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Vivari Channel in Albania links Lake Butrint with the Straits of Corfu. In physical geography and hydrology, a channel is a landform on which a relatively narrow body of water is situated, such as a river, river delta or strait. While channel typically refers to a natural formation, the cognate term canal denotes a similar artificial structure.
Blowhole – Hole at the top of a sea-cave which allows waves to force water or spray out of the hole; Channel – Narrow body of water; Cape – Large headland extending into a body of water, usually the sea; Calanque – Narrow inlet on the Mediterranean coast; Cliff – Tall, near vertical rock face; Coast – Area where land meets the sea ...
Channel patterns are found in rivers, streams, and other bodies of water that transport water from one place to another.Systems of branching river channels dissect most of the sub-aerial landscape, each in a valley proportioned to its size.
Many guts are straits but some are at a river mouths where tidal currents are strong. The comparatively large quantities of water that flow quite quickly through a gut can cause heavy erosion that results in a channel deeper than the rest of the surrounding seabed, and the currents may present a hazard to ships and boats at times.
Water tends to be stagnant or may flow slowly on a seasonal basis. [5] In North America, "slough" may refer to a side-channel from or feeding a river, or an inlet or natural channel only sporadically filled with water. [3] An example of this is Finn Slough on the Fraser River, whose lower reaches have dozens of notable sloughs.
A wide variety of river and stream channel types exist in limnology, the study of inland waters.All these can be divided into two groups by using the water-flow gradient as either low gradient channels for streams or rivers with less than two percent (2%) flow gradient, or high gradient channels for those with greater than a 2% gradient.
Angular cheilitis typically starts with a red dry patch on the corners of the mouth. It can be on one or both sides, with a dry, scaly appearance, according to the Cleveland Clinic.
Where the new channel's slope is about the same as the old channel's slope, a partial avulsion will occur in which both channels are occupied by flow. [9] An example of an erosional avulsion is the 2006 avulsion of the Suncook River in New Hampshire , in which heavy rains caused flow levels to rise.
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