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AG 2002 12 16 (Regular)
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AG 2002 12 16 (Regular)
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Last modified
3/2/2006 5:02:05 PM
Creation date
11/27/2017 11:44:46 AM
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Meeting Minutes
Doc Type
Agenda
Meeting Minutes - Date
12/16/2002
Board
Board of Commissioners
Meeting Type
Regular
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NATURAL FEATURES AND SOILS <br /> <br />The northeastern region consists primarily of four types of soils: Enon-Mecklenburg-Poinexter, <br />Badin-Tatum-Georgeville, Goldston-Badin, and Kirksey -Misenheimer-Badin. Each of these <br />four soils share similar characteristics that support the vast farm and cropland usage in the area. <br />These characteristics include grades that range from gently sloping to very steep; compositions <br />that allow the soils to be well drained; and each has a clayey subsoil. Each of these soils also <br />have their own limitations, according to the United States Department of Agriculture (USDA), <br />such as slow permeability rates, high shrink-swell potential, erosion, and depth of bedrock. The <br />slow peri~eability rate indicates that water travels slowly as it moves through saturated soils, this <br />means that the land percolates slowly which is important information for properties using septic <br />systems. The shrink-swell potential means that the soils tend to contract and expand over the <br />course of time. This is an important factor when considering the building of roads, building <br />foundations, and/or other structures that could suffer from cracks due to the movement of the soil. <br />Erosion refers to the wearing away of the soil and is caused by many natural and man-made <br />factors. The effects of erosion are most apparent along river and streambeds where the root base <br />of trees are exposed because the soil has been stripped away by water. The depth of bedrock is <br />important when considering how far down one must drill in order to install a well system or deep <br />footings. The USDA Soil Survey of Cabarrus County indicates that the soil types that can <br />support urban development best are those included in the Cecil and Hiwassee series which are <br />subsets of the four soils mentioned previously, each of which can be found throughout the <br />northeast region. <br /> <br />This region of Cabarrus County is dotted with many creeks and floodplains. The primary water <br />features in the Rockwell area are the Second and Jennie Wolf Creeks. The Rimer and Watts <br />Crossing areas include Dutch Buffalo, Jennie Wolf, Saw Mill, Black Run, and Little Buffalo <br />Creeks. The Town of Mount Pleasant also includes Saw Mill, Dutch Buffalo, Little Buffalo <br />Creeks as well as Adams, Little Bear and MeAllister Creeks and Butcher Branch as it significant <br />water features. Each of these creeks and branches create floodplains that should be protected from <br />any developmental disturbances. Fortunately, Cabarrus County has adopted the Flood Damage <br />Prevention Ordinance that will regulate development along these floodplains. The Town of <br />Mount Pleasant has also increased its developmental restrictions when it adopted the Unified <br />Development Ordinance. It is important to protect these waterways and floodplains for water <br />quality and environmental reasons and most importantly for storm water management. <br /> <br /> <br />
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