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Journal articles on the topic 'Fiordland'

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Author: Grafiati

Published: 4 June 2021

Last updated: 31 January 2023

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1

JEWELL, TONY. "Two new species of Hemiandrus (Orthoptera: Anostostomatidae) from Fiordland National Park, New Zealand." Zootaxa 1542, no. 1 (August 6, 2007): 49–57. http://dx.doi.org/10.11646/zootaxa.1542.1.4.

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Two new species of Hemiandrus are described from alpine habitat in the Sinbad Gully of Fiordland National Park, New Zealand. H. superba n. sp. is the largest known member of the genus, and H. nitaweta n. sp. is perhaps the most brilliantly colored. Fiordland is a major centre of diversity for Hemiandrus; a photographic overview and key to the species recorded from the Park are provided.

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2

Blatchford, Hannah J., Keith A. Klepeis, Joshua J. Schwartz, Richard Jongens, Rose E. Turnbull, Elena A. Miranda, Matthew A. Coble, and Andrew R. C. Kylander-Clark. "Interplay of Cretaceous transpressional deformation and continental arc magmatism in a long-lived crustal boundary, central Fiordland, New Zealand." Geosphere 16, no. 5 (August 31, 2020): 1225–48. http://dx.doi.org/10.1130/ges02251.1.

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Abstract Recovering the time-evolving relationship between arc magmatism and deformation, and the influence of anisotropies (inherited foliations, crustal-scale features, and thermal gradients), is critical for interpreting the location, timing, and geometry of transpressional structures in continental arcs. We investigated these themes of magma-deformation interactions and preexisting anisotropies within a middle- and lower-crustal section of Cretaceous arc crust coinciding with a Paleozoic boundary in central Fiordland, New Zealand. We present new structural mapping and results of Zr-in-titanite thermometry and U-Pb zircon and titanite geochronology from an Early Cretaceous batholith and its host rock. The data reveal how the expression of transpression in the middle and lower crust of a continental magmatic arc evolved during emplacement and crystallization of the ∼2300 km2 lower-crustal Western Fiordland Orthogneiss (WFO) batholith. Two structures within Fiordland’s architecture of transpressional shear zones are identified. The gently dipping Misty shear zone records syn-magmatic oblique-sinistral thrust motion between ca. 123 and ca. 118 Ma, along the lower-crustal WFO Misty Pluton margin. The subhorizontal South Adams Burn thrust records mid-crustal arc-normal shortening between ca. 114 and ca. 111 Ma. Both structures are localized within and reactivate a recently described >10 km-wide Paleozoic crustal boundary, and show that deformation migrated upwards between ca. 118 and ca. 114 Ma. WFO emplacement and crystallization (mainly 118–115 Ma) coincided with elevated (>750 °C) middle- and lower-crustal Zr-in-titanite temperatures and the onset of mid-crustal cooling at 5.9 ± 2.0 °C Ma−1 between ca. 118 and ca. 95 Ma. We suggest that reduced strength contrasts across lower-crustal pluton margins during crystallization caused deformation to migrate upwards into thermally weakened rocks of the mid-crust. The migration was accompanied by partitioning of deformation into domains of arc-normal shortening in Paleozoic metasedimentary rocks and domains that combined shortening and strike-slip deformation in crustal-scale subvertical, transpressional shear zones previously documented in Fiordland. U-Pb titanite dates indicate Carboniferous–Cretaceous (re)crystallization, consistent with reactivation of the inherited boundary. Our results show that spatio-temporal patterns of transpression are influenced by magma emplacement and crystallization and by the thermal structure of a reactivated boundary.

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3

Roberts, Clive D. "Fiordland is a special place." New Zealand Journal of Marine and Freshwater Research 35, no. 4 (December 2001): 649–51. http://dx.doi.org/10.1080/00288330.2001.9517031.

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4

Blattner, Peter. "The North Fiordland transcurrent convergence." New Zealand Journal of Geology and Geophysics 34, no. 4 (December 1991): 533–42. http://dx.doi.org/10.1080/00288306.1991.9514488.

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5

Smith, Warwick D. "New Zealand earthquakes in 1989." Bulletin of the New Zealand Society for Earthquake Engineering 23, no. 2 (June 30, 1990): 97–101. http://dx.doi.org/10.5459/bnzsee.23.2.97-101.

