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2900 - Site Mitigation Program
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PR0522629
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Last modified
2/15/2019 10:54:59 AM
Creation date
2/15/2019 10:19:41 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2900 - Site Mitigation Program
File Section
WORK PLANS
RECORD_ID
PR0522629
PE
2950
FACILITY_ID
FA0015420
FACILITY_NAME
CALIFORNIA STREET MEDICAL BLDG
STREET_NUMBER
1617
Direction
N
STREET_NAME
CALIFORNIA
STREET_TYPE
ST
City
STOCKTON
Zip
95204
APN
12715050
CURRENT_STATUS
02
SITE_LOCATION
1617 N CALIFORNIA ST
P_LOCATION
01
P_DISTRICT
002
QC Status
Approved
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EHD - Public
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11 August 2004 - <br /> AGE-NC Project No. 04=1180 <br /> Page 2 of 8 <br /> concentrations of contaminants detected in sample P1-W did not justify placement of the site into <br /> the Local Oversight Program (LOP): _ <br /> 2.2. REGIONAL GEOLOGIC/HYDROGEOLOGIC SETTING <br /> The site is situated within the southern portion of the Great Valley Geomorphic Province of <br /> California, a large, elongate, northwest trending, asymmetric structural trough; the northern and <br /> southern portions of the Province have been designated the Sacramento and San Joaquin Valleys, <br /> respectively. The Province is bordered by the Coast Ranges to the west,the Klamath Mountains and <br /> Cascade Range to the north, and the Sierra Nevada'to the east. <br /> The Great Valley has been filled with sediments derived from Both marine and continental sources. <br /> Thickness of the sedimentary fill ranges from thin veneers along the valley edges to more than <br /> 20,000 feet in the south central portion of the valley. The sedimentary formations range in age from <br /> Jurassic to Recent,with the older deposits being primarily marine in origin and the younger deposits <br /> being primarily continental. Continental-derived sediments were primarily deposited in lacustrine, <br /> fluvial,and alluvial environments with sediment sources being the mountain ranges surrounding the <br /> valley(Olmsted and Davis, 1961);the site itself is located on unconsolidated and semi-consolidated <br /> alluvium, lake, playa and terrace deposits of Quaternary age (California Division of Mines and <br /> Geology, 1977).Rocks composing the basement complex of the Province have not been completely <br /> defined but are believed to be metamorphic and igneous in origin. <br /> The Modesto, Riverbank and Turlock Lake Formations and overlying Recent alluvium are the <br /> principal sources of domestic ground water in the 13,500-square mile San Joaquin Valley Ground <br /> Water Basin(Basin 5-22). The estimated depth to ground water at the site is approximately 30 to 40 <br /> feet below surface grade based on information from surrounding sites monitored by AGE.However, <br /> this may be greatly modified by local recharge and discharge patterns. <br /> 3.0. SCOPE OF WORK <br /> At the request of the entities involved in the property transfer of the site,AGE proposes to drill and <br /> install one ground water monitoring well approximately 30-feet northeast(inferred down-gradient <br /> direction)of boring P 1 (June 2004). The monitoring well installation and sampling will include the <br /> following tasks: <br /> • Permitting and pre-field work activities; <br /> • Drilling and completion of the monitoring well; <br /> Advanced GeoEnvironmental,Inc. <br />
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