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The Rock CycleRock – mixture of minerals, glass or organic matter.
Granite: igneous rockMica
Plagioclase
Orthoclase
Horneblend
quartz
Rock CycleOlder rocks are recycled to make younger rocks.Various processes that alter the rocks;
MeltingTemperature and pressureWeathering, erosion and deposition
Three basic rock groups are formed:
Igneous – melting and cooling
Sedimentary – weathering, erosion and deposition
• Cementing and compacting
Metamorphic – temperature and pressure
Igneous Rocks
Formed from molten material in earth’s crust that emerges or remains in earth’s crust.
Magma – liquid rock UNDER crust
Lava – liquid rock ON crust
Two kinds of igneous rocks
Intrusive igneous rocks –
Cooled slowly
Texture – coarse grained - time for large crystal growth
Found in surface of earth after weathering
Pumice Frothy or Glassy threadsSilica basedGases emitted from lava at explosion cause strings that make threadsSo light it floats on water
Scoria
Large holes made by gas escaping from lava
Volcanic cinders
Lava rock
Basaltic – darker than pumice
Igneous rock classified by composition
Basalt – dense, heavy, dark colored
- rich in Fe and Mg
- lava quick moving
- ocean bottoms
Granitic – light colored, lower density
- magma thick contains Si and O2
- continental plates
- contains great deal of gases (explosive)
Andesite Andesite – between basalt and granite
- violent eruptions
Igneous rocks can be classified by;
CompositionBasalt – ferromagnesium – Fe and Mg
Granite – potassium and silicates SiO2
Texture:Large crystalsSmall/no crystals
Place of cooling:Intrusiveextrusive