Volcanism, structure and petrology of the Whiritoa – Whangamata coastal section, Coromandel volcanic zone, New Zealand: facies model evidence for the Tunaiti calderaJournal Paper
Briggs, R.M.; Fulton, B.W., 1990. Expand
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Wave climate and sediment transport within Tauranga Harbour, in the vicinity of of Pilot BayThesis
de Lange, W.P., 1988, unpublished DPhil thesis, University of Waikato, New Zealand. Expand
Wave process and beach responses on a coarse gravel deltaThesis
Stephen, W.J.M., 1974, Unpublished PhD thesis, University of Canterbury, New Zealand. Expand
Wave spectra for shallow meso-tidal estuarine lagoon: Bay of Plenty, New ZealandJournal Paper
de Lange, W.P., 1990, Journal of Coastal Research. Expand
Web site characteristics, dispersal and species status of New Zealand’s katipō spiders, Latrodectus katipo and L. atritusThesis
Griffiths, J.W., 2001. Expand
Westport harbour
Furkert, F.W., 1947, Transactions of the Royal Society of New Zealand. Expand
When seaweeds go bad: an overview of outbreaks of nuisance quantities of marine macroalgae in New Zealand
Nelson, W.A; Neill, K.F; D'Archino, R., 2015, New Zealand journal of marine and freshwater research. Expand
When the earth blisters: Exploring reccurent liquefaction features in the coastal system of Christchurch, New ZealandJournal Paper
Bucci, M.G.; Almond, P.; Villamor, P.; Ries, W.; Smith, C.; Tuttle, M., 2017, Terra Nova. Expand
Why does Tauranga Harbour exist?Conference Paper
de Lange, W.P.; Fox, B.R.S.; Moon, V.G., 2017, Presented at the New Zealand Coastal Society – Te Hunga Takutai o Aotearoa Annual Conference. Expand
Wind and sand: the dune partners
Judd, W., New Zealand Geographic. Expand