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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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elsewhere, present data previously unpublished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