What Is A Butte

Discover what a butte is in geology and geography, how it forms, its key characteristics, and examples of these isolated, flat-topped hills.

Have More Questions →

Definition of a Butte

A butte (pronounced "byoot") is an isolated hill with steep, often vertical, sides and a small, relatively flat top. It is typically a prominent, solitary landform that stands out from the surrounding terrain.

Formation Process

Buttes form through differential erosion. They are remnants of larger elevated landforms, such as mesas or plateaus, where softer rock layers around them have eroded away. A harder, more resistant caprock layer at the summit protects the underlying, less resistant rock from faster weathering and erosion.

Characteristics and Appearance

Key characteristics of a butte include its isolated nature, a relatively small summit area compared to its base, and steep, cliff-like slopes. Their striking appearance, often resembling towers or columns, makes them distinctive features in many landscapes, particularly in arid and semi-arid regions.

Examples and Significance

Well-known examples of buttes can be found in the American Southwest, such as Merrick Butte and Monument Valley in Arizona and Utah. Buttes serve as valuable geological indicators, illustrating long-term erosional patterns and often providing unique ecological niches as isolated habitats for specific flora and fauna.

Frequently Asked Questions

What is the primary difference between a butte and a mesa?
How long does it take for a butte to form?
Are buttes always found in deserts or arid environments?
Do buttes only consist of sedimentary rock?