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[[File:Meander-en.svg|Meander-en|thumb]] [[File:rio-cauto-cuba.JPG|rio-cauto-cuba|thumb|left]] [[File:Zoltan_Kluger._The_Jordan,_near_the_Dead_Sea.jpg|Zoltan Kluger. The Jordan, near the Dead Sea|thumb|left]] [[File:Bend2.png|Bend2|thumb]] [[File:Meandri_uvca.jpg|Meandri uvca|thumb]] [[File:The_Carstairs_meanders_from_the_air_(geograph_5676421).jpg|The Carstairs meanders from the air (geograph 5676421)|thumb]] '''Meander''' refers to a winding curve or bend in a [[river]], [[stream]], or other type of [[watercourse]]. It is a feature of [[fluvial geomorphology]], which is the study of the processes shaping rivers and the landscapes through which they flow. Meanders form as a result of varying water flow velocity within the river channel, typically in the middle and lower courses of a river where the gradient has decreased sufficiently to allow for the deposition of sediments and the lateral migration of the river channel.

==Formation==
The formation of meanders is primarily due to the process of [[lateral erosion]] and deposition. As water flows through a river channel, it tends to erode the outer banks where velocity is higher due to the greater length of the curve, and deposit sediments on the inner banks where velocity is lower. This process, known as [[helical flow]], results in the distinctive sinuous pattern of a meandering river. Over time, meanders can become more pronounced due to the feedback mechanism where erosion and deposition further exaggerate the curvature of the river.

==Features==
Meanders are characterized by several distinct features:
* '''Point bar''': A deposit of sediment on the inner bank of a meander, formed by the slower flow of water which can carry less sediment.
* '''Cut bank''': The outer bank of a meander, which is subject to erosion by the faster-flowing water.
* '''Oxbow lake''': A crescent-shaped lake formed when a meander is cut off from the main river channel, often as a result of the river finding a shorter, more direct course through the deposition of sediments.
* '''Meander scar''': An isolated remnant of a former meander loop, identifiable as an indented mark on the landscape after an oxbow lake has dried up or been filled in.

==Types of Meanders==
Meanders can vary significantly in size and complexity, from simple single loops to complex networks of intertwined loops known as [[braided rivers]]. The specific characteristics of a meander depend on a variety of factors, including the volume and speed of water flow, the composition and erodibility of the riverbanks, and the slope of the surrounding terrain.

==Ecological and Geographical Significance==
Meanders play a crucial role in shaping the [[ecosystem]]s and [[geography]] of their surrounding landscapes. They contribute to the diversity of [[habitat]]s in riverine environments, supporting a wide range of [[species]]. The dynamic nature of meanders, with their continual process of erosion and deposition, creates a mosaic of habitats that can support high levels of biodiversity.

Furthermore, meanders are significant in [[human geography]] and [[history]]. Many civilizations have developed and thrived along meandering rivers, utilizing the fertile lands for agriculture and the rivers for transportation, water supply, and as natural defenses.

==Conservation==
The conservation of meandering rivers is important for maintaining [[biodiversity]], [[water quality]], and the health of aquatic and riparian ecosystems. Human activities, such as the construction of levees, dams, and channels, can alter the natural flow of rivers, leading to the loss of meanders and associated habitats. Efforts to restore meanders involve re-establishing the river's natural flow patterns, which can help to revive ecosystems and improve water quality.

[[Category:Geomorphology]]
[[Category:Hydrology]]
[[Category:River morphology]]
{{geography-stub}}

Meander - Revision history

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