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ARCHIVED REPORTS XR0011668
EnvironmentalHealth
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EHD Program Facility Records by Street Name
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EL DORADO
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2900 - Site Mitigation Program
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PR0009146
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ARCHIVED REPORTS XR0011668
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Entry Properties
Last modified
7/11/2019 1:16:59 PM
Creation date
7/11/2019 11:26:37 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2900 - Site Mitigation Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0011668
RECORD_ID
PR0009146
PE
2960
FACILITY_ID
FA0004093
FACILITY_NAME
LIGHTHOUSE SCHOOL
STREET_NUMBER
222
Direction
N
STREET_NAME
EL DORADO
STREET_TYPE
ST
City
STOCKTON
Zip
95202
APN
13910022
CURRENT_STATUS
02
SITE_LOCATION
222 N EL DORADO ST
P_LOCATION
01
QC Status
Approved
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EHD - Public
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Clayton <br /> f1.l R4 i;,�1E`�4: <br /> r rl\Sl lT 1�'t <br /> 2.0 <br /> A site location and topographic map is provided in Figure 1. Figure 2 is a schematic <br /> of the site and its immediate surroundings. <br /> The subject site is located at the northeastern corner of the intersection of Channel <br /> and El Dorado streets in Stockton, California. The building onsite has a basement <br /> and two floors. The subject site measures approximately 16,000 square feet. <br /> Presently, there is a Pacific Bell Telephone office in the basement, staffed by one <br /> maintenance employee. Otherwise the building is unoccupied. File boxes and <br /> telephone equipment were observed at different locations throughout the building. <br /> 2.1 REGIONAL HYDROGEOLOGIC SETTING <br /> According to a water contour map plotted during spring 1990 and data obtained from— <br /> nearby monitoring wells, the depth to groundwater at the subject site is estimated to <br /> be approximately 35 feet. <br /> The groundwater gradient, based on the 1990 water contour map, is toward the east. <br /> Data obtained from the installation of three monitoring wells at an adjacent site, 141 <br /> North El Dorado Street, confirmed the easterly groundwater flow direction. <br /> Since no data from groundwater or monitoring wells were found at the subject site, <br /> Clayton was unable to obtain information on the depth to groundwater or the <br /> groundwater flow direction directly beneath the site. Groundwater levels often <br /> fluctuate seasonally or as the result of local landscape irrigation. The local flow <br /> direction beneath the site may be naturally influenced by zones of higher permeability <br /> such as buried stream channels, or artificially influenced by nearby well pumping or <br /> recharge. <br /> According to our investigation, the Stockton Deep Water Channel extends <br /> underground to the south of the subject site (Figure 2). Review of a 1968 <br /> topographic map did not show any indication that this channel extends under the <br /> subject site. <br /> 2.2 HISTORY OF LAND USE <br /> Clayton researched the history of the site by reviewing aerial photos and records <br /> available from the assessor's office, records office, and building and planning <br /> department. The following aerial photos were reviewed: <br /> Photo M Number j <br /> 06077-183-111 January 1983 <br /> Unknown 1952 - <br /> Uaknown 1937 <br /> -2- <br /> 33420-arep <br />
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