Movie:Shelf Incision: Difference between revisions

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{{Attribute movie3
{{Attribute movie3
|Animation model name=DELIM, fluvial-coastal evolution model  
|Animation model name=DELIM, fluvial-coastal evolution model
|First name contributor=Sergio
|First name contributor=Sergio
|Last name contributor=Fagherazzi  
|Last name contributor=Fagherazzi
|Location movie=North America
|Location movie=North America
|Timespan movie=glacial-interglacial sea level cycle
|Timespan movie=glacial-interglacial sea level cycle
Line 21: Line 21:
|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.
}}
{{Movie theory2
|Theory movie=Fluvial coastal reworking as a result of sea level change in glacial-interglacial time periods.
}}
}}
{{Movie theory2}}
{{Movie references2}}
{{Movie references2}}

Revision as of 13:34, 16 August 2010

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