Sample: Preece_2000_Klondike_District_Little_Blanche_Creek
Sample ID: |
Preece_2000_Klondike_District_Little_Blanche_Creek [1] [2] |
Station ID: |
Klondike_District_Regional_Tephra |
AT Num: |
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Volcano: |
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Possible source: |
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Eruption: |
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Collector: |
Preece, S. J. |
Date sampled: |
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Sample type 1: |
Tephra Fall |
Color: |
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Final unit: |
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Text Description: |
Associated with sands and gravels, but the stratigraphic identity of the host sediments is uncertain. The composition reported here is the average of two samples: UT1054, UT1455. Type II beds have more crystals than type I beds, and the glass is mainly in the form of highly inflated pumice. Feldspar, orthopyroxene, and green amphibole are common with minor or trace amounts of red amphibole, clinopyroxene, iron-titanium oxides, apatite, and zircon. |
Sample Location: |
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References Cited
Preece, S. J., Westgate, J. A., Alloway, B. V., and Milner, M. W., 2000, Characterization, identity, distribution, and source of late Cenozoic tephra beds in the Klondike District of the Yukon, Canada: Canadian Journal of Earth Sciences, v. 37, n. 7, p. 983-996.
Froese, D.G, Westgate, J.A., and Alloway, B.V., (eds.), 2005, Field trip guide for the International Field Conference and Workshop on Tephrochronology and Volcanism: Institute of Geological and Nuclear Sciences Science Report 2005/26, Dawson City, Yukon Territory, Canada, July 31-August 8, 2005, 132 p.