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SAMPLE INFO : Jensen_Palisades-9_average-Pop.1
Sample ID:Jensen_Palisades-9_average-Pop.1
Station ID:Jensen_Palisades_East
Latitude:65.1
Longitude:-153.19997
Datum:NAD83
Sample Type 1:Tephra Fall
 Text Description:
The composition reported here is the average of analyses of two samples: UA1467 and UA1468. Present at two of the three gullies that comprise Site D2, including one gully where it is ~10 cm below P10. The tephra is present as pink-orange semi-continuous pods ~0.5-3 cm thick that are within, or up to 40 cm below, the base of the Matheus and others (2003) middle peat (Fig. 2; Jensen and others, 2013). Glass morphology is distinct; the dominantly thick-walled pumice contains such abundant microlites that vesicles are deformed, and pure glass analyses are difficult. Some brown glass is present, and mineralogy consists of plagioclase, which is frequently zoned, and pyroxene.

References:
The Palisades is a key reference site for the middle Pleistocene of eastern Beringia: new evidence from paleomagnetics and regional tephrostratigraphy

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
Jensen_Palisades_East65.1-153.19997Jensen, B. J. L. The Palisades are on the south bank of the Yukon River in Nowitna National Wildlife Refuge, ~70 km downstream of Tanana village. Palisades East forms a heavily gullied, cliff-like exposure that is generally ~40-45 m in height, but ranges from ~25 m high at Site E to ~55-60 m high at Site D. It is difficult to access safely, with many near-vertical exposures and overhanging blocks of frozen sediment that frequently break free into the Yukon River. Location imprecisely georeferenced from Figure 1 in Jensen et al. (2013). Multiple sections were mapped and sampled across Palisades East: Site B1, B2, IB4, F, D1, and D2. See Jensen et al. (2013).The composition reported here is the average of analyses of two samples: UA1467 and UA1468. Present at two of the three gullies that comprise Site D2, including one gully where it is ~10 cm below P10. The tephra is present as pink-orange semi-continuous pods ~0.5-3 cm thick that are within, or up to 40 cm below, the base of the Matheus and others (2003) middle peat (Fig. 2; Jensen and others, 2013). Glass morphology is distinct; the dominantly thick-walled pumice contains such abundant microlites that vesicles are deformed, and pure glass analyses are difficult. Some brown glass is present, and mineralogy consists of plagioclase, which is frequently zoned, and pyroxene.Jensen_Palisades-9_average-Pop.1Tephra FallCumulateGlass 66.33 0.45 16.65 4.18 0.14 1.36 4.7 4.52 1.47 9361EMP4.18Cl=0.19; H2O=2.38EMP

SAMPLE LOCATION

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