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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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e<br />

Bull's<br />

Point<br />

C o o t e s<br />

P a r a<br />

Sassafras Point<br />

d i s<br />

Princess Point<br />

Cattail marsh<br />

Shallow water<br />

N<br />

0 1000 m<br />

J. Skiba<br />

Figure 5.5. Cootes Paradise.<br />

seems the most reasonable interpretation at present. Its<br />

geographic situation is typical of later Iroquoian village<br />

sites, and atypical of known Princess Point components.<br />

The radiocarbon dates for Lone Pine and its seriation<br />

later than Porteous suggest that Lone Pine could<br />

be considered a Glen Meyer site. On the other hand,<br />

the pottery styles from both Porteous and Lone Pine<br />

have clearer affinities with Princess Point than with<br />

later Glen Meyer ceramics. We will return to this<br />

thorny issue later in the paper.<br />

Young 1 (AfGx-6)<br />

The Young 1 site was discovered during Stothers’<br />

survey of the lower Grand River Valley. It is a small site<br />

located on a terrace above the Grand River, on the edge<br />

of a knoll about 400 m from the river and about 0.5 km<br />

from the Grand Banks site. It is heavily plough disturbed<br />

except for a fencerow running over the knoll,<br />

and is underlain by heavy clay. The plowing has<br />

brought heavy clay through to the surface, making<br />

excavation exceedingly difficult and screening nearly<br />

impossible. Nevertheless, a number of shovel test pits<br />

were excavated as well as two 1 sq. m test squares in<br />

1993. A very small and fragmentary artifact sample<br />

was recovered, including cord-wrapped stick marked<br />

rim sherd and a limited number of flakes. Young 1 may<br />

be a short-term seasonal camp, perhaps a spring refuge<br />

from minor flooding for inhabitants of the Grand<br />

Banks site, but data are too limited to be definitive.<br />

Cootes Paradise<br />

Cootes Paradise is a sizable wetland at the western<br />

tip of Lake Ontario (Figure 5.5). Until about one hundred<br />

years ago, it was apparently a true marshland<br />

dominated by cattail and sedge. Modification through<br />

canal construction and the introduction of carp produced<br />

the present body of shallow open water (Figure<br />

5.5). Excavations were conducted at the Princess Point<br />

type site by Stothers and Kenyon in 1968, and by Noble<br />

in 1969 (Stothers 1969). Also in 1969, Stothers conducted<br />

an archaeological survey around the periphery of<br />

Cootes Paradise and found an additional six Princess<br />

Point sites (Stothers n.d.). The Old Lilac Gardens site<br />

underwent mitigative excavation in 1984 to rescue a<br />

portion of it from impact by the construction of<br />

Highway 403 (Knight 1984). Smith directed two<br />

University of Toronto archaeological field schools, one<br />

in 1995 and another in 1996, in the Royal Botanical<br />

Gardens area of Cootes Paradise (Smith 1996c).<br />

The Princess Point occupation of Cootes Paradise is<br />

represented by a variety of settlement locations and<br />

sizes, although estimates of site dimension for most of<br />

these is hampered by a lack of extensive investigation.<br />

Both the Princess Point (AhGx-1) and Sassafras Point<br />

(AhGx-3) sites are situated on low-lying peninsulas<br />

and appear to be the largest occupations at Cootes<br />

Paradise. The Old Lilac Gardens site (AhGx-6), is located<br />

on a peninsula higher above the water and is smaller<br />

than either Princess or Sassafras Point. The<br />

Chapter 5 Recent Developments in the Archaeology of the Princess Point Complex in Southern Ontario 107

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