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Last modified
7/14/2009 5:02:34 PM
Creation date
5/22/2009 7:40:32 PM
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UCREFRP
UCREFRP Catalog Number
9292
Author
Trammell, M. and T. Chart.
Title
Aspinall Unit Studies Nursery Habitat Studies Colorado River 1992--1996.
USFW Year
1998.
USFW - Doc Type
Moab, Utah.
Copyright Material
NO
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t <br />25 <br />APPENDIX A <br />Table Al . List of habitat types as defined by Rokowski and Schmidt,1996. Utah State University. <br />Secondary Channel (SeC) -habitats formed by the erosion/ deposition cycle of small secondary channels during passage of <br />a flood, and revealed by receding water levels. Usually retaining slight flow until late in the year. <br />ScourChannel (SC) -habitats formed by the erosion/deposition cycle of small channels behind large alternating sandbars. <br />Scoured out during floods and revealed by receding water levels. Usually relatively deep and permanent. <br />Migrating Sand Waves (MS) -habitats formed by the relative movement of adjacent migrating sand waves. Relatively <br />shallow and ephemeral. <br />Horseshoe Vortex (HS) -habitats formed by scour holes generated at high flows at the upstream ends of islands due to <br />development of horseshoe vortex patterns. Moderately deep and semi-permanent <br />Flood Plain (FP) -habitats formed by the inundation of abandoned channels or floodplains. Related to seasonal high flows <br />or rainfall events. <br />Flooded Tributary Mouth (FT) -habitats formed by rising river levels flooding into tributary mouths. Related to seasonal <br />high flows or rainfall events. <br />Shoreline Eddy (SB) -habitats formed by recirculating areas due to irregularities of the bank <br />Constricted Reach Eddy (CE) -habitats formed by large eddies generated by constriction of the channel by debris fans. <br />Shoreline (SH) -Shallow, sloping shoreline areas. <br />
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