Dissected plateau Dissected plateau A dissected plateau is a plateau area that has been severely eroded so that the relief is sharp. Such an area may be referred to as mountainous, but dissected plateaus are distinguishable from orogenic mountain belts by the lack of folding, metamorphism, extensive faulting, or magmatic activity that accompanies orogeny. The Allegheny Plateau, the Cumberland Plateau, the Ozark Plateau, and the Catskill Mountains in the United States and the Blue Mountains in Australia and the Deccan Plateau in India are examples of dissected plateaus formed after regional uplift. These older uplifts have been eroded by creeks and rivers
Tsalka Plateau precipitation rate is 740 millimetres. The Tsalka Reservoir occupies the centre of the plateau. Most likely covered largely by forests from Neolithic through Middle Bronze Age ca. 1500 BC, the land today represents mainly ancient dolomitic lava and is largely infertile. Before the Soviet Union, crop growing on the plateau was hindered by severe weather conditions, hail and field mice, which is why animal husbandry and beekeeping were more preferred forms of agriculture. The Tsalka plateau is home to the ancient Trialeti culture, with tumuli dating back to the second millennium BC, discovered in the 1930s. Some tumuli have stone-lined