Results 51 to 60 of about 4,124 (186)
Tephra layers in marine sediments are widely used to correlate and date paleoclimate and paleoceanography records, and to determine spatiotemporal changes in magmatic evolution and eruption frequency.
Iona M. McIntosh +5 more
doaj +1 more source
Rainfall‐induced landslides involving on Auckland Volcanic Field scoria cones are highly unusual, compared with widespread landsliding in the surrounding Auckland clay‐rich residual soils. Indeed, while Auckland can suffer from thousands of rainfall‐induced shallow landslides from severe storms at subdecadal timescales, these are usually limited to ...
Beatrice Bertelli, Martin Brook
wiley +1 more source
Identification of unambiguous signals of volcanic unrest is crucial in hazard assessment. Processes leading to phreatic and phreatomagmatic eruptions remain poorly understood, inhibiting effective eruption forecasting.
J. M. deMoor +10 more
doaj +1 more source
The 1963–1967 shallow-to-emergent eruption in Iceland’s Vestmannaeyjar earned a place in the history of volcanology by creating the island of Surtsey while under close observation of volcanologist Sigurdur Thorarinsson (Sigurður Þórarinsson in Icelandic).
Andrea Verolino +4 more
doaj +1 more source
Phreatomagmatic deposits and stratigraphic reconstruction at Debunscha Maar (Mt Cameroon volcano) [PDF]
The Debunscha Maar (DM) is located on the southwest flank of Mount Cameroon, an active stratovolcano on the Cameroon volcanic line (CVL). Here, we present the physical characteristics of the pyroclastic deposits at DM with the aim of deciphering tephra ...
Devey, Colin W. +2 more
core +1 more source
Abstract Two sediment cores were collected from a submarine sediment wave field on the flank of Macauley volcano. Combined with seismic reflection surveys and numerical modeling, we present an integrated model of the formation of large‐scale, eruption‐fed, submarine sediment waves. The sediment waves are large (>100 m high, 1.5 km wide, tens of km long)
Shannon E. Frey +3 more
wiley +1 more source
A basaltic phreatomagmatic eruptive centre at Acacia Bay, Taupo Volcanic Centre [PDF]
Abstract Basaltic tuffs seen in shoreline exposures at Acacia Bay township on Lake Taupo are interpreted as the heavily eroded relicts of a phreatomagmatic tuff ring and its associated outlying deposits. The tuff ring consists largely of ejected pumiceous lake sediments, which incorporate 15–20 volume % of juvenile basalt whose residual heat has caused
C. J. N. Wilson, I. E. M. Smith
openaire +1 more source
Abstract Grande Comore, the westernmost island within the Madagascar Comoros Volcanic (MCV) chain, hosts two juxtaposed basaltic volcanoes, Karthala and La Grille, with contrasting lava geochemical signatures and eruption frequencies. Their formation and dynamics have been explained either by a mantle plume or, more recently, as part of a ...
François J. P. Lötter +6 more
wiley +1 more source
The Kuchino-Erabujima Volcano has experienced multiple phreatomagmatic eruptions since 2015. Monitoring ground deformation at active volcanoes is essential for understanding magma supply systems and predicting volcanic activity.
Misa Ichimura +4 more
doaj +1 more source
The phreatomagmatic eruption at Aso volcano on October 8, 2016, released PDC and fallout up to 320 km from the vent, providing an opportunity to study the dispersal and sedimentation of tephra bearing wet and dry aggregates.
Tomohiro Tsuji +2 more
doaj +1 more source

