An Elemental Analysis of the Glacial Deposits of the Vestfold Hills, Antarctica
Metadata record for data from ASAC Project 135 Taken from the abstracts of some of the referenced papers: Vestfold Hills, Antarctica exhibits marked contrasts in the weathering surface and glacial sediments between its eastern and western parts. The boundary between these zones coincides with a regi...
Other Authors: | , , |
---|---|
Format: | Dataset |
Language: | unknown |
Published: |
Australian Antarctic Data Centre
|
Subjects: | |
Online Access: | https://researchdata.ands.org.au/an-elemental-analysis-hills-antarctica/699705 https://doi.org/10.4225/15/55E91FC8B85CB https://data.aad.gov.au/metadata/records/ASAC_135 https://data.aad.gov.au/metadata/records/ASAC_1343_phytoplankton http://nla.gov.au/nla.party-617536 |
id |
ftands:oai:ands.org.au::699705 |
---|---|
record_format |
openpolar |
institution |
Open Polar |
collection |
Research Data Australia (Australian National Data Service - ANDS) |
op_collection_id |
ftands |
language |
unknown |
topic |
climatologyMeteorologyAtmosphere geoscientificInformation inlandWaters GLACIERS EARTH SCIENCE CRYOSPHERE GLACIERS/ICE SHEETS salt line deglaciation radiocarbon dating CONTINENT > ANTARCTICA GEOGRAPHIC REGION > POLAR |
spellingShingle |
climatologyMeteorologyAtmosphere geoscientificInformation inlandWaters GLACIERS EARTH SCIENCE CRYOSPHERE GLACIERS/ICE SHEETS salt line deglaciation radiocarbon dating CONTINENT > ANTARCTICA GEOGRAPHIC REGION > POLAR An Elemental Analysis of the Glacial Deposits of the Vestfold Hills, Antarctica |
topic_facet |
climatologyMeteorologyAtmosphere geoscientificInformation inlandWaters GLACIERS EARTH SCIENCE CRYOSPHERE GLACIERS/ICE SHEETS salt line deglaciation radiocarbon dating CONTINENT > ANTARCTICA GEOGRAPHIC REGION > POLAR |
description |
Metadata record for data from ASAC Project 135 Taken from the abstracts of some of the referenced papers: Vestfold Hills, Antarctica exhibits marked contrasts in the weathering surface and glacial sediments between its eastern and western parts. The boundary between these zones coincides with a regional chemical boundary termed the 'salt line'. The area west of the salt line is saturated with marine-derived halite and thenardite that are particularly aggressive agents of rock weathering. In contrast, the area east of the salt line exhibits significantly fewer deposits of these salts. Rock surfaces west of the salt line are characterised by well-developed weathering forms, while glacial polish and striae are largely absent. In contrast, rock surfaces to the east commonly retain glacial polish and striae. In places, differential weathering has caused thin basaltic dykes and felsic veins to stand above the surrounding gneiss. The rate of lowering of the gneiss and dykes to the west of the salt line has been estimated at 0.024 mm and 0.015 mm per year respectively. These measurements suggest that the weathering surface in parts of the Vestfold Hills may record more than 70ka of subaerial exposure. Glacial sediments are much more abundant, coarser and better sorted northwest of the salt line than to the southeast. The abundant grus produced by physical weathering is coarser grained and better sorted that that produced by subglacial erosion. Such sediment lying on the land surface would be transported and redeposited during glacial advances. The change in nature of the sediments to either side of the salt line, together with the weathering forms found on clasts in the moraines, indicates that the weathering surface prior to the last glacial advance was similar to that of today and must also have developed during long periods of subaerial exposure. ##### Radiocarbon dating of marine, lacustrine or terrestrial biogenic deposits is the main technique used to determine when deglaciation of the oases of East Antarctica occurred. However, at many of the oases of East Antarctica, including the Schirmacher Oasis, Stillwell