The preceding has been a selected sample of essentially unedited field notes not including much detail and barely mentioning the carefully drawn maps, and horizontal and vertical profiles that accompanied the written description. Profiles showing soil color changes were done in color, using colored pencils in an attempt to duplicate the colors observed. Photographs, both black and white and color were taken whenever anything showed up of possible use for record or interpretation. (The Editors).
A north-south cross sectional profile along the R22 line shows a rise of 3.4 feet from the south base line to a point of maximum elevation some 400 feet north. The midden deposit shows a corresponding increase in depth. The zero base line was on the south end of the site in an area that appears to have been destroyed by an early St. Francis River meander. Excavation was carried on from this point to square 40R22, a distance of 400 feet north, but not to the northern end of the site which is some distance beyond. The northern portion of the profile indicated that this was an area of major house building activity while to the south and just north of the area washed out by the St. Francis River meander there is some indication of a court or open community center. The ancient river meander was filled with a bluish sandy clay. This ends near stake 9R22 with a datum elevation of 1.2 feet above the base line.
From 5 to 8R22 there was a sandy deposit below the plow line which probably represents a deposit from standing water as the meander activity comes to a stop and filling in became a slow silting process. From 8 to 17R22 there was a thin hard-packed deposit from .2 to .3 feet in depth. Test pits through this section yielded almost no archaeological material while just north of 17R22 the midden deposit abruptly deepened. This area, almost 100 feet north-south, was also seen on the east-west profile. It is this area that gives the impression of being a plaza or community center (Fig. 2).
Starting just north of this open area there was a bank of clean sand and the midden deposit below suddenly dipped downward until at 21R22 it was quite pronounced with evidence of a sand boil. This disturbance was due to the New Madrid earthquake and can be clearly seen in many areas of this state. Here, the evidence for land subsidence, along with large sand boils originating from considerable depth, is clear. This earthquake evidence was no longer apparent north of square 29R22 and the full undisturbed midden deposit of 1.5 foot depth gives evidence of the Indian occupation. At square 40R22 the deposit was 1.8 feet deep and it is at this point that houses 2 and 3 were found. The excavation was not carried any farther north.