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5 Monster Glacier Collapse Caught On Camera

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INCREDIBLE COLLAPSE TRIGGERED BY GLACIER CALVING | South America, Chile

An incredibly large chunk of the Grey Glacier's ice-sheet breaks off and flips over in a spectacular way in Southern Patagonia, Chile. The ice-sheet of the Grey Glacier is currently declining due to increasing temperatures and changes in rainfall. It is part of the 'Southern Patagonian Ice Field', the world's 2nd largest contiguous extrapolar ice field and the largest freshwater reservoir in South America.

The Grey Glacier is famous for insane glacier wall collapses during the summer when large icebergs – often up to 100 feet in height – are breaking off the glacier and collapsing into the water of the 'Lago Grey'. In the right time of the year big blocks of ice break off the glacier and drop into the water. The waves created by such glacier calving events often splash dozens of meters through the air. The glacier itself is about 6 km (3.7 mi) wide and has an average height of over 30 m (100 ft) above the surface of the water.

Thankfully, no-one was injured as boats stay at a safe distance from the glacier (for a good reason).

Glacier calving, also known as ice calving, or iceberg calving, is the breaking of ice chunks from the edge of a glacier. The sudden release and breaking away of a mass of ice from a glacier or iceberg often causes large waves around the area and can result in a shooter which is a large chunk of the submerged portion of the iceberg surfacing above the water. The ice that breaks away can be classified as an iceberg, but may also be a growler, bergy bit, or a crevasse wall breakaway. The entry of the ice into the water causes large, and often hazardous waves. (Find out more here:

© Laura Q. / LS
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TOP 5 Amazing ICEBERG COLLAPSE Caught On Camera

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ICEBERG COLLAPSE
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5 Monster Glacier Collapse Caught On Camera #shorts

5 Monster Glacier Collapse Caught On Camera

Knik glacier Alaska |Knik glacier underwater footage #shorts


Ultimate Adventure 2019 Episode 1, Off Roading to Knik Glacier in Alaska #UA2019

The Knik Glacier is an ice field located 50 miles (80 km) east of Anchorage, Alaska on the northern end of the Chugach Mountains. The ice field averages over 25 miles (40 km) long and over 5 miles (8.0 km) across, making it one of the largest glaciers in southcentral Alaska. Knik Glacier feeds the 25-mile (40 km) long Knik River which empties into the Knik Arm section of Cook Inlet.Many of the tourist coming to entertain there selves from this cold glacier.
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Incredible GLACIER CALVING & TSUNAMI WAVE Caught On Camera! | Glacier Wall Collapse (Greenland)

Huge Icebergs collapsing and breaking from the Ilulissat Glacier are often up to 3,000 feet in height (1,000 meter) and are broken up by the force of the glacier and icebergs further up the fjord. Subscribe for more ►

Greenland is home to the only permanent ice sheet outside Antarctica. The sheet covers 3/4 of Greenland's land mass. The Ilulissat Icefjord drains 6.5% of the Greenland ice sheet and produces around 10% of all Greenland icebergs. Some 35 billion tonnes of icebergs calve off and pass out of the fjord every year (Find out more here: In the last 25 years, the Greenland Ice Sheet is rapidly melting, having lost 3.8 trillion tons of ice between 1992 and 2018, a new study from NASA and the European Space Agency (ESA) finds. The melting ice has added 0.4 inches (11 millimeters) to sea level rise. Its cumulative 3.8 trillion tons of melted ice is equivalent to adding the water from 120 million Olympic-size swimming pools to the ocean every year (Find out more here:

Ice calving, also known as glacier calving or iceberg calving, is the breaking of ice chunks from the edge of a glacier. It is the sudden release and breaking away of a mass of ice from a glacier, iceberg, ice front, ice shelf, or crevasse. The ice that breaks away can be classified as an iceberg, but may also be a growler, bergy bit, or a crevasse wall breakaway. The entry of the ice into the water causes large, and often hazardous waves. The waves formed in locations like Johns Hopkins Glacier can be so large that boats cannot approach closer than 3 kilometres. These events have become major tourist attractions. Many glaciers terminate at oceans or freshwater lakes which results naturally with the calving of large numbers of icebergs. Calving of Greenland's glaciers produce 12,000 to 15,000 icebergs each year alone (Find out more here:

About this video: Incredible glacier calving & tsunami wave caught on camera (Bo B.)
This video is showing huge icebergs flipping over and subsequently a series of multiple iceberg and glacier wall collapses. Due to the enormous amount of ice falling into the water, the glacier calving event even triggered a series of mini-tsunami waves up to 16 feet in height (5 m) breaking on the shore.

