This topic contains a solution. Click here to go to the answer

Author Question: Transform-fault boundaries usually form A) between two segments of a mid-ocean ridge. B) between ... (Read 61 times)

Lisaclaire

  • Hero Member
  • *****
  • Posts: 569
Transform-fault boundaries usually form
 
  A) between two segments of a mid-ocean ridge.
  B) between two other transform-fault boundaries.
  C) between a mid-ocean ridge and a subduction zone.
  D) in the rift of a mid-ocean ridge.

Question 2

How does movement in a normal fault differ from that in a reverse fault?
 
  What will be an ideal response?



Related Topics

Need homework help now?

Ask unlimited questions for free

Ask a Question
Marked as best answer by a Subject Expert

jasonq

  • Sr. Member
  • ****
  • Posts: 335
Answer to Question 1

Answer: A

Answer to Question 2

Answer: In a normal fault, movement along the fault is caused by tensional stress in the crust; this causes the hanging wall to move downward with respect to the footwall. In a reverse fault, movement along the fault is caused by compressional stress in the crust; this causes the hanging wall to move upward with respect to the footwall.





 

Did you know?

Bacteria have been found alive in a lake buried one half mile under ice in Antarctica.

Did you know?

Multiple experimental evidences have confirmed that at the molecular level, cancer is caused by lesions in cellular DNA.

Did you know?

As the western states of America were settled, pioneers often had to drink rancid water from ponds and other sources. This often resulted in chronic diarrhea, causing many cases of dehydration and death that could have been avoided if clean water had been available.

Did you know?

Never take aspirin without food because it is likely to irritate your stomach. Never give aspirin to children under age 12. Overdoses of aspirin have the potential to cause deafness.

Did you know?

The B-complex vitamins and vitamin C are not stored in the body and must be replaced each day.

For a complete list of videos, visit our video library