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These channels are classified as a composite form of which the individual channel belts may have braided, meandering or straight channels. Although similar to, and even encompass other channel types, anastomosed rivers are their own entity and have just begun to be studied by geologists , revealing that much is still unknown.
Tom Davies (born 22 September 1990 [2] [3] [4]), known online as GeoWizard, is a British YouTuber and adventurer known for his skill in playing the internet geography game GeoGuessr and his "straight line mission" adventures, in which he attempts to cross regions on foot in as close to a straight line as possible.
This is a list of notable successful swims across the English Channel, [1] a straight-line distance of at least 18.2 nautical miles (20.9 mi; 33.7 km). [2] Aerial view of the Strait of Dover Ted Heaton (in water) being fed by assistants during his 1910 swim Monument in Dover to Channel swimmers
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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.
Direct-to-video or straight-to-video refers to the release of a film, television series, short or special to the public immediately on home video formats rather than an initial theatrical release [1] or television premiere. This distribution strategy was prevalent before streaming platforms came to dominate the TV and movie distribution markets.
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.
A subglacial meltwater channel is a channel beneath an ice mass, such as ice sheets and valley glaciers, roughly parallel to the main ice flow direction.These meltwater channels can have different sizes, ranging from very small channels of a metre deep and wide to big valleys which can be up to a kilometre wide.