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Northern edge of Iceberg B-15A in the Ross Sea, Antarctica, 29 January 2001. Iceberg B-15 was the largest recorded iceberg by area. [Note 1] It measured around 295 by 37 kilometres (159 by 20 nautical miles), with a surface area of 11,000 square kilometres (3,200 square nautical miles), about the size of the island of Jamaica.
An iceberg is a piece of fresh water ice more than 15 meters (16 yards) long [1] that has broken off a glacier or an ice shelf and is floating freely in open water. [2] [3] Smaller chunks of floating glacially derived ice are called "growlers" or "bergy bits".
For size comparison, the Titanic, the largest ship in the world at the time, had a total length of 882 feet and 9 inches (around 269 metres). She was up to 92 feet and 6 inches wide (about 28 metres). Her draught (from waterline to keel) was 34 feet and 6 inches (about 10 metres) in front. [36]
The melting of Alaska's Juneau icefield, home to more than 1,000 glaciers, is accelerating. It slowly shriveled from its peak size at the end of the Little Ice Age around 1850, but then that melt ...
Pillow drift – A pillow drift is a snow drift crossing a roadway and usually 3 to 4.5 metres (10–15 feet) in width and 30 cm to 90 cm (1–3 feet) in depth. [ 28 ] Sastrugi – Sastrugi are snow surface features sculpted by wind into ridges and grooves up to 3 meters high, [ 29 ] with the ridges facing into the prevailing wind.
The storm will impact about 200,000 square miles with snowfall rates of 1 to 2 inches per hour in some areas. ... 3 pounds, while a cubic foot of heavy, wet snow can weigh as much as 10 pounds ...
On the other hand, the East Antarctic ice sheet is far more stable and may only cause 0.5 m (1 ft 8 in) - 0.9 m (2 ft 11 in) of sea level rise from the current level of warming, which is a small fraction of the 53.3 m (175 ft) contained in the full ice sheet. Around 3 °C (5.4 °F), vulnerable locations like Wilkes Basin and Aurora Basin may ...
Most lakes in the world occupy basins scoured out by glaciers. Glacial motion can be fast (up to 30 metres per day (98 ft/d), observed on Jakobshavn Isbræ in Greenland) [1] or slow (0.5 metres per year (20 in/year) on small glaciers or in the center of ice sheets), but is typically around 25 centimetres per day (9.8 in/d). [2]
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