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ROCKS: Defined
Magma ,[object Object],Crystallization ,[object Object]
may occur beneath the surface or at the surface.,[object Object]
Igneous Rocks Made by Fire
volcanic or extrusive ,[object Object]
 they are extruded onto the surface.plutonic or intrusive ,[object Object]
they intrude existing rocks.,[object Object]
composed of ions that move about freely.Crystallization ,[object Object],[object Object]
slow cooling results in the formation of large crystals.
quick cooling results the formation of solid mass of small intergrown crystals.,[object Object],[object Object]
Porphyritic Texture 	- has large crystals embedded with  a matrix of smaller crystals.
Glassy Texture 	- results when the ions do not have sufficient time to unite into an orderly crystalline structure.
Obsidian ,[object Object],Pumice - volcanic rock that exhibits a glassy texture.
Mineral Composition ,[object Object]
 minerals that form at about the same temperature are found together in the same igneous rock.,[object Object]
Granite ,[object Object]
 slabs of polished granite are commonly used for tombstones, monuments, and as building stones.,[object Object]
 rhyolite deposits are less common and generally less voluminous.,[object Object]
Basaltic Rocks ,[object Object]
 because of their iron content, basaltic rocks are typically darker and denser than granitic rocks.,[object Object]
Andesitic or Intermediate Composition - rocks with a composition between granitic and basiltic rocks.
Peridotite - opposite side of the compositional spectrum from granitic rocks.
Sedimentary Rocks
Sediments are loose, unconsolidated accumulations of mineral rock particles that have been transported by wind, water, ice, or gravity and redeposited. Derived from the Latin sedimentum means settling, reference to a solid material settling out of a fluid.
Formation: ,[object Object]
precipitation of crystals out of solution.
 usually, the particle are broken down further during this transport phase.
 sediment become lithified, or turned to rock.,[object Object]
formed from the products of the mechanical breakup of other rocks.
broken up into smaller and smaller pieces and ultimately, into individual mineral grains.,[object Object]
 other major energy sources (petroleum and natural gas) occur in pores of sedimentary rocks.
other sedimentary rocks are major sources of iron, aluminum, manganese, fertilizer, and sand and gravel.,[object Object]
Classifying Sedimentary Rocks Detrital Sedimentary Rocks ,[object Object]
 the rock is called conglomerate if the sediment is rounded.
the rock is called breccia if the pieces are angular.,[object Object]
Chemical Sedimentary Rocks ,[object Object]
does not remain dissolved in water indefinitely.,[object Object]
Chalk– soft, porous rock made up almost entirely of the hard parts of microscopic organisms. Travertine – type of limestone that decorates taverns.
Coal ,[object Object]
the end product of the burial of large amounts of plant material over extended periods,[object Object]
Lithification of Sediment ,[object Object],Cementation – another important means by which sediments are converted to sedimentary rock.
Features of Sedimentary Rocks
[object Object]
Strata – the single most characteristic feature of sedimentary rocks.
Sedimentary rocks provide geologists with evidence deciphering past environments.,[object Object]
[object Object]
every metamorphic rock has a parent rock – the rock from which it was formed.,[object Object]
most changes occur at the elevated temperatures and pressures that exist in the zone beginning a few kilometers below Earth’s surface and extending into the upper mantle.,[object Object]
Agents of Metamorphism
Heat as a Metamorphic Agent ,[object Object]
it provides energy to drive chemical reactions that result in the recrystallization of existing minerals and/or the formation of new minerals.,[object Object]
Pressure (Stress) as a Metamorphic Content ,[object Object]
the deeper you go in the ocean, the greater you confining pressure.
the for the rock that is buried.,[object Object]
Chemically Active Fluids ,[object Object]
believed to play an important role in some types of metamorphism.
hot fluids aid in the recrystallization of mineral grains by dissolving material from regions of high stress then precipitating this material in areas of low stress.,[object Object]

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Rock Classifications