General morphology and processes
Wadis are located on gently sloping, nearly flat parts of deserts; commonly they begin on the distal portions of alluvial fans
and extend to inland sabkhas
or dry lakes
. In basin and range topography
, wadis trend along basin axes at the terminus of fans. Permanent channels do not exist, due to lack of continual water flow. Wadis have braided stream
patterns because of the deficiency of water and the abundance of sediments
. Water percolates down into the stream bed, causing an abrupt loss of energy and resulting in vast deposition. Wadis may develop dams of sediment that change the stream patterns in the next flash flood
Wind also causes sediment deposition. When wadi sediments are underwater or moist, wind sediments are deposited over them. Thus, wadi sediments contain both wind and water sediments.
Sediments and sedimentary structures
Wadi sediments may contain a range of material, from gravel to mud, and the sedimentary structures vary widely. Thus, wadi sediments are the most diverse of all desert environments.
Flash floods result from severe energy conditions and can result in a wide range of sedimentary structures, including ripples and common plane beds. Gravels commonly display imbrications
, and mud drapes show desiccation cracks. Wind activity also generates sedimentary structures, including large-scale cross-stratification and wedge-shaped cross-sets. A typical wadi sequence consists of alternating units of wind and water sediments; each unit ranging from about 10–30 cm (3.9–11.8 in). Sediment laid by water shows complete fining upward sequence. Gravels show imbrication. Wind deposits are cross-stratified and covered with mud-cracked deposits. Some horizontal loess
may also be present.
Modern English usage differentiates wadis from canyons
by the action and prevalence of water. Wadis, as drainage courses, are formed by water, but are distinguished from river valleys or gullies in that surface water is intermittent or ephemeral. Wadis are generally dry year round, except after a rain. The desert environment is characterized by sudden but infrequent heavy rainfall, often resulting in flash floods
. Crossing wadis at certain times of the year can be dangerous as a result.
Wadis tend to be associated with centers of human population because sub-surface water is sometimes available in them. Nomadic and pastoral desert peoples will rely on seasonal vegetation found in wadis, even in regions as dry as the Sahara
, as they travel in complex transhumance
The centrality of wadis to water — and human life — in desert environments gave birth to the distinct sub-field of wadi hydrology in the 1990s.
Deposition in a wadi is rapid because of the sudden loss of stream velocity
and seepage of water into the porous sediment. Wadi deposits are thus usually mixed gravels and sands. These sediments are often altered by eolian
Over time, wadi deposits may become "inverted wadis," where former underground water caused vegetation and sediment to fill in the eroded channel, turning previous washes into ridges running through desert regions.
Dry fluvial channel cutting through columnar basalt
, southern Africa
- Alluvial desert – A desert surface covered with closely packed, interlocking angular or rounded rock fragments of pebble and cobble size.
- Arroyo (creek) – A dry creek or stream bed with flow after rain
- Canyon – Deep ravine between cliffs
- Coulee – Type of valley or drainage zone
- Gulch – Deep V-shaped valley formed by erosion
- Gully – Landform created by running water eroding sharply into soil
- Oasis – Isolated source of fresh water in a desert
- Wād Ṭuwā in the Sinai peninsula, holy Muslim site
- ^ "Torrent valley". Insight on the Scriptures. Volume 2: Jehova - Zuzim and Index. Watch Tower Bible and Tract Society of New York. 1988. p. 1115. The term “wadi” (Arabic) is also used to designate a torrent valley ... whereas others are torrents during the rainy season but dry up completely during the rainless season.
- ^ Ayuntamiento de Guadalajara, Guadalajara tourist guide, p.5. Archived 1 July 2012 at the Wayback Machine, retrieved 17 August 2013
- ^ Review of Wheater, Howard ; Al Weshah, Radwan, Hydrology of Wadi systems -IHP Regional Network on Wadi Hydrology in the Arab Region, UNESCO - Technical documents in hydrology vol 55, SC.2002/WS/33,(2002).
- ^ Achite, Mohamed; Ouillon, Sylvain (September 2007). "Suspended sediment transport in a semiarid watershed, Wadi Abd, Algeria (1973–1995)". Journal of Hydrology. 343 (3–4): 187–202. Bibcode:2007JHyd..343..187A. doi:10.1016/j.jhydrol.2007.06.026.
- ^ Alimsk (20 December 2013). "Wadi Bani Khalid & Wadi Hawer". Oman Tripper. Retrieved 25 March 2018.
- ^ Pedro. "Visiting Wadi Bani Khalid, Oman: A Desert Paradise". Travel With Pedro. Retrieved 25 March 2018.
- Summary: Drainage Courses, Wadis. United States Army Corps of Engineers. Desert Processes Working Group; Knowledge Sciences, Inc. (n.d), retrieved 2008-08-26.
- Summary: Summary: Drainage Courses, Wadis - Inverted. United States Army Corps of Engineers. Desert Processes Working Group; Knowledge Sciences, Inc. (n.d), retrieved 2008-08-2onments
- Gelennie, K. W., 1970 Deserts sedimentary Environments. Developments in Sedimentology, v.14. Elsevier, Amsterdam, 222p.
Wikimedia Commons has media related to Wadis
Look up wadi
in Wiktionary, the free dictionary.
Last edited on 10 June 2021, at 12:05
Content is available under CC BY-SA 3.0
unless otherwise noted.