Magma degassing process during Plinian eruptions
نویسندگان
چکیده
منابع مشابه
Magma degassing during the Plinian eruption of Novarupta, Alaska, 1912
[1] We have modeled the nucleation and isothermal growth of bubbles in dacite from the 1912 Plinian eruption of Novarupta, Alaska. Bubble growth calculations account for the exsolution of H2O and CO2, beginning with bubble nucleation and ending when bubble sizes reproduced the observed size distribution of vesicles in Novarupta pumice clasts. Assuming classical nucleation theory, bubbles nuclea...
متن کاملDegassing during quiescence as a trigger of magma ascent and volcanic eruptions
Understanding the mechanisms that control the start-up of volcanic unrest is crucial to improve the forecasting of eruptions at active volcanoes. Among the most active volcanoes in the world are the so-called persistently degassing ones (e.g., Etna, Italy; Merapi, Indonesia), which emit massive amounts of gas during quiescence (several kilotonnes per day) and erupt every few months or years. Th...
متن کاملMagma degassing during subglacial eruptions and its use to reconstruct palaeo-ice thicknesses
15 16 The degassing of magmatic volatiles during eruptions beneath ice sheets and glaciers, 17 as recorded by the dissolved volatile content quenched in volcanic rocks, could 18 provide powerful new constraints on former ice thicknesses in volcanic areas. As 19 volcanic rocks are readily dateable using radiometric methods, subglacial volcanoes 20 may therefore provide crucial information on the...
متن کاملA Neurocomputing Approach for Monitoring Plinian Volcanic Eruptions Using Infrasound
Plinian volcanic eruptions can inject a substantial amount of volcanic ash and gas into the stratosphere, which can present a severe hazard to commercial air traffic. A hazardous volcanic ash eruption was reported on April 14, 2010, and London’s aviation authority issued an alert that an ash plume was moving from an eruption in Iceland towards northwestern Europe. This eruption resulted in the ...
متن کاملDepth of origin of magma in eruptions
Many volcanic hazard factors--such as the likelihood and duration of an eruption, the eruption style, and the probability of its triggering large landslides or caldera collapses--relate to the depth of the magma source. Yet, the magma source depths are commonly poorly known, even in frequently erupting volcanoes such as Hekla in Iceland and Etna in Italy. Here we show how the length-thickness r...
متن کاملذخیره در منابع من
با ذخیره ی این منبع در منابع من، دسترسی به آن را برای استفاده های بعدی آسان تر کنید
ژورنال
عنوان ژورنال: Journal of Volcanology and Geothermal Research
سال: 2010
ISSN: 0377-0273
DOI: 10.1016/j.jvolgeores.2010.02.018