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SAMPLE INFO : Froese_2003_Chester_Bluff_Charley_River_tephra_ave
Sample ID:Froese_2003_Chester_Bluff_Charley_River_tephra_ave
Station ID:Froese_2003_Chester_Bluff_tephra_averages
Latitude:65.33
Longitude:-142.73997
Datum:NAD83
Sample Type 1:Tephra Fall
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:
Recurring middle Pleistocene outburst floods in east-central Alaska

GEOCHEM DATA
StationIDLatitudeLongitudeGeologistDateVisitedAge InfoVolcanoEruptionLocation DescriptionText DescriptionSample IDSample Type 1Sample Type 2Final UnitMaterialCoeffSiO2TiO2Al2O3FeOTMnOMgOCaONa2OK2OP2O5Total-majorsREF majorsMETH majorsFe2O3/Fe203T origFeO/FeOT origVolatiles csvMETH volatilesCsRbBaSrLaCePrNdSmEuGdTbDyHoErTmYbLuYZrNbHfTaPbThUScVCrFeCoNiCuZnGaMoAsNaKRef trace1METH trace1RbBaSrLaCeNdSmEuGdDyErYbLuYZrNbPbThUScTiVCrNiCuZnGaRef trace2METH trace2Light csvHalogen csvother major csvother lile csvother ree csvother hfse csvother hpe csvother tm csvother misc csv
Froese_2003_Chester_Bluff_tephra_averages65.33-142.73997Froese, 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_aveTephra FallCumulateGlass 72.58 0.23 15.75 1.71 0.08 0.56 2.04 4.54 2.44 10291EMP1.71Cl=0.07; H2O=5.67EMP

SAMPLE LOCATION

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