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Physical Process

Badlands Formation

Geomorphology

The carving of intricately dissected, sparsely vegetated terrain from soft sedimentary rock or clay by rapid rill and gully erosion, typically in semi-arid climates where infrequent but intense rainfall strips soil faster than vegetation can stabilize it. The result is a maze of narrow ridges, ravines and hoodoos with almost no soil cover, as seen in the badlands of the Dakotas and northern China's Loess Plateau.

Facts
Process Type
Hydrological 1
Timescale
About 25 millimetres (1 inch) per year at Badlands National Park 1
Connections

Caused By

Sources
1. Badlands (Wikipedia)
  • Formation section
    Badlands arise from a combination of an impermeable but easily eroded ground surface, sparse vegetation, and infrequent but heavy rainfall.
  • Erosion rate section
    However, it has been estimated that the badlands of Badlands National Park erode at the relatively high rate of about one inch or 25 millimetres per year.
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