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Text Description: Charley River tephra consists mostly of fine-grained pumiceous glass with a small amount of blocky, poorly vesicular glass. It is heavily contaminated with detrital minerals, but a few primary grains of feldspar, FeTi oxides, biotite, hornblende, orthopyroxene, and apatite were identified. The composition reported here is the average of four samples from the Chester Bluff area: UT1667, UT1677, UT1683, and UT1745. 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 | > 560000 ± 80000 glass - FT; 10291; Weighted mean of two diameter-corrected fission-track ages obtained on sample of the GI tephra (UT802). The Charley River tephra occurs stratigraphically below the GI tephra and is therefore older. | 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. | Charley River tephra consists mostly of fine-grained pumiceous glass with a small amount of blocky, poorly vesicular glass. It is heavily contaminated with detrital minerals, but a few primary grains of feldspar, FeTi oxides, biotite, hornblende, orthopyroxene, and apatite were identified. The composition reported here is the average of four samples from the Chester Bluff area: UT1667, UT1677, UT1683, and UT1745. | Froese_2003_Chester_Bluff_Charley_River_tephra_ave | Tephra Fall | Cumulate | Glass | 72.58 | 0.23 | 15.75 | 1.71 | 0.08 | 0.56 | 2.04 | 4.54 | 2.44 | 10291 | EMP | 1.71 | Cl=0.07; H2O=5.67 | EMP |
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