A butte // is an isolated hill with steep, often vertical sides and a small, relatively flat top; buttes are smaller than mesas, plateaus, and table landforms. The word butte comes from a French word meaning "small hill"; its use is prevalent in the Western United States, including the southwest where "mesa" is also used for the larger landform. Because of their distinctive shapes, buttes are frequently landmarks in plains and mountainous areas. In differentiating mesas and buttes, geographers use the rule of thumb that a mesa has a top that is wider than its height, while a butte has a top that is narrower than its height.
The Mitten Buttes of Monument Valley in Arizona are two of the most distinctive and widely-recognized buttes. Monument Valley and the Mittens provided backgrounds in scenes from many western-themed films, including seven movies directed by John Ford.[note 1] The Devils Tower in northeastern Wyoming is a laccolithic butte composed of igneous rock rather than sandstone, limestone or other sedimentary rocks.
Three other notable formations that are either named butte or may be considered buttes even though they do not conform to the formal geographer's rule are Scotts Bluff in Nebraska which is actually a collection of five bluffs, Crested Butte which is a 12,168 ft (3,709 m) mountain in Colorado, and Elephant Butte which is now an island in Elephant Butte Reservoir in New Mexico.
Among the well-known non-flat-topped buttes in the United States are Bear Butte, South Dakota and Black Butte, Oregon. In many cases, buttes have been given other names that do not use the word butte, for example, Courthouse Rock, Nebraska. Also, some large hills that are technically not buttes have names using the word butte, examples of which are Kamiak Butte and Chelan Butte in Washington State.
Buttes form by weathering and erosion when hard caprock overlies a layer of less resistant rock that is eventually worn away. The harder rock on top of the butte resists erosion. The caprock provides protection for the less resistant rock below from wind abrasion which leaves it standing isolated. As the top is further eroded by abrasion and weathering, the excess material that falls off adds to the scree or talus slope around the base. On a much smaller scale, the same process forms hoodoos.
- "Mesa and Butte". Science Clarified. 2008. Archived from the original on 2 December 2013.
- "Devils Tower National Monument - Geologic Formations". National Park Service. 10 Mar 2014. Retrieved 13 Mar 2014.
- Davis, George Herbert (1999). Structural Geology of the Colorado Plateau Region of Southern Utah, with Special Emphasis on Deformation Bands. G.S.A. Special Paper 342. Boulder, Colorado: Geological Society of America. p. 30. ISBN 978-0-8137-2342-6.
- Hill, R.T. 1890. A brief description of the Cretaceous rocks of Texas and their economic value. In: Dumble, E.T. (ed.), First Annual Report of the Geological Survey of Texas, 1889. Austin: State Printing Office, pp. 105-141.
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