This thesis describes the results of a study of 33 tephra layers found within two peat sections near Anchor Point and Homer, Alaska, on the lower Kenai Peninsula. Numerous lower Cook Inlet volcanoes have been active through the Holocene. Tephra layers found at these two sites provide a partial record of their eruptive activity. The hazards that accompany this activity have increased as populations and commercial activities expand and air traffic over the region increases. The tephras analyzed for this study provide an initial geochemical database for the lower Cook Inlet volcanoes. The database is available in electronic format at the U.S. Geological Survey, Alaska Volcano Observatory. The Anchor Point and Homer sections contain tephras from Augustine, Iliamna, and possibly other volcanoes in the region. Anchor Point, the principal section for this study, yielded ten 14C ages ranging from 645 ± 85 cal yr BP at a depth of 14 cm to 8810 ± 205 cal yr BP at 270 cm. Seventeen tephra layers from Anchor Point and 16 from Homer were characterized by stratigraphic position, age, and grain-discrete major-element geochemical analysis by electron microprobe. Nine tephra layers are correlated by geochemical analysis between the Anchor Point and Homer sections. Several newly discovered tephra layers have been correlated with source volcanoes, three with Augustine and at least seven with Iliamna Volcano. The average recurrence interval of tephra fall events at Anchor Point is approximately 520 yrs.
| Identifer | oai:union.ndltd.org:UTAHS/oai:digitalcommons.usu.edu:etd-7783 |
| Date | 01 May 2000 |
| Creators | Lemke, Kathleen J. |
| Publisher | DigitalCommons@USU |
| Source Sets | Utah State University |
| Detected Language | English |
| Type | text |
| Format | application/pdf |
| Source | All Graduate Theses and Dissertations |
| Rights | Copyright for this work is held by the author. Transmission or reproduction of materials protected by copyright beyond that allowed by fair use requires the written permission of the copyright owners. Works not in the public domain cannot be commercially exploited without permission of the copyright owner. Responsibility for any use rests exclusively with the user. For more information contact digitalcommons@usu.edu. |
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