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y ' <br /> I e .rp <br /> located 4 1/2 miles to the east_ The junction Of highways ]? and <br /> Be, the two major roadways in th�:, area, is 2 miles to the east. <br /> GEOLOGIC w TOPOGRAHIC SETTING: The property is located on thOf <br /> e <br /> eastern edge ❑f the Sacramento Valley at an elevation ed <br /> approximately 95 feet MSL; (Plate II. ) Ag9reD <br /> iter are extracted <br /> r❑ arty on the southeast. <br /> from the various abandoned stream channels and tributar,.es Of e <br /> which borders the P P but because of the <br /> hlakelumne River, <br /> is to the west, determine the <br /> The regional 9 it is difficult to <br /> of the terrain, The Mokelumne fiver, which <br /> irregularitydegree ❑f accuracy. <br /> slope with any Nevada Mountains to the ,:.art, and <br /> has its source in the Sierra regrates being mined, meanders in <br /> provides the source far the ag9 ties into the Delta area in <br /> a general southwest direction and amp <br /> the city of Stockton. <br /> & PROFILE: According to the publication <br /> SOIL CLASSIFICATION <br /> San Joaquin County California" issued by the <br /> entitled "Sails Of <br /> Of California College of <br /> primarily ❑f <br /> Division of Soils °thehsoilslinr5this area consist Columbia clay <br /> Agriculture, <br /> (1915-?1)_ Hanford sandy loam, <br /> Columbia very fine sandy loam, <br /> . Plate IV is a composite of maps <br /> loam, and hear Creek clay loam <br /> the general configuration of the <br /> from that publication showing from <br /> Vdr1.Pu5 soil types. These soils thsydhaveedundeveloped tprofiies, <br /> lain sediments? profiles, <br /> fans or flood P underlain by unc❑lidated material- ❑f the <br /> and are generally Dared upon the drillers log <br /> indices vary from 54 to 85. the soil depth is about 6 <br /> water well located on the property, cobbles, <br /> feet, and is underlain by alternating beds Of sandiies within <br /> and clays. Most of the property <br /> Rilie whose <br /> cemented gravels, watercourse of the Mokelumne <br /> the meandering Comanche Dam. <br /> discharge is now controlled by <br /> TO GROUNDWATER: Based on static water level measurements <br /> eewater <br /> DEPTH property, <br /> taken from the water well located on April 1976pto 99.5' BGL in <br /> table has dropped from 90-3' DisBGL in Ap also show <br /> November, 7988. County Flood Control riingfi1983 maps (Plate V,) <br /> yearly fluctuations in the area; enact surveyed elevations of <br /> indicates a depth of about 85'BGL; but visual inspection <br /> the Wall or excavations are not available, <br /> ❑f the property indicates that the water level measurements agree <br /> in elevations. <br /> quite well when adjusted for differences <br /> wells <br /> s 0 <br /> LOCATION OF WELLS: 1'i ate VI shgroundwaterthe aby❑nthe fCounty r Flood <br /> used for measuring depths to 9 there are no water <br /> Control District. According to this map, well on the <br /> --_---wells within one (1) mile of this site. The water operations <br /> property was drxlled_rn- <br /> and_i s__used_f or Plant <br />