a slight swell on the order of 30 cm (12 in) above the normal sea surface. In deep water it is possible that a tsunami could pass beneath a ship without the crew of the vessel noticing. As it approaches land, the wave height of an ordinary tsunami increases dramatically as the sea floor slopes upward and the base of the wave pushes the water column above it upwards. Ordinary tsunamis, even those associated with the most powerful strike-slip earthquakes, typically do not reach heights in excess of 30 m (100 ft).[2][3]

By contrast, megatsunamis are caused by landslides and other impact events that displace large volumes of water, resulting in waves that may exceed the height of an ordinary tsunami by tens or even hundreds of metres. Underwater earthquakes or volcanic eruptions do not normally generate megatsunamis, but landslides next to bodies of water resulting from earthquakes or volcanic eruptions can, since they cause a much larger amount of water displacement. If the landslide or impact occurs in a limited body of water, as happened at the Vajont Dam (1963) and in Lituya Bay (1958) then the water may be unable to disperse and one or more exceedingly large waves may result.[4]

Determining a height range typical of megatsunamis is a complex and scientifically debated topic. This complexity is increased due to the fact that two different heights are often reported for tsunamis – the height of the wave itself in open water, and the height to which it surges when it encounters land. Depending upon the locale, this second or so-called "run-up height" can be several times larger than the wave's height just before reaching shore.[5] While there is currently no minimum or average height classification for megatsunamis that is broadly accepted by the scientific community, the limited number of observed megatsunami events in recent history have all had run-up heights that exceeded 100 metres (300 ft). The megatsunami in Spirit Lake, Washington, USA that was caused by the 1980 eruption of Mount St. Helens reached 260 metres (853 ft), while the tallest megatsunami ever recorded (Lituya Bay in 1958) reached a run-up height of 520 metres (1,720 ft).[6] It is also possible that much larger megatsunamis occurred in prehistory; researchers analyzing the geological structures left behind by prehistoric asteroid impacts have suggested that these events could have resulted in megatsunamis that exceeded 1,500 metres (4,900 ft) in height.[7]

Recognition of the concept of megatsunami

Before the 1950s, scientists had theorized that tsunamis orders of magnitude larger than those observed with earthquakes could have occurred as a result of ancient geological processes, but no concrete evidence of the existence of these "monster waves" had yet been gathered. Geologists searching for oil in Alaska in 1953 observed that in Lituya Bay, mature tree growth did not extend to the shoreline as it did in many other bays in the region. Rather, there was a band of younger trees closer to the shore. Forestry workers, glaciologists, and geographers call the boundary between these bands a trim line. Trees just above the trim line showed severe scarring on their seaward side, while those from below the trim line did not. This indicated that a large force had impacted all of the elder trees above the trim line, and presumably had killed off all the trees below it. Based on this evidence, the scientists hypothesized that there had been an unusually large wave or waves in the deep inlet. Because this is a recently deglaciated fjord with steep slopes and crossed by a major fault (the Fairweather Fault), one possibility was that this wave was a landslide-generated tsunami.[8]

On July 9, 1958, a 7.8 title|Moment mag. scale|Mw|dotted=no}} strike-slip earthquake in southeast Alaska caused 80,000,000 metric tons (90,000,000 short tons) of rock and ice to drop into the deep water at the head of Lituya Bay. The block fell almost vertically and hit the water with sufficient force to create a wave that surged up the opposite side of the head of the bay to a height of 520 metres (1,710 feet), and was still many tens of metres high further down the bay when it carried eyewitnesses Howard Ulrich and his son Howard Jr. over the trees in their fishing boat. They were washed back into the bay and both survived.[8]

Analysis of mechanism

The mechanism giving rise to megatsunamis was analysed for the Lituya Bay event in a study presented at the Tsunami Society in 1999;[9] this model was considerably developed and modified by a second study in 2010.

Although the earthquake which caused the megatsunami was considered very energetic, it was determined that it could not have been the sole contributor based on the measured height of the wave. Neither water drainage from a lake, nor a landslide, nor the force of the earthquake itself were sufficient to create a megatsunami of the size observed, although all of these may have been contributing factors.

Instead, the megatsunami was caused by a combination of events in quick succession. The primary event occurred in the form of a large and sudden impulsive impact when about 40 million cubic yards of rock several hundred metres above the bay was fractured by the earthquake, and fell "practically as a monolithic unit" down the almost-vertical slope and into the bay.[9] The rockfall also caused air to be "dragged along" due to viscosity effects, which added to the volume of displacement, and further impacted the sediment on the floor of the bay, creating a large crater. The study concluded that:

The giant wave runup of 1,720 feet (524 m) at the head of the Bay and the subsequent huge wave along the main body of Lituya Bay which occurred on July 9, 1958, were caused primarily by an enormous subaerial rockfall into Gilbert Inlet at the head of Lituya Bay, triggered by dynamic earthquake ground motions along the Fairweather Fault.

The large monolithic mass of rock struck the sediments at bottom of Gilbert Inlet at the head of the bay with great force. The impact created a large crater and displaced and folded recent and Tertiary deposits and sedimentary layers to an unknown depth. The displaced water and the displacement and folding of the sediments broke and uplifted 1,300 feet of ice along the entire front face of the Lituya Glacier at the north end of Gilbert Inlet. Also, the impact and the sediment displacement by the rockfall resulted in an air bubble and in water splashing action that reached the 1,720-foot (524 m) elevation on the other side of the head of Gilbert Inlet. The same rockfall impact, in combination with the strong ground movements, the net vertical crustal uplift of about 3.5 feet, and an overall tilting seaward of the entire crustal block on which Lituya Bay was situated, generated the giant solitary gravity wave which swept the main body of the bay.

This was the most likely scenario of the event – the "PC model" that was adopted for subsequent mathematical modeling studies with source dimensions and parameters provided as input. Subsequent mathematical modeling at the Los Alamos National Laboratory (Mader, 1999, Mader & Gittings, 2002) supported the proposed mechanism and indicated that there was indeed sufficient volume of water and an adequately deep layer of sediments in the Lituya Bay inlet to account for the giant wave runup and the subsequent inundation. The modeling reproduced the documented physical observations of runup.

A 2010 model examined the amount of infill on the floor of the bay, which was many times larger than that of the rockfall alone, and also the energy and height of the waves, and the accounts given by eyewitnesses, concluded that there had been a "dual slide" involving a rockfall, which also triggered a release of 5 to 10 times its volume of sediment trapped by the adjacent Lituya Glacier, as an almost immediate and many times larger second slide, a ratio comparable with other events where this "dual slide" effect is known to have happened.[10]

