Mudflats or mud flats, also known as tidal flats or, in Ireland, slob or slobs, [1][2] are coastal wetlands that form in intertidal areas where sediments have been deposited by tides or rivers.

2017年4月25日 · Also known as tidal flats, mudflats are formed upon the deposition of mud by tides or rivers. This coastal landform usually occurs in sheltered areas of the coast like bays, coves, lagoons, estuaries, etc.

Mudflats, or otherwise known as tidal flats, are coastal wetlands that form when mud is left behind by tides or rivers. They’re found in sheltered regions such as bayous, lagoons, estuaries, and bays. Mudflats might be seen geologically as exposed layers of bay mud, a result from :

2017年12月8日 · Mudflats form when silt and mud are brought in by seas, oceans, and tributaries. The mud and the silt are deposited into bays and lagoons when the tide comes in. The water mixes with the mud and silt, creating the muddy quicksand that occurs in mudflats. Once the tide lowers, the mudflats are exposed along with what inhabits them.

MUDFLAT definition: 1. a flat area of very wet soil near the sea that is covered at high tide (= the time when the sea…. Learn more.

In coastal areas sheltered from waves, slow-moving tides gently lap over a flat expanse of fine mud. Covered at high tide and exposed during low tide, mudflats support a wealth of life; bristle worms, bivalves and mud snails - all food for flocks of wading birds.

A mud flat is defined as the upper zone of tidal flats where depositional processes are dominated by the fallout of suspended sediment, including sortable silts, flocs, and aggregates. It is characterized by intense bioturbation and the presence of various biogenic structures. You might find these chapters and articles relevant to this topic.