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Sample: UT1791

Sample ID: UT1791 [1] [2] [3]
Station ID: Sixtymile_River_1
AT Num:
Volcano:
Possible source:
Eruption:
Collector: Westgate, J. A.
Date sampled:
Sample type 1: Tephra Fall
Color: white
Final unit:
Text Description: Gold Run tephra occurs as white pods and lenses, up to 10 cm thick, in the upper part of a thick diamict, which is likely of colluvial origin. From Preece et al. (2011): 0.5 cm thick; pumice with rare blocky grains; in sand and silt; on strath 18 m above the Sixtymile River; 417 cm above top of bench gravel; field name JJO244.
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

[3] Revision of the tephrostratigraphy of the lower Sixtymile River area, Yukon Territory, Canada, 2011

Westgate, J.A., Preece, S.J., and Jackson Jr., L.E., 2011, Revision of the tephrostratigraphy of the lower Sixtymile River area, Yukon Territory, Canada: Canadian Journal of Earth Sciences, v. 48, n. 3, p. 695-701, doi:10.1139/E10-106.