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Agenda - 06-04-1981
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Agenda - 06-04-1981
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9/19/2016 2:29:23 PM
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BOCC
Date
6/4/1981
Meeting Type
Public Hearing
Document Type
Agenda
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r2 <br /> ..,,, <br /> hazard potential. The floodway is that area within the stream bunks <br /> and adjacent to it required in order to discharge the 100-year flood <br /> , - <br /> without raising the water surface elevation more than one foot above <br /> : <br /> be flood level at any point. It is cruc3a1 that the floodway be <br /> kept free of obstacles so that this fUnction will not be disrupted. <br /> The floodway fringe is the area bordering the floodway which will be <br /> inundated during a flood and which serves to hold the floodwaters <br /> until it can be carried away in the floodway channel. <br /> In addition to the 100-year flood prone area, consideration is also <br /> given to the 500-year flood prone area, the area of land susceptible <br /> to inundation duzaIng a storm which would occur on the average once <br /> every 500 years. The relative probability of these two storm events <br /> suggests fewer constraints and, therefore, minimal land use regu- <br /> lations in the 500-year flood prone area as opposed to the 100-year <br /> flood prone area. <br /> The U.S. Army Corps of Engineers prepared maps at a scale of 1" = 1000' <br /> for Orange County showing the floodway, the 100-year floodway fringe and <br /> the 500-year floodway fringe for all streams draining more than one <br /> square mile of watershed. Orange County applied and was admitted to the <br /> Flood Insurance Program, and has consequently adopted a Flood Prevention <br /> Ordinance. This ordinance constitutes a major regulatory tool affect- <br /> ing the use of lands constrained by flood hazards. <br /> Soil Conditions <br /> ... The interaction of different rock types, local topography, temperature <br /> 1 changes, rain, flora and fauna has produced soils which reflect the <br /> geological and dramatic Conditions of Orange County. Soils on the <br /> County range from well drained, gently sloping uplands to steeply sloped, <br /> shallow to bedrock soils, to flat soils subject to flooding along <br /> , <br /> ' streams. <br /> Perhaps no other natural environmental factor has as much influence on <br /> land use and land development as soil conditions. Regardless of the <br /> particular land use, soils are the most important factor determining <br /> the suitability of the land for that use. Soil characteristics such as <br /> depth to bedrock, permeability, shrink-swell potential, erodibility and <br /> drainage are important factors influencing land use soils present <br /> constraints to development ranging from slight limitations to severe <br /> limitations. In general, the costs of site preparation and construction <br /> will increase as the severity of soil limitations in an area increases. <br /> The Soil Conservation Service (SCS) completed a soil survey of Orange <br /> County in 1976. Each soil type in Orange County has been described in <br /> terms of these characteristics and their potential use and management <br /> requirements. The Orange County Planning Department in conjunction with <br /> Mr. Robert Kirby, an SCS scientist, combined the 38 soil types identi- <br /> fied in the soil survey into ten suitability categories based on simi- <br /> lar characteristics as described in the report, A Pl- : Guide to the <br /> Orange County, North Carolina <br /> This allows the general public to 'mow- in a broad manner what types of <br /> development are suitable for certain uses, including septic tanks, foun- <br /> dations, roads and prime agricultural land. The soil suitability classi- <br /> fication system identifies the constraints posed by the various categories: <br />
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