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SU0004094
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SU0004094
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Last modified
10/27/2020 1:02:10 PM
Creation date
9/6/2019 10:43:21 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
RECORD_ID
SU0004094
FACILITY_NAME
QX-01-0002
STREET_NUMBER
36736
Direction
S
STREET_NAME
KOSTER
STREET_TYPE
RD
City
TRACY
ENTERED_DATE
5/12/2004 12:00:00 AM
SITE_LOCATION
36736 S KOSTER RD
RECEIVED_DATE
1/8/2002 12:00:00 AM
QC Status
Approved
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SJGOV\wng
Supplemental fields
FilePath
\MIGRATIONS\K\KOSTER\36736\QX-01-02_PA-0200065\SU0004094\EIR 2004.PDF
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EHD - Public
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5. ALTERNATIVP.S <br /> 5.4 ALTERNATIVES CONSIDERED BUT REJECTED AS _ <br /> INFEASIBLE <br /> An off-site alternative in the Laguna Formation of the foothills was considered for inclusion in <br /> this EIR in order to eliminate the significant and unavoidable impact to farmland by finding a site <br /> located outside of the Central Valley that would not include prime farm land, farm land of <br /> statewide importance, and Williamson Act Contract land. <br /> This off-site alternative was rejected because of the lack of an adequate aggregate resource to <br /> meet the sponsor's basic objectives. Many resource sectors in the Laguna Formation of the <br /> foothills were not controlled by an aggregate company or encroached upon by competing land use <br /> as of 19881 (CGS, 1988). However, since 1988 many of these sectors have been developed as a <br /> result of growth in the Bay area,thus making any underlying resource unavailable for mining <br /> and/or extraction. Some new developments in the area include New Jerusalem and the Diablo <br /> Valley(Don Depraw,CGS). <br /> The Laguna Formation is one of several alluvial rock units found directly west of the Sierra <br /> Foothills. Sediments of the Laguna Formation are derived from weathering and erosion of <br /> resistant bedrock units in the Foothills. The Laguna Formation is an unsuitable material for PCC- <br /> grade aggregate due to several constraints,described below. First, since the Laguna Formation is <br /> Pliocene in age,it is significantly older than most material in the area which meets aggregate _ <br /> standards. Due to its age, significant weathering rinds,or fine-grained brittle outer casings, are <br /> present on gravel clasts. During mining, the brittle casing commonly becomes dislodged from the <br /> gravel, adding unwanted fine-grained material to the aggregate mixture. The formation itself is <br /> not easily crushable,but largely cemented,making extraction and processing difficult. Second, <br /> since the Laguna Formation is derived from the Sierra Nevada, volcanic clasts present in its <br /> matrix cause mining and processing difficulties. Third,due to significant clay content in the <br /> Laguna Formation,it costs more to process. Deflocculants,or chemicals used to remove clay and <br /> make a material more fluid,have to be used just to remove the clay. Many cycles of processing <br /> are often needed. There is no known instance of in which the Laguna Formation is used as an — <br /> aggregate material in the Sacramento/San Joaquin County area. The Laguna Formation is used <br /> primarily as a gravel subbase material (building foundations,etc.),but even then presents <br /> processing difficulties due to its clay content. No reports or studies have been published on the <br /> Laguna Formation(Don Depraw,CGS). <br /> 1 CGS Special Report 160,Mineral Land Classification:Portland Cement Concrete Aggregate in the Stockton-Lodi <br /> P-C Region(San Joaquin County,California)is the most recent report which assesses the resource sectors in the <br /> proposed project area. It was published in 1988. _ <br /> RMC Pacific Venmhs Qnany Musing and Re Ih fton Project 5-20 ESA/203015 <br /> Administrative Draft Em March 2004 <br />
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