11.1 Folding and Faulting
Factors Affecting Deformation- Temperature & pressure
- Rock type
- Time
- Most crustal deformation occurs along plate margins.
• Deformation - changes in original shape/size of rock body.
This peak is part of the
Karakoram Range in Pakistan.
Types of Stress1. Tensional
2. Compressional
3. Shear
Folds (in sedimentary rock strata) Anticlines - upfolding, or arching (A).
Synclines - linear downfolds (U) found with anticlines.
Monoclines - large step-like folds.
Monocline located near Mexican Hat, Utah.
Anticlines & Synclines
Folding and FaultingAnticline
Syncline
Faults Normal - hanging wall block moves down relative to footwall block.
Reverse - hanging wall block moves up relative to footwall. High angle – dips
greater than 45o (If less than 45o then the fault is called a thrust fault)
Strike-Slip - movement horizontal & parallel to the trend of the fault surface.
Normal Fault - caused the vertical
displacement of these beds located near
Kanab, Utah.
Arrows show the relative motion of
rock units.
RR
R
R
LL
L
L
Fault
1. How does rock folding differ from rock faulting?
2. What makes a reverse fault different from a thrust fault?
3. What is the difference between a hanging wall block and a footwall block?
Use Chapter 11.1 of your textbook to answer the following questions at the end of your notes. Please write out the question in a different color, or you can highlight or underline the question.