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SU0003960 SSCRPT
Environmental Health - Public
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SU0003960 SSCRPT
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Entry Properties
Last modified
5/7/2020 11:30:25 AM
Creation date
9/5/2019 10:41:02 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
FileName_PostFix
SSCRPT
RECORD_ID
SU0003960
PE
2622
FACILITY_NAME
PA-0200045
STREET_NUMBER
147
Direction
N
STREET_NAME
GERTRUDE
STREET_TYPE
AVE
City
STOCKTON
ENTERED_DATE
5/11/2004 12:00:00 AM
SITE_LOCATION
147 N GERTRUDE AVE
RECEIVED_DATE
2/12/2002 12:00:00 AM
QC Status
Approved
Scanner
SJGOV\rtan
Supplemental fields
FilePath
\MIGRATIONS\G\GERTRUDE\147\PA-0200045\SU0003960\SSC RPT.PDF
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EHD - Public
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GEOCHECK® - PHYSICAL SETTING SOURCE SUMMARY <br /> r Slte-Speclgc Hydrogeolog/cat Data•: <br /> Search Radius: 2.0 miles <br /> Location Relative to TP: 1 -2 Miles NW <br /> Site Name: Brea Agricultural Svcs#2 <br /> Site EPA ID Number: CAD068847870 <br /> Groundwater Flow Direction: SW ON SITE AND NNW ON A REGIONAL BASIS. <br /> Measured Depth to Water: 71 feet. <br /> Hydraulic Connection: A clay layer separates the surticial aquifer and the underlying <br /> confined lower aquifer. <br /> .. Sole Source Aquifer: No information about a sole source aquifer is available <br /> Data Quality: Information based on site-specific subsurface investigations is <br /> documented in the CERCLIS investigation report(s) <br /> AOUIFLOW® <br /> Search Radius:2.000 Miles. <br /> EDR has developed the AQUIFLOW Information System to provide data on the general direction of groundwater <br /> flow at specific points. EDR has reviewed reports submitted by environmental professionals to regulatory <br /> authorities at select sites and has extracted the date of the report,groundwater flow direction as determined <br /> hydrogeologically,and the depth to water table. <br /> r, <br /> LOCATION GENERAL DIRECTION <br /> MAP ID FROM TP GROUNDWATER FLOW <br /> Not Reported <br /> r <br /> GROUNDWATER FLOW VELOCITY INFORMATION <br /> Groundwater flow velocity information for a particular site is best determined by a qualified environmental professional <br /> using site specific geologic and soil strata data.If such data are not reasonably ascertainable,it may be necessary <br /> to rely on other sources of information,including geologic age identification,rock stratigraphic unit and soil <br /> characteristics data collected on nearby properties and regional soil information. In general,contaminant plumes <br /> move more quickly through sandy-gravelly types of soils than silty-clayey types of soils. <br /> GEOLOGIC INFORMATION IN GENERAL AREA OF TARGET PROPERTY <br /> Geologic information can be used by the environmental professional in forming an opinion about the relative speed <br /> at which contaminant migration may be occurring. <br /> r ROCK STRATIGRAPHIC UNIT GEOLOGIC AGE IDENTIFICATION <br /> Era: Cenozoic Category: Stratifed Sequence <br /> System: Quaternary <br /> Series: Quaternary <br /> Code: Q (decoded above as Era,System&Senes) <br /> Geologic Age and Rock Stratigraphic Unit Source: P.G.Schruben, R.E.Arndt and W.J. Bawiec,Geology <br /> of the Conterminous U.S.at 1:2,500,000 Scale-a digital representation of the 1974 P.B.King and H.M.Beikman <br /> Map, USGS Digital Data Series DDS- 11 (1994). <br /> DOMINANT SOIL COMPOSITION IN GENERAL AREA OF TARGET PROPERTY <br /> r The U.S.Department of Agriculture's(USDA)Soil Conservation Service(SCS)leads the National Cooperative Soil <br /> Survey(NCSS)and is responsible for collecting,storing, maintaining and distributing soil survey information <br /> for privately owned lands in the United States.A soil map in a soil survey is a representation of soil patterns <br /> in a landscape.Soil maps for STATSGO are compiled by generalizing more detailed(SSURGO)soil survey maps. <br /> The following information is based on Soil Conservation Service STATSGO data. <br /> Ca�reEsa&Wk mMmmmlelflagpnu CmmpaLrbW eM LledlYy lnb,ma�tb SSWN (CERCLIS, Mw IpareM AIId IM lnb,malM aM opinbn¢pnMmBOere pvae d,M OIM EPA,epo,l�al.eTld�wa�e mmpleleE Wer <br /> a TC0733735.4r Page A-3 <br /> V <br />
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