Hills, Amery Oasis, Larsemann Hills, Taylor Islands and Grearson Oasis, snow and ice presently forms extensive blankets that fills valleys and some lake basins, covers perennial lake ice and in places overwhelms local topography to form ice domes up to hundreds of square kilometres in area. Field observations from Larsemann Hills and Taylor Islands suggest that under these conditions, terrestrial and lacustrine biogenic sedimentation is neither widespread nor abundant. If similar conditions prevailed in and around the oases immediately following retreat of the ice sheet, then a lengthy hiatus might exist between deglaciation and the onset of widespread or abundant biogenic sedimentation. As a result, radiocarbon dating might be a clumsy tool with which to reconstruct deglaciation history, and independent dating methods that record emergence of the hilltops from the continental ice must be employed as well. |
author2 |
COLHOUN, ERIC (hasPrincipalInvestigator) COLHOUN, ERIC (processor) Australian Antarctic Data Centre (publisher) |
format |
Dataset |
title |
An Elemental Analysis of the Glacial Deposits of the Vestfold Hills, Antarctica |
title_short |
An Elemental Analysis of the Glacial Deposits of the Vestfold Hills, Antarctica |
title_full |
An Elemental Analysis of the Glacial Deposits of the Vestfold Hills, Antarctica |
title_fullStr |
An Elemental Analysis of the Glacial Deposits of the Vestfold Hills, Antarctica |
title_full_unstemmed |
An Elemental Analysis of the Glacial Deposits of the Vestfold Hills, Antarctica |
title_sort |
elemental analysis of the glacial deposits of the vestfold hills, antarctica |
publisher |
Australian Antarctic Data Centre |
url |
https://researchdata.ands.org.au/an-elemental-analysis-hills-antarctica/699705 https://doi.org/10.4225/15/55E91FC8B85CB https://data.aad.gov.au/metadata/records/ASAC_135 https://data.aad.gov.au/metadata/records/ASAC_1343_phytoplankton http://nla.gov.au/nla.party-617536 |
op_coverage |
Spatial: northlimit=-68.0; southlimit=-68.5; westlimit=78.0; eastLimit=78.5; projection=WGS84 Temporal: From 1988-09-30 to 1995-03-31 |
long_lat |
ENVELOPE(-94.063,-94.063,56.565,56.565) ENVELOPE(76.217,76.217,-69.400,-69.400) ENVELOPE(59.467,59.467,-67.417,-67.417) ENVELOPE(100.302,100.302,-66.164,-66.164) ENVELOPE(78.0,78.5,-68.0,-68.5) |
geographic |
East Antarctica Vestfold Hills Vestfold Amery Larsemann Hills Stillwell Hills Taylor Islands |
geographic_facet |
East Antarctica Vestfold Hills Vestfold Amery Larsemann Hills Stillwell Hills Taylor Islands |
genre |
Antarc* Antarctica East Antarctica Ice Sheet Taylor Islands |
genre_facet |
Antarc* Antarctica East Antarctica Ice Sheet Taylor Islands |
op_source |
Australian Antarctic Data Centre |
op_relation |
https://researchdata.ands.org.au/an-elemental-analysis-hills-antarctica/699705 fa4191ab-dcaf-4524-91e2-dbf3c887d01b doi:10.4225/15/55E91FC8B85CB ASAC_135 https://data.aad.gov.au/metadata/records/ASAC_135 https://data.aad.gov.au/metadata/records/ASAC_1343_phytoplankton http://nla.gov.au/nla.party-617536 |
op_doi |
https://doi.org/10.4225/15/55E91FC8B85CB |
_version_ |
1766245842299125760 |
spelling |
ftands:oai:ands.org.au::699705 2023-05-15T13:46:57+02:00 An Elemental Analysis of the Glacial Deposits of the Vestfold Hills, Antarctica COLHOUN, ERIC (hasPrincipalInvestigator) COLHOUN, ERIC (processor) Australian Antarctic Data Centre (publisher) Spatial: northlimit=-68.0; southlimit=-68.5; westlimit=78.0; eastLimit=78.5; projection=WGS84 Temporal: From 1988-09-30 to 1995-03-31 https://researchdata.ands.org.au/an-elemental-analysis-hills-antarctica/699705 https://doi.org/10.4225/15/55E91FC8B85CB https://data.aad.gov.au/metadata/records/ASAC_135 https://data.aad.gov.au/metadata/records/ASAC_1343_phytoplankton http://nla.gov.au/nla.party-617536 unknown Australian Antarctic Data Centre https://researchdata.ands.org.au/an-elemental-analysis-hills-antarctica/699705 fa4191ab-dcaf-4524-91e2-dbf3c887d01b doi:10.4225/15/55E91FC8B85CB