TOP TEN / / ROCKS.
Dictionary definition:
- Relatively hard, naturally formed mineral or petrified matter; stone.
- A relatively small piece or fragment of such material. A relatively large body of such material, as a cliff or peak.
- A naturally formed aggregate of mineral matter constituting a significant part of the earth's crust.
- One that is similar to or suggestive of a mass of stone in stability, firmness, or dependability: The family has been his rock during this difficult time.
Wiki definition:
In geology, rock or stone is a naturally occurring solid aggregate of minerals and/or mineraloids.
The Earth's outer solid layer, the lithosphere, is made of rock. In general, rocks are of three types, namely igneous, sedimentary, and metamorphic. The scientific study of rocks is called petrology, and petrology is an essential component of geology.
Different types of rock:
Igneous
- Andesite - an Intermediate volcanic rock
- Anorthosite - an igneous ultramafic rock composed predominantly of plagioclase
- Aplite - a very fine grained intrusive igneous rock
- Basalt - a volcanic rock of mafic composition
- Basanite - a volcanic rock of mafic composition; essentially a silica undersaturated basalt
- Boninite - a high-magnesian basalt dominated by pyroxene
- Carbonatite - a rare igneous rock composed of >50% carbonate minerals
- Charnockite - a type of granite containing pyroxene
- Enderbite - a variety of charnockite
- Dacite - a felsic to intermediate volcanic rock with high iron content
- Diabase or dolerite - an intrusive mafic rock forming dykes or sills
- Diorite - a coarse grained intermediate plutonic rock composed of plagioclase, pyroxene and/or amphibole
- Dunite - an ultramafic cumulate rock composed of olivine and accessories
- Essexite - a silica undersaturated mafic plutonic rock (essentially a foid-bearing gabbro)
- Foidolite - a plutonic igneous rock composed of >90% feldspathoid minerals
- Gabbro - a coarse grained plutonic rock composed of pyroxene and plagioclase basically equivalent to basalt
- Granite - a coarse grained plutonic rock composed of orthoclase, plagioclase and quartz
- Granodiorite - a granitic plutonic rock with plagioclase > orthoclase
- Granophyre - a subvolcanic intrusive rock of granitic composition
- Harzburgite - a variety of peridotite; an ultramafic cumulate rock
- Hornblendite - a mafic or ultramafic cumulate rock dominated by >90% hornblende
- Hyaloclastite - a volcanic rock composed primarily of glasses and glassy tuff
- Icelandite - a volcanic rock
- Ignimbrite - a fragmental volcanic rock
- Ijolite - a very rare silica-undersaturated plutonic rock
- Kimberlite - a rare ultramafic, ultrapotassic volcanic rock and a source of diamonds
- Komatiite - an ancient ultramafic volcanic rock
- Lamproite - an ultrapotassic volcanic rock
- Lamprophyre - an ultramafic, ultrapotassic intrusive rock dominated by mafic phenocrysts in a feldspar groundmass
- Latite - a silica undersaturated form of andesite
- Lherzolite - an ultramafic rock, essentially a peridotite
- Monzogranite - a silica undersaturated granite with <5% normative quartz
- Monzonite - a plutonic rock with <5% normative quartz
- Nepheline syenite - a silica undersaturated plutonic rock with nepheline replacing orthoclase
- Nephelinite - a silica undersaturated plutonic rock with >90% nepheline
- Norite - a hypersthene bearing gabbro
- Obsidian - a type of volcanic glass
- Pegmatite - an igneous rock (or metamorphic rock) with giant sized crystals
- Peridotite - a plutonic or cumulate ultramafic rock composed of >90% olivine
- Phonolite - a silica undersaturated volcanic rock; essentially similar to nepheline syenite
- Picrite - an olivine-bearing basalt
- Porphyry - a rock, usually granitic, with a porphyritic texture
- Pumice - a fine grained, extremely vesicular volcanic rock
- Pyroxenite - a coarse grained plutonic rock composed of >90% pyroxene
- Quartz diorite - a diorite with >5% modal quartz
- Quartz monzonite - an intermediate plutonic rock, essentially a monzonite with 5-10% modal quartz
- Rhyodacite - a felsic volcanic rock which is intermediate between a rhyolite and a dacite
- Rhyolite - a felsic volcanic rock
- Comendite - a peralkaline rhyolite
- Pantellerite - an alkaline rhyolite-rhyodacite with amphibole phenocrysts
- Scoria - an extremely vesicular mafic volcanic rock
- Sovite - a coarse grained carbonatite rock
- Syenite - a plutonic rock dominated by orthoclase feldspar; a type of granitoid
- Tachylyte - essentially a basaltic glass
- Tephrite - a silica undersaturated volcanic rock; can be a generic term
- Tonalite - a plagioclase-dominant granitoid
- Trachyandesite - an alkaline intermediate volcanic rock
- Benmoreite - sodic trachyandesite
- Basaltic trachyandesite
- Mugearite - sodic basaltic trachyandesite
- Shoshonite - potassic basaltic trachyandesite
- Trachyte - a silica undersaturated volcanic rock; essentially a feldspathoid-bearing rhyolite
- Troctolite - a plutonic ultramafic rock containing olivine, pyroxene and plagioclase
- Trondhjemite - a form of tonalite where plagioclase-group feldspar is oligoclase
- Tuff - a fine grained volcanic rock formed from volcanic ash
- Websterite - a type of pyroxenite, composed of clinoproxene and orthopyroxene
- Wehrlite - an ultramafic plutonic or cumulate rock, a type of peridotite, composed of olivine and clinopyroxene
- Argillite - a sedimentary rock composed primarily of clay-sized particles
- Arkose - a sedimentary rock similar to sandstone
- Banded iron formation - a fine grained chemical sedimentary rock composed of iron oxide minerals
- Breccia - a sedimentary or tectonic rock composed of fragments of other, broken rocks
- Cataclasite - a rock formed by faulting
- Chalk - a sedimentary rock composed primarily of coccolith fossils
- Chert - a fine grained chemical sedimentary rock composed of silica
- Claystone - a sedimentary rock formed from clay
