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Rock or stone is a natural substance, a solid "aggregate of one or more "minerals or "mineraloids. For example, "granite, a common rock, is a combination of the minerals "quartz, "feldspar and "biotite. The Earth's outer solid layer, the "lithosphere, is made of rock.

Rock has been used by mankind throughout history. The minerals and metals found in rocks have been essential to human civilization.[1]

Three major groups of rocks are defined: "igneous, "sedimentary, and "metamorphic. The scientific study of rocks is called "petrology, which is an essential component of geology.

Contents

Classification[edit]

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Rock outcrop along a mountain creek near "Orosí, "Costa Rica.

At a granular level, rocks are composed of grains of minerals, which, in turn, are "homogeneous solids formed from a "chemical compound that is arranged in an orderly manner. The "aggregate minerals forming the rock are held together by "chemical bonds. The types and abundance of minerals in a rock are determined by the manner in which the rock was formed. Many rocks contain "silica (SiO2); a compound of "silicon and "oxygen that forms 74.3% of the "Earth's crust. This material forms "crystals with other compounds in the rock. The proportion of silica in rocks and minerals is a major factor in determining their name and properties.[2]

Rocks are geologically classified according to characteristics such as mineral and chemical composition, "permeability, the "texture of the constituent particles, and "particle size. These physical properties are the end result of the processes that formed the rocks.[3] Over the course of time, rocks can transform from one type into another, as described by the geological model called the "rock cycle. These events produce three general classes of rock: "igneous, "sedimentary, and "metamorphic.

The three classes of rocks are subdivided into many groups. However, there are no hard and fast boundaries between allied rocks. By increase or decrease in the proportions of their constituent minerals they pass by every gradation into one another, the distinctive structures also of one kind of rock may often be traced gradually merging into those of another. Hence the definitions adopted in establishing rock nomenclature merely correspond to more or less arbitrary selected points in a continuously graduated series.[4]

Igneous rock[edit]

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Sample of igneous "gabbro

"Igneous rock (derived from the "Latin word igneus meaning of fire, from ignis meaning fire) forms through the cooling and "solidification of "magma or "lava. This magma can be derived from partial melts of pre-existing rocks in either a "planet's "mantle or "crust. Typically, the melting of rocks is caused by one or more of three processes: an increase in temperature, a decrease in pressure, or a change in composition.

Igneous rocks are divided into two main categories: "plutonic rock and "volcanic. "Plutonic or "intrusive rocks result when magma cools and "crystallizes slowly within the "Earth's crust. A common example of this type is "granite. Volcanic or "extrusive rocks result from magma reaching the surface either as "lava or fragmental ejecta, forming minerals such as "pumice or "basalt.[3] The chemical abundance and the rate of cooling of magma typically forms a sequence known as "Bowen's reaction series. Most major igneous rocks are found along this scale.[2]

About 64.7% of the Earth's crust by volume consists of igneous rocks; making it the most plentiful category. Of these, 66% are basalts and "gabbros, 16% are granite, and 17% "granodiorites and "diorites. Only 0.6% are "syenites and 0.3% "peridotites and "dunites. The oceanic crust is 99% basalt, which is an igneous rock of "mafic composition. Granites and similar rocks, known as meta-granitoids, form much of the continental crust.[5] Over 700 types of igneous rocks have been described, most of them having formed beneath the surface of "Earth's "crust. These have diverse properties, depending on their composition and the temperature and pressure conditions in which they were formed.

Sedimentary rock[edit]

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Sedimentary "sandstone with "iron oxide bands

"Sedimentary rocks are formed at the earth's surface by the accumulation and cementation of fragments of earlier rocks, minerals, and organisms[6] or as chemical precipitates and organic growths in water ("sedimentation). This process causes "clastic "sediments (pieces of rock) or "organic particles ("detritus) to settle and accumulate, or for minerals to chemically "precipitate ("evaporite) from a "solution. The particulate matter then undergoes compaction and "cementation at moderate temperatures and pressures ("diagenesis).

Before being deposited, sediments are formed by "weathering of earlier rocks by "erosion in a source area and then transported to the place of deposition by "water, "wind, "ice, "mass movement or "glaciers (agents of "denudation). Mud rocks comprise 65% ("mudstone, "shale and "siltstone); "sandstones 20 to 25% and "carbonate rocks 10 to 15% ("limestone and "dolostone).[3] About 7.9% of the crust by volume is composed of sedimentary rocks, with 82% of those being shales, while the remainder consists of limestone (6%), sandstone and "arkoses (12%).[5] Sedimentary rocks often contain "fossils. Sedimentary rocks form under the influence of gravity and typically are deposited in horizontal or near horizontal layers or "strata and may be referred to as stratified rocks. A small fraction of sedimentary rocks deposited on steep slopes will show cross bedding where one layer stops abruptly along an interface where another layer eroded the first as it was laid atop the first.

