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Text Description: Gray, medium-grained biotite quartz diorite with a color index of 16. Volume percentages are: zoned and unzoned andesine-oligoclase, 56; orthoclase, 7.2; quartz, 21; biotite, 8.0; hornblende, 3.6; clinopyroxene, 2.4; opaque oxide, 1.0; chlorite, 0.4; apatite, 0.3; sphene and epidote, trace. This rock, from the east shore of Bay of Waterfalls, is located near the edge of the largest pluton. Coarser and darker border phases with septa of recrystallized basaltic rocks occur just a few yards from this rock, but the main contact is underwater in Bay of Waterfalls. Characteristically, rocks this close to the border are more mafic than the main mass, and appear blotchy from irregular concentrations of dark minerals. 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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specimen 1 | 51.72 | -176.83 | Unknown, Unknown | 1952-01-01 | Bay of Waterfalls, southwest Adak Island | Gray, medium-grained biotite quartz diorite with a color index of 16. Volume percentages are: zoned and unzoned andesine-oligoclase, 56; orthoclase, 7.2; quartz, 21; biotite, 8.0; hornblende, 3.6; clinopyroxene, 2.4; opaque oxide, 1.0; chlorite, 0.4; apatite, 0.3; sphene and epidote, trace. This rock, from the east shore of Bay of Waterfalls, is located near the edge of the largest pluton. Coarser and darker border phases with septa of recrystallized basaltic rocks occur just a few yards from this rock, but the main contact is underwater in Bay of Waterfalls. Characteristically, rocks this close to the border are more mafic than the main mass, and appear blotchy from irregular concentrations of dark minerals. | specimen 1 | Countryrock | Enclave/Inclusion | Whole-rock | 62.19 | 0.68 | 16.99 | 5.13 | 0.1 | 2.48 | 5.41 | 4.18 | 1.82 | 0.26 | 99.98 | 356 | NN | 2.61 | 2.77 | H2OM=0.08; H2OP=0.58; CO2=0.02; Cl=0.05; F=0.03 | NN | 41.1 | 705 | 16 | units are percent 1.5 | 745 | XRF: Rb, Sr, Ni; NN: K; | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
specimen 1 | 51.72 | -176.83 | Unknown, Unknown | 1952-01-01 | Bay of Waterfalls, southwest Adak Island | Gray, medium-grained biotite quartz diorite with a color index of 16. Volume percentages are: zoned and unzoned andesine-oligoclase, 56; orthoclase, 7.2; quartz, 21; biotite, 8.0; hornblende, 3.6; clinopyroxene, 2.4; opaque oxide, 1.0; chlorite, 0.4; apatite, 0.3; sphene and epidote, trace. This rock, from the east shore of Bay of Waterfalls, is located near the edge of the largest pluton. Coarser and darker border phases with septa of recrystallized basaltic rocks occur just a few yards from this rock, but the main contact is underwater in Bay of Waterfalls. Characteristically, rocks this close to the border are more mafic than the main mass, and appear blotchy from irregular concentrations of dark minerals. | specimen 1 | Countryrock | Enclave/Inclusion | Whole-rock | H2OM=0.08; H2OP=0.58; CO2=0.02; Cl=0.05; F=0.03 | NN | 356 |
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