16 Undergraduate Research Oral Session

Monday, 15 April 2024
1:30 PM - 2:50 PM
Victoria


SOIL MORPHOLOGY ON STEEP UPLAND SLOPES IN THE BLUE RIDGE: DID NATIVE AMERICANS QUARRY HERE?

Paper number: 16-3
Program: Theme Sessions
Time: 1:45 PM – 1:55 PM


Authors


Abstract

Both historical records of Native American settlements and archaeological models of the Blue Ridge indicate that Cherokee settlements in western North Carolina were located in valley bottoms with easy access to water and flat terrain for building. However, there is increasing evidence that across America many Native communities quarried and spent significant time on steep, upland slopes. We completed soil geomorphic analysis as part of a larger project aimed at investigating Paleo Indian or Cherokee occupation or quarrying in the Mills River area. Specifically, we examined soils on the ridgeline, the upper slope, and the mid-slope to understand how hillslopes formed, when colluvium stabilized, and how stable the hillslopes are today. Our process included describing fourteen soil profiles in the field as well as completing loss-on-ignition and particle size methods in the laboratory. Ridgetop profiles were primarily erosional, while upper and mid-slope profiles have thick sedimentary deposits at the surface. On the upper slope location, colluvium containing Holocene cultural material overlies saprolite approaching bedrock. The mismatch between very old saprolite and what appears to be Holocene colluvium would seem to suggest that bare bedrock or saprolite may have been exposed during the Pleistocene as no Pleistocene sediments are observed in the field area. Although CRM firms have found Native American artifacts in the form of hammerstones and quartz flakes, we observe no significant landscape change that would be attributed to heavy quarrying on the ridge. Further geologic and/or geomorphic mapping may provide additional insights or expose better evidence of quarrying in the area.

Geological Society of America Abstracts with Programs. Vol. 56, No. 2

doi: 10.1130/abs/2024SE-397957

© Copyright 2024 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.