Abstract
The Auckland Volcanic Field (AVF) comprises at least 52 monogenetic eruption centres dispersed over ∼360 km2. Eruptions have occurred sporadically since 250 ka, predominantly when glacio-eustatic sea levels were lower than today. Now that around 35 % of the field is covered by shallow water (up to 30 m depth), any eruption occurring in the present or near future within this area may display Surtseyan dynamics. The North Head tuff cone evidences eruptive dynamics caused by magma interaction with seawater. The first stages of the eruption comprise a phreatomagmatic phase that built a 48-m-high tuff cone. North Head tuff deposits contain few lithic fragments (<10 vol%) and are characterized by deposits from collapsing tephra jets and fall from relatively wet tephra columns. The conditions needed for this eruption existed between 128 and 116 ka, when the sea level in the Auckland area was at least 10–12 m above the pre-eruptive surface. The hazards associated with this type of eruption pose a risk to the densely populated coastal residential zones and the activities of one of the busiest harbours in New Zealand.
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Agustín-Flores J, Németh K, Cronin S, Lindsay J, Kereszturi G, Brand B, Smith IEM (2014) Phreatomagmatic eruptions through unconsolidated coastal plain sequences, Maungataketake, Auckland Volcanic Field (New Zealand). J Volcanol Geotherm Res 180:203–224
Allen SR, Smith IEM (1994) Eruption styles and volcanic hazard in the Auckland Volcanic Field, New Zealand. Geosci Rep Shizuoka Univ 20:5–14
Allen SR, Bryner VF, Smith IEM, Balance PF (1996) Facies analysis of pyroclast deposits within basaltic tuff-rings of the Auckland volcanic field, New Zealand. N Z J Geol Geophys 39:309–327
Ballance PF (1974) An inter-arc flysch basin in northern New Zealand: Waitemata Group (Upper Oligocene to Lower Miocene). J Geol 82:439–471
Beavan RJ, Litchfield NJ (2012) Vertical movement around New Zealand coastline: implications for sea-level rise. GNS Science Report 2012/29, September 2012, p 41
Bebbington MS, Cronin SJ (2011) Spatio-temporal hazard estimation in the Auckland Volcanic Field, New Zealand, with a new event-order model. Bull Volcanol 73:55–72
Belousov A, Belousova M (2001) Eruptive processes, effects and deposits of the 1996 and the ancient basaltic phreatomagmatic eruptions in Karymskoye lake, Kamchatcka, Russia. In: White JDL, Riggs, NR (eds), Volcaniclastic sedimentation in lacustrine settings, Blackwell, Oxford, p 35–60
Brand BD, Clarke AB (2009) The architecture, eruptive history, and evolution of the Table Rock Complex, Oregon: from a Surtseyan to an energetic maar eruption. J Volcanol Geotherm Res 180:203–224
Cole PD, Guest JE, Duncan AM, Pacheco JM (2001) Capelinhos 1957–1958, Faial, Azores: deposits formed by an emergent surtseyan eruption. Bull Volcanol 63:204–220
Crowcroft G, Smaill A (2001) Auckland. In: Rosen MR, White PA (eds) Groundwaters of New Zealand. New Zealand Hydrological Society Inc, Wellington, New Zealand, pp 303–313
Fisher RV, Schmincke H-U (1984) Pyroclastic rocks. Springer-Verlag, Berlin, p 472
Folk RL, Ward WC (1957) Brazos river bar: a study in the significance of grain size parameters. J Sed Petrol 27:3–26
Hannah J, Bell R, Paulik R (2011) Auckland: a case study in the regional assessment of long-term sea level change. FIG Working Week 2011, Bridging the gap between cultures, Marrakech, Morocco, 18–22 May 2011, p 16
Hayward BW (1979) Eruptive history of the early to mid Miocene Waitakere Volcanic arc and paleogeography of the Waitemata Basin, northern New Zealand. J R Soc N Z 9:297–320
Hayward BW (1993) The tempestuous 10 million year life of a double arc and intra-arc basin—New Zealand’s Northland Basin in the early Miocene. In: Balance PF (ed) Sedimentary basins of the world, vol 2, South Pacific sedimentary basis. Elsevier, Amsterdam, pp 113–142
Hayward BW, Murdoch G, Maitland G (2011) Volcanoes of Auckland, the essential guide. Auckland University Press, New Zealand, p 234
Houghton BF, Wilson CJN (1989) A vesicularity index for pyroclastic deposits. Bull Volcanol 51:451–462
