Ch. 10 Rocks & The Rock Cycle. The Parent Material for all rock is….. Magma!!!

26
Ch. 10 Rocks & The Rock Cycle

Transcript of Ch. 10 Rocks & The Rock Cycle. The Parent Material for all rock is….. Magma!!!

Page 1: Ch. 10 Rocks & The Rock Cycle. The Parent Material for all rock is….. Magma!!!

Ch. 10 Rocks & The Rock Cycle

Page 2: Ch. 10 Rocks & The Rock Cycle. The Parent Material for all rock is….. Magma!!!

The Parent Material for all rock is…..

Magma!!!

Page 3: Ch. 10 Rocks & The Rock Cycle. The Parent Material for all rock is….. Magma!!!

3 Major Types of Rock

• Igneous Rock: forms when magma cools and hardens.

• Sedimentary Rock: forms from sediment that is compacted and cemented together.

• Metamorphic Rock: forms from rock that is changed by intense heat and pressure.

Page 4: Ch. 10 Rocks & The Rock Cycle. The Parent Material for all rock is….. Magma!!!

The Rock Cycle• All of the changes that can occur to rock.

• Does Igneous Rock always have to become sedimentary rock?

Page 5: Ch. 10 Rocks & The Rock Cycle. The Parent Material for all rock is….. Magma!!!

• Before becoming sedimentary rock, what must metamorphic rock become???

Page 6: Ch. 10 Rocks & The Rock Cycle. The Parent Material for all rock is….. Magma!!!

• What processes result in rock turning into sediment?

Page 7: Ch. 10 Rocks & The Rock Cycle. The Parent Material for all rock is….. Magma!!!

Igneous Rock

Classified into two general categories based on where the magma cooled and solidified:

1. Intrusive Igneous Rock: Magma cooled below the crust

2. Extrusive Igneous Rock: Magma cooled rapidly on the surface of Earth

Page 8: Ch. 10 Rocks & The Rock Cycle. The Parent Material for all rock is….. Magma!!!

Texture of Igneous Rock• What influences texture? The size of crystals found in the rock.

• What influences crystal size? Cooling rate (how fast the magma cooled)

Page 9: Ch. 10 Rocks & The Rock Cycle. The Parent Material for all rock is….. Magma!!!

• Cooling slowly allows large crystals to form. • Cooling rapidly allows small crystals to form.

• Intrusive Igneous rock cools slowly. • Extrusive Igneous rock cools very rapidly.

Which type of Igneous rock would have small crystals?

Which type of Igneous rock would have large crystals?

Page 10: Ch. 10 Rocks & The Rock Cycle. The Parent Material for all rock is….. Magma!!!

• Crystals formed in sample A might be found in what type of rock?

• Crystals formed in sample B might be found in what type of rock?

Sample A Sample B

Page 11: Ch. 10 Rocks & The Rock Cycle. The Parent Material for all rock is….. Magma!!!

What about igneous rock that doesn’t seem to have crystals???

• Silica-rich, viscous, felsic lava that cools rapidly forms Obsidian (Volcanic Glass)

• Magma that has a high amount of dissolved gasses and cools rapidly forms “pockets” or holes around the trapped gas. This creates a rock full of small holes such as pumice.

Page 12: Ch. 10 Rocks & The Rock Cycle. The Parent Material for all rock is….. Magma!!!

Composition of Igneous Rock

• Determined by the chemicals found in the magma that forms the rock.

Three types of igneous rock families:1. Felsic: High in silica, these contain silicate minerals

2. Intermediate: intermediates between mafic and felsic chemical composition

3. Mafic: Low in silica, but rich in iron and magnesium.

Page 13: Ch. 10 Rocks & The Rock Cycle. The Parent Material for all rock is….. Magma!!!

Types of Igneous Rock Structures

1. Intrusions: igneous rock masses that form underground.

2. Extrusions: igneous rock masses that form on the surface.

Page 14: Ch. 10 Rocks & The Rock Cycle. The Parent Material for all rock is….. Magma!!!

Igneous Rock StructuresFill In the names of the structures on your diagram.

Page 15: Ch. 10 Rocks & The Rock Cycle. The Parent Material for all rock is….. Magma!!!

Sedimentary Rock

• Review Question: How was sedimentary rock formed???

Page 16: Ch. 10 Rocks & The Rock Cycle. The Parent Material for all rock is….. Magma!!!

3 Types of Sedimentary Rock

1. Clastic Sedimentary Rock2. Chemical Sedimentary Rock3. Organic Sedimentary Rock

Page 17: Ch. 10 Rocks & The Rock Cycle. The Parent Material for all rock is….. Magma!!!

Clastic Sedimentary Rock• Deposits of rock fragments are compacted and

cemented together.

• Classified by size of sediment that forms the rock. – Conglomerate: rounded gravel sized fragments– Sandstones: made of sand size grains– Shale: clay sized particles

Sandstone

Shale

Page 18: Ch. 10 Rocks & The Rock Cycle. The Parent Material for all rock is….. Magma!!!

Chemical Sedimentary Rock

• Rocks that form from minerals once dissolved in water.– Precipitates: Rocks formed from minerals that

solidify in water– Evaporites: Rocks formed from minerals left

behind when water evaporates.

Page 19: Ch. 10 Rocks & The Rock Cycle. The Parent Material for all rock is….. Magma!!!

Organic Sedimentary Rock

• Formed from the remains of once living organisms. – Examples:• Coal- forms from decayed plants and animals• Limestone- forms from the shells of once living

organisms

Page 20: Ch. 10 Rocks & The Rock Cycle. The Parent Material for all rock is….. Magma!!!

Sedimentary Rock Features

• Stratification: Layering of rock• Ripple Marks: formed by wind or water• Mud Cracks: formed when muddy deposits

dry and shrink• Fossils: remains or traces of once living

organisms • Concretions: nodules with in the rock that are

composed of different chemicals.

Page 21: Ch. 10 Rocks & The Rock Cycle. The Parent Material for all rock is….. Magma!!!

Metamorphic Rock• Existing rock that is changed into another

form by intense heat and pressure• Forms deep beneath the surface of earth.

Page 22: Ch. 10 Rocks & The Rock Cycle. The Parent Material for all rock is….. Magma!!!

Two Types of metamorphism

1. Contact metamorphism2. Regional metamorphism

Page 23: Ch. 10 Rocks & The Rock Cycle. The Parent Material for all rock is….. Magma!!!

Contact Metamorphism

• When hot magma pushes through rock, the heat from the magma can change the surrounding rock.

Page 24: Ch. 10 Rocks & The Rock Cycle. The Parent Material for all rock is….. Magma!!!

Regional Metamorphism

• Occurs during tectonic activity

• This plate movement creates heat and pressure at plate edges.

• This heat and pressure transforms the surrounding rock

Page 25: Ch. 10 Rocks & The Rock Cycle. The Parent Material for all rock is….. Magma!!!

Classification of Metamorphic Rock

• Metamorphic Rocks are classified according to texture.

Metamorphic Rock Classifications1.Foliated: have parrallel bands

of minerals2.Nonfoliated: metamorphic rock

without mineral bands

Foliated

Nonfoliated

Page 26: Ch. 10 Rocks & The Rock Cycle. The Parent Material for all rock is….. Magma!!!

THE END!!!