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During 1989 the Seismological Observatory recorded and analysed 9892 earthquakes in the New Zealand region. Preliminary locations and magnitudes are now available for all these events. This is about five times the number usually analysed in previous years, thanks to the new digital recording equipment which is being installed throughout the country. No earthquakes reached magnitude 6 during the year, although one of magnitude 5.9 in Fiordland was close to that figure. This caused intensity MM VI throughout Fiordland, and lower intensities elsewhere in the southern half of the South Island. Earthquakes of magnitude 5 and greater are listed: they indicate an ongoing level of activity commensurate with New Zealand's seismic history and geographic location.

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6

Warham, John. "THE FIORDLAND CRESTED PENGUIN EUDYPTES PACHYRHYNCHUS." Ibis 116, no. 1 (April 3, 2008): 1–27. http://dx.doi.org/10.1111/j.1474-919x.1974.tb00220.x.

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7

McGinty, P. "The 2003, Mw 7.2 Fiordland earthquake, and its near-source aftershock strong motion data." Bulletin of the New Zealand Society for Earthquake Engineering 37, no. 3 (September 30, 2004): 139–45. http://dx.doi.org/10.5459/bnzsee.37.3.139-145.

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The 2003 Fiordland earthquake was not only the best ever recorded subduction interface earthquake to occur in New Zealand, it also provided the opportunity to collect near-source strong-motion data produced by its aftershocks covering a wide magnitude range. Near source strong-motion data had been lacking in the New Zealand data set, on which current attenuation models are based. Here the author presents some preliminary results relating recorded peak ground accelerations in the near-source field to current attenuation models. The near-source data from the 2003 Fiordland earthquake sequence has shown that the observed data has a greater magnitude-dependence than that predicted by the current attenuation models. This new data will help to improve current models and will lead to a better understanding of the attenuation process associated with New Zealand subduction interface earthquakes.

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8

Davis, JP, and SR Wing. "Niche partitioning in the Fiordland wrasse guild." Marine Ecology Progress Series 446 (February 2, 2012): 207–20. http://dx.doi.org/10.3354/meps09452.

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9

Wing, SR, and L. Jack. "Fiordland: the ecological basis for ecosystem management." New Zealand Journal of Marine and Freshwater Research 48, no. 4 (April 30, 2014): 577–93. http://dx.doi.org/10.1080/00288330.2014.897636.

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10

Van Dissen, R., J. Cousins, R. Robinson, and M. Reyners. "The Fiordland earthquake of 10 August, 1993." Bulletin of the New Zealand Society for Earthquake Engineering 27, no. 2 (June 30, 1994): 147–54. http://dx.doi.org/10.5459/bnzsee.27.2.147-154.

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On 10 August, 1993, a ML 6.7 (Ms 7.1, Mw 7.0) earthquake occurred c. 10 km offshore of western Fiordland, New Zealand (45.2° S, 166.7° E). Its hypocentre is approximately 20 km deep which places it on, or close to, the interface between the subducted Australian plate and the overriding Pacific plate. The focal mechanism for the mainshock indicates reverse faulting on either a steep west-dipping, or shallow southeast-dipping plane. Analysis of a subset of the over 7,000 recorded aftershocks defines a shallow (c. 15°) southeast-dipping plane, roughly 25 km long and 15 km wide, that probably represents the rupture surface of the mainshock. The earthquake was strongly felt by fishermen offshore in the epicentral region. Onshore, there were no reports of damage to man-made structures. The maximum peak ground acceleration recorded was 0.08 g at Te Anau, about 73 km from the epicentre. The attenuation of peak horizontal ground acceleration for this event is similar to the attenuation of other shallow crustal earthquakes in New Zealand. The number of landslides triggered by this event is at least an order-of-magnitude less than the number of pre-existing landslide scars. The highest concentration of new slides appears to be in the Vancouver Arm/Hall Arm region, c. 45 km south-southeast from the epicentre. Many of the new slides were narrow, shallow seated failures, or small reactivated portions of older slides. The two largest earthquake-triggered landslides observed are located near Hall Arm, and in the Freeman Burn north of Lake Manapouri. Except perhaps for these two slides, all other observed earthquake-triggered slides will be indistinguishable from storm-generated slides once re-vegetated.

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11

Bradshaw, J. Y. "Geology of crystalline rocks of northern Fiordland: Details of the granulite facies Western Fiordland Orthogneiss and associated rock units." New Zealand Journal of Geology and Geophysics 33, no. 3 (July 1990): 465–84. http://dx.doi.org/10.1080/00288306.1990.10425702.

