Reconstructing the glacial history of Marguerite Bay, Antarctic Peninsula: A combined geomorphological and sedimentological approach
Geological and geophysical data were interpreted to reconstruct the glacial history of Marguerite Bay. Antarctic Peninsula, since the Last Glacial Maximum. An extensive paleo-subglacial meltwater drainage system, which drained the lower Peninsula since at least the Last Glacial Maximum, was mapped o...
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ftriceuniv:oai:scholarship.rice.edu:1911/18953 2023-05-15T13:39:43+02:00 Reconstructing the glacial history of Marguerite Bay, Antarctic Peninsula: A combined geomorphological and sedimentological approach Oakes Fretwell, Lisa Anderson, John B. 2006 228 p. application/pdf https://hdl.handle.net/1911/18953 eng eng Oakes Fretwell, Lisa. "Reconstructing the glacial history of Marguerite Bay, Antarctic Peninsula: A combined geomorphological and sedimentological approach." (2006) Diss., Rice University. https://hdl.handle.net/1911/18953 . https://hdl.handle.net/1911/18953 THESIS GEOL. 2006 FRETWELL Geology Thesis Text 2006 ftriceuniv 2022-08-09T20:31:19Z Geological and geophysical data were interpreted to reconstruct the glacial history of Marguerite Bay. Antarctic Peninsula, since the Last Glacial Maximum. An extensive paleo-subglacial meltwater drainage system, which drained the lower Peninsula since at least the Last Glacial Maximum, was mapped on the inner-shelf. A distinct organization of flow is seen across the inner-shelf, as relatively small-scale randomly-oriented linked-cavities feed into larger, linear channels and tunnel valleys. Meltwater discharge estimates suggest that production from steady-state processes (geothermal heat and frictional heat dissipation) were enhanced locally by the sudden up-glacier release of subglacially-stored meltwater. Such large instantaneous meltwater releases may have led to periods of rapid sliding, or intermittent ice-bed separation, within the system. Evidence of glacial erosion on bedrock highs, in the form of striations and grooves, suggests that ice flow remained relatively slow outside the main troughs. As sediment accumulated on the mid-shelf, free meltwater became incorporated into the porous sedimentary strata, thus enabling the facilitation of sediment deformation and relatively rapid ice flow. The presence of mega-scale glacial lineations on the outer-shelf, which clearly extend to the shelf-break where gullies erode downslope, further supports a relatively rapid ice flow, and suggests that maximum ice extent during the Last Glacial Maximum was at the shelf-break. Therefore, ice flow behavior in the bay and trough was primarily controlled by subglacial substrate, the occurrence of subglacial meltwater and local topography. Sediment facies were interpreted as subglacial, proximal-grounding zone, sub-ice shelf, fjord and ice-distal/open marine, based primarily on lithologic attributes, shear strength and down-core magnetic susceptibility response. AMS dating of specific glaciomarine sediment facies implies that grounded ice retreated diachronously across the outer-shelf, retreating initially within the trough ... Thesis Antarc* Antarctic Antarctic Peninsula Ice Shelf Rice University: Digital Scholarship Archive Antarctic Antarctic Peninsula Marguerite ENVELOPE(141.378,141.378,-66.787,-66.787) Marguerite Bay ENVELOPE(-68.000,-68.000,-68.500,-68.500) |
institution |
Open Polar |
collection |
Rice University: Digital Scholarship Archive |
op_collection_id |
ftriceuniv |
language |
English |
topic |
Geology |
spellingShingle |
Geology Oakes Fretwell, Lisa Reconstructing the glacial history of Marguerite Bay, Antarctic Peninsula: A combined geomorphological and sedimentological approach |
topic_facet |
Geology |
description |
Geological and geophysical data were interpreted to reconstruct the glacial history of Marguerite Bay. Antarctic Peninsula, since the Last Glacial Maximum. An extensive paleo-subglacial meltwater drainage system, which drained the lower Peninsula since at least the Last Glacial Maximum, was mapped on the inner-shelf. A distinct organization of flow is seen across the inner-shelf, as relatively small-scale randomly-oriented linked-cavities feed into larger, linear channels and tunnel valleys. Meltwater discharge estimates suggest that production from steady-state processes (geothermal heat and frictional heat dissipation) were enhanced locally by the sudden up-glacier release of subglacially-stored meltwater. Such large instantaneous meltwater releases may have led to periods of rapid sliding, or intermittent ice-bed separation, within the system. Evidence of glacial erosion on bedrock highs, in the form of striations and grooves, suggests that ice flow remained relatively slow outside the main troughs. As sediment accumulated on the mid-shelf, free meltwater became incorporated into the porous sedimentary strata, thus enabling the facilitation of sediment deformation and relatively rapid ice flow. The presence of mega-scale glacial lineations on the outer-shelf, which clearly extend to the shelf-break where gullies erode downslope, further supports a relatively rapid ice flow, and suggests that maximum ice extent during the Last Glacial Maximum was at the shelf-break. Therefore, ice flow behavior in the bay and trough was primarily controlled by subglacial substrate, the occurrence of subglacial meltwater and local topography. Sediment facies were interpreted as subglacial, proximal-grounding zone, sub-ice shelf, fjord and ice-distal/open marine, based primarily on lithologic attributes, shear strength and down-core magnetic susceptibility response. AMS dating of specific glaciomarine sediment facies implies that grounded ice retreated diachronously across the outer-shelf, retreating initially within the trough ... |
author2 |
Anderson, John B. |
format |
Thesis |
author |
Oakes Fretwell, Lisa |
author_facet |
Oakes Fretwell, Lisa |
author_sort |
Oakes Fretwell, Lisa |
title |
Reconstructing the glacial history of Marguerite Bay, Antarctic Peninsula: A combined geomorphological and sedimentological approach |
title_short |
Reconstructing the glacial history of Marguerite Bay, Antarctic Peninsula: A combined geomorphological and sedimentological approach |
title_full |
Reconstructing the glacial history of Marguerite Bay, Antarctic Peninsula: A combined geomorphological and sedimentological approach |
title_fullStr |
Reconstructing the glacial history of Marguerite Bay, Antarctic Peninsula: A combined geomorphological and sedimentological approach |
title_full_unstemmed |
Reconstructing the glacial history of Marguerite Bay, Antarctic Peninsula: A combined geomorphological and sedimentological approach |
title_sort |
reconstructing the glacial history of marguerite bay, antarctic peninsula: a combined geomorphological and sedimentological approach |
publishDate |
2006 |
url |
https://hdl.handle.net/1911/18953 |
long_lat |
ENVELOPE(141.378,141.378,-66.787,-66.787) ENVELOPE(-68.000,-68.000,-68.500,-68.500) |
geographic |
Antarctic Antarctic Peninsula Marguerite Marguerite Bay |
geographic_facet |
Antarctic Antarctic Peninsula Marguerite Marguerite Bay |
genre |
Antarc* Antarctic Antarctic Peninsula Ice Shelf |
genre_facet |
Antarc* Antarctic Antarctic Peninsula Ice Shelf |
op_relation |
Oakes Fretwell, Lisa. "Reconstructing the glacial history of Marguerite Bay, Antarctic Peninsula: A combined geomorphological and sedimentological approach." (2006) Diss., Rice University. https://hdl.handle.net/1911/18953 . https://hdl.handle.net/1911/18953 THESIS GEOL. 2006 FRETWELL |
_version_ |
1766122541171081216 |