A.
There are areas within Fredon Township which are underlain by carbonate bedrock such as limestone and dolomite. The solution of the bedrock causes surface depressions, open drainage passages, and the development of irregular, subsurface rock topography known as karst. These conditions make such areas unstable and susceptible to subsidence and surface collapse. As a result, the alteration of drainage patterns in these areas by the placement of impervious coverage, grade changes, or increased loads from site improvements can lead to land subsidence and sinkholes.
B.
Fractures or solution openings and fissures in the limestone rock may lead to public or private water supplies, making those sources especially susceptible to groundwater contamination. Contamination of water sources can occur from solid and liquid wastes, contaminated surface water, septic tank effluent, or other hazardous substances moving through fractures or solution openings and fissures within the rock.
C.
Carbonate aquifers are an important source of groundwater in Fredon Township. The Township relies on a clean supply of subsurface water to foster and promote human health, welfare and economic and social development. Therefore, the purposes of enacting this chapter are to protect, preserve and enhance a sensitive and valuable potable groundwater resource area and to reduce the frequency of structural damage to public and private improvements by sinkhole collapse or subsidence in areas of limestone geology, thus protecting the public health, safety and welfare and insuring orderly development within the Township.