Movie:Braided plain Arctic River: Difference between revisions
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|First name contributor=Joep | |First name contributor=Joep | ||
|Last name contributor=Storms | |Last name contributor=Storms | ||
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|Grade level=Under graduate (13-16), Graduate / Professional | |Grade level=Under graduate (13-16), Graduate / Professional | ||
|One-line movie description=Braided river darining West Greenland Ice Sheet | |One-line movie description=Braided river darining West Greenland Ice Sheet | ||
|Extended movie description=Rivers draining the West Greenland Ice Sheet are highly dynamic braided rivers. The water is of a milky color, because of the glacial flour it carries in suspension. In addition, the flow velocities are high and sound of coarse, cobble-sized bedload clashing into each other at the bed is evident. Banks and bars consist of a mix of cobbles, pebbles and fine sandy to silty material. The river is shallow. | |Extended movie description=Rivers draining the West Greenland Ice Sheet are highly dynamic braided rivers. The water is of a milky color, because of the glacial flour it carries in suspension. In addition, the flow velocities are high and sound of coarse, cobble-sized bedload clashing into each other at the bed is evident. Banks and bars consist of a mix of cobbles, pebbles and fine sandy to silty material. The river is shallow. | ||
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{{Movie theory2}} | {{Movie theory2}} | ||
{{Movie references2}} | {{Movie references2}} | ||
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Revision as of 11:21, 19 June 2013
Information Page: Braided plain Arctic River
Play Movie
Braidplain of Arctic River
Key Attributes
| Domain: | terrestrial, hydrology |
| Keywords: | Braided River |
| Keywords: | Arctic River |
| Model name: | |
| Name: | Joep, Storms |
| Where: | West Greenland |
| When: | seconds |
Short Description
Grade level: Under graduate (13-16), Graduate / Professional
Statement: Braided river darining West Greenland Ice Sheet
Abstract: Rivers draining the West Greenland Ice Sheet are highly dynamic braided rivers. The water is of a milky color, because of the glacial flour it carries in suspension. In addition, the flow velocities are high and sound of coarse, cobble-sized bedload clashing into each other at the bed is evident. Banks and bars consist of a mix of cobbles, pebbles and fine sandy to silty material. The river is shallow.
Theory
Links
References
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