|
The Red Hills is the name of a physiographic region located mostly in Clark, Comanche and Barber counties in southern and central Kansas. This undulating terrain of red-tinted sediments, a product of the underlying geology, does not fit the conventional description of the Great Plains landscape of Kansas. The red bed sediments of the Red Hills were deposited in an arid continental closed basin that formed within the Pangaean supercontinent during the Permian Period.〔Warren, J.K. 2006. Evaporites: sediments, resources and hydrocarbons. Berlin: Springer-Verlag, 1035 pp. (See p. 308 for "Permian lacustrine redbeds, Kansas")〕 Water often flooded this basin forming ephemeral playas of somewhat acidic waters.〔Benison, K.C. and Goldstein, R.H. 2001. Evaporites and siliciclastics of the Permian Nippewalla Group of Kansas, USA: a case for non-marine deposition in saline lakes and saline pans. Sedimentology 48(1):165-188.〕 The shallow playas were intermittently flooded then dried leaving a mixture of lacustrine sediments and gypsum evaporites. The red color derives from the oxidation of iron contained within the deposits. The region is also known as the Gyp Hills, because of the large natural deposits of gypsum in this area. The dissolution of underlying gypsum beds has led to the formation of sinkholes which are common features within the Red Hills region.〔 Big Basin and Little Basin are two well-known sinkholes in western Clark County. The Red Hills have scenic vistas and some small steep canyons. High points include Mount Nebo (), Mount Jesus () and Mount Lookout (), in Clark County, Kansas. ==See also== *Big Basin Prairie Preserve *Tallgrass Prairie National Preserve *Flint Hills 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「Red Hills (Kansas)」の詳細全文を読む スポンサード リンク
|