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I 1 Sierra Nevada Batholith to the east The sediments range in age andfrom Recent to Cretaceous & Possibly epeated re�rori�iu�der, 4c�� Ilnds , gravels, silts, & clays produced by r outwash from the Sierras. ' Relief is very flat, less than 5' /mile, with drainage to the s the Sacramento-Stockton Delta area. The southeast toward one mile to the north---northeast, and Calaveras River is about Mormon Slough is roughly 2 miles to the sc�uLti. PLATE r�- f iri USGS topographic sheet, shows tha e location of the property relation to other nearby features. ' SOlL Ci,ASSIF I(:A'I'XON- ty Of According to the 1952 publication issued' byishe. Uniiversitockton California, Berkley, the soil is this are Adobe Clay. It is a dark grey to brown alluvial :,ull dere-Ved as outwash from basic igneous sources, ( ie, the Sierra NhavdngBath- olith ) It Is considered to have imperfect drainage, ' hardpan subsoil layers generally underlain with unconsolidated material. The Storie Index, 28, gives it a Ql&5biflcaL0" as poor. PLATE III is a portion of a soils presiiie maty irvsri Lim, above publication_ DEPrfl TO GROUNDWATER- Based upon the fall 1992 water table map issued by 6.t`vunuwa�.er e Sall Joaquin County Flood Control District, 'r�r��r. IY,� ge was measured at between 60' & �(0' bgl a E, t��i s IouaL.Lon, more ms ' recent data indicates that water levels have rr � uau�Uuc bus 5' since those measurements were made. However, lashed data, the highest water level in the last 10 gears was ' measured at about 27 ' bgl at this site LOCA' ION OF NEARBY__WELLS= er ' The wells that the Flood Conearattachedict PLATEeVfwhichor trevealsl measurements are shown on th that there are no control Caurtity fmiesi�erevnotns�archedthe in ' site Due to time const order to locate any additional commercial , domestic, or ground- water monitoring wells. None were noted in the area during a field visit, but If' neceessary,tfurther investigation will be conducted Prior to ca 2