Examples

Prehistoric

  • An astronomical object between 37 and 58 kilometres (23 and 36 mi) wide traveling at 20 kilometres (12.4 mi) per second struck the Earth 3.26 billion years ago east of what is now Johannesburg, South Africa , near South Africa's border with Swaziland, in what was then an Archean ocean that covered most of the planet, creating a crater about 500 kilometres (310 mi) wide. The impact generated a megastunami that probably extended to a depth of thousands of meters beneath the surface of the ocean and rose to the height of a skyscraper when it reached shorelines.[11][12][13]
  • The asteroid linked to the extinction of dinosaurs, which created the Chicxulub crater in the Yucatán Peninsula approximately 66 million years ago, would have caused a megatsunami over 100 metres (330 ft) tall. The height of the tsunami was limited due to relatively shallow sea in the area of the impact; had the asteroid struck in the deep sea the megatsunami would have been 4.6 kilometres (2.9 mi) tall. Among the mechanisms triggering megatsunamis, the direct impact, shockwaves, returning water in the crater with a new push outward and seismic waves with a magnitude up to ~11[14][15][16][17] A more recent simulation of the global effects of the Chicxulub megatsunami showed an initial wave height of 1.5 kilometres (0.9 mi), with later waves up to 100 metres (330 ft) in height in the Gulf of Mexico, and up to 14 metres (46 ft) in the North Atlantic and South Pacific; the discovery of mega-ripples in Louisiana via seismic imaging data, with average wavelengths of 600 metres (2,000 ft) and average wave heights of 16 metres (52 ft), looks like to confirm it.[18][19] David Shonting and Cathy Ezrailson propose an "Edgerton effect" mechanism generating the megatsunami, similar to a milk drop falling on water that triggers a crown-shape water column, with a comparable height to the Chicxulub impactor's, that means over 10–12 kilometres (6–7 mi) for the initial seawater forced outward by the explosion and blast waves; then, its collapse triggers megatsunamis changing their height according to the different water depth, raising up to 500 metres (1,600 ft).[20] Furthermore, the initial shock wave via impact triggered seismic waves producing giant landslides and slumping around the region (the largest known event deposits on Earth) with subsequently megatsunamis of various sizes,[21] and seiches of 10 to 100 metres (30 to 300 ft) in Tanis, 3,000 kilometres (1,900 mi) away, part of a vast inland sea at the time and directly triggered via seismic shaking by the impact within a few minutes.[22]
  • During the Messinian the coasts of northern Chile were likely struck by various megatsunamis.[23]
  • A megatsunami affected the coast of south–central Chile in the Pliocene as evidenced by the sedimentary record of Ranquil Formation.[24]
  • The Eltanin impact in the southeast Pacific Ocean 2.5 million years ago caused a megatsunami that was over 200 metres (660 ft) high in southern Chile and the Antarctic Peninsula; the wave swept across much of the Pacific Ocean.
  • The northern half of the East Molokai Volcano on Molokai in Hawaii suffered a catastrophic collapse about 1.5 million years ago, generating a megatsunami, and now lies as a debris field scattered northward across the ocean bottom,[25] while what remains on the island are the highest sea cliffs in the world.[26] The megatsunami may have reached a height of 610 metres (2,000 ft) near its origin and reached California and Mexico.[27]
  • The existence of large scattered boulders in only one of the four marine terraces of Herradura Bay south of the Chilean city of Coquimbo has been interpreted by Roland Paskoff as the result of a mega-tsunami that occurred in the Middle Pleistocene.[28]
  • In Hawaii, a megatsunami at least 400 metres (1,312 ft) in height deposited marine sediments at a modern-day elevation of 326 metres (1,070 ft) — 375 to 425 metres (1,230 to 1,394 ft) above sea level at the time the wave struck — on Lanai about 105,000 years ago. The tsunami also deposited such sediments at an elevation of 60 to 80 metres (197 to 262 ft) on Oahu, Molokai, Maui, and the island of Hawaii.[29]
  • The collapse of the ancestral Mount Amarelo on Fogo in the Cape Verde Islands about 73,000 years ago triggered a megatsunami which struck Santiago, 55 kilometres (34 mi; 30 nmi) away, with a height of at least 170 metres (558 ft) and a run-up height of over 270 metres (886 ft).[30]
  • A major collapse of the western edge of the Lake Tahoe basin, a landslide with a volume of 12.5 cubic kilometres (3.0 cu mi) which formed McKinney Bay between 21,000 and 12,000 years ago, generated megatsunamis/seiche waves with an initial height of probably about 100 m (330 ft) and caused the lake's water to slosh back and forth for days. Much of the water in the megatsunamis washed over the lake's outlet at what is now Tahoe City, California, and flooded down the Truckee River, carrying house-sized boulders as far downstream as the California-Nevada border at what is now Verdi, California.[31][32]
  • In the North Sea, the Storegga Slide caused a megatsunami approximately 8,200 years ago.[33] It is estimated to have completely flooded the remainder of Doggerland.[34]
  • Around 6370 BCE, a 25-cubic-kilometre (6 cu mi) landslide on the eastern slope of Mount Etna in Sicily into the Mediterranean Sea triggered a megatsunami in the Eastern Mediterranean with an initial wave height along the eastern coast of Sicily of 40 metres (131 ft). It struck the Neolithic village of Atlit Yam off the coast of Israel with a height of 2.5 metres (8 ft 2 in), prompting the village's abandonment.[35][36][37][38][39]
  • Around 5,650 B.C., a landslide in Greenland created a megatsunami with a run-up height on Alluttoq Island of 41 to 66 metres (135 to 217 ft).[40]
  • Around 5,350 B.C., a landslide in Greenland created a megatsunami with a run-up height on Alluttoq Island of 45 to 70 metres (148 to 230 ft).[40]

Historic

c. 2000 BC: Réunion

c. 1600 BC: Santorini

Main page: Earth:Minoan eruption
  • The Thera volcano erupted, the force of the eruption causing megatsunamis which affected the whole Aegean Sea and the eastern Mediterranean Sea.

Modern

1674: Ambon Island, Banda Sea

On February 17, 1674, between 19:30 and 20:00 local time, an earthquake struck the Maluku Islands. Ambon Island received run-up heights of 100 metres (328 ft), making the wave far too large to be caused by the quake itself. Instead, it was probably the result of an underwater landslide triggered by the earthquake. The quake and tsunami killed 2,347 people.[42]

1731: Storfjorden, Norway

At 10:00 p.m. on January 8, 1731, a landslide with a volume of possibly 6,000,000 cubic metres (7,800,000 cu yd) fell from the mountain Skafjell from a height of 500 metres (1,640 ft) into the Storfjorden opposite Stranda, Norway . The slide generated a megatsunami 30 metres (100 ft) in height that struck Stranda, flooding the area for 100 metres (330 ft) inland and destroying the church and all but two boathouses, as well as many boats. Damaging waves struck as far as way as Ørskog. The waves killed 17 people.[43]

1741: Oshima-Ōshima, Sea of Japan

An eruption of Oshima-Ōshima occurred that lasted from 18 August 1741 to 1 May 1742. On 29 August 1741, a devastating tsunami occurred.[44] It killed at least 1,467 people along a 120-kilometre (75 mi) section of the coast, excluding native residents whose deaths were not recorded. Wave heights for Gankakezawa have been estimated at 34 metres (112 ft) based on oral histories, while an estimate of 13 metres (43 ft) is derived from written records. At Sado Island, over 350 kilometres (217 mi; 189 nmi) away, a wave height of 2 to 5 metres (6 ft 7 in to 16 ft 5 in) has been estimated based on descriptions of the damage, while oral records suggest a height of 8 metres (26 ft). Wave heights have been estimated at 3 to 4 metres (9.8 to 13.1 ft) even as far away as the Korean Peninsula.[45] There is still no consensus in the debate as to what caused it but much evidence points to a landslide and debris avalanche along the flank of the volcano. An alternative hypothesis holds that an earthquake caused the tsunami.[46][47][48][49] The event reduced the elevation of the peak of Hishiyama from 850 to 722 metres (2,789 to 2,369 ft). An estimated 2.4-cubic-kilometre (0.58 cu mi) section of the volcano collapsed onto the seafloor north of the island; the collapse was similar in size to the 2.3-cubic-kilometre (0.55 cu mi) collapse which occurred during the 1980 eruption of Mount St. Helens.[50]

1756: Langfjorden, Norway

Just before 8:00 p.m. on February 22, 1756, a landslide with a volume of 12,000,000 to 15,000,000 cubic metres (16,000,000 to 20,000,000 cu yd) travelled at high speed from a height of 400 metres (1,300 ft) on the side of the mountain Tjellafjellet into the Langfjorden about 1 kilometre (0.6 mi) west of Tjelle, Norway, between Tjelle and Gramsgrø. The slide generated three megatsunamis in the Langfjorden and the Eresfjorden with heights of 40 to 50 metres (130 to 160 ft). The waves flooded the shore for 200 metres (660 ft) inland in some areas, destroying farms and other inhabited areas. Damaging waves struck as far away as Veøy, 25 kilometres (16 mi) from the landslide — where they washed inland 20 metres (66 ft) above normal flood levels — and Gjermundnes, 40 kilometres (25 mi) from the slide. The waves killed 32 people and destroyed 168 buildings, 196 boats, large amounts of forest, and roads and boat landings.[51]

1792: Mount Unzen, Japan

On 21 May 1792, a flank of the Mayamaya dome of Mount Unzen collapsed after two large earthquakes. This had been preceded by a series of earthquakes coming from the mountain, beginning near the end of 1791. Initial wave heights were 100 metres (330 ft), but when they hit the other side of Ariake Bay, they were only 10 to 20 metres (33 to 66 ft) in height, though one location received 57-metre (187 ft) waves due to seafloor topography. The waves bounced back to Shimabara, which, when they hit, accounted for about half of the tsunami's victims. According to estimates, 10,000 people were killed by the tsunami, and a further 5,000 were killed by the landslide. As of 2011, it was the deadliest known volcanic event in Japan.[52]

