Journal articles: 'Taupo'

1

Druitt, Tim. "Turbulent times at Taupo." Nature 381, no. 6582 (June 1996): 476–77. http://dx.doi.org/10.1038/381476a0.

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2

Wilson, C. J. N. "Emplacement of Taupo ignimbrite." Nature 385, no. 6614 (January 1997): 306–7. http://dx.doi.org/10.1038/385306a0.

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3

Dade, W. Brian, and Herbert E. Huppert. "Emplacement of Taupo ignimbrite." Nature 385, no. 6614 (January 1997): 307–8. http://dx.doi.org/10.1038/385307a0.

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4

Stirling, M. W., and C. J. N. Wilson. "Development of a volcanic hazard model for New Zealand." Bulletin of the New Zealand Society for Earthquake Engineering 35, no. 4 (December 31, 2002): 266–77. http://dx.doi.org/10.5459/bnzsee.35.4.266-277.

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We commence development of a volcanic hazard model for New Zealand by applying the well- established methods of probabilistic seismic hazard analysis to volcanoes. As part of this work we use seismologically-based methods to develop eruption volume - frequency distributions for the Okataina and Taupo volcanoes of the central Taupo Volcanic Zone, New Zealand. Our procedure is to use the geologic and historical record of large eruptions (erupted magma volumes ≥ 0.01 cubic km for Taupo and ≥ 0.5 cubic km for Okataina) to construct eruption volume-frequency distributions for the two volcanoes. The two volcanoes show log-log distributions of decreasing frequency as a function of eruption volume, analogous to the shape of earthquake magnitude-frequency distributions constructed from seismicity catalogues. On the basis of these eruption volume-frequency distributions we estimate the maximum eruption volumes that Taupo and Okataina are capable of producing at probability levels of relevance to engineers and planners. We find that a maximum eruption volume of 0.1 cubic km is expected from Taupo with a 10% probability in 50 years, while Okataina may not produce a large eruption at this probability level. However, at the more conservative 2% probability in 50 years, both volcanoes are expected to produce large eruptions (0.5 cubic km for Okataina and 1 cubic km for Taupo). Our study therefore shows significant differences in eruption probabilities for volcanoes in the same physiographic region, and therefore highlights the importance of establishing unique eruption databases for all volcanoes in a hazard analysis.

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5

Hogg, Alan G. "When was the Taupo eruption?" Quaternary International 279-280 (November 2012): 204. http://dx.doi.org/10.1016/j.quaint.2012.08.381.

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Darby, Desmond J., Kathleen M. Hodgkinson, and Graeme H. Blick. "Geodetic measurement of deformation in the Taupo Volcanic Zone, New Zealand: The north Taupo network revisited." New Zealand Journal of Geology and Geophysics 43, no. 2 (June 2000): 157–70. http://dx.doi.org/10.1080/00288306.2000.9514878.

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7

Gilmour, Alex E., and Ron A. Heath. "Barotropic and baroclinic waves in Lake Taupo." New Zealand Journal of Marine and Freshwater Research 23, no. 2 (June 1989): 189–94. http://dx.doi.org/10.1080/00288330.1989.9516355.

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8

Sparks, R. J., W. H. Melhuish, J. W. A. McKee, John Ogden, J. G. Palmer, and B. P. J. Molloy. "14C Calibration in the Southern Hemisphere and the Date of the Last Taupo Eruption: Evidence from Tree-Ring Sequences." Radiocarbon 37, no. 2 (1995): 155–63. http://dx.doi.org/10.1017/s0033822200030599.

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Tree rings from a section of Prumnopitys taxifolia (matai) covering the period ad 1335–1745 have been radiocarbon dated and used to generate a 14C calibration curve for southern hemisphere wood. Comparison of this curve with calibration data for northern hemisphere wood does not show a systematic difference between 14C ages measured in the northern and southern hemispheres. A floating chronology covering 270 yr and terminating at the last Taupo (New Zealand) eruption, derived from a sequence of 10-yr samples of tree rings from Phyllocladus trichomanoides (celery pine, or tanekaha), is also consistent with the absence of a systematic north-south difference, and together with the matai data, fixes the date of the Taupo eruption at ad 232 ± 15.

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9

Couper, Steve, Jason Ewert, Ted Anderson, and Ian Wallace. "Natural Nutrient Removal Taupo District Land Disposal Scheme." Proceedings of the Water Environment Federation 2009, no. 12 (January 1, 2009): 3837–51. http://dx.doi.org/10.2175/193864709793953728.

