Rock layers subjected to tension are commonly shortened in the direction of stress by either faulting or folding.

Name: Rock layers subjected to tension are commonly shortened in the direction of stress by either faulting or folding.
Brand: Quizplus
Rating: 4.9 (62 reviews)

Question

Quizplus · Accepted Answer

Rock layers subjected to tension are typically elongated or stretched in the direction of stress, not shortened. Shortening occurs under compressional stress, leading to folding or faulting that shortens and thickens the crust.

Rock Layers Subjected to Tension Are Commonly Shortened in the Direction