A questionnaire to survey the common petrological monitoring procedures adopted by
volcano monitoring institutions has been developed, aimed at identifying prevailing …

Volcano tourism and tourism to geothermal destinations is increasingly popular. If such
endeavors are to be a sustainable sector of the tourism industry, tourists must be made …

The characteristics of magma supply, storage, and transport are among the most critical
parameters governing volcanic activity, yet they remain largely unconstrained because all …

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 …

Intra-oceanic arc systems (IOASs) represent the oceanic endmember of arc–trench systems
and have been the most important sites of juvenile continental crust formation for as long as …

The dichotomy between explosive volcanic eruptions, which produce pyroclasts, and
effusive eruptions, which produce lava, is defined by the presence or absence of …

Olivine composition and zoning patterns are widely used to reconstruct the evolution of
mafic magmas from source to surface and to extract time scales of magmatic processes …

Active basaltic eruptions enable time-series analysis of geochemical and geophysical
properties, providing constraints on mantle composition and eruption processes,,–. The …

The Pu'u'Ō'ō-Kūpaianaha eruption on the east rift zone of Kilauea Volcano, Island of Hawai'i,
began on January 3, 1983. The early years of the eruption are vividly remembered for lava …

Rangitoto Volcano is the youngest and largest eruptive centre in the monogenetic intraplate
Auckland Volcanic Field (AVF). The stratigraphy of Rangitoto pyroclastic deposits that have …