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Bedforms of Thwaites Glacier, West Antarctica: Character and Origin


Identification_Information:
Citation:
Citation_Information:
Originator:Pennsylvania State University
Title:
Bedforms of Thwaites Glacier, West Antarctica: Character and Origin
Other_Citation_Details:
R.B. Alley1, N. Holschuh2,3, D.R. MacAyeal4, B.R. Parizek1, L. Zoet5, K. Riverman6, A. Muto7, K. Christianson2, E. Clyne1, S. Anandakrishnan1, N. Stevens5, GHOST Collaboration† 1Department of Geosciences, and Earth and Environmental Systems Institute, Pennsylvania State University, University Park, PA, USA 2Department of Earth and Space Sciences, University of Washington, Seattle, WA, USA 3Department of Geology, Amherst College, Amherst, MA, USA 4Department of Geophysical Sciences, University of Chicago, Chicago, IL, USA 5Department of Geoscience, University of Wisconsin, Madison, WI, USA 6Department of Earth Science, University of Oregon, Eugene, OR, USA 7Department of Earth and Environmental Science, Temple University, Philadelphia, PA, USA
Online_Linkage: https://thwaitesglacier.org/projects/ghost
Online_Linkage: http://www.datacommons.psu.edu/
Description:
Abstract:
Bedforms of Thwaites Glacier, West Antarctica both record and affect ice flow. Thwaites Glacier flows across the tectonic fabric of the West Antarctic rift system with its bedrock highs and sedimentary basins.  Swath radar and seismic surveys of the glacier bed have revealed soft-sediment flutes 100 m or more high extending 15 km or more across basins downglacier from bedrock highs, and ending at prominent hard-bedded moats on stoss sides of the next topographic highs. We use simple models to show that ice flow against topography generates high pressure between ice and till upglacier along the bed over a distance that scales with the topography.  This high pressure would exclude ice-contact water there and thus increase ice-till coupling and till flux there, removing till to allow bedrock erosion and create moats.  Till carried across highlands would then be deposited in lee-side positions, remaining soft on top to approach steady-state by matching till-deformational fluxes from upglacier of the topography, and prograding downglacier over time. The bedforms of the part of Thwaites surveyed here are prominent because ice flow has persisted over a long time on this geological setting, not because ice flow is anomalous.  Bedform development likely has caused evolution of ice flow over time.
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publication date
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Bounding_Coordinates:
West_Bounding_Coordinate:-180
East_Bounding_Coordinate:180
North_Bounding_Coordinate:90
South_Bounding_Coordinate:-90
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Theme:
Theme_Keyword_Thesaurus:ISO 19115 Topic Categories
Theme_Keyword:climatologyMeteorologyAtmosphere
Access_Constraints:None.
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Point_of_Contact:
Contact_Information:
Contact_Organization_Primary:
Contact_Organization:Pennsylvania State University
Contact_Person:Richard Alley
Contact_Address:
Address_Type:mailing address
Address:
306 Deike Building
Address:
Department of Geosciences
City:University Park
State_or_Province:Pennsylvania
Postal_Code:16802
Country:United States
Contact_Voice_Telephone:(814) 863-1700
Contact_Electronic_Mail_Address:ralley@essc.psu.edu
Native_Data_Set_Environment:
Microsoft Windows 2000 Version 5.0 (Build 2195) Service Pack 4; ESRI ArcCatalog 8.3.0.800
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Distributor:
Contact_Information:
Contact_Person_Primary:
Contact_Organization:Penn State Data Commons
Contact_Address:
Address_Type:mailing and physical address
Address:
115 Land and Water Building
City:University Park
State_or_Province:Pennsylvania
Postal_Code:16802
Country:United States
Contact_Voice_Telephone:(814) 865 - 8792
Contact_Electronic_Mail_Address:datacommons@psu.edu
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The USER shall indemnify, save harmless, and, if requested, defend those parties involved with the development and distribution of this data, their officers, agents, and employees from and against any suits, claims, or actions for injury, death, or property damage arising out of the use of or any defect in the FILES or any accompanying documentation. Those parties involved with the development and distribution excluded any and all implied warranties, including warranties or merchantability and fitness for a particular purpose and makes no warranty or representation, either express or implied, with respect to the FILES or accompanying documentation, including its quality, performance, merchantability, or fitness for a particular purpose. The FILES and documentation are provided "as is" and the USER assumes the entire risk as to its quality and performance. Those parties involved with the development and distribution of this data will not be liable for any direct, indirect, special, incidental, or consequential damages arising out of the use or inability to use the FILES or any accompanying documentation.
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Metadata_Reference_Information:
Metadata_Contact:
Contact_Information:
Contact_Organization_Primary:
Contact_Organization:Penn State Data Commons
Contact_Position:Metadata Coordinator
Contact_Address:
Address_Type:mailing address
Address:
115 Land and Water Building
City:University Park
State_or_Province:Pennsylvania
Postal_Code:16802
Country:United States
Contact_Voice_Telephone:814-865-8792
Contact_Electronic_Mail_Address:datacommons@psu.edu
Metadata_Standard_Name:FGDC Content Standards for Digital Geospatial Metadata
Metadata_Standard_Version:FGDC-STD-001-1998
Metadata_Time_Convention:local time
Metadata_Extensions:
Profile_Name:ESRI Metadata Profile
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