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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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The appearance of the thicker-walled pottery during<br />

the late Middle Woodland to early Late Woodland<br />

transition period suggests this might have been a<br />

period of initial experimentation with maize and its<br />

cooking. Subsequent to this, thinner-walled vessels<br />

begin to appear, and some of these resemble the<br />

Middle and Late Owasco types (Ritchie and<br />

MacNeish 1949). As Braun (1980:96, 1983:118-119) has<br />

argued, changes in ceramic manufacture during the<br />

Woodland period may reflect changes in dietary patterns,<br />

such as a shift to the greater use of starchy<br />

seeds, which are best cooked through long simmering<br />

or boiling in order to increase palatability and<br />

digestibility. Thinner, denser walls and finer temper<br />

would increase the vessel’s performance in these circumstances.<br />

The later Middle and Late Woodland<br />

vessels from Winney’s Rift were better suited to withstand<br />

thermal shock due to longer boiling than were<br />

the earlier Middle Woodland vessels, which were produced<br />

to withstand breakage from mechanical stress.<br />

In addition to the large component at Winney‘s<br />

Rift, the transitional Middle to Late Woodland vessels<br />

have been recovered from several sites in Saratoga<br />

County. The combination of both Middle Woodland<br />

and Late Woodland ceramic traits in the same component,<br />

and often on the same vessel, appears to be characteristic<br />

of the upper Hudson River area on this time<br />

level. Because of this, the stage division between the<br />

Middle and Late Woodland based on Ritchie and<br />

MacNeish’s (1949) ceramic typology does not resemble<br />

that reported elsewhere in New York State<br />

(Brumbach 1995:58). Thermoluminescence (TL) and<br />

radiocarbon dating place these vessels at A.D. 1200-<br />

1300, and contemporaneous with early Late<br />

Woodland Owasco ceramics found elsewhere in New<br />

York (Brumbach 1995:58). A sherd from Winney’s Rift,<br />

dated by TL to A.D. 1310±75 (Alpha-2324), was constructed<br />

and decorated with a combination of attributes<br />

of the Middle Woodland type Jack’s Reef Corded<br />

Collar and the Late Woodland type Levanna Corded<br />

Collar (Ritchie and MacNeish 1949). Carbon samples<br />

from a feature and an associated living floor at the<br />

Mechanicville Road site in Saratoga County containing<br />

similar pottery, produced dates of A.D. 1220±70<br />

(DICARB 1565) and A.D. 1300±40 (DICARB 1567),<br />

both uncorrected (Hartgen Archeological Associates,<br />

Inc., 1983:227).<br />

After ca. A.D. 1200-1300, there were additional<br />

changes in ceramic manufacture: Vessel walls become<br />

progressively thinner, presumably because the technology<br />

necessary to construct a larger vessel without<br />

greatly increasing the thickness of the wall was<br />

achieved. The appearance of these vessels seems to<br />

signal concurrent changes in the diet with an<br />

increased reliance on maize, eventually leading to the<br />

focus described in the early 1600s documents.<br />

The Late Woodland pottery of the upper Hudson<br />

River continues to undergo major changes in manufacturing<br />

technique, and by A.D. 1400, came to resemble<br />

both in style and technology the pottery produced<br />

at the Mohawk Iroquois villages to the west (Bender<br />

and Brumbach 1992; Brumbach 1975, 1995), and to a<br />

lesser degree, pottery recovered from Late Woodland<br />

Delaware sites of New Jersey and southern New York<br />

(Kraft 1986). These large Late Woodland vessels tend<br />

to be globular in shape with modeled collared rims<br />

and incised decorations. Walls are extremely thin and<br />

the paste is very compact with fine aplastics. Exterior<br />

surfaces are smoothed and often finished by polishing<br />

or burnishing. Coiling as a building technique<br />

appears to have been replaced by another hand-building<br />

method termed “drawing” (Rice 1987:124-125).<br />

That fish continued to be an important dietary staple<br />

in the upper Hudson Valley even after A.D. <strong>700</strong> is<br />

demonstrated by the recovery of hundreds of small<br />

fish vertebrae from flotation samples at Winney’s Rift.<br />

Additionally, Late Woodland features recorded at this<br />

site include a large hearth with charcoal-saturated<br />

soil, but few rocks. We interpret it as a feature that<br />

might have served for the smoke drying of fish.<br />

However, even as fishing remained an important economic<br />

activity, changes in harvesting technology<br />

apparently were taking place. Winney’s Rift produced<br />

a number of net sinkers, an artifact type almost absent<br />

from Schuylerville. The shift to a different location for<br />

fishing, combined with inferred changes in labor allocation<br />

(as we argue below), appears to have had consequences<br />

for the technology involved in fish harvesting.<br />

Perhaps this period saw a shift away from the use<br />

of fixed weirs and natural impediments alone to an<br />

increase in the use of more portable set nets.<br />

These data on the technology of fish harvesting,<br />

resource processing, and ceramic production thus<br />

indicate that significant but gradual changes were<br />

taking place in upper Hudson Valley subsistence systems.<br />

In addition, shifts in settlement geography from<br />

prime fishing locations (Schuylerville) to locations<br />

favorable to both fishing and gardening (Winney’s<br />

Rift), and later during the middle Late Woodland to<br />

locations in proximity to more arable garden lands on<br />

the islands and floodplains of the major rivers, support<br />

our arguments. The shifts in settlement locations<br />

along Fish Creek mirrors large-scale settlement shifts<br />

for this period identified in Bender and Curtin’s<br />

236 Brumbach and Bender

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