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SU0003904 SSNL
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SU0003904 SSNL
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Entry Properties
Last modified
5/7/2020 11:30:17 AM
Creation date
9/6/2019 10:53:19 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
FileName_PostFix
SSNL
RECORD_ID
SU0003904
PE
2622
FACILITY_NAME
PA-0300009
STREET_NUMBER
20499
Direction
E
STREET_NAME
LIBERTY
STREET_TYPE
RD
City
CLEMENTS
APN
00919001
ENTERED_DATE
5/11/2004 12:00:00 AM
SITE_LOCATION
20499 E LIBERTY RD
RECEIVED_DATE
1/21/2003 12:00:00 AM
P_LOCATION
99
P_DISTRICT
004
QC Status
Approved
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\MIGRATIONS\L\LIBERTY\20499\PA-0300009\SU0003904\SS STDY.PDF
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EHD - Public
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April 29, 2003 <br /> Job Number. LG03-103 <br /> Page 4 <br /> There are no wells on the subject property;therefore, no water quality samples were <br /> taken. <br /> VL GEOLOGY, SOILS, AND PERCOLATION TEST <br /> The surficial geology of the site is separated into many areas comprised of three types of <br /> geologic formations. The Mehrten Formation is the oldest on the subject property. It is described <br /> as andesitic conglomerate, sandstone, mudstone and lahars. The Mehrten Formation formed in <br /> the Miocene and Pliocene epochs of which the Miocene(oldest)began 24 million years ago. <br /> The Laguna Formation is the second oldest formation on the subject property. It is <br /> described as arkosic gravel, sand and silt with some inter-bedded volcanic detritus derived from <br /> the Mehrten Formation; moderately consolidated in contrast with weaker consolidation of <br /> younger deposits below the soil zone (Redding and Corning soils, deep variant). The Laguna <br /> Formation formed during the Pliocene epoch,which began approximately five million years ago. <br /> The Modesto Formation- Foothill is the most recently deposited formation found on the <br /> subject property. It is described as derived alluvial silt, clay and minor sand forming terraces, <br /> upper fans and following distributaries across lower fans; abundant volcanic detritus (Honcut, <br /> Wyman, Capay soils). The Modesto Formation-Foothill was formed during the Pleistocene <br /> epoch which began 1.6 million years ago.' The Riverbank in the San Joaquin Valley is <br /> predominantly arkosic alluvium while the Sacramento Valley contains more mafic igneous rock <br /> fragments' (Plate 6). Essentially, these formations are consolidated older alluvium. <br /> The surface and near surface soils located on the site are reported to be the Corning- <br /> Redding complex, Kaseberg loamy sand,Kaseberg fine sandy loam, Pardee cobbly loam, Redding <br /> ` gravelly complex and the Yellowlark gravelly loam(Plate 7).° Table 3 presents an excerpt of <br /> some selected engineering properties for soils located on the subject property. <br /> 'Marchand,D.E. and Bartow,J.A-, 1979. Preliminary Geologic Map Of Cenozoic Deposits Of The <br /> Bellotti Quadrangle, California;U.S. Geologic Survey Open File Report 79.664, scale 1:62,500. <br /> 3 Helley,E.J.,and Harwood,D.S., 1985. Geologic map of the Cenozoic Deposits of the Sacramento <br /> tr Valley and Sierran Foothills,California;U.S. Geologic Survey Miscellaneous Field Studies Map,MF-1790,scale <br /> 1:62,500. <br /> t. ° USDA Soil Conservation Service, 1992, Soil Survey of San Joaquin County,California, Sheet 7. <br /> 6. <br /> pFFS 4 <br /> 6. <br /> O <br />
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