Evolution of landscapes on the double mountain fork of the brazos river,West Texas: Implications for preservation and visibility of the archaeological record |
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| Authors: | Michael D Blum James T Abbott Salvatore Valastro |
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| Abstract: | The Double Mountain Fork of the Brazos River is an ephemeral stream that flows across the western Rolling Plains of West Texas. Intensive pedestrian archaeological survey, covering some 8700 acres of the drainage, produced a site inventory with a general paucity of identifiable Paleoindian and Early to Middle Archaic components, whereas Late Archaic and Late Prehistoric sites were widespread and found in a diversity of landscape positions. Geoarchaeological investigations were conducted in conjunction with this survey and later testing activities, and suggested that much of this temporally and spatially skewed archaeological record may be attributable to the evolution of landscapes during the late Pleistocene and Holocene time period, rather than original occupation intensities. Most of the landscape in the study area has been subject to erosional stripping, but in selected localities late Pleistocene and Holocene depositional landform-sediment assemblages of fluvial, alluvial/colluvial fan, and eolian origin are preserved. With few exceptions, however, depositional contexts or stable geomorphic surfaces more than 3000 years old are erosionally truncated, completely absent, or deeply buried. As a result, a bias is imposed that renders older cultural records either poorly preserved or deeply buried and of low visibility to traditional survey techniques. Similar natural formation processes are likely at other locations on the western Rolling Plains, and should be considered during interpretation of prehistoric population dynamics in the area. The biases imposed by such natural formation processes on the western Rolling Plains are slightly different from other areas in the Southern Great Plains of the United States, but in most cases the known archaeological record corresponds with opportunities for preservation and visibility provided by geologic trajectories, and may reflect little on spatial and temporal discontinuities in prehistoric cultural activity. |
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