The deformed rocks of Iran are shaped as a result of sturdy mountain ridges and valleys within the Larger Caucasus mountain vary, southwest of the Caspian Sea. Between 10 million and 50 million years in the past, its development was marked by sedimentary layers crushed throughout the first impression between the Arabian and Eurasian tectonic plates. The vividly colored rocks produced by the sedimentary layers gathered over millennia vary in tone from terracotta to greenish to bluish. Utilizing satellite tv for pc footage, NASA’s Jet Propulsion Laboratory and Earth Observatory have proven how the panorama tended to cluster over time.
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