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SU0004819 SSCRPT
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SU0004819 SSCRPT
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Entry Properties
Last modified
5/7/2020 11:31:14 AM
Creation date
9/5/2019 10:44:05 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
FileName_PostFix
SSCRPT
RECORD_ID
SU0004819
PE
2622
FACILITY_NAME
PA-0500036
STREET_NUMBER
18353
Direction
W
STREET_NAME
GRANT LINE
STREET_TYPE
RD
City
TRACY
APN
20945014
ENTERED_DATE
2/9/2005 12:00:00 AM
SITE_LOCATION
18353 W GRANT LINE RD
RECEIVED_DATE
2/1/2005 12:00:00 AM
P_LOCATION
99
P_DISTRICT
005
QC Status
Approved
Scanner
SJGOV\rtan
Supplemental fields
FilePath
\MIGRATIONS\G\GRANT LINE\18353\PA-0500036\SU0004819\SSC RPT.PDF
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EHD - Public
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`/ <br /> TEIXEIRA-SOUZA PROPERTY Page 11 <br /> WKA No. 5475.03 <br /> L June 2, 2003 <br /> L <br /> subject property slopes northeasterly, therefore we estimate ground water flow direction as <br /> ,I <br /> northeasterly. <br /> Regional Geology <br /> The subject property is located in the central portion of the Great Valley geomorphic province of <br /> California. The Great Valley lies between the mountains and foothills of the Sierra Nevada <br /> Range to the east and the California Coast Ranges to the west. The geologic formations of the <br /> Great Valley are typified by thick sequences of alluvial (river) sediments deposited during the <br /> filling of a large ancient basin. <br /> The 1985 USGS Geologic Map of the Late Cenozoic Deposits of the Sacramento Valley and <br /> Northern Sierra Foothills, California, shows the subject property to be underlain by the Lower <br /> member of the Modesto Formation. The Lower member geologic unit is characterized by <br /> unconsolidated, slightly weathered gravel, sand, silt and clay. <br /> Soils <br /> Review of the 1998 U.S. Department of Agriculture, Soil Conservation Service(SCS) Soil <br /> Survey of San Joaquin County, California, indicates that the near-surface soils of the project area <br /> ` consist of four soil types. The predominant soils consist of"Stomar clay loam, 0 to 2 percent <br /> slopes." The other soil types are"Vernalis clay loam, 0 to 2 percent slopes", "Capay clay, 0 to 2 <br /> �. percent slopes" and"Stomar clay loam, wet, 0 to 2 percent slopes" <br /> ` The Stomar clay loam formed in alluvium derived from sedimentary rock sources. This soil is <br /> typically grayish brown clay approximately 19-inches thick. The subsoil, approximately 30- <br /> Linches thick, is a mixture of brown clay loam and clay that is underlain by yellowish brown clay <br /> loam at a depth of 60-inches. <br /> 6. The Vernalis clay loam formed in alluvium derived from mixed rock sources. The upper layer of <br /> the surface layer is typically brown clay loam approximately 9-inches thick. The lower portion <br /> of the surface layer is grayish brown and brown clay loam and pale brown loam approximately <br /> 38-inches thick. The subsoil, approximately 60-inches thick, is pale brown fine sandy loam. <br /> I <br /> INK <br /> L WALLACE-KUHL <br /> 6 ASSOCIATES INC. <br />
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