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Late Quaternary distal tephra-fall deposits in lacustrine sediments, Kenai Peninsula, Alaska

Published online by Cambridge University Press:  20 January 2017

Christian S. de Fontaine ,
Darrell S. Kaufman ,
R. Scott Anderson ,
Al Werner ,
Christopher F. Waythomas  and
Thomas A. Brown
Christian S. de Fontaine
Affiliation:
Department of Geology, Northern Arizona University, Flagstaff, AZ 86011-4099, USA
Darrell S. Kaufman*
Affiliation:
Department of Geology/Center for Environmental Sciences and Education, Northern Arizona University, Flagstaff, AZ 86011-4099, USA
R. Scott Anderson
Affiliation:
Center for Environmental Sciences and Education/Quaternary Sciences Program, Northern Arizona University, Flagstaff, AZ 86011-5694, USA
Al Werner
Affiliation:
Department of Earth and Environment, Mount Holyoke College, South Hadley, MA 01075, USA
Christopher F. Waythomas
Affiliation:
U.S. Geological Survey and Alaska Volcano Observatory, 4230 University Drive, Suite 201, Anchorage, AK 99508, USA
Thomas A. Brown
Affiliation:
Center for Accelerator Mass Spectrometry, Lawrence Livermore National Laboratory, L-397, 7000 East Avenue, Livermore, CA 94551, USA
*
*Corresponding author. Fax: +1 928 523 9220.E-mail address:[email protected] (D.S. Kaufman)
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Abstract

Tephra-fall deposits from Cook Inlet volcanoes were detected in sediment cores from Tustumena and Paradox Lakes, Kenai Peninsula, Alaska, using magnetic susceptibility and petrography. The ages of tephra layers were estimated using 21 14C ages on macrofossils. Tephras layers are typically fine, gray ash, 1–5 mm thick, and composed of varying proportions of glass shards, pumice, and glass-coated phenocrysts. Of the two lakes, Paradox Lake contained a higher frequency of tephra (0.8 tephra/100 yr; 109 over the 13,200-yr record). The unusually large number of tephra in this lake relative to others previously studied in the area is attributed to the lake's physiography, sedimentology, and limnology. The frequency of ash fall was not constant through the Holocene. In Paradox Lake, tephra layers are absent between ca. 800–2200, 3800–4800, and 9000–10,300 cal yr BP, despite continuously layered lacustrine sediment. In contrast, between 5000 and 9000 cal yr BP, an average of 1.7 tephra layers are present per 100 yr. The peak period of tephra fall (7000–9000 cal yr BP; 2.6 tephra/100 yr) in Paradox Lake is consistent with the increase in volcanism between 7000 and 9000 yr ago recorded in the Greenland ice cores.

Keywords

TephraLacustrine sedimentVolcanic ashAsh fallTephrochronologyLate QuaternaryCook InletAlaska
Type
Research Article
Information
Quaternary Research , Volume 68 , Issue 1 , July 2007 , pp. 64 - 78
Copyright
University of Washington

