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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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1949 (Figure 7.2). In this publication, Owasco vessels<br />

are described as cordmarked containers with cordwrapped<br />

stick and paddle motifs appearing on the<br />

shoulder, lip, and exterior rims (Lenig 2000; Ritchie and<br />

MacNeish 1949). Although Ritchie (1994:290) indicates<br />

that Owasco vessels were predominantly manufactured<br />

by the paddle and anvil method, fracture plains<br />

indicative of coiling have been identified on early<br />

Owasco ceramics in New York (Prezzano 1986; Rieth<br />

1997, this volume), suggesting that more than one<br />

method may have been used in the construction of<br />

these containers. Ceramics found on sites dating to the<br />

Carpenter Brook phase generally exhibit elongated<br />

bodies and everted rims. Over time, the bodies become<br />

more globular and the rims outflaring. Most vessels<br />

were collared with rounded bases and incised exterior<br />

designs by the Castle Creek Phase (Prezzano 1986;<br />

Ritchie and MacNeish 1949).<br />

Owasco vessels found on early Late Prehistoric sites<br />

in New York and Pennsylvania are largely grit<br />

(crushed rock) tempered. Quartz is often identified as<br />

the major constituent of grit, with gneiss, shale, and<br />

other crushed crystalline materials occurring in much<br />

smaller frequencies (Ritchie and MacNeish 1949:114-<br />

115). Although Lucy (1991a) indicates that chert-tempered<br />

containers are regularly found on Owasco sites<br />

in northern Pennsylvania, such containers are not regularly<br />

found on sites in New York (Rieth 1997; Ritchie<br />

and Funk 1973; Ritchie and MacNeish 1949). Shell tempering<br />

also does not appear to have been extensively<br />

used, as evidenced by the limited number of shell-tempered<br />

sherds from Owasco sites (Crannell 1970; Ritchie<br />

1944). <strong>Change</strong>s in lateral pore spaces, temper density,<br />

and temper size are noted (Prezzano 1986; Rieth,<br />

Chapter 11, this volume), and suggest changes in the<br />

manufacture of Owasco containers over time.<br />

Figure 7.2. Drawing of a Carpenter Brook Cord-on-<br />

Cord sherd from the Tioga Point Farm site.<br />

Problems Inherent in the Use of Ceramic Types<br />

<strong>Northeast</strong> archaeologists have applied the type concept<br />

to the study of prehistoric ceramics since the first<br />

half of the twentieth century (e.g., Ritchie 1944; Ritchie<br />

and MacNeish 1949). Recently, however, some<br />

<strong>Northeast</strong> archaeologists (Chilton 1999; Lizee et al.<br />

1995; Pretola 2000) have questioned the role and applicability<br />

of the type concept to the study of archaeological<br />

ceramics. As used here, a type is defined as “a<br />

group of objects exhibiting interrelated similar features<br />

which have temporal and spatial significance” (Ritchie<br />

and MacNeish 1949:98). Recently, Chilton (1999:98) has<br />

argued that ceramic types often serve as shorthand for<br />

a range of stylistic attributes and are often used to refer<br />

to distinct archaeological cultures eventually becoming<br />

conflated with specific ethnic groups.<br />

There are several problems with the type concept<br />

and its application to the study of prehistoric ceramics<br />

in northcentral Pennsylvania. Among the most serious<br />

problems is the fact that Clemson Island and Owasco<br />

types (and its resulting classifications) are not derived<br />

from theory used to explain the past (Adams and<br />

Adams 1991:312-312; Dunnell 1986:180, 192-193; Hart<br />

1999). Unfortunately, the belief that classification is<br />

equivalent to theory has resulted in the construction of<br />

units that are extentionally defined, often masking the<br />

unique attributes of archaeological assemblages, making<br />

it easy to argue for the continuity of types through<br />

time (Hart 1999; Pretola 2000:6). In central<br />

Pennsylvania, as ceramics with unique or diverse<br />

attributes are identified, they are often dealt with either<br />

by (1) introducing new types into existing classification<br />

systems, or (2) splitting existing types into smaller,<br />

more detailed units (i.e., Hay et al. 1987; Hatch 1980;<br />

Stewart 1990, 1994). The result is a classification<br />

scheme that is both cumbersome to use and subject to<br />

continuous revision (Hart 1999). As demonstrated in<br />

southern New England (Chilton 1999:100), continuous<br />

revision ultimately obscures existing typologies, making<br />

it difficult to place sherds within known types since<br />

they exhibit traits belonging to several types.<br />

A second problem is that type names developed for<br />

specific geographic regions are often applied to similar<br />

types in other regions with little or no investigation of<br />

the timing and/or origin of such traits and often resulting<br />

in the false conclusion that one group was greatly<br />

influenced by another (Chilton 1999:100). In northcentral<br />

Pennsylvania, ceramic types belonging to the<br />

Owasco tradition (e.g., Levanna Cord-on-Cord,<br />

Carpenter Brook Cord-on-Cord, etc.) are often applied<br />

to Clemson Island containers, leading to the impression<br />

138 Rieth

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