The interplay between environmental and magmatic conditions in eruption style transitions within a fissure-aligned monogenetic volcanic system of Auckland, New …
Recent conceptual geological frameworks of continental monogenetic volcanism highlight
that the small magma volume eruptions, resulting volcanic geology and edifice architecture …
that the small magma volume eruptions, resulting volcanic geology and edifice architecture …
Influences on the variability of eruption sequences and style transitions in the Auckland Volcanic Field, New Zealand
Monogenetic basaltic volcanism is characterised by a complex array of eruptive behaviours,
reflecting spatial and temporal variability of the magmatic properties (eg composition …
reflecting spatial and temporal variability of the magmatic properties (eg composition …
Shallow-seated controls on styles of explosive basaltic volcanism: a case study from New Zealand
The pyroclastic deposits of many basaltic volcanic centres show abrupt transitions between
contrasting eruptive styles, eg, Hawaiian versus Strombolian, ordry'magmatic versuswet' …
contrasting eruptive styles, eg, Hawaiian versus Strombolian, ordry'magmatic versuswet' …
[HTML][HTML] The role of phreatomagmatism in the formation of complex monogenetic volcanic systems in a low-lying coastal plain
Monogenetic volcanoes are characterised worldwide by a single eruptive phase that is short-
lived, with small eruptive volumes that produce a wide range and complexity of landforms …
lived, with small eruptive volumes that produce a wide range and complexity of landforms …
Transition from effusive to explosive phases in andesite eruptions—a case-study from the AD1655 eruption of Mt. Taranaki, New Zealand
The extrusion of viscous andesite lava forming domes can terminate in explosive activity. To
understand the driving forces behind this behaviour, a study of an AD1655 eruption episode …
understand the driving forces behind this behaviour, a study of an AD1655 eruption episode …
Relating magma composition to eruption variability at andesitic volcanoes: a case study from Mount Taranaki, New Zealand
MB Turner, SJ Cronin, MS Bebbington… - …, 2011 - pubs.geoscienceworld.org
Acquiring accurate eruption records and understanding the volcanic processes behind
eruption periodicity are important in the development of realistic hazard assessments and …
eruption periodicity are important in the development of realistic hazard assessments and …
Understanding the evolution of a small-volume silicic fissure eruption: Puketerata Volcanic Complex, Taupo Volcanic Zone, New Zealand
Abstract The Puketerata Volcanic Complex formed as a result of a series of rhyolitic
eruptions along a 2.5 km long NE-trending eruptive fissure at the southern margin of Maroa …
eruptions along a 2.5 km long NE-trending eruptive fissure at the southern margin of Maroa …
Shallow subaqueous to emergent intra-caldera silicic volcanism of the Motuoapa Peninsula, Taupo Volcanic Zone, New Zealand–new constraints from geologic …
Motuoapa Peninsula, located in the southeast of the Taupo Volcanic Centre, New Zealand,
is dominated by a silicic pyroclastic cone and overlaying lavas. The pyroclastic succession …
is dominated by a silicic pyroclastic cone and overlaying lavas. The pyroclastic succession …
Phreatomagmatic and water-influenced Strombolian eruptions of a small-volume parasitic cone complex on the southern ringplain of Mt. Ruapehu, New Zealand …
Abstract The Ohakune Volcanic Complex is a late Pleistocene tuff ring–scoria/spatter cone
complex located south of Ruapehu volcano. This small-volume volcano consists of an outer …
complex located south of Ruapehu volcano. This small-volume volcano consists of an outer …
Phreatomagmatic eruptions through unconsolidated coastal plain sequences, Maungataketake, Auckland volcanic field (New Zealand)
Maungataketake is a monogenetic basaltic volcano formed at~ 85–89 ka in the southern
part of the Auckland Volcanic Field (AVF), New Zealand. It comprises a basal 1100-m …
part of the Auckland Volcanic Field (AVF), New Zealand. It comprises a basal 1100-m …