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10

Gilmour, Alex E. "Seiche characteristics in Lake Taupo, New Zealand (Note)." New Zealand Journal of Marine and Freshwater Research 25, no. 2 (June 1991): 163–66. http://dx.doi.org/10.1080/00288330.1991.9516466.

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11

Edgar, N. B. "Land use in the Taupo catchment, New Zealand." New Zealand Journal of Marine and Freshwater Research 33, no. 3 (September 1999): 375–83. http://dx.doi.org/10.1080/00288330.1999.9516884.

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12

White, Brian R., and Isabelle Chambefort. "Geothermal development history of the Taupo Volcanic Zone." Geothermics 59 (January 2016): 148–67. http://dx.doi.org/10.1016/j.geothermics.2015.10.001.

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13

Betteridge, K., J. Crush, S. Ledgard, and M. S. Barton. "Nitrogen leaching implications of poor pasture persistence." NZGA: Research and Practice Series 15 (January 1, 2011): 79–84. http://dx.doi.org/10.33584/rps.15.2011.3220.

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Farmers have indicated that perennial pastures sown in the Lake Taupo catchment revert to low quality species within 8 to 10 years. These may be renewed with perennial pasture species following an autumn then spring cropping regime, or resown pasture-topasture by direct-drilling into glyphosate-sprayed turf or following full cultivation. Vegetation which is desiccated and/or ploughed-under before sowing will decay and release mineral nitrogen (N). The mineral N from these sources is available for newly sown plants but can also be leached. In a large, replicated, rotationally cattle-grazed trial near Lake Taupo, new pasture was established with the high sugar ryegrass (HSG) Aberdart in one treatment only by direct-drilling, following glyphosate application in late summer. Existing pasture remained in Control plots. Renovated pasture leached 63 kg nitrate-N ha-1 in the 8 months following establishment compared 8 kg nitrate-N ha-1 in Control (P

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14

Davy, Bryan. "Seismic Reflection Profiling of the Taupo Caldera, New Zealand." Exploration Geophysics 24, no. 3-4 (September 1993): 443–54. http://dx.doi.org/10.1071/eg993443.

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15

Barker, S. J., A. R. Van Eaton, L. G. Mastin, C. J. N. Wilson, M. A. Thompson, T. M. Wilson, C. Davis, and J. A. Renwick. "Modeling Ash Dispersal From Future Eruptions of Taupo Supervolcano." Geochemistry, Geophysics, Geosystems 20, no. 7 (July 2019): 3375–401. http://dx.doi.org/10.1029/2018gc008152.

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16

Bibby, H. M., G. F. Risk, T. G. Caldwell, W. Heise, and S. L. Bennie. "Resistivity structure of western Taupo Volcanic Zone, New Zealand." New Zealand Journal of Geology and Geophysics 51, no. 3 (September 2008): 231–44. http://dx.doi.org/10.1080/00288300809509862.

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17

Webb, Terry H., B. G. Ferris, and J. S. Harris. "The Lake Taupo, New Zealand, earthquake swarms of 1983." New Zealand Journal of Geology and Geophysics 29, no. 4 (October 1986): 377–89. http://dx.doi.org/10.1080/00288306.1986.10422160.

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18

McLellan, J. G., N. H. S. Oliver, B. E. Hobbs, and J. V. Rowland. "Convection stability in the Taupo Volcanic Zone, New Zealand." Journal of Geochemical Exploration 101, no. 1 (April 2009): 69. http://dx.doi.org/10.1016/j.gexplo.2008.12.002.

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19

Febrianto, Ridwan, Ian Thain, and Sadiq J. Zarrouk. "The geothermal heating system at Taupo Hospital, New Zealand." Geothermics 59 (January 2016): 347–56. http://dx.doi.org/10.1016/j.geothermics.2015.02.001.

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20

Moore, PR. "The Taupo obsidian source, central North Island, New Zealand." Journal of the Royal Society of New Zealand 41, no. 2 (May 17, 2011): 205–15. http://dx.doi.org/10.1080/03036758.2010.529919.

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21

Seebeck, Hannu, Andrew Nicol, Pilar Villamor, John Ristau, and Jarg Pettinga. "Structure and kinematics of the Taupo Rift, New Zealand." Tectonics 33, no. 6 (June 2014): 1178–99. http://dx.doi.org/10.1002/2014tc003569.

