For the purposes of this chapter, the following definitions shall apply:
APPROVING AUTHORITYThe Board constituted pursuant to the Municipal Land Use Law, N.J.S.A. 40:55D-1 et seq., which, for applications involving site plan or subdivision approval, is the Planning Board or Zoning Board of Adjustment of this township.
APPLICABLE DEVELOPMENT ACTIVITY or ACTIVITIESDevelopment (as defined in the Municipal Land Use Law) in the Carbonate Rock District which requires major subdivision or major site plan approval under Chapter
64, Development Regulations, of this Code.
BEDDINGThe arrangement of a sedimentary rock in layers of varying thickness and character.
BEDROCKA general term for the rock that underlies soil or other unconsolidated material.
CARBONATE ROCKRock consisting chiefly of calcium and magnesium carbonates.
CARBONATE ROCK DISTRICTThose land areas underlain by carbonate rock formation, as shown on the Washington Township Carbonate Rock District Map, annexed to this chapter as an appendix. (Additional information regarding land areas underlain by carbonate rock, as an aid to interpreting the map, can be gained from the New Jersey Geological Survey's Warren County Geology Map, found in a publication entitled "Environmental Geology of Warren County, New Jersey," by G.C. Herman et al [Open File Map 15B, NJGS, 1994]).
CLOSED DEPRESSIONA shallow, dish-shaped hollow on the land surface which, in area of limestone geology, may be indicative of old sinkholes or incipient collapse.
DISAPPEARING STREAMA stream that enters the subsurface through a sinkhole or other surface entrance.
DOLOMITEA carbonate rock that contains more than 15% magnesium carbonate.
FAULTA surface or zone of rock fracture along which there has been noticeable differential movement.
GEOTECHNICAL INVESTIGATION PROGRAMA program which identifies the geologic nature of the bedrock materials underlying a site and provides solutions directed at preserving the water quality and assuring the safety of any planned facility or improvement built over carbonate rocks.
JOINTA fracture in rock, generally more or less vertical or transverse to bedding, along which no appreciable movement has occurred.
KARSTA type of topography that is formed over limestone or dolomite by dissolving or solutioning of the carbonate rocks, characterized by sinkholes, closed depressions, caves, solution channels, internal drainage and irregular bedrock surfaces.
LIMESTONEA carbonate sedimentary rock consisting chiefly of calcium carbonate. Limestone is commonly used as a general term for that class of rocks which consists of at least 80% calcium or magnesium carbonate. In this chapter, the term "limestone" shall be used generically to refer to carbonate rocks, limestone formations and Precambrian marbles.
SINKHOLE (DOLINE)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.
SOLUTION CHANNELSTubular or planar channels formed by solution in carbonate rock terrains, usually along joints and bedding planes. These openings are the main water carrier in carbonate rocks.
VOIDOpening in the soil or rock materials.