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SR0066540 SSCRPT
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SR0066540 SSCRPT
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Entry Properties
Last modified
1/8/2020 9:56:05 AM
Creation date
9/4/2019 10:25:42 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
FileName_PostFix
SSCRPT
RECORD_ID
SR0066540
PE
2603
STREET_NUMBER
26290
Direction
S
STREET_NAME
BIRD
STREET_TYPE
RD
City
TRACY
Zip
95304
APN
23919032
ENTERED_DATE
2/7/2013 12:00:00 AM
SITE_LOCATION
26290 S BIRD RD
P_LOCATION
99
P_DISTRICT
005
QC Status
Approved
Scanner
SJGOV\sballwahn
Supplemental fields
FilePath
\MIGRATIONS\B\BIRD\26290 & 26500\(STAND ALONE) SUR SUB RPT\(STAND ALONE) SUR SUB RPT.PDF
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EHD - Public
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Surface&Subsurface Contamination Report Page 10 <br /> Sandhu Farms <br /> Project No. 655.1 <br /> August 15, 2012 <br /> 2.0 SITE DESCRIPTION <br /> 2.1 Property Location and Description <br /> The Property consists of two agricultural parcels and portions of two others that <br /> are contiguous, and have a total area of about 287 acres. The Property occupies <br /> almost all of the south half of Section 31 of T2S, R6E, MDB&M. It is situated on <br /> the east side of Bird Road and is bounded by Bird Road to the west and I-5 to the <br /> east. A private road forms the north boundary and an irrigation ditch is near <br /> the south boundary. The Property is operated as part of"Sandhu Farms". The <br /> served by septic sewage systems, and an offsite domestic water well, and a <br /> Banta Carbona Irrigation District's lined irrigation ditch provides irrigation <br /> water. Stormwater is drained internally. The area is shown on the United <br /> States Geological Survey topographic map, Vernalis California Quadrangle, <br /> California, 7.5-minute series. <br /> 2.2 Geologic and Hydrologic Conditions <br /> Soils& Geology <br /> The Central valley is notable for thick sedimentary deposits which range in age <br /> from recent to Eocene and older and which may extend to depths of more than <br /> 20,000 feet. These sediments are derived from the Sierra range to the east and <br /> the Coast Ranges to the west. <br /> The shallow sediments are known as the Tulare Formation. A widespread clay <br /> deposit, the Corcoran Clay (or E-clay), divides the upper and lower members of <br /> the Tulare Formation. The Tulare sediments lying above the Corcoran Clay are <br /> entirely Pleistocene in age. The Corcoran Clay is about 60 feet thick in the <br /> Vernalis-New Jerusalem area and it serves as an effective aquitard. It lies <br /> approximately 150 to 200 feet below the ground surface. It is believed that most <br /> major irrigation and water supply wells are completed below the Corcoran Clay <br /> zone. <br /> The USDA Soils Conservation Service Soil Survey of San Joaquin County, <br /> California. October 1992 soil survey report classifies soil in San Joaquin County. <br /> The Survey generally classifies the soils in this area of as part of the Columbia- <br /> Temple Association; deep, imperfectly drained soils of the Capay association; <br /> moderately well drained fine textured soils of the San Joaquin River flood plain. <br /> The specific on-site soil type is known as Capay clay, wet, 0-2% slopes. This is <br /> deep, moderately well drained brownish clay soil oveylying a silty clay loam. It <br /> is relatively impermeable. <br /> 2937 Veneman Ave.,#B240 Geo-Phase Environmental Inc. Phone: (209)569.0293 <br /> Modesto, CA 95356 Fax: (209)569.0295 <br />
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