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Sample: UT1806

Sample ID: UT1806 [1] [2]
Station ID: Thistle_Creek
AT Num:
Volcano:
Possible source:
Eruption:
Collector: Westgate, J. A.
Date sampled:
Sample type 1: Tephra Fall
Color:
Final unit:
Text Description: Gold Run tephra occurs in the lower part of the lower organic-rich silt bed at this section, and has a normal magnetic polarity, and is deformed in places by loading into the host silts.
Sample Location:

References Cited

[1] Gold Run Tephra: a middle Pleistocene stratigraphic and paleoenvironmental marker across west-central Yukon Territory, Canada, 2009

Westgate, J.A., Preece, S.J., Froese, D.G., Telka, A.M., Storer, J.E., Pearce, N.J.G., Enkin, R.J., Jackson, L.E. Jr., LeBarge, W., and Perkins, W.T., 2009, Gold Run Tephra: a middle Pleistocene stratigraphic and paleoenvironmental marker across west-central Yukon Territory, Canada: Canadian Journal of Earth Sciences, v. 46, n. 6, p. 465-478, doi:10.1139/E09-029.

[2] 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