Results 171 to 180 of about 22,175 (200)
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Structural stability of andesite volcanoes and lava domes

Philosophical Transactions of the Royal Society of London. Series A: Mathematical, Physical and Engineering Sciences, 2000
Slope failures resulting from structural instability of andesitic volcanic edifices can generate mobile debris avalanches that travel long distances down or beyond the flanks of volcanoes. More than 20 major slope failures have occurred worldwide over the past 500 years, a rate exceeding that of caldera collapse.
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Causes and consequences of pressurisation in lava dome eruptions

Earth and Planetary Science Letters, 1997
Abstract High total and fluid pressures develop in the interior of high-viscosity lava domes and in the uppermost parts of the feeding conduit system as a consequence of degassing. Two effects are recognised and are modelled quantitatively. First, large increases in magma viscosity result from degassing during magma ascent.
openaire   +1 more source

Lava Dome Eruptions

2015
Eliza S. Calder   +3 more
openaire   +1 more source

Mechanical and topographic factors influencing lava dome growth and collapse

Journal of Volcanology and Geothermal Research, 2021
Claire E Harnett, Michael Heap
exaly  

Šumovit Greben, a tale of a rhyolitic lava dome

Goldschmidt2022 abstracts, 2022
Molnár, Kata   +8 more
openaire   +1 more source

Evolution of the mechanics of the 2004–2008 Mt. St. Helens lava dome with time and temperature

Earth and Planetary Science Letters, 2011
Peter R Sammonds   +2 more
exaly  

Insights into lava dome and spine extrusion using analogue sandbox experiments

Earth and Planetary Science Letters, 2020
Edgar Zorn   +2 more
exaly  

lava dome

2009
openaire   +1 more source

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