BLISTER DIAGRAM (IMAGE)
Caption
Meltwater-filled cavities push the surface of the ice sheet upward (left), then cause it to gradually drop down (right) as the water permeates the subglacial drainage system. This rise and fall can be used to estimate a property of the subglacial drainage system known as transmissivity.
Credit
Image by Ching-Yao Lai, Department of Geosciences
Usage Restrictions
None.
License
Original content