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Rocks are classified according to characteristics such as mineral and chemical composition, permeability, texture of the constituent particles, and particle size. These physical properties are the result of the processes that formed the rocks. Over the course of time, rocks can transform from one type into another, as described by a geological model called the rock cycle. This transformation produces three general classes of rock: OKSO Damn right I am a Sooners Fan now and forever custom name cap igneous, sedimentary and metamorphic. Those three classes are subdivided into many groups. There are, however, no hard and fast boundaries between allied rocks. By increase or decrease in the proportions of their minerals, they pass through gradations from one to the other; the distinctive structures of one kind of rock may thus be traced gradually merging into those of another. Hence the definitions adopted in rock names simply correspond to selected points in a continuously graduated series.
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Igneous rock is formed through the cooling and solidification of magma or lava. This magma may 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. Sedimentary rocks are formed at the earth’s surface by the accumulation and cementation of fragments of earlier rocks, minerals, and organisms or as chemical precipitates and organic growths in water . This process causes clastic sediments or organic particles to settle and accumulate, or for minerals to chemically precipitate from a solution. The particulate matter then undergoes compaction and cementation at moderate temperatures and pressures .
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