Inselbergs are isolated rises above a plain which consist of hard bedrock. If they have a soil cover, then this is very sparse. They vary in height depending on their development, and they take on different forms, as far as both ground plan and cross section are concerned, according to their genesis and lithology. Microforms caused by weathering can have formed on the rock surfaces.When describing inselberg formation, one must take into account weathering and erosion, which are above all regulated by soaking. This, in turn, is controlled by climate, soil cover, the lithology, the water balance, and the vegetation. In addition, the production of organic acids is an important factor for weathering.Inselbergs are clearly defined landscape elements, which allows observation of the interplay of various physiogeographic factors. This geoecological viewpoint is more comprehensive than merely stating that inselbergs are hard or massive rock. On the other hand, inselbergs are independent systems, which can be better understood by taking into account geomorphological processes and their evolution. In Phytogeomorphology Howard and Mitchell (1985) stress the interdependence of land forms and plants. Whilst the former grew over a long period of time and therefore can show a trend in their development, the latter have conformed to to day's conditions. "Thus, in combination, the two form a powerful tool for the survey, management, and planning of our environment:' Diversity of Forms and TerminologyBornhardt (1900) described inselbergs or inselberg landscapes as isolated rises which he had recognized as being an independent type of relief in

No abstract

No abstract

No abstract

No abstract