- Coal - a sedimentary rock formed from organic matter
- Conglomerate - a sedimentary rock composed of large rounded fragments of other rocks
- Diamictite - a poorly sorted conglomerate
- Coquina - a sedimentary carbonate rock formed by accumulation of abundant shell fossils and fragments
- Diatomite - a sedimentary rock formed from diatom fossils
- Dolomite or dolostone - a carbonate rock composed of the mineral dolomite +/- calcite
- Evaporite - a chemical sedimentary rock formed by accumulation of minerals after evaporation
- Flint - a form of chert
- Greywacke - an immature sandstone with quartz, feldspar and rock fragments within a clay matrix
- Gritstone - essentially a coarse sandstone formed from small pebbles
- Itacolumite - porous, yellow sandstone
- Jaspillite - an iron-rich chemical sedimentary rock similar to chert or banded iron formation
- Laterite - a residual sedimentary rock formed from a parent rock under tropical conditions
- Lignite - a sedimentary rock composed of organic material; otherwise known as Brown Coal
- Limestone - a sedimentary rock composed primarily of carbonate minerals
- Marl - a limestone with a considerable proportion of silicate material
- Mudstone - a sedimentary rock composed of clay and muds
- Oil shale - a sedimentary rock composed dominantly of organic material
- Oolite - a chemical sedimentary limestone
- Sandstone - a clastic sedimentary rock defined by its grain size
- Shale - a clastic sedimentary rock defined by its grain size
- Siltstone - a clastic sedimentary rock defined by its grain size
- Travertine - a sedimentary rock containing calcite and iron oxides
- Turbidite - a particular sequence of sedimentary rocks which form within the deep ocean environment
- Wackestone - a matrix-supported carbonate sedimentary rock.
- Amphibolite - a metamorphic rock composed primarily of amphibole
- Blueschist - a metamorphic rock composed of sodic amphiboles with a distinct blue color
- Eclogite - an ultra-high grade metamorphosed basalt or gabbro; also a facies of metamorphic rocks
- Gneiss - a coarse grained metamorphic rock
- Gossan - the product of the weathering of a sulfide rock or ore body
- Granulite - a high grade metamorphic rock formed from basalt; also a facies of metamorphic rocks
- Greenschist - a generic term for a mafic metamorphic rock dominated by green amphiboles
- Hornfels - a metamorphic rock formed by heating by an igneous rock
- Marble - a metamorphosed limestone
- Migmatite - a high grade metamorphic rock verging upon melting into a magma
- Mylonite - a metamorphic rock formed by shearing
- Pelite - a metamorphic rock with a protolith of clay-rich (siltstone) sedimentary rock
- Phyllite - a low grade metamorphic rock composed mostly of micaceous minerals
- Psammite - a metamorphic rock with a protolith of quartz-rich (sandstone) sedimentary rock
- Pseudotachylite - a glass formed by melting within a fault via friction
- Quartzite - a metamorphosed sandstone typically composed of >95% quartz
- Schist - a low to medium grade metamorphic rock
- Serpentinite - a metamorphosed ultramafic rock dominated by serpentine minerals
- Skarn - a metasomatic rock
- Slate - a low grade metamorphic rock formed from shale or silts
- Suevite - a rock formed by partial melting during a meteorite impact
- Talc carbonate - a metamorphosed ultramafic rock with talc as an essential constituent; similar to a serpentinite
- Whiteschist - a high pressure metamorphic rock containing talc + kyanite
Rock classification.
From what I remember of YR7 science, different types of rock are grouped into either:
Metamorphic / / Sedimentary / / Igneous.
Rocks are generally classified by mineral and chemical composition, by the texture of the constituent particles and by the processes that formed them. These indicators separate rocks into igneous, sedimentary, and metamorphic. They are further classified according to particle size. The transformation of one rock type to another is described by the geological model called the rock cycle.
Igneous rocks are formed when molten magma cools and 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 (example granite), while volcanic or extrusive rocks result from magma reaching the surface either as lava or fragmental ejecta (examples pumice and basalt).[1]
Sedimentary rocks are formed by deposition of either clastic sediments, organic matter, or chemical precipitates (evaporites), followed by compaction of the particulate matter and cementation during diagenesis. Sedimentary rocks form at or near the Earth's surface. Mud rocks comprise 65% (mudstone, shale and siltstone); sandstones 20 to 25% and carbonate rocks 10 to 15% (limestone and dolostone).[1]
Metamorphic rocks are formed by subjecting any rock type (including previously formed metamorphic rock) to different temperature and pressure
conditions than those in which the original rock was formed. These
temperatures and pressures are always higher than those at the Earth's
surface and must be sufficiently high so as to change the original
minerals into other mineral types or else into other forms of the same
minerals (e.g. by recrystallization).[1]
The three classes of rocks—the igneous, the sedimentary and the
metamorphic—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 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 selected points (more or less arbitrary) in a continuously
graduated series.
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 more than 2 million years. 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.
The prehistory and history of civilization is classified into the Stone Age, Bronze Age, and Iron Age. Although the Stone Age has ended virtually everywhere, rocks continue to be used to construct buildings and infrastructure. When so used, rocks are called dimension stone.
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