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

ABSTRACT Tephra deposits in Aotearoa New Zealand (ANZ) have been studied for> 180
years. The now-global discipline of tephrochronology, which has some developmental roots …

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 …

Abstract “Volcanic field” is a term commonly used to loosely describe a group of volcanoes.
Often, it is implicitly assumed that the volcanoes on a volcanic field are small, monogenetic …

Layers of far-travelled volcanic ash (tephra) from explosive volcanic eruptions provide
stratigraphic and numerical dating horizons in sedimentary and volcanic sequences. Such …

Although analyses of tephra-derived glass shards have been undertaken in New Zealand
for nearly four decades (pioneered by Paul Froggatt), our study is the first to systematically …

Detailed volcano-stratigraphy and 40 Ar/39 Ar dating are used for the first time to reconstruct
the eruptive evolution of the Alchichica maar and to contribute to the understanding of maar …

Following resolution of a long-standing debate over the timing of the initial settlement of New
Zealand from Polynesia (late 13th century), a prevailing paradigm has developed that …

Linking tephras back to their source centre (s) in volcanic fields is crucial not only to
reconstruct the eruptive history of the volcanic field but also to understand tephra dispersal …

Kissomlyó is a small-volume Pliocene alkaline basaltic eruptive centre located in the
monogenetic Little Hungarian Plain Volcanic Field (western Pannonian Basin). It consists of …