| http://www.w3.org/ns/prov#value | - Typically their topography is not as regular as where folding is the most important process, but it is usually dominated by parallel ridges of resistant rock divided by valleys of weaker rock, as in the eastern flank of the Canadian Rocky Mountains or in the Jura Mountains of France and Switzerland.Most fold and thrust belts are bounded on one side, or lie parallel to, a belt or terrain of crystal
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