The rock cycle is relevant to the study of minerals
and gemstones because it explains how they are formed. Minerals form
at different points of the cycle.
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6.Rock of Continental Crust
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1.Erosion, Transport, Deposition
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5.Igneous Rock
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2.Sediment
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4.Metamorphic Rock
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3.Sedimentary Rock
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The rock cycle shown above operates in an anticlockwise
direction.
If we begin at point 1, products of erosion, transport
and deposition become sedimentary rock (on a long time scale) after
being subjected to pressure by compaction. Then metamorphism may occur
(rocks are altered by heat and or pressure) and there may be chemical
reactions and the formation of metamorphic rock.
When metamorphic or sedimentary rocks subside they
may reach depths at which internal processes can melt rock and convert
it to magma. When this rises to the surface (via volcanoes) igneous
rock is formed. If uplift occurs erosion, transportation and deposition
begin again.
These processes are occurring today and have done throughout
the earth's history. Minerals and gemstones are formed at different
points on the cycle.
