FW Stress: tensional Fault Type: normal fault Answer Here Stress: Type your answer here Fault Type: Type your answer here Stress: Type your answer here Fault Type: Type your answer here HW Answer Here Answer Here Stress: Type your answer here Fault Type: Type your answer here Answer Here Stress: Type your answer here Fault Type: Type your answer here Stress: Type your answer here Fault Type: Type your answer here
FW Stress: tensional Fault Type: normal fault Answer Here Stress: Type your answer here Fault Type: Type your answer here Stress: Type your answer here Fault Type: Type your answer here HW Answer Here Answer Here Stress: Type your answer here Fault Type: Type your answer here Answer Here Stress: Type your answer here Fault Type: Type your answer here Stress: Type your answer here Fault Type: Type your answer here
Applications and Investigations in Earth Science (9th Edition)
9th Edition
ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Chapter1: The Study Of Minerals
Section: Chapter Questions
Problem 1LR
Related questions
Question
In this part of the lab you will be determining different types of stress and identifying the types of faults that they
create. For each of the dip-slip faults below identify the type of stress that has occurred, name the type of fault shown
as either normal, reverse, left-lateral, or right-lateral, and if it is a dip-slip fault determine which fault block is the
hanging wall (HW) or footwall (FW). The first fault is an example that was completed for you.

Transcribed Image Text:FW
Stress: tensional
Fault Type: normal fault
Answer
Here
Stress: Type your answer here
Fault Type: Type your answer here
Stress: Type your answer here
Fault Type: Type your answer here
HW
Answer
Here
Answer
Here
Stress: Type your answer here
Fault Type: Type your answer here
Answer
Here
Stress: Type your answer here
Fault Type: Type your answer here
Stress: Type your answer here
Fault Type: Type your answer here
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