flanksteilheid
Flanksteilheit is a term used in geology and geomorphology to describe the steepness or inclination of a slope's side. It is a fundamental characteristic of landforms, influencing processes such as erosion, mass wasting, and the distribution of vegetation. The concept of flanksteilheit is important for understanding how landscapes evolve and how stable they are.
In technical contexts, flanksteilheit is often quantified using angles or gradients. A steeper flanksteilheit generally implies
Flanksteilheit is a key parameter in various fields, including hazard assessment, civil engineering, and ecological studies.