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12

Reyners, Martin, Peter McGinty, Simon Cox, Ian Turnbull, Tim O'Neill, Ken Gledhill, Graham Hancox, et al. "The Mw 7.2 Fiordland earthquake of August 21, 2003." Bulletin of the New Zealand Society for Earthquake Engineering 36, no. 4 (December 31, 2003): 233–48. http://dx.doi.org/10.5459/bnzsee.36.4.233-248.

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The Mw 7.2 Fiordland earthquake of August 21 2003 was the largest shallow earthquake to occur in New Zealand for 35 years. Because of its location in an unpopulated area, it caused only minor damage to buildings, roads and infrastructure. It triggered numerous landslides on steep slopes in the epicentral region, where intensities reached MM9. Deployments of portable seismographs, strong motion recorders and GPS receivers in the epicentral region immediately after the event have established that the earthquake involved thrusting at the shallow part of the subduction interface between the Australian and Pacific plates. Recently installed strong motion recorders of the GeoNet network have ensured that the earthquake is New Zealand's best recorded subduction interface event. Microzonation effects are clear in some of the records. Current peak ground acceleration attenuation relationships for New Zealand subduction interface earthquakes underprediet the ground motions recorded during the earthquake, as was the case for previous large events in Fiordland in 1993 and 1989. The four portable strong motion recorders installed in the epicentral region have provided excellent near-field data on the larger aftershocks, with recorded peak ground accelerations ranging up to 0.28g from a nearby ML 6.1 event.

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13

Lusseau, David, Liz Slooten, and Rohan J. C. Currey. "Unsustainable Dolphin-watching Tourism in Fiordland, New Zealand." Tourism in Marine Environments 3, no. 2 (December 1, 2006): 173–78. http://dx.doi.org/10.3727/154427306779435184.

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14

McQueen, Shirley M., Lloyd S. Davis, and Graham Young. "The Reproductive Endocrinology of Fiordland Crested PenguinsEudyptes pachyrhynchus." Emu - Austral Ornithology 98, no. 2 (June 1998): 127–31. http://dx.doi.org/10.1071/mu98013.

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15

ALLIBONE, A. H., L. A. MILAN, N. R. DACZKO, and I. M. TURNBULL. "Granulite facies thermal aureoles and metastable amphibolite facies assemblages adjacent to the Western Fiordland Orthogneiss in southwest Fiordland, New Zealand." Journal of Metamorphic Geology 27, no. 5 (June 2009): 349–69. http://dx.doi.org/10.1111/j.1525-1314.2009.00822.x.

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16

Van Houtte, Chris, Stephen Bannister, Caroline Holden, Sandra Bourguignon, and Graeme McVerry. "The New Zealand Strong Motion Database." Bulletin of the New Zealand Society for Earthquake Engineering 50, no. 1 (March 31, 2017): 1–20. http://dx.doi.org/10.5459/bnzsee.50.1.1-20.

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This article summarises work that has been undertaken to compile the New Zealand Strong Motion Database, which is intended to be a significant resource for both researchers and practitioners. The database contains 276 New Zealand earthquakes that were recorded by strong motion instruments from GeoNet and earlier network operators. The events have moment magnitudes ranging from 3.5 to 7.8. A total of 134 of these events (49%) have been classified as occurring in the overlying crust, with 33 events (12%) located on the Fiordland subduction interface and 7 on the Hikurangi subduction interface (3%). 8 events (3%) are deemed to have occurred within the subducting Australian Plate at the Fiordland subduction zone, and 94 events (34%) within the subducting Pacific Plate on the Hikurangi subduction zone. There are a total of 4,148 uniformly-processed recordings associated with these earthquakes, from which acceleration, velocity and displacement time-series, Fourier amplitude spectra of acceleration, and acceleration response spectra have been computed. 598 recordings from the New Zealand database are identified as being suitable for future use in time-domain analyses of structural response. All data are publicly available at http://info.geonet.org.nz/x/TQAdAQ.

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17

Poupart, TA, SM Waugh, CA Bost, A. Kato, CM Miskelly, KM Rogers, and JPY Arnould. "Foraging ecology of a winter breeder, the Fiordland penguin." Marine Ecology Progress Series 614 (April 4, 2019): 183–97. http://dx.doi.org/10.3354/meps12910.

