Summary
The Applachian Plateau Physiographic Province of the United States has severe landslide problems that are attributed primarily to steep topography and thick colluvial soils. Two basic modes of colluvial soil accumulation on hillsides are identified: 1) on rock benches; and 2) in swales.
The large colluvial masses, unless disturbed by construction activity, were assumed to be stable and to have developed under periglacial conditions. However, processes of colluvial slope development and a recent landslide, activated by abnormally high precipitation at McMechen, indicate that such colluvial masses form continuously and do not require periglacial conditions to explain their existence.
Résumé
La région physiographique de Plateau des Appalaches aux Etats-Unis a des serieux problèmes de glissements de terrain, dus principalement à une topographie escarpée et à de profonds sols colluviaux. On trouve deux sortes principales d’accumulation colluviale sur les collines: (1) sur les bancs d’alluvion rocheux, (2) dans les creux.
Ces grandes masses colluviales, à moins d’être dérangées par une activité de construction, étaient supposées d’être stables et formées dans des conditions périglaciaires. Cependant, des processus de formation de pente colluviale et un récent glissement de terrain, accéléré par des précipitations anormalement hautes à McMechen, indiquent que de telles masses colluviales se forment de façon continue et ne requièrent pas de conditions périglaciaires pour leur développement.
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Gray, R.E., Gardner, G.D. Processes of colluvial slope development at MC Mechen, west Virginia. Bulletin of the International Association of Engineering Geology 16, 29–32 (1977). https://doi.org/10.1007/BF02591439
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DOI: https://doi.org/10.1007/BF02591439