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The cultural period of origin for the flakes could not be determined . This site is really outside of the project boundaries (Figure 1 ) . No other archaeological surveys had been reported in the St . Mary ' s project area. An archaeological survey for Cate ' s Ford Access Area for the Eno River State Park in 1982 ( found south of the St . Mary ' s Road project boundaries) revealed a thin scatter of Archaic and Woodland period artifacts along a ridgetop ( 31 Orl 76 ; Hargrove 1982 : 27) . A few additional lithics of undetermined origin were also recovered from a severely eroded portion of the Park (Area 1 , ARC- Or4 ) . In 1940 Joffre L . Coe recorded the presence of two sites located at the confluence of Buckwater Creek and the Eno River. Site 31 Orl2 , found in the northwest corner of that intersection, contained "potsherds, projectile points , a lead shot, and an atlat" fragment (North Carolina Archaeological Site Form, on file at the Office of State Archaeology in Raleigh) . The site he recorded immed iately ately to the east (31 Or14, northeast corner of the confluence) yielded "Sherds, projectile points, blades, [a] soapstone sherd, abraiding stone, chips, cs (chipped stone) drill frag(ment) " (North Carolina Archaeological Site Form, on file at the Office of State Archaeology in Raleigh) . Based on these results, combined with the results of a general countywide archaeological assessment (Daniel 1994 : 95 -97), it is anticipated that prehistoric sites will be found in the vicinity of the St. Mary ' s Corridor. Adapting Daniel ' s predictive model to the St. Mary ' s Project, archaeologists can divide oject area into three zones of differing site probability for prehist the pr oric sites : Zone I , with the highest density of sites and the highest probability for intact, subsurface remains , takes in inhabitable floodplains and terraces or ridges just above floodplains . In the St. Mary ' s Road vicinity, this zone would parallel the Eno River and some of its larger creek tributaries . The site- filled Occaneechi Bend at Hillsborough is a good example of a Zone I area. Some of the better-drained floodplains along Buckwater Creek and areas adjacent to Little Creek and Strouds Creek might qualify as Zone I . Zone II , a medium probability area, takes in ridges and hilltops within one kilometer (about 3 , 300 feet) of the main drainage channels . Prehistoric sites are common in this area and a few sites might have intact, subsurface remains, although these remains will not be as common as in Zone I . The Zone II areas along St . Mary' s Road take in most of the corridor from Hillsborough as far east as the intersection with New Sharon Church Road , Zone III , the low probability area, consists of other upland areas, mostly ridges and hilltops more than a kilometer (about 3 , 300 feet) from main drainage channels . Most of these sites are low density lithic sites dating to the Archaic period in plowzone or surface contexts . Most of the St. Mary ' s study area runs through these upland inter- riverme areas . Daniel ( 1994 : 95 - 97) does mention the historic archaeological potential for these zones of relative archaeological site probability. He states that one could expect mill sites in those portions of Zone 1 which contain selected criteria for mill and mill dam placement (e . g . , strong stream gradient , fieldstone for construction) . A number of historic mills were once "seated" along the Eno River and some of its tributaries, such as Stroud ' s Creek ( see below) . The hilltops and ridges of Zone II , the upland areas within about 3 , 300 feet of the main drainage channels, are expected to contain occasional historic farmsteads and/or cemeteries (Daniel 1994 : 95) . The probability of discovering historic sites in the remaining uplands (Zone III) is not specifically discussed (Daniel 21