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SU0006529 SSCRPT
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SU0006529 SSCRPT
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Last modified
5/7/2020 11:32:29 AM
Creation date
9/5/2019 10:46:16 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
FileName_PostFix
SSCRPT
RECORD_ID
SU0006529
PE
2611
FACILITY_NAME
PA-0700093
STREET_NUMBER
19530
Direction
W
STREET_NAME
GRANT LINE
STREET_TYPE
RD
City
TRACY
APN
20907023
ENTERED_DATE
4/18/2007 12:00:00 AM
SITE_LOCATION
19530 W GRANT LINE RD
RECEIVED_DATE
4/18/2007 12:00:00 AM
P_LOCATION
99
P_DISTRICT
005
QC Status
Approved
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SJGOV\rtan
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FilePath
\MIGRATIONS\G\GRANT LINE\19530\PA-0700093\SU0006529\SSC RPT.PDF
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EHD - Public
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Buck&Mendoza Property July 20,2005 <br /> Phase I Environmental Assessment <br /> Page:6 <br /> 3.1 Site Location <br /> Maps have been provided in order to give a picture of the location of the subject property. <br /> Maps included are a vicinity map (Figure 1), a parcel map and site maps (Appendix A), <br /> and a record search index map (Appendix E). <br /> 3.2 Description of the Area <br /> The subject property is located in a rural area northwest of Tracy known as Mountain near <br /> Altamont Pass and the San Joaquin and Alameda County Lines. It is surrounded by <br /> pasture and farm lane along with some residences or small ranches. A natural gas and oil <br /> pipeline run diagonally across the Mendoza parcel. <br /> 3.3 Geology & Hydrology <br /> i <br /> The Central San Joaquin Valley is floored by unconsolidated quaternary sediments to <br /> depths of 400 feet or more. All of these units can be considered soils in the engineering <br /> sense, as they are unconsolidated. <br /> The sediments of the Central Valley were deposited as a series of coalescing alluvial fans. <br /> The fans originated where valleys of-major streams that drained the Sierras, emptied into <br /> the broad expanses of the Central Valley. The coarser sediments, which comprise the <br /> fans, are mainly arkosic in composition. They were derived from erosion associated with <br /> glacial stages in the mountains. The finer grained sediments are predominantly composed <br /> of rock flour washed out of the former extensive glaciers in the Sierras (Arkley, 1964). <br /> E <br /> There are layers of clay and layers of hardpan throughout the Mountain House area. These <br /> layers are not considered discontinuous, and communication between "perched" water, <br /> shallow aquifers and deeper aquifers are believed to occur in the Central Valley. <br /> Groundwater, in this area, ranges from 10 to 60 feet from the surface with the gradient in <br /> the north/northeast direction. <br /> 3.4 Asbestos and Lead Based Paints <br /> An inspection was made of the properties for asbestos and lead based paint related health <br /> hazards. Building materials that contain asbestos in a friable condition can pose a health <br /> hazard. Friable asbestos sources were not observed and analytical samples were not taken. <br /> However, if the structures were to be demolished, potential asbestos containing building <br /> materials such as the flooring tiles and roofing material used in construction of the house <br /> would have to be tested for asbestos, and possibly removed by a licensed asbestos <br /> removal contractor. Some sheet rock wall materials naturally contain asbestos and would <br /> also have to be considered during a demolition. <br /> I <br />
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