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Text Description: GI tephra occurs at site B approximately 8 m above the newly identified Charley River tephra that is also present at site A. GI tephra consists mostly of colorless, bubble-wall glass shards with some brown glass and pumice fragments. Mineral grains, which are sparse, include feldspar, apatite, and orthopyroxene. The composition reported here is the average of two samples from the Chester Bluff area: UT1666 and UT1743. Two populations of glass identified by Froese et al. (2003), and a single point with a different composition. References: ![]() |
StationID | Latitude | Longitude | Geologist | DateVisited | Age Info | Volcano | Eruption | Location Description | Text Description | Sample ID | Sample Type 1 | Sample Type 2 | Final Unit | Material | Coeff | SiO2 | TiO2 | Al2O3 | FeOT | MnO | MgO | CaO | Na2O | K2O | P2O5 | Total-majors | REF majors | METH majors | Fe2O3/Fe203T orig | FeO/FeOT orig | Volatiles csv | METH volatiles | Cs | Rb | Ba | Sr | La | Ce | Pr | Nd | Sm | Eu | Gd | Tb | Dy | Ho | Er | Tm | Yb | Lu | Y | Zr | Nb | Hf | Ta | Pb | Th | U | Sc | V | Cr | Fe | Co | Ni | Cu | Zn | Ga | Mo | As | Na | K | Ref trace1 | METH trace1 | Rb | Ba | Sr | La | Ce | Nd | Sm | Eu | Gd | Dy | Er | Yb | Lu | Y | Zr | Nb | Pb | Th | U | Sc | Ti | V | Cr | Ni | Cu | Zn | Ga | Ref trace2 | METH trace2 | Light csv | Halogen csv | other major csv | other lile csv | other ree csv | other hfse csv | other hpe csv | other tm csv | other misc csv | |
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Froese_2003_Chester_Bluff_tephra_averages | 65.33 | -142.73997 | Froese, D. G. | 1999-01-01 | Exposures at Chester Bluff on the north side of the Yukon River opposite the mouth of the Charley River, Alaska. Location imprecisely georeferenced from Figure 2 of Froese et al. (2003). Glass compositions are averages calculated from analyses of multiple tephra samples from the same tephra beds in the area. Individual sample IDs (analyses of which contribute to the average tephra bed composition) are noted in the sample descriptions. | GI tephra occurs at site B approximately 8 m above the newly identified Charley River tephra that is also present at site A. GI tephra consists mostly of colorless, bubble-wall glass shards with some brown glass and pumice fragments. Mineral grains, which are sparse, include feldspar, apatite, and orthopyroxene. The composition reported here is the average of two samples from the Chester Bluff area: UT1666 and UT1743. Two populations of glass identified by Froese et al. (2003), and a single point with a different composition. | Froese_2003_Chester_Bluff_GI_tephra_average-P2 | Tephra Fall | Cumulate | Glass | 70.3 | 0.62 | 14.48 | 3.47 | 0.1 | 0.53 | 1.99 | 4.45 | 3.85 | 10291 | EMP | 3.47 | Cl=0.2; H2O=4.46 | EMP |
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