My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
7256
CWCB
>
UCREFRP
>
Public
>
7256
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
7/14/2009 5:02:29 PM
Creation date
5/20/2009 3:40:27 PM
Metadata
Fields
Template:
UCREFRP
UCREFRP Catalog Number
7256
Author
Radant, R. D., et al.
Title
Colorado Squawfish Investigations - White River, Utah.
USFW Year
1983.
USFW - Doc Type
Salt Lake City, Utah.
Copyright Material
NO
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
45
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 />. <br /> <br />stratum within the study area (Stratum X) was originally delineated as <br />the area between Rangely, Colorado, river mile (RM) 94.5 and the Ignacio <br />Bridge, RM 59.3 in Utah (Miller et ale 1982a). For the purpose of our <br />investigations, that portion of Stratum X within the study boundary <br />(Utah-Colorado state line to the Ignacio Bridge) was designated Stratum <br />X2. This 12.7-mi (20.4-km) section contains the most diverse habitat. <br />The river flows through steep canyons, has a higher gradient than <br />adjacent strata and has riffles with cObble/rubble and rubble/cobble <br />substrate (Miller et ale 1982a). <br />The middle Stratum (Y) begins at the Ignacio Bridge, RM 59.3 and ends <br />38 mi (61.1 km) downstream at the Mountain Fuel Bridge, RM 21.3. In this <br />section, the river flows through more open canyons and has a substrate <br />mixture of sand/silt where water velocities are low and cobble/rubble or <br />rubble/boulder in high gradient, high velocity reaches (Miller et ale <br />1982a). <br /> <br /> <br />The lowest Stratum (Z) begins at the Mountain Fuel Bridge, RM 21.3 <br /> <br />and extends 21.3 mi (33.8 km) downstream to the confluence of the White <br /> <br />with the Green River. In this stratum, the river flows through a wide <br /> <br />flood plain and is characterized by lower gradient, lower velocities and <br /> <br />smaller substrate than is found in upstream strata. <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />. <br /> <br />5 <br /> <br />. <br />
The URL can be used to link to this page
Your browser does not support the video tag.