Thermal Convection in Ice Sheets: We Look But Do Not See

Thermal convection in the Antarctic and Greenland ice sheets has been dismissed on the grounds that radio-echo stratigraphy is undisturbed for long distances. However, the undisturbed stratigraphy lies, for the most part, above the density inversion in polar ice sheets and therefore does not disprov...

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Bibliographic Details
Main Author: Hughes, Terence J.
Format: Text
Language:unknown
Published: DigitalCommons@UMaine 1985
Subjects:
Online Access:https://digitalcommons.library.umaine.edu/ers_facpub/110
https://digitalcommons.library.umaine.edu/cgi/viewcontent.cgi?article=1109&context=ers_facpub