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MHY-14-1992 17 15 FROM Mills Associates TO San Joaquin Co P.05 <br /> BUCKEYE RANCH ( 4-1-92 ) 5 <br /> excavatable material and possible human remains needs to be <br /> defined at this site . <br /> JANUARY 24, 1992 VISIT TO THE PROPOSED BUCKEYE RANCH PROJECT <br /> On January* 24', 1992 Dave Fisher visited the project with. <br /> Professor Johnson. One of the main goals of ,this visit was to <br /> collect a small number of soil samples to see if the limits of <br /> the midden deposits within the project could be defined using a <br /> varietv of chemical tests . The site which encompasses <br /> wa visi a and two soil samples were collected. A simple was <br /> co lecte rom a 15 foot diaMete it and another sample was <br /> extracts rom an adjacent pit 3� eet on its longest side in the <br /> location of One sample came from , ( near Site <br /> , and another was taken east of tnis location. Three <br /> samples were taken beginning at <br /> ( these locations corresnond fairlY closely to locaLions . <br /> 3, 1 , and 20 shown on a <br /> that is on file at the <br /> A Copy vi Luis map was included in the <br /> record search and was provided to- the consulting <br /> archaeologists . The tenth sample came from near the center of <br /> , and the last soil was collected from <br /> -near the proposed • <br /> The eleven soil samples were extracted below the grass and duff <br /> level from depths of ten to 20 centimeters . Each sample was <br /> tested for phosphates . carbonates , pH, and the color was <br /> determined using a Munsell soil color chart . Prior to collecting <br /> the soil it was determined on the basis of soil maps .prepared by <br /> the Soil Conservation Service that most of the existing soils in <br /> the project had a pH of acid to neutral . Investigations by <br /> archaeologists at California State University, Sacramento ( CSUS ) <br /> since 1975 have shown that archaeological sites throu;pout much <br /> of the Sacramento valley and Delta tend to have alkaline pH <br /> levels and if they are late in time carbonates will also be <br /> present . Additional studies have also demonstrated that the <br /> relative depth to which carbonates have leached in an <br /> archaeological midden ,can provide. a relative idea concerning the <br /> possible antiquity of the site. This method was pioneered. by <br /> James Johnston at CSUS . in 1974-1975. He had been an agricultural <br /> sciences major at California Polytechnic University and had <br /> extensive experience with soil chemistry. -The carbonate dating <br /> technique has been used extensively in the southern Cascade <br /> Mountains , in the upper Sacramento valley, on the western side of <br /> the lower- Sacramento valley and Delta (particularly on Laguna <br /> Creek at CA-SAC-265 (Sheeders 1983; between the Cosumnes and <br /> Mokelumne Rivers ) and CA-SAC-267 (Johnson 1976 ; on the Cosumnes <br /> River near Sloughhouse ) . In order for it to work carbonates have <br /> to be present , the surrounding soils must be acidic or neutral <br /> and the archaeological deposits must be alkaline. All of these <br /> conditions are met at Buckeye Ranch and the almost exact <br /> definition of the limits of the middens and their probable <br /> general antiquity can be determined by collecting and analyzing a <br /> series of small samples ( less than 50 grams ) taken from <br /> relatively shallow depths within the soil . This methodology is <br /> relatively inexpensive and used in con4unction with auguring to <br /> determine accurate depths of the identified deposits can be <br />