My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
PROJ00455
CWCB
>
Loan Projects
>
Backfile
>
1-1000
>
PROJ00455
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
11/19/2009 11:43:26 AM
Creation date
10/5/2006 11:56:06 PM
Metadata
Fields
Template:
Loan Projects
Contract/PO #
C153583
Contractor Name
Ute Water Conservancy District
Water District
0
Bill Number
XB 99-999
Loan Projects - Doc Type
Feasibility Study
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
105
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).
Show annotations
View images
View plain text
<br />i <br />! <br /> <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />:1 <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />Section VI (Crom Station 764+05 to Station 767+25) <br />The subsurface conditions along this section can be characterized as river bed <br />deposits, consisting of cobbles, gravel, and sand. The thickness of this material is <br />estimated to be between 30 to 40 feet. Based on CDOH bore-hole information and <br />interviews with local contractors with previous construction experience near the <br />Colorado River, the subsurface material at this location consists of a layer of gravel <br />with occasional boulders 4 to 5 feet in thickness. This layer overlays a series of <br />sandy silt and gravelly sand layers with occasional boulders to depths of up to 40 feet <br />below the stream bed. <br /> <br />Section VII (from Station 767+25 to Station 810+25) <br />The subsurface condition along this section consists of flood plain alluvial deposits <br />consisting of fines and silt overlaying sandstone bedrock. The depth to bedrock is <br />estimated to be more than 30 feet below the existing ground surface. Due to the <br />close proximity of the Colorado River the subsurface materials are expected to be <br />saturated. The area along the Colorado River contains dense to very dense riparian <br />vegetation. <br /> <br />Section VIII (from Station 810+25 to Station 814+75) <br />The subsurface condition along this section can be characterized as river-bed <br />deposits, consisting of cobbles, gravel, and sand. The thickness of this river deposited <br />material is estimated to be between 40 to 50 feet. <br /> <br />Section IX (from Station 814+75 to Station 816+25) <br />The subsurface condition along this section consists partly of natural soils and partly <br />embankment material used in construction of 1-70. The natural soils and <br />embankment materials are anticipated to be similar to natural soils encountered <br />along section I and II. There is the possibility for large boulders in the embankment <br />material. Groundwater along this section at the proposed excavation depths is <br />estimated to be 10 to 15 feet below the existing 1-70 surface. <br /> <br />Section X (from Station 816+25 to Station 822+21) <br />The subsurface conditions along this section can be characterized by relatively thin <br />layers of alluvial and colluvial deposits mainly consisting of sand, gravel and boulders <br />overlaying the sandstone bedrock. The depth to bedrock is estimated to be from 5 <br />to 10 feet below the existing ground surface. Groundwater along this section to the <br />proposed pipeline installation depth is anticipated to be non-existent. <br /> <br />27 <br />
The URL can be used to link to this page
Your browser does not support the video tag.