Landsat recently captured the most widespread meltwater pooling ever recorded on Antarctica's George VI Ice Shelf. Some melting is expected during the Antarctic summer, but the sheer extent of the stunning aqua ponds that have appeared amid the continent's warmest summer on record is remarkable.
Where are Earth’s glaciers located?
Glaciers exist on every continent except Australia. Approximate distribution is:
- 91% in Antarctica
- 8% in Greenland
- Less than 0.5% in North America (about 0.1% in Alaska)
- 0.2% in Asia
- Less than 0.1% are in South America, Europe, Africa, New Zealand, and Indonesia.
Related
How long can we expect the present Interglacial period to last? How long can we expect the present Interglacial period to last?
No one knows for sure. In the Devils Hole, Nevada paleoclimate record, the last four interglacials lasted over ~20,000 years with the warmest portion being a relatively stable period of 10,000 to 15,000 years duration. This is consistent with what is seen in the Vostok ice core from Antarctica and several records of sea level high stands. These data suggest that an equally long duration should be...
How old is glacier ice? How old is glacier ice?
The age of the oldest glacier ice in Antarctica may approach 1,000,000 years old The age of the oldest glacier ice in Greenland is more than 100,000 years old The age of the oldest Alaskan glacier ice ever recovered (from a basin between Mt. Bona and Mt. Churchill) is about 30,000 years old. Glacier flow moves newly formed ice through the entire length of a typical Alaskan valley glacier in 100...
Do ice worms exist? Do ice worms exist?
Yes, ice worms do, in fact, exist! They are small worms that live in glacial ice in Alaska, Washington, Oregon, and British Columbia; they have not been found in glaciers elsewhere. Contrary to stories and songs, they do not give glacier ice its blue color and they don't grow to lengths of 50 feet. These myths were made popular by poet Robert Service and the annual Cordova Iceworm Festival in...
Is glacier ice a type of rock? Is glacier ice a type of rock?
Glacier ice, like limestone (for example), is a type of rock. Glacier ice is actually a mono-mineralic rock (a rock made of only one mineral, like limestone which is composed of the mineral calcite). The mineral ice is the crystalline form of water (H 2O). Most glacier ice forms through the metamorphism of tens of thousands of individual snowflakes into crystals of glacier ice. Each snowflake is a...
Why is glacier ice blue? Why is glacier ice blue?
Glacier ice is blue because the red (long wavelengths) part of white light is absorbed by ice and the blue (short wavelengths) light is transmitted and scattered. The longer the path light travels in ice, the more blue it appears. Learn more: USGS Water Science School - Glaciers: Things to Know
Where are glaciers found in continental North America? Where are glaciers found in continental North America?
Glaciers exist in both the United States and Canada. Most U.S. glaciers are in Alaska; others can be found in Washington, Oregon, California, Montana, Wyoming, Colorado, and Nevada (Wheeler Peak Glacier in Great Basin National Park). Utah’s Timpanogos Glacier is now a rock glacier (in which the ice is hidden by rocks), and Idaho’s Otto Glacier has melted away. Canada has glaciers in Alberta...
How does present glacier extent and sea level compare to the extent of glaciers and global sea level during the Last Glacial Maximum (LGM)? How does present glacier extent and sea level compare to the extent of glaciers and global sea level during the Last Glacial Maximum (LGM)?
The Last Glacial Maximum (LGM) occurred about 20,000 years ago, during the last phase of the Pleistocene epoch. At that time, global sea level was more than 400 feet lower than it is today, and glaciers covered approximately: 8% of Earth’s surface 25% of Earth’s land area 33% of Alaska Beginning about 15,000 years ago, continental glaciers retreated and sea level began to rise. Sea level reached...
How would sea level change if all glaciers melted? How would sea level change if all glaciers melted?
