Foothills are geographically defined as gradual increase in elevation at the base of a mountain range. They are a transition zone between plains and low relief hills to the adjacent topographically high mountains.
Foothills border mountains, especially those which are reached through low ridges that increase in size closer and closer to the mountain.
Areas where foothills exist, or areas commonly referred to as the foothills, include:
- The Sierra Nevada foothills of California
- The Foothills of the San Gabriel Valley in Los Angeles County, California
- The Colorado Front Range along the Rocky Mountains in Colorado
- The Wasatch Front along the Wasatch Mountains in Utah
- The Rocky Mountain Foothills in British Columbia and Alberta, Canada
- The Alpine foothills around the European Alps
- The Silesian Foothills in Silesia
- The Siwalik Hills along the Himalayas in the Indian subcontinent
- The Catalina Foothills in Tucson, Arizona
- The foothills in Western North Carolina and Northwestern South Carolina
- The Margalla hills near the Himalayas in Pakistan
- The Duars, Chos and Terai on the foothills of Himalayas (India)
- The foothills around Boise in Idaho
- 'The foothills' of the Dandenong Ranges in Melbourne, Australia. Genereally the area from Ferntree Gully/Boronia/The Basin through to Belgrave.
- Physical Geography - Juanico, Meliton - Google Books. Books.google.com. Retrieved 2014-05-15.
|This article needs additional citations for verification. (September 2014)|
|Look up foothill in Wiktionary, the free dictionary.|
|This article relating to topography is a stub. You can help Wikipedia by expanding it.|