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An ice stream is a region of fast-moving ice within an ice sheet. It is a type of glacier, a body of ice that moves under its own weight. They can move upwards of 1,000 metres (3,300 ft) a year, and can be up to 50 kilometres (31 mi) in width, and hundreds of kilometers in length. They tend to be about 2 km (1.2 mi) deep at the thickest, and constitute…
Regions, Antarctica & Mechanics
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| Subject | Predicate | Object | Confidence | Src |
|---|---|---|---|---|
| Ice stream | is a | region of fast-moving ice within an ice sheet | 0.90 | text |
| bathymetric troughs indicate where paleo-ice streams in Antarctica extended during the Last Glacial Maximum | instance of | Geomorphic features | 0.80 | text |
| bed characteristic | instance of | this reinforces the importance of internal factors | 0.80 | text |
| slope | instance of | this reinforces the importance of internal factors | 0.80 | text |
| and drainage basin size in determining ice stream dynamics | instance of | this reinforces the importance of internal factors | 0.80 | text |
| Ice stream | related to Antarctica | The Antarctic Ice Sheet | 0.60 | section |
| Ice stream | related to Antarctica | The | 0.60 | section |
| Ice stream | related to Antarctica | East Antarctica | 0.60 | section |
| Ice stream | related to Antarctica | Lambert Glacier | 0.60 | section |
| Ice stream | related to Antarctica | In West Antarctica | 0.60 | section |
| Ice stream | related to Antarctica | Pine Island | 0.60 | section |
| Ice stream | related to Antarctica | Thwaites Glaciers | 0.60 | section |
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