Volcanic, tectonic, and tsunamigenic events recorded in peats near Millers Landing, Homer, Alaska

Thesis (M.S.) University of Alaska Fairbanks, 2006 The Millers Landing peat deposit is located on the western side of Kachemak Bay, near Homer, Alaska. Distal tephra deposits from past eruptions of Augustine Volcano, Redoubt Volcano, Spurr Volcano, and Katmai Volcano are preserved within the peat. E...

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Main Author: Davis, Kathleen Melissa
Format: Thesis
Language:English
Published: 2006
Subjects:
Online Access:http://hdl.handle.net/11122/5781
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spelling ftunivalaska:oai:scholarworks.alaska.edu:11122/5781 2023-05-15T16:57:47+02:00 Volcanic, tectonic, and tsunamigenic events recorded in peats near Millers Landing, Homer, Alaska Davis, Kathleen Melissa 2006-05 http://hdl.handle.net/11122/5781 en_US eng http://hdl.handle.net/11122/5781 Department of Geology and Geophysics Thesis ms 2006 ftunivalaska 2023-02-23T21:36:30Z Thesis (M.S.) University of Alaska Fairbanks, 2006 The Millers Landing peat deposit is located on the western side of Kachemak Bay, near Homer, Alaska. Distal tephra deposits from past eruptions of Augustine Volcano, Redoubt Volcano, Spurr Volcano, and Katmai Volcano are preserved within the peat. Evidence of active tectonism is found where a meter of marine silt overlies the peat deposits at Millers Landing. The marine mud deposits record co-seismic subsidence and post-seismic uplift as a result of a prehistoric great earthquake, ca. 1000 yr. B.P. along the northern Pacific plate boundary along the subduction interface. The uplift rate of Millers Landing over the past 1000 years has a minimum uplift rate of 3.0 mm/yr. Since 1995 Millers Landing has been an experiencing a post-seismic uplift rate of 5.4 +/- 0.6 mm/yr from the 1964 Prince William Sound earthquake. The Millers Landing peat deposits also contained nine layers of sand and beach gravel. The sedimentology is identical to classic tsunami depositional facies that have been identified in other tectonically active areas and we interpret these deposits as evidence of prehistoric tsunami events. The upper layer of two thick sand units, dated at ca. 3600 yr. B.P. by radiocarbon dating, is directly overlain by a 1.2 cm thick grayish white tephra. The tephra is from Redoubt Volcano and records a tsunami triggered by Mt. Redoubt's debris avalanche and lahar which are also dated at 3600 yrs B.P. The other sand deposits present within the peat are evidence of tectonically-triggered tsunamis. The recognition of tephras, tsunami deposits, and evidence of prehistoric co-seismic subsidence indicates the potential for geohazard assessment of Millers Landing and the entire Homer, Alaska region. Thesis Kachemak Alaska University of Alaska: ScholarWorks@UA Fairbanks Landing The ENVELOPE(161.417,161.417,-78.367,-78.367) Pacific
institution Open Polar
collection University of Alaska: ScholarWorks@UA
op_collection_id ftunivalaska
language English
description Thesis (M.S.) University of Alaska Fairbanks, 2006 The Millers Landing peat deposit is located on the western side of Kachemak Bay, near Homer, Alaska. Distal tephra deposits from past eruptions of Augustine Volcano, Redoubt Volcano, Spurr Volcano, and Katmai Volcano are preserved within the peat. Evidence of active tectonism is found where a meter of marine silt overlies the peat deposits at Millers Landing. The marine mud deposits record co-seismic subsidence and post-seismic uplift as a result of a prehistoric great earthquake, ca. 1000 yr. B.P. along the northern Pacific plate boundary along the subduction interface. The uplift rate of Millers Landing over the past 1000 years has a minimum uplift rate of 3.0 mm/yr. Since 1995 Millers Landing has been an experiencing a post-seismic uplift rate of 5.4 +/- 0.6 mm/yr from the 1964 Prince William Sound earthquake. The Millers Landing peat deposits also contained nine layers of sand and beach gravel. The sedimentology is identical to classic tsunami depositional facies that have been identified in other tectonically active areas and we interpret these deposits as evidence of prehistoric tsunami events. The upper layer of two thick sand units, dated at ca. 3600 yr. B.P. by radiocarbon dating, is directly overlain by a 1.2 cm thick grayish white tephra. The tephra is from Redoubt Volcano and records a tsunami triggered by Mt. Redoubt's debris avalanche and lahar which are also dated at 3600 yrs B.P. The other sand deposits present within the peat are evidence of tectonically-triggered tsunamis. The recognition of tephras, tsunami deposits, and evidence of prehistoric co-seismic subsidence indicates the potential for geohazard assessment of Millers Landing and the entire Homer, Alaska region.
format Thesis
author Davis, Kathleen Melissa
spellingShingle Davis, Kathleen Melissa
Volcanic, tectonic, and tsunamigenic events recorded in peats near Millers Landing, Homer, Alaska
author_facet Davis, Kathleen Melissa
author_sort Davis, Kathleen Melissa
title Volcanic, tectonic, and tsunamigenic events recorded in peats near Millers Landing, Homer, Alaska
title_short Volcanic, tectonic, and tsunamigenic events recorded in peats near Millers Landing, Homer, Alaska
title_full Volcanic, tectonic, and tsunamigenic events recorded in peats near Millers Landing, Homer, Alaska
title_fullStr Volcanic, tectonic, and tsunamigenic events recorded in peats near Millers Landing, Homer, Alaska
title_full_unstemmed Volcanic, tectonic, and tsunamigenic events recorded in peats near Millers Landing, Homer, Alaska
title_sort volcanic, tectonic, and tsunamigenic events recorded in peats near millers landing, homer, alaska
publishDate 2006
url http://hdl.handle.net/11122/5781
long_lat ENVELOPE(161.417,161.417,-78.367,-78.367)
geographic Fairbanks
Landing The
Pacific
geographic_facet Fairbanks
Landing The
Pacific
genre Kachemak
Alaska
genre_facet Kachemak
Alaska
op_relation http://hdl.handle.net/11122/5781
Department of Geology and Geophysics
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