Laserfiche WebLink
Subsurface Investigation Report <br /> HUGHES PROPERTY <br /> 322 and 400 North Sacramento Street, Lodi, California <br /> 1.0. INTRODUCTION <br /> At the request of Mr. James V. DeMera of Mullen, Sullivan & Newton, Advanced <br /> GeoEnvironmental, Inc. (AGE) has prepared the enclosed Subsurface Investigation Report for <br /> 322 and 400 North Sacramento Street, Lodi, California (site). The work was performed as part of <br /> a pending property transfer. The scope of work included the advancement of six soil borings, <br /> collection and analysis of soil samples, and preparation of this report. The location of the site is <br /> — illustrated on Figure 1. A plan of the site is illustrated on Figure 2. <br /> This report has been prepared in accordance with guidelines issued by the Central Valley Regional <br /> Water Quality Control Board(CVRWQCB)for the subsurface investigation of underground storage <br /> tank(UST) sites. <br /> 2.0. BACKGROUND <br /> The subject property,located at 322 and 400 North Sacramento Street in the city of Lodi, California, <br /> is situated in an area of mixed commercial and light industrial use. The property (400 North <br /> Sacramento Street) was formerly occupied by Hughes Spray Chemical and Brea Agricultural <br /> Services from the 1920s until the early 1980s. The southern parcel (322 North Sacramento Street) <br /> was reportedly utilized as an automotive towing and wrecking yard for a number of years. Both <br /> properties are presently undeveloped. <br /> 2.1. REGIONAL GEOLOGIC/HYDROGEOLOGIC SETTING <br /> The property is situated within the Great Valley Geomorphic Province of California, a large, <br /> elongate, northwest trending, asymmetric structural trough. The Great Valley Province has been <br /> filled with thick sequences of sediment ranging in age from Jurassic to Recent,creating a nearly flat <br /> — lying alluvial plain that extends from the Tehachapi Mountains in the south to the Klamath <br /> Mountains in the north.The western and eastern boundaries of this province are the California Coast <br /> Range and the Sierra Nevada,respectively.Rocks composing the basement complex of the province <br /> have not been completely defined but are believed to be of metamorphic and igneous origins. The <br /> northern and southern portions of the Great Valley Province have been designated the Sacramento <br /> and San Joaquin Valleys, respectively. <br /> The Modesto, Riverbank, and Turlock Lake Formations and overlying Recent alluvium are the <br /> principal source of domestic ground water in the 13,500-square-mile San Joaquin Valley Ground <br /> Water Basin (Basin 5-22). This basin is drained primarily by the San Joaquin River. The nearest <br /> surface water feature in the vicinity of the property is the Mokelumne River,approximately 1/2-mile <br /> Advanced GeoEvironmental,Inc. <br />