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Marine tephrochronology of the Mt. Edgecumbe Volcanic Field, Southeast Alaska, USA

Published online by Cambridge University Press:  20 January 2017

Jason A. Addison ,
James E. Beget ,
Thomas A. Ager  and
Bruce P. Finney
Jason A. Addison*
Affiliation:
Alaska Quaternary Center and Department of Geology and Geophysics, University of Alaska Fairbanks, 900 Yukon Drive, PO Box 755780, Fairbanks, AK 99775-5780, USA Alaska Quaternary Center, PO Box 755940, University of Alaska Fairbanks, Fairbanks, AK 99775-5940, USA
James E. Beget
Affiliation:
Alaska Quaternary Center and Department of Geology and Geophysics, University of Alaska Fairbanks, 900 Yukon Drive, PO Box 755780, Fairbanks, AK 99775-5780, USA Alaska Quaternary Center, PO Box 755940, University of Alaska Fairbanks, Fairbanks, AK 99775-5940, USA
Thomas A. Ager
Affiliation:
U.S. Geological Survey, Mail Stop 980, Box 25045, Denver Federal Center, Denver, CO 80225, USA
Bruce P. Finney
Affiliation:
Department of Biological Sciences, Idaho State University, Pocatello, ID 83209-8007, USA
*
*Corresponding author. 308 Reichardt Building, AK 99775-5780, USA.E-mail addresses:[email protected] (J.A. Addison), [email protected] (J.E. Beget), [email protected] (T.A. Ager), [email protected] (B.P. Finney).
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Abstract

The Mt. Edgecumbe Volcanic Field (MEVF), located on Kruzof Island near Sitka Sound in southeast Alaska, experienced a large multiple-stage eruption during the last glacial maximum (LGM)-Holocene transition that generated a regionally extensive series of compositionally similar rhyolite tephra horizons and a single well-dated dacite (MEd) tephra. Marine sediment cores collected from adjacent basins to the MEVF contain both tephra-fall and pyroclastic flow deposits that consist primarily of rhyolitic tephra and a minor dacitic tephra unit. The recovered dacite tephra correlates with the MEd tephra, whereas many of the rhyolitic tephras correlate with published MEVF rhyolites. Correlations were based on age constraints and major oxide compositions of glass shards. In addition to LGM-Holocene macroscopic tephra units, four marine cryptotephras were also identified. Three of these units appear to be derived from mid-Holocene MEVF activity, while the youngest cryptotephra corresponds well with the White River Ash eruption at ∼ 1147 cal yr BP. Furthermore, the sedimentology of the Sitka Sound marine core EW0408-40JC and high-resolution SWATH bathymetry both suggest that extensive pyroclastic flow deposits associated with the activity that generated the MEd tephra underlie Sitka Sound, and that any future MEVF activity may pose significant risk to local population centers.

