Portal:Wetlands
Introduction
A wetland is a land area that is saturated with water, either permanently or seasonally, such that it takes on the characteristics of a distinct ecosystem. The primary factor that distinguishes wetlands from other land forms or water bodies is the characteristic vegetation of aquatic plants, adapted to the unique hydric soil. Wetlands play a number of roles in the environment, principally water purification, flood control, carbon sink and shoreline stability. Wetlands are also considered the most biologically diverse of all ecosystems, serving as home to a wide range of plant and animal life. Wetlands occur naturally on every continent except Antarctica, the largest including the Amazon River basin, the West Siberian Plain, and the Pantanal in South America. The water found in wetlands can be freshwater, brackish, or saltwater. The main wetland types include swamps, marshes, bogs, and fens; and sub-types include mangrove, carr, pocosin, and varzea.
The UN Millennium Ecosystem Assessment determined that environmental degradation is more prominent within wetland systems than any other ecosystem on Earth. International conservation efforts are being used in conjunction with the development of rapid assessment tools to inform people about wetland issues.
Constructed wetlands can be used to treat municipal and industrial wastewater as well as stormwater runoff and they also play a role in water-sensitive urban design.
Selected article
River deltas form when a river carrying sediment reaches either (1) a body of standing water, such as a lake, ocean, or reservoir, (2) another river that cannot remove the sediment quickly enough to stop delta formation, or (3) an inland region where the water spreads out and deposits sediments. The tidal currents also cannot be too strong, as sediment would wash out into the water body faster than the river deposits it. Of course, the river must carry enough sediment to layer into deltas over time. The river's velocity decreases rapidly, causing it to deposit the majority, if not all, of its load. This alluvium builds up to form the river delta. When the flow enters the standing water, it is no longer confined to its channel and expands in width. This flow expansion results in a decrease in the flow velocity, which diminishes the ability of the flow to transport sediment. As a result, sediment drops out of the flow and deposits. Over time, this single channel builds a deltaic lobe (such as the bird's-foot of the Mississippi or Ural river deltas), pushing its mouth into the standing water. As the deltaic lobe advances, the gradient of the river channel becomes lower because the river channel is longer but has the same change in elevation (see slope). (Full article...)
General images
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Vernal pools are ponded only during the wetter part of the year. (from Marsh) -
Bog with October morning mist in Mukri, Estonia (from Bog) -
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Marsh in shallow water on a lakeshore (from Marsh) -
The wetlands of Cape May, New Jersey, U.S. comprise an extensive hydrological network that makes them an ornithologically important location to study the many birds which use the preserve as a place to nest. (from Wetland) -
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Difference between swamp and marsh (from Swamp)
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Small extreme rich fen in southwestern Minnesota. The white flowers, Parnassia glauca, are a fen indicator species in Minnesota. (from Fen) -
Fog rising over the Mukri bog near Mukri, Estonia. The bog has an area of 2,147 hectares (5,310 acres) and has been protected since 1992. (from Wetland)
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Avaste Fen, Estonia. Sedges dominate the landscape, woody shrubs and trees are sparse. (from Fen) -
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Marshlands are often noted within wetlands, as seen here at the Jamaica Bay Wildlife Refuge in New York City. (from Wetland) -
Precipitation accumulates in many bogs, forming bog pools, such as Koitjärve bog in Estonia. (from Bog) -
Bud of water lotus (Nelumbo nucifera), an aquatic plant. (from Wetland) -
Wetland at the Broadmoor Wildlife Sanctuary in Massachusetts, United States, in February (from Wetland) -
Marshlands are often noted within wetlands, as seen here in the New Jersey Meadowlands at Lyndhurst, New Jersey, U.S. (from Marsh) -
