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{{Short description|Elevated area of land with a flat top and sides}}{{About|the geological formation|other uses}}File:Over Monument Valley, Navajo Nation.jpg|thumb|Aerial view of mesas in Monument Valley, on the Colorado PlateauColorado PlateauA mesa is an isolated, flat-topped elevation, ridge or hill, which is bounded from all sides by steep escarpments and stands distinctly above a surrounding plain. Mesas characteristically consist of flat-lying soft sedimentary rocks capped by a more resistant layer or layers of harder rock, e.g. shales overlain by sandstones. The resistant layer acts as a caprock that forms the flat summit of a mesa. The caprock can consist of either sedimentary rocks such as sandstone and limestone; dissected lava flows; or a deeply eroded duricrust. Unlike plateau, whose usage does not imply horizontal layers of bedrock, e.g. Tibetan Plateau, the term mesa applies exclusively to the landforms built of flat-lying strata. Instead, flat-topped plateaus are specifically known as tablelands.Duszyński, F., Migoń, P. and Strzelecki, M.C., 2019. Escarpment retreat in sedimentary tablelands and cuesta landscapes–Landforms, mechanisms and patterns. Earth-Science Reviews,' no. 102890. doi.org/10.1016/j.earscirev.2019.102890Migoń, P., 2004a. Mesa. In: Goudie, A.S. (Ed.), Encyclopedia of Geomorphology. Routledge, London, pp. 668. {{ISBN|9780415272988}}Neuendorf, Klaus K.E. Mehl, James P., Jr. Jackson, Julia A.. (2011). Glossary of Geology (5th Edition). American Geosciences Institute. {{ISBN|9781680151787}}File:Cockburn Range.jpg|thumb|Cockburn Range, Kimberley, Western AustraliaWestern Australia

Names, definition and etymology

As noted by geologist Kirk Bryan in 1922, mesas "...stand distinctly above the surrounding country, as a table stands above the floor upon which it rests".JOURNAL, Bryan, K., 1922, Erosion and Sedimentation in the Papago Country, Arizona, US Geological Survey Bulletin, 730, 19–90, It is from this appearance that the term mesa was adopted from the Spanish word (wiktionary:mesa#Spanish|mesa), meaning "table".A mesa is similar to, but has a more extensive summit area than a butte. There is no agreed size limit that separates mesas from either buttes or plateaus. For example, the flat-topped mountains which are known as mesas in the Cockburn Range of North Western Australia have areas as large as {{convert|350|km2|mi2|abbr=on}}. In contrast, flat topped hills with areas as small as {{convert|0.1|km2|mi2|abbr=on}} in the Elbe Sandstone Mountains, Germany, are described as mesas.Less strictly, a very broad, flat-topped, usually isolated hill or mountain of moderate height bounded on at least one side by a steep cliff or slope and representing an erosion remnant also have been called mesas.In the English-language geomorphic and geologic literature, other terms for mesa have also been used. For example, in the Roraima region of Venezuela, the traditional name, tepui, from the local Pomón language, and the term table mountains have been used to describe local flat-topped mountains.Briceño, H.O. and Schubert, C., 1990. Geomorphology of the Gran Sabana, Guayana Shield, southeastern Venezuela. Geomorphology, 3(2), pp.125-141.Doerr, S.H., 1999. Karst-like landforms and hydrology in quartzites of the Venezuelan Guyana shield: Pseudokarst or" real" karst?. Zeitschrift fur Geomorphologie, 43(1), pp.1-17. Similar landforms in Australia are known as tablehills, table-top hills, tent hills, or jump ups (jump-ups).Jack, R.L., 1915. The Geology and prospects of the Region to the South of the Musgrave Ranges, and the Geology of the Western Portion of the Great Australian Artesian Basin. Geol. Survey South Australia Bulletin 5, pp. 72.{{Citation|title=Macquarie dictionary : Australia's national dictionary online|url=https://trove.nla.gov.au/work/18855142|publication-date=2021|publisher=Macquarie Library|access-date=11 March 2021}}WEB, 2012, Land Zones of Queensland,weblink 11 March 2021, Queensland Government, 62–63, The German term Tafelberg has also been used in the English scientific literature in the past.King, L.C., 1942. South African Scenery. A Textbook of Geomorphology. Oliver and Boyd, Edinburgh, London (340 pp.).