Keywords

TephraAlaskaNorth Pacific OceanCryptotephraMt. EdgecumbeWhite River AshMarine sedimentQuaternaryHoloceneGulf of Alaska
Type
Original Articles
Information
Quaternary Research , Volume 73 , Issue 2 , March 2010 , pp. 277 - 292
Copyright
University of Washington

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References

Barron, J.A., Bukry, D., Dean, W.E., Addison, J.A., Finney, B.P., (2009). Paleoceanography of the Gulf of Alaska during the past 15,000 years: results from diatoms, silicoflagellates, and geochemistry. Marine Micropaleontology 72, 176–195.Google Scholar
Beget, J.E., Keskinen, M.J., (2003). Trace-element geochemistry of individual glass shards of the Old Crow tephra and the age of the Delta glaciation, central Alaska. Quaternary Research 60, 63–69.Google Scholar
Beget, J.E., Motyka, R.J., (1998). New dates on late Pleistocene dacitic tephra from the Mount Edgecumbe volcanic field, southeastern Alaska. Quaternary Research 49, 123–125.CrossRefGoogle Scholar
Beget, J.E., Mason, O., Anderson, P., (1992). Age, extent and climatic significance of the c. 3400"BP Aniakchak tephra, western Alaska, USA. Holocene 2, 51–56.Google Scholar
Beget, J.E., Stihler, S.D., Stone, D.B., (1994). A 500-year-long record of tephra falls from Redoubt volcano and other volcanos in Upper Cook Inlet, Alaska. Journal of Volcanology and Geothermal Research 62, 55–67.Google Scholar
Beget, J., Gardner, C., Davis, K., (2008). Volcanic tsunamis and prehistoric cultural transitions in Cook Inlet, Alaska. Journal of Volcanology and Geothermal Research 176, 377–386.Google Scholar
Blockley, S.P.E., Pyne-O'Donnell, S.D.F., Lowe, J.J., Matthews, I.P., Stone, A., Pollard, A.M., Turney, C.S.M., Molyneux, E.G., (2005). A new and less destructive laboratory procedure for the physical separation of distal glass tephra shards from sediments. Quaternary Science Reviews 24, 1952–1960.Google Scholar
Borchardt, G.A., (1974). The SIMAN coefficient for similarity analysis. Classification Society Bulletin 3, 2–8.Google Scholar
Borchardt, G.A., Aruscavage, P.J., Millard Jr., H.T., (1972). Correlation of the Bishop Ash, a Pleistocene marker bed, using instrumental neutron activation analysis. Journal of Sedimentary Petrology 42, 301–306.Google Scholar
Carey, S., Sigurdsson, H., Mandeville, C.W., Bronto, S., (2000). Volcanic hazards from pyroclastic flow discharge into the sea: examples from the 1883 eruption of Krakatau, Indonesia. McCoy, F.W., Heiken, G., Volcanic Hazards and Disasters in Human Antiquity. Geological Society of America, Boulder, CO., 1–14.Google Scholar
Carey, S., Morelli, D., Sigurdsson, H., Bronto, S., (2001). Tsunami deposits from major explosive eruptions: an example from the 1883 eruption of Krakatau. Geology 29, 347–350.Google Scholar
Child, J.K., Beget, J.E., Werner, A., (1998). Three Holocene tephras identified in lacustrine sediment cores from the Wonder Lake area, Denali National Park and Preserve, Alaska, USA. Arctic and Alpine Research 30, 89–95.Google Scholar
Clague, J.J., Evans, S.G., Rampton, V.N., Woodsworth, G.J., (1995). Improved age estimates for the White River and Bridge River tephras, western Canada. Canadian Journal of Earth Sciences 32, 1172–1179.Google Scholar
Cole, R.B., DeCelles, P.G., (1991). Subaerial to submarine transitions in early Miocene pyroclastic flow deposits, southern San Joaquin basin, California. Geological Society of America Bulletin 103, 221–235.2.3.CO;2>CrossRefGoogle Scholar
Davies, S.M., Hoek, W.Z., Bohncke, S.J.P., Lowe, J.J., O'Donnell, S.P., Turney, C.S.M., (2005). Detection of Lateglacial distal tephra layers in the Netherlands. Boreas 34, 123–135.Google Scholar
