Movie:River incision dominated by fault block: Difference between revisions
m Text replacement - "Last name contributor=" to "Last name contributor =" |
m Text replacement - "Movie keywords=" to "Movie keywords = " |
||
Line 9: | Line 9: | ||
}} | }} | ||
{{Attribute movie2 | {{Attribute movie2 | ||
|Movie keywords=River Incision | |Movie keywords = River Incision | ||
}} | }} | ||
{{Attribute movie2 | {{Attribute movie2 | ||
|Movie keywords=Landscape Evolution Model | |Movie keywords = Landscape Evolution Model | ||
}} | }} | ||
{{Attribute movie3 | {{Attribute movie3 |
Revision as of 13:57, 1 June 2015
Information Page: River incision dominated by fault block
Play Animation
Incision in Fault Block Zone
Key Attributes
Domain: | terrestrial |
Keywords: | River Incision |
Keywords: | Landscape Evolution Model |
Model name: | CHILD |
Name: | Greg, Tucker |
Where: | -- |
When: | -- |
Short Description
Grade level: Graduate / Professional
Statement: landscape evolution dominated by fault blocks
Abstract: This movie shows a simulation of a pair of normal-fault blocks separated by a vertical fault. The lower left edge is fixed through time, and represents a shallow shelf just below sea level. The inner block of the landscape rises at a steady rate, while the outer block subsides. Initially, the relief and erosion rate are small, and the subsiding basin is underfilled. Notice the progradation of a fan-delta complex. As relief and sediment flux increase, the fan deltas reach the shallow shelf and the basin becomes filled (or "over-filled" , meaning that there is more than enough sediment to keep filling the basin as it continues to subside).
Theory
Links
References
The part "]]" of the query was not understood.</br>Results might not be as expected.