[Ord. #2015-16]
For the purposes of this section, the following definitions shall apply:
AGRICULTURAL USEShall mean the production, keeping or maintenance of plants or animals for sale, lease or personal use.
BEDDINGShall mean the arrangement of a sedimentary rock in layers of varying thickness and character.
BEDROCKShall mean a general term for the rock that underlies soil or other unconsolidated material.
CARBONATE ROCKShall mean rock consisting chiefly of calcium and magnesium carbonates.
CAVEShall mean a natural opening of a size permitting human exploration and extending into a region of sharply reduced or no light.
CLOSED DEPRESSIONShall mean a shallow, dish-shaped hollow on the land surface which, in areas of limestone geology, may be indicative of old sinkholes or incipient collapse.
COLLAPSE SINKHOLEShall mean a sinkhole caused by the collapse of the roof of a bedrock cavern.
DEVELOPMENTFor this section, shall be defined as set forth in the Municipal Land Use Law.
DISAPPEARING STREAMShall mean a stream that enters the subsurface through a sinkhole or other entrance.
DISSOLUTIONShall mean a space or cavity in or between rocks, formed by the solution of part of the rock material.
DOLOMITEShall mean a carbonate rock that contains more than fifteen (15%) percent magnesium carbonate.
DRAINAGEShall mean the process by which water moves from an area by stream or overland sheet flow and/or the removal of excess surface water from soil by downward flow through the soil profile.
FAULTShall mean a surface or zone of rock fracture along which there has been noticeable differential movement.
FISSUREShall mean an extensive crack, break, or fracture in the rock.
GEOLOGIC INVESTIGATION PROGRAMShall mean a program which identifies the geologic nature of the bedrock materials underlying the site, and provides solutions directed at preserving the water quality and assuring the safety of any planned facility or improvement built over carbonate rocks.
JOINTShall mean a fracture in rock generally more or less vertical or transverse to bedding, along which no appreciable movement has occurred.
KARSTShall mean a type of topography that is formed over limestone or dolomite by dissolving or solution of the carbonate rocks, characterized by sinkholes, closed depressions, caves, solution channels, internal drainage, and irregular bedrock surfaces.
LIMESTONEShall mean a carbonate sedimentary rock consisting primarily of calcium carbonate. Limestone is commonly used as a general term for that class of rocks, which consists of at least eighty (80%) percent calcium or magnesium carbonate. In this subsection the term "limestone" shall be used generically to refer to carbonate rocks, limestone formations and Precambrian marble.
LINEATIONShall mean any straight line or alignment of natural features seen on an aerial photograph or any geographically referenced source. Although some lineations may be geologically controlled, ground-based geologic investigations are necessary to define their existence and significance.
MARBLEShall mean a metamorphic rock consisting primarily of crystallized limestone or dolomite.
OUTCROPShall mean an exposure of bedrock projecting through the ground surface.
PINNACLEShall mean an irregular rock projection often buried beneath the ground surface.
SHEAR ZONEShall mean a zone in which shearing has occurred on a large scale so that the rock is crushed and brecciated (broken).
SINKHOLE (DOLINE)Shall mean a localized land subsidence, generally a funnel-shaped or steep-sided depression, caused by the dissolution of underlying carbonate rocks or the subsidence of the land surface into a subterranean passage, cavity or cave. Sinkholes are formed by the underground removal of soil and rock material.
SOILShall mean the material found in the surface layer of the earth's crust which may be moved by a spade or shovel.
SOLUTIONED CARBONATESShall mean carbonate rocks that have had cavities formed, fractures widened, and passages in the rock created through the dissolution of the rock by the passage of surface water.
SOLUTION CHANNELSShall mean tubular or planar channels formed by solution in carbonate rock terrains, usually along joints and bedding planes. These openings may serve as the water-bearing openings in carbonate rocks.
SOLUTION SINKHOLEShall mean a depression formed from the slow dissolution of bedrock.
SPRINGShall mean a place where water naturally flows from rock or soil upon the land or body of surface water.
SUBSIDENCE SINKHOLESShall mean sinkholes formed by the downward settlement of unconsolidated overburden into openings in the underlying, soluble bedrock.
SURFACE RUNOFFShall mean the part of the precipitation that passes over the surface of the soil.
VOIDShall mean an opening in the soil or rock materials.