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SAMPLE INFO : 80cnd01
Sample ID:80cnd01
Station ID:80cnd01
Latitude:62.1225
Longitude:-144.365
Datum:NAD83
Date Sampled:1980-01-01
Sample Type 1:Lava
Text Description:
CAF - Chetaslina andesite flow- of Nye (1983).

References:
Petrology and geochemistry of Okmok and Wrangell volcanoes, Alaska
Geochemistry of some Quaternary lavas from the Aleutian Arc and Mt. Wrangell

GEOCHEM DATA
StationIDLatitudeLongitudeGeologistDateVisitedAge InfoVolcanoEruptionLocation DescriptionText DescriptionSample IDSample Type 1Sample Type 2Geologic UnitMaterialSiO2TiO2Al2O3FeOTMnOMgOCaONa2OK2OP2O5Total-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
80cnd0162.1225-144.365Nye, C. J.1980-01-01 WrangellThese flows were collected from cliffs bordering the ground moraine of a retreating, unnamed, glacier south of the Sanford Glacier. These flows span 700 m of continous stratigraphic section with no apparent time break, except for a weathering surface immediately above 80cnd01. Individual samples are no closer than every other flow, and in many cases 3-4 flows may be spanned between individuals.CAF - Chetaslina andesite flow- of Nye (1983).80cnd01LavaWhole-rock 56.37 0.988 16.98 0.119 6.02 7.93 3.75 1.077 0.217 100.4613291XRF6.55 0.504959549 20.08376773 407.5385176 533.1591833 14.55383249 30.3195624 3.876237087 16.04231468 3.684369646 1.252228739 3.780114186 0.631576604 3.828996992 0.759422705 2.039901629 0.296360013 1.77314778 0.283455328 19.29736009 123.5782164 6.197097025 3.207764214 0.41571818 4.434998876 2.417942607 0.856281405 21.36400748 0 13291ICPMS 21 411 526 13 27 14 19 129 5.9 5 3 22 176 124 140 76 69 1813291XRF
80cnd0162.1225-144.365Nye, C. J.1980-01-01 WrangellThese flows were collected from cliffs bordering the ground moraine of a retreating, unnamed, glacier south of the Sanford Glacier. These flows span 700 m of continous stratigraphic section with no apparent time break, except for a weathering surface immediately above 80cnd01. Individual samples are no closer than every other flow, and in many cases 3-4 flows may be spanned between individuals.CAF - Chetaslina andesite flow- of Nye (1983).80cnd01LavaWhole-rock 55.61 0.94 16.89 5.94 7.91 4.18 1.03 0.21 100.1147XRF7.29 21 446 510 14 31 14 20 129 8.9 5635 173 120 144 47XRF

SAMPLE LOCATION

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