Terrestrial laser scanning observations of geomorphic changes and varying lava lake levels at Erebus volcano, Antarctica

A Terrestrial Laser Scanning (TLS) instrument was used to image the topography of the Main Crater at Erebus volcano each December in 2008, 2009, and 2010. Our high-spatial resolution TLS scans provide unique insights into annual and decadal scale geomorphic evolution of the summit area when integrat...

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Main Authors: Jones, LK, Kyle, PR, Oppenheimer, C, Frechette, JD, Okal, MH
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier BV 2015
Subjects:
TLS
Online Access:https://www.repository.cam.ac.uk/handle/1810/247889
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record_format openpolar
spelling ftunivcam:oai:www.repository.cam.ac.uk:1810/247889 2024-02-04T09:55:33+01:00 Terrestrial laser scanning observations of geomorphic changes and varying lava lake levels at Erebus volcano, Antarctica Jones, LK Kyle, PR Oppenheimer, C Frechette, JD Okal, MH 2015 application/pdf https://www.repository.cam.ac.uk/handle/1810/247889 English eng eng Elsevier BV http://dx.doi.org/10.1016/j.jvolgeores.2015.02.011 Journal of Volcanology and Geothermal Research https://www.repository.cam.ac.uk/handle/1810/247889 Attribution 2.0 UK: England & Wales http://creativecommons.org/licenses/by/2.0/uk/ Erebus TLS Lidar Geomorphology Lava lake Article 2015 ftunivcam 2024-01-11T23:28:52Z A Terrestrial Laser Scanning (TLS) instrument was used to image the topography of the Main Crater at Erebus volcano each December in 2008, 2009, and 2010. Our high-spatial resolution TLS scans provide unique insights into annual and decadal scale geomorphic evolution of the summit area when integrated with comparable data collected by an airborne instrument in 2001. We observe both a pattern of subsidence within the Inner Crater of the volcano and an ~ 3 m per-year drop in the lava lake level over the same time period that are suggestive of decreasing overpressure in an underlying magma reservoir. We also scanned the active phonolite lava lake hosted within the Inner Crater, and recorded rapid cyclic fluctuations in the level of the lake. These were sporadically interrupted by minor explosions by bursting gas bubbles at the lake surface. The TLS data permit calculation of lake level rise and fall speeds and associated rates of volumetric change within the lake. These new observations, when considered with prior determinations of rates of lake surface motion and gas output, are indicative of unsteady magma flow in the conduit and its associated variability in gas volume fraction. This material is based upon work supported by the National Science Foundation (Division of Polar Programs) under Grants ANT0838817 and ANT1142083. The Optech ILRIS 3D TLS instrument was provided by the UNAVCO Polar group with support from NSF grant award ANT0723223. CO receives additional support from the NEC Centre for the Observation and Modeling of Earthquakes, volcanoes and Tectonics (COMET). We gratefully acknowledge the following for assisting with fieldwork on Erebus: Nelia Dunbar, Bill McIntosh, Aaron Curtis, Nels Iverson, Matt Zimmerer, Melissa Kammerer, Nial Peters, Kayla Iacovino, Yves Moussallam, Tehnuka Ilanko, Anna Barford, and Harry Keys. We also acknowledge tremendous logistical support from the staff and the civilian contractors working out of McMurdo station on behalf of the Division of Polar Programs of NSF. We ... Article in Journal/Newspaper Antarc* Antarctica Apollo - University of Cambridge Repository McMurdo Station ENVELOPE(166.667,166.667,-77.850,-77.850) Dunbar ENVELOPE(-60.199,-60.199,-62.473,-62.473) McIntosh ENVELOPE(168.683,168.683,-77.517,-77.517) Lava Lake ENVELOPE(-128.996,-128.996,55.046,55.046) Main Crater ENVELOPE(167.167,167.167,-77.533,-77.533) Inner Crater ENVELOPE(167.167,167.167,-77.533,-77.533)
institution Open Polar
collection Apollo - University of Cambridge Repository
op_collection_id ftunivcam
language English
topic Erebus
TLS
Lidar
Geomorphology
Lava lake
spellingShingle Erebus
