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  • Mass movement of mancos shale crust near Caineville, Utah : a 30-year record
  • This study was designed to quantify rates of mass movement of the surficial material on the Mancos Shale badland, over a 30-year period, and determine what effects slope position, angle, and aspect had on the rates of mass movement. About two-thirds
  • Wind erosion of Mancos Shale badland ridges by sudden drops in pressure
  • One process of erosion of Mancos Shale badlands near Hanksville, Utah, appears to be caused by nearly instantaneous drops in air pressure accompanying gusts of wind. A series of sharp-crested bedrock ridges trend nearly perpendicular to the strong
  • Sediment and solute yield from Mancos Shale hillslopes, Colorado and Utah in Badland geomorphology and piping.
  • Remarques sur la dynamique de surface et l'écoulement sur les versants taillés dans les schistes de Mancos d'après des études de parcelles et de versants naturels. Les apports solides et dissous sont liés aux volume et aux pics d'écoulement mais
  • Patterns in the aggregate stability of Mancos Shale derived soils
  • Salt and sediment contributions to the Colorado River and its tributaries pose economic and environmental concerns for the United States and Mexico. Land use decisions promoting the aggregation of Mancos Shale derived soils are one way to reduce
  • A drainage basin simulation model is used to interpret the morphometry and historical evolution of Mancos Shale badlands in Utah. Field relationships and simulation modelling indicate that the badlands have resulted from rapid downcutting