7.1 stress in earth’s crust the way tectonic plates move

7.1 STRESS IN EARTH’S CRUST

The Way Tectonic Plates Move

Learning Targets

1. Describe the anatomy of an earthquake and relate plate tectonics (different types of plate boundaries) to earthquakes.

2. Describe how stress builds up earthquakes

Stress

1. Plate movement is never smootha) Plates made of solid, rough rock

2. Stress builds up at plate boundaries

a)Fold - Rocks bendb)Fracture - Rocks break

3.Earthquake = removal of stress

Stress

1.Mantle convection cells puts a lot of stress on the rocks of the lithosphere.

Types of Stress

1. Confining: pressure from all directionsa) No deformation

2. Compression: pushed togethera) Fractures or folds

3. Tension: pulled apart (extension)a) Stretch or break

4. Shear: parallel but opposite (scissors)a) Break and slide past one another

Types of Stress

1. What type of plate boundarya) Confining - Results from being

buriedb) Compression - Convergentc) Tension -Divergentd) Shear - Transform

Elastic vs. Plastic

1. Rocks under stress will deforma) Elastically: bend then return to

original shape

2. Rocks under more stress will deform

a) Plastically: bend without the ability to return to the original shape

Geologic Structures

1. Folds2. Joints3. Faults

Geologic Structures - Folds

1. Folds: bends in rock due to compression

a) Monocline: non-horizontal layeringb) Anticline: Upward bulgec) Syncline: Downward bulge

Geologic Structures - Joints

2. Joints: breaks where rocks do not move

Geologic Structures - Faults

3. Faults: breaks where rocks have moved

Fault

Fracture – If the stress continues, the rock will break

Types of Faults: Dip-slip & Strike-slip

Geologic Structures Summary

1. Folds: bends in rock due to compression

a) Monocline: non-horizontal layeringb) Anticline: Upward bulgec) Syncline: Downward bulge

2. Joints: breaks where rocks do not move

3. Faults: breaks where rocks have moved