
What do you understand by the term "intermontane plateau"? Where would you find one in Asia?
Answer
555.9k+ views
Hint:The Intermontane Plateaus of the Western United States is one of eight U.S. states. The region is made up of plateaus and mountain ranges. It is divided into body parts, each divided into body parts.
Complete answer:
A fenced-in or surrounded mountain is known as a central mountain range. The Plateau of Tibet and the Plateau of Mongolia are two mountains in central Asia. The Plateau of Tibet is surrounded by the Kunlun Mountains in the north and the Himalayas in the south. The province was elevated and subdivided into large blocks by errors or mutations in a single body and as a result was exposed to long-term losses in the central erosion cycle. They are also widely promoted with a revitalized movement of some faulty lines. The current erosion cycle was introduced towards the end of the higher education period when the deepest trenches in the region were submerged. They are also evident in the construction of a series of large, south-facing, sloping ridges of an unusual structure at the edges of high-rise buildings to the north. Each decline stops when the resistant formulation exceeds the weakness. Each drop is divided into the next high point with a broad step of weak fibers.
Note: The state of Plateau, west of the mountains south of Rocky, is well-known for its large forms. These have improved the overall size of the Palaeozoic, Mesozoic and Tertiary structures in almost the middle, as well as dry climate.
Complete answer:
A fenced-in or surrounded mountain is known as a central mountain range. The Plateau of Tibet and the Plateau of Mongolia are two mountains in central Asia. The Plateau of Tibet is surrounded by the Kunlun Mountains in the north and the Himalayas in the south. The province was elevated and subdivided into large blocks by errors or mutations in a single body and as a result was exposed to long-term losses in the central erosion cycle. They are also widely promoted with a revitalized movement of some faulty lines. The current erosion cycle was introduced towards the end of the higher education period when the deepest trenches in the region were submerged. They are also evident in the construction of a series of large, south-facing, sloping ridges of an unusual structure at the edges of high-rise buildings to the north. Each decline stops when the resistant formulation exceeds the weakness. Each drop is divided into the next high point with a broad step of weak fibers.
Note: The state of Plateau, west of the mountains south of Rocky, is well-known for its large forms. These have improved the overall size of the Palaeozoic, Mesozoic and Tertiary structures in almost the middle, as well as dry climate.
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