Hamoun Jazmoriyan

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Hamoon Jazmourian, a young tectonic subsidence, 150 km west of Iranshahr, 350 meters above sea level.

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The area of the wetland of Hamoon Jazmourian is 3300 km2 in the high season, and due to the climatic conditions, in most cases, most of it becomes salt clay and clay clay.

  • Background information

    In the past, it was believed to be the southern edge of the Lut Bloc, but now it is believed that the Jasmourian is a kind of downhill subsidence in which the formation of the Omani oceanic subduction is submerged, as well as the operation of fault lines with Drowning, in particular the Bashaghrd fault complex, have played a role.
  • Specific information

    There are numerous permanent and temporary rivers and streams, among which the Bampour and Hell River are more important.
  • Best time

    Hamoon Lagoon is a seasonal lake that varies greatly in wet and dry seasons. As long as it disappears in most places late in the summer and early autumn.
  • Must know

    Hamoon Jazmourian is at the center of a young tectonic subsidence, located between the Jabal Barz mountains (north) and Bashagurt Mountains (south).

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