Formation

File:HarQatum.jpg|thumb|right|Har Qatum, a mesa located on the southern edge of Makhtesh Ramon, IsraelIsraelMesas form by weathering and erosion of horizontally layered rocks that have been uplifted by tectonic activity. Variations in the ability of different types of rock to resist weathering and erosion cause the weaker types of rocks to be eroded away, leaving the more resistant types of rocks topographically higher than their surroundings.BOOK, Easterbrook, Don J., Surface Processes and Landforms, 1999, Prentice Hall, Upper Saddle River, NJ, 9780138609580, This process is called differential erosion. The most resistant rock types include sandstone, conglomerate, quartzite, basalt, chert, limestone, lava flows and sills. Lava flows and sills, in particular, are very resistant to weathering and erosion, and often form the flat top, or caprock, of a mesa. The less resistant rock layers are mainly made up of shale, a softer rock that weathers and erodes more easily.The differences in strength of various rock layers are what give mesas their distinctive shape. Less resistant rocks are eroded away on the surface into valleys, where they collect water drainage from the surrounding area, while the more resistant layers are left standing out. A large area of very resistant rock, such as a sill, may shield the layers below it from erosion while the softer rock surrounding it is eroded into valleys, thus forming a caprock.Differences in rock type also reflect on the sides of a mesa, as instead of smooth slopes, the sides are broken into a staircase pattern called "cliff-and-bench topography". The more resistant layers form the cliffs, or stairsteps, while the less resistant layers form gentle slopes, or benches, between the cliffs. Cliffs retreat and are eventually cut off from the main cliff, or plateau, by basal sapping. When the cliff edge does not retreat uniformly but instead is indented by headward eroding streams, a section can be cut off from the main cliff, forming a mesa.Basal sapping occurs as water flowing around the rock layers of the mesa erodes the underlying soft shale layers, either as surface runoff from the mesa top or from groundwater moving through permeable overlying layers, which leads to slumping and flowage of the shale.BOOK, Choreley, Richard J., Stanley A. Schumm, David E. Sugden, David E. Sugden, Geomorphology, 1985, Methuen, New York, As the underlying shale erodes away, it can no longer support the overlying cliff layers, which collapse and retreat. When the caprock has caved away to the point where only little remains, it is known as a butte.

Examples and locations

Australia

File:Mount Conner - panoramio.jpg|thumb|Mount ConnerMount ConnerFile:Amadiya - panorama.jpg|thumb|290px|AmadiyaAmadiya

• Cockburn Range, Western AustraliaBOOK, Burbridge, Andrew, Mckenzie, NL, Kenneally, Kevin F, Nature Conservation Reserves in the Kimberley, Western Australia, 1991, Department of Conservation and Land Management, 9780646033747,weblink 4 July 2021,
• Mount Conner, Northern TerritoryBOOK, Report, 1966, The Department,weblink

Czech Republic

• Děčínský Sněžník

France

• Mont Aiguille, Auvergne-Rhône-Alpes

Germany

• Königstein, SaxonyKindred by Choice Germans and American Indians Since 1800, Glenn H Penny, 2013
• Lilienstein, SaxonyLilienstein – a mesa with a symbolic character
• Papststein, Saxony
• Pfaffenstein, SaxonyWEB, Jancewicz, Kacper, Morphological diversity of mesas in Elbsandsteingebirg,weblink ResearchGate, 4 July 2021,
• Quirl, Saxony

Iraq

• Amadiya, Kurdistan Region

Ireland

• Kings Mountain, County SligoJournal of Earth Sciences Royal Dublin Society. (1980). Ireland: The Society.
• Knocknarea, County Sligo
• Knocknashee, County Sligo

Israel

• Masada, Southern DistrictWEB, Masada - Definition, History, Siege & Facts,weblink Encyclopedia Britannica, 4 July 2021,
• Har Qatum

Italy

• Monte Santo, Sardinia

United Kingdom

England

File:Ingleborough from Little Ingleborough - geograph.org.uk - 548604.jpg|thumb|IngleboroughIngleborough

• Castle Folds, CumbriaBOOK, 2009, Zalozoba ZRC, 9789612541613, 286,weblink 4 July 2021, Karst Rock Features. Karren sculpturing: Karren sculpturing,
• Cross Fell, CumbriaLakeland - The Wildlife of Cumbria, Derek A Ratcliffe
• Goldsborough Carr, County DurhamReading, H. G. (1954) The stratigraphy and structure of the syncline of stainmore, Durham theses,

