Continental Crumple Zone: Zagros
The Arabian tectonic plate and the Eurasian plate meet in continental collision at the Zagros mountain range in southwest Iran. The Zagros are among the world’s most seismically active mountains, formed as a “fold-and-thrust” belt around 1500km long and 300 km wide. Part of the Alpine-Himalayan belt, Earth’s crust is shortening at up to 9 mm per year at the Zagros Mountains, accommodated as both thrust faults in the basement rocks and folds in the overlying sediments.
(via earthstory)






