11.7 How do earthquakes relate to rock deformation?

Deformation of Rocks
Why study rock deformation?
Why study rock deformation?
Why study rock deformation?
Why study rock deformation?
Why study rock deformation?
Why study rock deformation?
Why study rock deformation?
Why study rock deformation?
Why study rock deformation?
Why study rock deformation?
Why study rock deformation?
Why study rock deformation?
Why study rock deformation?
Why study rock deformation?
11.1 What do deformed rocks look like?
11.1 What do deformed rocks look like?
11.1 What do deformed rocks look like?
11.1 What do deformed rocks look like?
11.1 What do deformed rocks look like?
11.1 What do deformed rocks look like?
11.1 What do deformed rocks look like?
11.1 What do deformed rocks look like?
11.1 What do deformed rocks look like?
11.1 What do deformed rocks look like?
11.1 What do deformed rocks look like?
11.1 What do deformed rocks look like?
11.1 What do deformed rocks look like?
11.1 What do deformed rocks look like?
11.1 What do deformed rocks look like?
11.1 What do deformed rocks look like?
11.1 What do deformed rocks look like?
11.1 What do deformed rocks look like?
11.2 How are resources related to geologic structures?
11.2 How are resources related to geologic structures?
11.2 How are resources related to geologic structures?
11.2 How are resources related to geologic structures?
11.3 Why do rocks deform?
11.3 Why do rocks deform?
11.3 Why do rocks deform?
11.3 Why do rocks deform?
11.3 Why do rocks deform?
11.4 How do we know ... why some rocks break and others flow?
11.4 How do we know ... why some rocks break and others flow?
11.4 How do we know ... why some rocks break and others flow?
11.4 How do we know ... why some rocks break and others flow?
11.4 How do we know ... why some rocks break and others flow?
11.4 How do we know ... why some rocks break and others flow?
11.4 How do we know ... why some rocks break and others flow?
11.5 How do geologic structures relate to stress, strain, and strength?
11.5 How do geologic structures relate to stress, strain, and strength?
11.5 How do geologic structures relate to stress, strain, and strength?
11.5 How do geologic structures relate to stress, strain, and strength?
11.5 How do geologic structures relate to stress, strain, and strength?
11.5 How do geologic structures relate to stress, strain, and strength?
11.5 How do geologic structures relate to stress, strain, and strength?
11.5 How do geologic structures relate to stress, strain, and strength?
11.5 How do geologic structures relate to stress, strain, and strength?
11.6 How does strength vary in the lithosphere?
11.6 How does strength vary in the lithosphere?
11.6 How does strength vary in the lithosphere?
11.7 How do earthquakes relate to rock deformation?
11.7 How do earthquakes relate to rock deformation?
11.7 How do earthquakes relate to rock deformation?
11.7 How do earthquakes relate to rock deformation?
Elastic Rebound
11.7 How do earthquakes relate to rock deformation?
11.7 How do earthquakes relate to rock deformation?
11.7 How do earthquakes relate to rock deformation?
11.8 How are earthquakes measured?
11.8 How are earthquakes measured?
11.8 How are earthquakes measured?
11.8 How are earthquakes measured?
11.8 How are earthquakes measured?
11.8 How are earthquakes measured?
11.8 How are earthquakes measured?
11.8 How are earthquakes measured?
11.8 How are earthquakes measured?
11.9 Why are earthquakes destructive?
11.9 Why are earthquakes destructive?
11.9 Why are earthquakes destructive?
11.9 Why are earthquakes destructive?
11.9 Why are earthquakes destructive?
11.9 Why are earthquakes destructive?
11.9 Why are earthquakes destructive?
11.9 Why are earthquakes destructive?
11.9 Why are earthquakes destructive?
11.9 Why are earthquakes destructive?
11.9 Why are earthquakes destructive?

Text and Images from Slide

Map showing location of aftershocks along a fault after a major earthquake.

Fig 11.32

Plot of aftershocks along a fault system in Alaska. Aftershocks may stay in the mainshock region, or may transfer to adjoining faults as stresses change and adjust.

lecture11

Table of Contents

Text and Images from Slide