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22

Houghton, B. F., E. F. Lloyd, C. J. N. Wilson, and M. A. Lanphere. "K‐Ar ages from the Western Dome Belt and associated rhyolitic lavas in the Maroa‐Taupo area, Taupo Volcanic Zone, New Zealand." New Zealand Journal of Geology and Geophysics 34, no. 1 (March 1991): 99–101. http://dx.doi.org/10.1080/00288306.1991.9514444.

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23

Barkle, Greg, Tim Clough, and Roland Stenger. "Denitrification capacity in the vadose zone at three sites in the Lake Taupo catchment, New Zealand." Soil Research 45, no. 2 (2007): 91. http://dx.doi.org/10.1071/sr06141.

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Land use in the Lake Taupo catchment is under scrutiny, as early signs of deteriorating water quality in Lake Taupo have been observed. Although the fate of contaminants in soil and groundwater are comparatively well studied, the transformations in the lower vadose zone, i.e. the zone between the soil and the groundwater, are less well understood. The capacity for NO3-N removal via biological denitrification, based on utilising the resident C substrate, in the vadose zone of the Lake Taupo catchment is quantified in this work. Complete vadose zone profiles were sampled at 3 sites (Rangiatea, Waihora, and Kinloch), from the soil surface down to the watertable in approximately 0.5-m depth increments. Texture, allophane content, pH, and concentrations of extractable NO3-N, NH4-N, and dissolved organic carbon were determined. Incubations were undertaken to determine the denitrification capacity of the vadose zone materials amended with NO3-15N, but no added carbon substrate, and maintained under anaerobic conditions at 28°C. Gas samples were taken from the headspace after 48 h and analysed for N2 and N2O. In soil depths down to about 1.2 m, the denitrification capacity ranged from 0.03 to 9.18 kg N/ha.day, and below this depth it ranged from <0.01 to 0.09 kg N/ha.day. A palaeosol layer in the Waihora profile had an enhanced denitrification capacity compared with the other samples in deeper zones of the profiles. In the surface sampling, at least 99.9% of the gas recovered from the 15N applied was in the form of N2. In contrast, no N2 gas production could be detected in any sample from below the second sampling depth, with only N2O detected. Denitrification capacities of all vadose zone materials were low when compared with other studies. Thus, careful land management is required to avoid groundwater contamination by nitrate leaching from the root-zone of the pasture.

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24

Dunn, C. E., and A. B. Christie. "Tree ferns and tea trees in biogeochemical exploration for epithermal Au and Ag in New Zealand." Geochemistry: Exploration, Environment, Analysis 20, no. 3 (July 25, 2019): 299–314. http://dx.doi.org/10.1144/geochem2019-047.

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Biogeochemical orientation surveys were undertaken at low sulphidation epithermal Au–Ag occurrences in the Hauraki Goldfield–Coromandel Volcanic Zone and the Taupo Volcanic Zone, and at the Waiotapu active geothermal area in the Taupo Volcanic Zone. Several plant species were sampled, including the foliage of tree ferns and tea trees. The ferns – silver fern (ponga), rough tree fern (wheki) and black tree fern (mamaku) – were ubiquitous and were the easiest species to sample, although tea tree was the dominant genus at Waiotapu. At the Waiotapu geothermal area, significantly higher concentrations of Ag, Au, Sb, As, Cs and Rb were present in samples close to Champagne Pool than elsewhere, confirming its location as the main outflow source of Au, Ag and their pathfinder elements. The fern survey areas at Luck at Last mine, Pine Sinter and Ohui in the Coromandel Volcanic Zone each exhibited biogeochemical anomalies, which successfully highlighted most of the known quartz veins and provided additional anomalies for further investigation. Rough tree fern was the most common species at Goldmine Hill, Puhipuhi (Taupo Volcanic Zone). Although this species absorbs lower concentrations of many elements than the silver fern, the spatial distribution of elements is of greater significance than their absolute concentrations. The highest Au, Ag, As and Al concentrations occurred in samples from a ridge extending WNW from Goldmine Hill. Sb and Bi were at anomalous levels in an area peripheral to the precious metal anomalies, indicating the potential zonation of elements distal from the Au and Ag deposits.Supplementary material: The full datasets on the fern and tea tree chemistry, including quality assurance/quality control and multi-element plots, are available free of charge through the GNS Science website (search for Dunn) at http://shop.gns.cri.nz/publications/science-reports/.

