Damavand Volcano, Tehran (Iran)
by Mostafa Ganjian, Tehran, Islamic Repablic of Iran
Submitted on 10 January 2010
Featured on GeoLog, the official blog of the European Geosciences Union
Categories
- Earth Magnetism & Rock Physics (334)
- Field (2636)
- Geochemistry, Mineralogy, Petrology & Volcanology (815)
Location
- Asia (974)
- Southern Asia (259)
- Iran (Islamic Republic of) (114)
- Exact location (52.1315 E, 35.9447 N)
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Canon S3IS
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Credit: Mostafa Ganjian (distributed via imaggeo.egu.eu)
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Konstantinos Kourtidis 11 years ago
A nice cap cloud can be seen at the top of the mountain. Cap cloud is an orographic cloud that is formed over a mountain peak, formed by the cooling and condensation of moist air climbing up and over the peak. Cap clouds appear to remain stationary.