Sample: Y-102
| Sample ID: | Y-102 [1] |
| Station ID: | Y-102 |
| AT Num: | |
| Volcano: | Kaguyak |
| Possible source: | |
| Eruption: | Kaguyak CFE |
| Collector: | Fierstein, J. E. |
| Date sampled: | 2000-00-00 |
| Sample type 1: | pyroclastic density current |
| Color: | |
| Final unit: | |
| Text Description: | Kaguyak Ignimbrite. tall bluffs of ignimbrite; lower 10 m of exposure is massive ignimbrite, but there are 7 well-defined PCZ zones in the upper 2/3 of the section as well as a few less-well defined zones. Exposed thickness 25-30 m. PCZs 0.75-1.5 m. LCZ: 0.75-1.5 m. See text for MC and ML. Pumice clasts: white to buff pumice most common, but grey scoria is present, and there is abundant banded pumice here; markedly more than at other locations. Lithic clasts: most lithics are grey dacite lava; there is a minor amount of clasts with yellow-orange altered rinds or films |
| Sample Location: |
References Cited
[1] Kaguyak dome field and its Holocene caldera, Alaska Peninsula, 2008
Fierstein, Judy, and Hildreth, Wes, 2008, Kaguyak dome field and its Holocene caldera, Alaska Peninsula: Journal of Volcanology and Geothermal Research, v. 177, n. 2, p. 340-366, doi:10.1016/j.jvolgeores.2008.05.016 .
full-text PDF 3.16 MB