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Rock On!. By: Kelcie Kawakami, Katie Guza, Lauren Masters, Nicole Warburton, Laura Newcombe. What is Rock?. Consolidated or unconsolidated solid mineral matter Different types of rock: Igneous Sedimentary Metamorphic. Rock Cycle. The Rock Cycle. Began when earth was volcanic - PowerPoint PPT Presentation
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What is Rock?What is Rock? Consolidated or
unconsolidated solid mineral matter
Different types of rock:
IgneousSedimentary Metamorphic
The Rock CycleThe Rock Cycle
Began when earth was volcanicIgneous rocks are broken into sediments
by erosion and weatheringThey’re compacted together to form
sedimentary rocks
The Rock CycleThe Rock Cycle
Then, they were buried underground and the head and pressure made them metamorphic rocks
Then, they meet again and become igneous rock
Part 1 of the Rock CyclePart 1 of the Rock Cycle
It starts with a volcanic eruption.
Depending on where the lava cools, it can make one of two types of igneous rock.
MagmaMagma Molten/partially molten
rock beneath the earths surface
Magma forms when rock is heated by high temperatures beneath the earth’s surface (between 625 and 1200° Celsius)
MagmaMagma
Products used for road -building, construction, manufacturing, landscaping
Crushed lava rockPumiceCinders
MagmaMagmaThey’re good for
pollution-free thermal/electric energy
ex. Steam from the geysers of No. Cal has enough energy to produce the electricity needed for San Francisco
Igneous RocksIgneous Rocks
Factors that influence when melting occurs are:
Chemistry, material, pressure, presence of gases in the rock
GraniteGranite
Formed by slowly cooling pockets of magma trapped under earth
Used for long-lasting monuments, decoration etc
Extrusive RocksExtrusive Rocks
Above GroundWhen volcanoes
erupt, the magma that is visible above the earth is called lava
Intrusive RocksIntrusive Rocks
Below GroundFormed when
magma from deep within the earth is trapped
When its cooled, it’s called igneous
Part 2 Of the Rock CyclePart 2 Of the Rock Cycle Particles from the earth are transported down
Creates a level of sediment–Makes sedimentary rocks.
Four cycles of Sedimentary rocks:WeatheringTransportationDeposition Lithification.
Sedimentary RocksSedimentary Rocks
Made as layers of material settle into each other over time
They’re created from hardened sediment, therefore they are sedimentary rocks
Spotting Sedimentary Rocks
Spotting Sedimentary Rocks
Layers, bands, or stripes across them
Contain fossils of animals and plants
Scrapes easily Crumbles easily
Clastic and Nonclastic Sedimentary Rocks
Clastic and Nonclastic Sedimentary Rocks
Both contain:FossilsRipple marksMud cracksRaindrops from when the rock was formed
Clastic Sedimentary RocksClastic Sedimentary Rocks
Formed by weatherExamples–When rocks
break down into pebbles, sand, or clay due to wind, ice, and water
Nonclastic Sedimentary Rocks
Nonclastic Sedimentary Rocks
Formed from chemical reactions (usually in the ocean)
Examples:LimestoneRock SaltRock GypsumChert
Classification of Sedimentary Rocks
Classification of Sedimentary Rocks
ConglomerateCoarse, rounded grains64mm-256mm
BrecciaCoarse, angular grains2mm-64mm
SandstoneGrains2mm-1/16mm
Shale
Part 3 Of the Rock CyclePart 3 Of the Rock Cycle
Creation of metamorphic rocksSedimentary rocks are pushed down–Depending on the temperature and
pressure that the rock is subjected to, it can create different types of metamorphic rock.
Metamorphic RocksMetamorphic Rocks Rocks that have been
changed physically (structurally or mineralogically) by heat, pressure, or chemically active fluids
“metamorphic” means “to change form”
Metamorphic RocksMetamorphic Rocks
Affect of changes in temperature and pressure: Minerals in the rock rearrange themselves into layers OR they recrystallize into bigger crystals
They do not melt…if they did melt, they would turn into magma and therefore start the rock cycle over again
Characteristics of Metamorphic RocksCharacteristics of
Metamorphic Rocks
Have the texture of interlocking grains Layers Light and dark stripes or bands Makes a “ching” noise rather than a “chunk”
noise when tapped
Foliated Metamorphic Rocks
Foliated Metamorphic Rocks
When the rocks experience unequal pressure, the rock’s minerals rearrange themselves to reduce the overall pressure on the rock
These rocks look striped
MineralsMinerals
Inorganic Have identical chemical makeup and also their
crystal shape. If there is metal in them , they are shiny. If there is no metal, they are dull.
Plate TectonicsPlate Tectonics
It is responsible for part of the rock cycleRecycles rock materialsCreates the movement for the rock cycle.
Types of Igneous RocksTypes of Igneous Rocks
Volcanic (Quickly cooled molten rock near the earth’s crust)
Plutonic (Slowly cooled rock really deep under ground.)
The Common Elements of the Earth’s Crust
The Common Elements of the Earth’s Crust
Silicate minerals: ( make up 95% of the volume of igneous rocks)
FeldsparsQuartzMicasPyroxenes Amphiboles Olivine
What is the Difference Between a Rock and a
Mineral?
What is the Difference Between a Rock and a
Mineral?
A mineral is homogenous ( pure, made of one substance)
A rock is a Heterogeneous mix of minerals.
Rock Cycle SongRock Cycle Song
( Don't forget to sing this as a "Round"; after all, it is the Rock "Cycle"! )
(Sing to the tune of "Row, Row, Row Your Boat")
SEDIMENTARY rock Has been formed in layers
Often found near water sources With fossils from decayers
Then there's IGNEOUS rock Here since Earth was born
Molten Lava, cooled and hardened That's how it is formed
These two types of rocks Can also be transformed
With pressure, heat and chemicals METAMORPHIC they'll become.
BibliographyBibliography
http://www.rocksandminerals.com/rockcycle.htm
http://www.minsocam.org/MSA/K12/rkcycle/rkcycleindex.html
http://www.chariho.k12.ri.us/curriculum/MISmart/ocean/rocksong.htm