How are plateaus different from mountain ranges?

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While plateaus and mountain ranges are both elevated landforms, they are distinguished primarily by their surface relief and topography.

A plateau is an extensive upland area characterized by low relative relief and a remarkably flat surface, even when situated at high altitudes. In contrast, mountains are defined by their prominence above surrounding terrain, typically exhibiting steep slopes, confined summits, and significant local relief.123

Key differences include:

  • Topography: Mountains are usually found in elongated chains or belts featuring ridges and valleys. Plateaus are defined by their broad, flat horizons, though they may be interrupted by deep canyons or, in some cases, contain smaller mountain ranges within their boundaries.312
  • Geologic Structure: While both can be formed by volcanism, crustal shortening, or thermal expansion, plateaus often result from processes that uplift a surface while maintaining its flatness, such as the heating of the lithosphere. Mountain ranges are typically the result of intense deformation, folding, and faulting that create high-relief, rugged terrain.45

It is important to note that these features can coexist; for example, the Altiplano is a high plateau integrated within the Andes mountain belt.13