Durham University. Available at Durham E-Theses Online:weblink

• Higger Tor, South YorkshireJOURNAL, University of Peshawar - Bulletin of the Centre of Excellence in Geology, 7-8, 3,weblink Bulletin of the Centre of Excellence in Geology, 1975,
• Ingleborough, North Yorkshire
• Pen-y-ghent, North YorkshireBOOK, Wood, Harold, Preece, Dorothy, Modern Geography ...: The British Isles, 1948,weblink 9 July 2022,
• Shacklesborough, County Durham

Scotland

• Healabhal Mhòr, Isle of SkyeNEWS, Reid, T.R., A Lord's Leaky Roof vs. a Changing Scotland,weblink 10 August 2022, The Washington Post, 2 November 2000,

United States

Many but not all American mesas lie within the Basin and Range Province.

Arizona

• Anderson Mesa
• Black Mesa
• Black Mesa
• Black Mesa
• Black Mountain
• Cummings Mesa
• First Mesa
• Horseshoe Mesa
• Indian Mesa
• Second Mesa

Arkansas

• Mount Magazine

California

• Redonda Mesa

Colorado

File:Mesa in Colorado.jpg|thumb|Mount Garfield, a mesa in Colorado]]

• Battlement Mesa
• Grand Mesa - largest flat-topped mountain in the world.National Geographic Encyclopedia (2016)
• Green Mountain
• Log Hill Mesa
• North Table Mountain
• Raton Mesa

Nevada

• Mormon Mesa
• Pahute Mesa

Oklahoma

• Black Mesa
• Mesa de Maya

Texas

• Floating MesaWEB, Floating Mesa, Bushland, Texas,weblink Atlas Obscura, 19 October 2021,
• Llano Estacado

Utah

• Checkerboard Mesa
• Crazy Quilt Mesa
• Hurricane Mesa
• Sams Mesa
• Smith Mesa
• South Caineville Mesa
• Thompson Mesa
• Wildcat Mesa
• Wingate Mesa

Wisconsin

• Gibraltar Rock
• Grandad Bluff
• Mile Bluff
• Quincy Bluff
• Rattlesnake Mound

On Mars

File:PIA21585 - A Mesa in Noctis Labyrinthus.jpg|thumb|A mesa in Noctis Labyrinthus on Mars, viewed by HiRISEHiRISEA transitional zone on Mars, known as fretted terrain, lies between highly cratered highlands and less cratered lowlands. The younger lowland exhibits steep walled mesas and knobs. The mesa and knobs are separated by flat lying lowlands. They are thought to form from ice-facilitated mass wasting processes from ground or atmospheric sources. The mesas and knobs decrease in size with increasing distance from the highland escarpment. The relief of the mesas range from nearly {{Convert|2|km|mi|abbr=on|sp=us}} to {{Convert|100|m|ft|abbr=on|sp=us}} depending on the distance they are from the escarpment.Baker, David M. Morphological Analyses of Mesas and Knobs in the Northwest Fretted Terrain of Mars; Constraints on the Presence and Distribution of Ice-Facilitated Mass-Wasting. Ed. Alexander K. Stewart and James W. Head. Vol. 40. Issue 2. pp. 72. United States: Geological Society of America (GSA) : Boulder, CO, United States, 2008.

See also

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• {{annotated link|Amba (landform)|Amba}}
• {{annotated link|Archipelago}}
• {{annotated link|Butte}}
• {{annotated link|Dissected plateau}}
• {{annotated link|Mensa (geology)|Mensa}}
• {{annotated link|Mesa Verde National Park}}
• {{annotated link|Nor'Wester Mountains}} – Group of mountains immediately south of Thunder Bay, Ontario, Canada
• {{annotated link|Pingdingshan}} – Chinese city named after a local mesa
• {{annotated link|Potrero (landform)|Potrero}}
• {{annotated link|Table (landform)|Table hill}}
• {{annotated link|Table Mountain}}
• {{annotated link|Tepui}}
• {{annotated link|Tundra}}
• {{annotated link|Tuya}}

{{div col end}}

References

{{Commons category|Mesas}}{{Wiktionary}}{{Reflist}}{{Authority control}}