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Butte

Isolated hill with steep, often vertical sides and a small, relatively flat top

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Monument Valley, the buttes are clearly stratified, with three principal layers. The lowest layer is Organ Rock Formation-(skirts, slope-former), the middle De Chelly Sandstone-(vertical cliffs) and t
Wolfgang Staudt from Saarbruecken, Germany · CC BY 2.0

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Through Geomorphology, Hill and Landform

To differentiate the two landforms, 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. Due to their distinctive shapes, buttes are frequently landmarks in plains and mountainous areas.

Formation

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.

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