As used in this article, the following terms shall have the meanings indicated:
BUFFERThe protected upland areas adjacent to wetlands and surface waters in the Conservation Overlay District other than the wetlands themselves.
ORDINARY HIGH-WATER MARKThe line on the shore, running parallel to the main stem of the river, established by the fluctuations of water and indicated by physical characteristics such as a clear, natural line impressed on the immediate bank, shelving, changes in the character of soil, destruction of soil, destruction of terrestrial vegetation, the presence of litter and debris, or other appropriate means that consider the characteristics of the surrounding areas. Where the ordinary high-water mark is not easily discernible, the ordinary high-water mark may be determined by the Department of Environment Services. Source: Comprehensive Shoreland Protection Act, page 7 from the State of New Hampshire web page, 1998.
OVERLAY DISTRICTA zoning district superimposed on one or more established underlying zoning districts to impose supplemental restrictions on uses in these districts.
POORLY DRAINED SOILAs defined by high-intensity soil maps for New Hampshire sponsored by the Society of Soil Scientists of Northern New England Special Publication No. 1, September 2002.
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VERNAL POOLSA. Temporary bodies of water that flood each year for a few months during the spring and summer. Vernal or "spring" pools fill up with melting snow and early rains, then usually dry up by mid to late summer. Some relatively deep pools may remain flooded for a few years but become completely dry in seasons with very low rainfall. Autumnal pools fill during the fall with rising groundwater.
B. Because vernal pools are not permanently flooded, they do not support fish populations and thus provide safe breeding sites for several amphibian and invertebrate species, including wood frogs, spotted salamanders, and fairy shrimp. These species have evolved life cycles that depend on temporary pools.
C. Vernal pools vary in size, ranging from several square feet to several acres. They can be found in a variety of sites, such as isolated depressions in the woods, kettle holes, and gravel pits. Many are within larger wetlands, such as oxbows in river floodplains and pools in forested swamps or scrub-shrub wetlands. Their common characteristics are the absence of fish, temporary flooding regime, and the presence of vernal pool species. Suitable pools must have enough leaf litter and other debris to provide food sources and cover for the species that breed in them. Source: ASNH Conservation Fact Sheet: Vernal Pools.
VERY POORLY DRAINED SOILAs defined by high-intensity soil maps for New Hampshire sponsored by the Society of Soil Scientists of Northern New England Special Publication No. 1, September 2002.
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WETLANDAs defined by the National Food Security Act Manual (Soil Conservation Service, 1994) and the Corps of Engineers Wetlands Delineation Manual (1987) and the most recent version of the Regional Supplement to the Corp of Engineers Wetland Delineation Manual: Northcentral and Northeast Region, those areas that are inundated or saturated by surface water or groundwater at a frequency and duration sufficient to support, and that under normal circumstances do support, a prevalence of vegetation typically adapted for a life in saturated soil conditions. Wetlands include, but are not limited to, swamps, marshes, bogs and similar areas.
[Amended 3-5-2019]