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gravel

 
(grăv'əl) pronunciation
n.
  1. An unconsolidated mixture of rock fragments or pebbles.
  2. Pathology. The sandlike granular material of urinary calculi.
tr.v., -eled, or -elled, -el·ing, or -el·ling, -els, or -els.
  1. To apply a surface of rock fragments or pebbles to.
  2. To confuse; perplex.
  3. Informal. To irritate.

[Middle English, from Old French gravele, diminutive of grave, pebbly shore, of Celtic origin.]


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Aggregate of more or less rounded rock fragments coarser than sand (i.e., more than 0.08 in., or 2 mm, in diameter). Gravel beds in some places contain heavy metallic ore minerals, such as cassiterite (a major source of tin), or native metals, such as gold, in nuggets or flakes. Deposits accumulate in parts of stream channels or on beaches where the water moves too rapidly to permit sand to remain. Because of changing conditions, gravel formations generally are more limited and more variable in coarseness, thickness, and configuration than sand or clay deposits. In many regions gravel terraces (or raised beaches) extend great distances inland, indicating that the sea at one time stood higher than it does today. Gravels are widely used building materials.

For more information on gravel, visit Britannica.com.

An unconsolidated sedimentary aggregate containing more than 50% by weight of gravel-sized particles (mean diameter greater than 0.08 in. or 2 mm). The gravel-sized particles are termed the framework; those less than 0.08 in. in diameter are the matrix. There is an important distinction between framework-supported and matrix-supported gravels. The latter may possess a muddy matrix, in which case they are termed diamictons. Typically, diamictons are unstratified internally, contain subangular framework clasts, and are deposited by mass-flow processes such as debris flow or glacial-ice transport. Water-laid gravels are typically stratified or cross-stratified and are framework-supported, with subangular to rounded clasts in a sand matrix. Less commonly, they may be sand-matrix-supported, or they may lack matrix and then are termed openwork gravels. Water-worn gravel clasts tend to conform to the shape of triaxial ellipsoids and develop preferred orientation, with long axes normal to stream flow and intermediate axes dipping gently upstream.

The consolidated equivalents of gravels are conglomerates and breccias, the latter including only angular particles. Paleoenvironmental indicators for conglomerates include stratification, size grading, particle roundness, particle orientation, and matrix–framework relations. See also Breccia; Conglomerate; Sedimentary rocks.


geology A particle size, typically 2 to 64 mm (0.787 to 2.5 in).

A loose deposit of rock fragments rounded by river erosion. The lower size limit of gravel is 2 mm but the upper limit is either 10 mm, 20 mm, 50 mm, or 60 mm according to different authorities. While river gravels are well rounded as a result of attrition, solifluction gravels, produced by freeze-thaw, are more angular. The plateau gravels of southern England are extensive deposits between 0 and 1250 m above sea level, made of flint and chert fragments in a mould of sand and clay. They were deposited by solifluction and meltwater during the Pleistocene.

A coarse granular aggregate, larger than sand; formed either naturally or by crushing rock; will pass a 76.1-mm (3-in.) sieve and be retained on a 4.76-mm (No. 4) sieve.



[De]

Medium to large particles of more than 2mm across forming constituent components of natural and anthropogenic sediments and deposits. Gravel is often subdivided into: granular, pebble, cobble, and boulder gravel.

gravel, particles of rock, i.e., stones and pebbles, usually round in form and intermediate in size between sand grains and boulders. Gravel is composed of various kinds of rock, the most common constituent being the mineral quartz. Deposits of gravel are formed as a result of the weathering of rocks and the erosive and concentrating action of rivers and waves. Sometimes gravel becomes consolidated into the sedimentary rock called conglomerate. Gravel is used extensively in building roads and in making concrete. For road building it is crushed into angular particles of uniform size. One or more layers of gravel underlie the road surface. A small percentage of clay must be present to act as a binder when gravel is used in macadam for road surfaces. When used as a coarse aggregate for concrete, gravel must be clean and free from clay and organic matter. Commercially, it is classified according to the size of the particles. In areas where natural deposits are inadequate, gravel is produced by quarrying and crushing durable rocks, such as sandstone, limestone, or basalt.


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gravel

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pronunciation

IN BRIEF: Small pieces of rocks and stones.

pronunciation Some people use gravel on their garden paths.

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Calculus occurring in small particles.

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categories related to 'gravel'

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For a list of words related to gravel, see:

  See crossword solutions for the clue Gravel.
Gravel (largest fragment in this photo is about 4 cm)
A gravel road in Terre Haute, Indiana
Gravel being unloaded from a barge

Gravel play /ˈɡrævəl/ is composed of unconsolidated rock fragments that have a general particle size range and include size classes from granule- to boulder-sized fragments. Gravel can be sub-categorized into granule (>2 to 4 mm or 0.079 to 0.16 in) and cobble (>64 to 256 mm or 2.5 to 10.1 in). One cubic yard of gravel typically weighs about 3000 pounds (or a cubic metre is about 1,800 kilograms).

Gravel is an important commercial product, with a number of applications. Many roadways are surfaced with gravel, especially in rural areas where there is little traffic. Globally, far more roads are surfaced with gravel than with concrete or tarmac; Russia alone has over 400,000 km (250,000 mi) of gravel-surfaced roads.[citation needed] Both sand and small gravel are also important for the manufacture of concrete.

