Syn‐eruptive hydration of volcanic ash records pyroclast‐water interaction in explosive eruptions

Author(s):  
Michael R. Hudak ◽  
Ilya N. Bindeman ◽  
Matthew W. Loewen ◽  
Thomas Giachetti
1998 ◽  
Vol 35 (3) ◽  
pp. 290-301 ◽  
Author(s):  
M B Lambert

Nine stromatolite localities in the Back River volcanic complex occur at the boundary between 2692 Ma felsic dome-flow complexes, marking the latest eruptions of this stratovolcano, and overlying turbiditic sedimentary rocks of the Beechy Lake Group, Yellowknife Supergroup. Stromatolites form lenses isolated within coarse volcanic breccia at margins of felsic dome-flow complexes, and 2 m thick bioherms that extend laterally for hundreds of metres. Thin units contain wavy laminae and open-spaced, linked mounds, which form thin encrustations on breccia blocks, or clusters of mounds with low synoptic relief. Thick successions comprise undulatory, flat laminated dolomite that contains wrinkled wavy laminae, pseudocolumnar forms, and locally elongate, low-relief mounds. These units typically contain millimetre-scale layers of fine volcanic ash at regular intervals, testifying periodic explosive eruptions during deposition of microbial mats. The stromatolites, which are identified by gross morphology and distinctive laminae, are all stratiform types. Carbonate units all occur on the seaward side of the volcanic dome-flow complexes that straddled the shoreline around the volcano. The stromatolites probably represent isolated microbial communities that may have developed around areas of fumarolic (or hydrothermal) activity associated with these domes. Stratigraphy seaward from the domes comprises carbonate-cemented dome-flanking breccia, stromatolitic and oolitic carbonate, pebbly rhyolite volcarenite, carbonaceous mudstones, banded iron formation, and turbidites. Thus the stromatolites mark a local environment where life flourished in an Archean sea that lapped onto active volcanic domes along the shallow flanks of an emergent stratovolcano.


2007 ◽  
Vol 45 ◽  
pp. 87-94 ◽  
Author(s):  
H. Tuffen ◽  
D.W. McGarvie ◽  
J.S. Gilbert

AbstractSimple analytical models of subglacial eruptions are presented, which simulate evolving subglacial cavities and volcanic edifices during rhyolitic eruptions beneath temperate glaciers. They show that the relative sizes of cavity and edifice may strongly influence the eruption mechanisms. Intrusive eruptions will occur if the edifice fills the cavity, with rising magma quenched within the edifice and slow melting of ice. Explosive magma–water interaction may occur if a water- or steam-filled gap develops above the edifice. Meltwater is assumed to drain away continuously, but any gap above the edifice will be filled by meltwater or steam. Ductile roof closure will occur if the glacier weight exceeds the cavity pressure and is modelled here using Nye’s law. The results show that the effusion rate is an important control on the eruption style, with explosive eruptions favoured by large effusion rates. The models are used to explain contrasting eruption mechanisms during various Quaternary subglacial rhyolite eruptions at Torfajökull, Iceland. Although the models are simplistic, they are first attempts to unravel the complex feedbacks between subglacial eruption mechanisms and glacier response that can lead to a variety of eruptive scenarios and associated hazards.


