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Mesas in the Glass Mountains of western Oklahoma.

Several mesas near Los Alamos, New Mexico.

Tucumcari Mountain is a mesa outside of Tucumcari, New Mexico.

A mesa (Spanish, Portuguese, Arabic and Arwi for "table") is an elevated area of land with a flat top and sides that are usually steep cliffs. It takes its name from its characteristic table-top shape. It is a characteristic landform of arid environments, particularly the southwestern United States. Many examples are also found in Spain, North and South Africa, Arabia, India, Australia, and the Badlands and Colorado regions of North America. The largest mesa in the world is considered to be the Grand Mesa in western Colorado in the United States. Urraca Mesa in northern New Mexico is particularly famous for being "haunted" in local tradition.

Etymology

The term mesa is used in the southwestern United States, in both English and Spanish, to describe a flat-topped mountain or hill. Elsewhere, in Spanish such a landform is more usually known as a meseta.

Formation

Mesas form usually in areas where horizontally layered rocks are uplifted by tectonic activity, but may form also in its absence.

Mesas are formed by weathering and erosion. Variations in the ability of different types of rock to resist weathering and erosion cause the weaker types of rocks to be eroded away, leaving the more resistant types of rocks topographically higher relative to their surroundings.¹ This process is called differential erosion. The most resistant rock types include sandstone, conglomerate, quartzite, chert, limestone, lava flows and sills.¹ Lava flows and sills, in particular, are very resistant to weathering and erosion, and often form the flat top, or caprock, of a mesa. The less resistant rock layers are mainly made up of shale, a softer rock that weathers and erodes more easily.¹

The differences in strength of various rock layers is what gives mesas their distinctive shape. Less resistant rocks are eroded away on the surface into valleys, where they collect water drainage from the surrounding area, while the more resistant layers are left standing out.¹ A large area of very resistant rock, such as a sill may shield the layers below it from erosion while the softer rock surrounding it is eroded into valleys, thus forming a caprock. Differences in rock type also reflect on the sides of a mesa, as instead of smooth slopes, the sides are broken into a staircase pattern called "cliff-and-bench topography."¹ The more resistant layers form the cliffs, or stair steps, while the less resistant layers form gentle slopes, or benches, between the cliffs. Cliffs retreat and are eventually cut off from the main cliff, or plateau, by basal sapping. When the cliff edge does not retreat uniformly, but instead is indented by headward eroding streams, a section can be cut off from the main cliff, forming a mesa.¹ Basal sapping occurs as water flowing around the rock layers of the mesa erodes the underlying soft shale layers, either as surface runoff from the mesa top or from groundwater moving through permeable overlying layers, which leads to slumping and flowage of the shale.² As the underlying shale erodes away, it can no longer support the overlying cliff layers, which collapse and retreat. When the caprock has caved away to the point where only a little remains, it is known as a butte.

See also

• Plateau
• Dissected plateau
• Butte
• Potrero
• Tepui
• Tuya
• Table Mountain

References

1. ^ ^{a b c d e f} Easterbrook, Don J. (1999). Surface Processes and Landforms. Upper Saddle River, NJ: Prentice Hall. 
2. ^ Choreley, Richard J.; Stanley A. Schumm, David E. Sugden (1985). Geomorphology. New York: Methuen. 

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