DISCHARGES INTO WETLANDSIncludes, without limitation, any discharge from the project that flows to a wetland resource or buffer zone through new or existing drainage structures, including existing road drainage pipes that empty into wetland resources or buffer zones regardless of the distance between the project site and the wetlands resources or buffer zones.
DISTANCEAll distances noted in the Bylaw (excluding depth), such as buffer zones distances, are planar distances measured along a single elevation. Consequently, on steeply sloped topography the measured over-ground distance may not accurately reflect the distances specified in the permits and conditions specified by the Bylaw. In particular, the 100-foot buffer zone on steeply sloped land will measure considerably more than 100 feet when measured over-ground on site.
EXISTINGAs used in the Bylaw shall mean lawfully existing in full as of the date the regulations were adopted. The term existing shall also include approved Site Plan Reviews permitted under §
3.1 of the Westborough Zoning Bylaws and approved Definitive Subdivision Plans for the construction of roadways and associated utilities but excluding any individual lot development.
FLOOD STORAGE AS AN ALTERATIONThe term 'alter' includes storage of flood waters and stormwater runoff waters in wetlands. Storage of flood waters and stormwater runoff is prohibited unless the Conservation Commission deems that such action would enhance wetland values and functions.
ISOLATED LAND SUBJECT TO FLOODING (ILSF)A. As provided in 310 CMR 10.57(2)(b)1 through 3, the Town of Westborough definition of an Isolated Land Subject to Flooding" . . .is an isolated depression or closed basin without an inlet or an outlet. It is an area which at least once a year confines standing water to a volume of at least 1/4 acre-feet and to an average depth of at least six inches. Isolated Land Subject to Flooding may be underlain by pervious material, which in turn may be covered by a mat of organic peat or muck . . . The boundary of Isolated Land Subject to Flooding is the perimeter of the largest observed or recorded volume of water confined in said area."
B. If there is a question regarding whether the extent of water confined in an ILSF, calculations to determine the volume of standing water shall be based on the total volume (rather than peak rate) of run-off from the drainage area contributing to the ILSF and the assumption that there is no infiltration of said run-off into the soil within the Isolated Land Subject to Flooding as stated in 310 CMR 10.57(2)(b)3.
PARKING LOTAny area, paved or unpaved, that is used for parking, storage, loading or unloading of vehicles or the storage of any item.
PASSIVE PASSAGEConnotes passage by foot for the purposes of passive recreation, as defined above.
RARE SPECIESAs defined in 310 CMR 10.04: "mean those vertebrate and invertebrate animal species officially listed as endangered, threatened, or of special concern by the Massachusetts Division of Fisheries and Wildlife under 321 CMR 10.60."
RECREATIONConnotes passive recreation activities that do not conflict with or diminish other wetland values and functions. Examples include, without limitation, bird watching and other nature studies, walking and hiking, canoeing, and as appropriate fishing, hunting, etc.
STRUCTUREAnything constructed or erected, the use of which requires fixed location on the ground, or attachment to something located on the ground, including swimming pools and mobile homes, but not including retaining walls or similar devices, signs, exterior lighting, pavement or fences. All other activities not constituting a structure shall be subject to setbacks that apply to limits of disturbance as defined in Article
6.
VERNAL POOL SPECIESA vernal pool species is defined in the Division of Fisheries and Wildlife - Natural Heritage and Endangered Species Program's "Guidelines for the Certification of Vernal Pool Habitat" dated March 2009 and any subsequent revisions.
VOLUME OF A DETENTION/RETENTION BASINBasin volume shall be calculated as that volume contained between the basin's one-hundred-year flood elevation and the lowest elevation of the basin floor.