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Earthquakes in Iran from 1990 to 2006, by United States Geological Survey Iran Faults. Iran is one of the most seismically active countries in the world, being crossed by several major faults that cover at least 90% of the country. [1] As a result, earthquakes in Iran occur often and are destructive.
Central Iran in a broad sense, comprising the whole area between the North and South Iranian ranges. Within the Iranian plate the Central-East Iran microplate is bordered by the Great Kavir Fault in the north, by the Nain–Baft Fault in the west and southwest and by the Harirud Fault in the east. It is surrounded by the Upper Cretaceous to ...
You can propose images to clean up, improve, create or translate as well. Captions. English. Iran Faults map Items portrayed in this file ...
The library of the Geological Survey and Mineral Exploration of Iran (GSI) was established in 1959 with the aim of collecting, organizing and disseminating geological information. The GSI library currently has the most complete collection of specialized books and publications in geosciences with more than 10,000 titles of books and reports in ...
San Andreas Fault System (Banning fault, Mission Creek fault, South Pass fault, San Jacinto fault, Elsinore fault) 1300: California, United States: Dextral strike-slip: Active: 1906 San Francisco (M7.7 to 8.25), 1989 Loma Prieta (M6.9) San Ramón Fault: Chile: Thrust fault: Sawtooth Fault: Idaho, United States: Normal fault: Seattle Fault ...
Satellite images reveal fault line through city near epicentre of Turkey’s deadly earthquake. Emily Atkinson. February 10, 2023 at 8:54 AM.
Parts of northwestern Iran are part of the Armenian highlands, which adjoins it topographically with other parts of neighbouring Turkey, Armenia, Azerbaijan, and Georgia. [4] Iran has only two expanses of lowlands: the Khuzestan Plain in the southwest and the Caspian Sea coastal plain in the north. The former is a roughly triangular-shaped ...
In geology, the plateau region of Iran primarily formed from the accretionary Gondwanan terranes between the Turan platform to the north and the Zagros fold and thrust belt; the suture zone between the northward moving Arabian plate and the Eurasian continent is the Iranian plateau.