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SU0004149
Environmental Health - Public
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SU0004149
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Last modified
10/27/2020 1:00:10 PM
Creation date
9/6/2019 10:44:51 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
RECORD_ID
SU0004149
FACILITY_NAME
QX-96-0001
STREET_NUMBER
36869
Direction
S
STREET_NAME
KOSTER
STREET_TYPE
RD
City
TRACY
ENTERED_DATE
5/12/2004 12:00:00 AM
SITE_LOCATION
36869 S KOSTER RD
RECEIVED_DATE
9/22/1996 12:00:00 AM
QC Status
Approved
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\MIGRATIONS\K\KOSTER\36869\QX-96-01_EIR 96-3\SU0004149\PUB REC REL APPL.PDF
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EHD - Public
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excavations which include the existing permitted Quarry Excavation permit for Teichert <br /> Aggregates (QX-91-5), and the existing and proposed expansion for a Quarry Excavation <br /> permit for Brown Sand (QX-94-1). The project site is also within the "Buffer Area" of the <br /> San Joaquin Kit Fox Habitat Conservation Plan (HCP). <br /> Geological Setting x t <br /> FThe project site and the surrounding area is underlain by an Alluvial Fan Deposit from the <br /> Holocene Age formed by Hospital Creek. The deposit is more than 150 feet in depth <br /> consisting of silty gravel interlaced with silty clay areas up to twenty feet in depth. <br /> Overburden consists of silty clay to an average depth of four feet. <br /> The Hospital Creek drainage is located in the Diablo Range southwest of Tracy, California. s� <br /> Flow in this drainage is confined to the winter and spring months and is historically dry <br /> during the summer and fall. The drainage has a steep hydraulic gradient and extends from <br /> the easterly slopes of Mt. Oso. <br /> The Alluvial Fan Deposit consists of sedimentary, metavolcanic, and ultramafic rocks with <br /> sand and clay matrix. The portions of the fan on this project have been sampled to a depth <br /> of 125 feet and were consistent with other borings in the area. Maximum size of the gravel <br /> was less than 18 inches. According to the proponent, the fine matrix of the deposit <br /> provides a dense and stable foundation for excavation slopes. <br /> The proposed project would extract the gravel from the fan deposit to a depth of <br /> approximately 125 feet. Bottom of the excavation would be 10 feet above the existing <br /> water table. Soil from striping and clay pockets found during excavation would be <br /> stockpiled for future use in the reclamation of the project. At the conclusion of the <br /> excavation, five feet of top soil and fines from the proposed settlement basins would be <br /> placed on the pit floor to bring it up to a finished elevation of 120 feet. <br /> There is no evidence of soluble heavy metals or other materials of a chemical nature that <br /> would contaminate surface runoff or groundwater. All wash water would be contained on <br /> the project site for recycling use. <br /> Hydrology <br /> The groundwater table depicted on the drill log of a well drilled on the west side of the <br /> property in 1991 showed the water table at a depth of approximately 135 feet. Quarry <br /> excavation would extend to 125 feet, which is ten feet above groundwater. No excavation <br /> would be done below the water table. <br /> The natural slope of the project site is to the northeast in the direction of the proposed <br /> aggregate processing plant location. Surface water drainage would be confined to the <br /> project site with no runoff to adjacent property. All wash water used in aggregate <br /> production would be recycled and confined to settlement ponds on the project site. <br /> Surface or process water would not be discharged from the project site. Fresh water to <br /> Draft Environmental Impact Report 3-4 ER-96-3 <br />
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