Skip to main content

and
  1. Article

    Open Access

    A model volcanic fissure with adjustable geometry and wall temperature

    Fissure eruptions initiate with magma ascending and spreading through cracks in the ground that can extend for kilometres at the surface. Eruptions eventually localise to form one or a few persistent conduits ...

    R. P. Cole, J. D. L. White, R. J. M. Baxter, M. H. Bowman in Bulletin of Volcanology (2023)

  2. Article

    Open Access

    Evaluation of short-term probabilistic eruption forecasting at Whakaari, New Zealand

    Phreatic explosions at volcanoes are difficult to forecast but can be locally devastating, as illustrated by the deadly 2019 Whakaari (New Zealand) eruption. Quantifying eruption likelihood is essential for ri...

    D. E. Dempsey, A. W. Kempa-Liehr, A. Ardid, A. Li, S. Orenia in Bulletin of Volcanology (2022)

  3. No Access

    Article

    Spatiotemporal variations in eruption style and magnitude at Yasur volcano, Vanuatu: part 2—extending Strombolian eruption classifications

    In this companion study to Simons et al. (Bull Volcanol 82, 2020a), we examine Strombolian style explosive activity at Yasur (Vanuatu) over 11 weeks via seismic, thermal-infrared and visual observations. In part ...

    Benjamin Clifford Simons, S. J. Cronin, J. D. Eccles in Bulletin of Volcanology (2020)

  4. No Access

    Article

    Spatiotemporal variations in eruption style, magnitude and vent morphology at Yasur volcano, Vanuatu: insights into the conduit system

    Using visual, seismic, SO2-gas and thermal infrared data collected over 3 months, we observed systematic variations in the steady-state Strombolian-style activity of Yasur volcano. Observations reveal insights in...

    B. C. Simons, S. J. Cronin, J. D. Eccles, M. S. Bebbington in Bulletin of Volcanology (2020)

  5. No Access

    Article

    Computable general equilibrium modelling of economic impacts from volcanic event scenarios at regional and national scale, Mt. Taranaki, New Zealand

    The economic impacts of volcanism extend well beyond the direct costs of loss of life and asset damage. This paper presents one of the first attempts to assess the economic consequences of disruption associate...

    G. W. McDonald, S. J. Cronin, J.-H. Kim, N. J. Smith in Bulletin of Volcanology (2017)

  6. No Access

    Article

    New insights into the evolution of the magmatic system of a composite andesite volcano revealed by clasts from distal mass-flow deposits: Ruapehu volcano, New Zealand

    Stratovolcanoes characteristically build large composite edifices over long periods with stacked lavas intercalated with pyroclastic deposits. In most cases, only the most recent volcanic products are exposed ...

    M. Tost, R. C. Price, S. J. Cronin, I. E. M. Smith in Bulletin of Volcanology (2016)

  7. No Access

    Article

    Transport and deposition processes of the hydrothermal blast of the 6 August 2012 Te Maari eruption, Mt. Tongariro

    The 2012 eruption of Tongariro volcano (New Zealand) produced highly mobile, low-temperature, blast-derived pyroclastic density currents after partial collapse of the western flank of the Upper Te Maari crater...

    E. C. P. Breard, G. Lube, S. J. Cronin, G. A. Valentine in Bulletin of Volcanology (2015)

  8. No Access

    Article

    Linking distal volcaniclastic sedimentation and stratigraphy with the development of Ruapehu volcano, New Zealand

    Long-lived stratovolcanoes are often characterized by cycles that include pulses of explosive and effusive eruptive activity, periodic flank collapses, and long periods of eruptive quiescence. Reconstructing t...

    M. Tost, S. J. Cronin in Bulletin of Volcanology (2015)

  9. No Access

    Article

    The Al-Du’aythah volcanic cones, Al-Madinah City: implications for volcanic hazards in northern Harrat Rahat, Kingdom of Saudi Arabia

    The basaltic Al-Du’aythah volcanic cones lie in the northern part of the extensive lava field of Harrat Rahat, and only 13 km from the centre of Al-Madinah City, in the Kingdom of Saudi Arabia. Historical reco...

