Information
Digital ID
geo000656-028
UNLV Special Collections provides copies of materials to facilitate private study, scholarship, or research. Material not in the public domain may be used according to fair use of copyrighted materials as defined by copyright law. Please cite us.
Please note that UNLV may not own the copyright to these materials and cannot provide permission to publish or distribute materials when UNLV is not the copyright holder. The user is solely responsible for determining the copyright status of materials and obtaining permission to use material from the copyright holder and for determining whether any permissions relating to any other rights are necessary for the intended use, and for obtaining all required permissions beyond that allowed by fair use.
Read more about our reproduction and use policy.
I agree.than frag-basin ;et of . th at Even nder-v. As >f the Id be on of yhich after vhich it the 1 1. I tooth. :en in gnifi-uated n the Fig. 38. Site A , A rea IS a, M. R. Harrington beginning excavation; b, recovering a charcoal sample (Peck, Rozaire and Simpson). eroded surface of the northeastern wall of the basin, between Ash Beds 1 and 2, was noted by H arrington (Fig. 38) in 1955. Rozaire was placed in charge of the excavation. A trench paralleling the ridge was dug to determine general dimensions of the feature; another trench was cut into the ridge at the western edge of the feature. Large pieces of bone were found in the m ain charcoal area and side trench. The first trench resulted in a profile of the feature cut parallel to the ridge. This exposed very marked soil changes (Fig. 39) and two pits containing high concentrations of charcoal. The characteristic yellowish-orange coloring of the soil around the charcoal area was very marked. It is believed that this coloring was caused by heat. 81