ASAC_135 https://data.aad.gov.au/metadata/records/ASAC_135 https://data.aad.gov.au/metadata/records/ASAC_1343_phytoplankton http://nla.gov.au/nla.party-617536 Australian Antarctic Data Centre climatologyMeteorologyAtmosphere geoscientificInformation inlandWaters GLACIERS EARTH SCIENCE CRYOSPHERE GLACIERS/ICE SHEETS salt line deglaciation radiocarbon dating CONTINENT > ANTARCTICA GEOGRAPHIC REGION > POLAR dataset ftands https://doi.org/10.4225/15/55E91FC8B85CB 2020-01-05T21:16:37Z Metadata record for data from ASAC Project 135 Taken from the abstracts of some of the referenced papers: Vestfold Hills, Antarctica exhibits marked contrasts in the weathering surface and glacial sediments between its eastern and western parts. The boundary between these zones coincides with a regional chemical boundary termed the 'salt line'. The area west of the salt line is saturated with marine-derived halite and thenardite that are particularly aggressive agents of rock weathering. In contrast, the area east of the salt line exhibits significantly fewer deposits of these salts. Rock surfaces west of the salt line are characterised by well-developed weathering forms, while glacial polish and striae are largely absent. In contrast, rock surfaces to the east commonly retain glacial polish and striae. In places, differential weathering has caused thin basaltic dykes and felsic veins to stand above the surrounding gneiss. The rate of lowering of the gneiss and dykes to the west of the salt line has been estimated at 0.024 mm and 0.015 mm per year respectively. These measurements suggest that the weathering surface in parts of the Vestfold Hills may record more than 70ka of subaerial exposure. Glacial sediments are much more abundant, coarser and better sorted northwest of the salt line than to the southeast. The abundant grus produced by physical weathering is coarser grained and better sorted that that produced by subglacial erosion. Such sediment lying on the land surface would be transported and redeposited during glacial advances. The change in nature of the sediments to either side of the salt line, together with the weathering forms found on clasts in the moraines, indicates that the weathering surface prior to the last glacial advance was similar to that of today and must also have developed during long periods of subaerial exposure. ##### Radiocarbon dating of marine, lacustrine or terrestrial biogenic deposits is the main technique used to determine when deglaciation of the oases of East Antarctica occurred. However, at many of the oases of East Antarctica, including the Schirmacher Oasis, Stillwell Hills, Amery Oasis, Larsemann Hills, Taylor Islands and Grearson Oasis, snow and ice presently forms extensive blankets that fills valleys and some lake basins, covers perennial lake ice and in places overwhelms local topography to form ice domes up to hundreds of square kilometres in area. Field observations from Larsemann Hills and Taylor Islands suggest that under these conditions, terrestrial and lacustrine biogenic sedimentation is neither widespread nor abundant. If similar conditions prevailed in and around the oases immediately following retreat of the ice sheet, then a lengthy hiatus might exist between deglaciation and the onset of widespread or abundant biogenic sedimentation. As a result, radiocarbon dating might be a clumsy tool with which to reconstruct deglaciation history, and independent dating methods that record emergence of the hilltops from the continental ice must be employed as well. Dataset Antarc* Antarctica East Antarctica Ice Sheet Taylor Islands Research Data Australia (Australian National Data Service - ANDS) East Antarctica Vestfold Hills Vestfold Amery ENVELOPE(-94.063,-94.063,56.565,56.565) Larsemann Hills ENVELOPE(76.217,76.217,-69.400,-69.400) Stillwell Hills ENVELOPE(59.467,59.467,-67.417,-67.417) Taylor Islands ENVELOPE(100.302,100.302,-66.164,-66.164) ENVELOPE(78.0,78.5,-68.0,-68.5) |