Arc Volcanism in New Zealand
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Coastal and Marine Ecological Classification Standard (2012)
FGDC-STD-018-2012 Coastal and Marine Ecological Classification Standard Marine and Coastal Spatial Data Subcommittee Federal Geographic Data Committee June, 2012 Federal Geographic Data Committee FGDC-STD-018-2012 Coastal and Marine Ecological Classification Standard, June 2012 ______________________________________________________________________________________ CONTENTS PAGE 1. Introduction ..................................................................................................................... 1 1.1 Objectives ................................................................................................................ 1 1.2 Need ......................................................................................................................... 2 1.3 Scope ........................................................................................................................ 2 1.4 Application ............................................................................................................... 3 1.5 Relationship to Previous FGDC Standards .............................................................. 4 1.6 Development Procedures ......................................................................................... 5 1.7 Guiding Principles ................................................................................................... 7 1.7.1 Build a Scientifically Sound Ecological Classification .................................... 7 1.7.2 Meet the Needs of a Wide Range of Users ...................................................... -
Status of Pacific Island Coral Reef Fisheries by Tim Adams1, Paul Dalzell1 and Richard Farman2
Status of Pacific Island coral reef fisheries by Tim Adams1, Paul Dalzell1 and Richard Farman2 1. SPC Coastal Fisheries Programme 2. Service de la mer, Province Sud, Nouméa, New Caledonia (paper presented at 8th International Coral Reef Symposium, Panama, 1996) Abstract It is difficult to determine the status of fisheries on Pacific Islands coral reefs. The region is economically undeveloped, sparsely populated and its coral reefs are scattered over a vast area. Resultant constraints on monitoring and investigation mean that quantitative information is rare. The few available quantitative indicators are summarised here alongside opinions based on extensive practical experience. Most anecdotal reports about exploitation of Pacific Island marine life that reach the global press concern adverse aspects of fisheries and this, in context with the definite crises being experienced in other global fisheries, particularly southeast Asian reef-fisheries, has led to a general feeling of pessimism about the broad impact of fishing on Pacific Island reefs. However, the available evidence suggests that Pacific Island reef fisheries as a whole do not exert an excessive pressure on reefs and that (high) local protein nutritional demands can be sustained at least for the immediate future. However, it is urgent that this apparent overall sustainability be consolidated through state-recognised management arrangements; it is necessary that some specific overfishing problems be addressed; and it is particularly important that the adverse influence of terrestrial activities and run-off on the carrying capacity of coral reefs fisheries be mitigated. Introduction Fisheries on Pacific Island coral reefs, despite the increasing pace of outside influence, are still overwhelmingly subsistence fisheries. -
Articles Ranging in Resents Both Gravitational Acceleration and the Effect of Bed Size from Tens of Meters to a Few Centimeters in Diameter
