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Sediments, Water, and Inland Ice Flow: A Geologic Control on Ice Stream Tributaries?. Leo E. Peters Sridhar Anandakrishnan, Richard B. Alley, J. Paul Winberry, Donald E. Voigt, Andrew M. Smith, Donald D. Blankenship, David L. Morse WAIS Conference Friday, September 30, 2005.
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Sediments, Water, and Inland Ice Flow: A Geologic Control on Ice Stream Tributaries? Leo E. Peters Sridhar Anandakrishnan, Richard B. Alley, J. Paul Winberry, Donald E. Voigt, Andrew M. Smith, Donald D. Blankenship, David L. Morse WAIS Conference Friday, September 30, 2005
Outline • Importance of Subglacial Sediments • Previous Work along the Siple Coast • Along the Ice Streams • Onset of Kamb and Bindschadler • Seismic Reflection and Results • Interpretation/Conclusions
Subglacial Sediments and Streaming Ice Flow Paleoshoreline ? ? ? Sediments
Siple Coast “Ground-Truthing” C1B Whillans DT/DL CT Kamb Seismic Reflection/Refraction Seismic Reflection - Shown Bindschadler
C1B Whillans Kamb Bindschadler
Sediments Above and Below the Onset Direction of Ice Flow Peters et al. (accepted by JGR-Solid Earth)
The C1B Reflection Seismic Profile Direction of Ice Flow
The C1B Reflection Seismic Profile Direction of Ice Flow Direction of Ice Flow Base of Ice Sedimentary Structure Base of Sediments Basement
Whillans DT/DL Kamb Bindschadler
Sediments Above the Onset Peters et al. (accepted by JGR-Solid Earth)
The DL Reflection Seismic Profile Direction of Ice Flow Depth Below Surface (meters) Depth Below Surface (meters)
The DL Reflection Seismic Profile Direction of Ice Flow Depth Below Surface (meters) Depth Below Surface (meters) No Amplitude Phase Change = Till
The DL Reflection Seismic Profile Direction of Ice Flow Depth Below Surface (meters) Depth Below Surface (meters) Amplitude Phase Change = Dilatant Till
The DL Reflection Seismic Profile Direction of Ice Flow Blue = Dilatant Till Red = Till Depth Below Surface (meters) Depth Below Surface (meters)
Whillans CT Kamb Bindschadler
The CT Reflection Seismic Profile Blue = Dilatant Till to Water Red = Till
Siple Coast Ice Dynamics ? ? ? ? Pine Island Glacier: faster flow… Different geologic conditions??? Variability across the Siple Coast