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  • Print publication year: 1968
  • Online publication date: March 2008


from PART 1 - THE LAND
This chapter deals with the geology of Iran, the information of which is somewhat uneven. The stratigraphical column in Iran contains samples of all the systems, from Pre-Cambrian to Quaternary; and from the beginning of the Palaeozoic onwards, diagnostic fossils are sometimes abundant. An introduction to the geomorphology of the country can be made by journeying across it from south-west to north-east. Starting then from the Shaṭṭ al-ʿArab near Ābādān and crossing an occasionally flooded alluvial plain for seventy miles, never far from the meanders of the Karun river, one comes to a series of low isolated ridges of brown sandstone, the Ahvāz hills. The Zagros range skirts its south-western side for 800 miles and beyond the Zagros are the plains of Iraq or Mesopotamia, the growing delta of the Euphrates and Tigris, and the Persian Gulf. These elements forming the west of the region have features of structural history in common.
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The Cambridge History of Iran
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