Sample: Carson_Cold_Bay_Regional_Tephra _B
Sample ID: |
Carson_Cold_Bay_Regional_Tephra _B [1] [2] |
Station ID: |
Cold_Bay_Regional_Tephra |
AT Num: |
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Volcano: |
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Possible source: |
Roundtop |
Eruption: |
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Collector: |
Carson, E. C. |
Date sampled: |
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Sample type 1: |
Tephra Fall |
Color: |
gray to light brown |
Final unit: |
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Text Description: |
Average calculated from analyses of seven individual samples from seven different locations (see individual samples for description): 96TDS3A, 96JF9A, 96TDS15Q, 97EC18N, 96TDS30A, 96TDS33A, 97EC15E (see Figure 14a in Carson 1998). Scattered 1-2 cm pumice lapilli, gray to light brown, dispersed in a 10-15 cm thick sediment horizon. Tephra collected from beneath the Funk/Fisher ash or directly above the late Wisconsin diamicton. Composed of easily recognizable 1-2 cm lapilli fragments evenly dispersed within a layer of non-volcanic (typically eolian) interstitial sediment. |
Sample Location: |
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References Cited
Carson, E. C., 1998, Holocene tephrochronology of the Cold Bay area, Southwest Alaska Peninsula: University of Wisconsin-Madison unpublished M.S. thesis, 178 p.
Carson, E. C., Fournelle, J. H., Miller, T. P., and Mickelson, D. M., 2002, Holocene tephrochronology of the Cold Bay area, southwest Alaska Peninsula: Quaternary Science Reviews, v. 21, n. 20-22, p. 2213-2228.