Zobrazeno 1 - 10
of 60
pro vyhledávání: '"Vincent E. Neall"'
Autor:
Ian E. M. Smith, Jon N. Procter, Manuela Tost, Vincent E. Neall, Shane J. Cronin, Richard C. Price
Publikováno v:
Geological Society of America Bulletin. 127:266-280
Debris avalanches caused by the collapse of volcanic flanks pose a great risk to inhabited areas and may permanently change the surrounding landscape and its drainage systems. In this research, we explored the interplay between a debris avalanche and
Publikováno v:
New Zealand Journal of Geology and Geophysics. 57:369-377
The Maitahi Formation is a regionally extensive, lithologically and texturally distinctive Middle Pleistocene volcanogenic-sedimentary deposit in western Taranaki, New Zealand that warrants recognition as a formal lithostratigraphic unit. Maitahi str
Publikováno v:
Geomorphology. 136:15-30
Volcanic domes may be emplaced rapidly and with few hazardous consequences, even at the summit of large stratovolcanoes. In this study the most recent activity of Mt. Taranaki in New Zealand is shown to have been a passive effusion of a c. 5.9 millio
Publikováno v:
Quaternary International. 246:352-363
Holocene volcanism at the Tongariro Volcanic Centre (TgVC), at the south-western end of the Taupo Volcanic Zone (TVZ), New Zealand, involved eruptions from at least three centres and was dominated by numerous “small” eruptions of VEI 1–4. These
Autor:
Jonathan Procter, Rébecca Keigler, Katherine A. Hodgson, Shane J. Cronin, Jean-Claude Thouret, Jérôme A. Lecointre, Vincent E. Neall
Publikováno v:
Geomorphology
Geomorphology, Elsevier, 2011, 133, pp.57-79. ⟨10.1016/j.geomorph.2011.06.019⟩
Geomorphology, 2011, 133, pp.57-79. ⟨10.1016/j.geomorph.2011.06.019⟩
Geomorphology, Elsevier, 2011, 133, pp.57-79. ⟨10.1016/j.geomorph.2011.06.019⟩
Geomorphology, 2011, 133, pp.57-79. ⟨10.1016/j.geomorph.2011.06.019⟩
In the North Island of New Zealand, the andesitic Tongariro Volcanic Centre encompasses the Tongariro complex, the Mt. Ngauruhoe cone, and the country's largest stratovolcano, Mt. Ruapehu. This volcano is surrounded by an equally large volume of Late
Autor:
David R. Gaylord, Vincent E. Neall
Publikováno v:
Geological Society of America Bulletin. 124:181-199
The Maitahi Formation is a large-volume (>7.5 km 3 ) debris-avalanche deposit that resulted from a mid-Pleistocene (ca. 0.24–0.21 Ma) collapse of Pouakai Volcano, Taranaki Peninsula, New Zealand. It is best exposed at intermediate distances (12–1
Publikováno v:
International Journal of Earth Sciences. 100:1937-1966
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 exposures show a range of volcaniclastic lithofa
Publikováno v:
Bulletin of Volcanology. 73:27-37
New studies of the deposits from the latest caldera-forming eruption (the “Dk” event) at Dakataua Volcano, New Britain Island, Papua New Guinea, help identify an intense space-time concentration of large-scale volcanism during the 7th century AD
Publikováno v:
Journal of Quaternary Science. 25:1169-1178
Tephras provide one of the most reliable methods of time control and synchronisation within Quaternary sequences. We report on the identification of two widespread rhyolitic tephras – the Kawakawa and Rangitawa tephras – preserved in extensive pe
Autor:
Shane J. Cronin, Michael F. Sheridan, Harry Keys, Ian C. Fuller, Vincent E. Neall, Jonathan Procter
Publikováno v:
Geomorphology. 116:162-174
Rapid changes in small areas at the apex of alluvial fans may have devastating consequences by directing downstream flood or lahar impacts into catchments of widely varying population or infrastructure vulnerability. During a series of lahars in 1995