My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
WORK PLANS
Environmental Health - Public
>
EHD Program Facility Records by Street Name
>
C
>
CHARTER
>
1419
>
3500 - Local Oversight Program
>
PR0544465
>
WORK PLANS
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
5/16/2019 11:54:59 AM
Creation date
5/16/2019 11:30:23 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
WORK PLANS
RECORD_ID
PR0544465
PE
3528
FACILITY_ID
FA0005837
FACILITY_NAME
STEFANOS GASOLINE*
STREET_NUMBER
1419
Direction
E
STREET_NAME
CHARTER
STREET_TYPE
WAY
City
STOCKTON
Zip
95205
APN
15137016
CURRENT_STATUS
02
SITE_LOCATION
1419 E CHARTER WAY
P_LOCATION
01
P_DISTRICT
001
QC Status
Approved
Scanner
SJGOV\wng
Tags
EHD - Public
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
135
PDF
Print
Pages to print
Enter page numbers and/or page ranges separated by commas. For example, 1,3,5-12.
After downloading, print the document using a PDF reader (e.g. Adobe Reader).
View images
View plain text
Nw <br /> SITE BACKGROUND INFORMATION <br /> Former STEFANO'S GAS STATION <br /> 1419 East Charter Way, Stockton, California <br /> The site is located at 1419 East Charter Way, Stockton, California. The site was formerly utilized <br /> as a gasoline service station and is currently a vacant lot with low topographic relief It is bounded <br /> by Sierra Nevada Street to the west and East Charter Way to the south. <br /> REGIONAL GEOLOGICAL/HYDROGEOLOGICAL 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 Sacramento and <br /> San Joaquin Valleys comprise the northern and southern portions of the Province. The Province is <br /> bordered by the Coast Ranges to the west,the Klamath Mountains and Cascade Range to the north, <br /> 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; the site itself is located on unconsolidated and semi-consolidated alluvium, lake,playa and <br /> terrace deposits of Quaternary age. Rocks composing the basement complex of the Province have <br /> not been completely 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).Based on information from quarterly monitoring events performed at the <br /> site, the depth to ground water on-site is approximately 40 to 45 feet below surface grade (bsg). <br /> Ground water generally flows towards the south to southeast. <br /> GROUND WATER DEPTH AND FLOW DIRECTION <br /> Ground water is currently encountered at a depth of approximately 40 feet bsg in on-site ground <br /> water monitoring wells; the flow direction is generally towards the south to southeast.Historically, <br /> the depths to ground water measured in the on-site monitoring wells and soil borings have ranged <br /> from approximately 39 to 46 feet bsg; relative ground water elevation maps for the site have been <br /> included in previous quarterly reports prepared by Wright Enviromnental Services, Incorporated <br /> (WES) and AGE. <br /> Advanced GeoEnvironmental,Inc. <br />
The URL can be used to link to this page
Your browser does not support the video tag.