- Preferred Labelskos:prefLabel
fluvial incised valley (BGU-T)
- URI
- https://pid.geoscience.gov.au/def/voc/ga/GeomorphologySettings/fluvial_incised_valley ↗Go to the persistent identifier link
- Within Vocab
- Marine geomorphology - Part 2 Geomorphology
| Preferred Labelskos:prefLabel | fluvial incised valley (BGU-T) |
|---|---|
| Definitionskos:definition | A type of SUBAERIAL VALLEY; fluvially-eroded, elongate paleotopographic lows that are generally larger than a single channel, and usually develop during a fall in relative sea level and so display abrupt basinward shift of facies at their base. INCISED VALLEY fills typically begin to accumulate during base-level rise (Zaitlin et al., 1994). Cross-shelf and coastal plain (BGU-sT) INCISED VALLEY fills have relatively distinct facies (Wang et al., 2020). Cf. COASTAL INCISED VALLEY |
| Broaderbroader |
fluvial subaerial valley (BGU)
|
| See AlsoseeAlso | Marine geomorphology - Part 2 Geomorphology |
| Is Defined ByisDefinedBy | Marine geomorphology - Part 2 Geomorphology |
Alternate Profiles
Different views and formats:
Alternate Profiles ?Profiles (alternative information views) encoded in various Media Types (HTML, text, RDF, JSON etc.) are available for this resource.