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Text Description: Postulated intracaldera lavas exposed at base of south face of Mount Sanford. Detailed traverse (section C on map sheet; see also, fig. 2) through accessible part of exposure reveals rather uniform series of flat-lying, aphyric to porphyritic olivine basaltic andesite flows in which silica content ranges only from 53.1 to 55.3% (samples 84-ARh-79a to 79e and 79g to 79l). Porphyritic flows predominate; they typically contain phenocrysts of plagioclase (10-25%, as large as 5 mm), olivine (1-6%, 1-2 mm; generally corroded), and hypersthene (trace), in pilotaxitic groundmass. Three whole-rock K-Ar ages on lava flows from lower part of section are 0.73+/-0.08, 0.85+/-0.02, and 0.86+/-0.22 Ma (sample 74-ALe-65);dike (Qsdi) that cuts two oldest flows has K-Ar age of 0.78+/-0.08 Ma (sample 74-ALe-63). These ages are approximately the same as those of some flows that are topographically higher in complex Sanford shields. 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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84-ARh-79j | 62.19 | -144.18998 | Richter, D. H. | 1984-00-00 | Sanford | Sanford intracaldera (?) Within Section C in Gulkana A-1 quadrangle, depicted in Richter and others, 1994 | Postulated intracaldera lavas exposed at base of south face of Mount Sanford. Detailed traverse (section C on map sheet; see also, fig. 2) through accessible part of exposure reveals rather uniform series of flat-lying, aphyric to porphyritic olivine basaltic andesite flows in which silica content ranges only from 53.1 to 55.3% (samples 84-ARh-79a to 79e and 79g to 79l). Porphyritic flows predominate; they typically contain phenocrysts of plagioclase (10-25%, as large as 5 mm), olivine (1-6%, 1-2 mm; generally corroded), and hypersthene (trace), in pilotaxitic groundmass. Three whole-rock K-Ar ages on lava flows from lower part of section are 0.73+/-0.08, 0.85+/-0.02, and 0.86+/-0.22 Ma (sample 74-ALe-65);dike (Qsdi) that cuts two oldest flows has K-Ar age of 0.78+/-0.08 Ma (sample 74-ALe-63). These ages are approximately the same as those of some flows that are topographically higher in complex Sanford shields. | 84-ARh-79j | Lava | Whole-rock | 53.3 | 1.24 | 18 | 7.83 | 0.13 | 5.38 | 8.41 | 3.33 | 1.2 | 0.31 | 100.26 | 2262 | NN | 2.64 | 5.45 | H2OP=0.72; H2OM=0.15; CO2=0.01 | RAPIDA |
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