There is still some uncertainty about the full volume of glaciers and ice caps on Earth, but if all of them were to melt, global sea level would rise approximately 70 meters (approximately 230 feet), flooding every coastal city on the planet. Learn more: USGS Water Science School: Glaciers and Icecaps National Snow and Ice Data Center: Facts about Glaciers U.S. Global Change Research Program: Sea...
What are the impacts of glacier loss, other than losing an aesthetic landscape feature? What are the impacts of glacier loss, other than losing an aesthetic landscape feature?
Glaciers act as reservoirs of water that persist through summer. Continual melt from glaciers contributes water to the ecosystem throughout dry months, creating perennial stream habitat and a water source for plants and animals. The cold runoff from glaciers also affects downstream water temperatures. Many aquatic species in mountainous environments require cold water temperatures to survive. Some...
What is a glacier? What is a glacier?
A glacier is a large, perennial accumulation of crystalline ice, snow, rock, sediment, and often liquid water that originates on land and moves down slope under the influence of its own weight and gravity. Typically, glaciers exist and may even form in areas where: mean annual temperatures are close to the freezing point winter precipitation produces significant accumulations of snow temperatures...
Landsat recently captured the most widespread meltwater pooling ever recorded on Antarctica's George VI Ice Shelf. Some melting is expected during the Antarctic summer, but the sheer extent of the stunning aqua ponds that have appeared amid the continent's warmest summer on record is remarkable.
Meltwater lakes form on the surface of Greenland’s Petermann Glacier
Meltwater lakes form on the surface of Greenland’s Petermann GlacierMeltwater lakes form on the surface of Greenland’s Petermann Glacier, seen here in a June 2019 Landsat image. A new study finds that the number, and elevation, of meltwater lakes in Greenalnd is increasing. Credit: NASA/USGS
Meltwater lakes form on the surface of Greenland’s Petermann Glacier
Meltwater lakes form on the surface of Greenland’s Petermann GlacierMeltwater lakes form on the surface of Greenland’s Petermann Glacier, seen here in a June 2019 Landsat image. A new study finds that the number, and elevation, of meltwater lakes in Greenalnd is increasing. Credit: NASA/USGS
Mapping the glacier's edge in Glacier National Park.
Mapping the glacier's edge in Glacier National Park.Mapping the glacier's edge in Glacier National Park.
Mapping the glacier's edge in Glacier National Park.
Mapping the glacier's edge in Glacier National Park.Mapping the glacier's edge in Glacier National Park.
A scientist hikes up to a glacier in Glacier National Park.
A scientist hikes up to a glacier in Glacier National Park.A scientist hikes up to a glacier in Glacier National Park.
A scientist hikes up to a glacier in Glacier National Park.
A scientist hikes up to a glacier in Glacier National Park.A scientist hikes up to a glacier in Glacier National Park.
Sheridan glacier and Sheridan river from the air, rich in fine glacial flour.
Sheridan glacier and Sheridan river from the air, rich in fine glacial flour.
video thumbnail: USGS Public Lecture Series: Baked Alaska--What's Happening to the Glaciers in Alaska?
USGS Public Lecture Series: Baked Alaska--What's Happening to the Glaciers in Alaska?
USGS Public Lecture Series: Baked Alaska--What's Happening to the Glaciers in Alaska?Glaciers are Earth's largest reservoir of freshwater. As they change, so does global sea level. Alaska has one of the largest accumulations of glaciers anywhere on Earth outside of the Polar regions. For most of the past half century, Alaska has experienced a significant increase in temperature that has profoundly impacted its glaciers. Join USGS scientist Dr.
USGS Public Lecture Series: Baked Alaska--What's Happening to the Glaciers in Alaska?
USGS Public Lecture Series: Baked Alaska--What's Happening to the Glaciers in Alaska?Glaciers are Earth's largest reservoir of freshwater. As they change, so does global sea level. Alaska has one of the largest accumulations of glaciers anywhere on Earth outside of the Polar regions. For most of the past half century, Alaska has experienced a significant increase in temperature that has profoundly impacted its glaciers. Join USGS scientist Dr.