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18

Brewin, Paul E., P. Keith Probert, and Mike F. Barker. "Deep‐basin macrobenthos of Doubtful Sound, Fiordland, New Zealand." New Zealand Journal of Marine and Freshwater Research 42, no. 1 (March 2008): 1–21. http://dx.doi.org/10.1080/00288330809509932.

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19

Mortimer, N., P. B. Gans, F. V. Foley, M. B. Turner, N. Daczko, M. Robertson, and I. M. Turnbull. "Geology and Age of Solander Volcano, Fiordland, New Zealand." Journal of Geology 121, no. 5 (September 2013): 475–87. http://dx.doi.org/10.1086/671397.

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20

Scott, JM, and JM Palin. "Molybdenite in Pomona Island Granite at Lake Manapouri, Fiordland." New Zealand Journal of Geology and Geophysics 54, no. 3 (September 2011): 347–52. http://dx.doi.org/10.1080/00288306.2011.580768.

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21

Bishop, D. G., and David G. Howell. "An Oligocene submarine rockfall/avalanche breccia, Fiordland, New Zealand." New Zealand Journal of Geology and Geophysics 28, no. 2 (April 1985): 233–41. http://dx.doi.org/10.1080/00288306.1985.10422223.

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22

Gibson, G. M., and T. R. Ireland. "Granulite formation during continental extension in Fiordland, New Zealand." Nature 375, no. 6531 (June 1995): 479–82. http://dx.doi.org/10.1038/375479a0.

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23

Morris, Simon J. "Two new species ofSigausfrom Fiordland, New Zealand (Orthoptera: Acrididae)." New Zealand Entomologist 26, no. 1 (December 2003): 65–74. http://dx.doi.org/10.1080/00779962.2003.9722110.

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24

CHAPPLE, DAVID G., TRENT P. BELL, STEPHANIE N. J. CHAPPLE, KIMBERLY A. MILLER, CHARLES H. DAUGHERTY, and GEOFF B. PATTERSON. "Phylogeography and taxonomic revision of the New Zealand cryptic skink (Oligosoma inconspicuum; Reptilia: Scincidae) species complex." Zootaxa 2782, no. 1 (March 3, 2011): 1. http://dx.doi.org/10.11646/zootaxa.2782.1.1.

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The New Zealand skink fauna is highly diverse and contains numerous cryptic, undescribed or hitherto undiscovered species. We completed a taxonomic revision of the cryptic skink (Oligosoma inconspicuum) species complex using molecular (550 bp of the ND2 mitochondrial gene) and morphological analyses. Four new species are described, with each diagnosable by a range of morphological characters and genetic differentiation from several closely related species: O. inconspicuum (sensu stricto), O. notosaurus, O. maccanni, O. stenotis and O. grande. Oligosoma tekakahu sp. nov. is restricted to Chalky Island in Fiordland, and is most closely related to O. inconspicuum and O. notosaurus. The other three new species are restricted to particular mountainous regions in central and western Otago (O. burganae sp. nov., Lammermoor and Rock and Pillar Ranges; O. toka sp. nov., Nevis Valley; O. repens sp. nov., Eyre Mountains) and are most closely related to O. stenotis and O. grande. We also re-described O. inconspicuum. Two proposed new taxa, the ‘Big Bay’ skink and ‘Mahogany’ skink, were found to represent Westland/Fiordland populations of O. inconspicuum rather than distinct taxa. We discuss the evolutionary and phylogeographic implications of cryptic and ‘anti-cryptic’ species within the O. inconspicuum species complex, and suggest that morphologically aberrant populations are the result of local adaptation to novel selective regimes.

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25

Stevens, Leigh, Mark Gibbs, Julian Roberts, Dayne Maxwell, and Rob Service. "ECOLOGICAL RISK ASSESSMENT – A HIGH SPEED VERSION USED IN NEW ZEALAND." International Oil Spill Conference Proceedings 2005, no. 1 (May 1, 2005): 271–76. http://dx.doi.org/10.7901/2169-3358-2005-1-271.

