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Archaeological Investigations at Yourhaney Plantation (38GE18)

Archaeological Investigations at Yourhaney Plantation (38GE18)

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226Table 39. Attributes of Projectile Points from <strong>38GE18</strong>.Type M<strong>at</strong>erial L W T BL HW NotesHump couldn't be removed –Triangular Porphyritic Rhyolite unk. 2.4 0.9tip broken (Bag 97)Triangular Porphyritic Rhyolite unk. 2.5 0.6 tip broken (Bag 157)Triangular Plain Rhyolite unk. 1.9 0.5 tip broken (Bag 68)Small Savannah RiverStemmed Orthoquartzite 5.3 3.5 1.1 4.5 2 Bag 7Morrow Mountain II Porphytric Rhyolite 4.3 3 1.2 2.6 1.9 Bag 2Palmer Corner Notched Flow Banded Rhyolite 3.4 2.2 1 2.6 1.2 very tip end broken off (Bag 8)Projectile PointsTOOLSRel<strong>at</strong>ively few projectile points were recovered from the excav<strong>at</strong>ions <strong>at</strong> Yauhannah Bluff. A total ofsix points were recovered and their characteristics are presented in Table 39. Three triangularpoints were recovered, which were manufactured from metavolcanic m<strong>at</strong>erials. One appears tohave broken during manufacture, as it had a large hump on one side th<strong>at</strong> apparently could not beremoved. Their width ranged from 1.9 to 2.5 cms and thickness (without the hump) ranged from0.5 to 0.6 cms. A trend for decreasing triangular size through time occurs from the MiddleWoodland on (Coe 1964; Keel 1976). Basal width of triangular points has been thought to be apotentially good discrimin<strong>at</strong>or of temporal affili<strong>at</strong>ion. At 38SU83 in the Upper Coastal Plain,Blanton (et al. 1986) was able to deline<strong>at</strong>e three distinct groups of triangular point. Those withbases averaging 1.2 cm were <strong>at</strong>tributed to the Pee Dee (Mississippian) component. Pointsassoci<strong>at</strong>ed with the other two groups all had basal widths of not less than 1.7 cms and weregenerally deposited deep. They were in associ<strong>at</strong>ion with Woodland assemblages. A roughlysimilar p<strong>at</strong>tern was observed <strong>at</strong> the M<strong>at</strong>tasee Lake sites on the Santee River (Anderson et al. 1982:151-155). It is therefore assumed th<strong>at</strong> these are all affili<strong>at</strong>ed with Woodland contexts. Thesepoints were recovered from Fe<strong>at</strong>ure 108, which was a burned tree (Bag 68), Fe<strong>at</strong>ure 141 – anhistoric post (Bag 97), and Fe<strong>at</strong>ure 288 – another historic post (Bag 157).The Small Savannah River Stemmed point was surface collected from grid point N510E548 (Bag7), which is in the vicinity of the stick and clay chimney associ<strong>at</strong>ed with the main plant<strong>at</strong>ion house.Savannah River Stemmed points d<strong>at</strong>e from the L<strong>at</strong>e Archaic to Early Woodland periods. Oliver(1985) and Coe (1964) indic<strong>at</strong>e th<strong>at</strong> Savannah River Stemmed points become smaller over timewith the evolution being Savannah River Stemmed, Small Savannah River Stemmed, and GypsyStemmed. Oliver (1985) st<strong>at</strong>es th<strong>at</strong> the Small Savannah River Stemmed marks the terminal part ofthe L<strong>at</strong>e Archaic Period.The Morrow Mountain II point was surface collected during the mechanical stripping of the site(Bag 2). According to Coe (1964: 37) Morrow Mountain II points are typically 3.0 to 8.0 inlength, averaging 6.0 cms. The width ranges from 1.8 to 3.0, averaging 2.0 cms.

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