Sandstone (redirected from Sandstones)

sandstone, sedimentary rock formed by the cementing together of grains of sand. The usual cementing material in sandstone is calcium carbonate, iron oxides, or silica, and the hardness of sandstone varies according to the character of the cementing material; quartz sandstones cemented with quartz are the hardest. Sandstones are commonly gray, buff, red, or brown although green and some other colors are also found. Green sandstones often contain, in addition to sand and glauconite, fossil shells and iron oxides; those that break apart easily are known as greensands and are sometimes used to replenish depleted potash in soils. Sandstones are widely used in construction and industry. Varieties of sandstone include arkose, which contains feldspar and resembles granite, and graywacke, a gray or sometimes greenish or black rock composed of quartz and fledspar with numerous fragments of other rocks, such as shale, slate, quartzite, granite, and basalt. Sandstone may be crushed to the form of loose sand grains, which can then be put to the same industrial uses as sand. See brownstone.

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sandstone

Sedimentary rock formed from sand-sized grains (0.0025–0.08 in., or 0.06–2 mm, in diameter). The spaces between grains may be empty or filled with either a chemical cement of silica or calcium carbonate or a fine-grained matrix of silt and clay particles. The principal mineral constituents of the grain framework are quartz, feldspar, and rock fragments. Sandstones are quarried for use as building stone. Because of their abundance, diversity, and mineralogy, sandstones are also important to geologists as indicators of erosional and depositional processes. See also graywacke.

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sandstone

any of a group of common sedimentary rocks consisting of sand grains consolidated with such materials as quartz, haematite, and clay minerals: used widely in building

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sandstone [′san‚stōn]

(petrology)

A detrital sedimentary rock consisting of individual grains of sand-size particles 0.06 to 2 millimeters in diameter either set in a fine-grained matrix (silt or clay) or bonded by chemical cement.

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sandstone

Sedimentary rock composed of sand-sized grains, naturally cemented by mineral materials. In most sandstone used for building, quartz grains predominate; often used for decorative elements in buildings because it is easy to carve.

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Sandstone 

a sedimentary rock composed of sand grains cemented by clay, carbonate, siliceous, or other material. Like sand, sandstones are divided into small-grain (0.1–0.25 mm), medium-grain (0.25–0.5 mm), and large-grain (0.5 mm) varieties according to the predominant particle size. They are also divided mineralogically into monomineral and polymineral quartz sandstones, arkosic sandstones, and graywackes.

The density of sandstone is 2,250–2,670 kg per cu m; its porosity is 0.69–6.70 percent, and its water absorption, 0.63–6.0 percent. Sandstone with siliceous and carbonate cementing material has the best physicomechanical properties, and sandstone with clay cement, the poorest. The refractoriness of sandstone also differs, with the greatest heat resistance (up to 1,700°C) characteristic for pure quartz sandstone with siliceous cement. Sandstone is used in construction as wall and facing material and in rubble work. It is also used to make gravel for road building and concrete-making. Quartz sandstone with a SiO₂ content of more than 95 percent is used in the production of Dinas brick, as a flux in smelting copper and nickel, and in manufacturing glass.