Most glaciers in Washington and Alaska are dramatically shrinking in response to a warming climate.
Most glaciers in Washington and Alaska are dramatically shrinking in response to a warming climate.
Surprise Glacier, Harriman Fiord, western Prince William Sound.
Surprise Glacier, Harriman Fiord, western Prince William Sound.
Serpentine Glacier, Harriman Fiord, western Prince William Sound, AK.
Serpentine Glacier, Harriman Fiord, western Prince William Sound, AK.
Coxe Glacier, Barry Arm, western Prince William Sound
Coxe Glacier, Barry Arm, western Prince William Sound
Upper slopes of Glacier Peak, Washington.
Upper slopes of Glacier Peak, Washington.
Peter Haeussler prepares to measure the offset of a crevasse on the Canwell Glacier.
Peter Haeussler prepares to measure the offset of a crevasse on the Canwell Glacier.
Soaring, snow-capped peaks and ridges of the eastern Himalaya Mountains create an irregular white-on-red patchwork between major rivers in southwestern China. The Himalayas are made up of three parallel mountain ranges that together extend more than 2,900 kilometers.
Soaring, snow-capped peaks and ridges of the eastern Himalaya Mountains create an irregular white-on-red patchwork between major rivers in southwestern China. The Himalayas are made up of three parallel mountain ranges that together extend more than 2,900 kilometers.
This picture was taken from the base of the Hayden Glacier in the Three Sisters Wilderness Area.
This picture was taken from the base of the Hayden Glacier in the Three Sisters Wilderness Area.
Cryospheric sciences at the U.S. Geological Survey Cryospheric sciences at the U.S. Geological Survey
Sculpted by water, elevated by earthquakes—The coastal landscape of Glacier Bay National Park, Alaska Sculpted by water, elevated by earthquakes—The coastal landscape of Glacier Bay National Park, Alaska
The United States National Climate Assessment - Alaska Technical Regional Report The United States National Climate Assessment - Alaska Technical Regional Report
State of the Earth’s cryosphere at the beginning of the 21st century: Glaciers, global snow cover, floating ice, and permafrost and periglacial environments State of the Earth’s cryosphere at the beginning of the 21st century: Glaciers, global snow cover, floating ice, and permafrost and periglacial environments
Glaciers of Asia Glaciers of Asia
Fifty-year record of glacier change reveals shifting climate in the Pacific Northwest and Alaska, USA Fifty-year record of glacier change reveals shifting climate in the Pacific Northwest and Alaska, USA
Satellite Image Atlas of Glaciers of the World Satellite Image Atlas of Glaciers of the World
Satellite image atlas of glaciers of the world — North America Satellite image atlas of glaciers of the world — North America
Satellite image atlas of glaciers of the world Satellite image atlas of glaciers of the world
Related
How long can we expect the present Interglacial period to last? How long can we expect the present Interglacial period to last?
No one knows for sure. In the Devils Hole, Nevada paleoclimate record, the last four interglacials lasted over ~20,000 years with the warmest portion being a relatively stable period of 10,000 to 15,000 years duration. This is consistent with what is seen in the Vostok ice core from Antarctica and several records of sea level high stands. These data suggest that an equally long duration should be...
How old is glacier ice? How old is glacier ice?
The age of the oldest glacier ice in Antarctica may approach 1,000,000 years old The age of the oldest glacier ice in Greenland is more than 100,000 years old The age of the oldest Alaskan glacier ice ever recovered (from a basin between Mt. Bona and Mt. Churchill) is about 30,000 years old. Glacier flow moves newly formed ice through the entire length of a typical Alaskan valley glacier in 100...
Do ice worms exist? Do ice worms exist?
Yes, ice worms do, in fact, exist! They are small worms that live in glacial ice in Alaska, Washington, Oregon, and British Columbia; they have not been found in glaciers elsewhere. Contrary to stories and songs, they do not give glacier ice its blue color and they don't grow to lengths of 50 feet. These myths were made popular by poet Robert Service and the annual Cordova Iceworm Festival in...