1853–1854: Lituya Bay, Alaska

Sometime between August 1853 and May 1854, a megatsunami occurred in Lituya Bay in what was then Russian America. Studies of Lituya Bay between 1948 and 1953 first identified the event, which probably occurred because of a large landslide on the south shore of the bay near Mudslide Creek. The wave had a maximum run-up height of 120 metres (394 ft), flooding the coast of the bay up to 230 metres (750 ft) inland.[53]

1874: Lituya Bay, Alaska

A study of Lituya Bay in 1953 concluded that sometime around 1874, perhaps in May 1874, another megatsunami occurred in Lituya Bay in Alaska. Probably occurring because of a large landslide on the south shore of the bay in the Mudslide Creek Valley, the wave had a maximum run-up height of 24 metres (80 ft), flooding the coast of the bay up to 640 metres (2,100 ft) inland.[54]

1883: Krakatoa, Sunda Strait

The eruption of Krakatoa created pyroclastic flows which generated megatsunamis when they hit the waters of the Sunda Strait on 27 August 1883. The waves reached heights of up to 24 metres (79 feet) along the south coast of Sumatra and up to 42 metres (138 feet) along the west coast of Java.[55] The tsunamis were powerful enough to kill over 30,000 people, and their effect was such that an area of land in Banten had its human settlements wiped out, and they never repopulated. (This area rewilded and was later declared a national park.) The steamship Berouw, a colonial gunboat, was flung over a mile (1.6 km) inland on Sumatra by the wave, killing its entire crew. Pyroclastic flows scorched several thousand people to death in southern Sumatra, and two ships reported severe winds and tephra, though they were too far away to be scorched. Two thirds of the island collapsed into the sea after the event.[56] Groups of human skeletons were found floating on pumice numerous times, up to a year after the event.[57] The eruption also generated what is often called the loudest sound in history, which was heard 4,800 kilometres (3,000 mi; 2,600 nmi) away on Rodrigues in the Indian Ocean.

1905: Lovatnet, Norway

On January 15, 1905, a landslide on the slope of the mountain Ramnefjellet with a volume of 350,000 cubic metres (460,000 cu yd) fell from a height of 500 metres (1,600 ft) into the southern end of the lake Lovatnet in Norway, generating three megatsunamis of up to 40.5 metres (133 ft) in height. The waves destroyed the villages of Bødal and Nesdal near the southern end of the lake, killing 61 people — half their combined population — and 261 farm animals and destroying 60 houses, all the local boathouses, and 70 to 80 boats, one of which — the tourist boat Lodalen — was thrown 300 metres (1,000 ft) inland by the last wave and wrecked. At the northern end of the 11.7-kilometre (7.3 mi) long lake, a wave measured at almost 6 metres (20 ft) destroyed a bridge.[58]

1905: Disenchantment Bay, Alaska

On July 4, 1905, an overhanging glacier — since known as the Fallen Glacier — broke loose, slid out of its valley, and fell 300 metres (1,000 ft) down a steep slope into Disenchantment Bay in Alaska, clearing vegetation along a path 0.8 kilometres (0.5 mi) wide. When it entered the water, it generated a megatsunami which broke tree branches 34 metres (110 ft) above ground level 0.8 kilometres (0.5 mi) away. The wave killed vegetation to a height of 20 metres (65 ft) at a distance of 5 kilometres (3 mi) from the landslide, and it reached heights of from 15 to 35 metres (50 to 115 ft) at different locations on the coast of Haenke Island. At a distance of 24 kilometres (15 mi) from the slide, observers at Russell Fjord reported a series of large waves that caused the water level to rise and fall 5 to 6 metres (15 to 20 ft) for a half-hour.[59]

1934: Tafjorden, Norway

On April 7, 1934, a landslide on the slope of the mountain Langhamaren with a volume of 3,000,000 cubic metres (3,900,000 cu yd) fell from a height of about 730 metres (2,395 ft) into the Tafjorden in Norway, generating three megatsunamis, the last and largest of which reached a height of between 62 and 63.5 metres (203 and 208 ft) on the opposite shore. Large waves struck Tafjord and Fjørå. The waves killed 23 people at Tafjord, where the last and largest wave was 17 metres (56 ft) tall and struck at an estimated speed of 160 kilometres per hour (100 mph), flooding the town for 300 metres (328 yd) inland and killing 23 people. At Fjørå, waves reached 13 metres (43 ft), destroyed buildings, removed all soil, and killed 17 people. Damaging waves struck as far as 50 kilometres (31 mi) away, and waves were detected at a distance of 100 kilometres (62 mi) from the landslide. One survivor suffered serious injuries requiring hospitalization.[60]

1936: Lovatnet, Norway

On September 13, 1936, a landslide on the slope of the mountain Ramnefjellet with a volume of 1,000,000 cubic metres (1,300,000 cu yd) fell from a height of 800 metres (3,000 ft) into the southern end of the lake Lovatnet in Norway, generating three megatsunamis, the largest of which reached a height of 74 metres (243 ft). The waves destroyed all farms at Bødal and most farms at Nesdal — completely washing away 16 farms — as well as 100 houses, bridges, a power station, a workshop, a sawmill, several grain mills, a restaurant, a schoolhouse, and all boats on the lake. A 12.6-metre (41 ft) wave struck the southern end of the 11.7-kilometre (7.3 mi) long lake and caused damaging flooding in the Loelva River, the lake's northern outlet. The waves killed 74 people and severely injured 11.[58]

1936: Lituya Bay, Alaska

On October 27, 1936, a megatsunami occurred in Lituya Bay in Alaska with a maximum run-up height of 150 metres (490 ft) in Crillon Inlet at the head of the bay. The four eyewitnesses to the wave in Lituya Bay itself all survived and described it as between 30 and 76 metres (100 and 250 ft) high. The maximum inundation distance was 610 metres (2,000 ft) inland along the north shore of the bay. The cause of the megatsunami remains unclear, but may have been a submarine landslide.[61]

1958: Lituya Bay, Alaska, US

Damage from the 1958 Lituya Bay megatsunami can be seen in this oblique aerial photograph of Lituya Bay, Alaska as the lighter areas at the shore where trees have been stripped away. The red arrow shows the location of the landslide, and the yellow arrow shows the location of the high point of the wave sweeping over the headland.

On July 9, 1958, a giant landslide at the head of Lituya Bay in Alaska, caused by an earthquake, generated a wave that washed out trees to a maximum elevation of 520 metres (1,710 ft) at the entrance of Gilbert Inlet.[62] The wave surged over the headland, stripping trees and soil down to bedrock, and surged along the fjord which forms Lituya Bay, destroying two fishing boats anchored there and killing two people.[8] This was the highest wave of any kind ever recorded.[citation needed] The subsequent study of this event led to the establishment of the term "megatsunami," to distinguish it from ordinary tsunamis.[citation needed]

1963: Vajont Dam, Italy

On October 9, 1963, a landslide above Vajont Dam in Italy produced a 250 m (820 ft) surge that overtopped the dam and destroyed the villages of Longarone, Pirago, Rivalta, Villanova, and Faè, killing nearly 2,000 people. This is currently the only known example of a megatsunami that was indirectly caused by human activities.[63]

1980: Spirit Lake, Washington, US

On May 18, 1980, the upper 400 metres (1,300 ft) of Mount St. Helens collapsed, creating a landslide. This released the pressure on the magma trapped beneath the summit bulge which exploded as a lateral blast, which then released the pressure on the magma chamber and resulted in a plinian eruption.

