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
Bié Plateau Railway connects it to the ocean and its principal towns are Huambo and Kuito. Bié Plateau The Bié Plateau or Central Plateau of Angola is a plateau that occupies most of central Angola. The elevation of the plateau is from 1,520 m to 1,830 m. Several major rivers originate from the plateau such as the Cunene River, the Kuanza River, and the Kwango River. Its climate is cool and has enough rainfall to allow for the cultivation of coffee, corn, rice, sisal, sugarcane, and peanuts. Along the more elevated parts, more rain falls, but it gradually declines further within. About