Dixon, E.J., Smith, G.S., (1990). A regional application of tephrochronology in Alaska. Lasca, N.P., Donahue, J., Archaeological Geology of North America. Geological Society of America, Boulder, CO., 383–398.Google Scholar
Downes, H., (1985). Evidence for magma heterogeneity in the White River Ash (Yukon Territory). Canadian Journal of Earth Sciences 22, 929–934.Google Scholar
Eberlein, G.D., Churkin Jr., M., (1970). Tlevak Basalt, west coast of Prince of Wales Island, southeastern Alaska. Cohee, G.V., Bates, R.G., Wright, W.B., Changes in stratigraphic nomenclature by the U.S. Geological Survey, 1968. Geological Survey Bulletin 1294-A. United States Government Printing Office, Washington D.C., 25–55.Google Scholar
Engstrom, D.R., Hansen, B.C.S., Wright, H.E., (1990). A possible Younger Dryas record in southeastern Alaska. Science 250, 1383–1385.Google Scholar
Fairbanks, R.G., (1989). A 17,000-year glacio-eustatic sea-level record"influence of glacial melting rates on the Younger Dryas event and deep-ocean circulation. Nature 342, 637–642.Google Scholar
Fierstein, J., (2007). Explosive eruptive record in the Katmai region, Alaska Peninsula: an overview. Bulletin of Volcanology 69, 469–509.Google Scholar
Fisher, R.V., (1979). Models for pyroclastic surges and pyroclastic flows. Journal of Volcanology and Geothermal Research 6, 305–318.Google Scholar
Fisher, D.A., Wake, C.P., Kreutz, K., Yalcin, K., Steig, E.J., Mayewski, P.A., Anderson, L., Zheng, J., Rupper, S., Zdanowicz, C., Demuth, M., Waszkiewicz, M., Dahl-Jensen, D., Goto-Azuma, K., Bourgeois, J.B., Koerner, R., Sekerka, J., Osterberg, E.C., Abbott, M.B., Finney, B., Burns, S.J., (2004). Stable isotope records from Mt. Logan, Eclipse ice cores and nearby Jellybean Lake; water cycle of the North Pacific over 2000 years and over five vertical kilometers; sudden shifts and tropical connections. Geographie Physique et Quaternaire 58, 337–352.Google Scholar
Freundt, A., (2003). Entrance of hot pyroclastic flows into the sea: experimental observations. Bulletin of Volcanology 65, 144–164.Google Scholar
Goldstein, J., Newbury, D.E., Joy, D.C., Lyman, C.E., Echlin, P., Lifshin, E., Sawyer, L.C., Michael, J.R., (2003). Scanning Electron Microscopy and X-ray Microanalysis. Springer Science + Business Media, Inc., New York. Google Scholar
Greene, H.G., O'Connell, V.M., Wakefield, W.W., Brylinsky, C.K., (2007). The offshore Edgecumbe lava field, southeast Alaska: geologic and habitat characterization of a commercial fishing ground. Todd, B.J., Greene, H.G., Mapping the Seafloor for Habitat Characterization. Geological Association of Canada, 277–295.Google Scholar
Grewingk, C., (1850). Geology of Alaska and the Northwest Coast of America. The University of Alaska Press, Fairbanks, AK. Google Scholar
Haberle, S.G., Lumley, S.H., (1998). Age and origin of tephras recorded in postglacial lake sediments to the west of the southern Andes, 44"S to 47"S. Journal of Volcanology and Geothermal Research 84, 239–256.Google Scholar
Hillenbrand, C.D., Moreton, S.G., Caburlotto, A., Pudsey, C.J., Lucchi, R.G., Smellie, J.L., Benetti, S., Grobe, H., Hunt, J.B., Larter, R.D., (2008). Volcanic time-markers for Marine Isotopic Stages 6 and 5 in Southern Ocean sediments and Antarctic ice cores: implications for tephra correlations between palaeoclimatic records. Quaternary Science Reviews 27, 518–540.Google Scholar
Le Bas, M.J., Lemaitre, R.W., Streckeisen, A., Zanettin, B., (1986). A chemical classification of volcanic rocks based on the total alkali silica diagram. Journal of Petrology 27, 745–750.Google Scholar