One lobe of the avalanche surged onto Spirit Lake, causing a megatsunami which pushed the lake waters in a series of surges, which reached a maximum height of 260 metres (850 ft)[64] above the pre-eruption water level (about 975 m (3,199 ft) ASL). Above the upper limit of the tsunami, trees lie where they were knocked down by the pyroclastic surge; below the limit, the fallen trees and the surge deposits were removed by the megatsunami and deposited in Spirit Lake.[65]

2015: Taan Fiord, Alaska, US

On 9 August 2016, United States Geological Survey scientists survey run-up damage from the 17 October 2015 megatsunami in Taan Fiord. Based on visible damage to trees that remained standing, they estimated run-up heights in this area of 5 metres (16.4 ft).

At 8:19 p.m. Alaska Daylight Time on October 17, 2015, the side of a mountain collapsed, at the head of Taan Fiord, a finger of Icy Bay in Alaska.[66][67][68] Some of the resulting landslide came to rest on the toe of Tyndall Glacier,[66][69] but about 180,000,000 short tons (161,000,000 long tons; 163,000,000 metric tons) of rock with a volume of about 50,000,000 cubic metres (65,400,000 cu yd) fell into the fjord.[68][66][70][71] The landslide generated a megatsunami with an initial height of about 100 metres (330 feet)[69][72] that struck the opposite shore of the fjord, with a run-up height there of 193 metres (633 feet).[66][67]

Over the next 12 minutes,[67] the wave travelled down the fjord at a speed of up to 97 kilometres per hour (60 mph),[71] with run-up heights of over 100 metres (328 feet) in the upper fjord to between 30 and 100 metres (98 and 330 feet) or more in its middle section, and 20 metres (66 feet) or more at its mouth.[66][67] Still probably 12 metres (40 feet) tall when it entered Icy Bay,[72] the tsunami inundated parts of Icy Bay's shoreline with run-ups of 4 to 5 metres (13 to 16 feet) before dissipating into insignificance at distances of 5 kilometres (3.1 mi) from the mouth of Taan Fiord,[67] although the wave was detected 140 kilometres (87 miles) away.[66]

Occurring in an uninhabited area, the event was unwitnessed, and several hours passed before the signature of the landslide was noticed on seismographs at Columbia University in New York City.[67][73]

2017: Karrat Fjord, Greenland

On June 17, 2017, 35,000,000 to 58,000,000 cubic metres (46,000,000 to 76,000,000 cu yd) of rock on the mountain Ummiammakku fell from an elevation of roughly 1,000 metres (3,280 ft) into the waters of the Karrat Fjord. The event was thought to be caused by melting ice that destabilised the rock. It registered as a magnitude 4.1 earthquake and created a 100-metre (328 ft) wave. The settlement of Nuugaatsiaq, 32 kilometres (20 mi) away, saw run-up heights of 9 metres (30 ft). Eleven buildings were swept into the sea, four people died, and 170 residents of Nuugaatsiaq and Illorsuit were evacuated because of a danger of additional landslides and waves. The tsunami was noted at settlements as far as 100 kilometres (62 mi) away.[74][75][76][77][78]

2020: Paatuut, Greenland

On November 21, 2020, a landslide composed of 90,000,000 cubic metres (120,000,000 cu yd) of rock with a mass of 260,000,000 tons fell from an elevation of 1,000 to 1,400 metres (3,300 to 4,600 ft) at Paatuut on the Nuussuaq Peninsula on the west coast of Greenland, reaching a speed of 140 kilometres per hour (87 mph). About 30,000,000 cubic metres (39,000,000 cu yd) of material with a mass of 87,000,000 tons entered Sullorsuaq Strait (known in Danish as Vaigat Strait), generating a megatsunami. The wave had a run-up height of 50 metres (164 ft) near the landslide and 28 metres (92 ft) at Qullissat, the site of an abandoned settlement across the strait on Disko Island, 20 kilometres (11 nmi; 12 mi) away, where it inundated the coast as far as 100 metres (328 ft) inland. Refracted energy from the tsunami created a wave that destroyed boats at the closest populated village, Saqqaq, on the southwestern coast of the Nuussuaq Peninsula 40 kilometres (25 mi) from the landslide.[79]

2020: Elliot Creek, British Columbia, Canada

On 28 November 2020, unseasonably heavy rainfall triggered a landslide of 18,000,000 m3 (24,000,000 cu yd) into a glacial lake at the head of Elliot Creek. The sudden displacement of water generated a 100 m (330 ft) high megatsunami that cascaded down Elliot Creek and the Southgate River to the head of Bute Inlet, covering a total distance of over 60 km (37 mi). The event generated a magnitude 5.0 earthquake and destroyed over 8.5 km (5.3 mi) of salmon habitat along Elliot Creek.[80]

Potential future megatsunamis

In a BBC television documentary broadcast in 2000, experts said that they thought that a landslide on a volcanic ocean island is the most likely future cause of a megatsunami.[81] The size and power of a wave generated by such means could produce devastating effects, travelling across oceans and inundating up to 25 kilometres (16 mi) inland from the coast. This research was later found to be flawed.[82] The documentary was produced before the experts' scientific paper was published and before responses were given by other geologists. There have been megatsunamis in the past,[83] and future megatsunamis are possible but current geological consensus is that these are only local. A megatsunami in the Canary Islands would diminish to a normal tsunami by the time it reached the continents.[84] Also, the current consensus for La Palma is that the region conjectured to collapse is too small and too geologically stable to do so in the next 10,000 years, although there is evidence for past megatsunamis local to the Canary Islands thousands of years ago. Similar remarks apply to the suggestion of a megatsunami in Hawaii.[85]

British Columbia

Some geologists consider an unstable rock face at Mount Breakenridge, above the north end of the giant fresh-water fjord of Harrison Lake in the Fraser Valley of southwestern British Columbia, Canada, to be unstable enough to collapse into the lake, generating a megatsunami that might destroy the town of Harrison Hot Springs (located at its south end).[86]

Canary Islands

Main page: Earth:Cumbre Vieja tsunami hazard

Geologists Dr. Simon Day and Dr. Steven Neal Ward consider that a megatsunami could be generated during an eruption of Cumbre Vieja on the volcanic ocean island of La Palma, in the Canary Islands, Spain.[87][88] Day and Ward hypothesize[87][88] that if such an eruption causes the western flank to fail, a megatsunami could be generated.

In 1949, an eruption occurred at three of the volcano's vents—Duraznero, Hoyo Negro, and Llano del Banco. A local geologist, Juan Bonelli-Rubio, witnessed the eruption and recorded details on various phenomenon related to the eruption. Bonelli-Rubio visited the summit area of the volcano and found that a fissure about 2.5 kilometres (1.6 mi) long had opened on the east side of the summit. As a result, the western half of the volcano—which is the volcanically active arm of a triple-armed rift—had slipped approximately 2 metres (7 ft) downwards and 1 metre (3 ft) westwards towards the Atlantic Ocean.[89]

In 1971, an eruption occurred at the Teneguía vent at the southern end of the sub-aerial section of the volcano without any movement. The section affected by the 1949 eruption is currently stationary and does not appear to have moved since the initial rupture.[90]

Cumbre Vieja remained dormant until an eruption began on September 19, 2021.[91]

It is likely that several eruptions would be required before failure would occur on Cumbre Vieja.[87][88] The western half of the volcano has an approximate volume of 500 cubic kilometres (120 cu mi) and an estimated mass of 1.5 trillion metric tons (1.7×1012 short tons). If it were to catastrophically slide into the ocean, it could generate a wave with an initial height of about 1,000 metres (3,300 ft) at the island, and a likely height of around 50 metres (200 ft) at the Caribbean and the Eastern North American seaboard when it runs ashore eight or more hours later. Tens of millions of lives could be lost in the cities and/or towns of St. John's, Halifax, Boston, New York City , Baltimore, Washington, D.C., Miami, Havana and the rest of the eastern coasts of the United States and Canada, as well as many other cities on the Atlantic coast in Europe, South America and Africa.[87][88] The likelihood of this happening is a matter of vigorous debate.[92][needs update?]

Geologists and volcanologists are in general agreement that the initial study was flawed. The current geology does not suggest that a collapse is imminent. Indeed, it seems to be geologically impossible right now—the region conjectured as prone to collapse is too small and too stable to collapse within the next 10,000 years.[82] A closer study of deposits left in the ocean from previous landslides suggests that a landslide would likely occur as a series of smaller collapses rather than a single landslide. A megatsunami does seem possible locally in the distant future as there is geological evidence from past deposits suggesting that a megatsunami occurred with marine material deposited 41 to 188 metres (135 to 617 ft) above sea level between 32,000 and 1.75 million years ago.[83] This seems to have been local to Gran Canaria.