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Sunrise at Viru Bog, Estonia (from Wetland) -
Sugar Fen, Norfolk (from Fen) -
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Spaulding Fen, Wisconsin. (from Fen) -
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Marsh Arabs poling a mashoof (from Swamp) -
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Many kinds of birds nest in marshes; this one is a yellow-headed blackbird. (from Marsh) -
Many species of evergreen shrub are found in bogs, such as Labrador tea. (from Bog) -
A bog in Ostfriesland (from Bog) -
Sphagnum moss and sedges can produce floating bog mats along the shores of small lakes. This bog in Duck Lake, Oregon, US, supports populations of English sundew (Drosera anglica). (from Bog) -
A raised bog in Ķemeri National Park, Jūrmala, Latvia, formed approximately 10,000 years ago in the postglacial period and now a tourist attraction. (from Bog) -
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Snapping turtles are one of the many kinds of turtles found in wetlands. (from Wetland) -
Aerial view of prairie potholes (from Marsh) -
Wicken Fen, England. Grasses in the foreground are typical of a fen. (from Fen) -
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A small swamp in Padstow, New South Wales, Australia (from Swamp) -
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Wetlands contrast the hot, arid landscape around Middle Spring, Fish Springs National Wildlife Refuge, Utah (from Wetland) -
An expanse of wet Sphagnum bog in Frontenac National Park, Quebec, Canada. Spruce trees can be seen on a forested ridge in the background. (from Bog) -
Dernford Fen, Cambridgeshire (from Fen) -
Humid wetland in Pennsylvania before a rain. (from Wetland) -
White water lilies are a typical marsh plant in European areas of deeper water. (from Marsh) -
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Carnivorous plants, such as this Sarracenia purpurea pitcher plant of the eastern seaboard of North America, are often found in bogs. Capturing insects provides nitrogen and phosphorus, which are usually scarce in such conditions. (from Bog) -
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Kakerdaja Fen, Estonia (from Fen) -
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Categories
Related portals
Organizations
- America's Wetland Foundation
- Birds Korea
- Delta Waterfowl Foundation
- Ducks Unlimited
- Foundation for Ecological Security
- Irish Peatland Conservation Council
- National Wetlands Coalition
- Theodore Roosevelt Conservation Partnership
- Union Sportsmen's Alliance
- Wetlands International
- Wildfowl & Wetlands Trust
Topics
- Acrotelm
- Aquatic ecosystem
- Aquatic plants
- Atchafalaya Basin
- Backswamp
- Bayou
- Beach meadow
- Blackwater river
- Blanket bog
- Bog
- Bog bodies
- Bog butter
- Bog garden
- Bog iron
- Bog snorkelling
- Bog-wood
- Brackish marsh
- Callows
- Carr (landform)
- Cataract bog
- Cienega
- Coniferous swamp
- Converted wetland
- Dambo
- Drainage basin
- Drought refuge
- Estuary
- Everglades
- Fen
- Fen-meadow
- Flark
- Flooded grasslands and savannas
- Flood-meadow
- Floodplain
- Freshwater swamp forest
- Grass valley
- Guelta
- Halosere
- High Fens
- High marsh
- Hamuns
- Hydric soil
- Hydrology
- Hydrosere
- Igapó
- Ings
- Integrated constructed wetland
- Interdunal wetland
- Intertidal wetland
- Kettle (landform)
- Lagoon
- Lake ecosystem
- Limnology
- List of bogs
- List of fen plants
- Low marsh
- Meadowview Biological Research Station
- Marsh
- Marsh gas
- Mere
- Mire
- Misse
- Moorland
- Muck
- Mudflat
- Muskeg
- Myristica swamp
- Oasis
- Ombrotrophic
- Paludification
- Palustrine wetland
- Pantanal
- Peat
- Peat swamp forest
- Pond
- Pothole
- Prairie Pothole Region
- Ramsar site
- Reed bed
- Restoration of the Everglades
- Riparian zone
- River delta
- River ecosystem
- Salt marsh
- Salt marsh dieback
- Salt marsh die-off
- Salt pannes and pools
- Shrub swamp
- Slough (hydrology)
- Sphagnum
- String bog
- Sudd
- Swale
- Swamp
- Tropical peat
- Várzea forest
- Vernal pool
- Water stagnation
- Wetland classification
- Wetland conservation
- Wetland indicator status
- Wetland methane emissions
- Wetlands International
- Wetlands
- Wildfowl & Wetlands Trust
- Will-o'-the-wisp
- Yaéré
| Large-scale features | |
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| Alluvial rivers | |
| Bedrock river | |
| Bedforms | |
| Regional processes | |
| Mechanics | |
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