    H. Murcia, K. Németh, N. N. El-Masry, J. M. Lindsay in Bulletin of Volcanology (2015)

  10. Article

    Erratum to: Identifying multiple eruption phases from a compound tephra blanket: an example of the AD1256 Al-Madinah eruption, Saudi Arabia

    E. Kawabata, S. J. Cronin, M. S. Bebbington, M. R. H. Moufti in Bulletin of Volcanology (2015)

  11. No Access

    Article

    Identifying multiple eruption phases from a compound tephra blanket: an example of the AD1256 Al-Madinah eruption, Saudi Arabia

    Complex eruption episodes commonly produce several phases of tephra fall and/or concurrent falls from multiple vents. Phases of eruption are challenging to reconstruct from the geological record, especially wh...

    E. Kawabata, S. J. Cronin, M. S. Bebbington, M. R. H. Moufti in Bulletin of Volcanology (2015)

  12. No Access

    Article

    Transport and emplacement mechanisms of channelised long-runout debris avalanches, Ruapehu volcano, New Zealand

    The steep flanks of composite volcanoes are prone to collapse, producing debris avalanches that completely reshape the landscape. This study describes new insights into the runout of large debris avalanches en...

    M. Tost, S. J. Cronin, J. N. Procter in Bulletin of Volcanology (2014)

  13. No Access

    Article

    Post 19 ka B.P. eruptive history of Ulleung Island, Korea, inferred from an intra-caldera pyroclastic sequence

    Ulleung Island is a Quaternary volcanic island located in the mid-western part of the East Sea (Sea of Japan) back-arc basin, which has erupted from the Pliocene until the late Holocene. This study focuses on ...

    G. B. Kim, S. J. Cronin, W. S. Yoon, Y. K. Sohn in Bulletin of Volcanology (2014)

  14. No Access

    Article

    A medial to distal volcaniclastic record of an andesite stratovolcano: detailed stratigraphy of the ring-plain succession of south-west Taranaki, New Zealand

    The >25 ka volcaniclastic ring-plain succession in south-west Taranaki has been remapped to establish a much more detailed understanding of the older stratigraphic record of Mt. Taranaki. Coastal cliff exposur...

    A. V. Zernack, S. J. Cronin, V. E. Neall in International Journal of Earth Sciences (2011)

  15. No Access

    Article

    Mafic Plinian volcanism and ignimbrite emplacement at Tofua volcano, Tonga

    Tofua Island is the largest emergent mafic volcano within the Tofua arc, Tonga, southwest Pacific. The volcano is dominated by a distinctive caldera averaging 4 km in diameter, containing a freshwater lake in ...

    J. T. Caulfield, S. J. Cronin, S. P. Turner, L. B. Cooper in Bulletin of Volcanology (2011)

  16. No Access

    Article

    Ash storms: impacts of wind-remobilised volcanic ash on rural communities and agriculture following the 1991 Hudson eruption, southern Patagonia, Chile

    Tephra fall from the August 1991 eruption of Volcán Hudson affected some 100,000 km2 of Patagonia and was almost immediately reworked by strong winds, creating billowing clouds of remobilised ash, or ‘ash storms’...

    T. M. Wilson, J. W. Cole, C. Stewart, S. J. Cronin in Bulletin of Volcanology (2011)

  17. No Access

    Article

    The coalescence and organization of lahars at Semeru volcano, Indonesia

    We present multi-parameter geophysical measurements of rainfall-induced lahars at Semeru Volcano, East Java, using two observation sites 510 m apart, 11.5 km from the summit. Our study site in the Curah Lengko...

    E. E. Doyle, S. J. Cronin, S. E. Cole, J.-C. Thouret in Bulletin of Volcanology (2010)

  18. No Access

    Article

    Agronomic impact of tephra fallout from the 1995 and 1996 Ruapehu Volcano eruptions, New Zealand

     Eruptions from Ruapehu Volcano on 11 and 14 October 1995 and 17 June 1996 distributed at least 36×106 m3 of sulphur(S)-rich tephra over the central and eastern North Island of New Zealand. The tephras added betw...

    S. J. Cronin, M. J. Hedley, V. E. Neall, R. G. Smith in Environmental Geology (1998)

  19. No Access

    Article

    Sourcing and identifying andesitic tephras using major oxide titanomagnetite and hornblende chemistry, Egmont volcano and Tongariro Volcanic Centre, New Zealand

     Canonical discriminant function analysis was employed to discriminate between electron microprobe-determined titanomagnetite and hornblende analyses from Egmont volcano and Tongariro Volcanic Centre. Data set...

    S. J. Cronin, R. C. Wallace, V. E. Neall in Bulletin of Volcanology (1996)