Infinite photos and videos for every Wiki article · Find something interesting to watch in seconds
History
Page
View of the Larsen Ice Shelf grounding line between Mamelon Point and Hodges Point along the Foyn Coast of the Antarctic Peninsula. The floating ice s
View of the Larsen Ice Shelf grounding line between Mamelon Point and Hodges Point along the Foyn Coast of the Antarctic Peninsula. The floating ice shelf is in the left foreground, and the grounding line is visible as an abrupt change in surface slope due to flexure caused by the buoyancy force where the ice reaches flotation.
Some named Antarctic iceshelves.
Some named Antarctic iceshelves.
Ice shelf extending approximately 6 miles into the Antarctic Sound from Joinville Island
Ice shelf extending approximately 6 miles into the Antarctic Sound from Joinville Island
Panorama of Ross Ice Shelf
Panorama of Ross Ice Shelf
Page
An ice block, photographed at the Duluth Canal Park in Minnesota
An ice block, photographed at the Duluth Canal Park in Minnesota
This iceberg can stay afloat in spite of its size because it is less dense than water
This iceberg can stay afloat in spite of its size because it is less dense than water
So-called feather ice on the plateau near Alta, Norway. The crystals form at temperatures below −30 °C (−22 °F) and contain a lot of trapped air, maki
So-called feather ice on the plateau near Alta, Norway. The crystals form at temperatures below −30 °C (−22 °F) and contain a lot of trapped air, making them light enough to be supported by the thin branch
Frozen waterfall in southeast New York
Frozen waterfall in southeast New York