Nat. Hazards Earth Syst. Sci., 6, 671–685, 2006 www.nat-hazards-earth-syst-sci.net/6/671/2006/ Natural Hazards © Author(s) 2006. This work is licensed and Earth under a Creative Commons License. System Sciences Numerical simulation of tsunami generation by cold volcanic mass flows at Augustine Volcano, Alaska C. F. Waythomas1, P. Watts2, and J. S. Walder3 1U.S. Geological Survey, Alaska Volcano Observatory, Anchorage, AK, USA 2Applied Fluids Engineering Inc., Long Beach, CA, USA 3U.S. Geological Survey, Cascades Volcano Observatory, Vancouver, WA, USA Received: 18 April 2006 – Revised: 22 June 2006 – Accepted: 22 June 2006 – Published: 26 July 2006 Abstract. Many of the world’s active volcanoes are situated 1 Introduction on or near coastlines. During eruptions, diverse geophysical mass flows, including pyroclastic flows, debris avalanches, Many of the world’s active volcanoes are located within a and lahars, can deliver large volumes of unconsolidated de- few tens of kilometers of the sea or other large bodies of wa- bris to the ocean in a short period of time and thereby gen- ter. During eruptions, large volumes of volcaniclastic debris erate tsunamis. Deposits of both hot and cold volcanic mass may enter nearby water bodies, and under certain conditions, flows produced by eruptions of Aleutian arc volcanoes are this process may initiate tsunamis (Tinti et al., 1999; Tinti exposed at many locations along the coastlines of the Bering et al., 2003). Worldwide, tsunamis caused by volcanic erup- Sea, North Pacific Ocean, and Cook Inlet, indicating that tions are somewhat infrequent (Latter, 1981); however, doc- the flows entered the sea and in some cases may have ini- umented historical cases illustrate that loss of life and prop- tiated tsunamis. -
Protecting an Icon Managing Sources of Diffuse Nutrient Inflow to Lake Taupo, New Zealand Abstract Introduction Mandate for Acti
Diffuse Pollution Conference, Dublin 2003 1C Water Resources Management PROTECTING AN ICON MANAGING SOURCES OF DIFFUSE NUTRIENT INFLOW TO LAKE TAUPO, NEW ZEALAND Tony Petch1, Justine Young1, Bruce Thorrold2 and Bill Vant1 1Environment Waikato, PO Box 4010, Hamilton East, New Zealand 2Dexcel Ltd, Private Bag 3221, Hamilton ABSTRACT Lake Taupo is a large, near pristine lake in New Zealand, highly valued for its clear blue waters. Increasing loads of nitrogen from the surrounding catchment threaten lake water quality. A management proposal is presented that promotes a sustainable development pathway for the lake community thereby protecting the lake for all New Zealanders. A community change process to protect the environmental, economic, cultural and spiritual values of a lake is described Keywords: Community, economy, Lake Taupo, land use, management, nutrients, policy, water quality INTRODUCTION Lake Taupo is the largest lake in New Zealand (area 620 km2, mean depth 95m). It is highly valued for its crystal blue water and dramatic vistas. These features provide the basis of an international tourist mecca and a world-class trout fishery as well as an important local recreation area and preferred retirement location. The lake is also important spiritually and culturally to the local indigenous people, Ngati Tuwharetoa. Lake Taupo’s excellent water quality is derived from extremely low levels of plant nutrients and phytoplankton. Unlike many other lakes, nitrogen availability rather than phosphorus limits phytoplankton growth in Taupo. Increased nutrient flows, especially nitrogen, from intensifying rural land use and urban growth in the catchment promotes algal and phytoplankton growth and threatens water clarity and the excellent water quality of the lake. -
3D Visualisation Model of the Taupo Volcanic Zone Basement S.A
3D VISUALISATION MODEL OF THE TAUPO VOLCANIC ZONE BASEMENT S.A. Alcaraz 1, M.S. Rattenbury 2, M.D. Rosenberg 1, S. Soengkono 1, G. Bignall 1 and H. van Moerkerk 3 1 GNS Science, Wairakei Research Centre, Private Bag 2000, Taupo 3352, New Zealand 2 GNS Science, PO Box 30-368, Lower Hutt 5040, New Zealand 3 ARANZ Geo Ltd., PO Box 3894, Christchurch 8140, New Zealand [email protected] Keywords: 3D modelling, 3D visualisation, calderas, 2001). The TVZ has been drilled for geothermal and Taupo Volcanic Zone, Torlesse Supergroup, Leapfrog mineral exploration, with recent drilling including Geothermal exploration, production and injection of deep geothermal boreholes. These boreholes are providing new information ABSTRACT on the geology and structure of several TVZ geothermal The Taupo Volcanic Zone (TVZ; ~350 km long, ~60 km systems, including Wairakei-Tauhara (Rosenberg et al., wide) constitutes the southern portion of the active Lau- 2009; Bignall et al., 2010; Alcaraz et al., 2010), Ohaaki Havre-Taupo extensional back arc basin, and formed by (Milicich et al., 2008; Milicich et al., 2010b), Kawerau extension of crust above the Hikurangi subduction zone in (Milicich et al., 2010a; Alcaraz, 2010) and Ngatamariki the central North Island. The fault-controlled depression is (Bignall, 2009). infilled by Quaternary volcanic rock and sediments, with the top of underlying basement greywacke displaced up to In recent years, the New Zealand geothermal community 1-2 km below sea level. has come to consider the potential of untapped, deeper and hotter geothermal resources in the TVZ – i.e. beyond the 1 A geological basement model of top surface of the Torlesse to 3 km depth interval that defines most of the >240°C greywacke in the TVZ is presented. -