© Licet Studios GmbH – for further information about us, our content, or licensing / usage inquiries, you may check our website or contact us directly at: licensing@licetstudios.com.
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Glacier collapse on Juuku pass, Kyrgyzstan - insane video

July 8, 2022.
Juuku pass, Issyk-Kul region, Kyrgyz Republic

Credit: @harryshimmin

Large Iceberg Breaking near Ilulissat

Iceberg breaking up in the Ilulissat icefjord, close to an archaeological site called Sermermiut.

**A quick note - some of the external links to this video have mixed information. To be more precise, this is a large iceberg breaking up, which had already calved from the icecap. The large ones often collect at the end of the fjord, where it is a bit shallower. The NASA image at the end of the video shows this a bit more clearly**

For more information about the Ilulissat Icefjord:





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100 SCARY Tsunami And Wave Moments Caught On Camera

In this video, we have a look at some incredible clips of waves from all over the world.

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Thanks for watching and I'll see you again in the next one!

Glacier calving Tsunami

Glacier calving is a normal and natural process that occurs in many glaciers around the world. It is a form of ice mass loss where large chunks of ice break off from the glacier's terminus (the end of the glacier) and fall into a body of water, such as a lake or ocean. This process can also be referred to as glacial calving or ice calving.

Glacier calving happens because glaciers are constantly in motion, and they flow downhill under the influence of gravity. As glaciers reach bodies of water, the ice at the terminus becomes unstable and can crack and break off, forming icebergs or smaller ice chunks. The size of the calved icebergs can range from small pieces to massive chunks that can be as large as buildings.

Calving is a natural way for glaciers to adjust to changes in their environment, including changes in temperature, ice thickness, and the surrounding topography. However, in recent years, the process of calving has gained more attention due to concerns about climate change and its impact on glaciers. As temperatures rise, glaciers may experience accelerated melting and increased calving rates, contributing to rising sea levels and other environmental changes.

Overall, glacier calving is a regular part of the glacier's life cycle and plays a crucial role in shaping landscapes and influencing the movement of ice and water in polar and high-altitude regions.

Waves Sneak Up Reynisfjara Beach in Iceland and Knock Over Tourists

Taken on November 3rd, 2018 at Reynisfjara, also commonly known as the Black Sand Beach in Iceland. People didn't pay attention to warning signs about the dangerous waves that can sneak up the shore. They all got up afterwords and thankfully were ok. Be safe everyone!

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INCREDIBLE COLLAPSE triggered by glacier calving in Perito Moreno, Patagonia, Argentina | Glacier

INCREDIBLE COLLAPSE TRIGGERED BY GLACIER CALVING in Perito Moreno, Patagonia, Argentina | Glacier

We don't know it is global warming effect on glaciers, due to climate change or something else but Sometimes huge amount of ice release from glacier which is called glacier calving in Greenland, South Sawyer glacier, glacier national park, Montana, Alaska, Antarctica and many more places in the earth.

Ice calving, also known as glacier calving or iceberg calving, is the breaking of ice chunks from the edge of a glacier. It is a form of ice ablation or ice disruption and is normally caused by the glacier expanding.

It is the sudden release and breaking away of a mass of ice from a glacier, iceberg, ice front, ice shelf, or crevasse. The ice that breaks away can be classified as an iceberg, but may also be a growler, berg bit, or a crevasse wall breakaway.

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Epic Alaskan glacier calving caught on camera

The Holgate Glacier is located in Kenai Fjords National Park in Alaska. Check out this amazing footage of massive chunk of it falling into the water. So cool!

