According to the tectonic and sedimentology evidences, we can include Qeshm as part of the south of Zagros. The external similarities as well as the existing harmony between Qeshm Island's big anticlines and Zagros' anticlines are some proofs confirming this idea.The effect of Namakdan mount's salt dome on the west part of the island is totally abvious and has caused morphologic and tectonic changes in this part of the island.

Source: THE GEOTOURISM ATLAS OF QESHM ISLAND- Author and photographer: Alireza Amrikazemi- Translated into English: Abbas Mehrpooya- Minstry of Industries and Mines GEOLOGICAL SURVEY OF IRAN- National Geoscience Database of Iran.

Pictures

All the pictures were scaned of THE GEOTOURISM ATLAS OF QESHM ISLAND

A view of the fells in kargah Region and Badland type

A piece of rock which is a remnant of the southeast coast

A top view of the Qeshm Roof and the remaining ruins of Kalat-e-Koshtar

A single hill of marl and silt in the island with an interesting morphology