pip. n1)^' 2^5T JOHN H. KERR RESERVOIR BASIN — MILLER 



153 



Figure 23. — Jar-shape sequence found in the Clarksville site, 44Mcl4. 



55) . The main difference is in the temper. The Dan Kiver Series is 

 predominantly a crushed-quartz-tempered ware blending into a sand- 

 tempered ware, while the Clarksville Series is unitempered, i.e., sand- 

 tempered. No type of crushed stone was used as an aplastic within 

 the reservoir area. This trend reflects a northeasterly influence com- 

 ing in through central and northern Virginia from Maryland and 

 Pennsylvania and a connection with various Algonquian types indi- 

 cated by Parker (1920) and Holmes (1885; 1903). 



From the Early Woodland olla (pi. 56, h; fig. 24) evolved a vessel re- 

 taining the characteristic conoidal base but modified by the introduc- 

 tion of a pronounced shoulder surmounted by a vertical or slightly con- 

 stricted neck (fig. 25). Necks in some instances were elongated. Lip 

 configuration remained unchanged; paste characteristics were 

 stabilized. 



