kõverkiht

Kõverkiht is an Estonian term that translates to "curved layer" or "bent layer." It is primarily used in the context of geology and soil science to describe geological formations or soil horizons that are not horizontal but are inclined or folded. This curvature can result from various geological processes, such as tectonic forces, erosion, or depositional patterns.

In geology, kõverkiht can refer to stratified rock layers that have been deformed by folding or tilting over time. These deformations are evidence of past geological activity and can provide insights into the Earth's crustal movements. The angle and direction of the curvature are important characteristics for geologists studying these formations.

In soil science, kõverkiht might describe soil horizons that have been displaced or disturbed, leading to a non-horizontal arrangement. This can occur due to processes like solifluction in periglacial environments, mass wasting on slopes, or even human activities such as plowing or excavation. Understanding the nature of a kõverkiht in soil can be important for agricultural practices, land management, and understanding soil development. The term emphasizes the deviation from the typical horizontal layering expected in many undisturbed soil profiles.