My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
COMPLIANCE INFO_2019
EnvironmentalHealth
>
EHD Program Facility Records by Street Name
>
L
>
LOUISE
>
2112
>
2200 - Hazardous Waste Program
>
PR0538355
>
COMPLIANCE INFO_2019
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
9/17/2020 11:35:50 AM
Creation date
9/17/2020 10:26:34 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2200 - Hazardous Waste Program
File Section
COMPLIANCE INFO
FileName_PostFix
2019
RECORD_ID
PR0538355
PE
2227
FACILITY_ID
FA0022165
FACILITY_NAME
LATHROP WATER TREATMENT FACILITY / CORP YARD
STREET_NUMBER
2112
Direction
E
STREET_NAME
LOUISE
STREET_TYPE
Ave
City
Lathrop
Zip
95330
APN
19816003
CURRENT_STATUS
01
SITE_LOCATION
2112 E Louise Ave
QC Status
Approved
Scanner
KBlackwell
Tags
EHD - Public
Jump to thumbnail
< previous set
next set >
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
330
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
EnviroTech Consultants, Inc. Page 5 <br /> Site Investigation: Sampling Report <br /> Louise Avenue Water Treatment Facility <br /> 2.4 GEOLOGY, AND HYDROGEOLOGY <br /> 2.1 Area Geology <br /> The Site is located in the Great Valley Geomorphic Province(California Geological Survey 2002).The Great <br /> Valley generally trends north-south and is bordered by the Coast Ranges to the west and by the Sierra <br /> Nevada to the east. The Great Valley is an asymmetrical synclinal trough about 50 miles wide and 400 <br /> miles long with its axis off center to the west. Sediments have been deposited in this trough almost <br /> continuously since the Jurassic Period (about 160 million years ago). <br /> Lithology of the Great Valley consists of alluvial sediments known as the Great Valley Sequence, which is <br /> comprised of interbedded sedimentary units. The thickness of the Great Valley Sequence exceeds 25,000 <br /> feet in some areas. These sediments rest on a basement complex of metamorphic and igneous rocks. The <br /> surficial deposits are primarily eroded rock from the Sierra Nevada to the east and the Coast Range to the <br /> west. Because the synclinal trough was previously underwater, some of the sediments are of marine origin. <br /> A variety of unconsolidated Quaternary alluvial deposits are mapped in the site area;these represent active <br /> and inactive river and stream channel deposits, flood plain deposits, and alluvial outwash deposits. <br /> 2.2 Hydrogeology <br /> The Site is located within the Eastern San Joaquin Sub-basin of the San Joaquin River Valley Groundwater <br /> Basin as recognized by the California Department of Water Resources (DWR 2006). Groundwater-bearing <br /> formations in the vicinity of the Site consist of the Alluvium and Modesto/Riverbank Formations, Flood Basin <br /> Deposits, Laguna Formation, and Mehrten Formation. <br /> 5400 Rosedale Highway 0 Bakersfield, CA 93308 Tel 661.377.0073 Fax 661.377.0074 <br />
The URL can be used to link to this page
Your browser does not support the video tag.