Kruinvlak
Kruinvlak is a term used in geology and geography to describe the flat or gently sloping surface at the summit of a mountain or plateau. It is often the result of prolonged erosion by natural processes such as weathering, abrasion, and denudation. These flat-topped landforms can be found in various mountainous regions around the world, and their formation is influenced by factors like rock type, geological structure, and climate.
The formation of a kruinvlak typically occurs over geological timescales. Initially, a region of elevated land,
The presence of kruinvlakken can provide valuable insights into the past geological history and erosional processes