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Site name: Whistling Elk

Nearest town: Pierre; State/country: South Dakota; Type of site: Prehistoric fortified earth lodge village (Initial Coalescent); Date of site: AD 1300; Sponsor: National Center for Preservation Technology and Training (NCPTT); Collaborators: University of North Dakota Archaeological Field School.

Type of survey: Resistivity; Instrument: Geoscan Research RM-15; Prospection depth: 1 m; Sampling interval: 1 m x 0.5 m; Area surveyed: 184 x 110 m; Date of survey: 7/97 & 7/98.

Comments: This site is buried under approximately one meter of alluvium as revealed by limited excavations on the banks of the Missouri River in the late 1970s and recent tests. The resistivity survey was performed by the University of North Dakota Archaeological Field School. The data clearly reveal the complete fortification ditch, 5 bastion loops, numerous earthlodge (house) locations, possible middens, and other features. Of particular importance is the suggestion of an inner fortified village, with perhaps 4 bastion loops and a greater density of houses. The 1970s excavations of burned houses suggested that this village was attacked. This evidence may indicate subsequent reoccupation and reorganization of this village. For additional details, see The Whistling Elk Subsurface Imaging Project.

Type of survey: Conductivity; Instrument: Geonics EM-38; Prospection depth: 1.5 m, peak sensitivity at 0.4 m; Sampling interval: 1 m x 0.5 m; Area surveyed: 170 x 120 m; Date of survey: 7/97 & 7/98.

Comments:That conductivity is the inverse of resistivity is clearly shown in the reversal of the darkness scale assigned to the measurements (compare above) and by a graph of the conductivity and resistance data in two survey grids (second figure). Although obtained much more rapidly, conductivity data represent an average over a larger volume of earth than resistivity, making edges and boundaries somewhat less distinct. Moreover, with a peak sensitiviy at 0.4 m depth, features in the nearby plow zone are much more apparent. In the left figure, two former fields, unused since the 1960s, are indicated by differences in plow mark directions. For additional details, see The Whistling Elk Subsurface Imaging Project.

Type of survey: Magnetic gradiometry; Instrument: Geoscan Research FM-36 fluxgate gradiometer; Prospection depth: up to 1.5 m; Sampling interval: 1 m x 0.25 m; Area surveyed: 170 x 120 m; Date of survey: 7/97 & 7/98.

Comments:The magnetic survey, although appearing noisy at a global scale, reveals faint traces of the bastion shown by the resistivity and conductivity data (see above). Many of the magnetic extremes represent prehistoric burned features, including houses, palisades, and hearths. They also represent historic iron farming artifacts like broken plow parts. At a larger scale, the magnetic data are rich in detail. The second figure shows an Initial Coalescent square house and linear entranceway as revealed by the resistivity data. The correpsonding magnetic data indicate its central hearth, that its walls were burned, and there are even indications of the 4 central support posts which are known to have existed in each quadrant of a house of this period (verified through excavation). For additional details, see The Whistling Elk Subsurface Imaging Project.

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(updated: 7/00)