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Radiometric traverse along the Yukon River from Fort Yukon to Ruby, Alaska, 1949

Max G. White·John M. Stevens·John J. Matzko
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Abstract

In 1949, a radiometric traverse was made of rocks exposed along the banks of and near the Yukon River about Fort Yukon to Ruby, Alaska. Granitic rocks of Tertiary age and of Devonian or Carboniferous age and sandstone beds of Cretaceous age gave the highest readings obtained in the field. Other rock types examined were greenstone of Devonian or Carboniferous age and metamorphic rocks of Devonian and pre-Devonian age, sedimentary rocks, and liginite of Tertiary age, and alluvial deposits of Quaternary age. The most radioactive sample, from Melozitna River canyon, contained only 0.017 percent equivalent uranium.

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90° N90° S · 180° W ← longitude → 180° E
Source-reported bounding extent: 64.6876° to 66.0817° latitude; -155.7095° to -148.8671° longitude. This indicates report coverage, not an exact sampling location. View area on OpenStreetMap.

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BibTeXRIS

Max G. White, John M. Stevens, John J. Matzko. 1956. Radiometric traverse along the Yukon River from Fort Yukon to Ruby, Alaska, 1949. https://doi.org/10.3133/tem357

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