Lerbekmo, J.F., (2008). The White River Ash: largest Holocene Plinian tephra. Canadian Journal of Earth Sciences 45, 693–700.Google Scholar
Lowe, D.J., (2008). Globalization of tephrochronology: new views from Australasia. Progress in Physical Geography 32, 311–336.Google Scholar
Mashiotta, T.A., Thompson, L.G., Davis, M.E., (2004). The White River Ash: new evidence from the Bona-Churchill ice core record. Eos Trans. AGU 85, Fall Meet. Suppl.,()Abstract PP21A-1369.Google Scholar
McCoy, F.W., Heiken, G., (2000a). The Late-Bronze Age explosive eruption of Thera (Santorini), Greece: regional and local effects. McCoy, F.W., Heiken, G., Volcanic Hazards and Disasters in Human Antiquity. Geological Society of America, Boulder, CO., 43–70.Google Scholar
McCoy, F.W., Heiken, G., (2000b). Tsunami generated by the Late Bronze Age eruption of Thera (Santorini). Greece. Pure and Applied Geophysics 157, 1227–1256.Google Scholar
Miller, T.P., Smith, R.L., (1987). Late Quaternary caldera-forming eruptions in the eastern Aleutian arc, Alaska. Geology 15, 434–438.Google Scholar
Neal, C.A., McGimsey, R.G., Miller, T.P., Riehle, J.R., Waythomas, C.F., (2001). Preliminary volcano-hazard assessment for Aniakchak Volcano, Alaska. US Geological Survey, , Open-File Report. 00-519., Alaska Volcano Observatory, Anchorage, Alaska., 42.Google Scholar
Orton, G.J., (1996). Volcanic environments. Reading, H.G., Sedimentary environments: processes, facies, and stratigraphy. Blackwell Science, Oxford., 485–567.Google Scholar
Payne, R., Blackford, J., (2004). Distal tephra deposits in southeast Alaskan peatlands. Emond, D., Lewis, L., Yukon Exploration and Geology 2003. Whitehorse, Canada, Yukon Geological Survey., 191–197.Google Scholar
Payne, R., Blackford, J., van der Plicht, J., (2008). Using cryptotephras to extend regional tephrochronologies: an example from southeast Alaska and implications for hazard assessment. Quaternary Research 69, 42–55.Google Scholar
Pearce, N.J.G., Bendall, C.A., Westgate, J.A., (2008). Comment on "Some numerical considerations in the geochemical analysis of distal microtephra" by A.M. Pollard, S.P.E. Blockley and C.S. Lane. Applied Geochemistry 23, 1353–1364.Google Scholar
Pinney, D. S., (1993). "Late Quaternary glacial and volcanic stratigraphy near Windy Creek, Katmai National Park, Alaska.". Unpublished M.S. thesis, University of Alaska Fairbanks.Google Scholar
Pinney, D.S., Beget, J.E., (1991). Late Pleistocene volcanic deposits near the Valley of Ten Thousand Smokes, Katmai National Park, Alaska. Reger, R.D., Short Notes on Alaskan Geology 1991. State of Alaska, Division of Geological and Geophysical Surveys, Anchorage, AK, 45–54.Google Scholar
Pollard, A.M., Blockley, S.P.E., Lane, C.S., (2006). Some numerical considerations in the geochemical analysis of distal microtephra. Applied Geochemistry 21, 1692–1714.CrossRefGoogle Scholar
Reger, R.D., Sturmann, A.G., Berg, E.E., Burns, P.A.C., (2007). A guide to the Late Quaternary history of northern and western Kenai Peninsula, Alaska. State of Alaska Dept. of Natural Resources, Division of Geological and Geophysical Surveys, Fairbanks, Alaska., 120.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, G., Manning, S., 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, 0"26"cal kyr BP. Radiocarbon 46, 1029–1058.Google Scholar
Riehle, J.R., Brew, D.A., (1984). Explosive latest Pleistocene(?) and Holocene activity of the Mount Edgecumbe volcanic field, Alaska. Reed, K.M., Bartsch-Winkler, S., The United States Geological Survey in Alaska: accomplishments during 1982. 111–115.Google Scholar