Metamorphic rock[edit]

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Metamorphic banded "gneiss

"Metamorphic rocks are formed by subjecting any rock type—"sedimentary rock, "igneous rock or another older metamorphic rock—to different "temperature and "pressure conditions than those in which the original rock was formed. This process is called "metamorphism; meaning to "change in form". The result is a profound change in physical properties and chemistry of the stone. The original rock, known as the "protolith, transforms into other mineral types or other forms of the same minerals, by "recrystallization.[3] The temperatures and pressures required for this process are always higher than those found at the Earth's surface: temperatures greater than 150 to 200 °C and pressures of 1500 bars.[7] Metamorphic rocks compose 27.4% of the crust by volume.[5]

The three major classes of metamorphic rock are based upon the formation mechanism. An intrusion of magma that heats the surrounding rock causes contact metamorphism—a temperature-dominated transformation. Pressure metamorphism occurs when sediments are buried deep under the ground; pressure is dominant, and temperature plays a smaller role. This is termed burial metamorphism, and it can result in rocks such as "jade. Where both heat and pressure play a role, the mechanism is termed regional metamorphism. This is typically found in mountain-building regions.[2]

Depending on the structure, metamorphic rocks are divided into two general categories. Those that possess a texture are referred to as "foliated; the remainders are termed non-foliated. The name of the rock is then determined based on the types of minerals present. "Schists are foliated rocks that are primarily composed of "lamellar minerals such as "micas. A "gneiss has visible bands of differing "lightness, with a common example being the granite gneiss. Other varieties of foliated rock include "slates, "phyllites, and "mylonite. Familiar examples of non-foliated metamorphic rocks include "marble, "soapstone, and "serpentine. This branch contains "quartzite—a metamorphosed form of "sandstone—and "hornfels.[2]

Human use[edit]

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Ceremonial "cairn of rocks, an "ovoo, from "Mongolia

The use of rocks has had a huge impact on the cultural and technological development of the human race. Rocks have been used by humans and other "hominids for at least "2.5 million years.[8] "Lithic technology marks some of the oldest and continuously used technologies. The "mining of rocks for their "metal "ore content has been one of the most important factors of human advancement, which has progressed at different rates in different places in part because of the kind of metals available from the rocks of a region.

Mining[edit]

Mining is the extraction of "valuable "minerals or other "geological materials from the earth, from an "ore body, "vein or ("coal) seam. This term also includes the removal of soil. Materials recovered by mining include "base metals, "precious metals, "iron, "uranium, "coal, "diamonds, "limestone, "oil shale, "rock salt and "potash. Mining is required to obtain any material that cannot be grown through "agricultural processes, or created "artificially in a "laboratory or "factory. Mining in a wider sense comprises extraction of any "resource (e.g. "petroleum, "natural gas, "salt or even "water) from the earth.[9]

Mining of rock and metals has been done since "prehistoric times. Modern mining processes involve "prospecting for ore bodies, analysis of the profit potential of a proposed mine, extraction of the desired materials and finally reclamation of the land to prepare it for other uses once mining ceases.[10]

The nature of mining processes creates a potential negative impact on the environment both during the mining operations and for years after the mine has closed. This impact has led to most of the world's nations adopting regulations to manage negative effects of mining operations.[11]

See also[edit]

References[edit]

  1. ^ Roberts, Dar. "Rocks and classifications". Department of Geography, University of California, Santa Barbara. Archived from the original on 31 October 2012. Retrieved 11 November 2012. 
  2. ^ a b c d Wilson, James Robert (1995), A collector's guide to rock, mineral & fossil localities of Utah, Utah Geological Survey, pp. 1–22, "ISBN "1557913366, archived from the original on 19 November 2016. 
  3. ^ a b c d Blatt, Harvey; Tracy, Robert J. (1996). Petrology (2nd ed.). W. H. Freeman. "ISBN "0-7167-2438-3. 
  4. ^ ""Public Domain One or more of the preceding sentences incorporates text from a publication now in the "public domainChisholm, Hugh, ed. (1911). "Petrology". "Encyclopædia Britannica (11th ed.). Cambridge University Press. 
  5. ^ a b c Bucher, Kurt; Grapes, Rodney (2011), Petrogenesis of Metamorphic Rocks, Springer, pp. 23–24, "ISBN "3540741682, archived from the original on 19 November 2016. 
  6. ^ Gilluly, James (1959). Principles of Geology. W.H. Freeman. Archived from the original on 7 November 2017. 
  7. ^ Blatt, Harvey and Robert J. Tracy, Petrology, W.H.Freeman, 2nd ed., 1996, p.355 "ISBN "0-7167-2438-3
  8. ^ William Haviland, Dana Walrath, Harald Prins, Bunny McBride, Evolution and Prehistory: The Human Challenge, p. 166
  9. ^ Botin, J.A., ed. (2009). Sustainable Management of Mining Operations. Denver, CO, USA: Society for Mining, Metallurgy, and Exploration. "ISBN "9780873352673. 
  10. ^ Wilson, Arthur (1996). The Living Rock: The Story of Metals Since Earliest Times and Their Impact on Developing Civilization. Cambridge, England: Woodhead Publishing. "ISBN "1855733013. 
  11. ^ Terrascope. "Environmental Risks of Mining". The Future of strategic Natural Resources. Cambridge, MA, USA: Massachusetts Institute of Technology. Archived from the original on 20 September 2014. Retrieved 10 September 2014. 

External links[edit]

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