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ABSTRACT Cooperative oil spill Ecological Risk Assessment (C-ERA) is a preparedness tool that seeks consensus-based decisions regarding potential spill and spill response impacts. The established US Coast Guard ERA approach has generally used 1–2 multi-day workshops, several weeks apart, to identify and work through key issues. In New Zealand (NZ), funding limitations required a faster approach. This paper describes the advantages and disadvantages encountered during a modified 1-day version of the ERA conducted for the Fiordland region. Fiordland is a highly valued and remote National Park and World Heritage Area of 1.25 million Ha, with ∼200km of exposed coastline, and ∼1800km internal coastline including 15 main fiords. The unique climate, topography, bathymetry and oceanography, in addition to limited access and infrastructure, make marine pollution response inherently difficult. Recent increases in cruise ship and commercial maritime activity has increased the spill risk, especially for fuel oil. Information previously gathered from interest/advocate groups and government agencies was used to identify priority resources and summarise the spill risk. Then, at a 1-day workshop, six experts in Fiordland ecology, spill response and ERA processes defined the most ecologically important areas and priority resources across the region, and their susceptibility to oil. Levels of concern were applied to each area and identified resource, and the preferred response options and their feasibility defined. Outputs were presented on a series of planning maps and site sheets completed for each priority area after the workshop which were circulated for stakeholder review. The approach enabled a defensible response plan to be generated quickly and cheaply. It secured input from agencies who would not have participated had a greater time input been required and generated a concise document for public consultation and a template for ongoing refinement. The success of the approach was due largely to the high level of trust between scientific and response agencies in NZ, and a shared desire to rapidly improve response planning outcomes. Disadvantages were the inability to fully review and include all available technical information, limited public consultation, and tight time pressures. Examples are given of the benefit of the plan following its use during a recent spill of marine diesel.

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26

Wood, Ray, Rick Herzer, Rupert Sutherland, and Anne Melhuish. "Cretaceous‐Tertiary tectonic history of the Fiordland margin, New Zealand." New Zealand Journal of Geology and Geophysics 43, no. 2 (June 2000): 289–302. http://dx.doi.org/10.1080/00288306.2000.9514887.

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27

Annala, John H., and Bruce L. Bycroft. "Growth of rock lobsters (Jasus edwardsii)in Fiordland, New Zealand." New Zealand Journal of Marine and Freshwater Research 22, no. 1 (March 1988): 29–41. http://dx.doi.org/10.1080/00288330.1988.9516275.

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28

McLean, Ian G., Stephanie D. Kayes, Jan O. Murie, Lloyd S. Davis, and David M. Lambert. "Genetic monogamy mirrors social monogamy in the Fiordland crested penguin." New Zealand Journal of Zoology 27, no. 4 (January 2000): 311–16. http://dx.doi.org/10.1080/03014223.2000.9518240.

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29

Augustinus, Paul C. "Outlet glacier trough size-drainage area relationships, Fiordland, New Zealand." Geomorphology 4, no. 5 (March 1992): 347–61. http://dx.doi.org/10.1016/0169-555x(92)90028-m.

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30

Elliott, Graeme, Murray Willans, Hannah Edmonds, and David Crouchley. "Stoat invasion, eradication and re-invasion of islands in Fiordland." New Zealand Journal of Zoology 37, no. 1 (March 2010): 1–12. http://dx.doi.org/10.1080/03014221003602166.

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31

BELL, TRENT P., and GEOFF B. PATTERSON. "A rare alpine skink Oligosoma pikitanga n. sp. (Reptilia: Scincidae) from Llawrenny Peaks, Fiordland, New Zealand." Zootaxa 1882, no. 1 (September 22, 2008): 57. http://dx.doi.org/10.11646/zootaxa.1882.1.3.

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A new species of alpine skink, Oligosoma pikitanga, is described from the Llawrenny Peaks, Fiordland, New Zealand. This species is diagnosed on the basis of strong morphological, ecological, and genetic differentiation from the following relatives O. acrinasum, O. infrapunctatum, O. otagense, O. taumakae and O. waimatense. The species is characterized by a shiny black base colour with bright green dorsal blotches, lateral pinkish spots and a vivid orange belly. It appears this new taxon is extremely rare, and at enhanced risk from introduced mammalian predators.

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32

Hegg, Danilo, Darryl I. MacKenzie, and Ian G. Jamieson. "Use of Bayesian population viability analysis to assess multiple management decisions in the recovery programme for the Endangered takahe Porphyrio hochstetteri." Oryx 47, no. 1 (January 2013): 144–52. http://dx.doi.org/10.1017/s0030605311001736.

