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Last modified
7/14/2009 5:02:30 PM
Creation date
5/20/2009 3:24:05 PM
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UCREFRP
UCREFRP Catalog Number
7401
Author
U.S. Bureau of Reclamation.
Title
Ruedi Reservoir, Colorado Round II Water Marketing Program, Final Supplement to the Environmental Statement, Fryingpan - Arkansas Projects, Colorado.
USFW Year
1989.
USFW - Doc Type
Billings, Montana.
Copyright Material
NO
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3.15 <br />Habitat characterization surveys for the Fryingpan River conducted in <br />October 1982 revealed that the ratio of pools and runs to riffles is about 0.7 <br />(Appendix B, Table B.2 and Figures B.1 to B.8). Based on observations at eight <br />study reaches, the percentage of total area comprised of riffles and pool/runs <br />is 57 percent and 43 percent, respectively. In most instances, water depth <br />provides adequate cover in pool/runs, exceeding 30 percent of the total reach <br />area at five of eight study reaches. A section of the river about 0.8 miles in <br />length near the confluence with Seven Castles Creek is unique due to the <br />abundance of deep runs and pools. Cover for adult and juvenile trout is <br />excellent in this section of river due to extensive macrophyte beds, undercut <br />banks, and depth. Bottom substrates at most sections of the river are dominated <br />by cobbles and boulders. Spawning gravels seem to be limited to a few sections <br />located below the dam, near the Taylor Creek and Seven Castles Creek <br />confluences. <br />. The study segment for the Roaring Fork River extends from the confluence <br />with the Fryingpan River near Basalt to the confluence with the Colorado River <br />at Glenwood Springs (Figure 3.1). Generally, the physical and chemical <br />characteristics in this section of the Roaring Fork River represent fair to good <br />quality habitat for trout (Table 3.7 and Appendix B, Table B.3). A brief <br />description of the more important habitat characteristics is provided below. <br />Habitat characteristics in the Roaring Fork River are quite different in <br />the upper (between Basalt and Carbondale) and lower sections (just below <br />Carbondale to confluence with Colorado River) (Appendix B, Table B.4 and Figures <br />B.9 to B.14). In general, the lower section of the Roaring Fork River is much <br />wider and deeper and contains more pools and runs and more cover for trout than <br />the upper section. Based on six study reaches in the Roaring Fork River (Figure <br />3.1), the average percentage of area comprised of riffles and pools/runs in the <br />upper section (Reaches 1 through 4) are 70 and 30 percent respectively, while <br />values in the lower section are 43 and 57 percent, respectively. Similarly, the <br />percentage of area providing cover for juvenile and adult trout is higher in the <br />lower section with a mean value of 49 percent compared to 22 percent in the upper <br />section. Substrate is similar throughout most of the river with boulders and <br />cobbles representing the dominant size groups. Limited spawning gravels appear <br />to be available in the mainstem of the river with only two study reaches <br />exhibiting about 0.5 percent of the total area as potential spawning substrate.
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