|
Text Description: Tephra present in several cores from Shilak Lake, at a depth of 30-50 cm in individual cores depending on localized sedimentation rates. 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 | |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
SK-11 | 60.5 | -150.49998 | Stihler, S. D. | 1987-01-01 | 400 ± 50 stratigraphy; 89; Age is approximate. Age estimate based upon sedimentation rate estimates and interpolation between the historic tephras at the top of the cores and the 500-year-old tephra layer B from Mount St. Augustine found lower in the cores from Shilak Lake. | 1550-- | Skilak Lake, Kenai Peninsula, Alaska. Location imprecisely georeferenced from Figure 1 in Stihler et al. (1991). | Tephra present in several cores from Shilak Lake, at a depth of 30-50 cm in individual cores depending on localized sedimentation rates. | SK-11-3-15 | Tephra Fall | Cumulate | Glass | 77.85 | 0.25 | 12.4 | 0.17 | 0.97 | 3.74 | 3.41 | 89 | EMP | 1.11 | Cl=0.1; H2O=1.02 | EMP | ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
SK-11 | 60.5 | -150.49998 | Stihler, S. D. | 1987-01-01 | 400 ± 50 stratigraphy; 89; Age is approximate. Age estimate based upon sedimentation rate estimates and interpolation between the historic tephras at the top of the cores and the 500-year-old tephra layer B from Mount St. Augustine found lower in the cores from Shilak Lake. | 1550-- | Skilak Lake, Kenai Peninsula, Alaska. Location imprecisely georeferenced from Figure 1 in Stihler et al. (1991). | Tephra present in several cores from Shilak Lake, at a depth of 30-50 cm in individual cores depending on localized sedimentation rates. | SK-11-3-15 | Tephra Fall | Cumulate | Glass | 77.82 | 0.24 | 12.42 | 0.16 | 0.88 | 3.71 | 3.58 | 805 | EMP | 1.1 | Cl=0.1 | EMP |
This website is supported by the U.S. Geological Survey under Cooperative Agreement Grant G22AC00137
Mention of trade names or commercial products does not constitute their endorsement by the U.S. Geological Survey.