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AbstractPopulation modelling is an invaluable tool for identifying effective management strategies for threatened species whose populations are too small for experimental manipulation. Recently developed Bayesian approaches allow us to combine deterministic models with probability distributions to create stochastic models that account for uncertainty. We illustrate this approach in the case of the takahe Porphyrio hochstetteri, an Endangered flightless rail, which is supported by one of New Zealand's costliest recovery programmes. Using mark–recapture and logistic regression models implemented in a Bayesian framework we calculated demographic parameters for a fully stochastic population model based on 25 years of data collected from the last wild population of takahe in the Murchison Mountains, Fiordland. Our model results show that stoat trapping, captive rearing and cross-fostering of eggs/chicks in wild pairs all have a positive effect on takahe demography. If it were not for these management actions the Fiordland population would probably be declining (λ = 0.985; confidence interval, CI = 0.39–1.08), with a non-negligible risk of quasi-extinction (P = 16%) within 20 years. The captive rearing of eggs and chicks has been the main factor responsible for the positive growth observed during the last decade but in the future expanding stoat trapping to cover the entire Murchison Mountains would be the single most beneficial management action for the takahe population (λ = 1.038; CI = 0.86–1.10), followed by captive rearing (λ = 1.027; CI = 0.85–1.09).

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33

BROWN, E. H. "High-pressure metamorphism caused by magma loading in Fiordland, New Zealand." Journal of Metamorphic Geology 14, no. 4 (July 1996): 441–52. http://dx.doi.org/10.1046/j.1525-1314.1996.06024.x.

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34

Annala, John H., and Bruce L. Bycroft. "Movements of rock lobsters (Jasus edwardsii) tagged in Fiordland, New Zealand." New Zealand Journal of Marine and Freshwater Research 27, no. 2 (June 1993): 183–90. http://dx.doi.org/10.1080/00288330.1993.9516556.

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35

Bishop, D. G. "Inferred uplift rates from raised marine surfaces, southern Fiordland, New Zealand." New Zealand Journal of Geology and Geophysics 28, no. 2 (April 1985): 243–51. http://dx.doi.org/10.1080/00288306.1985.10422224.

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36

Owens, I. F., and B. B. Fitzharris. "Assessing Avalanche-Risk Levels on Walking Tracks in Fiordland, New Zealand." Annals of Glaciology 13 (1989): 231–36. http://dx.doi.org/10.3189/s0260305500007953.

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Walking tracks which cross relatively rugged avalanche-prone terrain are becoming increasingly popular in New Zealand. Consequently, there exists the need to develop a methodology by which it will be possible objectively to assess the avalanche hazard in the vicinity of the tracks. This paper outlines some procedures that have been used to map avalanche paths, and introduces modifications to an internationally used highway hazard index employed to quantify the danger to walkers. The Fiordland region of south-west New Zealand is an area of spectacular scenic beauty, made famous by the Milford Track which has been walked by large numbers of tourists since the late nineteenth century. In recent years, avalanches have killed one person on the track, severely damaged a lodge, and destroyed several small bridges. Other walking tracks have been opened to tourists in this century and one of these, the Routeburn Track, is included in this study. Avalanche paths which affected the Milford and Routeburn Tracks were mapped in the field using well-established techniques and applying the results of previous research on the Milford Road, where historical records are available for a period of 50 years. The risk to walkers was assessed with a hazard index which depends on frequency of avalanches, numbers of paths, time taken to traverse each path, and numbers of walkers using the track. Results indicate that the avalanche hazard is low to moderate on the Milford Track and moderate on the Routeburn Track. The management implications of these findings are outlined.

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37

Reyners, Martin, Russell Robinson, Aasha Pancha, and Peter McGinty. "Stresses and strains in a twisted subduction zone-Fiordland, New Zealand." Geophysical Journal International 148, no. 3 (March 27, 2002): 637–48. http://dx.doi.org/10.1046/j.1365-246x.2002.01611.x.

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38

House, M. A. "Uplift in the Fiordland Region, New Zealand: Implications for Incipient Subduction." Science 297, no. 5589 (September 20, 2002): 2038–41. http://dx.doi.org/10.1126/science.1075328.

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39

Hill, Evelyn June. "A deep crustal shear zone exposed in western Fiordland, New Zealand." Tectonics 14, no. 5 (October 1995): 1172–81. http://dx.doi.org/10.1029/95tc01508.

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40

Owens, I. F., and B. B. Fitzharris. "Assessing Avalanche-Risk Levels on Walking Tracks in Fiordland, New Zealand." Annals of Glaciology 13 (1989): 231–36. http://dx.doi.org/10.1017/s0260305500007953.

