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

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

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

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Returning to O’Shea’s (1989) comparison, the<br />

Pawnee were located on the plains. They planted<br />

diverse varieties of maize in scattered fields, with<br />

interannual storage. Fallback wild plant foods; the<br />

coordinated, cooperative hunting of buffalo that<br />

could be cured for storage; and social obligations for<br />

sharing within the village were employed to minimize<br />

or buffer the risks associated with maize farming.<br />

The Huron, by contrast, were Eastern Woodlands<br />

maize farmers who planted diverse crops in large<br />

contiguous fields and utilized above ground storage<br />

facilities. Shortfalls were buffered by exploiting wild<br />

plants and animals, especially white-tailed deer,<br />

anadromous fish, and exchange between Huron<br />

villages and between the Huron and other tribes for<br />

animal protein. Winterhalder and Goland (1997:150)<br />

suggest that unlike the situation for the Pawnee, the<br />

patchy soils in the Eastern Woodlands forced the<br />

Huron to clear more area for planting and thus<br />

increased their labor costs; this factor made field dispersion<br />

more costly. Because large communal fields<br />

were planted among the Huron, intravillage sharing<br />

was not as helpful for buffering shortages, because<br />

household harvests were all synchronized.<br />

While Winterhalder and Goland’s thesis seems reasonable,<br />

we disagree with their belief that soil conditions<br />

and suitability for maize cultivation compelled<br />

the Huron to concentrate their fields. The Huron were<br />

in a situation in which they could utilize riverine settings<br />

as well as uplands. The Pawnee, however, would<br />

have been limited to only riverine areas because they<br />

did not possess the technology to effectively utilize<br />

prairie soils, which have an especially thick sod. Even<br />

burning would not have made prairie soils any more<br />

usable for the cultivation of domesticates.<br />

Since the Huron, often referred to as a confederation,<br />

practiced intervillage sharing and intergroup<br />

exchange to obtain needed resources to both supplement<br />

their diet and/or buffer perceived shortages, a<br />

high degree of coordination was needed. Boone<br />

(1992:317) attributes such coordinated effort to the<br />

existence of social hierarchies that arise when population<br />

emigration and dispersal are not logistically<br />

viable options to offset population growth.<br />

Based on the above discussion, some of the strategies<br />

and tactics employed prehistorically to mitigate<br />

perturbations associated with farming, population<br />

growth, sedentism, and population aggregation<br />

should be detectable in subsistence residues and<br />

archaeological settlement patterning data (Rafferty<br />

1994). For example, temporal and spatial variability in<br />

storage facilities can be monitored in conjunction with<br />

an examination of subsistence remains. The size and<br />

spatial arrangement of settlements over time may also<br />

reveal responses to resource selection and the subsequent<br />

risks of those decisions. Another usable measure<br />

for examining issues of dietary decisions, labor<br />

organization, and population density is any spatialtemporal<br />

variability in dwelling size. An examination<br />

of these variables is attempted using the Late<br />

Woodland and Late Prehistoric databases (ca. A.D.<br />

400 to 1400) for the central Ohio Valley.<br />

THE LATE WOODLAND DATABASE<br />

Within central Ohio, a small number of late Late<br />

Woodland sites have been excavated or systematically<br />

surveyed. Within the northern Scioto drainage<br />

(Figure 2.4), data are available from the Walter S. Cole<br />

(Potter 1966), Ufferman (Barkes 1978), DECCO<br />

(Barkes 1982), and the Hartley Farm and Scioto<br />

Woods sites (Church 1992). In the central portion of<br />

the Scioto drainage data are available from Sabre<br />

Farms (Nass et al. 1990), Continental Construction<br />

(Pacheco 1987), Peters Cave (Prufer and McKenzie<br />

1966), and Harness-28 (Otto 1983). Located to the east<br />

in the Muskingum River drainage are Philo II and<br />

Longacre (Morton 1984, 1989), Locust (Seeman 1985),<br />

and the Hunter 1 (Church 1991) sites, and the<br />

Childers and Woods sites (Shott and Jefferies 1990;<br />

1992) in West Virginia (Figure 2.4).<br />

During the early Late Woodland period (ca. A.D.<br />

400-<strong>700</strong>), sites were nucleated, multihousehold settlements<br />

(1-3 ha in size) located on bluffs of major rivers<br />

or streams, and frequently surrounded by an earthwork<br />

or ditch feature (Church 1987; Dancey 1988).<br />

This pattern stands in contrast to the preceding<br />

Middle Woodland pattern of dispersed household<br />

units (Dancey 1988, 1991, 1992). Mounds are not present<br />

at these sites (e.g., Water Plant [Dancey et al.<br />

1987], Zencor/Scioto Trails [Otto 1982], and<br />

Highbanks in Franklin County, Ohio). However, during<br />

the succeeding late Late Woodland period (ca.<br />

A.D. <strong>700</strong>-950/1000), the settlement pattern changed in<br />

three ways. First, site location shifted predominantly<br />

to river and stream terraces or floodplains. Second,<br />

the area of a site occupied at any one time decreased<br />

in size. Third, site types varied considerably, as evidenced<br />

by structure and associated features (Table<br />

2.1). For example, in the northern Scioto drainage,<br />

sites like Walter S. Cole, Ufferman, DECCO, and<br />

Hartley Farm vary between 0.1 and 0.4 ha in size and<br />

are scattered along the terrace and floodplain of the<br />

16 Church and Nass

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