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References

Ager, T.A., Sims, J.D.(1984). Postglacial pollen and tephra records from lakes in the Cook Inlet region, southern Alaska. Conrad, W.L., Elliot, R.L. The United States Geological Survey in Alaska: Accomplishments during 1981 U.S. Geological Survey Circular 868, 103–105.Google Scholar
Anderson, R.Y., Nuhfer, E.B., Dean, W.E.(1985). Sinking of volcanic ash in uncompacted sediment in Williams Lake, Washington. Science, 225, 505–508.Google Scholar
Anderson, R.S., Hallett, D.J., Berg, E., Jass, R.B., Toney, J.L., de Fontaine, C.S., DeVolder, A.(2006). Holocene development of boreal forest and fire regimes on the Kenai Lowlands of Alaska. The Holocene, 16, 791–803.Google Scholar
Begét, J.E., Stihler, S.D., Stone, D.B.("t et al., 1994). A 500-year-long record of tephra falls from Redoubt Volcanoand other volcanoes in upper Cook Inlet, Alaska. Journal of Volcanology and Geothermal Research, 62, 55–67.CrossRefGoogle Scholar
Beierle, B., Bond, J.(2002). Density-induced settling of tephra through organic lake sediments. Journal of Paleolimnology, 28, 4 433–440.Google Scholar
Bradley, D.C., Wilson, F.H.(1998). Reconnaissance bedrock geology of the southeastern part of the Kenai Quadrangle, Alaska. Kelley, K.D., Gough, L.P. Geologic Studies in Alaska by the U.S. Geological Survey, 1998 U.S. Geological Survey Professional Paper 1615, 59–63.Google Scholar
Braitseva, O.A., Melekestsev, I.V., Ponomareva, V.V., Sulerzhitsky, L.D.(1995). Ages of calderas, large explosive craters and active volcanoes in the Kuril–Kamchatka region, Russia. Bulletin of Volcanology, 57, 6 383–402.Google Scholar
de Fontaine, C.S. (2003). Late Quaternary distal tephra in lacustrine sediments of the upper Cook Inlet [M.S. thesis]. Northern Arizona University, Flagstaff, AZ.111pp.Google Scholar
Fierstein, J, Hildreth, W.(2000). Preliminary volcano-hazard assessment for the Katmai volcanic cluster. Alaska. U. S..Geological Survey Open-File Report 00-489., Google Scholar
Hancock, J.R., Werner, A.(2002). A Holocene ash-fall reconstruction for Anchorage, Alaska. Geological Society of America Abstracts with Programs, 34, 12 Google Scholar
Heegaard, E., Birks, H.J.B., Telford, R.J.(2005). Relationships between calibrated ages and depth in stratigraphical sequences: an estimation procedure by mixed-effect regression. The Holocene, 15, 612–618.Google Scholar
Kathan, K.M., Werner, A., Kaufman, D.S., de Fontaine, C., Kingsbury, E.M.(2004). Intrabasinal variability of Holocene tephra in a small kettle lake, Lorraine Lake, upper Cook Inlet, Alaska. Geological Society of America Abstracts with Programs (Northeastern and Southeastern Section Joint Meeting), 36, 2 Google Scholar
Lacasse, C. (2001). Influence of climate variability on the atmospheric transport of Icelandic tephra in the subpolar North Atlantic. Global and Planetary Change, 29, 31–55.Google Scholar
Lemke, K.J. (2000). Holocene tephrostratigraphy, southern Kenai Peninsula, lower Cook Inlet, Alaska [M.S. thesis]. Utah State University, Logan.96pp.Google Scholar
Lowe, D.J., Hunt, J.B.(2001). A summary of terminology used in tephra related studies. Juvigné, E.T., Raynal, J.-P. Tephras: Chronology, Archaeology. CDERAD éditeur: Goudet, 1, Les Dossiers de l'Archeo-Logis, 17–22.Google Scholar
Mason, B.G., Pyle, D.M., Dade, W.B., Jupp, T.(2004). Seasonality of volcanic eruptions. Journal of Geophysical Research, 109, B04206 CrossRefGoogle Scholar
McGimsey, R.G., Neal, C.A., Riley, C.M.(2001). Areal distribution, thickness, mass, volume, and grain size of tephra-fall deposits from the eruptions of Crater Peak vent, Mt. Spurr Volcano. Alaska. U.S0.Geological Survey Open-File Report 01-370, 32 pp.Google Scholar
Miller, T.P., McGimsey, R.G., Richter, D.H., Riehle, J.R., Nye, C.J., Yount, M.E., Dumoulin, J.A.(1998). Catalog of the historically active volcanoes of Alaska. U.S. Geological Survey Open-File Report OF 98-0582, 104 pp.Google Scholar
Nakada, M., Yokose, H.(1992). Ice age as a trigger of active Quaternary volcanism and tectonism. Tectonophysics, 212, 321–329.Google Scholar
Nowaczyk, N.R. (2001). Logging of magnetic susceptibility. Last, W.M., Smol, J.P. Tracking environmental change using lake sediments, Volume 1: Basin analysis, coring, and chronological techniques Kluwer Academic Publishers, Dordrecht.75–97.Google Scholar
