Movie:Shelf Incision: Difference between revisions
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{{Movie description | {{Movie description | ||
|Grade level=Graduate / Professional | |Grade level=Graduate / Professional | ||
|One-line movie description=Simulation of fluvial incision in the shelf | |One-line movie description = Simulation of fluvial incision in the shelf | ||
|Extended movie description=Simulation of fluvial incision in the shelf during a glacial-interglacial sea level cycle. This simulation represents the East Coast of the US, i.e. close to Chesapeak Bay and Delaware Bay. During lowstand, at glacial maximum the entire shelf is actively incised and reworked by fluvial systems. | |Extended movie description=Simulation of fluvial incision in the shelf during a glacial-interglacial sea level cycle. This simulation represents the East Coast of the US, i.e. close to Chesapeak Bay and Delaware Bay. During lowstand, at glacial maximum the entire shelf is actively incised and reworked by fluvial systems. | ||
}} | }} | ||
Revision as of 13:30, 1 June 2015
Information Page: Shelf Incision
Play Animation
Lowstand Shelf Evolution
Key Attributes
| Domain: | coastal |
| Keywords: | Lowstand Shelf Evolution |
| Model name: | DELIM, fluvial-coastal evolution model |
| Name: | Sergio, Fagherazzi |
| Where: | North America |
| When: | glacial-interglacial sea level cycle |
Short Description
Grade level: Graduate / Professional
Statement: Simulation of fluvial incision in the shelf
Abstract: Simulation of fluvial incision in the shelf during a glacial-interglacial sea level cycle. This simulation represents the East Coast of the US, i.e. close to Chesapeak Bay and Delaware Bay. During lowstand, at glacial maximum the entire shelf is actively incised and reworked by fluvial systems.
Theory
Fluvial coastal reworking as a result of sea level change in glacial-interglacial time periods.
Links
References
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