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Text Description: Lava or ash sample from Katmai National Park. References:  Part I: The Mt. Edgecumbe volcanic field, Alaska: an example of tholeiitic and calc-alkaline volcanism, Part II: Characteristics of andesitic to dacitic volcanism at Katmai National Park, Alaska |
| 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 | |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Kosco_Katmai_CR-2 | 58.279 | -154.9533 | Kosco, D. G. | Katmai | Lava or ash sample from Katmai National Park. | Kosco_Katmai_CR-2 | Lava | Whole-rock | 66.97 | 0.57 | 15.23 | 4.27 | 0.09 | 2.11 | 4.31 | 4.3 | 2.05 | 99.28 | 30 | XRF | 4.27 | 47.1 | 712.1 | 220.1 | 22.7 | 36.3 | 35.8 | n.d. | original text says this value is for Su 6.5 | 37 | 178.2 | bdl | 20.2 | 10.6 | 84.3 | 15.4 | 17.9 | 62.1 | 11.1 | 30 | XRF |
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