Author(s):  
С.И. Мальковский ◽  
А.А. Сорокин ◽  
О.А. Гирина

Пепловые облака и шлейфы, возникающие при эксплозивных извержениях вулканов Камчатки и Курил, представляют большую опасность для авиации. Поэтому актуальными задачами являются прогнозирование и анализ их перемещения. Для их решения в составе АИС Сигнал создана подсистема моделирования, позволяющая прогнозировать направление, скорость и высоту перемещения пепловых облаков и шлейфов в атмосфере. В то же время для более точной оценки представляемой ими опасности требуется определять не только их качественные, но и количественные характеристики. В статье рассмотрены результаты работ по развитию возможностей АИС Сигнал. Дано описание разработанных инструментов, позволяющих прогнозировать концентрацию пепла на эшелонах полетов самолетов, а также мощность и массу пепла, выпавшего на поверхность земли. Приводятся результаты выполненных численных экспериментов, показавших хорошую согласованность со спутниковыми данными. Purpose. Ash clouds and plumes forming during explosive eruptions of the volcanoes of Kamchatka and the Kuril Islands pose a great danger to aviation flights. In this regard, the urgent and important task is to predict and analyze their movement. To solve this task, a modelling subsystem based on the PUFF model was created as part of the automated information system (AIS) Signal. It allows to predict the direction, speed and height of the propagation of ash clouds and plumes in the atmosphere. At the same time, for more accurate assessment of the danger of ash clouds and plumes, it is necessary to determine not only their qualitative, but also quantitative characteristics, for example, the concentration of ash at the flight levels of aircrafts, the amount of ash deposited on the surface, etc. To solve this problem, research was done to expand the capabilities of the AIS Signal by integrating the Eulerian FALL3D model into it. The present article presents the results of this work. Methodology. Implementation of system and user interfaces for automating the processes of collecting and preparing auxiliary data (reference information about volcanoes, meteorological data, etc.), performing numerical calculations in the FALL3D model and visualizing the results obtained, was carried out on the basis of similar interfaces created earlier in AIS Signal for the PUFF model. This significantly accelerate the process of integration the FALL3D model into the existing AIS modelling subsystem. Implementation of the operating modes of the subsystem and evaluating the efficiency of its functioning were carried out as part of the study of ash clouds and plumes propagation that formed during explosive events on the volcanoes of Kamchatka. Findings. As part of the integration of the FALL3D model into the modelling subsystem, informational interaction of its software components with the services of AIS Signal was organized. Algorithms for the formation of collections of meteorological data necessary for the functioning of the model were proposed and implemented. User interfaces have been created that allow specialists to calculate the characteristics of ash clouds with the ability to set detailed initial parameters for an explosive event and model settings. Originality. The integration of the FALL3D model into the AIS Signal significantly expands its ability to predict propagation of ash clouds and plumes formed during explosive eruptions of the volcanoes of Kamchatka and the Kuril Islands. In addition to the instruments for determining the direction, speed, and height of the spread of volcanic ash, tools have been developed to determine the ash concentration at the flight levels of aircrafts, as well as the thickness and mass of the ashfall. Numerical experiments have showed a good agreement between the obtained modelling results and the satellite data.


Geology ◽  
2019 ◽  
Vol 47 (5) ◽  
pp. e462-e462
Author(s):  
A. Aravena ◽  
M. de' Michieli Vitturi ◽  
R. Cioni ◽  
A. Neri

2021 ◽  
Author(s):  
Olga Girina ◽  
Melnikov Dmitry ◽  
Manevich Alexander ◽  
Nuzhdaev Anton ◽  
Romanova Iraida ◽  
...  

<p>Strong explosive eruptions of volcanoes are the most dangerous for aircraft because they can produce in a few hours or days to the atmosphere and the stratosphere till several cubic kilometers of volcanic ash and aerosols. Ash plumes and the clouds, depending on the power of the eruption, the strength and wind speed, can travel thousands of kilometers from the volcano for several days, remaining hazardous to aircraft, as the melting temperature of small particles of ash below the operating temperature of jet engines.</p><p>There are 30 active volcanoes in the Kamchatka, and several of them are continuously active. Scientists of KVERT monitor Kamchatkan volcanoes since 1993. In 2020, four of these volcanoes (Sheveluch, Klyuchevskoy, Bezymianny, and Karymsky) had strong and moderate explosive eruptions.</p><p>The eruptive activity of Sheveluch volcano began since 1980 (growth of the lava dome) and it is continuing at present. In 2020, strong explosions sent ash up to 7-10 km a.s.l. on 08 April, and 22 and 29 December. Ash from explosions rose up to 5-6 km a.s.l. on 13 June, and 24 December. Ash plumes extended more 625 km mainly to the south-east of the volcano. A form of resuspended ash was observed on 20 April, 28 June, 24 August, and 07-10 October: ash plumes extended for 310 km to the northeast and southeast of the volcano. Activity of Sheveluch was dangerous to international and local aviation.</p><p>Two moderate explosive-effusive eruptions of Klyuchevskoy volcano occurred in 2020: first from 01 November 2019 till 03 July 2020, and second from 30 September, it is continuing in 2021. Explosions sent ash up to 7 km a.s.l., gas-steam plumes containing some amount of ash extended for 465 km to the different directions of the volcano. The lava flows moved along Apakhonchichsky and Kozyrevsky chutes. Activity of the volcano was dangerous to local aviation.</p><p>The strong explosive eruption of Bezymianny volcano occurred on 21 October: explosions sent ash up to 11 km a.s.l., the large ash cloud was located over Klyuchevskoy group of volcanoes long time and later drifted up to1200 km to the southeast of the volcano. Activity of the volcano was dangerous to international and local aviation.</p><p>Eruptive activity of Karymsky volcano was uneven in 2020: ash explosions were observed from one (June) to seven (October) days a month, for five months the volcano was quiet. Explosions rose ash up to 8 km a.s.l. (08 November), ash plumes and clouds drifted for 380 km to the different directions of the volcano. The eruptive volcanic activity was observed in April, May, June, July, October, November, and December. Activity of Karymsky was dangerous to international and local aviation.</p>


Geology ◽  
2018 ◽  
Vol 46 (10) ◽  
pp. 867-870 ◽  
Author(s):  
Alvaro Aravena ◽  
Mattia de’ Michieli Vitturi ◽  
Raffaello Cioni ◽  
Augusto Neri

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