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Northeast Subsistence-Settlement Change: A.D. 700 –1300

Northeast Subsistence-Settlement Change: A.D. 700 –1300

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Figure 6.1. Early Late Woodland (Late Woodland I) in southwestern Ontario.<br />

(Walker et al. 1998).<br />

Systematic coring of the Grand Banks site detailed<br />

the floodplain structure there (Crawford et al. 1998;<br />

Walker et al. 1998). In recent years we have turned to<br />

more efficiently surveying floodplain geomorphology<br />

using ground-penetrating radar. In general, stable<br />

floodplains have one or two back channels taking<br />

water away from occupations during high-water seasons.<br />

These channels also provide habitats for wetland<br />

plants and animals of economic importance to people.<br />

The large river bar below the Meyer site (Figure 6.2),<br />

with limited evidence of occupation, has evidence of<br />

complex channel braiding. The lack of stability, particularly<br />

in the downriver portion of the river bar would<br />

have discouraged human habitation there.<br />

RECENTLY INVESTIGATED SITES IN<br />

THE LOWER GRAND RIVER VALLEY<br />

Bell Flats (AfGx-151)<br />

and Armstrong Flats (AfGx-152)<br />

Two sites discovered by our survey are Bell Flats<br />

and Armstrong Flats (Figures 6.2, 6.3). Bell Flats is on<br />

a narrow section of the pinched river flat at the base<br />

of a terrace. Preliminary investigations indicate the<br />

presence of an artifact-bearing palaeosol about 40 cm<br />

below the surface. Recent alluvial deposition has created<br />

a smaller and lower second river bar, where<br />

Armstrong Flats is situated (Figure 6.2). The higher bar<br />

has a palaeosol at a depth of approximately 40 cm,<br />

from which artifacts have been recovered. Both sites<br />

appear to date no later than Princess Point due to the<br />

presence of cordmarked pottery only. A third locale,<br />

Meyer Flats, has not been investigated, but this<br />

appears to be another floodplain site associated with<br />

a well-defined palaeosol (Figure 6.2).<br />

CNR Bridge (AfGx-5)<br />

The CNR Bridge site is situated on the upriver limit<br />

of a river bar (Figure 6.4). The soils here are predominantly<br />

clay. Closer to the river, an alluvial deposit is<br />

over 80 cm thick. Artifacts include nine core fragments,<br />

a stone pipe fragment, and a small collection<br />

of tools including a drill tip, three projectile point<br />

midsections, and a scraper. A single decorated rim<br />

sherd is among the 55 ceramic fragments. Two<br />

palaeosols are present at the southern extent of our<br />

excavations. An artifact bearing palaeosol is 40-60 cm<br />

below the surface, and a second sterile (to date)<br />

palaeosol is 80 cm below the surface.<br />

118 Crawford and Smith

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