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FLOOD04049
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Last modified
1/25/2010 6:45:07 PM
Creation date
10/5/2006 12:18:19 AM
Metadata
Fields
Template:
Floodplain Documents
County
Denver
Community
All
Stream Name
All
Basin
South Platte
Title
Riverine Erosion Hazard Areas Mapping Feasibility Study Executive Summary
Date
9/1/1999
Prepared For
State of Colorado
Prepared By
FEMA
Floodplain - Doc Type
Educational/Technical/Reference Information
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<br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />Some analysis methods are based on the hypothesis that the stream system tends toward <br />a state of dynamic equilibrium in which the channel adjusts to changes in the water and <br />sediment supply regimes. These methods include simple equations called "regime <br />relationships," techniques based on mechanical stability conditions, and complex <br />ccmputer models. These equilibrium-based approaches have difficulties in accounting for <br />ever-changing land use ccnditions. <br /> <br />In addition to fluvial processes, numerous climatic, environmental and geotechnical factors <br />are involved, Hydrodynamically induced erosion and deposition and the occurrence of <br />mass failure of the streambanks drive channel cross sectional changes. Induced effects <br />include changes in roughness, bed material ccmposition, vegetation cover, and planform. <br />Prediction of cross sectional adjustments can only be acccmplished for site-specific <br />ccnditions after the most significant geomorphological factors have been identified. <br />Therefore, any prediction of channel geometry should be based on sound field <br />observations, <br /> <br />Literature Review <br /> <br />Of several hundred pieces of literature, 108 articles and reports were evaluated to survey <br />methods currently in use to predict channel changes. Of this set, 12 case studies were <br />selected for detailed review. The map below shows the geographic region covered by all <br />of the case studies ccmbined, The general features of the case studies are summarized <br />in the table on the next page. <br /> <br /> <br /> <br />Iowa Streambank <br />Erosion Study <br /> <br />Utah River Stability <br />Studies <br /> <br />Minnesota Stream <br />Meander Study <br /> <br />Platte River, NE <br />Geomorphic Study <br /> <br />u. Mississippi/Illinois <br />Waterway Study <br /> <br />King Co, WA <br />Channel Migration <br /> <br />San Diego Co" CA <br />Alluvial Studies <br /> <br />Arizona Lateral <br />Migration Standards <br /> <br />Rillito Creek Tucson AZ <br />Probabilistic Study <br /> <br />Santa Cruz River, AZ. <br />Geomorphologic Study <br /> <br />Location of case studies, <br /> <br />8 <br />
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