My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
FIELD DOCUMENTS_CASE 2
EnvironmentalHealth
>
EHD Program Facility Records by Street Name
>
M
>
MARIPOSA
>
13521
>
3500 - Local Oversight Program
>
PR0545534
>
FIELD DOCUMENTS_CASE 2
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
3/13/2020 1:49:23 AM
Creation date
3/12/2020 11:59:56 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
FIELD DOCUMENTS
FileName_PostFix
CASE 2
RECORD_ID
PR0545534
PE
3528
FACILITY_ID
FA0001457
FACILITY_NAME
COLLEGEVILLE MARKET & CAFE
STREET_NUMBER
13521
Direction
E
STREET_NAME
MARIPOSA
STREET_TYPE
RD
City
STOCKTON
Zip
95215
APN
18306007
CURRENT_STATUS
02
SITE_LOCATION
13521 E MARIPOSA RD
P_LOCATION
99
P_DISTRICT
004
QC Status
Approved
Scanner
SJGOV\sballwahn
Tags
EHD - Public
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
65
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
07 January 2004 <br /> AGE-NC Project No. 02-0970 <br /> Page 2 of 4 <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 closest surface water feature to the site is the South Fork of Little John Creek is located <br /> approximately 2,000 feet south of the site. Water from the creek drains into the San Joaquin River <br /> Deep Water Channel. <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 sedimentary units are relatively horizontal and continuous over the <br /> �• area. The estimated depth to ground water at the site is approximately 80 to 90 feet below surface <br /> grade (bsg),based on the map titled Lines of Equal Depth to Groundwater, Spring 1999 published <br /> by the San Joaquin County Flood Control District and Water Conservation District(FCD&WCD) <br /> The map titled Lines of Equal Elevation of Groundwater, Spring 1999, also published by the <br /> FCD&WCD, provides indeterminate data concerning local ground water elevation and flow <br /> direction. The prevailing ground water flow direction east of Stockton generally ranges from west <br /> to southwest, but this may be greatly modified by local recharge and discharge patterns. <br /> `r 3.0. SOIL ASSESSMENT ACTIVITIES <br /> Its is AGE's understanding that petroleum hydrocarbon-impacted soil was encountered during the <br /> v performance of a dispenser island upgrade.Based on the findings of investigation performed during <br /> the dispenser island upgrades, the EHD required further investigation of the area northwest of the <br /> dispenser island. <br /> 3.1. PROCEDURES <br /> On 08 November 2002, AGE advanced one soil probe borings using GeoProbe "direct-push" <br /> techniques near the northwest side of the dispenser island(Figure 2). The boring was advanced to <br /> approximately 20 feet below surface grade(bsg).Soil samples were collected from the boring at five- <br /> foot intervals beginning at five feet bsg. <br /> 3.2. SOIL SAMPLE ANALYSIS <br /> Selected soil samples were analyzed by a State of California Department of Health Services(DHS)- <br /> certified laboratory for the following constituents: <br /> Advanced GeoEnvironmental,Inc. <br /> v <br />
The URL can be used to link to this page
Your browser does not support the video tag.