Glossary
This glossary provides non-technical definitions of technical terms, some of which are used in this manual. This is by no means an exhaustive list of all the terminology pertaining to tidal marshes. For more detailed reference to tidal marsh terminology, see the references listed in Section 9 of this manual.
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accretion |
the gradual build up of surface elevations due to the deposition of suspended sediments on the marsh surface |
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aquatic |
in or near water in such habitats as ponds, lakes, rivers and oceans |
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back-barrier marsh |
a marsh that forms in the low-lying area behind a barrier beach formation |
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barrier beach |
an elongated landform created by the deposition of sedimentary materials by wind and wave currents, usually parallel to the shoreline, with water on at least two sides, and composed of sand, gravel, or cobblestones |
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brackish marsh |
tidal marshes where the average water salinity is less than 18 parts per thousand (ppt) but greater than 0.5 ppt, which is the upper limit of salinity in a freshwater tidal wetland |
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buffer zone |
an undeveloped area bordering on a wetland that serves to lessen the impact of disturbance (e.g., urban development) |
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deepwater habitats |
permanently flooded areas deeper than 6.6 feet (e.g., lakes) |
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degraded |
characterized by loss of natural ecological structure or function |
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dominant plant community |
a single species or association of plants that are indicative of the ecology of an area, e.g. in a cattail marsh the dominant plant community is cattails |
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drainage pattern |
the paths followed by surface runoff from precipitation within a watershed |
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ecology |
the study of interactions between living things and their environment |
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ecological integrity |
the natural (undisturbed) quality of an ecosystem |
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ecosystem |
a community of plants and animals and the physical environment they inhabit (such as estuaries and tidal wetlands) which results from the interactions among soil, climate, vegetation, and animal life |
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emergent plant |
erect, rooted, herbaceous plants that can tolerate flooded soil conditions, but not prolonged periods of being completely submerged, these include grasses, sedges, rushes, and rooted aquatic plants; there are two types of emergent plants: |
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estuary |
areas where saltwater from the ocean mixes with freshwater from inland rivers and surface runoff |
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evaluation unit (EU) |
subsection of a tidal marsh delineated by tidal restrictions used as the basic unit for evaluation of the marsh system |
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fill |
material, usually associated with the dredging of a harbor or inlet, placed on the surface of the marsh; the change in elevation caused by the disposal of this material in the marsh can lead to the loss of the area as a functioning tidal marsh |
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freshwater source |
the point of origin of nontidal waters including rivers, streams and surface runoff |
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freshwater tidal marshes |
marshes that are tidally influenced, but where the average water salinity is less than 0.5 parts per thousand |
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geomorphology |
the study of the natural processes involved in the creation of landforms such as tidal marshes and barrier beaches |
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habitat |
the environment in which the requirements of a specific plant or animal are met |
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herbaceous plant |
a non-woody plant with a soft stem (e.g., bulrushes and cattails) |
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high marsh |
areas of tidal marshes that are irregularly flooded (frequently beyond the reach of daily flooding) and are typically dominated by salt hay grass (Spartina patens) |
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hydrology |
the scientific study of the properties, circulation, and distribution of water as it occurs in the atmosphere and at the earth’s surface as streamflow, precipitation, soil moisture, and ground water |
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hydrologic regime |
the frequency and duration of flooding and/or saturation |
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hydroperiod |
the duration of typical flooding/saturation events; in tidal marshes, the hydroperiod can range from daily flooding to irregular flooding (e.g., every few days, weeks, or months); depends on the marsh elevation |
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intertidal emergent |
an erect rooted herbaceous plant growing in the intertidal zone |
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intertidal zone |
areas that are alternately exposed and flooded by tides |
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invasive species |
plant species that, when introduced to an ecosystem, can disturb the natural balance and habitat diversity by invading and dominating the natural tidal marsh plant community, frequently establishing dense monotypic (single species) stands of vegetation |
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low marsh |
areas of marsh that are flooded twice a day and are dominated by saltwater cordgrass (Spartina alterniflora) |
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marine |
relating to ocean environments |
