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ARCHIVED REPORTS_XR0009069
EnvironmentalHealth
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EHD Program Facility Records by Street Name
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WASHINGTON
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2825
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3500 - Local Oversight Program
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PR0545822
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ARCHIVED REPORTS_XR0009069
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Last modified
7/15/2020 2:50:59 PM
Creation date
7/15/2020 1:28:35 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0009069
RECORD_ID
PR0545822
PE
3528
FACILITY_ID
FA0005566
FACILITY_NAME
RIVERSIDE CEMENT COMPANY
STREET_NUMBER
2825
Direction
W
STREET_NAME
WASHINGTON
STREET_TYPE
ST
City
STOCKTON
Zip
95203
CURRENT_STATUS
02
SITE_LOCATION
2825 W WASHINGTON ST
P_LOCATION
01
P_DISTRICT
001
QC Status
Approved
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LSauers
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EHD - Public
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AL CONTACT PERSON: <br /> Steve Yocam, (209) 948-0520 <br /> LEGAL DESCRIPTION: <br /> The property consists of approximately five (5) acres located in <br /> Section 8, T 1N, R-BE. , M.D. B.& M. , San Joaquin County, CA. <br /> REGIONAL GEOGRAPHIC _LOCATION: <br /> As mentioned above, the property is located within the Port of <br /> Stockton complex, just east of the U. S. Naval Communication <br /> facility located on Rough & Ready Island, a short distance to the <br /> west of the Port Administration Buildings. It is accessed from <br /> W. Washington Blvd. , which can be reached from Interstate 5 via <br /> the Fresno Ave. exit. <br /> The surrounding area is zoned for industrial & manufacturing; <br /> Tri-Delta Fertilizer company is to the north, a railroad spur on <br /> the east, and undeveloped vacant land on the west. There are no <br /> • residences within 1/2 mile of the site. PLATE I shows the <br /> location of the property in relation to nearby features. <br /> GEOLOGIC & GEOMORPHIC SETTING:. <br /> The property is located in the southern portion of the Sacramento <br /> Valley, at the eastern end of what is referred to as the San <br /> Joaquin Delta. This is a large area of sloughs, islands, and <br /> channels that were formed by the meanderings of the Mokelumne, <br /> San Joaquin & Calaveras rivers. The Burns Cutoff is a short <br /> distance to the west; it empties into the Stockton Deepwater <br /> Channel just to the north. <br /> The topography is essentially flat, with drainage towards the <br /> west at less than 5' per mile. Sediments consist primarily of <br /> unconsolidated clays, silts, sands, and some gravels, typical of <br /> recent floodplain deposits Refer to PLATE II for details. <br /> SOIL TYPES: <br /> According to a 1952 University of California publication, soils <br /> in the area consist of Columbia silty clay Loam, dredger fill, <br /> and "madeland. " The soil profile revealed by the removal of the <br /> UST indicated that the top 3-4' consists of fill, underlain by <br /> undifferentiated flood plain deposits. PLATE III shows the <br /> general soil profile in the area_ <br /> i <br /> 2 <br />
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