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Rocks
are made of one or more minerals.
Minerals are natural, inorganic solids. ( Inorganic = made from non-living
materials which do not have carbon ) Each mineral is made of specific
elements and has a specific crystal structure. A mineral may be one
element such as copper (Cu) or gold (Au), or it may be a mixture of
several elements. About 2,500 different minerals have been described.
There
are three kinds of rocks: Igneous, Sedimentary, and Metamorphic.
Igneous Rocks
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Igneous
rocks are made from lava or magma. Lava and magma are made of
hot, melted minerals. Lava is found on or near the Earth's surface.
Magma is found far beneath the Earth's surface.
Extrusive igneous rocks are made from lava that cooled quickly.
Extrusive rocks generally have either no crystals or very tiny
crystals. Intrusive igneous rocks are made from slow-cooling magma.
Intrusive rocks have large crystals.
Extrusive
Igneous Rocks: pumice, basalt, obsidian, scoria, rhyolite, andesite
Intrusive Igneous Rocks: granite, gabbro, diorite
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Sedimentary
Rocks
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On
Earth's surface, wind, ice, and water can break rock into pieces.
They can also carry rock pieces to another place. Usually, the
rock pieces, called sediments, drop from the wind or water to
make a layer. The layer can be buried under other layers of sediments.
Sometimes, the sediments can even be made from seashells and bodies
of plants and animals. Fossils are found in sedimentary rocks.
After a long time the sediments can be cemented together to make
sedimentary rock. In this way, igneous rock can become sedimentary
rock.
Detrital sedimentary rocks are made from broken pieces of other
rocks.
Chemical sedimentary rocks
Organic sedimentary rocks are made from the bodies of dead animals
or plants.
Detrital
Sedimentary Rocks: sandstone, shale, siltstone, conglomerate,
coal
Chemical Sedimentary Rocks: chemical limestone, halite
Organic Sedimentary Rocks: fossil-rich limestone, coquina, coal
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Metamorphic
Rocks
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Metamorphic
rocks are made from older rocks, either igneous or sedimentary.
These rocks are changed by great heat and/or pressure deep beneath
the earth's surface. The heat and pressure makes crystals in the
rock. If the rock already has crystals, the heat makes the crystals
larger. Sometimes the pressure flattens the crystals into layers.
With great heat and pressure, these rocks change to:
| granite |
gneiss |
| shale |
slate |
| slate |
phyllite,
schist, gneiss |
| basalt |
gneiss |
| sandstone |
quartzite |
| limestone |
marble |
Foliated
metamorphic rocks have layers or bands of crystals. (slate, gneiss)
Nonfoliated metamorphic rocks do not have layers or bands of crystals.
(marble, quartzite)
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