Mudflats or mud flats, also known as tidal flats, are coastal wetlands that form when mud is deposited by tides or rivers. They are found in sheltered areas such as bays, bayous, lagoons, and estuaries. Mudflats may be viewed geologically as exposed layers of bay mud, resulting from deposition of estuarine silts, clays and marine animal detritus. Most of the sediment within a mudflat is within the intertidal zone, and thus the flat is submerged and exposed approximately twice daily.
In the past tidal flats were considered unhealthy, economically unimportant areas and were often dredged and developed into agricultural land. Several especially shallow mudflat areas, such as the Wadden Sea, are now popular among those practising the sport of mudflat hiking.
On the Baltic Sea coast of Germany in places, mudflats are exposed not by tidal action, but by wind-action driving water away from the shallows into the sea. These wind-affected mudflats are called windwatts in German.
Tidal flats, along with intertidal salt marshes and mangrove forests, are important ecosystems. They usually support a large population of wildlife, and are a key habitat that allows tens of millions of migratory shorebirds to migrate from breeding sites in the northern hemisphere to non-breeding areas in the southern hemisphere. They are often of vital importance to migratory birds, as well as certain species of crabs, mollusks and fish. In the United Kingdom mudflats have been classified as a Biodiversity Action Plan priority habitat.
The maintenance of mudflats is important in preventing coastal erosion. However, mudflats worldwide are under threat from predicted sea level rises, land claims for development, dredging due to shipping purposes, and chemical pollution.
Mudflat sediment deposits are focused into the intertidal zone which is composed of a barren zone, marsh and salt pan. Within these areas are various ratios of sand and mud that make up the sedimentary layers. The associated growth of coastal sediment deposits can be attributed to rates of subsidence along with rates of deposition (example: silt transported via river) and changes in sea level.
Barren zones extend from the lowest portion of the intertidal zone to the marsh areas. Beginning in close proximity to the tidal bars, sand dominated layers are prominent and become increasingly muddy throughout the tidal channels. Common bedding types include laminated sand, ripple bedding, and bay mud. Bioturbation also has a strong presence in barren zones.
Marshes contain an abundance of herbaceous plants while the sediment layers consist of thin sand and mud layers. Mudcracks are a common as well as wavy bedding planes. Marshes are also the origins of coal/peat layers because of the abundant decaying plant life.
Salt pans can be distinguished in that they contain thinly laminated layers of clayey silt. The main source of the silt comes from rivers. Dried up mud along with wind erosion forms silt dunes. When flooding, rain or tides come in, the dried sediment is then re-distributed.
Selected example areas
- Arcachon Bay, France
- Banc d'Arguin, Mauritania
- Great Rann of Kutch, India
- Belhaven, East Lothian Scotland, United Kingdom
- Bridgwater Bay and Morecambe Bay, United Kingdom
- Cape Cod Bay, Massachusetts, United States
- Cook Inlet, Alaska, United States
- Lindisfarne Island, England, United Kingdom
- Minas Basin, Nova Scotia, Canada
- Padilla Bay, Washington, United States
- Plymouth Bay, Massachusetts, United States
- Port of Tacoma, Washington, United States
- Skagit Bay, Washington
- Snettisham Norfolk England, United Kingdom
- Wadden Sea: Netherlands, Germany, Denmark
- West coast of Andros Island, Bahamas
- Yellow Sea, China, Korea
- Moreton Bay, Queensland, Australia
- Dredging Indian River Lagoon Wetlands 1920 - 1950s
- Tidal flat habitats
- Mud crab (Scylla serrata) culture in tidal flats with existing mangroves
- Manko - Tidal Flat, Mangrove Forest
- Reineck, H.E, and I.B Singh, Deposistional Sedimentary Enviornments, 2nd Ed. New York: Springer-Verlag Berlin Heidelberg, 1980, pp. 418-428
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