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SU0009663 SSCRPT
Environmental Health - Public
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SU0009663 SSCRPT
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Entry Properties
Last modified
5/7/2020 11:34:08 AM
Creation date
9/6/2019 10:56:12 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
FileName_PostFix
SSCRPT
RECORD_ID
SU0009663
PE
2622
FACILITY_NAME
PA-1300090
STREET_NUMBER
260
Direction
E
STREET_NAME
LINNE
STREET_TYPE
RD
City
TRACY
Zip
95304-
ENTERED_DATE
6/12/2013 12:00:00 AM
SITE_LOCATION
260 E LINNE RD
RECEIVED_DATE
6/12/2013 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\L\LINNE\260\PA-1300090\SU0009663\SSCR.PDF
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EHD - Public
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Surface&Subsurface Contamination Report Page 10 <br /> 700 W.Linne Rd.,Tracy <br /> Project No. 662,1 <br /> February 11,2013 <br /> grade and flows in a northeasterly direction. Groundwater monitoring data from a remedial <br /> investigation at 3780 W. Linne Road, about 1 mile west of the Property, suggest that locally, <br /> groundwater lies at about 12 feet below grade and flows in a north easterly direction. <br /> The nearest open body of water is the San Joaquin River, about 1 mile to the east. An <br /> ephemeral stream lies near the southeast boundary of the Property and is included in the <br /> federal wetlands inventory. According to maps in the EDR report, the Property does not lie <br /> within a 100-year flood zone. <br /> In much of the Central Valley, the shallow groundwater contains marginally potable water, <br /> and generally the only water production wells completed opposite this zone are domestic <br /> wells. The shallow aquifer is composed of shallow sand, and silt alluvium deposited on the <br /> valley floor. Hotchkiss & Balding, in their 1971 US Geological Survey report, Geology. <br /> Hydroloey, and Water Quality of the Tracy-Dos Palos Area San Joaquin Valley. California, <br /> (Open File Report 72-169) described the aquifers and their characteristics for the Tracy-Dos <br /> Palos area. In the Vernalis-New Jerusalem area, the recent alluvium is generally less than <br /> 100 feet thick and directly overlies the Tulare Formation, a Plio-Pleistocene age, mixed <br /> clastic sequence of clay, silt, sand and gravel. There is little to distinguish the contact <br /> between the base of the alluvium from the top of the Tulare Formation <br /> Petroleum Production <br /> Based on oil and gas production maps produced by the California Division of Oil, Gas and <br /> Geothermal Resources, the lies within the confines of the northern part of the Vernalis Gas <br /> Field. Three wells have been drilled on the Property. One well, Paulson 32-9 was <br /> abandoned as a dry hole and never was completed as a gas producer, while Paulson 14-9 and <br /> Vintage TLW 26-1 were completed as gas producing wells. The Vernalis field produces <br /> natural gas from a depth of about 4,000 to 5,000 feet from the Cretaceous age Panoche <br /> Formation. <br /> Federal Wetlands <br /> Based on information on the map in the EDR report (Appendix D) the Propedoes not , <br /> ft' <br /> include lands recognized in the federal wetlands inventory, although lands ng the/ <br /> wet a <br /> ephemeral stream near the southeast property line are included in the federal nds ' <br /> inventory. <br /> Radon <br /> Soil testing by EPA and CaliO Department of Toxic Substance Control show that <br /> naturally occurring radon does not pos a human health risk in the Central Valley. <br /> 2937 Veneman Ave.,#13240 Geo-Phase Environmental Inc. Phone: (209)569-0293 <br /> Modesto,CA 95366 Fax: (209)569-0295 <br />
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