3 types of rocks.ppt
TRANSCRIPT
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3 types of rocks
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3 types of rocks• There are 3 types of
rocks found on Earth: – Igneous –
Sedimentary – Metamorphic
• Knowing thedi erences between
these 3 types ofrocks allows us tolearn about Earth spast!
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Igneous "ocks # $ormation• Igneous "ocks are
formed by melting,cooling, and crystallization ofother rocks!
• Igneous rocks form asa result of volcanicactivity, hot spots,and melting thatoccurs in themantle !
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Igneous rocks• Igneous rocks are common along plate
boundaries or mantle hot spots
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Igneous "ocks #%lassi&cation
• Igneous rocks areclassi&ed using theirte'ture in the following
ways: – (lassy – )phanitic *no +isible
crystals, – -haneritic *+isible
crystals, – -orphyritic *Some +isible
and some not +isible
crystals,
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Igneous "ocks # Te'ture• %rystal si.e is used
to classify igneousrocks!
•
%rystals form as therock cools/ and thecrystal si.e can tellus a lot about its
cooling history: – The larger the
crystals, theslower it cooled.
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Igneous "ocks # Te'ture• Glassy igneous
rocks ha+e nocrystal structure/and probablyformed by +eryrapid cooling *suchas on the surface
of a la+a/ or whena la+a enters thewater!,
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Igneous "ocks # Te'ture• Aphanitic rocks
ha+e no +isiblecrystals/ and
probably formed byfast cooling abo+eground!
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Igneous "ocks # Te'ture• Phaneritic rocks
ha+e +isiblecrystals/ and
probably formed byslow cooling belowground!
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Igneous "ocks # Te'ture• Porphyritic rocks
ha+e both +isibleand non+isible
crystals/ andprobably formed bytwo di erentcooling e+ents!
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Igneous "ocks #%lassi&cation
• Dark igneous rocks areformed from basaltic orma&c magma! *Ma&cbecause it contains a lotof magnesium and iron,!
• The magma that formsthese rocks is usually+ery hot *around01112%, and +iscous*about the same+iscosity as ketchup!,
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Igneous "ocks #%lassi&cation
• Light colored igneousrocks are formed fromsilicic *high silicacontent, or felsicmagmas!
• The magmas that formthese rocks is usuallymore cool/ *lower than
412%,/ and more+iscous *about the+iscosity of peanutbutter!,
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Igneous rocks # $ormations•
Structures andformations seen inigneous rocksinclude:
– 5e'agonalcolumnar 6oints
– -ahoehoe la+a7ows
– 8ikes/ sills/ andbatholiths*plutons,
– -illow basalts – 9olcanoes
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Igneous "ocks # E'amples• The most common
types of igneousrocks include:
–
"hyolite – )ndesite – asalt – Granite – 8iorite – (abbro
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Igneous rocks charted
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Sedimentary "ocks #$ormation
• Sedimentary rocks areformed byweathering, erosion,deposition,compaction, andcementation of otherrocks!
• Sedimentary rocks
form in areas wherewater, wind, orgravity depositsediments.
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Sedimentary rocks #formation
• Sedimentary rocksare likely to form inareas such as:
–
8eltas – <eaches – "i+ers – (laciers – Sand dunes – Shallow seas – 8eep oceans
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Sedimentary rocks #%lassi&cation
• Sedimentary rocksare classi&ed intotwo groups:
–
%lastic rocks – %hemically formed
rocks
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Sedimentary rocks =%lassi&cation
• Sedimentary rocksare !lastic if theyare made of piecesof other rocks thatha+e beenweathered anderoded!
•
%lastic rocks aregrouped based onthe si.e of grain thatthey are made from!
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Sedimentary rocks #%lassi&cation
• 9ery small particlesmake up mudrock!
• Medium si.ed
particles make upsandstone!
• >arge particlesmake upconglomerates!
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Sedimentary rocks #%lassi&cation
• Sedimentary rocksthat form fromchemical processes
are calledbiochemical rocks*formed from li+ingthings, or !hemical
precipitates*formed from lakesor shallow seas!,
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Sedimentary rocks #formations
• Structures andformations seen insedimentary rocks
include: – Strati&cation – %ross bedding – (raded bedding – "ipple marks – Mud cracks – $ossils
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Sedimentary rocks #E'amples
• Some of the mostcommon types ofsedimentary rocksinclude:
– %onglomerate – Sandstone – Shale – >imestone – (ypsum – ?olites – %hert *including black
7int and red 6asper,
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Sedimentary rocks # Story• hat do you know
about the history ofthe Earth in the
place where thisrock was found;
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Metamorphic rocks #$ormation
• Metamorphic rocksare formed by heatand pressure changing one type ofrock into anothertype of rock!
• Metamorphic rocksform near lavaintrusions / at platesubduction zones /and in deepmountain roots !
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Metamorphic rocks #$ormation
• >a+a intrusions canpro+ide heat thatcauses
metamorphic rocksto form! Thesesmall areas ofmetamorphic rock
form from contactmetamorphosis.
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Metamorphic rocks #$ormation
• "ocks thatmetamorphosebecause ofincreasing heat andpressure found atplate subduction.ones and in deepmountain roots form
large areas ofmetamorphic rockthrough regionalmetamorphosis.
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Metamorphic rocks #%lassi&cation
• Metamorphic rocksare classi&ed into @ma6or groups:
–
$oliated – Aonfoliated
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Metamorphic rocks #%lassi&cation
• "oliated rocks form whendi erential pressurecauses minerals to formin layers!
• These rocks will ha+estripes or planes that theywill break easily along!
• These BstripesC don tusually line up with theoriginal bedding planes insedimentary rocks!
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Metamorphic rocks• #on$oliated
metamorphic rocksformed in areas
where the pressurefrom all sides waseDual/ so there isno BlinearC Duality
to the rocks!
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Metamorphic rocks #$ormations
• Structures andformations seen inmetamorphic rocks
include: – $olding – -lastic deformation – Stretching – )lternating dark
and light layers*gneissic foliation,
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Metamorphic rocks #E'amples
• Some common typesof metamorphic rockinclude:
– Slate – Schist – (neiss – )mphibolite –
Marble – uart.ite – Metaconglomerate
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Metamorphic rocks #%harted
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Metamorphic rocks # story• hat do you know
about the history ofthe Earth in the
place where thisrock was found;