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Text Description: CG -Chetaslina Gl homogeneous- 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 |
| StationID | Latitude | Longitude | Geologist | DateVisited | Age Info | Volcano | Eruption | Location Description | Text Description | Sample ID | Sample Type 1 | Sample Type 2 | Final Unit | Material | 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 | |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 79cne26 | 61.9763 | -144.305 | Nye, C. J. | 1979-01-01 | Wrangell | The single largest continuous stratigraphic section exposed on Mt. Wrangell holds up the ridge immediately north of the Chetaslina Glacier. Samples 79cne01-79cne29 are superposed flows collected from altitudes between 4500 and 7500 ft. on a spur off the larger ridge. * * * Larger numbers are further upsection. | CG -Chetaslina Gl homogeneous- of Nye (1983). | 79cne26 | Lava | Whole-rock | 62.54 | 0.864 | 16.41 | 0.091 | 3.17 | 5.56 | 3.94 | 2.12 | 0.204 | 99.77 | 13291 | XRF | 5.1 | 0.972270155 | 55.14187788 | 598 | 511.8814962 | 18 | 37 | 4.916345584 | 18 | 4.251569037 | 1.103368581 | 3.991505844 | 0.655548867 | 3.915210674 | 0.779435952 | 2.105135095 | 0.309276288 | 1.880911423 | 0.29425089 | 20.01249747 | 186.4088148 | 6.543790863 | 5.035568991 | 0.503780998 | 9 | 9 | 2.164676179 | 14 | 134 | 53 | 0 | 35 | 59 | 18 | 13291 | ICPMS: Cs, Rb, Sr, Pr, Sm, Eu, Gd, Tb, Dy, Ho, Er, Tm, Yb, Lu, Y, Zr, Nb, Hf, Ta, U; XRF: Ba, La, Ce, Nd, Pb, Th, Sc, V, Cr, Cu, Zn, Ga; | |||||||||||||||||||||||||||||||||||||||||||||||||||||
| 79cne26 | 61.9763 | -144.305 | Nye, C. J. | 1979-01-01 | Wrangell | The single largest continuous stratigraphic section exposed on Mt. Wrangell holds up the ridge immediately north of the Chetaslina Glacier. Samples 79cne01-79cne29 are superposed flows collected from altitudes between 4500 and 7500 ft. on a spur off the larger ridge. * * * Larger numbers are further upsection. | CG -Chetaslina Gl homogeneous- of Nye (1983). | 79cne26 | Lava | Whole-rock | 61.58 | 0.84 | 16.38 | 0.09 | 3.26 | 5.69 | 4.21 | 2.06 | 0.2 | 100.69 | 47 | XRF | 5.7 | 58 | 527 | 23 | 214 | 10.1 | 44 | 17184 | 47 | XRF |
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