Tarawera 1886: an integrated review of volcanological and geochemical characteristics of a complex basaltic eruption
The cataclysmic basaltic eruption of Mt. Tarawera in 1886 represents a significant cultural
and scientific event for New Zealand. This review utilises published and new observations …
and scientific event for New Zealand. This review utilises published and new observations …
Physical characterization of long‐lasting hybrid eruptions: the 2021 Tajogaite eruption of Cumbre Vieja (La Palma, Canary Islands)
Long‐lasting, hybrid eruptions can be of complex description and classification, especially
when associated with multiple eruptive styles and multiple products. The 2021 Tajogaite …
when associated with multiple eruptive styles and multiple products. The 2021 Tajogaite …
[HTML][HTML] The summer 2019 basaltic Vulcanian eruptions (paroxysms) of Stromboli
G Giordano, G De Astis - Bulletin of Volcanology, 2021 - Springer
Stromboli is an active, open conduit mafic volcano, whose persistent mild Strombolian
activity is occasionally punctuated by much stronger explosions, known as paroxysms …
activity is occasionally punctuated by much stronger explosions, known as paroxysms …
[HTML][HTML] Monogenetic basaltic volcanoes: genetic classification, growth, geomorphology and degradation
G Kereszturi, K Németh - Updates in volcanology-new advances in …, 2012 - intechopen.com
Plate motion and associated tectonics explain the location of magmatic systems along plate
boundaries [1], however, they cannot give satisfactory explanations of the origin of intra …
boundaries [1], however, they cannot give satisfactory explanations of the origin of intra …
Monogenetic volcanic fields: Origin, sedimentary record, and relationship with polygenetic volcanism
K Németh - What is a volcano, 2010 - books.google.com
ABSTRACT INTRODUCTION that are commonly, but not exclusively, small in eruptive
volume. Monogenetic volcanic fields commonly consist of large numbers of volcanic clusters …
volume. Monogenetic volcanic fields commonly consist of large numbers of volcanic clusters …
Volcanically extruded phosphides as an abiotic source of Venusian phosphine
We hypothesize that trace amounts of phosphides formed in the mantle are a plausible
abiotic source of the Venusian phosphine observed by Greaves et al.[Nat. Astron., https://doi …
abiotic source of the Venusian phosphine observed by Greaves et al.[Nat. Astron., https://doi …
Magma fragmentation in highly explosive basaltic eruptions induced by rapid crystallization
Basaltic eruptions are the most common form of volcanism on Earth and planetary bodies.
The low viscosity of basaltic magmas inhibits fragmentation, which favours effusive and lava …
The low viscosity of basaltic magmas inhibits fragmentation, which favours effusive and lava …
Basaltic explosive volcanism: constraints from deposits and models
BF Houghton, HM Gonnermann - Geochemistry, 2008 - Elsevier
Basaltic pyroclastic volcanism takes place over a range of scales and styles, from weak
discrete Strombolian explosions (∼ 102–103kgs− 1) to Plinian eruptions of moderate …
discrete Strombolian explosions (∼ 102–103kgs− 1) to Plinian eruptions of moderate …
Degassing-driven crystallisation in basalts
Syn-eruptive crystallisation can drastically increase magma viscosity, with profound
implications for conduit dynamics, lava emplacement and volcanic hazards. There is …
implications for conduit dynamics, lava emplacement and volcanic hazards. There is …
In situ observation of nanolite growth in volcanic melt: A driving force for explosive eruptions
Although gas exsolution is a major driving force behind explosive volcanic eruptions,
viscosity is critical in controlling the escape of bubbles and switching between explosive and …
viscosity is critical in controlling the escape of bubbles and switching between explosive and …