By Tony Duff
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Geological history of the north-eastern ring plain of Ruapehu volcano, New Zealand. Quaternary International, 34-36, 21-28. DE LANGE, W. P. & HULL, A. G. 1994. Tsunami hazard for the Auckland region - a report for the Auckland Regional Council. Department of Earth Sciences, University of Waikato & Institute of Geological and Nuclear Sciences Limited. DIBBLE, R. R & NEALL, V. E. 1984. Volcanic hazards in New Zealand. In: SPEDEN, 1. G. & CROZIER, M. J. (eds) Natural Hazards in Nee, Zealand. New Zealand National Commission for UNESCO, Wellington, 332-374 - - , NAIRN, I.
Although urban development across the Auckland Isthmus (Fig. 2) has destroyed or obscured much of the Quaternary geology, much valuable work can still be undertaken there to assist with assessment of the tephra hazard for Auckland from CNI eruptions. Three types of investigation could be pursued profitably: 1. extrapolation from tephra isopachs determined for localities intermediate between Auckland and the CNI volcanoes; 2. review of CNI tephras previously reported in the Auckland and Northland areas, coupled with field observations at new sites; 3.
MuNRo, A. J. 1994. Holocene evolution and palaeolimnology of a barrier spit, northwestern Matakana Island, Bay of Plenty, New Zealand. MSc thesis, Library, University of Waikato, Hamilton, New Zealand. - 26 T. M. GILES ET AL. NEWNHAM, R. M. ALLOWAY,B. V. A. in press. The East Interglacial/Glacial cycle in Taranaki, western North Island, New Zealand: regional synthesis and new sites. Palynology. , DE LANGE, P. J. & LOWE, D. J. 1995a. Holocene vegetation, climate and history of a raised bog complex, northern New Zealand, based on palynology, plant macrofossils and tephrochronology.
A Very Condensed Daily Practice of White Tara by Tony Duff