Wood Calderas and Geothermal Systems in The
WOOD CALDERAS AND GEOTHERMAL SYSTEMS IN THE TAUPO VOLCANIC ZONE, NEW ZEALAND C Peter Wood Institute of Geological Nuclear Sciences Ltd, Wairakei Research Centre Taupo, New Zealand Key Words: Calderas, Geothermal Systems, Taupo Volcanic Zone. New Zcaland 2. TAUPO VOLCANIC ZONE The Taupo Volcanic Zone Fig. 1) is the consequence of plate subduction beneath the North Island of New Zcaland. ABSTRACT The thin continental crust (-15 km, Stem and Davey, 1987) spreads at rates up to 18 (Darby and Williams, 1991) Silicic calderas and geothermal systems in Taupo Volcanic in active rifting and subsidence. Since c. 1.6 Ma, the Zone (TVZ) of New Zealand are spatially related. Eight calderas, central TVZ has been the most frequently active and productive active since 1.6 Ma, occupy 45% of the Boundaries of region of rhyolitic volcanism on earth (Houghton et al., 1994). calderas arc often speculative, but of 20 geothermal systems producing an estimated 10 - 15 of rhyolite, and considercd, 15 occur on or next to a caldera margin where there is subordinate dacite, andesite and basalt. Debate continues whether enhanced deep permeability: the best examples are at Haroharo TVZ is a migrating andesitic arc and zone of asymmetric crustal where systems occur at the intersection of volcanic lineations and spreading (eg. Stem, or an andesite-dacite arc with bimodal caldera embayments, and at Rotorua. Drillhole evidence supports rhyolite-basalt back arc (eg. Cole, 1990). Whichever is the case, a realignment of caldera margin through the Wairakei- it is a matter of observation that most geothermal fields are geothermal field. Four geothermal systems have no known contained within the area of rhyolite volcanism. -
Exploring Submarine Arc Volcanoes Steven Carey University of Rhode Island, [email protected]
University of Rhode Island DigitalCommons@URI Graduate School of Oceanography Faculty Graduate School of Oceanography Publications 2007 Exploring Submarine Arc Volcanoes Steven Carey University of Rhode Island, [email protected] Haraldur Sigurdsson University of Rhode Island Follow this and additional works at: https://digitalcommons.uri.edu/gsofacpubs Terms of Use All rights reserved under copyright. Citation/Publisher Attribution Carey, S., and H. Sigurdsson. 2007. Exploring submarine arc volcanoes. Oceanography 20(4):80–89, https://doi.org/10.5670/ oceanog.2007.08. Available at: https://doi.org/10.5670/oceanog.2007.08 This Article is brought to you for free and open access by the Graduate School of Oceanography at DigitalCommons@URI. It has been accepted for inclusion in Graduate School of Oceanography Faculty Publications by an authorized administrator of DigitalCommons@URI. For more information, please contact [email protected]. This article has This been published in or collective redistirbution of any portion of this article by photocopy machine, reposting, or other means is permitted only with the approval of The approval portionthe ofwith any permitted articleonly photocopy by is of machine, reposting, this means or collective or other redistirbution SP ec I A L Iss U E On Ocean E X P L O R ATIO N Oceanography , Volume 20, Number 4, a quarterly journal of The 20, Number 4, a quarterly , Volume O ceanography Society. Copyright 2007 by The 2007 by Copyright Society. ceanography Exploring O ceanography Society. All rights All reserved. Society. ceanography O Submarine Arc Volcanoes or Th e [email protected] Send Society. ceanography to: correspondence all B Y S T even C A R E Y an D H A R A LDUR SIGURD ss O N Three quarters of Earth’s volcanic activ- although a significant part of arc volca- tion of tsunamis (Latter, 1981). -
The Taupo Eruption Sequence of AD 232±10 in Aotearoa New
