The Quaternary Stratigraphy of the Henrys Fork and Western Browns Park, Northeastern Uinta Mountains, Utah and Wyoming
The landscape evolution of the northeastern Uinta Mountains and the manner in which climatic and tectonic forcing have influenced it are not well constrained. Surficial deposits covering ~325 km2 below the glacial termini in the Henrys Fork and ~50 km2 along the Green River in western Browns Park we...
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| Format: | Others |
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DigitalCommons@USU
2005
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| Online Access: | https://digitalcommons.usu.edu/etd/6734 https://digitalcommons.usu.edu/cgi/viewcontent.cgi?article=7799&context=etd |