Movie:Braided Streams in a fan-delta: Difference between revisions
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|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. | ||
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{{Movie theory2}} | {{Movie theory2 | ||
|Theory movie=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. | |||
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{{Movie references2}} | {{Movie references2}} | ||
Revision as of 13:06, 19 August 2010
Information Page: Braided Streams in a fan-delta
Play Laboratory
Key Attributes
| Domain: | terrestrial |
| Model name: | Animation 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.
