We interpret high spatial variability of bedforms as indicating a complex mechanical and hydrodynamic regime at the former
ice stream beds, consistent with observations from some modern ice streams.
Data from modern
ice stream beds are difficult to obtain, but where ice advanced onto continental shelves during glacial periods, extensive areas of the former bed can be imaged using modern swath sonar tools.
Not exact matches
Pictures from Huygens show cobbles of
ice that resemble water - worn rocks on a terrestrial
stream bed.
«It was literally one of the first days that we were driving across the
ice stream, doing what we thought was a pretty standard survey, that I saw the
bed of the
ice just dropping away,» Bingham said.
A subglacial aquifer
bed model and water pressure dependent basal sliding relationship for a West Antarctic
ice stream.
Fast - flowing
ice streams draining the WAIS (Pine Island Glacier and Thwaites Glacier in particular) into the Amundsen Sea have a grounding line on a reverse
bed slope, becoming deeper inland.
I reduced
ice -
bed coupling along
ice streams to generate these profiles.
The gap is up to 1.4 m (60 inches) wide, and is filled with water at a pressure nearly high enough to lift the
ice stream off its
bed.
The thick and slow - moving interior
ice reservoir is generally fixed to the underlying bedrock while the
ice streams glide over lubricated
beds at velocities of up to several hundred metres per year.