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Text Description: Noatak basin sample 95AHa 022. Lens of pinkish tephra as much as 4 cm thick near the base of the silt near the north end of the bluff. Clear, platy glass shards with secondary but significant percentage of bubble-junction shards, both as much as 80-100 mm in diameter. Very few juvenile ferromagnesium phenocrysts are present in the tephra, but small, euhedral crystals of clinopyroxene and orthopyroxene and rare amphibole and biotite were identified in grain mounts. 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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Nk-26 | 67.9 | -158.29997 | Unknown, Unknown | Exposure Nk-26 is situated 8 km north of the Cutler River confluence and extends for 0.5 km along the east bank of the Noatak River, Alaska. The bluff intersects a depositional surface about 40 m high that is inset within the Cutler moraine. Location imprecisely georeferenced from Figure 4 in Elias and others (1999). | Noatak basin sample 95AHa 022. Lens of pinkish tephra as much as 4 cm thick near the base of the silt near the north end of the bluff. Clear, platy glass shards with secondary but significant percentage of bubble-junction shards, both as much as 80-100 mm in diameter. Very few juvenile ferromagnesium phenocrysts are present in the tephra, but small, euhedral crystals of clinopyroxene and orthopyroxene and rare amphibole and biotite were identified in grain mounts. | ACT2007 | Tephra Fall | Cumulate | Glass | 75.25 | 0.39 | 12.94 | 0.29 | 1.4 | 3.83 | 3.79 | 100 | 2131 | EMP | 1.84 | Cl=0.27; H2O=3.56 | EMP |
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