Is glacier ice a type of rock? Is glacier ice a type of rock?
Glacier ice, like limestone (for example), is a type of rock. Glacier ice is actually a mono-mineralic rock (a rock made of only one mineral, like limestone which is composed of the mineral calcite). The mineral ice is the crystalline form of water (H 2O). Most glacier ice forms through the metamorphism of tens of thousands of individual snowflakes into crystals of glacier ice. Each snowflake is a...
Why is glacier ice blue? Why is glacier ice blue?
Glacier ice is blue because the red (long wavelengths) part of white light is absorbed by ice and the blue (short wavelengths) light is transmitted and scattered. The longer the path light travels in ice, the more blue it appears. Learn more: USGS Water Science School - Glaciers: Things to Know
Where are glaciers found in continental North America? Where are glaciers found in continental North America?
Glaciers exist in both the United States and Canada. Most U.S. glaciers are in Alaska; others can be found in Washington, Oregon, California, Montana, Wyoming, Colorado, and Nevada (Wheeler Peak Glacier in Great Basin National Park). Utah’s Timpanogos Glacier is now a rock glacier (in which the ice is hidden by rocks), and Idaho’s Otto Glacier has melted away. Canada has glaciers in Alberta...
How does present glacier extent and sea level compare to the extent of glaciers and global sea level during the Last Glacial Maximum (LGM)? How does present glacier extent and sea level compare to the extent of glaciers and global sea level during the Last Glacial Maximum (LGM)?
The Last Glacial Maximum (LGM) occurred about 20,000 years ago, during the last phase of the Pleistocene epoch. At that time, global sea level was more than 400 feet lower than it is today, and glaciers covered approximately: 8% of Earth’s surface 25% of Earth’s land area 33% of Alaska Beginning about 15,000 years ago, continental glaciers retreated and sea level began to rise. Sea level reached...
How would sea level change if all glaciers melted? How would sea level change if all glaciers melted?
There is still some uncertainty about the full volume of glaciers and ice caps on Earth, but if all of them were to melt, global sea level would rise approximately 70 meters (approximately 230 feet), flooding every coastal city on the planet. Learn more: USGS Water Science School: Glaciers and Icecaps National Snow and Ice Data Center: Facts about Glaciers U.S. Global Change Research Program: Sea...
What are the impacts of glacier loss, other than losing an aesthetic landscape feature? What are the impacts of glacier loss, other than losing an aesthetic landscape feature?
Glaciers act as reservoirs of water that persist through summer. Continual melt from glaciers contributes water to the ecosystem throughout dry months, creating perennial stream habitat and a water source for plants and animals. The cold runoff from glaciers also affects downstream water temperatures. Many aquatic species in mountainous environments require cold water temperatures to survive. Some...
What is a glacier? What is a glacier?
A glacier is a large, perennial accumulation of crystalline ice, snow, rock, sediment, and often liquid water that originates on land and moves down slope under the influence of its own weight and gravity. Typically, glaciers exist and may even form in areas where: mean annual temperatures are close to the freezing point winter precipitation produces significant accumulations of snow temperatures...
Landsat recently captured the most widespread meltwater pooling ever recorded on Antarctica's George VI Ice Shelf. Some melting is expected during the Antarctic summer, but the sheer extent of the stunning aqua ponds that have appeared amid the continent's warmest summer on record is remarkable.
Landsat recently captured the most widespread meltwater pooling ever recorded on Antarctica's George VI Ice Shelf. Some melting is expected during the Antarctic summer, but the sheer extent of the stunning aqua ponds that have appeared amid the continent's warmest summer on record is remarkable.