TLS
Lidar
Geomorphology
Lava lake
Jones, LK
Kyle, PR
Oppenheimer, C
Frechette, JD
Okal, MH
Terrestrial laser scanning observations of geomorphic changes and varying lava lake levels at Erebus volcano, Antarctica
topic_facet Erebus
TLS
Lidar
Geomorphology
Lava lake
description A Terrestrial Laser Scanning (TLS) instrument was used to image the topography of the Main Crater at Erebus volcano each December in 2008, 2009, and 2010. Our high-spatial resolution TLS scans provide unique insights into annual and decadal scale geomorphic evolution of the summit area when integrated with comparable data collected by an airborne instrument in 2001. We observe both a pattern of subsidence within the Inner Crater of the volcano and an ~ 3 m per-year drop in the lava lake level over the same time period that are suggestive of decreasing overpressure in an underlying magma reservoir. We also scanned the active phonolite lava lake hosted within the Inner Crater, and recorded rapid cyclic fluctuations in the level of the lake. These were sporadically interrupted by minor explosions by bursting gas bubbles at the lake surface. The TLS data permit calculation of lake level rise and fall speeds and associated rates of volumetric change within the lake. These new observations, when considered with prior determinations of rates of lake surface motion and gas output, are indicative of unsteady magma flow in the conduit and its associated variability in gas volume fraction. This material is based upon work supported by the National Science Foundation (Division of Polar Programs) under Grants ANT0838817 and ANT1142083. The Optech ILRIS 3D TLS instrument was provided by the UNAVCO Polar group with support from NSF grant award ANT0723223. CO receives additional support from the NEC Centre for the Observation and Modeling of Earthquakes, volcanoes and Tectonics (COMET). We gratefully acknowledge the following for assisting with fieldwork on Erebus: Nelia Dunbar, Bill McIntosh, Aaron Curtis, Nels Iverson, Matt Zimmerer, Melissa Kammerer, Nial Peters, Kayla Iacovino, Yves Moussallam, Tehnuka Ilanko, Anna Barford, and Harry Keys. We also acknowledge tremendous logistical support from the staff and the civilian contractors working out of McMurdo station on behalf of the Division of Polar Programs of NSF. We ...
format Article in Journal/Newspaper
author Jones, LK
Kyle, PR
Oppenheimer, C
Frechette, JD
Okal, MH
author_facet Jones, LK
Kyle, PR
Oppenheimer, C
Frechette, JD
Okal, MH
author_sort Jones, LK
title Terrestrial laser scanning observations of geomorphic changes and varying lava lake levels at Erebus volcano, Antarctica
title_short Terrestrial laser scanning observations of geomorphic changes and varying lava lake levels at Erebus volcano, Antarctica
title_full Terrestrial laser scanning observations of geomorphic changes and varying lava lake levels at Erebus volcano, Antarctica
title_fullStr Terrestrial laser scanning observations of geomorphic changes and varying lava lake levels at Erebus volcano, Antarctica
title_full_unstemmed Terrestrial laser scanning observations of geomorphic changes and varying lava lake levels at Erebus volcano, Antarctica
title_sort terrestrial laser scanning observations of geomorphic changes and varying lava lake levels at erebus volcano, antarctica
publisher Elsevier BV
publishDate 2015
url https://www.repository.cam.ac.uk/handle/1810/247889
long_lat ENVELOPE(166.667,166.667,-77.850,-77.850)
ENVELOPE(-60.199,-60.199,-62.473,-62.473)
ENVELOPE(168.683,168.683,-77.517,-77.517)
ENVELOPE(-128.996,-128.996,55.046,55.046)
ENVELOPE(167.167,167.167,-77.533,-77.533)
ENVELOPE(167.167,167.167,-77.533,-77.533)
geographic McMurdo Station
Dunbar
McIntosh
Lava Lake
Main Crater
Inner Crater
geographic_facet McMurdo Station
Dunbar
McIntosh
Lava Lake
Main Crater
Inner Crater
genre Antarc*
Antarctica
genre_facet Antarc*
Antarctica
op_relation https://www.repository.cam.ac.uk/handle/1810/247889
op_rights Attribution 2.0 UK: England & Wales
http://creativecommons.org/licenses/by/2.0/uk/
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