The 25 September 2007 eruption of Mount Ruapehu, New Zealand: Directed ballistics, surtseyan jets, and ice-slurry lahars

2010 ◽  
Vol 191 (1-2) ◽  
pp. 1-14 ◽  
Author(s):  
G. Kilgour ◽  
V. Manville ◽  
F. Della Pasqua ◽  
A. Graettinger ◽  
K.A. Hodgson ◽  
...  
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2011 ◽  
Vol 73 (3) ◽  
pp. 243-250 ◽  
Author(s):  
G. Turner ◽  
M. Ingham ◽  
H. Bibby ◽  
H. Keys

2009 ◽  
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pp. 887-904 ◽  
Author(s):  
M. R. Ingham ◽  
H. M. Bibby ◽  
W. Heise ◽  
K. A. Jones ◽  
P. Cairns ◽  
...  

1990 ◽  
Vol 105 (6) ◽  
pp. 650-661 ◽  
Author(s):  
Ian J. Graham ◽  
Peter Blattner ◽  
Malcolm T. McCulloch

2014 ◽  
Vol 127 (1-2) ◽  
pp. 266-280 ◽  
Author(s):  
M. Tost ◽  
S.J. Cronin ◽  
J.N. Procter ◽  
I.E.M. Smith ◽  
V.E. Neall ◽  
...  

1958 ◽  
Vol 3 (24) ◽  
pp. 312-315
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L. O. Krenek
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AbstractDue to the abnormally warm summers of 1955 and 1956 the glaciers of Mount Ruapehu deteriorated to such an extent that the ash layer of the eruption of 1945 was exposed everywhere. This caused a development of ice cones similar to those occurring in Iceland. Various factors, especially heavy crevassing, which took place at the same time, are responsible for the different ways of development of dirt cones on Ruapehu.


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