Collaborative Research: Volcanic Records from the Siple and Taylor Dome Ice Cores, Antarctica
The primary goals of this project were to, 1) evaluate the volcanic acidity record in the Siple Dome A (SDMA) and B (SDMB) ice cores and the Taylor Dome ice core available through the sulfate time series developed by the glaciochemistry group at the University of Maine, 2) undertake a continuous sca...
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ftmaineuniv:oai:digitalcommons.library.umaine.edu:orsp_reports-1180 2023-05-15T14:03:23+02:00 Collaborative Research: Volcanic Records from the Siple and Taylor Dome Ice Cores, Antarctica Zielinski, George A. 2003-06-26T07:00:00Z application/pdf https://digitalcommons.library.umaine.edu/orsp_reports/172 https://digitalcommons.library.umaine.edu/cgi/viewcontent.cgi?article=1180&context=orsp_reports unknown DigitalCommons@UMaine https://digitalcommons.library.umaine.edu/orsp_reports/172 https://digitalcommons.library.umaine.edu/cgi/viewcontent.cgi?article=1180&context=orsp_reports This Item is protected by copyright and/or related rights. You are free to use this Item in any way that is permitted by the copyright and related rights legislation that applies to your use. In addition, no permission is required from the rights-holder(s) for educational uses. For other uses, you need to obtain permission from the rights-holder(s). University of Maine Office of Research Administration: Grant Reports Volcanic activity Volcanic glass Glaciology Volcanology text 2003 ftmaineuniv 2023-03-12T19:15:49Z The primary goals of this project were to, 1) evaluate the volcanic acidity record in the Siple Dome A (SDMA) and B (SDMB) ice cores and the Taylor Dome ice core available through the sulfate time series developed by the glaciochemistry group at the University of Maine, 2) undertake a continuous scan of the SDMA core and scan specific sections in the SDMB core to locate and analyze volcanic glass to determine glass composition, and thus source eruptions for the glass and potentially for volcanic sulfate found in the same layer, and 3) evaluate specific sections containing volcanic glass in the Taylor Dome ice core as noted by visible layers in that core. A specific use of these volcanic records is to identify products of known volcanic eruptions, where possible, thereby providing distinct time lines that are used in developing the depth-age scale for the individual ice cores. In addition, the evaluation of volcanic glass can help differentiate signals that originated from local (Antarctica) volcanic eruptions and those originating from mid-latitude southern hemisphere or equatorial eruptions. Text Antarc* Antarctica ice core The University of Maine: DigitalCommons@UMaine Siple ENVELOPE(-83.917,-83.917,-75.917,-75.917) Siple Dome ENVELOPE(-148.833,-148.833,-81.667,-81.667) Taylor Dome ENVELOPE(157.667,157.667,-77.667,-77.667) |
institution |
Open Polar |
collection |
The University of Maine: DigitalCommons@UMaine |
op_collection_id |
ftmaineuniv |
language |
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topic |
Volcanic activity Volcanic glass Glaciology Volcanology |
spellingShingle |
Volcanic activity Volcanic glass Glaciology Volcanology Zielinski, George A. Collaborative Research: Volcanic Records from the Siple and Taylor Dome Ice Cores, Antarctica |
topic_facet |
Volcanic activity Volcanic glass Glaciology Volcanology |
description |
The primary goals of this project were to, 1) evaluate the volcanic acidity record in the Siple Dome A (SDMA) and B (SDMB) ice cores and the Taylor Dome ice core available through the sulfate time series developed by the glaciochemistry group at the University of Maine, 2) undertake a continuous scan of the SDMA core and scan specific sections in the SDMB core to locate and analyze volcanic glass to determine glass composition, and thus source eruptions for the glass and potentially for volcanic sulfate found in the same layer, and 3) evaluate specific sections containing volcanic glass in the Taylor Dome ice core as noted by visible layers in that core. A specific use of these volcanic records is to identify products of known volcanic eruptions, where possible, thereby providing distinct time lines that are used in developing the depth-age scale for the individual ice cores. In addition, the evaluation of volcanic glass can help differentiate signals that originated from local (Antarctica) volcanic eruptions and those originating from mid-latitude southern hemisphere or equatorial eruptions. |
format |
Text |
author |
Zielinski, George A. |
author_facet |
Zielinski, George A. |
author_sort |
Zielinski, George A. |
title |
Collaborative Research: Volcanic Records from the Siple and Taylor Dome Ice Cores, Antarctica |
title_short |
Collaborative Research: Volcanic Records from the Siple and Taylor Dome Ice Cores, Antarctica |
title_full |
Collaborative Research: Volcanic Records from the Siple and Taylor Dome Ice Cores, Antarctica |
title_fullStr |
Collaborative Research: Volcanic Records from the Siple and Taylor Dome Ice Cores, Antarctica |
title_full_unstemmed |
Collaborative Research: Volcanic Records from the Siple and Taylor Dome Ice Cores, Antarctica |
title_sort |
collaborative research: volcanic records from the siple and taylor dome ice cores, antarctica |
publisher |
DigitalCommons@UMaine |
publishDate |
2003 |
url |
https://digitalcommons.library.umaine.edu/orsp_reports/172 https://digitalcommons.library.umaine.edu/cgi/viewcontent.cgi?article=1180&context=orsp_reports |
long_lat |
ENVELOPE(-83.917,-83.917,-75.917,-75.917) ENVELOPE(-148.833,-148.833,-81.667,-81.667) ENVELOPE(157.667,157.667,-77.667,-77.667) |
geographic |
Siple Siple Dome Taylor Dome |
geographic_facet |
Siple Siple Dome Taylor Dome |
genre |
Antarc* Antarctica ice core |
genre_facet |
Antarc* Antarctica ice core |
op_source |
University of Maine Office of Research Administration: Grant Reports |
op_relation |
https://digitalcommons.library.umaine.edu/orsp_reports/172 https://digitalcommons.library.umaine.edu/cgi/viewcontent.cgi?article=1180&context=orsp_reports |
op_rights |
This Item is protected by copyright and/or related rights. You are free to use this Item in any way that is permitted by the copyright and related rights legislation that applies to your use. In addition, no permission is required from the rights-holder(s) for educational uses. For other uses, you need to obtain permission from the rights-holder(s). |
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1766274018012299264 |