Sample: Westgate_2011_Flat_Creek_Type
| Sample ID: |
Westgate_2011_Flat_Creek_Type [1] |
| Station ID: |
Flat_Creek |
| AT Num: |
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| Volcano: |
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| Possible source: |
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| Eruption: |
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| Collector: |
Froese, D. G. |
| Date sampled: |
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| Sample type 1: |
Tephra Fall |
| Color: |
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| Final unit: |
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| Text Description: |
Flat Creek type tephra from type section. At its type site, the Flat Creek tephra occurs in a stratified diamict, interpreted as a glaciolacustrine debris flow, and has been locally deformed by growth of an ice wedge, now represented as an ice-wedge clast. |
| Sample Location: |
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References Cited
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.