Inselberg

"monadnock" redirects here. For other uses, see monadnock (disambiguation).
Inselberg in the state of Bahia, northeastern Brazil.
An inselberg in Western Sahara.

An inselberg or monadnock (pronunciation: /məˈnædnɒk/) is an isolated rock hill, knob, ridge, or small mountain that rises abruptly from a gently sloping or virtually level surrounding plain.

In southern and south-central Africa, a similar formation of granite is known as a koppie, an Afrikaans word ("little head") from the Dutch word kopje.[1]

If the inselberg is dome-shaped and formed from granite or gneiss, it can also be called a bornhardt, though not all bornhardts are inselbergs.

Plains containing various inselbergs, inselberg plains, occur in various parts of the world including the interior of Angola,[2] Namibia,[3] Tanzania,[4] Northern Finland[5] and Swedish Lapland.[6]

Etymology

Inselberg

The word inselberg is German for "island mountain"; the name was coined by geologist Wilhelm Bornhardt (1864–1946) in 1900 to describe the abundance of such features found in southern Africa.[7] At that time, the term applied only to arid landscape features. However, the term inselberg has since been used to describe a broader geography and range of rock features, leading to confusion about the precise definition of the term. In a 1973 study examining the use of the term, one researcher found that the term had been used for features in savannah climates 40% of the time, arid or semi-arid climates 32% of the time, humid-subtropical and arctic 12% of the time, and 6% each in humid-tropical and Mediterranean climates. As recently as 1972, the term has been defined as "steep-sided isolated hills rising relatively abruptly above gently sloping ground". This definition includes such features as buttes; conical hills with rectilinear sides typically found in arid regions; regolith-covered concave-convex hills; rock crests over regolith slopes; rock domes with near vertical sides; tors (koppies) formed of large boulders but with solid rock cores. Thus, the terms monadnock and inselberg may not perfectly match,[8] though some authors have explicitly argued these terms are in fact completely synonymous.[9]

Monadnock

Mount Monadnock in New Hampshire, United States

Monadnock is an originally Native American term for an isolated hill or a lone mountain that stands above the surrounding area, typically by surviving erosion. Geologists took the name from Mount Monadnock in southwestern New Hampshire.[10] It is thought to derive from the Abenaki language, from either menonadenak ("smooth mountain") or menadena ("isolated mountain").[11] In this context, monadnock is used to describe a mountain that rises from an area of relatively flat and/or lower terrain. For instance, Mount Monadnock rises 2,000 feet (610 m) above its surrounding terrain and stands, at 3,165 feet (965 m), nearly 1,000 feet (300 m) higher than any mountain peak within 30 miles (48 km).[12]

Geology

Pietra di Bismantova in the Apennines, Italy

Volcanic or other processes may give rise to a body of rock resistant to erosion, inside a body of softer rock such as limestone, which is more susceptible to erosion. When the less resistant rock is eroded away to form a plain, the more resistant rock is left behind as an isolated mountain. The strength of the uneroded rock is often attributed to the tightness of its jointing.[13]

The presence of a monadnock or inselberg typically indicates the existence of a nearby plateau or highland, or their remnants. This is especially the case for inselbergs composed of sedimentary rock, which will display the same stratigraphic units as this nearby plateau. However once exposed, the inselbergs are destroyed by marginal collapse of joint blocks and exfoliation sheets. This process leaves behind tors perched at their summits and, over time, a talus-bordered residual known as a castle kopje appears.[14][15]

Inselbergs can be reshaped by ice sheets much the same way as roche moutonnées. In northern Sweden this kind of inselbergs have been referred as flyggbergs.[16]:326–327[17]

Ecology

The kopjes of Eastern Africa tend to be a refuge for life in the Serengeti of Tanzania and Kenya. Where the soil is too thin or hard to support tree life in large areas, soil trapped by kopjes can be dense with trees while the surrounding land contains only short grass. Hollows in the rock surfaces provide catchments for rainwater.[18] Many animals have adapted to the use of kopjes, including the lion, the hyrax, and an abundance of bird and reptile life.

Houtkop (1,751 m), an outcrop of Drakensberg basalt beside the R26 route between Reitz and Daniëlsrus in the Riemland, Free State, South Africa
Koppie, Free State, South Africa
A koppie in Serengeti National Park, Tanzania
The granitic Spitzkoppe of Namibia, formed by early Cretaceous rifting and magmatism
A duricrust inselberg near Dori, Burkina Faso

See also

References

  1. ↑ Webster's New Explorer Dictionary of Word Origins (2004). Federal Street Press: New York.
  2. ↑ DEVELOPMENT OF A SOIL AND TERRAIN MAP/DATABASE FOR ANGOLA
  3. ↑ PRODUCTION OF AN AGRO.ECOLOGICAL ZONES MAP OF NAMIBIA (first approximation)
  4. ↑ Sundborg, Å., & Rapp, A. (1986). Erosion and sedimentation by water: problems and prospects. Ambio, 215-225.
  5. ↑ Ebert, K., Hall, A. M., Hättestrand, C., & Alm, G. (2009). Multi-phase development of a glaciated inselberg landscape.
  6. ↑ Rudberg, S. (1988). Gross morphology of Fennoskandia: six complementary ways of explanation. Geografiska Annaler. Series A. Physical Geography, 135-167.
  7. ↑ Holmes, Arthur (1978). Holmes Principles of Physical Geology Taylor & Francis: New York.
  8. ↑ Gerrard, John (1988). Rocks and Landforms Routledge: Florence, Kentucky.
  9. ↑ King, L.C., 1953, Canons of landscape evolution: Bulletin of the Geological Society of America, v. 64, no. 7, p. 721–752.
  10. ↑ Raymo, Chet and Raymo, Maureen E. (1989) Written in Stone: A Geologic History of the Northeastern United States. Globe Pequot, Chester, Connecticut.
  11. ↑ "Vermont Soils with Names of American Indian Origin" United States Department of Agriculture, Natural Resources Conservation Service. Retrieved January 6, 2008.
  12. ↑ Baldwin, Henry I. (1989). Monadnock Guide 4th edition. Concord, New Hampshire: Society for the Protection of New Hampshire Forests.
  13. ↑ "A Dictionary of Ecology" (2004). Encyclopedia.com. Retrieved November 28, 2009 <http://www.encyclopedia.com>
  14. ↑ "Summary: Inselbergs/Hills/Knobs" Desert Processes Working Group; Knowledge Sciences, Inc. Retrieved January 6, 2008.
  15. ↑ Easterbrook, Don J. "Chapter Three: Weathering." Surface Processes and Landforms. 2nd ed. Upper Saddle River, NJ: Prentice Hall, 1999. 45. Print.
  16. ↑ Douglas Benn and David Evans, Glaciers & Glaciation, Arnold, London, 1st ed. 1998 ISBN 9780340584316
  17. ↑ Lidmar-Bergström, Karna; Olvmo, Mats (2015). Plains, steps, hilly relief and valleys in northern Sweden – review, interpretations and implications for conclusions on Phanerozoic tectonics (PDF) (Report). Geological Survey of Sweden. p. 13. Retrieved June 29, 2016.
  18. ↑ Serengeti National Park Visitor Center, Tanzania

External links

Wikimedia Commons has media related to Monadnocks.
This article is issued from Wikipedia - version of the 11/21/2016. The text is available under the Creative Commons Attribution/Share Alike but additional terms may apply for the media files.