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2900 - Site Mitigation Program
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PR0522629
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Last modified
2/15/2019 11:32:53 AM
Creation date
2/15/2019 10:17:09 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2900 - Site Mitigation Program
File Section
FIELD DOCUMENTS
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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T <br /> 19 October 2004 <br /> AGE-NC Project No. 04-1180 <br /> Page 2 of 7 <br /> 2.3. REGIONAL GEOLOGIC/HYDROGEOLOGIC SETTING <br /> Lr <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 /> La <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 /> L� 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 /> 60 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 /> Ly 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. PROCEDURES <br /> The field work reported herein was performed in accordance with procedures outlined in the <br /> AGE-prepared Monitoring Well Installation Work Plan,dated 11 August 2004,and approved by the <br /> �- San Joaquin County'Environmental Health Department(SJCEHD).A boring permit and permit fee <br /> were submitted to the SJCEHD prior to implementation of field work.A copy of the approved permit <br /> is included in Appendix A. <br /> 3.1. MONITORING WELL INSTALLATION AND DEVELOPMENT <br /> One ground water monitoring well(MW-1)was installed on 19 August 2004 and developed on 23 <br /> August 2004. <br /> Lr Advanced GeoEnvironmental,Inc. <br /> Lir - <br />
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