Jungquartär und End-Mesolithikum in der Provinz Kerman (Iran)

Reinhold Huckriede
The main masses of detritus and silts („See-Löß"), deposited in water and filling the vast plateau-valleys of Kerman-area, seem to have been formed during semi-arid conditions till in older Holocene times. North of Buhabad and in the town of Kerman, areas which are now-days arid or nearly desertic, sediments of a brackisch lake and of shallow fresh-or oligohaline waters indicate that once precipitation and humidity were higher than doday. In Kerman they contain layers of...