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Mountains and mountain belts exist because tectonic processes have created and maintained high elevations in the face of erosion, which works to destroy them.
In general, intracontinental mountain belts are characterized by block faulting.
Moreover, high relief exists within mountain belts and ranges.
The extent to which this process is a major one in mountain belts is controversial.
The effect of this drainage is profoundly influenced by the presence of mountain belts.
Within many mountain belts are plateaus, which stand high but contain little relief.
Continental collisions are responsible for Alpine-, or Himalayan-, type mountain belts.
Most of the differences among mountain belts can be ascribed to some combination of these factors.
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Thus the Venezuelan Andes are an intracontinental mountain belt.
This may reflect the cooling of the granite during late uplift in a young mountain belt.
The central mountain belt contains some of the poorest land and climate for agriculture.
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