My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
SU0006108 SSCRPT
Environmental Health - Public
>
EHD Program Facility Records by Street Name
>
W
>
WELTY
>
34701
>
2600 - Land Use Program
>
PA-0600353
>
SU0006108 SSCRPT
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
5/7/2020 11:32:08 AM
Creation date
9/9/2019 11:03:38 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
FileName_PostFix
SSCRPT
RECORD_ID
SU0006108
PE
2611
FACILITY_NAME
PA-0600353
STREET_NUMBER
34701
Direction
S
STREET_NAME
WELTY
STREET_TYPE
RD
City
TRACY
APN
25518015
ENTERED_DATE
7/5/2006 12:00:00 AM
SITE_LOCATION
34701 S WELTY RD
RECEIVED_DATE
7/3/2006 12:00:00 AM
P_LOCATION
99
P_DISTRICT
005
QC Status
Approved
Scanner
SJGOV\rtan
Supplemental fields
FilePath
\MIGRATIONS\W\WELTY\34701\PA-0600353\SU0006108\SSC RPT.PDF
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.
/
208
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
` Surface &Subsurface Contamination Report Page 10 <br /> Sandhu Property <br /> Project No. 522.1 <br /> ` March 9, 2006 <br /> and silt alluvium deposited on the valley floor. Hotchkiss & Balding, in their <br /> ►� 1971 US Geological Survey report, Geology. Hydrology and Water Quality of the <br /> Tracy-Dos Palos Area San Joaquin Valley California, (Open File Report 72- <br /> 169) described the aquifers and their characteristics for the Tracy-Dos Palos <br /> ` area. In the Vernalis area, the recent alluvium is generally less than 100 feet <br /> thick and directly overlies the Tulare Formation, a Plio-Pleistocene age, mixed <br /> clastic sequence of clay, silt, sand and gravel. There is little to distinguish the <br /> contact between the base of the alluvium from the top of the Tulare Formation <br /> A widespread clay deposit, the Corcoran Clay (or E-clay), divides the upper and <br /> lower members of the Tulare Formation. The Tulare sediments lying above the <br /> Corcoran Clay are entirely Pleistocene in age. The Corcoran Clay is about 60 <br /> feet thick in the Vernalis area and it serves as an effective aquitard. It lies <br /> approximately 150 to 200 feet below the ground surface. It is believed that most <br /> major irrigation and water supply wells are completed below the Corcoran Clay <br /> zone. <br /> Federal Wetlands <br /> Based on information on the map in the EDR report (Appendix D) the Property <br /> does not include lands recognized in the federal wetlands inventory. <br /> • <br /> Radon <br /> Soil testing by EPA and California Department of Toxic Substance Control show <br /> that naturally occurring radon does not pose a material health risk in the <br /> Central Valley. <br /> ., 2.3 Past and Present Land Use of Property <br /> Current <br /> • The Property is the site of an undeveloped parcel of agricultural land. <br /> Prior <br /> The Property was used for several years during the 1940's as a prisoner of war <br /> camp. Before and since then, the Property has been used exclusively for % <br /> agricultural purposes. <br /> 2.4 Past and Present Land Use of Adjacent Properties <br /> The adjacent area has generally always been in agricultural use except for lots <br /> adjacent to the southwest. These parcels include several residences and an <br /> agricultural chemical sales and distribution facility. <br /> L 2937 Veneman Ave.,#B240 Geo-Phase Environmental Inc. Phone: (209) 569-0293 <br /> Modesto, CA 95356 Fax: (209) 569-0295 <br />
The URL can be used to link to this page
Your browser does not support the video tag.