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

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

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CHAPTER 4<br />

THE EARLY LATE WOODLAND<br />

IN THE SOUTHWESTERN LAKE ERIE LITTORAL REGION<br />

David M. Stothers and Timothy J. Abel<br />

INTRODUCTION<br />

This chapter is an overview of the current early Late<br />

Woodland (ca. A.D. 500-1300) database in the southwestern<br />

Lake Erie littoral region, essentially the area<br />

lying in northwestern Ohio and southeastern<br />

Michigan. Our aim is to review data previously published<br />

elsewhere, present data previously unpublished<br />

or unsynthesized, and provide an interpretation of the<br />

early Late Woodland time period. This interpretation is<br />

influenced by our readings on the roles that politics,<br />

power, and resource distribution have had in history<br />

(Wolf 1997). Many will doubt the applicability of such<br />

concepts to nonstratified societies as the early Late<br />

Woodland societies in the <strong>Northeast</strong> were, but such<br />

forces have existed for much of human history (Cobb<br />

1993) and no doubt influenced prehistoric societies —<br />

much more so, we believe, than many would<br />

acknowledge. The difficulty is not in the concepts but<br />

in our modern views of them, which are shaped by<br />

the society in which we live.<br />

CHRONOLOGY, TAXONOMY,<br />

AND CULTURE<br />

At the A.D. 500 time level, the southwestern Lake<br />

Erie region was occupied by two contiguous archaeological<br />

cultures (Figure 4.1). The westernmost culture,<br />

occupying the coastal marshes surrounding the western<br />

Lake Erie shoreline, is called the Western Basin<br />

Tradition (WBT), consisting of the Gibraltar (A.D. 500-<br />

750), Riviere au Vase (A.D. 750-1000), Younge (A.D.<br />

1000-1200), and Springwells (A.D. 1200-1350) phases.<br />

The cultural manifestation now attributed to the WBT<br />

Gibraltar phase was formerly subsumed into a poorly<br />

defined, noncontinuous and problematic “Wayne<br />

Tradition” (cf. Stothers 1999). Stothers (1994, 1995) has<br />

argued that the Wayne Tradition, and its attendant<br />

“Wayne Mortuary Complex” (Halsey 1999), are integral<br />

aspects of the WBT, which show continuity into<br />

the Riviere au Vase and Younge phases, and that use of<br />

the term in the southwestern Lake Erie region is taxonomically<br />

unsound. The terminology used here is<br />

derived from the cultural chronology forwarded by<br />

Stothers (1999).<br />

Present data suggest that this manifestation originated<br />

in southernmost peninsular Ontario and contiguous<br />

areas of Michigan (Murphy and Ferris 1990; Stothers<br />

and Bechtel 2000). The WBT appears to have been oriented<br />

to the stream estuaries and sand points of northwestern<br />

Lake Erie and Lake St. Clair, and by A.D. <strong>700</strong>,<br />

this manifestation had spread around the western end<br />

of Lake Erie and across the Erie Islands to occupy the<br />

coastal marshes of the southwestern Lake Erie shore. In<br />

the Sandusky Bay region, they appear to have<br />

encroached upon the other cultural manifestation of<br />

the region, the Sandusky Tradition (ST), which appears<br />

to have originated in northcentral Ohio from a Middle<br />

Woodland Esch phase base. The ST consists of the<br />

Green Creek (A.D. 500-1000), Eiden (A.D. 1000-1250),<br />

Wolf (A.D. 1250-1450), Fort Meigs (A.D. 1450-1550),<br />

and Indian Hills (A.D. 1550-1650) phases, of which<br />

only the first three are discussed here. By A.D. 1200, the<br />

ST had shifted to inland semipermanent settlements<br />

along major lake-draining streams, and territorially<br />

expanded westward around the western end of Lake<br />

Erie into southeastern Michigan and southwestern<br />

Ontario, eventually replacing the WBT. By A.D. 1300,<br />

the WBT had been pushed into the upper reaches of the<br />

Maumee River in Indiana, the upper lower peninsula<br />

of Michigan, and the upper Sydenham River in Ontario<br />

(Figure 4.2) (Stothers 1995, 1999; Stothers and Bechtel<br />

2000; Stothers and Schneider in press).<br />

<strong>Northeast</strong> <strong>Subsistence</strong>-<strong>Settlement</strong> <strong>Change</strong>: A.D. <strong>700</strong><strong>–1300</strong> by John P. Hart and Christina B. Rieth. New York State Museum<br />

© 2002 by the University of the State of New York, The State Education Department, Albany, New York. All rights reserved.<br />

Chapter 4 The Early Late Woodland in the Southwestern Lake Erie Littoral Region 73

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