A tableland is an area containing elevated landforms characterized by a distinct, flat, nearly level, or gently undulating surface. They often exhibit steep, cliff-like edges, know as escarpments, that separate them from surrounding lowlands. Depending on either their size, other physical characteristics, or geographic location, the landforms comprising a tableland are individually referred to by a number of names including either butte, mesa, plateau, potrero, tepui, or tuya. Table Mountains are also a type of tableland. [1] [2] A homologous landform under the sea is called either a tablemount or guyot.
Sedimentary tablelands are tablelands that typically have developed from the erosion of coarse-grained, clastic, sedimentary rocks in the form of relatively flat-lying sandstones and conglomerates that have not been strongly deformed by tectonics. The primary control on the geomorphology of sedimentary tablelands is the dip of the layers of the sandstones, conglomerates, and associated sedimentary strata. Sedimentary tablelands only form if the dip of the sedimentary layers is negligible. If the sedimentary layers are tilted, although otherwise little deformed, asymmetric ridges known as cuestas develop. [2] [3]
Areally extensive sedimentary tablelands are often known as plateaus. As plateaus are dissected by the headward erosion and incision of river and stream courses and the retreat of their bounding escarpments, plateaus are fragmented into tablelands of smaller and smaller extent known as mesas, buttes, or pinnacles. Further erosion eventually reduces these landforms to piles of bouderly rubble as known as rock labyrinths. The tepui of South America are a type of sedimentary tableland composed of erosional outliers of flat-lying Precambrian quartz arenite sandstone that tower over the surrounding jungle underlain by crystalline basement rocks. [3] [4]
Flat-lying, coarse-grained, clastic sedimentary rocks are not the only layered rocks that serve as the caprock that form the surface of tablelands. Flat-lying duricrusts and volcanic rocks also form the caprock of various tablelands. In case of duricrusts, e.g. laterite or silcrete, the formation of tablelands involves a three stage process. First, the formation of a thick indurated surface layer duricrust by deep weathering beneath a relatively flat surface. Second, the breaching and incision of the duricrust layer by rivers or streams. Finally, the inward migration of valley walls and escarpments by slope erosion and denudation of mesas and buttes. An example of such tablelands is the laterite-capped Panchgani Tableland of India. [5] Tablelands formed by the erosion of duricrusts are also quite common in parts of Australia and South America. [6] [7] In addition, the eruption of either lava or pyroclastic flows can deposit a solid surface layer of volcanic rock that is relatively flat. As in case of the duricrusts, the resulting lava or pyroclastic flows are sufficiently tough to form the flat-lying caprock of tablelands when breached and incised by rivers and streams. [8]
- ^ Neuendorf, K.K.E.; Mehl, Jr., J.P.; Jackson, J.A., eds. (2005). Glossary of Geology (5th ed.). Alexandria, VA: American Geological Institute. ISBN 0-922152-76-4. OCLC 894898557.
- ^ a b Duszyński, F.; Migoń, P.; Strzelecki, M.C. (September 2019). "Escarpment retreat in sedimentary tablelands and cuesta landscapes–Landforms, mechanisms and patterns". Earth-Science Reviews. 169: 102890. doi: 10.1016/j.earscirev.2019.102890.
- ^ a b Migoń, P.; Duszyński, F. (November 2022). "Landscapes and landforms in coarse clastic sedimentary tablelands–Is there a unifying theme?". Catena. 218: 106545. doi: 10.1016/j.catena.2022.106545.
- ^ Migoń, P.; Duszyński, F.; Jancewicz, K. and; Kotwicka, W. (October 2020). "Late evolutionary stages of residual hills in tablelands (Elbsandsteingebirge, Germany)". Geomorphology. 367: 107308. doi: 10.1016/j.geomorph.2020.107308.
- ^ Kumar, V.S. (2015). "The laterite-capped Panchgani Tableland, Deccan Traps". In Kale, V. (ed.). Landscapes and Landforms of India. World Geomorphological Landscapes. Springer. pp. 217–222. doi: 10.1007/978-94-017-8029-2_23. ISBN 978-94-017-8029-2.
- ^ Rabassa, J.; Carignano, C.; Cioccale, M. (2010). "Gondwana paleosurfaces in Argentina: an introduction". Geociências. 29 (4): 430–466.
- ^ Anand, R.R.; de Broekert, P. (2005). "Weathering history, landscape evolution and implications for exploration". In Anand, R.R.; de Broekert, P. (eds.). Regolith Landscape Evolution Across Australia: A Compilation of Regolith Landscape Case Studies With Regolith Landscape Evolution Models. Perth, West Australia: CRC LEME. pp. 2–40. ISBN 1-921039-30-2. OCLC 225089086.
- ^ Ferrill, D.A.; Morris, A.P.; McGinnis, R.N.; Smart, K.J.; Watson-Morris, M.J.; Wigginton, S.S. (2016). "Observations on normal-fault scarp morphology and fault system evolution of the Bishop Tuff in the Volcanic Tableland, Owens Valley, California, USA". Lithosphere. 8 (3): 238–253. doi: 10.1130/L476.1.
