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High steep elevation of the Earth's surface refers to mountainous regions or steep terrains, typically characterized by significant altitude and rugged topography. These areas are often formed by tectonic processes such as folding, faulting, and volcanic activity. Examples include the Himalayas and the Rocky Mountains, where the elevation can rise dramatically within short horizontal distances, creating dramatic landscapes and ecosystems. Such elevations can influence climate, biodiversity, and human activities in the surrounding regions.

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