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Text Description: Average composition of samples from Lone Spruce Pond (UA1963), Sunday Pond (UA1780), Little Swift Lake (Axford and Kaufman 2004) (UA1967), Waskey Lake (Levy et al. 2004) (UA1968), Arolik Lake (Kaufman et al. 2003) (UA1970), and subsamples from three levels in the soil pit near Cascade Lake (Kathan 2006) (UA1975, UA1976, UA1977). This tephra comprises the thickest bed in all lakes from the region (likely including Nimgun Lake, which was not analyzed and somewhat older than expected), and is essentially ubiquitous in outcrops and soil pits across the landscape. Tephra A contains a high percentage of bubble-wall and tricuspate shards, platy glass, elongate pumice, and pumice with large vesicles. Less common are blocky glass and pumice, which are occasionally crystal-rich. Brown and clear glass shards are present in roughly the same proportion. 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 | Coeff | 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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Ahklun_Mountains_Regional_Tephra | 59.6 | -160.39998 | Kaufman, D. S. | -1480-- | Ahklun Mountains, southwest Alaska; glass compositions are averages calculated from analyses of multiple correlated tephra present in lacustrine cores from the area. Individual sample IDs (analyses of which contribute to the average tephra bed composition) are noted in the sample descriptions. | Average composition of samples from Lone Spruce Pond (UA1963), Sunday Pond (UA1780), Little Swift Lake (Axford and Kaufman 2004) (UA1967), Waskey Lake (Levy et al. 2004) (UA1968), Arolik Lake (Kaufman et al. 2003) (UA1970), and subsamples from three levels in the soil pit near Cascade Lake (Kathan 2006) (UA1975, UA1976, UA1977). This tephra comprises the thickest bed in all lakes from the region (likely including Nimgun Lake, which was not analyzed and somewhat older than expected), and is essentially ubiquitous in outcrops and soil pits across the landscape. Tephra A contains a high percentage of bubble-wall and tricuspate shards, platy glass, elongate pumice, and pumice with large vesicles. Less common are blocky glass and pumice, which are occasionally crystal-rich. Brown and clear glass shards are present in roughly the same proportion. | Ahklun Mountains-Tephra-A(Aniakchak)-Pop.1_average | Tephra Fall | Cumulate | Glass | 59.02 | 1.37 | 16.5 | 7.59 | 0.21 | 2.81 | 6.41 | 4.42 | 1.55 | 7993 | EMP | 7.59 | Cl=0.12; H2O=2.51 | EMP |
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