{{Short description|Desert landscape with mostly rock instead of sand}} {{Other uses}}

[[File:La hamada noire du Tademayt 1890.jpg|thumb|upright=1.3|Hamada plateau at Tademaït, Algeria. Photograph by French explorer Fernand Foureau during his trans-Saharan journey in 1890.]] [[File:260 Boa Vista.jpg|thumb|Hamada in the interior of the Cape Verde island of Boa Vista.]] [[File:Hoggar-Hammada.jpg|thumb|Hamada desert near the Hoggar Mountains in Algeria.]] [[File:Erg chebbi cyclists.jpg|thumb|Cyclists ride over hamada to the Erg Chebbi dunes, Morocco.]]

A '''hamada''' ({{langx|ar|حمادة}},<!-- Please bring up any changes to the Arabic script on the talk page before changing it on this page --> {{Transliteration|ar|ḥammāda}}) is a type of desert landscape consisting of high, largely barren, hard rocky (basalt) plateaus, where most of the sand has been removed by deflation.<ref name=Springer>{{cite web|url=http://www.springerreference.com/docs/html/chapterdbid/43197.html|title=Hamada, Reg, Serir, Gibber, Saï|publisher=Springer Reference|year=2013|accessdate=2013-05-23}}</ref> The majority of the Sahara is hamada.<ref name=":0">{{Cite web |title=Rocky Desert (Hamada) - Features, Information, Facts |url=https://sand-boarding.com/rocky-desert/ |access-date=2022-07-20 |website=sand-boarding.com|date=27 May 2022 }}</ref> Other examples are Negev desert in Israel and the {{ill|Tinrhert plateau|it|Altopiano del Tinrhert}} in Algeria.<ref name=":0" />

==Formation== Hamadas are produced by the wind, which removes the fine products of weathering, an aeolian process known as deflation. The finer-grained products are taken away in suspension. At the same time, the sand is removed through saltation and surface creep, leaving behind a landscape of gravel, boulders and bare rock.<ref>B.W. Sparks. ''Geomorphology'', 2nd ed., pp. 322-3. Longman Group Ltd. 1972. ({{ISBN|0-582-48147-3}})</ref>

==Related landforms== Hamada is related to desert pavement (known variously as reg, serir, gibber, or saï), which occurs as stony plains or depressions covered with gravels or boulders rather than as highland plateaus.<ref name=Springer/>

Hamadas contrast with ''ergs'', which are large areas of shifting sand dunes.<ref>McKnight, Tom L. and Darrel Hess. ''Physical Geography: A Landscape Appreciation'', 8th ed., pp. 495-6. Upper Saddle River, NJ: Pearson Education, Inc. 2005. ({{ISBN|0-13-145139-1}})</ref>

==References== {{reflist}}

Category:Deserts and xeric shrublands Category:Arabic words and phrases

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