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Walking tracks which cross relatively rugged avalanche-prone terrain are becoming increasingly popular in New Zealand. Consequently, there exists the need to develop a methodology by which it will be possible objectively to assess the avalanche hazard in the vicinity of the tracks. This paper outlines some procedures that have been used to map avalanche paths, and introduces modifications to an internationally used highway hazard index employed to quantify the danger to walkers. The Fiordland region of south-west New Zealand is an area of spectacular scenic beauty, made famous by the Milford Track which has been walked by large numbers of tourists since the late nineteenth century. In recent years, avalanches have killed one person on the track, severely damaged a lodge, and destroyed several small bridges. Other walking tracks have been opened to tourists in this century and one of these, the Routeburn Track, is included in this study. Avalanche paths which affected the Milford and Routeburn Tracks were mapped in the field using well-established techniques and applying the results of previous research on the Milford Road, where historical records are available for a period of 50 years. The risk to walkers was assessed with a hazard index which depends on frequency of avalanches, numbers of paths, time taken to traverse each path, and numbers of walkers using the track. Results indicate that the avalanche hazard is low to moderate on the Milford Track and moderate on the Routeburn Track. The management implications of these findings are outlined.

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Taylor, Rowland H., and Bruce W. Thomas. "Rats eradicated from rugged breaksea island (170 HA), Fiordland, New Zealand." Biological Conservation 65, no. 3 (1993): 191–98. http://dx.doi.org/10.1016/0006-3207(93)90052-3.

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Barnes, P. M., R. A. Pickrill, H. C. Bostock, E. K. Dlabola, A. R. Gorman, and G. S. Wilson. "Relict proglacial deltas in Bradshaw and George sounds, Fiordland, New Zealand." Geological Society, London, Memoirs 46, no. 1 (2016): 91–92. http://dx.doi.org/10.1144/m46.59.

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Uslu, B., W. Power, D. Greenslade, M. Eblé, and V. Titov. "The July 15, 2009 Fiordland, New Zealand Tsunami: Real-Time Assessment." Pure and Applied Geophysics 168, no. 11 (March 11, 2011): 1963–72. http://dx.doi.org/10.1007/s00024-011-0281-7.

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Dlabola, E. K., G. S. Wilson, A. R. Gorman, C. R. Riesselman, and C. M. Moy. "A post-glacial relative sea-level curve from Fiordland, New Zealand." Global and Planetary Change 131 (August 2015): 104–14. http://dx.doi.org/10.1016/j.gloplacha.2015.05.010.

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Hamling, I. J., and S. Hreinsdóttir. "Reactivated afterslip induced by a large regional earthquake, Fiordland, New Zealand." Geophysical Research Letters 43, no. 6 (March 21, 2016): 2526–33. http://dx.doi.org/10.1002/2016gl067866.

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Stewart, Glenn H. "Forest dynamics and disturbance in a beech/hardwood forest, Fiordland, New Zealand." Vegetatio 68, no. 2 (December 1986): 115–26. http://dx.doi.org/10.1007/bf00045063.

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Scott, J. M., A. F. Cooper, and J. M. Palin. "Beehive Diorite: A Late Jurassic two‐pyroxene pluton at Lake Manapouri, Fiordland." New Zealand Journal of Geology and Geophysics 52, no. 2 (June 2009): 59–65. http://dx.doi.org/10.1080/00288300909509878.

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Otley, Helen, Jane Tansell, and Paul Scofield. "A comprehensive demographic assessment of the endangered Fiordland crested penguin Eudyptes pachyrhynchus." New Zealand Journal of Zoology 44, no. 2 (February 15, 2017): 144–62. http://dx.doi.org/10.1080/03014223.2017.1284135.

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Sander, Sylvia G., Barry Anderson, Malcolm R. Reid, Jonathan P. Kim, and Keith A. Hunter. "Trace metal chemistry in the pristine freshwater Lake Hauroko, Fiordland, New Zealand." Microchemical Journal 111 (July 2013): 74–81. http://dx.doi.org/10.1016/j.microc.2012.12.012.

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Mahesh, P., Bhaskar Kundu, J. K. Catherine, and V. K. Gahalaut. "Anatomy of the 2009 Fiordland earthquake (Mw 7.8), South Island, New Zealand." Geoscience Frontiers 2, no. 1 (January 2011): 17–22. http://dx.doi.org/10.1016/j.gsf.2010.12.002.

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