Long Term Geomorphic Evolution and Recession Models for the Lake Michigan Bluffs in Wisconsin, Part 1 |
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Long Term Geomorphic Evolution and Recession Models for the Lake ..., Part 2 Christopher Scott Peters No preview available - 1982 |
Common terms and phrases
approximate average beach Bender Park bluff angles bluff edge bluff face morphology bluff group bluff height bluff morphology bluff profile Bluff subgroup bluff toe cause changes Chapter cohesive considered County Profile County sec cycle decline develop discussed dynamic effect equilibrium eroding factors failure feet flow fluctuations geomorphic geomorphic changes greater group F gullies HORIZONTAL DISTANCE ft internal Kewaunee lake level Lake Michigan landform less located long term lower bluff magnitude major Manitowoc County mass movement material measured Milwaukee County monitoring northern Note occurred Ozaukee County pattern period Port Washington present processes profile shape protection Racine County rapid recession recession model representative result scale sediment Sheboygan County shoreline short term shown in Figure similar slides slope slumping soil southern stability steep straight subgroup E.1 suggest Table thresholds trees types upper bluff variable vegetated water level wave erosion