Movie:Braided Stream Morphology: Difference between revisions
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{{Movie description | {{Movie description | ||
|Grade level=Middle (6-8), High (9-12), Under graduate (13-16) | |Grade level=Middle (6-8), High (9-12), Under graduate (13-16) | ||
|One-line movie description=Braided Stream Morphology | |One-line movie description = Braided Stream Morphology | ||
|Extended movie description=This movie shows a small part of experiment XES 99-1 on braided streams. The basin in this experiment is 3 meters wide and 6 meters long. Sediment and water enter the basin from four input sites at the top of the basin. The auto cyclic events present in the movie are labeled. They include avulsion, lateral sweeping, channel expansion events, bar migration and nickpoint retreat. | |Extended movie description=This movie shows a small part of experiment XES 99-1 on braided streams. The basin in this experiment is 3 meters wide and 6 meters long. Sediment and water enter the basin from four input sites at the top of the basin. The auto cyclic events present in the movie are labeled. They include avulsion, lateral sweeping, channel expansion events, bar migration and nickpoint retreat. | ||
}} | }} |
Revision as of 13:34, 1 June 2015
Information Page: Braided Stream Morphology
Play Laboratory
Key Attributes
Domain: | terrestrial |
Keywords: | stream channel |
Keywords: | fluvial |
Keywords: | morphology |
Model name: | |
Name: | Chris, Paola |
Where: | - |
When: | - |
Short Description
Grade level: Middle (6-8), High (9-12), Under graduate (13-16)
Statement: Braided Stream Morphology
Abstract: This movie shows a small part of experiment XES 99-1 on braided streams. The basin in this experiment is 3 meters wide and 6 meters long. Sediment and water enter the basin from four input sites at the top of the basin. The auto cyclic events present in the movie are labeled. They include avulsion, lateral sweeping, channel expansion events, bar migration and nickpoint retreat.
Theory
Braided steams can occur in drainage basins that have high sediment content and/or in river environments that rapidly change channel depth and thus velocity such as alluvial fans, river deltas and peneplains.
Links
References
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