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Using cryptotephras to extend regional tephrochronologies: An example from southeast Alaska and implications for hazard assessment

Published online by Cambridge University Press:  20 January 2017

Richard Payne ,
Jeffrey Blackford  and
Johannes van der Plicht
Richard Payne*
Affiliation:
Department of Geography, Queen Mary, University of London, Mile End Road, London, E1 4NS, UK Department of Biology, University of Bergen, Allègaten 41, N-5007 Bergen, Norway Geography, School of Environment and Development, The University of Manchester, Oxford Road, Manchester, M13 9PL, UK
Jeffrey Blackford*
Affiliation:
Geography, School of Environment and Development, The University of Manchester, Oxford Road, Manchester, M13 9PL, UK
Johannes van der Plicht*
Affiliation:
Centre for Isotope Research, University of Groningen, P.O. Box 72, 9700 AB Groningen, The Netherlands Faculty of Archaeology, Leiden University, The Netherlands
*
*Corresponding author. Geography, School of Environment and Development, The University of Manchester, Oxford Road, Manchester, M13 9PL, UKE-mail addresses:Richard.Payne-2@manchester.ac.uk (R. Payne).
*Corresponding author. Geography, School of Environment and Development, The University of Manchester, Oxford Road, Manchester, M13 9PL, UKE-mail addresses:Richard.Payne-2@manchester.ac.uk (R. Payne).
*Corresponding author. Geography, School of Environment and Development, The University of Manchester, Oxford Road, Manchester, M13 9PL, UKE-mail addresses:Richard.Payne-2@manchester.ac.uk (R. Payne).
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Abstract

Cryptotephrochronology, the use of hidden, diminutive volcanic ash layers to date sediments, has rarely been applied outside western Europe but has the potential to improve the tephrochronology of other regions of the world. Here we present the first comprehensive cryptotephra study in Alaska. Cores were extracted from five peatland sites, with cryptotephras located by ashing and microscopy and their glass geochemistry examined using electron probe microanalysis. Glass geochemical data from nine tephras were compared between sites and with data from previous Alaskan tephra studies. One tephra present in all the cores is believed to represent a previously unidentified eruption of Mt. Churchill and is named here as the ‘Lena tephra’. A mid-Holocene tephra in one site is very similar to Aniakchak tephra and most likely represents a previously unidentified Aniakchak eruption, ca. 5300–5030 cal yr BP. Other tephras are from the late Holocene White River eruption, a mid-Holocene Mt. Churchill eruption, and possibly eruptions of Redoubt and Augustine volcanoes. These results show the potential of cryptotephras to expand the geographic limits of tephrochronology and demonstrate that Mt. Churchill has been more active in the Holocene than previously appreciated. This finding may necessitate reassessment of volcanic hazards in the region.

Keywords

TephraCryptotephraRadiocarbonWhite River AshMt ChurchillAniakchakAlaskaHolocene
Type
Research Article
Information
Quaternary Research , Volume 69 , Issue 1 , January 2008 , pp. 42 - 55
Copyright
Elsevier Inc.

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