地学雑誌 Journal of Geography(Chigaku Zasshi) 130(1)117141 2021 doi:10.5026/jgeography.130.117 The 100s: Significant Exposures of the World( No. 12) The Taupō Eruption Sequence of AD 232 ± 10 in Aotearoa New Zealand: A Retrospection * * David J. LOWE and Adrian PITTARI [Received 9 June, 2020; Accepted 13 August, 2020] Abstract The Taupō eruption, also known as eruption Y, occurred in late summer to early autumn (typically late March to early April) in AD 232 10 yr at Taupō volcano, an ‘inverse’ caldera volcano underlying Lake Taupō in the central Taupō Volcanic Zone, North Island, Aotearoa New Zealand. The complex rhyolitic eruption, the most powerful eruption globally in the last 5000 years, lasted between several days and several weeks and generated five markedly contrasting pyroclastic fall deposits( units Y1 to Y5) followed by the extremely violent emplacement of a low-aspect-ratio ignimbrite( unit Y6). The fall deposits include three phreatomagmatic units, Y1, Y3, and Y4, the latter two being the products of archetypal phreatoplinian events; and two magmatic units, Y2 and Y5, the latter being the product of an exceptionally powerful plinian (previously described as ‘ultraplinian’) event with an extreme magma discharge rate around 108 to 1010 kg s-1. The pyroclastic fall-generating eruptions were followed by the climactic emplace- ment of the entirely non-welded Taupō ignimbrite( Y6). It was generated by the catastrophic collapse of the 35 to 40-km-high plinian eruption column( Y5) that produced a very-fast-moving (600 to 900 km h-1), hot( up to 500°C) pyroclastic flow( density current) that covered about 20,000 km2 of central North Island over a near-circular area ~160 km in diameter, centred on Lake Taupō, in fewer than about ten to 15 minutes. -
Raised Marine Features, Radiocarbon Dates, and Sea Level Changes, Eastern Melville Peninsula, Arctic Canada’ L.A
ARCTIC VOL. 44, NO. 1 (MARCH 1991) R 63-73 Raised Marine Features, Radiocarbon Dates, and Sea Level Changes, Eastern Melville Peninsula, Arctic Canada’ L.A. DREDGE2 (Received 5 April 1990; accepted in revised form 9 October 1990) ABSTRACT. Radiocarbon dates from eastern Melville Peninsula indicatethat deglaciation of western Foxe Basin occurredabout 6900 years ago, although lateice persisted in an area northwest of Hall Lake and on the central plateau. Relative sea level was as high as 144 m above present at that time. ’ho new well-controlled sea level curves depict emergence as an exponential decay function. Marine limit elevations and nested curves indicate a major ice-loading centre in south-central Foxe Basin. Thesedata and archaeological dates suggest a secondary recent rebound centre in the northern part of the basin. Flights of raised beaches, prevalentin the area, are composed of angular limestone fragments and suggest that frost-riving occurs in shallow foreshore environments. The prominentwash line near the marine limit suggests that Foxe Basin had less sea ice cover prior to 6OOO years ago but that coastal processes have been similar to present since that time. Key words: Arctic, coasts, archaeology, radiocarbon dating, glacial history, emergence, sea level, geomorphology RESUMl?. Des datations au carbone radioactif dansla presqu’ile Melville orientale indiquent que la dbglaciation du Foxe bassin s’est produit vers 6900 ans, bien quela glace ait persist6 dans une zone situ& au nord-ouest du Lac etHall sur le plateau central.A cette bpoque, le niveau de la mer s’tlevait A 144 m au-dessus du niveau actuel. -
Educators Guide
EDUCATORS GUIDE 02 | Supervolcanoes Volcanism is one of the most creative and destructive processes on our planet. It can build huge mountain ranges, create islands rising from the ocean, and produce some of the most fertile soil on the planet. It can also destroy forests, obliterate buildings, and cause mass extinctions on a global scale. To understand volcanoes one must first understand the theory of plate tectonics. Plate tectonics, while generally accepted by the geologic community, is a relatively new theory devised in the late 1960’s. Plate tectonics and seafloor spreading are what geologists use to interpret the features and movements of Earth’s surface. According to plate tectonics, Earth’s surface, or crust, is made up of a patchwork of about a dozen large plates and many smaller plates that move relative to one another at speeds ranging from less than one to ten centimeters per year. These plates can move away from each other, collide into each other, slide past each other, or even be forced beneath each other. These “subduction zones” are generally where the most earthquakes and volcanoes occur. Yellowstone Magma Plume (left) and Toba Eruption (cover page) from Supervolcanoes. 01 | Supervolcanoes National Next Generation Science Standards Content Standards - Middle School Content Standards - High School MS-ESS2-a. Use plate tectonic models to support the HS-ESS2-a explanation that, due to convection, matter Use Earth system models to support cycles between Earth’s surface and deep explanations of how Earth’s internal and mantle. surface processes operate concurrently at different spatial and temporal scales to MS-ESS2-e form landscapes and seafloor features. -
