Damavand Volcano, Tehran (Iran)
by Mostafa Ganjian, Tehran, Islamic Repablic of Iran
Featured on GeoLog, the official blog of the European Geosciences Union
Categories
- Earth Magnetism & Rock Physics (345)
- Field (2770)
- Geochemistry, Mineralogy, Petrology & Volcanology (864)
Location
- Asia (1026)
- Southern Asia (277)
- Iran (Islamic Republic of) (116)
- Exact location (52.1315 E, 35.9447 N)
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Image properties
1600 × 1200 px;
image/jpeg; 590.4 KB
Camera:
Canon S3IS
Submitted on Jan. 10, 2010
Licence
Creative Commons Attribution-NonCommercial-ShareAlike 3.0 Unported (CC BY-NC-SA 3.0)
Credit
Mostafa Ganjian (distributed via imaggeo.egu.eu)
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Konstantinos Kourtidis 12 years, 10 months 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.