Riehle, J.R., Brew, D.A., Lanphere, M.A., (1989). Geologic map of the Mount Edgecumbe volcanic field, Kruzof Island, southeastern Alaska. Miscellaneous Investigations Series Map I 1983. U.S. Geological Survey, . Google Scholar
Riehle, J.R., Champion, D.E., Brew, D.A., Lanphere, M.A., (1992a). Pyroclastic deposits of the Mount Edgecumbe volcanic field, southeast Alaska: eruptions of a stratified magma chamber. Journal of Volcanology and Geothermal Research 53, 117–143.Google Scholar
Riehle, J.R., Mann, D.H., Peteet, D.M., Engstrom, D.R., Brew, D.A., Meyer, C.E., (1992b). The Mount Edgecumbe tephra deposits, a marker horizon in southeastern Alaska near the Pleistocene Holocene boundary. Quaternary Research 37, 183–202.Google Scholar
Richter, D.H., Preece, S.J., McGimsey, R.G., Westgate, J.A., (1995). Mount Churchill, Alaska: source of the late Holocene White River Ash. Canadian Journal of Earth Sciences 32, 741–748.Google Scholar
Riehle, J. R, Meyer, C. E, and Miyaoka, R. T., (1999). Data on Holocene tephra (volcanic ash) deposits in the Alaska Peninsula and lower Cook Inlet region of the Aleutian volcanic arc, Alaska. USGS Open-File Report 99-135.Google Scholar
Riehle, J.R., Ager, T.A., Reger, R.D., Pinney, D.S., Kaufman, D.S., (2008). Stratigraphic and compositional complexities of the late Quaternary Lethe tephra in South-central Alaska. Quaternary International 178, 210–228.Google Scholar
Robinson, S.D., (2001). Extending the late Holocene White River ash distribution, northwestern Canada. Arctic 54, 157–161.Google Scholar
Rosen, G.P., Jaeger, J.M., Stoner, J.S., Channell, J.E.T., (2005). Establishing the temporal resolution of high-latitude paleoclimatic and paleomagnetic signals in bioturbated Gulf of Alaska continental margin sediments. Eos Trans AGU 86, abstract H51G-0446.Google Scholar
Shane, P., Nairn, I.A., Martin, S.B., Smith, V.C., (2008). Compositional heterogeneity in tephra deposits resulting from the eruption of multiple magma bodies: Implications for tephrochronology. Quaternary International 178, 44–53.Google Scholar
(1993). Shipboard Science Party. Site 887. Rea, D.K., Basov, I.A., Janecek, T.R., Palmer-Julson, A., Proceedings of the Ocean Drilling Program, Initial Reports. Ocean Drilling Program, College Station, TX., 335–391.Google Scholar
Sikes, E.L., Samson, C.R., Guilderson, T.P., Howard, W.R., (2000). Old radiocarbon ages in the southwest Pacific Ocean during the last glacial period and deglaciation. Nature 405, 555–559.Google Scholar
Stoner, J.S., Jennings, A., Kristjansdottir, G.B., Dunhill, G., Andrews, J.T., Hardardottir, J., (2007). A paleomagnetic approach toward refining Holocene radiocarbon-based chronologies: paleoceanographic records from the north Iceland (MD99-2269) and east Greenland (MD99-2322) margins. Paleoceanography 22, 10.1029/2006PA001285.Google Scholar
Stuiver, M., Reimer, P.J., (1993). Extended 14C data base and revised CALIB 3.0 radiocarbon age calibration program. Radiocarbon 35, 137–189.Google Scholar
Telford, R.J., Heegaard, E., Birks, H.J.B., (2004). All age"depth models are wrong: but how badly?. Quaternary Science Reviews 23, 1–5.Google Scholar
Turney, C.S.M., Harkness, D.D., Lowe, J.J., (1997). The use of microtephra horizons to correlate late-glacial lake sediment successions in Scotland. Journal of Quaternary Science 12, 525–531.Google Scholar
Walinsky, S.E., Prahl, F.G., Mix, A.C., Finney, B.P., Jaeger, J.M., Rosen, G.P., (2009). Distribution and composition of organic matter in surface sediments of coastal southeast Alaska. Continental Shelf Research 29, 1565–1579.Google Scholar