Active Continental Margin
Encyclopedia of Marine Geosciences DOI 10.1007/978-94-007-6644-0_102-2 # Springer Science+Business Media Dordrecht 2014 Active Continental Margin Serge Lallemand* Géosciences Montpellier, University of Montpellier, Montpellier, France Synonyms Convergent boundary; Convergent margin; Destructive margin; Ocean-continent subduction; Oceanic subduction zone; Subduction zone Definition An active continental margin refers to the submerged edge of a continent overriding an oceanic lithosphere at a convergent plate boundary by opposition with a passive continental margin which is the remaining scar at the edge of a continent following continental break-up. The term “active” stresses the importance of the tectonic activity (seismicity, volcanism, mountain building) associated with plate convergence along that boundary. Today, people typically refer to a “subduction zone” rather than an “active margin.” Generalities Active continental margins, i.e., when an oceanic plate subducts beneath a continent, represent about two-thirds of the modern convergent margins. Their cumulated length has been estimated to 45,000 km (Lallemand et al., 2005). Most of them are located in the circum-Pacific (Japan, Kurils, Aleutians, and North, Middle, and South America), Southeast Asia (Ryukyus, Philippines, New Guinea), Indian Ocean (Java, Sumatra, Andaman, Makran), Mediterranean region (Aegea, Cala- bria), or Antilles. They are generally “active” over tens (Tonga, Mariana) or hundreds (Japan, South America) of millions of years. This longevity has consequences on their internal structure, especially in terms of continental growth by tectonic accretion of oceanic terranes, or by arc magmatism, but also sometimes in terms of continental consumption by tectonic erosion. Morphology A continental margin generally extends from the coast down to the abyssal plain (see Fig. -
Nitrogen Trading in Lake Taupo an Analysis and Evaluation of an Innovative Water Management Policy
Nitrogen Trading in Lake Taupo An Analysis and Evaluation of an Innovative Water Management Policy Madeline Duhon, Hugh McDonald and Suzi Kerr Motu Working Paper 15-07 Motu Economic and Public Policy Research June 2015 Author contact details Madeline Duhon Stanford University [email protected] Suzi Kerr Motu Economic and Public Policy Research [email protected] Hugh McDonald [email protected] Acknowledgements Special thanks to Colin Armer, George Asher, Sandra Barns, Mike Barton, Sharon Barton, Tim Bennetts, James Bowron, Graeme Fleming, Richard Gardiner, Suzie Greenhalgh, Mark Grinlinton, Natasha Hayward, Malcolm McLeod, Jon Palmer, Jocelyn Reeve, Alex Richardson, Gary Taylor, Geoff Thorp and Justine Young for their helpful insights and perspectives. Motu Economic and Public Policy Research PO Box 24390 Wellington New Zealand Email [email protected] Telephone +64 4 939 4250 Website www.motu.org.nz © 2014 Motu Economic and Public Policy Research Trust and the authors. Short extracts, not exceeding two paragraphs, may be quoted provided clear attribution is given. Motu Working Papers are research materials circulated by their authors for purposes of information and discussion. They have not necessarily undergone formal peer review or editorial treatment. ISSN 1176-2667 (Print), ISSN 1177-9047 (Online). i Abstract This paper provides an overview and early evaluation of the Lake Taupo nitrogen cap and trade programme, established as part of Waikato Regional Council’s 2011 Regional Plan Variation Five. The policy establishes a catchment-wide cap on nitrogen losses by allocating farmers individual nitrogen discharge allowances and allowing those farmers flexibility to trade allowances amongst themselves and to sell allowances to a public fund while remaining within the overall catchment cap.