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Text Description: Basaltic andesite magmatic inclusion. 15% phenocrysts of plagioclase and pyroxene. Groundmass is dominantly crystalline and consists of 30 x 200 micron plagioclase laths, 150 micron pyroxene, opaque oxides, and subordinate clear glass. Irregular voids largely bounded by crystals are abundant. Sparse chromite-bearing olivine crystals up to 1 x 2 mm have highly birefringent reaction halos. One of several diverse lithologies collected from single location consisting of avalanche debris sitting on top of Umbrella Glacier at ~2200 foot elevation. Location implies these all came from Iliamna, central peak. "i" denotes fist-sized rounded blobs of macroscopically different magma enclosed in homogeneous host. References: ![]() |
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 | |
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91CNI21i | 59.99421 | -153.16787 | Nye, C. J. | 1991-07-28 | Iliamna | Latitude and longitude determined using Google Earth. | Basaltic andesite magmatic inclusion. 15% phenocrysts of plagioclase and pyroxene. Groundmass is dominantly crystalline and consists of 30 x 200 micron plagioclase laths, 150 micron pyroxene, opaque oxides, and subordinate clear glass. Irregular voids largely bounded by crystals are abundant. Sparse chromite-bearing olivine crystals up to 1 x 2 mm have highly birefringent reaction halos. One of several diverse lithologies collected from single location consisting of avalanche debris sitting on top of Umbrella Glacier at ~2200 foot elevation. Location implies these all came from Iliamna, central peak. "i" denotes fist-sized rounded blobs of macroscopically different magma enclosed in homogeneous host. | 91CNI21i | Lava | Whole-rock | 54.31 | 0.708 | 18.99 | 0.152 | 4.94 | 9.06 | 3.7 | 0.577 | 0.132 | 100.52 | 13291 | XRF | 7.42 | 0.38766 | 6 | 201 | 484 | 4 | 15 | 1.87569 | 8.72332 | 2.38228 | 0.9121 | 2.64849 | 0.46007 | 2.94599 | 0.60599 | 1.6887 | 0.25913 | 1.67904 | 0.27404 | 16 | 70 | 1.4603 | 0.0872 | 3 | 0 | 0.41082 | 17 | 229 | 40 | 21 | 0 | 87 | 18 | 13291 | ICPMS: Cs, Pr, Nd, Sm, Eu, Gd, Tb, Dy, Ho, Er, Tm, Yb, Lu, Hf, Ta, U; XRF: Rb, Ba, Sr, La, Ce, Y, Zr, Pb, Sc, V, Cr, Ni, Zn, Ga; |
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