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The WORST Disaster on an Alaska Cruise #alaskacruise #travel #shorts

Polar Bears Witness A Sudden Glacier Collapse

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Glacier Calving - Wall collapse and tsunami waves

Glacier Calving - Wall collapse and tsunami waves at Jokulsarlon - Iceland.
04/09/2021

The Epic 4K Glacier Calving Video! #meltingglacier #compilation

Ice calving, also known as glacier calving or iceberg calving, is the breaking of ice chunks from the edge of a glacier. It is a form of ice ablation or ice disruption. It is the sudden release and breaking away of a mass of ice from a glacier, iceberg, ice front, ice shelf, or crevasse. The ice that breaks away can be classified as an iceberg, but may also be a growler, bergy bit, or a crevasse wall breakaway.

Calving of glaciers is often accompanied by a loud cracking or booming sound before blocks of ice up to 60 metres (200 ft) high break loose and crash into the water. The entry of the ice into the water causes large, and often hazardous waves. The waves formed in locations like Johns Hopkins Glacier can be so large that boats cannot approach closer than three kilometres (1+1⁄2 nautical miles). These events have become major tourist attractions in locations such as Alaska.

Many glaciers terminate at oceans or freshwater lakes which results naturally with the calving of large numbers of icebergs. Calving of Greenland's glaciers produce 12,000 to 15,000 icebergs each year alone.

Calving of ice shelves is often preceded by a rift. An ice shelf in steady state calves at roughly the same rate as the influx of new ice, and calving events may occur on subannual to decadal timescales to maintain an overall average mean position of the ice shelf front. When calving rates exceed the influx of new ice, ice front retreat occurs, and ice shelves may grow smaller and weaker.

Calving is when chunks of ice break off at the terminus, or end, of a glacier. Ice breaks because the forward motion of a glacier makes the terminus unstable. We call these resulting chunks of ice icebergs.

Why does Glacier calving happen?

The calving process begins when a rift opens in the edge of a glacier, caused by wind or water erosion, melting ice, or other events that cause the glacier to become unstable. This crack in the ice ultimately causes a block to break away from the land and form an iceberg, which falls into the ocean

Calving: a natural process

The breaking off of icebergs, known as calving, is a normal part of the life of a glacier-fed ice shelf, even when the icebergs calved are massive.

Ilulissat Icefjord


Ilulissat Icefjord where a massive glacial sheet produces more icebergs than any other site except Antarctica.

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75 000 h.p. The Biggest Nuclear Icebreaker

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This video was shot in the Arctic Ocean in March 2018. For 7 days our crew passed through the Barents Sea to Karsky around the Novaya Zemlya archipelago on the nuclear icebreaker Yamal - we saw the northern lights and polar bears, watched the ships stuck in the ice being towed, and were very cold.

In the video you can see two Russian icebreakers - “50 Years of Victory” and “Yamal” with a capacity of 75,000 horsepower and a distinctive shark mouth, which appeared on it in 1994 during one of the children's humanitarian programs. According to legend, someone suggested drawing a smiling shark mouth on the nose to make it more fun for children. At present, Russia has the only nuclear-powered icebreaker fleet in the world. They are used to provide wiring ships in the ices of the Northern Sea Route in the freezing ports of the Russian Federation, research expeditions, rescue operations and tourist cruises.

In addition to the extreme weather conditions, the shooting was complicated by the fact that the icebreaker was always in motion. And if the drone was flying over the radar tower, the recording file was damaged.

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Glacier ice bridge collapses in Perito Moreno, Patagonia, Argentina | Glacier | Shock wave (2/4)

The natural ice bridge in the glacier Perito Moreno in the Patagonia region, Argentina came crashing down and completely collapsed.

An arch forms regularly in a glacier called Perito Moreno as the water flow from a canal eats away at the ice.

For the first time in 16 years, the bridge fell in 2004 and since then it has come down every three to four years of so.