-
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Tables (landform) at Wikimedia Commons
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A tableland is an area containing elevated landforms characterized by a distinct, flat, nearly level, or gently undulating surface. They often exhibit steep, cliff-like edges, know as escarpments, that separate them from surrounding lowlands. Depending on either their size, other physical characteristics, or geographic location, the landforms comprising a tableland are individually referred to by a number of names including either butte, mesa, plateau, potrero, tepui, or tuya. Table Mountains are also a type of tableland. [1] [2] A homologous landform under the sea is called either a tablemount or guyot.
Sedimentary tablelands are tablelands that typically have developed from the erosion of coarse-grained, clastic, sedimentary rocks in the form of relatively flat-lying sandstones and conglomerates that have not been strongly deformed by tectonics. The primary control on the geomorphology of sedimentary tablelands is the dip of the layers of the sandstones, conglomerates, and associated sedimentary strata. Sedimentary tablelands only form if the dip of the sedimentary layers is negligible. If the sedimentary layers are tilted, although otherwise little deformed, asymmetric ridges known as cuestas develop. [2] [3]
Areally extensive sedimentary tablelands are often known as plateaus. As plateaus are dissected by the headward erosion and incision of river and stream courses and the retreat of their bounding escarpments, plateaus are fragmented into tablelands of smaller and smaller extent known as mesas, buttes, or pinnacles. Further erosion eventually reduces these landforms to piles of bouderly rubble as known as rock labyrinths. The tepui of South America are a type of sedimentary tableland composed of erosional outliers of flat-lying Precambrian quartz arenite sandstone that tower over the surrounding jungle underlain by crystalline basement rocks. [3] [4]
Flat-lying, coarse-grained, clastic sedimentary rocks are not the only layered rocks that serve as the caprock that form the surface of tablelands. Flat-lying duricrusts and volcanic rocks also form the caprock of various tablelands. In case of duricrusts, e.g. laterite or silcrete, the formation of tablelands involves a three stage process. First, the formation of a thick indurated surface layer duricrust by deep weathering beneath a relatively flat surface. Second, the breaching and incision of the duricrust layer by rivers or streams. Finally, the inward migration of valley walls and escarpments by slope erosion and denudation of mesas and buttes. An example of such tablelands is the laterite-capped Panchgani Tableland of India. [5] Tablelands formed by the erosion of duricrusts are also quite common in parts of Australia and South America. [6] [7] In addition, the eruption of either lava or pyroclastic flows can deposit a solid surface layer of volcanic rock that is relatively flat. As in case of the duricrusts, the resulting lava or pyroclastic flows are sufficiently tough to form the flat-lying caprock of tablelands when breached and incised by rivers and streams. [8]
- ^ Neuendorf, K.K.E.; Mehl, Jr., J.P.; Jackson, J.A., eds. (2005). Glossary of Geology (5th ed.). Alexandria, VA: American Geological Institute. ISBN 0-922152-76-4. OCLC 894898557.
- ^ a b Duszyński, F.; Migoń, P.; Strzelecki, M.C. (September 2019). "Escarpment retreat in sedimentary tablelands and cuesta landscapes–Landforms, mechanisms and patterns". Earth-Science Reviews. 169: 102890. doi: 10.1016/j.earscirev.2019.102890.
- ^ a b Migoń, P.; Duszyński, F. (November 2022). "Landscapes and landforms in coarse clastic sedimentary tablelands–Is there a unifying theme?". Catena. 218: 106545. doi: 10.1016/j.catena.2022.106545.
- ^ Migoń, P.; Duszyński, F.; Jancewicz, K. and; Kotwicka, W. (October 2020). "Late evolutionary stages of residual hills in tablelands (Elbsandsteingebirge, Germany)". Geomorphology. 367: 107308. doi: 10.1016/j.geomorph.2020.107308.
- ^ Kumar, V.S. (2015). "The laterite-capped Panchgani Tableland, Deccan Traps". In Kale, V. (ed.). Landscapes and Landforms of India. World Geomorphological Landscapes. Springer. pp. 217–222. doi: 10.1007/978-94-017-8029-2_23. ISBN 978-94-017-8029-2.
- ^ Rabassa, J.; Carignano, C.; Cioccale, M. (2010). "Gondwana paleosurfaces in Argentina: an introduction". Geociências. 29 (4): 430–466.
- ^ Anand, R.R.; de Broekert, P. (2005). "Weathering history, landscape evolution and implications for exploration". In Anand, R.R.; de Broekert, P. (eds.). Regolith Landscape Evolution Across Australia: A Compilation of Regolith Landscape Case Studies With Regolith Landscape Evolution Models. Perth, West Australia: CRC LEME. pp. 2–40. ISBN 1-921039-30-2. OCLC 225089086.
- ^ Ferrill, D.A.; Morris, A.P.; McGinnis, R.N.; Smart, K.J.; Watson-Morris, M.J.; Wigginton, S.S. (2016). "Observations on normal-fault scarp morphology and fault system evolution of the Bishop Tuff in the Volcanic Tableland, Owens Valley, California, USA". Lithosphere. 8 (3): 238–253. doi: 10.1130/L476.1.
-
Media related to
Tables (landform) at Wikimedia Commons
| ||
|
| This article related to topography is a stub. You can help Wikipedia by expanding it. |