Geologic structures found in mountain ranges formed by compression at convergent plate margins would likely include

Question

Quizplus · Accepted Answer

Mountain ranges formed by compression at convergent plate margins often exhibit a variety of geologic structures due to the intense pressure and deformation associated with plate collision. This includes overturned and recumbent folds, plunging folds, and reverse faulting, all of which are mechanisms through which the Earth's crust can deform under such stress.

Geologic Structures Found in Mountain Ranges Formed by Compression at Convergent