Day and Ward have admitted that their original analysis of the danger was based on several worst case assumptions.[93][94] A 2008 study examined this scenario and concluded that while it could cause a megatsunami, it would be local to the Canary Islands and would diminish in height, becoming a smaller tsunami by the time it reached the continents as the waves interfered and spread across the oceans.[84]

Hawaii

Sharp cliffs and associated ocean debris at the Kohala Volcano, Lanai and Molokai indicate that landslides from the flank of the Kilauea and Mauna Loa volcanoes in Hawaii may have triggered past megatsunamis, most recently at 120,000 BP.[95][96][97] A tsunami event is also possible, with the tsunami potentially reaching up to about 1 kilometre (3,300 ft) in height[98] According to the documentary National Geographic's Ultimate Disaster: Tsunami, if a big landslide occurred at Mauna Loa or the Hilina Slump, a 30-metre (98 ft) tsunami would take only thirty minutes to reach Honolulu. There, hundreds of thousands of people could be killed as the tsunami could level Honolulu and travel 25 kilometres (16 mi) inland. Also, the West Coast of America and the entire Pacific Rim could potentially be affected.

Other research suggests that such a single large landslide is not likely. Instead, it would collapse as a series of smaller landslides.[94]

In 2018, shortly after the beginning of the 2018 lower Puna eruption, a National Geographic article responded to such claims with "Will a monstrous landslide off the side of Kilauea trigger a monster tsunami bound for California? Short answer: No."[85]

In the same article, geologist Mika McKinnon stated:[85]

there are submarine landslides, and submarine landslides do trigger tsunamis, but these are really small, localized tsunamis. They don't produce tsunamis that move across the ocean. In all likelihood, it wouldn't even impact the other Hawaiian islands.

Another volcanologist, Janine Krippner, added:[85]

People are worried about the catastrophic crashing of the volcano into the ocean. There's no evidence that this will happen. It is slowly—really slowly—moving toward the ocean, but it's been happening for a very long time.

Despite this, evidence suggests that catastrophic collapses do occur on Hawaiian volcanoes and generate local tsunamis.[99]

Norway

Although known earlier to the local population, a crack 2 metres (6.6 ft) wide and 500 metres (1,640 ft) in length in the side of the mountain Åkerneset in Norway was rediscovered in 1983 and attracted scientific attention. It since has widened at a rate of 4 centimetres (1.6 in) per year. Geological analysis has revealed that a slab of rock 62 metres (203 ft) thick and at an elevation stretching from 150 to 900 metres (492 to 2,953 ft) is in motion. Geologists assess that an eventual catastrophic collapse of 18,000,000 to 54,000,000 cubic metres (24,000,000 to 71,000,000 cu yd) of rock into Sunnylvsfjorden is inevitable and could generate megatsunamis of 35 to 100 metres (115 to 328 ft) in height on the fjord′s opposite shore. The waves are expected to strike Hellesylt with a height of 35 to 85 metres (115 to 279 ft), Geiranger with a height of 30 to 70 metres (98 to 230 ft), Tafjord with a height of 14 metres (46 ft), and many other communities in Norway's Sunnmøre district with a height of several metres, and to be noticeable even at Ålesund. The predicted disaster is depicted in the 2015 Norwegian film The Wave.[100]

See also

  • 2004 Indian Ocean earthquake and tsunami
  • List of tsunamis
  • Tsunamis in lakes
  • Volcanic tsunami