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25

LIU, DONG, and ZHI-QIANG ZHANG. "New Zealand Austrophthiracarus (Acari, Oribatida, Steganacaridae): two new species from the North Island." Zootaxa 4500, no. 3 (October 16, 2018): 443. http://dx.doi.org/10.11646/zootaxa.4500.3.10.

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Two new species of Austrophthiracarus (Oribatida: Steganacaridae) from national parks on the North Island of New Zealand are described: Austrophthiracarus taranaki sp. nov. from moss along tracks in Wilkies Pools, Egmont National Park, Taranaki and Austrophthiracarus whirinaki sp. nov. from litter in Whirinaki Forest, between Rotorua and Taupo. An updated key to all known species of Austrophthiracarus in New Zealand is presented.

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26

Johnston, David, Brad Scott, Bruce Houghton, Douglas Paton, David Dowrick, Pilar Villamor, and John Savage. "Social and economic consequences of historic caldera unrest at the Taupo volcano, New Zealand and the management of future episodes of unrest." Bulletin of the New Zealand Society for Earthquake Engineering 35, no. 4 (December 31, 2002): 215–30. http://dx.doi.org/10.5459/bnzsee.35.4.215-230.

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In 1998, changes in a number of indicators (earthquakes and uplift) at two of New Zealand's active volcanic caldera systems (Okataina and Taupo) resulted in increased public, local and central government awareness and some concern about the potential significance of volcanic unrest at a caldera volcano. This paper summarises the episodes of unrest recorded at Taupo caldera since 1895. There have been four significant events (1895, 1922, 1963-64 and 1983) that have included earthquake activity and ground deformation. Caldera unrest is one of the most difficult situations the volcanological and emergency management communities will have to deal with. There is potential for adverse social and economic impacts to escalate unnecessarily, unless the event is managed appropriately. Adverse response to caldera unrest may take the form of the release of inappropriate advice, media speculation, unwarranted emergency declarations and premature cessation of economic activity and community services. A non-volcanic-crisis time provides the best opportunity to develop an understanding of the caldera unrest phenomena, and the best time to establish educational programmes, funding systems for enhanced emergency response and volcano surveillance and to develop co-ordinated contingency plans.

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27

Dade, W. Brian, and Herbert E. Huppert. "Emplacement of the Taupo ignimbrite by a dilute turbulent flow." Nature 381, no. 6582 (June 1996): 509–12. http://dx.doi.org/10.1038/381509a0.

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28

Sherburn, Steven. "Seismicity of the Lake Taupo region, New Zealand, 1985–90." New Zealand Journal of Geology and Geophysics 35, no. 3 (September 1992): 331–35. http://dx.doi.org/10.1080/00288306.1992.9514526.

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29

de Ronde, C. E. J., P. Stoffers, D. Garbe-Schönberg, B. W. Christenson, B. Jones, R. Manconi, P. R. L. Browne, et al. "Discovery of active hydrothermal venting in Lake Taupo, New Zealand." Journal of Volcanology and Geothermal Research 115, no. 3-4 (June 2002): 257–75. http://dx.doi.org/10.1016/s0377-0273(01)00332-8.

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30

Risk, G. F., H. M. Bibby, and T. G. Caldwell. "Resistivity structure of the central Taupo Volcanic Zone, New Zealand." Journal of Volcanology and Geothermal Research 90, no. 3-4 (June 1999): 163–81. http://dx.doi.org/10.1016/s0377-0273(99)00026-8.

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31

Simmons, Stuart F., Kevin L. Brown, Patrick R. L. Browne, and Julie V. Rowland. "Gold and silver resources in Taupo Volcanic Zone geothermal systems." Geothermics 59 (January 2016): 205–14. http://dx.doi.org/10.1016/j.geothermics.2015.07.009.

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32

Rawlence, David J. "Cyclomorphosis inAsterionella formosaHassall from Lake Taupo, North Island, New Zealand." Journal of the Royal Society of New Zealand 16, no. 2 (June 1986): 183–92. http://dx.doi.org/10.1080/03036758.1986.10418177.

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33

Acocella, V., K. Spinks, J. Cole, and A. Nicol. "Oblique back arc rifting of Taupo Volcanic Zone, New Zealand." Tectonics 22, no. 4 (August 2003): n/a. http://dx.doi.org/10.1029/2002tc001447.

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34

Whiteford, P. C. "Heat flow in the sediments of Lake Taupo, New Zealand." Tectonophysics 257, no. 1 (May 1996): 81–92. http://dx.doi.org/10.1016/0040-1951(95)00122-0.

