Metamorphism. In China… Why animorphs? Metamorphosis Meta= changed Morphosis= shape.

32
Metamorphism

Transcript of Metamorphism. In China… Why animorphs? Metamorphosis Meta= changed Morphosis= shape.

Metamorphism

In China…

Why animorphs?

Metamorphosis

Meta= changed

Morphosis= shape

Metamorphosis(caterpillar)

Metamorphism(rocks)

Metamorphic Rock

Rocks in which the structure, texture, or composition of rock have changed.

Metamorphic Rock

All 3 types of rock (metamorphic, igneous, & sedimentary) can be changed by heat, pressure, or combo of both

Origins of Metamorphic Rock

Can start out as an igneous or sedimentary rock or a metamorphic rock!

Changes into metamorphic rock at least 2 km below surface

3 Ways Rock Can CHANGE into a Metamorphic Rock

1. extreme heat(50-1000* C or more!)2. Extreme pressure (from rock layers above) 3. movements in Earth’s crust that rearrange minerals inside a rock into bands (layers/stripes).

2 Types of Metamorphism

1. contact metamorphism

2. regional metamorphism

2 Types of Metamorphism

1. contact metamorphism

* magma moves through the crust, it heats the surrounding rock and changes it. * The rock that magma touches directly experiences the most change.* Can change minerals into new minerals.* Where does this happen? Near igneous intrusion

Contact Metamorphism

Contact Metamorphism

2 Types of Metamorphism

2. regional metamorphism

*Temperature & pressure are increased, causing rock to become deformed and change chemically.• Happens when there is great

pressure from pieces of Earth’s crust colliding.

• Where does it happen? deep under mountains

or continents

Composition of Metamorphic Rock

Some minerals cannot survive at certain temperatures and pressures, so they change into new minerals.

SEE pg. 109

Foliated Rock

• Texture in which the mineral grains are parallel or arranged in plains or bands.

SEE PAGE 109

Non- Foliated Rock• Texture of metamorphic rock in which mineral

grains are arranged randomly.

2 examples: marble & quartzite

Non- Foliated Rock •How? •During metamorphism, recrystallization occurs

Add to sheet: • Recrystallization: process in which mineral

crystals change size or composition.Ex. Limestone undergoes metamorphosis and the calcite crystals become larger, thus forming marble.

Each time metamorphic rock is exposed to more heat and pressure, it becomes a new metamorphic rock. Ex. (See Figure 5 on pg. 109)

Gneiss (comes from schist)Slate (comes from sedimentary shale)

Deformation: (add to notes)a change in the shape of a rock caused by a force placed on it.

Forces might cause a rock to be stretched or squeezed

Non-foliated Rocks

Texture of metamorphic rock in which mineral grains are arranged randomly

Examples

Marble Quartzite

1..

Q: How do these become non-foliated metamoprhic rocks?

A: Metamorphism causes recrystallization (process in which mineral

crystals change size or composition).

Starts out as limestone,

recrystallization causes mineral grains to grow=

Marble.

Rock Cycle

Igneous Rock

Formed from magma & lava cooling and hardening.

Sedimentary Rock

Formed by weathering, erosion, deposition, compaction, cementation.

Metamorphic Rock

Formed by extreme heat & pressure.

ROCK CYCLE

All rocks can change into ANY other type of rock.

Rock Cycle

Rock Cycle

Rock Cycle Intro Video

https://www.youtube.com/watch?v=CvDw07iYaJQ Rock Cycle Movie

Start at 7:22-end

Rock Cycle Intro VideoAn Igneous rock, a sedimentary rock ,and a metamorphic rock can all become a new igneous rock if they melt into magma/lava, cool, and harden.

An Igneous rock, a sedimentary rock ,and a metamorphic rock can all become a new sedimentary rock if they are broken down, carried away as sediment, deposited, and then compacted and cemented together to form new rock.

An Igneous rock, a sedimentary rock ,and a metamorphic rock can all become a new metamorphic rock if they go through extreme heat and pressure.