North America
* Sierra Nevada, California, USA: One of the most iconic examples, featuring granite peaks like Mount Whitney, the highest point in the contiguous US.
* Teton Range, Wyoming, USA: Known for their sharp, jagged peaks and dramatic elevation changes.
* Wasatch Range, Utah, USA: Dominates the landscape of Salt Lake City and includes peaks like Mount Timpanogos.
* Basin and Range Province, Western USA: A vast region characterized by alternating mountain ranges and flat valleys, extending from Nevada to Arizona.
* Appalachian Mountains, Eastern USA: While mostly formed by folding, the Appalachian Mountains also feature fault blocks in some areas, particularly in the Blue Ridge Mountains.
Europe
* Vosges Mountains, France: A range bordering the Rhine Valley, known for its rolling hills and vineyards.
* Black Forest, Germany: Another range along the Rhine Valley, famous for its dense forests and spas.
* Pyrenees Mountains, Spain and France: While primarily formed by folding, the Pyrenees also have fault blocks that create distinct landscapes.
Asia
* Tian Shan Mountains, Central Asia: One of the largest fault block mountain ranges in the world, containing many peaks over 7,000 meters.
* Hindu Kush Mountains, Afghanistan and Pakistan: A major range within the Himalayas, known for its rugged terrain and strategic importance.
* Altai Mountains, Central Asia: A range spanning Russia, Mongolia, China, and Kazakhstan, known for its vast grasslands and rich mineral deposits.
Africa
* Drakensberg Mountains, South Africa: A prominent range known for its dramatic cliffs and stunning scenery.
* Atlas Mountains, North Africa: A range that runs across Morocco, Algeria, and Tunisia, known for its diverse landscapes and Berber culture.
South America
* Andes Mountains, South America: While the Andes are primarily formed by volcanic activity and subduction, some sections, like the Chilean Andes, feature prominent fault block mountains.
Australia
* Great Dividing Range, Australia: While not a fault block mountain range in the strict sense, the Great Dividing Range features sections of uplifted blocks.
Important Note: The formation of mountains is complex, and many ranges are formed by a combination of forces. While fault block mountains are prominent in certain regions, their formation is often interwoven with other processes like folding, volcanism, and erosion.
