River avulsions and their deposits
R Slingerland, ND Smith - Annu. Rev. Earth Planet. Sci., 2004 - annualreviews.org
▪ Abstract Avulsion is the natural process by which flow diverts out of an established river
channel into a new permanent course on the adjacent floodplain. Avulsions are primarily …
channel into a new permanent course on the adjacent floodplain. Avulsions are primarily …
Anastomosing rivers: a review of their classification, origin and sedimentary products
B Makaske - Earth-Science Reviews, 2001 - Elsevier
Anastomosing rivers constitute an important category of multi-channel rivers on alluvial
plains. Most often they seem to form under relatively low-energetic conditions near a (local) …
plains. Most often they seem to form under relatively low-energetic conditions near a (local) …
Process, form and change in dryland rivers: a review of recent research
S Tooth - Earth-Science Reviews, 2000 - Elsevier
Many of the world's extensive warm dryland regions support numerous, albeit often
infrequently flowing, rivers. Dryland rivers are increasingly a focus of scientific and applied …
infrequently flowing, rivers. Dryland rivers are increasingly a focus of scientific and applied …
Splitting rivers at their seams: bifurcations and avulsion
River bifurcations are critical but poorly understood elements of many geomorphological
systems. They are integral elements of alluvial fans, braided rivers, fluvial lowland plains …
systems. They are integral elements of alluvial fans, braided rivers, fluvial lowland plains …
Wetlands in drylands: geomorphological and sedimentological characteristics, with emphasis on examples from southern Africa
S Tooth, TS McCarthy - Progress in Physical Geography, 2007 - journals.sagepub.com
Wetlands are poorly documented features of many landscapes, and there is often little
understanding of the geomorphological controls on their origin, development and …
understanding of the geomorphological controls on their origin, development and …
The okavango delta
TS McCarthy, WN Ellery - Transactions of the Royal Society of …, 1998 - Taylor & Francis
SUMMARY The Okavango Delta is a large, low gradient (ca. 1: 3400), alluvial fan situated in
a graben structure which is an extension of the East African Rift system. The catchment is …
a graben structure which is an extension of the East African Rift system. The catchment is …
A nonlinear model of flow in meandering submarine and subaerial channels
A generalized model of flow in meandering subaqueous and subaerial channels is
developed. The conservation equations of mass and momentum are depth/layer integrated …
developed. The conservation equations of mass and momentum are depth/layer integrated …
The topography of the Okavango Delta, Botswana, and its tectonic and sedimentological implications
T Gumbricht, TS McCarthy… - South African Journal …, 2001 - pubs.geoscienceworld.org
A topographic map of the Okavango Delta and environs has been constructed using a
combination of elevation data including trigonometric beacons and spot heights from the …
combination of elevation data including trigonometric beacons and spot heights from the …
[PDF][PDF] Regional review: the hydrology of the Okavango Delta, Botswana-processes, data and modelling
C Milzow, L Kgotlhang… - Hydrogeology …, 2009 - research-collection.ethz.ch
The wetlands of the Okavango Delta accommodate a multitude of ecosystems with a large
diversity in fauna and flora. They not only provide the traditional livelihood of the local …
diversity in fauna and flora. They not only provide the traditional livelihood of the local …
Fluvial dynamics of an anabranching river system in Himalayan foreland basin, Baghmati river, north Bihar plains, India
Anabranching river systems are now regarded as a separate class in river classifications
owing to their distinctive morphological/hydrological characteristics and fluvial processes. A …
owing to their distinctive morphological/hydrological characteristics and fluvial processes. A …