My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
SU0000099 SSC RPT
Environmental Health - Public
>
EHD Program Facility Records by Street Name
>
S
>
SPARROW HAWK
>
13983
>
2600 - Land Use Program
>
MS-99-21
>
SU0000099 SSC RPT
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
11/25/2019 9:59:03 AM
Creation date
11/25/2019 9:42:46 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
FileName_PostFix
SSC RPT
RECORD_ID
SU0000099
PE
2622
FACILITY_NAME
MS-99-21
STREET_NUMBER
13983
Direction
E
STREET_NAME
SPARROW HAWK
STREET_TYPE
RD
ENTERED_DATE
8/8/2001 12:00:00 AM
SITE_LOCATION
13983 E SPARROW HAWK RD
P_LOCATION
99
P_DISTRICT
004
QC Status
Approved
Scanner
SJGOV\gmartinez
Tags
EHD - Public
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
91
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
k4 KL E I N F E L D E R <br /> TABLE 3 <br /> REGIONAL GEOLOGY AND HYDROGEOLOGY <br /> REGIONAL The site lies in the western part of the Great Valley Geomorphic Province <br /> GEOMORPHIC of California. The valley is approximately 400 miles long and averages 50 <br /> PROVINCE miles wide, comprising approximately 20,000 square miles. The valley has <br /> been tilled with a thick sequence of marine and nonmarine sediments from <br /> the late Jurassic to Holocene. The uppermost strata of the Great Valley <br /> represents, for the most part, the alluvial, flood, and delta plains of two <br /> major rivers (Sacramento and San ,Joaquin Rivers) and their tributaries. <br /> The valley deposits are derived from the Coast Ranges to the west and the <br /> Sierra Nevada to the east. Granitic and metamorphic rocks outcrop along <br /> the eastern and southeastern flanks of the valley. Marine sedimentary <br /> rocks outcrop along most of the western, southwestern, southern, and <br /> southeastern flanks; and volcanic rocks and deposits outcrop along the <br /> northeastern flanks of the valley. The valley geomorphology includes <br /> dissected uplands, low alluvial plains and fans, river flood plains and <br /> channels, and overflow lands and lake bottoms. <br /> The site is located in an area characterized by alluvial fan deposits. The <br /> majority of the native sediments include a heterogeneous mix of poorly <br /> sorted clay, silt, sand, and gravel. Some beds of claystone, siltstone, <br /> sandstone, and conglomerate can also be present. <br /> DEPTH TO According to the San Joaquin County Flood Control and Water <br /> REGIONAL Conservation District map entitled, "Lines of Equal Elevation of <br /> GROUNDWATER Groundwater, Spring 1998", The groundwater flow direction of the area <br /> AND DIRECTION tends towards the south. Groundwater is at an elevation of 20 feet below <br /> OF ANTICIPATED mean sea level. General groundwater depth and flow may be influenced by <br /> FLOW local pumping, rainfall, irrigation patterns and tidal fluctuations. <br /> Evaluatiod of such factors is beyond the scope of this assessment. <br /> 20-4328-0I.P01/2019R556 Page 6 of 21 <br /> Copyright 1999,Kleinfelder, Inc. .July 6, 1999 <br />
The URL can be used to link to this page
Your browser does not support the video tag.