References

Footnotes

  1. ↑ "Tsunami Characteristics". http://tsunami.org/tsunami-characteristics/. 
  2. ↑ "Tsunami Facts and Information". 2021. http://www.bom.gov.au/tsunami/info/index.shtml. 
  3. ↑ Reymond, D.; Okal, E.A.; Herbert, H.; Bourdet, M. (5 June 2012). "Rapid forecast of tsunami wave heights from a database of pre-computed simulations, and application during the 2011 Tohoku tsunami in French Polynesia". Geophysical Research Letters 39 (11). doi:10.1029/2012GL051640. Bibcode: 2012GeoRL..3911603R. https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2012GL051640. Retrieved 9 October 2023. 
  4. ↑ Fritz, Hermann M.; Mohammed, Fahad; Yoo, Jeseon (6 February 2009). "Lituya Bay Landslide Impact Generated Mega-Tsunami 50th Anniversary". Pure and Applied Geophysics 166 (1–2): 153–175. doi:10.1007/s00024-008-0435-4. Bibcode: 2009PApGe.166..153F. https://link.springer.com/article/10.1007/s00024-008-0435-4. Retrieved 9 October 2023. 
  5. ↑ Template:Cite tech report
  6. ↑ "Tsunamis". Washington State Department of Natural Resources. 2021. https://www.dnr.wa.gov/programs-and-services/geology/geologic-hazards/tsunamis/#historical-tsunamis-worldwide. 
  7. ↑ Kinsland, Gary L.; Egedahl, Kaare; Strong, Martell Albert; Ivy, Robert (13 June 2021). "Chicxulub impact tsunami megaripples in the subsurface of Louisiana: Imaged in petroleum industry seismic data". Earth and Planetary Science Letters 570: 117063. doi:10.1016/j.epsl.2021.117063. Bibcode: 2021E&PSL.57017063K. https://www.sciencedirect.com/science/article/pii/S0012821X21003186#fg0020. Retrieved 26 July 2021. 
  8. ↑ 8.0 8.1 8.2 Miller, Don J. (1960). "Giant Waves in Lituya Bay, Alaska". United States Geological Survey Professional Paper 354-C: 51–86. doi:10.3133/pp354C. 
  9. ↑ 9.0 9.1 The Mega-Tsunami of July 9, 1958 in Lituya Bay, Alaska: Analysis of Mechanism – George Pararas-Carayannis, Excerpts from Presentation at the Tsunami Symposium of Tsunami Society of May 25–27, 1999, in Honolulu, Hawaii, USA
  10. ↑ Ward, Steven N.; Day, Simon (2010). "Lituya Bay Landslide and Tsunami — A Tsunami Ball Approach". Journal of Earthquake and Tsunami 4 (4): 285–319. doi:10.1142/S1793431110000893. http://es.ucsc.edu/~ward/papers/Lituya.pdf. 
  11. ↑ Sleep, Norman H.; Lowe, Donald R. (3 March 2014). "Physics of crustal fracturing and chert dike formation triggered by asteroid impact, ∼3.26 Ga, Barberton greenstone belt, South Africa". Geochemistry, Geophysics, Geosystems 15 (4): 1054–1070. doi:10.1002/2014GC005229. https://agupubs.onlinelibrary.wiley.com/doi/full/10.1002/2014GC005229. Retrieved 19 December 2023. 
  12. ↑ "Scientists Reconstruct Ancient Impact That Dwarfs Dinosaur-Extinction Blast". 9 April 2014. https://news.agu.org/press-release/scientists-reconstruct-ancient-impact-that-dwarfs-dinosaur-extinction-blast/. 
  13. ↑ Achenbach, Joel (19 December 2023). "Scientists Reconstruct Ancient Impact That Dwarfs Dinosaur-Extinction Blast". https://www.washingtonpost.com/science/2023/12/19/early-earth-life-impacts-ocean/. 
  14. ↑ Bryant, Edward (June 2014). Tsunami: The Underrated Hazard. Springer. p. 178. ISBN 978-3-319-06133-7. https://books.google.com/books?id=tOkpBAAAQBAJ&pg=PA178. 
  15. ↑ Goto, Kazuhisa; Tada, Ryuji; Tajika, Eiichi; Bralower, Timothy J.; Hasegawa, Takashi; Matsui, Takafumi (2004). "Evidence for ocean water invasion into the Chicxulub crater at the Cretaceous/Tertiary boundary" (in en). Meteoritics & Planetary Science 39 (8): 1233–1247. doi:10.1111/j.1945-5100.2004.tb00943.x. ISSN 1945-5100. Bibcode: 2004M&PS...39.1233G. 
  16. ↑ "Generation and propagation of a tsunami from the Cretaceous-Tertiary impact event". 2021-10-20. https://www.researchgate.net/publication/228783220. 
  17. ↑ Gulick, Sean P. S.; Bralower, Timothy J.; Ormö, Jens; Hall, Brendon; Grice, Kliti; Schaefer, Bettina; Lyons, Shelby; Freeman, Katherine H. et al. (2019-09-24). "The first day of the Cenozoic" (in en). Proceedings of the National Academy of Sciences 116 (39): 19342–19351. doi:10.1073/pnas.1909479116. ISSN 0027-8424. PMID 31501350. Bibcode: 2019PNAS..11619342G. 
  18. ↑ "Dinosaur-Killing Asteroid Created A Mile-High Tsunami That Swept Through The World's Oceans". iflscience.com. January 8, 2019. https://www.iflscience.com/environment/dinosaurkilling-asteroid-created-a-milehigh-tsunami-that-swept-through-the-worlds-oceans/. 
  19. ↑ "Huge Global Tsunami Followed Dinosaur-Killing Asteroid Impact" (in en-US). 20 December 2018. https://eos.org/articles/huge-global-tsunami-followed-dinosaur-killing-asteroid-impact. 
  20. ↑ Shonting, D.; Ezrailson, C. (2017). Chicxulub: The Impact and Tsunami. Springer Praxis Books (PRAXIS). Springer Link. pp. 69–106. doi:10.1007/978-3-319-39487-9. ISBN 978-3-319-39487-9. https://link.springer.com/book/10.1007/978-3-319-39487-9. 
  21. ↑ Sanford, Jason C.; Snedden, John W.; Gulick, Sean P. S. (March 2016). "The Cretaceous-Paleogene boundary deposit in the Gulf of Mexico: Large-scale oceanic basin response to the Chicxulub impact" (in en). Journal of Geophysical Research: Solid Earth 121 (3): 1240–1261. doi:10.1002/2015JB012615. Bibcode: 2016JGRB..121.1240S. 
  22. ↑ DePalma, Robert A.; Smit, Jan; Burnham, David A.; Kuiper, Klaudia; Manning, Phillip L.; Oleinik, Anton; Larson, Peter; Maurrasse, Florentin J. et al. (2019-04-23). "A seismically induced onshore surge deposit at the KPg boundary, North Dakota" (in en). Proceedings of the National Academy of Sciences 116 (17): 8190–8199. doi:10.1073/pnas.1817407116. ISSN 0027-8424. PMID 30936306. Bibcode: 2019PNAS..116.8190D. 
  23. ↑ Le Roux, Jacobus P. (2015). "A critical examination of evidence used to re-interpret the Hornitos mega-breccia as a mass-flow deposit caused by cliff failure". Andean Geology 41 (1): 139–145. http://www.andeangeology.equipu.cl/index.php./revista1/article/view/V42n1-a08/html. 
  24. ↑ Le Roux, J.P.; Nielsen, Sven N.; Kemnitz, Helga; Henriquez, Álvaro (2008). "A Pliocene mega-tsunami deposit and associated features in the Ranquil Formation, southern Chile". Sedimentary Geology 203 (1): 164–180. doi:10.1016/j.sedgeo.2007.12.002. Bibcode: 2008SedG..203..164L. http://repositorio.uchile.cl/bitstream/handle/2250/125260/Le%20Roux_J_P.pdf?sequence=1. Retrieved 11 April 2016. 
  25. ↑ "Hawaiian landslides have been catastrophic". mbari.org. Monterey Bay Aquarium Research Institute. 2015-10-22. http://www.mbari.org/volcanism/Hawaii/HR-Landslides.htm. 
  26. ↑ Culliney, John L. (2006) Islands in a Far Sea: The Fate of Nature in Hawaii. Honolulu: University of Hawaii Press. p. 17.
  27. ↑ "Kalaupapa Settlement Boundary Study. Along North Shore to Halawa Valley, Molokai". National Park Service. 2001. https://www.nps.gov/kala/learn/management/upload/MinkVI.pdf. 
  28. ↑ Paskoff, Roland (1991). "Likely occurrence of mega-tsunami in the Middle Pleistocene near Coquimbo, Chile". Revista Geológica de Chile 18 (1): 87–91. http://www.andeangeology.cl/index.php/revista1/article/viewFile/2485/2690. Retrieved 17 July 2016. 
  29. ↑ Johnson, Carl; Mader, Charles L. (January 1995). "Modeling the 105 KA Lanai Tsunami". ResearchGate. https://www.researchgate.net/publication/264038439. 
  30. ↑ Ramalho, Ricardo S.; Winckler, Gisela; Madeira, José; Helffrich, George R.; Hipólito, Ana; Quartau, Rui; Adena, Katherine; Schaefer, Joerg M. (2015-10-01). "Hazard potential of volcanic flank collapses raised by new megatsunami evidence" (in en). Science Advances 1 (9): e1500456. doi:10.1126/sciadv.1500456. ISSN 2375-2548. PMID 26601287. Bibcode: 2015SciA....1E0456R. 
  31. ↑ Gardner, J.V. (July 2000). "The Lake Tahoe debris avalanche". Geological Society of Australia. 
  32. ↑ Alden, Andrew, "The 'Tahoe Tsunami': New Study Envisions Early Geologic Event," kqed.org, July 31, 2014, Retrieved 23 June 2020
  33. ↑ Bondevik, S.; Lovholt, F.; Harbitz, C.; Mangerud, J.; Dawsond, A.; Svendsen, J. I. (2005). "The Storegga Slide tsunami—comparing field observations with numerical simulations". Marine and Petroleum Geology 22 (1–2): 195–208. doi:10.1016/j.marpetgeo.2004.10.003. Bibcode: 2005MarPG..22..195B. 
  34. ↑ Rincon, Paul (1 May 2014). "Prehistoric North Sea 'Atlantis' hit by 5m tsunami". BBC News. https://www.bbc.com/news/science-environment-27224243. 
  35. ↑ Pareschi, Maria Teresa; Boschi, Enzo; Favalli, Mazzarini; Francesco, Massimiliano (1 July 2006). "Large submarine landslides offshore Mt. Etna". Geophysical Research Letters (GEOPHYSICAL RESEARCH LETTERS, VOL. 33, L13302, doi:10.1029/2006GL026064, 2006) 33 (13). doi:10.1029/2006GL026064. Bibcode: 2006GeoRL..3313302P. 
  36. ↑ Pareschi, Maria Teresa; Boschi, Enzo; Favalli, Massimiliano (28 November 2006). "Lost tsunami". Geophysical Research Letters (AGU) 33 (22). doi:10.1029/2006GL027790. Bibcode: 2006GeoRL..3322608P. 
  37. ↑ CISEM News (December 2006). "From the Etna to the Levantine shore – an ancient tsunami?". CISEM: The Mediterranean Science Commission. https://ciesm.org/news/mscience/12.htm. 
  38. ↑ Pareschi, Maria Teresa; Boschi, Enzo; Favalli, Massimiliano (30 August 2007). "Holocene tsunamis from Mount Etna and the fate of Israeli Neolithic communities". Geophysical Research Letters (AGU) 34 (16). doi:10.1029/2007GL030717. Bibcode: 2007GeoRL..3416317P. 
  39. ↑ Frébourg, Gregory; Hasler, Claude-Alain; Davaud, Eric (March 2010). "Catastrophic event recorded among Holocene eolianites (Sidi Salem Formation, SE Tunisia)". Sedimentary Geology, Volume 224, Issue 1, p. 38-48. https://www.sciencedirect.com/science/article/abs/pii/S0037073809002930. 
  40. ↑ 40.0 40.1 Korsgaard, Niels J.; Svennevig, Kristian; Søndergaard, Anne S.; Luetzenburg, Gregor; Oksman, Mimmi; Larsen, Nicolaj K. (13 March 2023). "Giant mid-Holocene landslide-generated tsunamis recorded in lake sediments from Saqqaq, West Greenland". European Geosciences Union. https://nhess.copernicus.org/preprints/nhess-2023-32/. 
  41. ↑ "Mega-tsunami: Wave of Destruction". BBC Two. 12 October 2000. http://www.bbc.co.uk/science/horizon/2000/mega_tsunami.shtml. 
  42. ↑ Pranantyo, Ignatius Ryan; Cummins, Phil R. (2020). "The 1674 Ambon Tsunami: Extreme Run-up Caused by an Earthquake-Triggered Landslide". Pure and Applied Geophysics 177 (3): 1639–1657. doi:10.1007/s00024-019-02390-2. https://link.springer.com/article/10.1007/s00024-019-02390-2. 
