North America:
* Sierra Nevada, California: A classic example of a fault-block mountain range formed by the uplift of the eastern side of a fault.
* Wasatch Range, Utah: Another prominent fault-block range, known for its steep slopes and high peaks.
* Teton Range, Wyoming: A dramatic range formed by the uplift of the western side of a fault, creating steep cliffs and valleys.
Europe:
* Vosges Mountains, France: Located on the eastern edge of the French plateau, these mountains are a classic example of a fault-block range.
* Black Forest Mountains, Germany: Another example of a fault-block range, characterized by its rolling hills and forested slopes.
Asia:
* Himalaya Mountains, Nepal and Tibet: While the Himalayas are primarily formed by tectonic collision, some sections exhibit fault-block features, such as the Nanga Parbat massif.
* Tien Shan Mountains, Central Asia: These mountains exhibit fault-block features along with folding and uplift caused by tectonic activity.
Africa:
* Atlas Mountains, Morocco and Algeria: These mountains have a complex history, but some sections show evidence of fault-block uplift.
* Drakensberg Mountains, South Africa: This range features some fault-block structures alongside erosion and other geological processes.
South America:
* Andes Mountains, South America: While mostly formed by tectonic convergence, some sections of the Andes exhibit fault-block features.
This is not an exhaustive list, but it showcases the diverse locations around the world where fault-block mountains can be found.
