kõrgmäestik
Kõrgmäestik refers to a high-altitude plateau or mountainous region characterized by its significant elevation above sea level. These areas are typically found in the interior of continents and are often bordered by lower-lying plains or coastal regions. The defining feature of a kõrgmäestik is its general flatness or undulating topography at high altitudes, rather than sharp, jagged peaks, which would be characteristic of a mäestik or mountain range.
The formation of kõrgmäestikud can be attributed to various geological processes, including tectonic uplift, volcanic activity,
Climate in kõrgmäestikud is typically cold and dry, with significant diurnal and seasonal temperature variations. Precipitation