11.3 Why do rocks deform?

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

cross section to show the folding during compressional strain.

Fig 11.15

A similar experiment using wax layers, which tend to bend before they break as a result of stress. Folded structures form as a result of stress. We also see flow and faulting under continued stress.

lecture11

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Text and Images from Slide