Cholok Hill

Iran / Esfahan / Natnaz /
Eco land from about 1 milioon years
Nearby cities:
Coordinates:   33°32'43"N   51°59'31"E

Comments

  • The Cholok Hill is one of the structures that formed during dextral strike-slip movements of Qom-Zefreh Fault after Pliocene. The Hill is a recumbent to overturned fold. The southern limb of the fold has cut by a local fault. In this hill Middle Miocene limestones located with angular unconformity on the folded Volcanic rocks of Eocene.
This article was last modified 17 years ago