geoterrasing

Geoterrasing is a hypothetical concept that combines elements of geology and terracing. It suggests a process by which natural geological formations are modified or shaped to create level surfaces, similar to agricultural terracing but on a much grander scale and often involving natural earthworks. This could occur through slow geological processes such as erosion and sedimentation, or potentially through massive, though speculative, natural events.

The idea envisions large-scale topographic alteration where natural forces, or perhaps even ancient, unknown civilizations, created stepped landscapes resembling natural terraces. These features might be found in areas with significant geological activity or long periods of stable erosion. Unlike human-made terraces, geoterraces would be formed by the inherent properties and actions of the Earth's crust and surface processes over vast timescales.

The term is not widely recognized in scientific literature and is largely theoretical or used in speculative contexts. It draws parallels to natural landforms that exhibit terraced appearances, such as certain alluvial fans, volcanic slopes, or layered sedimentary rock formations. The hypothetical nature of geoterrasing means its application is primarily in conceptual discussions or imaginative scenarios rather than established geological phenomena.