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The Rock Cycle – the interaction of processes that change rocks from one type to another Create PDF files without this message by purchasing novaPDF printer (http://www.novapdf.com)

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The Rock Cycle – the interaction of processes that change rocks from one type to another

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Steps

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Oxygen The most abundant element in Earth’s

crust.

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Nitrogen The most abundant element in the Earth’s

atmosphere.

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Iron The most abundant element in the Earth’s

core.

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Aluminum The element commercially extracted frp,

bauxite

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Relationships Between All Three Rocks All three rocks are being

recycled and converted to all of the classes

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Igneous Description – forms the bulk of the earth’s

crust. It is the main source of many non-fuel mineral resources.

Classification – Intrusive Igneous Rocks – formed from

the solidification of magma below ground

Extrusive Igneous Rocks – formed from the solidification of lava above ground

Rock Classification

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Igneous (Continued) Examples – Granite, Pumice,

Basalt, Diamond, Tourmaline, Garnet, Ruby, Sapphire

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Sedimentary Description – rock formed from

sediments. Most form when rocks are weathered and eroded into small pieces, transported, and deposited in a body of surface water.

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Clastic – pieces that are cemented together by quartz and calcium carbonate (Calcite). Examples: sandstone (sand stuck together), Conglomerate (rounded & concrete-looking) and Breccia (like conglomerate but w/ angular pieces)

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Sedimentary (Continued) Nonclastic – Chemical Precipitates – limestone

precipitates out and oozes to the bottom of the ocean (this is why there is a lot of limestone in S.A.)

Biochemical Sediments – like peat & coal

Petrified wood & opalized wood

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Metamorphic Description – when preexisting rock is

subjected to high temperatures (which may cause it to partially melt), high pressures, chemically active fluids, or a combination of these

Location – deep within the earth

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Examples: Contact Metamorphism- rock that is next to

a body of magmaEx. limestone under heat becomes marble through crystallization

Limestone -> marble

sandstone -> quartzite

shale -> hornfelds (slate)

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Dynamic Metamorphism – earth movement crushes & breaks rocks along a fault. Rocks may be brittle- (rock and mineral grains are broken and crushed) or it may be ductile-(plastic behavior occurs.)

Rocks formed along fault zones are called mylonites.

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Metamorphic (Continued) Regional Metamorphism – during

mountain building; great quantities of rock are subject to intense stresses and heatEx. cont. shelves ram together

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Progressive Metamorphism – One form of rock changing into another

shale->slate->schist->gneiss

coal->graphite

granite->gneiss

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