POTENTIAL FOR PRESERVATION OF ARCHAEOLOGICAL ARTIFACTS AT THE BAD VILLAGE CULTURAL SITE BASED ON GEOMORPHOLOGIC AND GIS MAPPING EFFORTS
Using a hand auger system, 589 sediment samples were collected at intervals of four inches from 10 boreholes, drilled to a combined depth of 196 feet. Samples were described for grain size (USDA texture class), Munsell color, redoximorphic state, and organic components. Additionally, historic maps from 1796, 1804, 1839, 1855, 1858, 1881, 1892, 1899, and 1917, were utilized, along with a LiDAR dataset, topographic map, and aerial photos from 1941, 1993, and 2008. Maps from 1858 and later were added to an ArcGIS project map and georeferenced for spatial analysis and visual inspection.
The primary landscape feature at the site is a low terrace defined by an erosional scarp ~2 to 7 feet high on its northeastern margin regarded as an old Missouri River cut bank. Stratigraphic interpretation from the boreholes within the low terrace reveals ~2 to 6 foot thick overbank sedimentation overlying channel fill. Recently obtained sedimentation rates in the Lower Missouri River valley suggest that channel fills at the cultural site have ages greater than ~390 years (based on OSL dating). Likewise, surficial features and historic maps indicate that Bow Creek and its tributary, West Bow Creek, have not traversed a sizable tract of land within the terrace for several hundreds of years. A boundary enclosing an area of 121.3 acres was mapped indicating the highest likelihood for preserved artifacts from the time period considered. The results of this study are being used by the Lewis and Clark National Historic Trail and the Midwest Archaeological Center to plan an archaeological survey of the site.