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35

Roper, Juliet, Eva Marie Collins, and Josef de Jong. "Lake Taupo: a multi-sector collaborative partnership towards sustainable development." Journal of Public Affairs 15, no. 2 (September 12, 2014): 143–52. http://dx.doi.org/10.1002/pa.1540.

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36

Smith, Victoria C., Phil Shane, and Ian A. Nairn. "Trends in rhyolite geochemistry, mineralogy, and magma storage during the last 50 kyr at Okataina and Taupo volcanic centres, Taupo Volcanic Zone, New Zealand." Journal of Volcanology and Geothermal Research 148, no. 3-4 (December 2005): 372–406. http://dx.doi.org/10.1016/j.jvolgeores.2005.05.005.

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37

Arunachalam, Murugesh, Jagdeep Singh-Ladhar, and Andrea McLachlan. "Advancing environmental sustainability via deliberative democracy." Sustainability Accounting, Management and Policy Journal 7, no. 3 (September 5, 2016): 402–27. http://dx.doi.org/10.1108/sampj-10-2014-0062.

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Purpose This paper aims to examine the planning and policy processes in relation to the pollution in Lake Taupo. This paper describes and explains the manifestation of the tenets of deliberative democracy and the impediments of mobilising the tenets in the planning and policy-making processes. Design/methodology/approach This interpretive case study makes sense of interview transcripts, minutes of meetings, media reports and public documents and adopts deliberative democratic theory as the theoretical framework for the interpretive analysis. Findings Some factors fostered and others challenged the mobilization of the tenets of deliberative democracy. Local government processes facilitated the expression of multiple views in relation to the impacts of human activities on the Lake. Confrontations and tensions were inevitable elements of the deliberative processes. Pre-determined outcomes and domination of local authorities, aiming for environmental sustainability of Lake Taupo, posed as challenges to the operation of deliberative democracy. Some stakeholders need to sacrifice more than others, but recognition of pluralism, conflicts and differences is an essential part of deliberative democracy. Originality/value There is scarcity of research that empirically examines local government processes in light of deliberative democratic principles. The study also extends environmental and social studies that have explored the arena approach to accountability and decision-making.

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38

Stokes, Stephen, and David J. Lowe. "Discriminant Function Analysis of Late Quaternary Tephras from Five Volcanoes in New Zealand Using Glass Shard Major Element Chemistry." Quaternary Research 30, no. 3 (November 1988): 270–83. http://dx.doi.org/10.1016/0033-5894(88)90003-8.

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The microprobe-determined glass shard major element chemistry of tephras derived from five North Island, New Zealand volcanoes (Mayor Island, Okataina, Taupo, Tongariro, and Mount Egmont) and younger than ca. 20,000 yr B.P. was subjected to discriminant function analysis. Four separate approaches were adopted to test the match of the tephras with their known sources: (1) an analysis of raw microprobe data; (2) an analysis of normalized data; (3) an analysis of the data transformed by calculating the log10 of oxide scores divided (arbitrarily) by the chlorine content; and (4) a repeat of (3) with multivariate outlier scores, as determined by principal components analysis, deleted. All yielded excellent classification functions (efficiencies of 91–100%), with the eruptives associated with each of the five volcanoes being chemically distinct from one another. In each approach, the first two canonical discriminant functions accounted for >90% of the variation between groups. The removal of multivariate outliers from the data set had only minor effects on the performance of the discriminant function procedures. Separate discriminant function analysis of the relatively alike Taupo and Okataina eruptives gave a greater degree of multivariate separation. The numerical classifications generated should enable unidentified tephras erupted since ca. 20,000 yr B.P. from the five volcanoes to be provisionally matched with their sources.

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39

Campbell, Kathleen A., T. F. Buddle, and P. R. L. Browne. "Late Pleistocene siliceous sinter associated with fluvial, lacustrine, volcaniclastic and landslide deposits at Tahunaatara, Taupo Volcanic Zone, New Zealand." Transactions of the Royal Society of Edinburgh: Earth Sciences 94, no. 4 (December 2003): 485–501. http://dx.doi.org/10.1017/s0263593300000833.

