Badlands of the Northern Great Plains: Hell with the Fires Out

  • Mark A. Gonzalez
Chapter

Abstract

Badlands occur worldwide and are especially common in the Northern Great Plains of North America. Badlands form where the erosive power of slopewash reaches its maximum expression and is optimized by the combination of steep, local topography; weakly indurated, readily eroded bedrock; and sparsely vegetated hillslopes. Erosional landforms include finely rilled hillslopes, pipes, gullies, pedestals, and hoodoos. Landslides modify many slopes. Depositional and transportational landforms include pediments, fans, and terraces. Clinker is common; it forms when seams of lignite burn subterraneously and bake overlying rock into a naturally fired brick. Badlands of the Northern Great Plains contain paleontological records of the final days of dinosaurs and the emergence of mammals. Badlands capture the imagination with its geologic wonders, paleontological treasures, and spellbinding vistas.

Keywords

Badlands clinker geomorphology Great Plains landforms 

References

  1. Biek RF, Gonzalez MA (2001) The geology of Theodore Roosevelt National Park: Billings and McKenzie counties, North Dakota. North Dakota Geol Surv Misc Series No 86. Bismarck, North DakotaGoogle Scholar
  2. Bluemle JP (1972) Pleistocene drainage development in North Dakota. Geol Soc Amer Bull 83:2189–2193CrossRefGoogle Scholar
  3. Bluemle JP (2000) The face of North Dakota, 3rd edn. North Dakota Geol Surv Educational Series 26. Bismarck, North DakotaGoogle Scholar
  4. Coates DA (1980) Formation of clinker by natural burning of coal beds in the Powder River Basin, Wyoming. In: Carter LM (ed) Proceedings of the fourth symposium on the Geology of Rocky Mountain Coal. Colorado Geol Surv Resource Series No 10:37–40Google Scholar
  5. Gonzalez MA (2001) Recent formation of arroyos in the Little Missouri Badlands of southwestern North Dakota. Geomorphology 38:63–84CrossRefGoogle Scholar
  6. Gries JP (2005) Roadside geology of South Dakota. Mountain Press, Missoula, Montana (4th printing)Google Scholar
  7. Hoganson JW, Murphy EC (2003) Geology of the Lewis and Clark Trail in North Dakota. Mountain Press, Missoula, MontanaGoogle Scholar
  8. Howard AD (1960) Cenozoic history of Northeastern Montana and Northwestern North Dakota with emphasis on the Pleistocene. US Geol Surv Prof Pap 326:107Google Scholar
  9. Murphy EC (2000) Landslides in Western North Dakota. Geol Soc Amer Abstracts with Programs 32(7):57Google Scholar
  10. Murphy EC, Hoganson JW, Forsman NF (1993) The Chadron, Brule, and Arikaree Formations in North Dakota: The Buttes of Southwestern North Dakota. North Dakota Geol Surv Report of Investigations No 96Google Scholar
  11. Roberts LNR, Kirschbaum MA (1995) Paleogeography of the Late Cretaceous of the Western Interior of middle North America: Coal distribution and sediment accumulation. US Geol Surv Prof Pap 1561:115Google Scholar
  12. Schoch HA (1974) Theodore Roosevelt: The story behind the scenery. KC Publications, Las Vegas, NevadaGoogle Scholar
  13. Schumm SA (1962) Erosion on miniature pediments in Badlands National Monument, South Dakota. Geol Soc Amer Bull 73:719–724CrossRefGoogle Scholar

Copyright information

© Springer Science+Business Media B.V. 2009

Authors and Affiliations

  • Mark A. Gonzalez
    • 1
  1. 1.Geoscientist with the Dakota Prairie Grasslands of the United StatesBismarckUSA

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