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Sample ID:UA2174-P2
Station ID:EW0408-66JC
Sample Type 1:Tephra Fall
Text Description:
From 1374-1376 cm depth. Sample is dispersed in bioturbated sediment.

Interaction between climate, volcanism, and isostatic rebound in Southeast Alaska during the last deglaciation

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
EW0408-66JC58.87-137.1Praetorius, Summer Marine sediment core located in proximity to the Mount Edgecumbe Volcanic Field (MEVF). Core spans 13.5 to 4.3 ka, with sedimentation rates ranging from 200-2000 cm/kyr during the deglacial period and 10cm/kyr during the Holocene. Datum not specified, assumed to be NAD83.From 1374-1376 cm depth. Sample is dispersed in bioturbated sediment.UA2174-P2Tephra FallCumulateGlass 49.55 1.74 16.25 10.52 0.16 6.8 11.11 3.62 0.23 10010761EMP10.52Cl=0.01; H2O=0.44EMP


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