| identifier | http://anzsoil.org/def/au/asls/landform/Channel-pattern | |||||||||||||||||||||
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| definition | In a traverse downstream, it may happen that tributaries enter the stream at frequent intervals, or that the stream splits into distributaries, or that these tendencies are absent (the non-tributary case) or are in balance with each other (the braided or anastomotic case called here reticulated) giving four classes of stream-wise channel pattern. | |||||||||||||||||||||
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