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Geological formation

Large gravel deposits are a common geological feature, being formed as a result of the weathering and erosion of rocks. The action of rivers and waves tends to pile up gravel in large accumulations. This can sometimes result in gravel becoming compacted and concreted into the sedimentary rock called conglomerate. Where natural gravel deposits are insufficient for human purposes, gravel is often produced by quarrying and crushing hard-wearing rocks, such as sandstone, limestone, or basalt. Quarries where gravel is extracted are known as gravel pits. Southern England possesses particularly large concentrations of them due to the widespread deposition of gravel in the region during the Ice Ages.

Modern production

As of 2006, the United States is the world's leading producer and consumer of gravel.[1][2]

Etymology

The word gravel comes from the Old French word gravele.[3]

Types

Gravel with stones sized roughly between 5 and 15 millimeter.
Disused gravel pit in Lower Saxony, Germany

Multiple types of gravel have been recognized,[by whom?] including:

  • Bank gravel: gravel intermixed with sand or clay.
  • Bench gravel: a bed of gravel located on the side of a valley above the present stream bottom, indicating the former location of the stream bed when it was at a higher level.
  • Creek rock: this is generally rounded, semi-polished stones, potentially of a wide range of types, that are dredged or scooped from river beds and creek beds. It is also often used as concrete aggregate and less often as a paving surface.
  • Crushed rock: rock that is mechanically broken into small pieces then sorted by filtering through different size mesh.
  • Crushed stone: this is generally limestone or dolomite that has been crushed and graded by screens to certain size classes. It is widely used in concrete and as a surfacing for roads and driveways, sometimes with tar applied over it. Crushed stone may also be made from granite and other rocks. A special type of limestone crushed stone is dense grade aggregate, or DGA, also known as crusher run, or colloquially as "crush and run". This is a mixed grade of mostly small crushed stone in a matrix of crushed limestone powder.
  • Fine gravel: gravel consisting of particles with a diameter of 2 to 4 mm.
  • Lag gravel: a surface accumulation of coarse gravel produced by the removal of finer particles.
  • Pay gravel: also known as "pay dirt"; a nickname for gravel with a high concentration of gold and other precious metals. The metals are recovered through gold panning.
  • Pea gravel: gravel that consists of small, rounded stones used in concrete surfaces. Also used for walkways, driveways and as a substrate in home aquariums.
  • Piedmont gravel: a coarse gravel carried down from high places by mountain streams and deposited on relatively flat ground, where the water runs more slowly.
  • Plateau gravel: a layer of gravel on a plateau or other region above the height at which stream-terrace gravel is usually found.
  • River run gravel: naturally deposited gravel found in and next to rivers and streams.

Relationship to plantlife

In locales where gravelly soil is predominant, plant life is generally more sparse.[4] This outcome derives from the inferior ability of gravels to retain moisture, as well as the corresponding paucity of mineral nutrients, since finer soils that contain such minerals are present in smaller amounts.

See also

References

  1. ^ Mineral Commodity Summaries 2006 2009
  2. ^ Industrial Sand And Gravel (Silica): World Production, By Country 2009
  3. ^ gravel. (n.d.). Collins English Dictionary - Complete & Unabridged 10th Edition. Retrieved December 09, 2011, from Dictionary.com website.
  4. ^ C.Michael Hogan. 2010. Abiotic factor. Encyclopedia of Earth. eds Emily Monosson and C. Cleveland. National Council for Science and the Environment. Washington DC

Translations:

Gravel

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Dansk (Danish)
n. - grus, nyregrus
v. tr. - strø grus på, gruse, irritere, sætte på grund

Nederlands (Dutch)
grind, steengruis, begrinten, in verwarring brengen, irriteren

Français (French)
n. - (Constr) graviers, gravillons, (Méd) calculs
v. tr. - couvrir de gravier

Deutsch (German)
n. - Kies, Geröll, Schotter, Harngrieß, Nierensand
v. - mit Kies bestreuen, verwirren

Ελληνική (Greek)
n. - αμμοχάλικο, χαλίκι
v. - χαλικοστρώνω

Italiano (Italian)
ghiaia, renella, inghiaiare, imbarazzare

Português (Portuguese)
n. - cascalho (m), cálculo (m) (Med.)
v. - cobrir com pedregulho, embaraçar

Русский (Russian)
гравий, посыпать гравием, мочевой песок, золотоносный песок

Español (Spanish)
n. - grava, ripio, cascajo, arenillas
v. tr. - cubrir con grava, dejar perplejo a alguien

Svenska (Swedish)
n. - grus, njurgrus (med.)
v. - grusa, bringa ur fattningen, reta

中文(简体)(Chinese (Simplified))
砂砾, 砂砾层, 铺碎石, 使搁浅, 使困惑

中文(繁體)(Chinese (Traditional))
n. - 砂礫, 砂礫層
v. tr. - 鋪碎石, 使擱淺, 使困惑

한국어 (Korean)
n. - 자갈, 사력층, (병) 요결석
v. tr. - 자갈을 깔다, 난처하게 하다, 화나게 하다

日本語 (Japanese)
n. - 砂利
v. - 砂利を敷く, 当惑させる, 怒らせる

العربيه (Arabic)
‏(الاسم) حصباء او حصمه : حجارة صغيرة لتعبير الطرق (فعل) يفرش او يغطي بالحصمه‏

עברית (Hebrew)
n. - ‮חצץ, חול וחצץ, אבנים, תערובת לציפוי כבישים, אבן בכליות‬
v. tr. - ‮כיסה בחצץ, הביך‬


 
 
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