One of the largest
landslides that can be easily recognized on satellite images is the Saidmarreh
Landslide in western Iran. The slide occurred about 10,000 years ago when about
20 cubic kilometers (about 5 cubic miles) of Lower Miocene and Eocene limestone
detached along bedding planes and slipped down the north flank of the Kabir Kuh
anticline. The maximum vertical descent was about 1600 meters (5250 feet).
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