Movie:Braided Streams in a fan-delta: Difference between revisions
From CSDMS
Watermann1 (talk | contribs) No edit summary |
No edit summary |
||
| Line 1: | Line 1: | ||
{{Upload movie | {{Upload movie | ||
|Movie type=Laboratory | |Movie type=Laboratory | ||
|Upload movie= | |Upload movie=Es2BdQXToqY | ||
|Upload image movie=XESbasin.jpg | |Upload image movie=XESbasin.jpg | ||
}} | }} | ||
Revision as of 08:47, 5 January 2011
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: | 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.
