Northwest Wyoming (Geographic Keyword)

DOCUMENT Citation Only R. A. Flayharty.

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DOCUMENT Citation Only Blaine O. Halliday.

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DOCUMENT Citation Only Michael Wilson. Diane J. Wilson.

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DOCUMENT Full-Text Kathryn Puseman.

The fill from a steep-sided, basin-shaped hearth at Site 48PA1831 in northwest Wyoming was floated to recover macrofloral remains. This hearth was excavated during well pad construction and is the only feature at the site. Macrofloral analysis is used to provide information concerning plant resources that may have been processed in this feature.

DOCUMENT Full-Text Raymond Kunselman. Wilfred M. Husted.

X-ray fluorescence spectroscopy was used to determine the source of 107 obsidian projectile points in surface collections from the Beartooth Mountains of south-central Montana and northwest Wyoming. Seventy-two percent of the points were from Obsidian Cliff in Yellowstone National Park, Wyoming. Evidence was found for change of source usage when the artifacts were grouped into cultural affiliation periods.

DOCUMENT Citation Only Steve Fuller.

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DOCUMENT Full-Text Linda Scott Cummings. Thomas E. Moutoux.

Goff Creek (48PA325) is located at an elevation of approximately 6400 feet in the Shoshone National Forest in Park County, northwest Wyoming. Thirty-seven stratigraphic pollen samples were examined to provide paleoenvironmental interpretations between approximately 6,000 BP and the present. The base of this record may represent a Paleoindian deposition; however, sediment accumulation between this level and approximately 6,000 BP was minimal or perhaps removed.