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MEGA-TSUNAMI caused by LANDSLIDE devastates village - Camera 1 | Greenland, Nuugaatsiaq

Shocking video captures the impact when one of the tallest tsunamis recorded in history hits and devastates the village of Nuugaatsiaq (Greenland) in the late evening hours, causing four deaths. Subscribe for extreme nature videos ►

In the evening of June 17th, 2017 (at about 9:40 pm local time), a gigantic landslide (measuring 300 m × 1,100 m = 980 ft × 3,610 ft) occurred on the southern slope of the Umiammakku Nunaat peninsula. Several dozen million cubic meters of rock and slope sediments fell about 1 km (3,300 ft) into the Kangilleq fjord, which triggered a tsunami that moved westward into the Karrat fjord complex. The tsunami wave, which was initially over 90 meters high (about 300 ft.), reached the small village Nuugaatsiaq with a wave height of about ten meters (about 30 ft.). It took the catastrophic tidal wave only seven minutes to cover the 32 kilometers distance to Nuugaatsiaq, which means it reached an average speed of 275 km/h. The tsunami dragged four people out to sea, who have since been considered dead. Furthermore, seven people were slightly injured and two people were seriously injured by the catastrophic natural disaster. Eleven buildings were destroyed. Rescue helicopters brought the approximately 200 local residents to the district capital of Uummannaq.

In 2018, a Swiss company observed the situation and found that the mountain slipped about 1 cm every day and one could expect another landslide at any time. The risk for this was rated at 11.5 out of 12, which is why a resettlement at this time was further excluded. Shortly thereafter it was announced that there was still danger from the mountain slope, making it impossible to end the evacuation. The village of Nuugaatsiaq has since been abandoned.

Was the Greenland tsunami a mega-tsunami? The Greenland tsunami may be considered as mega-tsunami (or impact tsunami) due to its incredible initial wave height of nearly 100 m / + 300 ft. By contrast to ordinary tsunamis, which usually reach an hight of about 30-100 ft., a megatsunami is a tsunami with an initial wave amplitude measured in several tens, hundreds, or possibly thousands of metres. Megatsunamis are caused by giant landslides and other impact events (including meteorite impacts in an ocean), while ordinary tsunamis are usually caused by underwater earthquakes or volcanic eruptions (which do not normally generate such large waves). Other recent megatsunamis include the wave associated with the 1883 eruption of Krakatoa (volcanic eruption), the 1958 Lituya Bay megatsunami (landslide into a bay), and the wave resulting from the Vajont Dam landslide (caused by human activity) (

When comparing this Greenland Tsunami with the 1958 Lituya Bay Mega-tsunami, it seems surprising that the landslide which triggered the Greenland Tsunami was actually even bigger than the landslide which triggered the 1958 Lituya Bay mega-tsunami (45 million m³ which fell about 1 km into the Kangilleq fjord // vs. // 30 million m³ which fell from an elevation of about 900 m into the Lituya Bay). Somehow the Lituya Bay wave ended up being way higher in its max. (+524 m Vs. 100 m). The Greenland Tsunami wave was way faster – it only took 7 minutes to cover the 32 km distance to Nuugaatsiaq (which equals and average speed of about 275 km/h) compared with the speed of the Lituya Bay wave (estimated to only 160-210 hm/h).

Additional information and insights about this Greenland Mega-Tsunami can be found here:

© Licet Studios GmbH, Greenland Mega-Tsunami Devastes Village (A. Larsen) – for further information about us, our content, or licensing / usage inquiries, you may check our website or contact us directly at: licensing@licetstudios.com.

INCREDIBLE GLACIER COLLAPSE IN ARGENTINA | ICE CALVING | NATURE IN 4K #shorts

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Massive Ice Calving at Aialik Glacier - Alaska May 2022

The Aialik Glacier is a glacier in Kenai Fjords National Park. About 15 miles from Seward, it is the largest glacier in Aialik Bay and drains the Harding Icefield. The Harding Icefield, the largest icefield contained entirely within the United States, is over 1,100 square miles and spawns some 40 glaciers. Aialik glacier is generally very stable and such massive calving events are rare. Most calving of the Aialik glacier occurs in May and June.

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