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Damavand Volcano Eruption: Fumaroles Seen At Summit, Iran, Tehran , Klyuchevskaya, Fasham Earthquake скачать в хорошем качестве

Damavand Volcano Eruption: Fumaroles Seen At Summit, Iran, Tehran , Klyuchevskaya, Fasham Earthquake 2 месяца назад

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Damavand Volcano Eruption: Fumaroles Seen At Summit, Iran, Tehran , Klyuchevskaya, Fasham Earthquake
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Damavand Volcano Eruption: Fumaroles Seen At Summit, Iran, Tehran , Klyuchevskaya, Fasham Earthquake

A comprehensive paper about Mount Damavand here: https://scholar.google.com/citations?... The geology of Damavand volcano, Alborz Mountains, northern Iran Authors Jon Davidson, Jamshid Hassanzadeh, Reinis Berzins, Daniel F Stockli, Behrooz Bashukooh, Brent Turrin, Ali Pandamouz Mount Damavand (Persian: دماوند [dæmɒːvænd] is a stratovolcano, the highest peak in Iran and Western Asia and the highest volcano in Asia and the 2nd highest volcano in the Eastern Hemisphere (after Mount Kilimanjaro), at an elevation of 5,671 metres (18,606 ft). Damāvand has a special place in Persian mythology and folklore. It is in the middle of the Alborz range, adjacent to Varārū, Sesang, Gol-e Zard, and Mīānrūd. It is near the southern coast of the Caspian Sea, in Amol County, Mazandaran Province, 66 km (41 mi) northeast of the city of Tehran. Mount Damāvand is the 12th most prominent peak in the world and the second most prominent in Asia after Mount Everest. It is part of the Volcanic Seven Summits mountaineering challenge. Damavand is a significant mountain in Persian mythology. It is the symbol of Iranian resistance against despotism and foreign rule in Persian poetry and literature. In Zoroastrian texts and mythology, the three-headed dragon Aži Dahāka was chained within Mount Damāvand, there to remain until the end of the world. In a later version of the same legend, the tyrant Zahhāk was also chained in a cave somewhere in Mount Damāvand after being defeated by Kāveh and Fereydūn. Persian poet Ferdowsi depicts this event in his masterpiece, the Shahnameh: {He brought Zahhak like a horse to mount Damavand, And tied him at the peak, tight and bound.} The mountain is said to hold magical powers in the Shahnameh. Damāvand has also been named in the Iranian legend of Arash (as recounted by Bal'ami) as the location from which the hero shot his magical arrow to mark the border of Iran, during the border dispute between Iran and Turan. The poem Damāvand by Mohammad Taqī Bahār is also one fine example of the mountain's significance in Persian literature. Mount Damavand is depicted on the reverse of the Iranian 10,000 rial banknote. The origins and meaning of the word "Damavand" is unclear, yet some prominent researchers have speculated that it probably means "The mountain from which smoke and ash arises", alluding to the volcanic nature of the mountain. Mount Damavand rises within the Alborz range in northern Iran, separating the Iranian plateau to the south from the Caspian Sea in the north. This range rises as a result of the collision between the Arabian and Eurasian tectonic plates. This sort of collision is similar to the collision between the Indian and Eurasion plates to the east, which is causing the Himalaya to rise and does not usually create volcanic activity. Despite this, recent research suggests that a hot region created by the collision is what caused the volcano to rise. Seismic wave patterns from earthquakes around the volcano indicate that a magma chamber is present between 2 and 5 kilometres (1.2 and 3.1 mi) below the surface. This is separated into two areas - an inner region of hot, likely molten, magma between 3 and 4.5 kilometres (1.9 and 2.8 mi) depth that is surrounded by an area of dense cooled magma. The top of the chamber is believed to lie to the south of the summit, trending somewhat to the west with depth. The volcano is crowned by a small crater with sulfuric deposits. Despite the lack of historical eruptions, ongoing thermal activity at Mount Damavand suggests the volcano is not extinct. Subsidence at a rate of 5 millimetres (0.20 in) per year and horizontal expansion at 6 millimetres (0.24 in) per year was observed there between 2003 and 2008.

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