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SU0004092
Environmental Health - Public
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EHD Program Facility Records by Street Name
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120 (STATE ROUTE 120)
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800
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2600 - Land Use Program
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QX-00-0001
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SU0004092
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Last modified
11/19/2024 4:01:42 PM
Creation date
9/8/2019 12:35:10 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
RECORD_ID
SU0004092
FACILITY_NAME
QX-00-0001
STREET_NUMBER
800
Direction
E
STREET_NAME
STATE ROUTE 120
City
LATHROP
ENTERED_DATE
5/12/2004 12:00:00 AM
SITE_LOCATION
800 E HWY 120
RECEIVED_DATE
1/29/2001 12:00:00 AM
QC Status
Approved
Scanner
SJGOV\wng
Supplemental fields
FilePath
\MIGRATIONS\O\HWY 120\800\QX-00-01 (PRE- APPLICATION)\SU0004092\CORRESPOND.PDF
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EHD - Public
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Any additional potential adverse impacts to Air Quality will be <br /> mitigated by Conditions of Approval in Landmark Lathrop Group ' s <br /> Authorities to Construct and Permits to Operate as imposed by the San <br /> Joaquin County Air Pollution Control District . Landmark Lathrop Group, <br /> LLC expects that operations will be regulated by permits issued . No <br /> adverse environmental changes or impacts will occur . <br /> 5 . 3 Surface and Groundwater Hydrology <br /> 5 . 3 . 1 Surface Water <br /> All storm water will be contained within the mine area . Storm water <br /> will be either diverted around disturbed areas or confined within the <br /> quarry pit . Electrically driven pumps will be utilized to move storm <br /> water from the open quarry to holding ponds used to settle out fines <br /> from the washing plant . Storm water will then be used in the washing <br /> of sands, clays and silts thereby reducing the amount of groundwater <br /> required to supplement process water <br /> 5 . 3 . 2 Groundwater <br /> Depth to shallow ground water beneath the property is 16 to 20 feet . <br /> Most wells in the area are drilled to a depth of 200-300 feet <br /> The entire area around the project site is a saturated formation of <br /> undifferentiated sand and clay . Groundwater migration is to the <br /> northwest and San Joaquin River . Recharge and discharge areas , <br /> horizontal/vertical inconsistencies in the types and location of <br /> subsurface clay layers, and proximity to active wells can influence this <br /> flow locally and regionally . <br /> Landmark Lathrop Group, LLC <br /> _ 2 - February 3, 2000 <br />
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