Movie:Sand Boil behind Levee: Difference between revisions

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{{Movie description
{{Movie description
|Grade level=Middle (6-8), High (9-12), Under graduate (13-16), Graduate / Professional
|Grade level=Middle (6-8), High (9-12), Under graduate (13-16), Graduate / Professional
|One-line movie description=sand boil results from seepage under levee
|One-line movie description = sand boil results from seepage under levee
|Extended movie description=This show the bubbling of sand near a levee in the lowlying farmlands, the sand seepage results from the  pressure gradient that is caused by high river stage in flood conditions. This example is near Bennington Levee, Indiana, where the White River was at flood stage in March 2011.  
|Extended movie description=This show the bubbling of sand near a levee in the lowlying farmlands, the sand seepage results from the  pressure gradient that is caused by high river stage in flood conditions. This example is near Bennington Levee, Indiana, where the White River was at flood stage in March 2011.  
The sand boil was an indicator of the underminng of the levee and a 25 ft breach did happen during this same flood.
The sand boil was an indicator of the underminng of the levee and a 25 ft breach did happen during this same flood.

Revision as of 13:34, 1 June 2015

Information Page: Sand Boil behind Levee

Play Movie


Sand Boil near Levee



Key Attributes

Domain: terrestrial, hydrology
Keywords: levee
Keywords: groundwater
Keywords: seepage
Keywords: flood risk
Model name:
Name: Chris, Lee fish
Where: Bennington Levee
When: March 2011


Short Description

Grade level: Middle (6-8), High (9-12), Under graduate (13-16), Graduate / Professional

Statement: sand boil results from seepage under levee

Abstract: This show the bubbling of sand near a levee in the lowlying farmlands, the sand seepage results from the pressure gradient that is caused by high river stage in flood conditions. This example is near Bennington Levee, Indiana, where the White River was at flood stage in March 2011. The sand boil was an indicator of the underminng of the levee and a 25 ft breach did happen during this same flood.

Theory

High river water that does not overtop a levee yet, can still create a tremendous water pressure. This pressure creates a potential for groundwater seepage of the water, through the underlying, permeable aquifer into the lowlands that are protected from direct flooding by an largely impermeable levee. Sand and water start bubbling up on the floodplain; usually indicating that undermining of the levee is going on.

Links

References



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