Movie:Braided Streams in a fan-delta: Difference between revisions
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|Grade level=High (9-12), Under graduate (13-16) | |Grade level=High (9-12), Under graduate (13-16) | ||
|One-line movie description=Braided Streams in a fan delta | |One-line movie description = Braided Streams in a fan delta | ||
|Extended movie description=Emplacement of the topset by braided streams in an experimental fan-delta undergoing subsidence. Most significant alluvial processes are labeled. | |Extended movie description=Emplacement of the topset by braided streams in an experimental fan-delta undergoing subsidence. Most significant alluvial processes are labeled. | ||
}} | }} | ||
Revision as of 13:23, 1 June 2015
Information Page: Braided Streams in a fan-delta
Play Laboratory
Key Attributes
| Domain: | terrestrial |
| Keywords: | stream channel |
| Keywords: | fluvial |
| Keywords: | morphology |
| Keywords: | delta |
| Model name: | |
| Name: | Gary, Parker |
| Where: | - |
| When: | - |
Short Description
Grade level: High (9-12), Under graduate (13-16)
Statement: Braided Streams in a fan delta
Abstract: Emplacement of the topset by braided streams in an experimental fan-delta undergoing subsidence. Most significant alluvial processes are labeled.
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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