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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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LOCAL LEVEL ANALYSIS<br />

Local level analysis of the Park Creek II site provided<br />

baseline data for modeling settlement and subsistence<br />

in the Upper Susquehanna Valley. The identification of<br />

activity areas, based on artifact and feature types, artifact<br />

densities and attributes, and their locations within<br />

a site, can inform upon activities performed by groups<br />

and individuals at a site or in a particular structure<br />

(Flannery and Winter 1976; Jamieson 1988; Kapches<br />

1979; Kent 1984, 1987, 1990; Nass 1989; Nass and Yerkes<br />

1995; Newell 1987; Prezzano 1992; Seymour and<br />

Schiffer 1987; Stahl 1985; von Gernet 1982; Warrick<br />

1984; Yellen 1977). When interpreted with care, activity<br />

areas can tell us about size and composition of households<br />

and communities, defense, interaction with other<br />

groups, crafts, production, and exchange (Allison 1999;<br />

Cameron 1993; Hayden 1982; Hitchcock 1987; Lyman<br />

1994; Rogers 1995; Schiffer 1987, 1995). From community<br />

layout one can understand “the more intangible<br />

aspects of past cultural behavior (residence patterns,<br />

socio-political organization and ceremonial activity)”<br />

(Warrick 1984:1; see also Jamieson 1988:308). In addition<br />

to artifact types and densities, features are important<br />

artifacts in that their functions and organization<br />

can tell much about community activities and social<br />

relations. Although identification of feature function is<br />

problematic in that not all feature contents represent<br />

the feature’s original function, features are important<br />

in identifying activity areas, as many activities may<br />

have centered around particular feature types (e.g.,<br />

hearths) (Schiffer 1987:32; Stewart 1977:17).<br />

Activities of groups and/or individuals at a site are<br />

reflected in the types and locations of artifacts, features,<br />

and structures. The spatial organization of a site provides<br />

insights into aspects of the economic and political<br />

organization of a given society in a given historical<br />

context (Matson 1996:107). The Park Creek II site was<br />

an ideal site for examining intrasite variability and<br />

community organization. Excavation methods were<br />

designed to obtain a variety of data types, including<br />

spatially controlled artifact distributions and feature<br />

data. Block excavations provided information on artifact<br />

patterning and the nature of occupation.<br />

THE PARK CREEK II SITE<br />

Archaeologists from the Public Archaeology<br />

Facility (PAF) identified the Park Creek II site (SUBi-<br />

1464) in 1993 during a cultural resource reconnaissance<br />

survey in advance of proposed improvements<br />

to New York State Route 17. At this time, a site examination<br />

was also conducted (Lain et al. 1993). The Park<br />

Creek II site was declared eligible for the National<br />

Register of Historic Places and construction plans<br />

could not be modified to avoid impacting the site.<br />

During the fall of 1998 and spring of 1999, PAF<br />

archaeologists performed data recovery excavations<br />

(Versaggi et al. 1996). The combined site examination<br />

and data recovery units covered an area of 24 m 2 at<br />

the site (Figure 10.2).<br />

Park Creek II was situated in an upland valley of<br />

the Susquehanna River, near West Windsor, New York<br />

(Figure 10.1). The site occurred in a long, narrow eastwest<br />

hollow, surrounded on two sides by steep ridges<br />

and was drained by Park Creek. This upland area<br />

consists of glacial till deposits that have been cut and<br />

eroded by creeks since glacial retreat.<br />

Site stratigraphy was complex, and, in brief, consisted<br />

of four A horizons (Cremeens 1999). The first two A<br />

horizons, A1 and A2, contained very low artifact densities<br />

and no features. Therefore, this analysis concentrated<br />

on the two lowest horizons, A3 and A4, respectively.<br />

The B2 horizon, which separated the A3 and A4<br />

horizons, was excluded from analysis given the difficulty<br />

of assigning the artifacts to either the A3 or A4<br />

horizons with any confidence. Four radiocarbon dates<br />

were obtained from feature contexts associated with<br />

the A3 and A4 horizons (Table 10.1). One radiocarbon<br />

assay returned a date of 2170±60 B.P., far too early for<br />

the early Late Prehistoric. However, this was also the<br />

only conventional radiocarbon assay, and a feature<br />

from the same horizon contained maize and produced<br />

an early Late Prehistoric date. Given these dates and<br />

the presence of maize, I believe that the A4 horizon represented<br />

a fourteenth century occupation and the A3,<br />

an early fifteenth century occupation.<br />

The Fourteenth Century Occupation<br />

at the Park Creek II Site<br />

Archaeologists identified 23 artifacts from feature<br />

and nonfeature contexts associated with the fourteenth<br />

century occupation (A4 horizon). Artifacts<br />

included cortical and noncortical flakes, one graver<br />

on a flake, and one ground-stone flake.<br />

Unlike most campsites, Park Creek II yielded a<br />

wealth of feature data. Feature function was interpreted<br />

using the variables of size and shape (Stewart<br />

1977), types of artifacts present (including floral and<br />

faunal remains), density of artifacts (particularly<br />

tools), and the presence of oxidized soil and/or<br />

Chapter 10 Upland Land Use Patterns during the Early Late Prehistoric (A.D. <strong>700</strong><strong>–1300</strong>) 195

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