Houghton BF, Wilson CJN, Smith IEM (1999) Shallow-seated controls on styles of explosive basaltic volcanism: a case study from New Zealand. J Volcanol Geotherm Res 91:97–120
Inman DL (1952) Measures for describing the size distribution of sediments. J Sed Petrol 22:125–145
Jakobsson SP (1972) On the consolidation and palagonitization of the tephra of the Surtsey volcanic Island, Iceland. Surtsey Res Progr Rep 6:121–128
Jakobsson SP (1978) Environmental factors controlling the palagonitization of the Surtsey tephra, Iceland. Bull Geol Soc Denmark 27:91–105
Kereszturi G, Németh K, Cronin JS, Agustin-Flores J, Smith IEM, Lindsay J (2013) A model for calculating eruptive volumes for monogenetic volcanoes—implication for the Quaternary Auckland Volcanic Field, New Zealand. J Volcanol Geotherm Res 266:16–33
Kereszturi G, Németh K, Cronin JS, Procter J, Agustin-Flores J (2014) Influences in the variability of eruption sequences and style transitions in the Auckland Volcanic Field. J Volcanol Geotherm Res 286:101–115
Kokelaar P (1983) The mechanism of Surtseyan volcanism. J Geol Soc Lond 140:939–944
Kokelaar P (1986) Magma-water interactions in subaqueous and emergent basaltic volcanism. Bull Volcanol 48:275–289
Lindsay JM, Marzocchi W, Jolly G, Constantinescu R, Selva J, Sandri L (2010) Towards real-time eruption forecasting in the Auckland Volcanic Field: application of BET_EF during the New Zealand National Disaster Exercise ‘Ruaumoko’. Bull Volcanol 72:185–204
Lorenz V (1970) Some aspects of the eruption mechanism of the Big Hole maar, central Oregon. Bull Geol Soc Am 81:1823–1830
Lorenz V (1974a) Studies of Surtsey tephra deposits. Surtsey Res Progr Rep 7:72–79
Lorenz V (1974b) Vesiculated tuffs and associated features. Sedimentology 21:273–291
Machado F (1958) Acitividade Vulcanica da Ilha do Faial (1957–1958) Atlantida vII: 225–236
Martin U, Németh K (2005) Eruptive and depositional history of a Pliocene tuff ring that developed in a fluvio-lacustrine basin: Kissomlyó volcano (western Hungary). J Volcanol Geotherm Res 147:342–356
Mastin LG (2007) Generation of fine hydromagmatic ash by growth and disintegration of glassy rinds. J Geophys Res 112:B02203. doi:10.1029/2005JB003883
Mastin LG, Spieler O, Downey WS (2009) An experimental study of hydromagmatic fragmentation through energetic non-explosive magma-water mixing. J Volcanol Geotherm Res 180:161–170
Mattsson HB (2010) Textural variation in juvenile pyroclasts from an emergent, Surtseyan-type, volcanic eruption: the Capelas tuff cone: São Miguel (Azores). J Volcanol Geotherm Res 189:81–91
Molloy C, Shane P, Augustinus P (2009) Eruption recurrence rates in a basaltic volcanic field based on tephra layers in maar sediments: implications for hazards in the Auckland volcanic field. Geol Soc Am Bull 121:1666–1677
Murtagh RM, White JDL (2013) Pyroclastic characteristics of a subaqueous to emergent Surtseyan eruption, Black Point volcano, California. J Volcanol Geotherm Res 267:75–91
Németh K, Cronin SJ, Charley D, Harrison M, Garae E (2006) Exploding lakes in Vanuatu—“Surtseyan-style” eruptions witnessed on Ambae Island. Episodes 29:87–92
Németh K, Cronin SJ, Smith IEM, Agustín-Flores J (2012) Amplified hazard of small-volume monogenetic eruptions due to environmental controls, Orakei Basin, Auckland Volcanic Field, New Zealand. Bull Volcanol 74:2121–2137
Pillans B (1983) Upper Quaternary marine terrace chronology and deformation, South Taranaki, New Zealand. Geology 11:292–297
Raza A, Brown RW, Ballance PF, Kamp PJJ (1999) Thermal history of the early Waitemata Basin and adjacent Waipapa Group, North Island, New Zealand. N Z J Geol Geophys 42:469–488
Sandri L, Jolly G, Lindsay J, Howe T, Marzocchi W (2012) Combining long- and short-term PVHA with cost-benefit analysis to support decision making in a volcanic crisis from the Auckland Volcanic Field, New Zealand. Bull Volcanol 74:705–723
Searle EJ (1959) Pleistocene and recent studies of the Waitemata Harbour; Part 2—North Shore and Shoal Bay. N Z J Geol Gephys 2:95–107
Siddall M, Chappell J, Potter E-K (2006) Eustatic sea level during the past interglacials. In: Sirocko F, Litt T, Claussen M, Sanchez-Goni M-F (eds) The climate of past interglacials. Elsevier, Amsterdam, pp 75–92
