Chapter 4 Plate Tectonics 4 4 Deforming the

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Chapter 4 Plate Tectonics 4 -4 Deforming the Earth’s Crust

Chapter 4 Plate Tectonics 4 -4 Deforming the Earth’s Crust

Essential Questions/Learning Goals: • • How does stress affect the Earth’s crust? Describe three

Essential Questions/Learning Goals: • • How does stress affect the Earth’s crust? Describe three major types of folds.

Science Terms: • Compression • Tension • Folding

Science Terms: • Compression • Tension • Folding

Section Introduction: • What is stress? – The amount of force per unit of

Section Introduction: • What is stress? – The amount of force per unit of area on a substance.

Deformation • What is deformation? – Changes in a rock’s shape due to stress

Deformation • What is deformation? – Changes in a rock’s shape due to stress • De = “undo” • Form = “shape” • –tion = “process of”

Compression • What is compression? – Stress that squeezes rocks together • What kind

Compression • What is compression? – Stress that squeezes rocks together • What kind of boundary has compression? – Convergent boundaries.

Tension • What is tension? – Stress that stretches rocks. • What kind of

Tension • What is tension? – Stress that stretches rocks. • What kind of boundary has tension? – Divergent

Folding • What are folds? – Bends in rocks due to stress.

Folding • What are folds? – Bends in rocks due to stress.

Types of Folds • The two most common types of folds are: – Anticlines:

Types of Folds • The two most common types of folds are: – Anticlines: • Upward folds (arches) – Synclines: • Downward folds (troughs)

What is a monocline fold? • A fold that has both ends of the

What is a monocline fold? • A fold that has both ends of the fold still horizontal. • There is a middle portion that bends downwards.

Monocline fold

Monocline fold

How big are folds? Folds can be as large as mountains Or As small

How big are folds? Folds can be as large as mountains Or As small as centimeters

Faulting • Essential Question: – How are three types of faults different from each

Faulting • Essential Question: – How are three types of faults different from each other? • Science Term Fault

What is a Fault? • A break in rocks where one rock slide past

What is a Fault? • A break in rocks where one rock slide past the other

Fault Illustration

Fault Illustration

 • What are the pieces of broken rock on each side of the

• What are the pieces of broken rock on each side of the fault called? – Fault blocks. • Two types: – Footwall – Hanging wall

Footwall • The block of rock beneath the fault – You can climb up

Footwall • The block of rock beneath the fault – You can climb up the footwall

Hanging Wall • The block of wall above the fault. • You could stand

Hanging Wall • The block of wall above the fault. • You could stand underneath a hanging wall.

Normal Faults • How do the fault blocks move in a Normal Fault? –

Normal Faults • How do the fault blocks move in a Normal Fault? – The hanging wall slides down the foot wall • What kind of stress makes a Normal Fault? – Tension • What kind of boundary are you likely to find a Normal Fault at? – Divergent Boundary

Reverse Faults • How do the fault blocks move in a Reverse Fault? –

Reverse Faults • How do the fault blocks move in a Reverse Fault? – The hanging wall slides up the footwall • What kind of stress makes a Reverse Fault? – Compression – What kind of boundary are you likely to find a Reverse Fault at? • Convergent

Telling the Difference Between Faults • How can you tell the difference between a

Telling the Difference Between Faults • How can you tell the difference between a normal fault and a reverse fault? – If you look at the rock layers, you can tell how the hanging wall and footwall have moved.

Strike Slip Faults • How do the fault blocks move in a strike slip

Strike Slip Faults • How do the fault blocks move in a strike slip fault? – The blocks grind and slide past each other horizontally – Example of a strike slip fault • San Andreas Fault

Plate Tectonics and Mountain Building • What kinds of mountains are built by Plate

Plate Tectonics and Mountain Building • What kinds of mountains are built by Plate Tectonics? – Folded mountains – Fault-block mountains – Volcanic mountains

Folded Mountains • How are these mountains formed? – Plates colliding at a… •

Folded Mountains • How are these mountains formed? – Plates colliding at a… • Convergent boundary – Examples: • Appalachian, Alps, Himalayas.

Fault-Block Mountains • How are these mountains formed? – Tension pulling huge blocks of

Fault-Block Mountains • How are these mountains formed? – Tension pulling huge blocks of rocks apart. • Gravity causes the hanging wall to slide down the footwall – Normal faulting

Fault-Block Mountains • Shape? – Can be very jagged and sharp looking. • Example:

Fault-Block Mountains • Shape? – Can be very jagged and sharp looking. • Example: – Tetons in Wyoming

Volcanic Mountains • How are these mountains formed? – When plates collide and one

Volcanic Mountains • How are these mountains formed? – When plates collide and one is… • Subducted – The melted crust rises to form volcanic mountains

Volcanic Mountains • Where are most volcanic mountains formed? – At plate boundaries such

Volcanic Mountains • Where are most volcanic mountains formed? – At plate boundaries such as…. • Subduction zones

What is the Ring of Fire? • It is the plate boundaries that are

What is the Ring of Fire? • It is the plate boundaries that are found around the Pacific Ocean

Uplift and Subsidence • What type of motion occurs in the crust in uplift

Uplift and Subsidence • What type of motion occurs in the crust in uplift and subsidence? – Vertical movement • Uplift? – Upward movement of blocks of rock • May or may not be deformed by stress • Subsidence? – Downward movement of blocks of rock • Usually are not deformed by stress.

Uplifting of Depressed Rocks • Rocks that have been pushed down by the weight

Uplifting of Depressed Rocks • Rocks that have been pushed down by the weight of glaciers will rise upwards after the glacier has melted away. • This is called… – Rebound • Does deformation occur? – No.

Subsidence of Cooler Rocks • As rocks cool, they take up less… – Space

Subsidence of Cooler Rocks • As rocks cool, they take up less… – Space or volume • What does this mean for the height of mountains? – They shrink!

Subsidence of Cooler Rocks • Where does this occur? – Mid ocean ridges. •

Subsidence of Cooler Rocks • Where does this occur? – Mid ocean ridges. • As the rocks get further from the MOR, the rocks cool and become more dense causing the ridges to become lower.

Tectonic Letdown • What happens to the crust when you stretch it? – It

Tectonic Letdown • What happens to the crust when you stretch it? – It will sink lower – This creates a… • Rift zone

Tectonic Letdown • What kind of boundary does this occur at? – A divergent

Tectonic Letdown • What kind of boundary does this occur at? – A divergent boundary • What kind of fault occurs here? – Normal faults.