supracontinental

Supracontinental refers to phenomena or entities that exist above or on the surface of a continent. In a geological context, it often describes features that are superimposed or external to the continental crust itself. For example, sedimentary basins that are not directly formed by the deformation of the continental crust but are rather a result of external depositional processes can be considered supracontinental. This term can also be applied to atmospheric or climatic conditions that are characteristic of a continental landmass.

In a broader sense, supracontinental can describe anything that is located on or above a continent, distinguishing it from features within the Earth's crust or oceanic realms. The concept emphasizes a position relative to the continental landmass, typically referring to surface or atmospheric phenomena. It is a descriptive term used to delineate location and scale within Earth's systems.