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marsh hydrology |
this term describes (1) the hydrologic pathways such as precipitation, surface runoff, ground water, tidal fluctuations and flooding rivers which transport nutrients to and from wetlands; (2) the water depth; (3) frequency and duration of flooding in tidal marshes |
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marsh peat |
the organic soil formed by the accumulation of dead marsh plant material and trapped sediments from tidal waters |
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marsh restoration |
improvement of existing marsh condition by reversing some of the adverse impacts caused by coastal development |
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marsh system |
an area of marsh associated with a single opening to the ocean, a single freshwater input, or adjacent to and contiguously along the shore of a tidal river or bay |
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mitigation |
activities taken to minimize or offset wetland impacts due to development or construction. Restoration and enhancement of existing wetlands or creation of new wetlands are forms of impact mitigation |
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non point source |
a pollution source that does not come from a single point. Typical non-point sources include parking lots, roads, and agricultural fields |
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open water |
areas within or adjacent to a marsh that are below mean low water and greater than 100 meters wide (330 feet); this manual uses an arbitrary division of 100 meters to distinguish between open water and tidal creeks |
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organic matter |
a combination of decayed and decaying plant and animal residue |
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overland flow |
a term to describe the sheet-like flow of water over a land surface, not concentrated in individual channels; usually associated with areas of low infiltration such as paved surfaces or surfaces lacking vegetation (see also surface runoff) |
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pannes |
shallow ponds that form on the surface of the marsh and hold salt water between tides |
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point source |
a pollution source that comes from an identifiable point, such as a factory discharge pipe or septic system outlet |
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primary consumer |
animals that eat plant material as their main source of energy |
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sea level |
the level of the surface of the ocean at its mean (average) position between high and low tide |
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sheet flow |
unchannelized flow of water across the surface of a marsh or upland |
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subsidence |
a sinking of the marsh surface, through compaction and degradation of marsh peat; often occurs when Spartina patens is deprived of tidal flow |
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spit |
a small point of land, especially sand or gravel, formed by the deposition of material by wind and water currents that runs into a body of water |
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spring high tide |
tides associated with the full and new moon that are higher and lower than the average tide |
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staddle |
a structure consisting of numerous pilings driven into the marsh on which to stack salt hay to keep it above the tidewaters until it could be hauled off |
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substrate |
the type of bottom sediments such as sand, gravel, peat |
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surface runoff |
the movement of water over the land surface (usually in defined channels), resulting from rainfall or snowmelt; percentage of precipitation that becomes runoff varies depending on the slope of the area, the degree of soil saturation, amount of vegetated coverage, or type of surface e.g. paved areas |
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tidal amplitude |
the variations in the height of tides caused by the lunar cycle, elevation above sea level, the barometric pressure, tidal restrictions and the seasons |
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tidal creeks |
streams in the tidal marsh that are less than 100 meters wide at mean low water and whose main source of water is dominated by tidal action |
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tidal flats |
areas that are irregularly exposed and are devoid of emergent vegetation, also called mud flats or unconsolidated bottom |
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transition zone |
area surrounding a wetland where conditions gradually change from wetland biota to upland biota |
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turbidity |
the clarity of the water column as determined by the presence of suspended particles making the water cloudy |
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upland islands |
areas of upland soils and vegetation located within a tidal marsh |
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vegetated tidal marsh |
marshes dominated by emergent vegetation and influenced by the tides |
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watershed wetlands |
the area from which all water including precipitation, streams and rivers drain to a single point those areas that are inundated or saturated by surface or ground water, support a prevalence of vegetation adapted to life in saturated conditions (i.e., hydrophytes), and are characterized by hydric soils; these include bogs, marshes, swamps, wet meadows, and similar areas |
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Zone of Influence |
area surrounding a wetland in which the activities that take place have an impact on the wetland; the Maine Citizens Tidal Marsh Guide considers a 1/2 mile Zone of Influence, with particular focus on activities within the 250 foot shoreland Zone |