Smith IEM, McGee LE, Lindsay JM (2009) Review of the petrology of the Auckland Volcanic Field. Institute of Earth Science and Engineering Report 1–2009.03. Auckland, New Zealand, p 36
Sohn YK, Chough SK (1989) Depositional processes of the Suwolbong tuff ring, Cheju Island (Korea). Sedimentology 36:837–855
Sohn YK, Chough SK (1992) The Ichulbong tuff cone, Cheju Island, South Korea; depositional processes and evolution of an emergent, Surtseyan-type tuff cone. Sedimentology 39:523–544
Sohn YK, Chough SK (1993) The Udo tuff cone, Cheju Island, South Korea: transformation of pyroclastic fall into debris flow and grain flow on a steep volcanic cone slope. Sedimentology 40:769–786
Sohn YK, Cronin SJ, Brena M, Smith IEM, Németh K, White JDL, Murtagh RM, Jeon YM, Kwon CW (2012) Ichulbong tuff cone, Jeju Island, Korea, revisited: a compound monogenetic volcano involving multiple magma pulses, shifting vents, and discrete eruptive phases. Geol Soc Am Bull 124:259–274
Solgevik H, Mattsson HB, Hermelin O (2007) Growth of an emergent tuff cone: fragmentation and depositional processes recorded in the Capelas tuff cone: São Miguel, Azores. J Volcanol Geotherm Res 159:246–266
Spörli KB, Eastwood VR (1997) Elliptical boundary of an intraplate volcanic field, Auckland, New Zealand. J Volcanol Geotherm Res 79:169–179
Spörli KB, Rowland JV (2007) Superposed deformation in turbidites and syn-sedimentary slides of the tectonically active Miocene Waitemata Basin, northern New Zealand. Basin Res 19:199–216
Stearns HT (1953) Causes of basaltic explosions. Bull Geol Soc Am 64:599
Thórarinsson S (1964) Surtsey, the new island in the North Atlantic. Almenna Bókafélagith, Reykjavík, pp 1–63
Valentine GA, Gregg TKP (2008) Continental basaltic volcanoes—processes and problems. J Volcanol Geotherm Res 177:857–873
Verwoerd WJ, Chevallier L (1987) Contrasting types of surtseyan tuff cones on Marion and Prince Edward islands, southwest Indian Ocean. Bull Volcanol 49:399–417
White JDL (1991) The depositional record of small, monogenetic volcanoes within terrestrial basins. In: Fisher, R.V., and Smith, G.A. (eds) Sedimentation in volcanic settings. SEPM (Soc Sediment Geol) Spec Publ 45: 155–171
White JDL (1996) Pre-emergent construction of a lacustrine basaltic volcano, Pahvant Butte, Utah (USA). Bull Volcanol 58:249–262
White JDL (2001) Eruption and reshaping of Pahvant Butte volcano in Pleistocene lake Bonneville. In: White JDL, Riggs, NR (eds), Volcaniclastic sedimentation in lacustrine settings. Blackwell, Oxford, p 61–80
White JDL, Houghton B (2000) Surtseyan and related phreatomagmatic eruptions. In: Sigurdsson H (ed) Encyclopedia of volcanoes. Academic, San Diego, pp 495–513
Wohletz KH (1983) Mechanisms of hydrovolcanic pyroclast formation: grain-size, scanning electron microscopy, and experimental studies. J Volcanol Geotherm Res 17:31–63
Wohletz KH, Sheridan MF (1983) Hydrovolcanic explosions II. Evolution of basaltic tuff rings and tuff cones. Am J Sci 283:385–413
Zimanowski B, Fröhlich G, Lorenz V (1991) Quantitative experiments on phreatomagmatic explosions. J Volcanol Geotherm Res 48:341–358
Acknowledgments
This research was supported by the New Zealand Natural Hazards Research Platform and by the Determining Volcanic Risk in Auckland (DEVORA) project. We also thank the School of Environment, Auckland University, for support, as well as Kate Arentsen for prompt and valuable organizational and administrative assistance; Anja Moebis, Doug Hopcroft and Ritchie Sims for technical assistance; and Jose Rivera and Marc Adamson for providing accommodation in Auckland. We highly appreciate the time and effort of journal reviewers Volker Lorenz and Alexander Belousov, associate Editor Pierre-Simon Ross and Executive Editor James White for their recommendations to improve this manuscript.
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Agustín-Flores, J., Németh, K., Cronin, S.J. et al. Construction of the North Head (Maungauika) tuff cone: a product of Surtseyan volcanism, rare in the Auckland Volcanic Field, New Zealand. Bull Volcanol 77, 11 (2015). https://doi.org/10.1007/s00445-014-0892-9
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DOI: https://doi.org/10.1007/s00445-014-0892-9