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A terrane in geology is a fragment of crustal material formed on, or broken off from, one tectonic plate and accreted — "sutured" — to crust lying on another plate. The crustal block or fragment preserves its own distinctive geologic history, which is different from that of the surrounding areas (hence the term "exotic" terrane). The suture zone between a terrane and the crust it attaches to is usually identifiable as a fault.

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Overview

A terrane is not necessarily an independent microplate in origin, since it may not contain the full thickness of the lithosphere. It is a piece of crust which has been transported laterally, usually as part of a larger plate, and is relatively buoyant due to thickness or low density. When the plate of which it was a part subducted under another plate, the terrane failed to subduct, detached from its transporting plate, and accreted onto the overriding plate. Therefore, the terrane transferred from one plate to the other. Typically, accreting terranes are portions of continental crust which have rifted off another continental mass and been transported surrounded by oceanic crust, or old island arcs formed at some distant subduction zone.

The concept of terranes developed from studies in the 1970s of the complicated Pacific Cordilleran ("backbone") orogenic margin of North America, a complex and diverse geological potpourri that was difficult to explain until the new science of plate tectonics illuminated the ability of crustal fragments to "drift" thousands of miles from their origin and fetch up, crumpled, against an exotic shore. Such terranes were dubbed "accreted terranes" by geologists.

It was soon determined that these exotic crustal slices had in fact originated as "suspect terranes" in regions at some considerable remove, frequently thousands of kilometers, from the orogenic belt where they had eventually ended up. It followed that the present orogenic belt was itself an accretionary collage, composed of numerous terranes derived from around the circum-Pacific region and now sutured together along major faults. These concepts were soon applied to other, older orogenic belts, e.g. the Appalachian belt of North America.... Support for the new hypothesis came not only from structural and lithological studies, but also from studies of faunal biodiversity and palaeomagnetism. (Carney et al.)

When terranes are composed of repeated accretionary events, and hence are composed of subunits with distinct history and structure, they may be called superterranes.[1]

List of terranes

See also

Notes

External links

References

  • J.N. Carney et al., Precambrian Rocks of England and Wales, GCReg. volume 20 (ISBN 978-1861074874)
  • John McPhee, Basin and Range, 1981 (Farrar, Straus and Giroux, New York).
  • John McPhee, In Suspect Terrain 1983 (Farrar, Straus and Giroux, New York).
  • John McPhee, Assembling California, 1993 (Farrar, Straus and Giroux, New York).

File:Maps-for-free Sierra
Relief map of Sierra Nevada
File:Alpine Fault SRTM (vertical).jpg
A shaded and colored image (i.e. terrain is enhanced) of varied terrain from the Shuttle Radar Topography Mission. This shows elevation model of New Zealand's Alpine Fault running about 500 km (300 mi) long. The escarpment is flanked by a vast chain of hills between the fault and the mountains of New Zealand's Southern Alps. Northeast is towards the top.

Terrain, or land relief, is the vertical and horizontal dimension of land surface. When relief is described underwater, the term bathymetry is used. Topography has recently become an additional synonym, though in many parts of the world it retains its original more general meaning of description of place.

Terrain is used as a general term in physical geography, referring to the lie of the land. This is usually expressed in terms of the elevation, slope, and orientation of terrain features. Terrain affects surface water flow and distribution. Over a large area, it can affect weather and climate patterns.

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Importance

The understanding of terrain is critical for many reasons.

  • The terrain of a region largely determines its suitability for human settlement: flatter, alluvial plains tend to have better farming soils than steeper, rockier uplands.
  • In terms of environmental quality, agriculture, and hydrology, understanding the terrain of an area enables the understanding of watershed boundaries, drainage characteristics, water movement, and impacts on water quality. Complex arrays of relief data are used as input parameters for hydrology transport models (such as the SWMM or DSSAM Models) to allow prediction of river water quality.
  • Understanding terrain also supports on soil conservation, especially in agriculture. Contour plowing is an established practice enabling sustainable agriculture on sloping land; it is the practice of plowing along lines of equal elevation instead of up and down a slope.
  • Terrain is militarily critical because it determines the ability of armed forces to take and hold areas, and move troops and material into and through areas. An understanding of terrain is basic to both defensive and offensive strategy.
  • Terrain is important in determining weather patterns. Two areas geographically close to each other may differ radically in precipitation levels or timing because of elevation differences or a "rain shadow" effect.
  • Since terrain comes in vast varieties, certain features can be specific according to one type terrain, but also other features can be specific to multiple types of terrain. Basically, different terrains can both share the same features as well as have their own unique features.

Geomorphology

Geomorphology is in large part the study of the formation of terrain or topography. Terrain is formed by intersecting processes:

Tectonic processes such as orogenies cause land to be elevated, and erosional or weathering processes cause land to be worn away to lower elevations.

Land surface parameters are quantitative measures of various morphometric properties of a surface. The most common examples are used to derive slope or aspect of a terrain or curvatures at each location. These measures can also be used to derive hydrological parameters that reflect flow/erosion processes. Climatic parameters are based on the modelling of solar radiation or air flow.

Land surface objects, or landforms, are definite physical objects (lines, points, areas) that differ from the surrounding objects. The most typical examples arelines of watersheds, stream patterns, ridges, break-lines, pools or borders of specific landforms.

See also

External links


Wiktionary

Up to date as of January 14, 2010
(Redirected to terrain article)

Definition from Wiktionary, a free dictionary

See also Terrain

Contents

English

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Etymology

From French terrain < Latin terrenum (land, ground), prop. neut. of terrenus (consisting of earth) < terra (earth).

Pronunciation

Noun

Singular
terrain

Plural
terrains

terrain (plural terrains)

  1. (geology) A single, distinctive rock formation; an area having a preponderance of a particular rock or group of rocks.
  2. An area of land or the particular features of it.

Related terms

Translations

External links

  • terrain in Webster’s Revised Unabridged Dictionary, G. & C. Merriam, 1913
  • terrain in The Century Dictionary, The Century Co., New York, 1911

Anagrams


French

Etymology

From Vulgar Latin terranum, from Latin terrenum.

Pronunciation

Noun

terrain m. (plural terrains)

  1. ground, landscape, terrain
    Un nouveau de terrain de football a été aménagé l'an dernier.

Anagrams








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