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SU0002195 SSNL
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SU0002195 SSNL
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Entry Properties
Last modified
5/7/2020 11:29:05 AM
Creation date
9/4/2019 10:35:15 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
FileName_PostFix
SSNL
RECORD_ID
SU0002195
PE
2626
FACILITY_NAME
UP-00-01
STREET_NUMBER
12505
Direction
E
STREET_NAME
BRANDT
STREET_TYPE
RD
City
LOCKEFORD
APN
05132010
ENTERED_DATE
10/23/2001 12:00:00 AM
SITE_LOCATION
12505 E BRANDT RD
QC Status
Approved
Scanner
SJGOV\rtan
Supplemental fields
FilePath
\MIGRATIONS\B\BRANDT\12505\UP-00-01\SU0002195\SS STDY.PDF
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EHD - Public
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April 13,_2000 <br /> Job Number: LG00-114, <br /> Pager if <br /> Table: Suminaa' of Available.Graund.Water Information <br />'-* Date,Source Groundwater Depth Notes . <br /> April.5' 2000,Three(3)Jsoil borings, Not encountered Moisture found in B-tat 10.5 ft, no . <br /> Neil O..,Anderson&Associates,Inc. moisture in B-2 and B-3.See plates <br /> 8, 9,"and 10. <br /> Spring.1998, San Joaquin County Flood.` About 110 to 120 feet Gradient about 12.5 feet/mile,Lt Control and Water Conservation District in depth. flov4ing southeast. <br /> map, J F <br /> Fall 1998, San Joaquin,County Flood Control" About 100 to 110 feet. Gradient about 25 feet/mile, <br /> and Water Conservation District. i .= in depth. flovvin southeast . <br /> Note: ND-Non-Detectable(or not found.at"detectable limits) ' <br /> The ground water-is fairly deep ih the Lockeford"area and was found to be approximately <br /> 100 to.120 feet for 1998. The flow direction is toward the southwest mith the highest,gradient 1 <br /> occurring in the-Summer-Fall period of about 25 feet per mile. No waterwells are known to exist <br /> on tke subject'property. A new water well ai d-storage,iank are planned to be set in the northwest <br /> `; 3 corner of the property. <br /> VI, GEOLOGY,'SOILS,AND PERCOLATION TEST <br /> � f <br /> l Tliesurficial sediment of the site and surrounding area is reported to be the lower merriber, <br /> of'the Pleistocene age}(about I1,000:to 2 million years ago)Riverbank Formation that.consists of r <br /> 'was <br /> alluvium farming-Molelumne River terraces and alluvial fans. The Riverbank Formation <br /> was mapped in'the"�ekeford area by Marchand and Bartow"+z in 1979,(Plate 6). The upper and <br /> ji <br /> middle units contain material that is chiefly composed of sand derived from glacial outwash. The <br /> upper and middle units of the Riverbank Formation observed on the site during shallow drilling. ' j <br /> appear to contain.more fine grained materials rather than sand as suggested by the ge'ologic'map. <br /> The surface and near surface soils located at the proposed project location are reported to <br /> be the San Joaquin loam(Plate 7). .The San Joaquin loam is described by the Soil Survey report <br /> as"moderately deep to a hard pan and moderately well drained. Typically,the surface.layer is.a <br /> Y. pinkish gray loath abdut 12 inches thick.,' The upper,14 inches of the subsoil is brown sandy clay <br />*- Marchand,D.E. and Bartow,J.A., 1979,Preliminary'geologic'map of the Bellota Quadrangle,' ' <br /> California. USGS Open Fh ile,Report 79-664. . <br /> 7 <br /> ' <br />
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