- Preferred Labelskos:prefLabel
mid-channel bar (BGU-T)
- URI
- https://pid.geoscience.gov.au/def/voc/ga/GeomorphologySettings/mid-channel_bar ↗Go to the persistent identifier link
- Within Vocab
- Marine geomorphology - Part 2 Geomorphology
| Preferred Labelskos:prefLabel | mid-channel bar (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 - Part 2 Geomorphology |
| Is Defined ByisDefinedBy | Marine geomorphology - Part 2 Geomorphology |
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