The only sample of Jensen_Palisades-7. Also the only sample collected at Site D1, where it was present as a wispy, white, discontinuous lamina <0.1 cm thick, reworked into the upper 20 cm of an organic-rich silt bed containing wood fragments up to 30 cm in length (see Figs. 2 and 4B of Jensen and others, 2013).
The Palisades is a key reference site for the middle Pleistocene of eastern Beringia: new evidence from paleomagnetics and regional tephrostratigraphy
|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|
|Jensen_Palisades_East||65.1||-153.19997||Jensen, 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 only sample of Jensen_Palisades-7. Also the only sample collected at Site D1, where it was present as a wispy, white, discontinuous lamina <0.1 cm thick, reworked into the upper 20 cm of an organic-rich silt bed containing wood fragments up to 30 cm in length (see Figs. 2 and 4B of Jensen and others, 2013).||UA1308-Pop.1||Tephra Fall||Cumulate||Glass||74.14||0.24||14.8||1.44||0.04||0.45||1.88||4.15||2.82||9361||EMP||1.44||Cl=0.04; H2O=5.58||EMP|
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