Monogenetic basaltic volcanoes are the most common volcanic landforms on the continents.
They encompass a range of morphologies from small pyroclastic constructs to larger shields …

ABSTRACT Auckland Volcanic Field (AVF) is a basaltic intraplate volcanic field in North
Island, New Zealand, upon which> 1.6 million people live. Seismic velocity tomography and …

Monogenetic volcanism produces small-volume volcanoes with a wide range of eruptive
styles, lithological features and geomorphic architectures. They are classified as spatter …

The 26.5 ka Oruanui eruption, from Taupo volcano in the central North Island of New
Zealand, is the largest known 'wet'eruption, generating 430km3 of fall deposits, 320km3 of …

Monogenetic volcanism is commonly represented by evolution of clusters of individual
volcanoes. Whereas the eruption duration of an individual volcano of a volcanic field is …

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 …

Abstract The July–August 2001 eruption of Mt. Etna stimulated widespread public and media
interest, caused significant damage to tourist facilities, and for several days threatened the …

A global equatorial set of layered deposits on Mars has been reexamined with Mars Global
Surveyor data. The stratigraphy, morphology, and erosional characteristics of units …

Monogenetic basaltic volcanism is characterised by a complex array of behaviours in the
spatial distribution of magma output and also temporal variability in magma flux and eruptive …

The Etna 122 BC basaltic eruption had two Plinian phases, each preceded and followed by
weak phreatic and phreatomagmatic activity. This study infers changing eruption dynamics …