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Unit 3 rock cycle sedimentary igneous metamorphic rocks 2 1 1

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The Rock CycleObjectives:Een.2.1.1 destruction of the 3 types of rocks weathering, heat & pressure, deposition, foliation, & bedding affects these types of rocks... As the earth’s plat

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The Rock Cycle

Objectives:Een.2.1.1

destruction of the 3 types of rocks

weathering, heat & pressure,

deposition, foliation, & bedding

affects these types of rocks.

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What are Rocks???

Earth They are a naturally occurring

collection of one or more minerals.

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The Rock Cycle

a cycle that continuously forms and changes rocks

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The rock cycle is used to explain how the

one type to another through time

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Convection is the driving force of the

rock cycle !

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Rock divisions occur in three major

families based on how they formed:

igneous , sedimentary , and

Plate tectonic movement is responsible for the recycling of rock materials As the earth’s plates slowly move, the rocks that make

up the plates are continuously recycled and change from one form

to another

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3 Types of Rocks

How are they formed???

3 Rock Types

Sedimentary Metamorphic Igneous

Weathering and ErosionChemical ActivityHeat, Pressure,

Melting, Cooling, and Solidification

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IGNEOUS ROCKS

is below the Earth’s surface It cools

and hardens to form INTRUSIVE

(inside) igneous rocks.

 It is lava when it is above/outside

the earth Then it cools and hardens

to form EXTRUSIVE igneous rock.

Igneous rocks form when molten rock

cools and becomes solid.

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TEXTURE OF IGNEOUS ROCKS

Crystal size is determined by cooling

 Large crystals indicate long cooling time

 Small crystals indicate short cooling time

 Porphyrytic – mixture of large & small crystal grains Requires two cooling.

Igneous rocks have different textures.

Texture is how a rock looks and feels.

Texture is based on the size of crystal

grains in the rocks

 Glassy/fine texture = extrusive

 Coarse/very course texture = intrusive

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Types of Igneous Rocks

Granite rocks are

igneous rocks which

were formed by slowly

cooling pockets of

magma that were

trapped beneath the

earth's surface Granite

is used for long lasting

monuments and for trim

and decoration on

buildings

Pumice rocks are igneous

rocks which were formed when lava cooled quickly above

ground You can see where little pockets of air had been

This rock is so light, that many pumice rocks will actually float

in water Pumice is actually a kind of glass and not a mixture

of minerals Because this rock

is so light, it is used quite often

as a decorative landscape stone

Obsidian rocks are

igneous rocks that form when lava cools quickly above ground Obsidian is actually glass and not a mixture of minerals The edges of this rock are very sharp

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SEDIMENTARY ROCKS

Any rock (igneous, sedimentary, or

metamorphic) exposed at the Earth's surface can become a sedimentary rock

Sedimentary rocks – are arranged in thick horizontal layers called bedding

The forces of wind, rain,

snow, and ice combine to

break down or dissolve

(weather), and carry away

(transport) rocks exposed at

the surface

Rain washes rock away

Little bits of Earth Wash downstream

Layer after layer Eroded Earth

is pressed on top

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Types of Sedimentary Rocks

Sandstone rocks

are sedimentary

rocks made from

small grains of the

minerals quartz

and feldspar They

often form in

layers as seen in

this picture They

are often used as

building stones

Limestone rocks are

sedimentary rocks that are made from the mineral calcite which came from the beds of evaporated seas and lakes and from sea animal shells This rock

is used in concrete and

is an excellent building stone for humid

regions

Shale rock is a type of

sedimentary rock formed from clay that is

compacted together by pressure They are used

to make bricks and other materials

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METAMORPHIC ROCKS

Have you heard that caterpillars can

metamorphose into butterflies? Well, rocks can

metamorphose too!

Rocks metamorphose

when they are in a place

that is very hot and

pressure is high

The term "metamorphic" means "to change form."

Sediment turns into Metamorphic rock

magma

Pressure and Heat Sediment sinks

squeezing under high pressure

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Metamorphic Rocks-Extreme Heat &

Pressure

Where does the heat

comes from?

Heat comes from

magma, from within

the earth’s interior.

Where does the

pressure comes from?

Pressure comes when

tectonic plates

converging or

squeezing together.

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Metamorphic Rocks-Extreme Heat &

Pressure

Regional

Metamorphism

Large geographic area

Example:

Where mountains form

Contact

Metamorphism

Small geographic area

Example:

When rocks come in

contact with magma

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Types of Metamorphic Rocks

Schist rocks are

metamorphic These rocks can

be formed from basalt, an

igneous rock; shale, a

sedimentary rock; or slate, a

metamorphic rock Through

tremendous heat and

pressure, these rocks were

transformed into this new kind

of rock Their atoms got

rearranged Forms foliation

Gneiss rocks are

metamorphic These rocks may have been granite, which is an igneous rock, but heat and pressure changed it You can see how the mineral grains in the rock were

flattened through tremendous heat and pressure, and the layers are arranged in

alternating patterns Foliation

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All rock (except for

meteorites!) that is

on Earth today is

made of the same

stuff as the rocks

that dinosaurs and

other ancient life

forms walked,

crawled or swam

over

While the stuff that

rocks are made

from stays the same,

the rocks

do not

Over millions of years, rocks are recycled into other rocks Moving

tectonic plates help to destroy and form

many types of rocks

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 http://www.minsocam.org/MSA/K12/rkcycle/

rkcycleindex.html

 http://www.bbc.co.uk/education/rocks/

rockcycle.shtml

 http://www.fi.edu/fellows/fellow1/oct98/create/

sediment.htm

earth/geology/rocks_intro.html

planets/earth/Continents.shtml

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