  43. ↑ Hoel, Christer, "The Skafjell Rock Avalanche in 1731," fjords.com Retrieved 23 June 2020
  44. ↑ "Significant Volcanic Eruption". https://www.ngdc.noaa.gov/hazel/view/hazards/volcano/event-more-info/2673. 
  45. ↑ Satake, Kenji (2007). "Volcanic origin of the 1741 Oshima-Oshima tsunami in the Japan Sea". Earth, Planets and Space 59 (5): 381–390. doi:10.1186/BF03352698. Bibcode: 2007EP&S...59..381S. https://earth-planets-space.springeropen.com/counter/pdf/10.1186/BF03352698.pdf. 
  46. ↑ Im Sang Oh; Alexander B. Rabinovich (1994). "Manifestation of Hokkaido Southwest (Okushiri) Tsunami, 12 July, 1993, at the Coast of Korea: Statistsl Characteristics Spectul Analysis, and Energy Decay". The International Journal of the Tsunami Society (Seoul National University) 12 (2): 93–116. ISSN 0736-5306. https://library.lanl.gov/tsunami/00394725.pdf. Retrieved 30 March 2021. 
  47. ↑ Katsui, Yoshio; Yamamoto, Masatsugu (1981). "The 1741-1742 Activity of Oshima-Ōshima Volcano, North Japan". Journal of the Faculty of Science, Geology and Mineralogy (Japan: Hokkaido University) 19 (4): 527–536. https://eprints.lib.hokudai.ac.jp/dspace/bitstream/2115/36702/1/19_4_p527-536.pdf. Retrieved 30 March 2021. 
  48. ↑ "Error: no |title= specified when using {{Cite web}}" (in ja). August 2014. https://www.mlit.go.jp/river/shinngikai_blog/daikibojishinchousa/dai08kai/sanko1.pdf. 
  49. ↑ Abe, Katsuyuki (1989). "Quantification of tsunamigenic earthquakes by the Mt scale". Tectonophysics 166 (1–3): 27–34. doi:10.1016/0040-1951(89)90202-3. ISSN 0040-1951. Bibcode: 1989Tectp.166...27A. https://www.sciencedirect.com/science/article/abs/pii/0040195189902023. Retrieved 30 March 2021. 
  50. ↑ Kenji Satake; Yukihiro Kato (1 February 2001). "The 1741 Oshima-Oshima Eruption: Extent and volume of submarine debris avalanche". Geophysical Research Letters 28 (3): 427–430. doi:10.1029/2000GL012175. Bibcode: 2001GeoRL..28..427S. 
  51. ↑ "Hoel, Christer, "The Tjelle Rock Avalanche in 1756," fjords.com Retrieved 22 June 2020". https://www.fjords.com/rock-avalanches-tjelle/. 
  52. ↑ Hays, Jeffrey (1990-11-17). "Unzen volcano and eruptions". https://factsanddetails.com/japan/cat26/sub160/entry-6600.html. 
  53. ↑ Lander, pp. 39–41.
  54. ↑ Lander, pp. 44–45.
  55. ↑ Bryant, Edward, Tsunami: The Underrated Hazard, Springer: New York, 2014, ISBN:978-3-319-06132-0, pp. 162–163.
  56. ↑ "How Volcanoes Work - Krakatau, Indonesia 1883". http://www.geology.sdsu.edu/how_volcanoes_work/Krakatau.html. 
  57. ↑ Winchester, Simon (2003). Krakatoa: The Day The World Exploded, August 27, 1883. Viking. ISBN 978-0-670-91430-2. 
  58. ↑ 58.0 58.1 Hoel, Christer, "The Loen Accidents in 1905 and 1936," fjords.com Retrieved 22 June 2020
  59. ↑ Lander, p. 57.
  60. ↑ Hoel, Christer, "The Tafjord Accident in 1934," fjords.com Retrieved 22 June 2020
  61. ↑ Lander, pp. 61–64.
  62. ↑ Mader, Charles L.; Gittings, Michael L. (2002). "Modeling the 1958 Lituya Bay Mega-Tsunami, II". Science of Tsunami Hazards 20 (5): 241–250. http://library.lanl.gov/tsunami/ts205.pdf. 
  63. ↑ "Vaiont Dam, Italy". http://www.uwsp.edu/geo/projects/geoweb/participants/Dutch/VTrips/Vaiont.HTM.  Vaiont Dam photos and virtual field trip (University of Wisconsin), retrieved 2009-07-01
  64. ↑ Voight et al. 1983
  65. ↑ [1]USGS Website. Geology of Interactions of Volcanoes, Snow, and Water: Tsunami on Spirit Lake early during 18 May 1980 eruption
  66. ↑ 66.0 66.1 66.2 66.3 66.4 66.5 researchgate.net The 2015 Landslide and Tsunami in Taan Fiord, Alaska
  67. ↑ 67.0 67.1 67.2 67.3 67.4 67.5 Higman, Bretwood, et al., "The 2015 landslide and tsunami in Taan Fiord, Alaska," nature.com, September 6, 2018 Retrieved 16 June 2020
  68. ↑ 68.0 68.1 nps.gov National Park Service, "Taan Fjord Landslide and Tsunami," nps.gov, Retrieved 16 June 2020
  69. ↑ 69.0 69.1 Rozell, Ned, "The giant wave of Icy Bay," alaska.edu, April 7, 2016 Retrieved 16 June 2020
  70. ↑ Underwood, Emily, "Study of Alaskan Landslide Could Improve Tsunami Modeling," eos.org, April 26, 2019 Retrieved 16 June 2020
  71. ↑ 71.0 71.1 Mooney, Chris, "One of the biggest tsunamis ever recorded was set off three years ago by a melting glacier," washingtonpost.com, September 6, 2018 Retrieved 16 June 2020
  72. ↑ 72.0 72.1 Stolz, Kit, "Why Scientists Are Worried About a Landslide No One Saw or Heard," atlasobscura.com, March 17, 2017 Retrieved 16 June 2020
  73. ↑ Morford Stacy, "Detecting Landslides from a Few Seismic Wiggles," columbia.edu, December 18, 2015 Retrieved 16 June 2020
  74. ↑ "After recon trip, researchers say Greenland tsunami in June reached 300 feet high". Georgia Institute of Technology. 25 July 2017. http://www.ce.gatech.edu/news/after-recon-trip-researchers-say-greenland-tsunami-june-reached-300-feet-high. 
  75. ↑ "Four missing after tsunami strikes Greenland coast". BBC News. 18 June 2017. https://www.bbc.com/news/world-europe-40320629. 
  76. ↑ "Greenland tsunami leaves four people missing". Irish Independent. 18 June 2017. http://www.independent.ie/world-news/greenland-tsunami-leaves-four-people-missing-35839239.html. 
  77. ↑ "17 June 2017, Karrat Fjord, Greenland Landslide & Tsunami". International Tsunami Information Center. http://itic.ioc-unesco.org/index.php?option=com_content&view=article&id=2164&Itemid=3237. 
  78. ↑ Svennevig, Kristian; Dahl-Jensen, Trine; Keiding, Marie; Boncori, John Peter Merryman; Larsen, Tine B.; Salehi, Sara; Solgaard, Anne Munck; Voss, Peter H. (8 December 2020). "Evolution of events before and after the 17 June 2017 rock avalanche at Karrat Fjord, West Greenland – a multidisciplinary approach to detecting and locating unstable rock slopes in a remote Arctic area". European Geosciences Union. https://esurf.copernicus.org/articles/8/1021/2020/. 
  79. ↑ Dahl-Jensen, Trine; Larsen, Lotte; Pedersen, Stig; Pedersen, Jerrik; Jepsen, Hans; Pedersen, Gunver; Nielsen, Tove; Pedersen, Asger et al. (2004). "Landslide and Tsunami 21 November 2000 in Paatuut, West Greenland". Ideas. https://ideas.repec.org/a/spr/nathaz/v31y2004i1p277-287.html. 
  80. ↑ "Landslide caused by melting B.C. glacier created massive tsunami, destroyed salmon habitat: study" (in en-US). Global News. https://globalnews.ca/news/8723389/bc-glacier-landslide-study/. 
  81. ↑ "Mega-tsunami: Wave of Destruction". Transcript. BBC Two television programme, first broadcast. 12 October 2000. http://www.bbc.co.uk/science/horizon/2000/mega_tsunami_transcript.shtml. 
  82. ↑ 82.0 82.1 "New Research Puts 'Killer La Palma Tsunami' At Distant Future". Science Daily, based on materials from the Delft University of Technology. September 21, 2006. https://www.sciencedaily.com/releases/2006/09/060920192823.htm. 
  83. ↑ 83.0 83.1 Pérez-Torrado, F. J.; Paris, R.; Cabrera, M. C; Schneider, J.-L.; Wassmer, P.; Carracedo, J. C.; Rodríguez-Santana, A.; & Santana, F. (2006). Tsunami deposits related to flank collapse in oceanic volcanoes: The Agaete Valley evidence, Gran Canaria, Canary Islands. Marine Geol. 227, 135–149
  84. ↑ 84.0 84.1 Løvholt, F.; Pedersen, G.; & Gisler, G. (2008). "Oceanic propagation of a potential tsunami from the La Palma Island." Journal of Geophysical Research: Oceans 113.C9.
  85. ↑ 85.0 85.1 85.2 85.3 Sarah Gibbons (May 17, 2018). "No, Hawaii's Volcano Won't Trigger a Mega-Tsunami". National Geographic. https://news.nationalgeographic.com/2018/05/kilauea-volcano-tsunami-explosive-hawaii-myths-explained-science/. 
  86. ↑ Evans, S.G.; Savigny, K.W. (1994). "Landslides in the Vancouver-Fraser Valley-Whistler region". Geological Survey of Canada. Ministry of Forests, Province of British Columbia. pp. 36 p. http://www.for.gov.bc.ca/hfd/library/ffip/Evans_SG1994.pdf. 
  87. ↑ 87.0 87.1 87.2 87.3 Day et al. 1999
  88. ↑ 88.0 88.1 88.2 88.3 Ward & Day 2001
  89. ↑ Bonelli-Rubio, J. M. (1950). Contribucion al estudio de la erupcion del Nambroque o San Juan. Madrid: Inst. Geografico y Catastral, 25 pp.
  90. ↑ As per Bonelli Rubio
  91. ↑ Jones, Sam (19 September 2021). "Spanish Canary Island volcano erupts after weeks of earthquakes" (in en). The Guardian. https://www.theguardian.com/world/2021/sep/19/spanish-canary-island-volcano-erupts-after-weeks-of-earthquakes. 
  92. ↑ Pararas-Carayannis 2002
  93. ↑ Ali Ayres (2004-10-29). "Tidal wave threat 'over-hyped'". BBC News. http://newsvote.bbc.co.uk/mpapps/pagetools/print/news.bbc.co.uk/2/hi/science/nature/3963563.stm. 
  94. ↑ 94.0 94.1 Pararas-Carayannis 2002.
  95. ↑ McMurtry, Gary M.; Fryer, Gerard J.; Tappin, David R.; Wilkinson, Ian P.; Williams, Mark; Fietzke, Jan; Garbe-Schoenberg, Dieter; Watts, Philip (1 September 2004). "Megatsunami deposits on Kohala volcano, Hawaii, from flank collapse of Mauna Loa". Geology 32 (9): 741. doi:10.1130/G20642.1. Bibcode: 2004Geo....32..741M. http://geology.geoscienceworld.org/cgi/content/full/32/9/741. 
  96. ↑ McMurtry, Gary M.; Fryer, Gerard J.; Tappin, David R.; Wilkinson, Ian P.; Williams, Mark; Fietzke, Jan; Garbe-Schoenberg, Dieter; Watts, Philip (September 1, 2004). "A Gigantic Tsunami in the Hawaiian Islands 120,000 Years Ago". Geology. SOEST Press Releases. http://www.soest.hawaii.edu/SOEST_News/PressReleases/Megatsunami/. 
  97. ↑ McMurtry, G. M.; Tappin, D. R.; Fryer, G. J.; Watts, P. (December 2002). "Megatsunami Deposits on the Island of Hawaii: Implications for the Origin of Similar Deposits in Hawaii and Confirmation of the 'Giant Wave Hypothesis'". AGU Fall Meeting Abstracts 51: OS51A–0148. Bibcode: 2002AGUFMOS51A0148M. 
  98. ↑ Britt, Robert Roy (14 December 2004). "The Megatsunami: Possible Modern Threat". LiveScience. http://www.livescience.com/environment/041214_tsunami_mega.html. 
  99. ↑ Fryer, G.J.; McMurtry, G.M. (June 12–15, 2005). "Megatsunami Deposits vs. High-stand Deposits in Hawai'i". NSF Tsunami Deposits Workshop. Department of Earth and Space Sciences, University of Washington. https://earthweb.ess.washington.edu/tsunami2/deposits/downloads/posters/fryer05worksmall.pdf. 
  100. ↑ Hole, Christer, "The Åkerneset Rock Avalanche," fjords.com Retrieved 23 June 2020

