Linked from

The 11 pages that link to Fold-and-thrust belt, each with the reason it gives.

• Zagros MountainsNarrower topic: Much of the Zagros consists of folded and faulted sedimentary rocks.

• Continental collisionBroader topic: These structures accommodate shortening at the margins of colliding continents.

• Alpine orogenyRelated: Alpine shortening produced thrust sheets and folds along the range's margins.

• Thrust faultBroader topic: It is a characteristic map-scale product of repeated thrusting.

• Himalayan orogenyRelated: This structural pattern characterizes much of the Himalayan foothills and range.

• Andean orogenyRelated: Such belts distribute compression along the eastern side of the Andes.

• Sierra Madre OrientalNarrower topic: The range is a prominent Mexican example of this mountain-building structure.

• Canadian RockiesRelated: The Rockies’ eastern ranges are a classic fold-and-thrust belt.

• Fold mountainsBroader topic: Many fold mountains contain belts where folds and thrust faults occur together.

• Geology of the AppalachiansBroader topic: These structures dominate the Valley and Ridge province.

• Judaean MountainsNarrower topic: The range’s structure belongs to a wider zone of regional deformation.