Most of the mountain ranges of Munster were formed as a result of folding.

Fold mountains are able to support different types of tourist activity.

When two plates collide, the heavier one sinks downwards into the mantle.

The upfold of a fold mountain is called the syncline.

The Alpine fold mountains are young and are still high.

The Andes Mountains formed when the Nazca Plate and South American plates collided.

There are no fold mountains in Ireland.

The Rocky Mountains is a fold mountain range in Europe

The downfold of a fold mountain is known as the syncline.