- Preferred Labelskos:prefLabel
mid-channel (BGU-T)
- URI
- https://pid.geoscience.gov.au/def/voc/ga/GeomorphologySettings/mid-channel ↗Go to the persistent identifier link
- Within Vocab
- Marine Geomorphology - Geomorphology Settings and Processes (Part 2)
Preferred Labelskos:prefLabel | mid-channel (BGU-T) |
---|---|
Definitionskos:definition | Most common in actively meandering channels and tend to develop in steeper channel sections downstream of rapidly eroding bends where the channel is overwidened, and though they have lower preservation potential (Goudie, 2006) they may evolve towards bank attachment (Hooke, 1986; Alabyan and Chalov, 1998). Cf BANK-ATTACHED BARS. |
Broaderbroader |
barform (BGU)
|
See AlsoseeAlso | Marine Geomorphology - Geomorphology Settings and Processes (Part 2) |
Is Defined ByisDefinedBy | Marine Geomorphology - Geomorphology Settings and Processes (Part 2) |
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