My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
SU0006227 SSCRPT
EnvironmentalHealth
>
EHD Program Facility Records by Street Name
>
M
>
MOUNTAIN HOUSE
>
22261
>
2600 - Land Use Program
>
PA-0600127
>
SU0006227 SSCRPT
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
12/17/2019 11:37:58 AM
Creation date
9/6/2019 10:17:52 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
FileName_PostFix
SSCRPT
RECORD_ID
SU0006227
PE
2620
FACILITY_NAME
PA-0600127
STREET_NUMBER
22261
Direction
S
STREET_NAME
MOUNTAIN HOUSE
STREET_TYPE
PKWY
City
MOUNTAIN HOUSE
ENTERED_DATE
8/29/2006 12:00:00 AM
SITE_LOCATION
22261 S MOUNTAIN HOUSE PKWY
RECEIVED_DATE
8/28/2006 12:00:00 AM
P_LOCATION
99
P_DISTRICT
005
QC Status
Approved
Scanner
SJGOV\sballwahn
Supplemental fields
FilePath
\MIGRATIONS\M\MOUNTAIN HOUSE PKWY\22261\PA-0600127\SU0006227\SSC RPT.PDF
Tags
EHD - Public
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
145
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
r <br /> L <br /> law MACHADO PROPERTY Page 8 <br /> WKA No. 6078.02 <br /> ` November 1, 2004 <br /> subject property,therefore, is predicted to have ranged from approximately 10 to 30 feet below <br /> the ground surface. The 1978 7.5 minute Clifton Court Forehay Topographic Quadrangle Map <br /> prepared by the U.S. Geological Survey, indicates that regional topography in the region of the <br /> L subject property slopes northeasterly, therefore we estimate groundwater flow direction as <br /> northeasterly. <br /> t <br /> L Regional Geology <br /> LThe subject property is located in the central portion of the Great Valley geomorphic province of <br /> California. The Great Valley lies between the mountains and foothills of the Sierra Nevada <br /> Range to the east and the California Coast Ranges to the west. The geologic formations of the <br /> L, Great Valley are typified by thick sequences of alluvial (river) sediments deposited during the <br /> filling of a large ancient basin. <br /> L The 1985 USGS Geologic Map of the Late Cenozoic Deposits of the Sacramento Valley and <br /> Northern Sierra Foothills, California, shows the subject property to be underlain by the Lower <br /> member of the Modesto Formation. The Lower member geologic unit is characterized by <br /> unconsolidated, slightly weathered gravel, sand, silt and clay. <br /> Soils <br /> Review of the 1998 U.S. Department of Agriculture, Soil Conservation Service (SCS)Soil <br /> Survey of San Joaquin County, California, indicates that the near-surface soils of the project area <br /> L consist of two soil types. The soil types are "Capay clay, 0 to 2 percent slopes" and"Stomar clay <br /> loam, 0 to 2 percent slopes." <br /> L <br /> The Capay clay formed in alluvium derived from mixed rock sources. The surface layer is <br /> typically grayish brown and dark grayish brown clay approximately 20-inches thick. The subsoil, <br /> 1 <br /> approximately 60-inches thick, consists of grayish brown, dark grayish brown, dark brown and <br /> pale brown clay. <br /> L <br /> The Stomar clay loam formed in alluvium derived from sedimentary rock sources. This soil is <br /> L typically grayish brown clay approximately 19-inches thick. The subsoil, approximately 30- <br /> inches thick, is a mixture of brown clay loam and clay that is underlain by yellowish brown clay <br /> loam at a depth of 60-inches. <br /> WALLACE•KUHL <br /> &ASSOCIATES ING <br />
The URL can be used to link to this page
Your browser does not support the video tag.