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