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Last modified
7/14/2009 5:02:34 PM
Creation date
5/22/2009 6:43:10 PM
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UCREFRP
UCREFRP Catalog Number
8267
Author
Elliott, J. G. and L. A. Hammack.
Title
Geomorphic and Sedimentologic Characteristics of Alluvial Reaches in the Black Canyon of the Gunnison National Monument, Colorado.
USFW Year
1999.
USFW - Doc Type
Water-Resources Investigations Report 99-4082,
Copyright Material
NO
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Table 1. Streamflow characteristics for the Gunnison River downstream <br />from the Gunnison Tunnel, U.S. Geological streamflow-gaging station 09128000 <br />[Recurrence interval, in years, equals reciprocal of exceedance probability, calculated with <br />annual instantaneous discharge peak; streamflow duration in percentage of time specific <br />discharge is equaled or exceeded calculated with daily mean discharge; ft3/s, cubic foot <br />per second; %, percentage] <br />Recurrence interval <br />Discharge Pre- Post- <br />(ft3/s) regulation regulation <br />1911-65 1966-94 <br />(years) (years) <br />500 <br />1,000 <br />1,140 <br />2,000 <br />2,200 <br />3,000 <br />4,000 <br />5,000 <br />5,140 <br />6,000 <br />7,000 <br />8,000 <br />9,000 <br />10,000 <br />11,000 <br />12,000 <br />13,000 <br />14,000 <br />15,000 <br />16,000 <br />17,000 <br />18,000 <br />19,000 <br />20,000 <br />1.01 <br />1.04 <br />1.09 <br />1.17 <br />1.18 <br />1.30 <br />1.50 <br />1.70 <br />2.0 <br />2.5 <br />3.2 <br />4.4 <br />6.0 <br />8.0 <br />11 <br />16 <br />24 <br />35 <br />55 <br />90 <br />1.01 <br />1.02 <br />1.18 <br />1.25 <br />1.65 <br />2.5 <br />4.0 <br />4.2 <br />6.0 <br />10 <br />16 <br />24 <br />35 <br />50 <br />75 <br />100 <br />Streamflow duration <br />pre- Post- <br />regulation regulation <br />1911-65 1966-94 <br />(% time) (% time) <br />80 80 <br />51 65 <br />28 47 <br />26 42 <br />19 17 <br />18 12 <br />14 4.0 <br />11 1.2 <br />7.9 0.72 <br />7.5 0.70 <br />5.8 0.60 <br />4.1 0.46 <br />2.8 0.28 <br />1.9 0.13 <br />1.2 0.03 <br />0.8 <br />0.5 <br />0.3 <br />0.16 <br />0.09 <br />table 2. A complete set of photographs taken from <br />these locations is in the possession of the NPS Water <br />Resources Division in Fort Collins, Colorado, and <br />selected photographs are presented in the appendix at <br />the end of this report. <br />Geomorphic Surveys <br />Surveys were made of the study reaches with a <br />total-station laser theodolite to quantify geomorphic <br />features, high-water elevations, channel cross-section <br />characteristics, and river gradient. Data from these <br />surveys also were used as input to one-dimensional, <br />water-surface profile models and sediment-entrain- <br />ment potential calculations. The Warner Point study <br />reach (fig. 4) was approximately 3,000 ft long and was <br />surveyed in 1990, 1994, and 1995. Twelve channel <br />cross sections were surveyed in the Warner Point reach <br />and were used to calibrate the one-dimensional, water- <br />surface profile model. Hydraulic-geometry character- <br />istics and sediment-entrainment potential were calcu- <br />lated at 8 of the 12 cross sections. Geomorphic <br />features surveyed included streambanks, alluvial bars, <br />and overflow channels between the bars and adjacent <br />talus slopes. <br />10 Geomorphic and Sedimentologic Characteristics of Alluvial Reaches in the Black Canyon of the Gunnison National Monument, <br />Colorado <br />
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