Station: WM97-61

Station ID: WM97-61 [1] [2] [3] [4] [5] [6] [7] [8] [9] [10]
Volcano:
Collector: Unknown, Unknown
Date visited:
NAD83 latitude: 58.7938
NAD83 longitude: -161.1875
Default location: No
Location description: Togiak Bay, Alaska. Datum not specified, assumed to be NAD83.
Station Location:
Samples:

References Cited

[1] Late Pliocene Dawson Cut forest bed and new tephrochronological findings in the Gold Hill Loess, east-central Alaska, 2009

Pewe, T.L., Westgate, J.A., Preece, S.J., Brown, P.M., and Leavitt, S.W., 2009, Late Pliocene Dawson Cut forest bed and new tephrochronological findings in the Gold Hill Loess, east-central Alaska: Geological Society of America Bulletin, v. 121, n. 1-2, p. 294-320, doi: 10.1130/B26323.1 .

[2] Old Crow tephra across eastern Beringia: a single cataclysmic eruption at the close of Marine Isotope Stage 6, 2011

Preece, S.J., Pearce, N.J.G., Westgate, J.A., Froese, D.G., Jensen, B.J.L., and Perkins, W.T., 2011, Old Crow tephra across eastern Beringia: a single cataclysmic eruption at the close of Marine Isotope Stage 6: Quaternary Science Reviews, v. 30, p. 2069-2099, doi:10.1016/j.quascirev.2010.04.020 .

[3] The Palisades is a key reference site for the middle Pleistocene of eastern Beringia: new evidence from paleomagnetics and regional tephrostratigraphy, 2013

Jensen, B.J.L., Reyes, A.V., Froese, D.G., and Stone, D.B., 2013, The Palisades is a key reference site for the middle Pleistocene of eastern Beringia: new evidence from paleomagnetics and regional tephrostratigraphy: Quaternary Science Reviews, v. 63, p. 91-108, http://dx.doi.org/10.1016/j.quascirev.2012.11.035

[4] The last interglacial to glacial transition, Togiak Bay, southwestern Alaska, 2001

Kaufman, D.S., Manley, W.F., Wolfe, A.P., Hu, F.S., Preece, S.J., Westgate, J.A., and Forman, S.L., 2001, The last interglacial to glacial transition, Togiak Bay, southwestern Alaska: Quaternary Research, v. 55, n. 2, p. 190-202.

[5] Permafrost response to last interglacial warming: field evidence from non-glaciated Yukon and Alaska, 2010

Reyes, A.V., Froese, D.G., and Jensen, B.L., 2010, Permafrost response to last interglacial warming: field evidence from non-glaciated Yukon and Alaska: Quaternary Science Reviews, v. 29, n. 23024, p. 3256-3274, doi: 10.1016/j.quascirev.2010.07.013 .

[6] A catalogue of late Cenozoic tephra beds in the Klondike Goldfields and adjacent areas, Yukon Territory, 2011

Preece, S.J., Westgate, J.A., Froese, D.G., Pearce, N.J.G., and Perkins, W.T., 2011, A catalogue of late Cenozoic tephra beds in the Klondike Goldfields and adjacent areas, Yukon Territory: Canadian Journal of Earth Sciences, v. 48, p. 1386-1418, doi: 10.1139/e10-110

[7] The application of ICP-MS methods to tephrochronological problems, 2004

Pearce, N.J.G., Westgate, J.A., Perkins, W.T., and Preece, S.J., 2004, The application of ICP-MS methods to tephrochronological problems: Applied Geochemistry, v. 19, n. 3, p. 289-322, doi: 10.1016/S0883-2927(03)00153-7 .

[8] Identification of last interglacial deposits in eastern Beringia: a cautionary note from the Palisades, interior Alaska, 2011

Reyes, A.V., Zazula, G.D., Kuzmina, S., Ager, T.A., Froese, D.G., 2011, Identification of last interglacial deposits in eastern Beringia: a cautionary note from the Palisades, interior Alaska: Journal of Quaternary Science, v. 26, n. 3, p. 345-352.

[9] Old Crow tephra (140 ± 10 ka) constrains penultimate Reid glaciation in central Yukon Territory, 2008

Ward, B.C., Bond, J.D., Froese, D., and Jensen, Britta, 2008, Old Crow tephra (140+/-10 ka) constrains penultimate Reid glaciation in central Yukon Territory: Quaternary Science Reviews, v. 27, p. 1909-1915.

[10] Holocene tephras in lake cores from northern British Columbia, Canada, 2008

Lakeman, T.R., Clague, J.J., Menounos, Brian, Osborn, G.D., Jensen, B.J.L., Froese, D.G., 2008, Holocene tephras in lake cores from northern British Columbia, Canada: Canadian Journal of Earth Science, v. 45, p. 935-947.