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SAMPLE INFO : Jensen_2011_Jackson_Hill_VT_tephra_average
Sample ID:Jensen_2011_Jackson_Hill_VT_tephra_average
Station ID:Jackson_Hill
Latitude:64.016
Longitude:-139.366
Datum:NAD83
Sample Type 1:Tephra Fall
Text Description:
Glass major element oxide composition reported is the average of analyses of three samples of VT tephra from Jackson Hill: UA1580, UT1562, and UT1637. Individual sample IDs analyzed for glass trace element composition are not reported.

References:
The variegated (VT) tephra: A new regional marker for middle to late marine isotope stage 5 across Yukon and 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
Jackson_Hill64.016-139.366Unknown, Unknown Jackson Hill is located on the south side of the lower Klondike River valley, above the canyon mouth of Bonanza Creek, Yukon Territory, Canada. Coordinates from Froese and others (2005); vary slightly from those reported in Jensen and others (2011). Datum not provided, assumed to be NAD83.Glass major element oxide composition reported is the average of analyses of three samples of VT tephra from Jackson Hill: UA1580, UT1562, and UT1637. Individual sample IDs analyzed for glass trace element composition are not reported.Jensen_2011_Jackson_Hill_VT_tephra_averageTephra FallCumulateGlass 70.48 0.59 14.75 3.22 0.1 0.7 2.52 4.57 2.9 7423EMP3.22Cl=0.17; H2O=2.65EMP 3.83 70.4 729 205 21.3 47.5 5.85 27.9 7.11 1.31 6.88 1.19 7.27 1.74 4.77 0.75 4.69 0.75 45 255 6.73 7.14 0.41 6.18 2.9 11.5 5.07 63.5 7423ICPMS

SAMPLE LOCATION

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