Development of Quantitative Weathering Indicators in Proximal Alluvial Sediments to Assess Glacial Activity in the Rock Record

Abstract: The proposed research seeks to test the hypothesis that chemical and physical weathering in proximal alluvial systems will show systematic and measurable variations between glacial and nonglacial systems. To accomplish this, the investigation will attempt to quantify the natural variation...

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Main Authors: Madden, Megan Elwood, Soreghan, Gerilyn
Format: Dataset
Language:unknown
Published: IEDA: US Antarctic Program Data Center 2011
Subjects:
Online Access:http://get.iedadata.org/metadata/iso/600110
id dataone:http://get.iedadata.org/metadata/iso/600110
record_format openpolar
spelling dataone:http://get.iedadata.org/metadata/iso/600110 2024-06-03T18:46:24+00:00 Development of Quantitative Weathering Indicators in Proximal Alluvial Sediments to Assess Glacial Activity in the Rock Record Madden, Megan Elwood Soreghan, Gerilyn ENVELOPE(-163.12865,-162.44835,-77.41693,-77.70258) BEGINDATE: 2009-06-15T00:00:00Z ENDDATE: 2011-05-31T00:00:00Z 2011-01-01T00:00:00Z http://get.iedadata.org/metadata/iso/600110 unknown IEDA: US Antarctic Program Data Center Antarctic Earth Sciences Chemistry:Fluid Chemistry:Rock Chemistry:Sediment Antarctica Critical Zone Glaciers/Ice Sheet Cryosphere Geochemistry US Antarctic Program Data Center (USAP-DC) Dataset 2011 dataone:urn:node:IEDA_USAP 2024-06-03T18:11:58Z Abstract: The proposed research seeks to test the hypothesis that chemical and physical weathering in proximal alluvial systems will show systematic and measurable variations between glacial and nonglacial systems. To accomplish this, the investigation will attempt to quantify the natural variation of chemical and physical weathering in granitoid-sourced proximal alluvial sediments in end-member glacial and nonglacial systems, when other, 'non-climatic' factors (e.g. provenance, drainage basin area and relief, sample grain size, sediment facies) are controlled. If chemical weathering in the proposed hot-humid, hot-arid, hot semi-arid nonglacial systems and the cool-wet, cold semi-arid, and cold-arid glacial systems show systematic variations, then chemical indices may be used to help differentiate paleoclimatic conditions. Continued reliance on students provides a broader impact of this proposed research and firmly grounds this effort in its educational mission. Dataset Antarc* Antarctic Antarctica Ice Sheet IEDA: US Antarctic Program Data Center (via DataONE) Antarctic ENVELOPE(-163.12865,-162.44835,-77.41693,-77.70258)
institution Open Polar
collection IEDA: US Antarctic Program Data Center (via DataONE)
op_collection_id dataone:urn:node:IEDA_USAP
language unknown
topic Antarctic Earth Sciences
Chemistry:Fluid
Chemistry:Rock
Chemistry:Sediment
Antarctica
Critical Zone
Glaciers/Ice Sheet
Cryosphere
Geochemistry
US Antarctic Program Data Center (USAP-DC)
spellingShingle Antarctic Earth Sciences
Chemistry:Fluid
Chemistry:Rock
Chemistry:Sediment
Antarctica
Critical Zone
Glaciers/Ice Sheet
Cryosphere
Geochemistry
US Antarctic Program Data Center (USAP-DC)
Madden, Megan Elwood
Soreghan, Gerilyn
Development of Quantitative Weathering Indicators in Proximal Alluvial Sediments to Assess Glacial Activity in the Rock Record
topic_facet Antarctic Earth Sciences
Chemistry:Fluid
Chemistry:Rock
Chemistry:Sediment
Antarctica
Critical Zone
Glaciers/Ice Sheet
Cryosphere
Geochemistry
US Antarctic Program Data Center (USAP-DC)
description Abstract: The proposed research seeks to test the hypothesis that chemical and physical weathering in proximal alluvial systems will show systematic and measurable variations between glacial and nonglacial systems. To accomplish this, the investigation will attempt to quantify the natural variation of chemical and physical weathering in granitoid-sourced proximal alluvial sediments in end-member glacial and nonglacial systems, when other, 'non-climatic' factors (e.g. provenance, drainage basin area and relief, sample grain size, sediment facies) are controlled. If chemical weathering in the proposed hot-humid, hot-arid, hot semi-arid nonglacial systems and the cool-wet, cold semi-arid, and cold-arid glacial systems show systematic variations, then chemical indices may be used to help differentiate paleoclimatic conditions. Continued reliance on students provides a broader impact of this proposed research and firmly grounds this effort in its educational mission.
format Dataset
author Madden, Megan Elwood
Soreghan, Gerilyn
author_facet Madden, Megan Elwood
Soreghan, Gerilyn
author_sort Madden, Megan Elwood
title Development of Quantitative Weathering Indicators in Proximal Alluvial Sediments to Assess Glacial Activity in the Rock Record
title_short Development of Quantitative Weathering Indicators in Proximal Alluvial Sediments to Assess Glacial Activity in the Rock Record
title_full Development of Quantitative Weathering Indicators in Proximal Alluvial Sediments to Assess Glacial Activity in the Rock Record
title_fullStr Development of Quantitative Weathering Indicators in Proximal Alluvial Sediments to Assess Glacial Activity in the Rock Record
title_full_unstemmed Development of Quantitative Weathering Indicators in Proximal Alluvial Sediments to Assess Glacial Activity in the Rock Record
title_sort development of quantitative weathering indicators in proximal alluvial sediments to assess glacial activity in the rock record
publisher IEDA: US Antarctic Program Data Center
publishDate 2011
url http://get.iedadata.org/metadata/iso/600110
op_coverage ENVELOPE(-163.12865,-162.44835,-77.41693,-77.70258)
BEGINDATE: 2009-06-15T00:00:00Z ENDDATE: 2011-05-31T00:00:00Z
long_lat ENVELOPE(-163.12865,-162.44835,-77.41693,-77.70258)
geographic Antarctic
geographic_facet Antarctic
genre Antarc*
Antarctic
Antarctica
Ice Sheet
genre_facet Antarc*
Antarctic
Antarctica
Ice Sheet
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