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Last modified
1/26/2010 3:16:29 PM
Creation date
10/12/2006 4:47:35 AM
Metadata
Fields
Template:
Water Supply Protection
File Number
8240.200.48.D.3
Description
Wolford Mountain
State
CO
Basin
Colorado Mainstem
Water Division
5
Date
3/12/1998
Title
Wolford Mountain Biological Opinion and attached MOU
Water Supply Pro - Doc Type
Biological Opinion
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<br />27 <br /> <br />Habitat Formation <br /> <br />The formation of a variety of channel habitats, including gravel/cobble bars <br />and substrates used by Colorado squawfish for spawning, is essential to ensure <br />the availability of the range of habitats required by all endangered fish life <br />stages to fulfill daily requirements (foraging, resting, spawning, avoiding <br />predation. etc.) under various flow conditions. The number and distribution <br />of these channel habitats can be described as channel habitat complexity, <br />diversity, or heterogeneity, Qsmundson and Kaeding (1991) found that adult <br />Colorado squawfish in the Grand Valley prefer river segments with a complex <br />morphometry over those that are simple. <br /> <br />Some important habitats. such as inundated floodplain depressions used by <br />razorback suckers, are located outside the channel. Floodplain depressions <br />are principally derived from abandoned main channels, side-channels. <br />backwaters, and meander cutoffs. <br /> <br />The creation of.complex channel habitat and the formation and eventual <br />abandonment of channel features from which floodplain depressions are formed <br />occur primarily during spring runoff when flows are of sufficient size and <br />duration to cause major changes in channel morphology through significant <br />erosion and deposition of bed and bank materials, The reduction in the <br />magnitude, duration. and frequency of high spring flows has slowed the rate at <br />which channel morphology changes. Consequently, the creation of complex <br />channel habitat and floodplain depressions has slowed. The placement of <br />riprap and other bank stabilization measures and the construction of dikes and <br />levees impede changes in channel morphology and contribute to the slowed <br />creation of complex channel habitat. In addition. the construction of dikes <br />and levees reduces existing channel habitat complexity by causing <br />channelization of the river. Dikes and levees also isolate existing <br />floodplain depressions from the channel during high flows. The slowed <br />creation of complex channel habitats and new floodplain depressions. the <br />reduction of existing channel habitat complexity. and the isolation of <br />existing floodplain depressions have acted to reduce the quantity and quality <br />of important habitat for endangered fishes. <br /> <br />Habitat Maintenance <br /> <br />Backwaters. used by various life stages of endangered fish, are damaged by the <br />deposition of fine sediments which reduces their depth and consequently their <br />duration and frequency of inundation. Gravel and cobble substrates. used by <br />squawfish for spawning, are affected by the infiltration of fine sediments. <br />The establishment of vegetation on backwater sediments and on bars further <br />
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