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- W2561731261 abstract "This article deals with the introduction and explanation of the two nueeardentes of “Mue’el Valley” and “Shirvandareh Valley” which are one type of the pyroclastic flows of Sabalan volcano. One of the features of nueeardente in these two valleys is the presence of large blocks in upstream of valley and the abundance of ash in downstream which it has happened in one stage in Mue’el and in several stages in Shirvandareh Valley. Considering the antiquity of the great Sabalan volcano and numerous changes that have happened during these long years in the region, determining the temperature of nueeardente was impossible. But what could be mentioned as a sign of high temperature because of nueeardente is the presence of rust ground mass on piece levels which indicate hot water steam (500°C to 600°C). Also puzzle breakings like those in these rocks should be the result of severe explosion blast and very fast movements of nueeardente that has broken these rocks instantly. These nueeardentes are pelean type and they are more or less synchronous, and the main reason could be the huge explosion which happened because of the second caldra’s subsidence. By comparing deposits of the two nueeardentes of Mue’el Valley and Shirvandareh Valley, it is observed that the extent, thickness, and size of blocks are higher in Shirvandareh than those in Mue’el Valley. Also considering higher levels of pieces’ adherence and hardness of deposits, it can be concluded that the temperature of this complex was higher than that of Mue’el Valley, and in general the power of Shirvandareh’s nueeardente is more than the Mue’el Valley’s." @default.
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- W2561731261 date "2016-01-01" @default.
- W2561731261 modified "2023-10-01" @default.
- W2561731261 title "The Nuée Ardentes of Sabalan Volcano in Iran" @default.
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- W2561731261 doi "https://doi.org/10.4236/ojg.2016.612110" @default.
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