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ABSTRACTThe Tahunaatara sinter, Taupo Volcanic Zone, New Zealand, is a ∼17–20-kyr-old hot-spring deposit of opal-A mineralogy. It is interbedded with fluvial, lacustrine and volcaniclastic sediments, some silicified by infusing thermal waters. The exposed sinter (∼4 m thick, 90 m long) was truncated at its southern margin by a landslide, which deposited a conglomerate (up to 2 m thick, 56 m long) of sinter blocks and associated strata nearby. Kaolinite-rich cobbles at the base of the conglomerate indicate a change in the thermal regime and its probable trigger: acid steamcondensate produced alteration. Clasts in the landslide are oriented SW, the same direction as flattened plant reeds entombed in sinter, and as intercalated fluvial beds. Thus, thermal waters, stream flow and the landslide all likely followed the same palaeo-valley, which is similar in terrain and stratigraphy to the Devonian Rhynie hydrothermal system. The plant-rich, layered, in situ sinter contains fossilised microbes and rare stromatolites, and was deposited on mid- to distal slopes adjacent to marshes. Ash falls, fluvial activity and ponding occurred during and after the thermal activity. Unsilicified tephric Ohakea loess (∼26–17 kyr BP) and Taupo Tephra (1·86 kyr BP) blanket both sinter and landslide. Today, the deposits form resistant remnants in a topographically inverted landscape.

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40

Matheson, FE, JL Tank, and KJ Costley. "Land use influences stream nitrate uptake in the Lake Taupo catchment." New Zealand Journal of Marine and Freshwater Research 45, no. 2 (June 2011): 287–300. http://dx.doi.org/10.1080/00288330.2011.562143.

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41

Bannister, Stephen, and Anne Melhuish. "Seismic scattering and reverberation, Kaingaroa plateau, Taupo Volcanic Zone, New Zealand." New Zealand Journal of Geology and Geophysics 40, no. 3 (September 1997): 375–81. http://dx.doi.org/10.1080/00288306.1997.9514768.

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42

Zachariasen, Judith, and Russ Van Dissen. "Paleoseismicity of the northern Horohoro Fault, Taupo Volcanic Zone, New Zealand." New Zealand Journal of Geology and Geophysics 44, no. 3 (September 2001): 391–401. http://dx.doi.org/10.1080/00288306.2001.9514946.

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43

Villamor, P., and K. R. Berryman. "Evolution of the southern termination of the Taupo Rift, New Zealand." New Zealand Journal of Geology and Geophysics 49, no. 1 (March 2006): 23–37. http://dx.doi.org/10.1080/00288306.2006.9515145.

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44

Robertson, Edwin I., and Frederick J. Davey. "The basement morphology under Tongariro National Park, southern Taupo Volcanic Zone." New Zealand Journal of Geology and Geophysics 61, no. 4 (September 16, 2018): 570–77. http://dx.doi.org/10.1080/00288306.2018.1518247.

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45

Timperley, M. H., and R. J. Vigor‐Brown. "Water chemistry of lakes in the Taupo Volcanic Zone, New Zealand." New Zealand Journal of Marine and Freshwater Research 20, no. 2 (June 1986): 173–83. http://dx.doi.org/10.1080/00288330.1986.9516141.

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46

Viner, A. B. "Hypolimnetic oxygen consumption in Lake Taupo, New Zealand: A preliminary assessment." New Zealand Journal of Marine and Freshwater Research 23, no. 3 (September 1989): 381–91. http://dx.doi.org/10.1080/00288330.1989.9516374.

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47

Viner, A. B. "Distribution of carbon, nitrogen, and phosphorus in Lake Taupo surface sediment." New Zealand Journal of Marine and Freshwater Research 23, no. 3 (September 1989): 393–99. http://dx.doi.org/10.1080/00288330.1989.9516375.

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48

Hawes, Ian, and Rob Smith. "Seasonal dynamics of epilithic periphyton in oligotrophic Lake Taupo, New Zealand." New Zealand Journal of Marine and Freshwater Research 28, no. 1 (March 1994): 1–12. http://dx.doi.org/10.1080/00288330.1994.9516592.

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49

Tretkoff, Ernie. "Research Spotlight: Understanding the magma distribution in the Taupo Volcanic Zone." Eos, Transactions American Geophysical Union 91, no. 25 (June 22, 2010): 228. http://dx.doi.org/10.1029/eo091i025p00228-01.

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50

Tanaka, H., G. M. Turner, B. F. Houghton, T. Tachibana, M. Kono, and M. O. McWilliams. "Palaeomagnetism and chronology of the central Taupo Volcanic Zone, New Zealand." Geophysical Journal International 124, no. 3 (March 1996): 919–34. http://dx.doi.org/10.1111/j.1365-246x.1996.tb05645.x.

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Journal articles on the topic 'Taupo'

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