Oswald, W.W., Anderson, P.M., Brown, T.A., Brubaker, L.B., Hu, F.S., Lozhkin, A.V., Tinner, W., Kaltenrieder, P.(2005). Effects of sample mass and macrofossil type on radiocarbon dating of arctic and boreal lake sediments. The Holocene, 15, 5 758–767.Google Scholar
Pearce, N.J.G., Westgate, J.A., Preece, S.J., Eastwood, W.J., Perkins, W.T.(2004). Identification of Aniakchak (Alaska) tephra in Greenland ice core challenges the 1645 BC date for Minoan eruption of Santorini. Geochemistry, Geophysics, Geosystems, 5, 5 Q03005 Google Scholar
Pyne-O'Donnell, S.D.F. (, 2003). The factors affecting distribution and preservation of microtephra particles in late glacial sediments. XVI INQUA Congress Programs with Abstracts 146 Google Scholar
Rampino, M.R., Self, S., Fairbridge, R.W.(1979). Can rapid climatic change cause volcanic eruptions?. Science, 206, 826–829.Google Scholar
Reimer, P.J., Baillie, M.G.L., Bard, E., Bayliss, A., Beck, J.W., Bertrand, C.J.H., Blackwell, P.G., Buck, C.E., Burr, G.S., Cutler, K.B., Damon, P.E., Edwards, R.L., Fairbanks, R.G., Friedrich, M., Guilderson, T.P., Hogg, A.G., Hughen, K.A., Kromer, B., McCormac, F.G., Manning, S.W., Ramsey, C.B., Reimer, R.W., Remmele, S., Southon, J.R., Stuiver, M., Talamo, S., Taylor, F.W., van der Plicht, J., Weyhenmeyer, C.E.(2004). IntCal04 Terrestrial radiocarbon age calibration, 26–0 ka BP. Radiocarbon, 46, 1029–1058.Google Scholar
Riehle, J.R. (1985). A reconnaissance of the major Holocene tephra deposits in the upper Cook Inlet region, Alaska. Journal of Volcanology and Geothermal Research, 26, 37–74.Google Scholar
Riehle, J.R., Bowers, P.M., Ager, T.A.(1990). The Hayes tephra deposits, an upper Holocene marker horizon in south-central Alaska. Quaternary Research, 33, 276–290.Google Scholar
Rymer, M.J., Sims, J.D.(1982). Lake-sediment evidence for the date of deglaciation of the Hidden Lake area, Kenai Peninsula, Alaska. Geology, 10, 314–316.Google Scholar
Sarna-Wojcicki, A.M. (2000). Tephrochronology. Noller, J.S., Sowers, J.M., Lettis, W.R. Quaternary geochronology: methods and applications, vol. 4, American Geophysical Union, AGU Reference Shelf.357–377.Google Scholar
Scott, W.E., McGimsey, R.G.(1994). Character, mass, distribution, and origin of tephra-fall deposits of the 1989–1990 eruption of Redoubt Volcano, south-central Alaska. Journal of Volcanology and Geothermal Research, 62, 251–272.Google Scholar
Stone, D.B., Nye, C.J., Stihler, S.D.(1990). Tephra layers and magnetic susceptibility measurements in lake sediments: Cook Inlet volcanism from pre-history to the present. Eos, Transactions, American Geophysical Union, 71, 1710 Google Scholar
Stuiver, M., Reimer, P.J.(1993). Extended 14-C database and revised CALIB 3.0 14-C age calibration program. Radiocarbon, 35, 215–230.Google Scholar
Swanson, S.E., Kienle, J.(1988). The 1986 eruption of Mount St. Augustine; field test of a hazard evaluation. Journal of Geophysical Research, 93, 4500–4520.CrossRefGoogle Scholar
Waythomas, C.F., Nye, C.J.(2002). Preliminary volcano-hazard assessment for Mount Spurr Volcano, Alaska. U.S.. Geological Survey Open-File Report 01-482., 40 pp.Google Scholar
Waythomas, C.F., Waitt, R.B.(1998). Preliminary volcano-hazard assessment for Augustine Volcano, Alaska. U.S.. Geological Survey Open-File Report 98-0106., 39 pp.Google Scholar
Waythomas, C.F., Dorava, J.M., Miller, T.P., Neal, C.A., McGimsey, R.G.(1997). Preliminary volcano-hazard assessment for Redoubt Volcano, Alaska. U.S.. Geological Survey Open-File Report 97-857., Google Scholar
Werner, A., Kathan, K.M., Kaufman, D.S., Hancock, J.R., Waythomas, C.F., Wallace, K.L.(2004). Using kettle lake records to date and interpret Holocene ash deposition in upper Cook Inlet, Anchorage, AK. Eos, Transactions, American Geophysical Union, 85, 47 Google Scholar
Zielinski, G.A. (2000). Use of paleo-records in determining variability within the volcanism–climate system. Quaternary Science Reviews, 19, 417–438.Google Scholar
Zielinski, G.A., Mayewski, P.A., Meeker, L.D., Whitlow, S., Twickler, M.S., Morrison, M., Meese, D.A., Gow, A.J., Alley, R.B.(1994). Record of volcanism since 7000 B.C. from the GISP2 Greenland ice core and implications for the volcano–climate system. Science, 264, 948–952.Google Scholar
Zielinski, G.A., Mayewski, P.A., Meeker, L.D., Whitlow, S., Twickler, M.S.(1996). A 110,000-yr record of explosive volcanism from the GISP2 (Greenland) ice core. Quaternary Research, 45, 109–118.CrossRefGoogle Scholar