Bibliography

Further reading

  • BBC 2 TV; 2000. Transcript "Mega-tsunami; Wave of Destruction", Horizon. First screened 21.30 hrs, Thursday, 12 October 2000.
  • Carracedo, J.C. (1994). "The Canary Islands: an example of structural control on the growth of large oceanic-island volcanoes". J. Volcanol. Geotherm. Res. 60 (3–4): 225–241. doi:10.1016/0377-0273(94)90053-1. Bibcode: 1994JVGR...60..225C. 
  • Carracedo, J.C. (1996). "A simple model for the genesis of large gravitational landslide hazards in the Canary Islands". Volcano Instability on the Earth and Other Planets. Special Publication. 110. London: Geological Society. pp. 125–135. 
  • Carracedo, J.C. (1999). "Growth, Structure, Instability and Collapse of Canarian Volcanoes and Comparisons with Hawaiian Volcanoes". J. Volcanol. Geotherm. Res. 94 (1–4): 1–19. doi:10.1016/S0377-0273(99)00095-5. Bibcode: 1999JVGR...94....1C. 
  • Moore, J.G. (1964). Giant Submarine Landslides on the Hawaiian Ridge. US Geologic Survey. pp. D95–8. Professional Paper 501-D. 
  • Pinter, N.; Ishman, S.E. (2008). "Impacts, mega-tsunami, and other extraordinary claims". GSA Today 18 (1): 37–38. doi:10.1130/GSAT01801GW.1. Bibcode: 2008GSAT...18a..37P. 
  • Rihm, R; Krastel, S. & CD109 Shipboard Scientific Party; 1998. Volcanoes and landslides in the Canaries. National Environment Research Council News. Summer, 16–17.
  • Siebert, L. (1984). "Large volcanic debris avalanches: characteristics of source areas, deposits and associated eruptions". J. Volcanol. Geotherm. Res. 22 (3–4): 163–197. doi:10.1016/0377-0273(84)90002-7. Bibcode: 1984JVGR...22..163S. 
  • Vallely, G.A. (2005). "Volcanic edifice instability and tsunami generation: Montaña Teide, Tenerife, Canary Islands (Spain)". Journal of the Open University Geological Society 26 (1): 53–64. 
  • Sandom, J.G., 2010, The Wave — A John Decker Thriller, Cornucopia Press, 2010. A thriller in which a megatsunami is intentionally created when a terrorist detonates a nuclear bomb on La Palma in the Canary Islands.
  • Ortiz, J.R., Bonelli Rubio, J.M., 1951. La erupción del Nambroque (junio-agosto de 1949). Madrid: Talleres del Instituto Geográfico y Catastral, 100 p., 1h. pleg.;23 cm

External links



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