In mountain sculpture, concave forms (valleys, basins, boilers) can be distinguished and convex (peaks, turns, kicks, bules). Convex forms combine into mountain ridges or mountainous massifs, these in turn in the mountain range. Band and massifs together with the foothills and mountains of downtime are made up of mountain chains. Several mountain chains with common geological features, created during the same folding, bear the name of the mountain system. Folded and framework mountains are created as a result of orogenic processes, while volcanic as a result of volcanic activities, and the final activity as a result of erosion and denudation activities mainly water.
In mountain sculpture, concave forms (valleys, basins, boilers) can be distinguished and convex (peaks, turns, kicks, bules). Convex forms combine into mountain ridges or mountainous massifs, these in turn in the mountain range. Band and massifs together with the foothills and mountains of downtime are made up of mountain chains. Several mountain chains with common geological features, created during the same folding, bear the name of the mountain system. Folded and framework mountains are created as a result of orogenic processes, while volcanic as a result of volcanic activities, and the final activity as a result of erosion and denudation activities mainly water.
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