Meltwater lakes form on the surface of Greenland’s Petermann Glacier
Meltwater lakes form on the surface of Greenland’s Petermann GlacierMeltwater lakes form on the surface of Greenland’s Petermann Glacier, seen here in a June 2019 Landsat image. A new study finds that the number, and elevation, of meltwater lakes in Greenalnd is increasing. Credit: NASA/USGS
Meltwater lakes form on the surface of Greenland’s Petermann Glacier
Meltwater lakes form on the surface of Greenland’s Petermann GlacierMeltwater lakes form on the surface of Greenland’s Petermann Glacier, seen here in a June 2019 Landsat image. A new study finds that the number, and elevation, of meltwater lakes in Greenalnd is increasing. Credit: NASA/USGS
Mapping the glacier's edge in Glacier National Park.
Mapping the glacier's edge in Glacier National Park.Mapping the glacier's edge in Glacier National Park.
Mapping the glacier's edge in Glacier National Park.
Mapping the glacier's edge in Glacier National Park.Mapping the glacier's edge in Glacier National Park.
A scientist hikes up to a glacier in Glacier National Park.
A scientist hikes up to a glacier in Glacier National Park.A scientist hikes up to a glacier in Glacier National Park.
A scientist hikes up to a glacier in Glacier National Park.
A scientist hikes up to a glacier in Glacier National Park.A scientist hikes up to a glacier in Glacier National Park.
Sheridan glacier and Sheridan river from the air, rich in fine glacial flour.
Sheridan glacier and Sheridan river from the air, rich in fine glacial flour.
video thumbnail: USGS Public Lecture Series: Baked Alaska--What's Happening to the Glaciers in Alaska?
USGS Public Lecture Series: Baked Alaska--What's Happening to the Glaciers in Alaska?
USGS Public Lecture Series: Baked Alaska--What's Happening to the Glaciers in Alaska?Glaciers are Earth's largest reservoir of freshwater. As they change, so does global sea level. Alaska has one of the largest accumulations of glaciers anywhere on Earth outside of the Polar regions. For most of the past half century, Alaska has experienced a significant increase in temperature that has profoundly impacted its glaciers. Join USGS scientist Dr.
USGS Public Lecture Series: Baked Alaska--What's Happening to the Glaciers in Alaska?
USGS Public Lecture Series: Baked Alaska--What's Happening to the Glaciers in Alaska?Glaciers are Earth's largest reservoir of freshwater. As they change, so does global sea level. Alaska has one of the largest accumulations of glaciers anywhere on Earth outside of the Polar regions. For most of the past half century, Alaska has experienced a significant increase in temperature that has profoundly impacted its glaciers. Join USGS scientist Dr.
Most glaciers in Washington and Alaska are dramatically shrinking in response to a warming climate.
Most glaciers in Washington and Alaska are dramatically shrinking in response to a warming climate.
Surprise Glacier, Harriman Fiord, western Prince William Sound.
Surprise Glacier, Harriman Fiord, western Prince William Sound.
Serpentine Glacier, Harriman Fiord, western Prince William Sound, AK.
Serpentine Glacier, Harriman Fiord, western Prince William Sound, AK.
Coxe Glacier, Barry Arm, western Prince William Sound
Coxe Glacier, Barry Arm, western Prince William Sound
Upper slopes of Glacier Peak, Washington.
Upper slopes of Glacier Peak, Washington.
Peter Haeussler prepares to measure the offset of a crevasse on the Canwell Glacier.
Peter Haeussler prepares to measure the offset of a crevasse on the Canwell Glacier.
Soaring, snow-capped peaks and ridges of the eastern Himalaya Mountains create an irregular white-on-red patchwork between major rivers in southwestern China. The Himalayas are made up of three parallel mountain ranges that together extend more than 2,900 kilometers.
Soaring, snow-capped peaks and ridges of the eastern Himalaya Mountains create an irregular white-on-red patchwork between major rivers in southwestern China. The Himalayas are made up of three parallel mountain ranges that together extend more than 2,900 kilometers.
This picture was taken from the base of the Hayden Glacier in the Three Sisters Wilderness Area.
This picture was taken from the base of the Hayden Glacier in the Three Sisters Wilderness Area.