Lava Eruption and Emplacement: Using Clues from Hawaii and Iceland to Probe the Lunar Past
Investigating recent eruptions on Earth is crucial to improving understanding of relationships between eruption dynamics and final lava flow morphologies. In this study, we investigated eruptions in Holuhraun, Iceland, and Kilauea, Hawaii to gain insight into the lava dynamics near the source vent,...
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ftnasantrs:oai:casi.ntrs.nasa.gov:20170005436 2023-05-15T16:48:19+02:00 Lava Eruption and Emplacement: Using Clues from Hawaii and Iceland to Probe the Lunar Past Young, K. E. Hamilton, C. W. Sutton, S. S. Whelley, P. L. Needham, Debra Hurwitz Scheidt, S. P. Richardson, J. A. Bleacher, J. E. Unclassified, Unlimited, Publicly available March 22, 2017 application/pdf http://hdl.handle.net/2060/20170005436 unknown Document ID: 20170005436 http://hdl.handle.net/2060/20170005436 Copyright, Distribution as joint owner in the copyright CASI Lunar and Planetary Science and Exploration MSFC-E-DAA-TN39618 Lunar and Planetary Science Conference; 20-24 Mar. 2017; The Woodlands, TX; United States 2017 ftnasantrs 2019-07-20T23:32:26Z Investigating recent eruptions on Earth is crucial to improving understanding of relationships between eruption dynamics and final lava flow morphologies. In this study, we investigated eruptions in Holuhraun, Iceland, and Kilauea, Hawaii to gain insight into the lava dynamics near the source vent, the initiation of lava channels, and the origin of down-channel features. Insights are applied to Rima Bode on the lunar nearside to deduce the sequence of events that formed this lunar sinuous rille system. These insights are crucial to correctly interpreting whether the volcanic features associated with Rima Bode directly relate to eruption conditions at the vent and, thus, can help us understand those eruption dynamics, or, alternatively, whether the features formed as a result of more localized influences on lava flow dynamics. For example, if the lava channel developed early in the eruption and was linked to pulses in vent activity, its morphology can be analyzed to interpret the flux and duration of the eruption. Conversely, if the lava channel initiated late in the eruption as the result of a catastrophic breaching of lava that had previously pooled within the vent [e.g., 1], then the final channel morphology will not indicate eruption dynamics but rather local dynamics associated with that breach event. Distinguishing between these two scenarios is crucial for correctly interpreting the intensity and duration of volcanic history on the Moon. Other/Unknown Material Iceland NASA Technical Reports Server (NTRS) Holuhraun ENVELOPE(-16.831,-16.831,64.852,64.852) Rima ENVELOPE(-45.400,-45.400,-60.633,-60.633) |
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Open Polar |
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NASA Technical Reports Server (NTRS) |
op_collection_id |
ftnasantrs |
language |
unknown |
topic |
Lunar and Planetary Science and Exploration |
spellingShingle |
Lunar and Planetary Science and Exploration Young, K. E. Hamilton, C. W. Sutton, S. S. Whelley, P. L. Needham, Debra Hurwitz Scheidt, S. P. Richardson, J. A. Bleacher, J. E. Lava Eruption and Emplacement: Using Clues from Hawaii and Iceland to Probe the Lunar Past |
topic_facet |
Lunar and Planetary Science and Exploration |
description |
Investigating recent eruptions on Earth is crucial to improving understanding of relationships between eruption dynamics and final lava flow morphologies. In this study, we investigated eruptions in Holuhraun, Iceland, and Kilauea, Hawaii to gain insight into the lava dynamics near the source vent, the initiation of lava channels, and the origin of down-channel features. Insights are applied to Rima Bode on the lunar nearside to deduce the sequence of events that formed this lunar sinuous rille system. These insights are crucial to correctly interpreting whether the volcanic features associated with Rima Bode directly relate to eruption conditions at the vent and, thus, can help us understand those eruption dynamics, or, alternatively, whether the features formed as a result of more localized influences on lava flow dynamics. For example, if the lava channel developed early in the eruption and was linked to pulses in vent activity, its morphology can be analyzed to interpret the flux and duration of the eruption. Conversely, if the lava channel initiated late in the eruption as the result of a catastrophic breaching of lava that had previously pooled within the vent [e.g., 1], then the final channel morphology will not indicate eruption dynamics but rather local dynamics associated with that breach event. Distinguishing between these two scenarios is crucial for correctly interpreting the intensity and duration of volcanic history on the Moon. |
format |
Other/Unknown Material |
author |
Young, K. E. Hamilton, C. W. Sutton, S. S. Whelley, P. L. Needham, Debra Hurwitz Scheidt, S. P. Richardson, J. A. Bleacher, J. E. |
author_facet |
Young, K. E. Hamilton, C. W. Sutton, S. S. Whelley, P. L. Needham, Debra Hurwitz Scheidt, S. P. Richardson, J. A. Bleacher, J. E. |
author_sort |
Young, K. E. |
title |
Lava Eruption and Emplacement: Using Clues from Hawaii and Iceland to Probe the Lunar Past |
title_short |
Lava Eruption and Emplacement: Using Clues from Hawaii and Iceland to Probe the Lunar Past |
title_full |
Lava Eruption and Emplacement: Using Clues from Hawaii and Iceland to Probe the Lunar Past |
title_fullStr |
Lava Eruption and Emplacement: Using Clues from Hawaii and Iceland to Probe the Lunar Past |
title_full_unstemmed |
Lava Eruption and Emplacement: Using Clues from Hawaii and Iceland to Probe the Lunar Past |
title_sort |
lava eruption and emplacement: using clues from hawaii and iceland to probe the lunar past |
publishDate |
2017 |
url |
http://hdl.handle.net/2060/20170005436 |
op_coverage |
Unclassified, Unlimited, Publicly available |
long_lat |
ENVELOPE(-16.831,-16.831,64.852,64.852) ENVELOPE(-45.400,-45.400,-60.633,-60.633) |
geographic |
Holuhraun Rima |
geographic_facet |
Holuhraun Rima |
genre |
Iceland |
genre_facet |
Iceland |
op_source |
CASI |
op_relation |
Document ID: 20170005436 http://hdl.handle.net/2060/20170005436 |
op_rights |
Copyright, Distribution as joint owner in the copyright |
_version_ |
1766038430390681600 |