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Water Resource Use a Matter of Perspective: a Case Study of The
WATER RESOURCE USE A MATTER OF PERSPECTIVE: A CASE STUDY OF THE KAITUNA RIVER CLAIM, WAITANGI TRIBUNAL a thesis submitted in partial fulfilment of the requirements for the degree of MASTER OF ARTS IN GEOGRAPHY in the university of canterbury . by. TIMOTHY W fRASER 1988 contents ACKNOWLEDGEMENTS iii LIST OF FIGURES, PLATES AND TABLES v LIST OF MAPS vi ABS1RACT vii CHAPTER PAGE one INTRODUCTION 1.1 Introduction .............................................. 1 1.2 A Case Study for Bicultural Research ............... .. 6 1.3 Thesis Structure ................................. .. 10 two THE SEWAGE DISPOSAL PROBLEM OF ROTORUA CITY: THE KAITUNA RIVER CLAIM 2.1 Introduction ........................................................ 14 2.2 The Problem ........................................................ 15 2.3 A General Response ........._...................................... 24 2.4. The Kaituna River Claim Waitangi Tribunal.................... 32 2.5 Options Pursued After the Waitangi Tribunal Hearing........ 38 2.6 Concluding Remarks .. .. .. .. ... .. .. .. .. .. ... ... 40 three A DOMINANT CULTURAL PERSPECTIVE: THE ENGINEERING SOLUTION 3.1 Introduction ........................................................ 42 3.2 Roots of a Technological Perspective .......................... 43 3.3 Rise of the Engineer .............................................. 47 3.4 Developing a Water Resource Use Strategy ................... 52 ii 3.5 Water and Soil Legislation: 1941 and 1967 ................... 55 3.6 The Dominant Perspective Challenged ........................ -
Anglers' Notice for Fish and Game Region Conservation
ANGLERS’ NOTICE FOR FISH AND GAME REGION CONSERVATION ACT 1987 FRESHWATER FISHERIES REGULATIONS 1983 Pursuant to section 26R(3) of the Conservation Act 1987, the Minister of Conservation approves the following Anglers’ Notice, subject to the First and Second Schedules of this Notice, for the following Fish and Game Region: Eastern NOTICE This Notice shall come into force on the 1st day of October 2017. 1. APPLICATION OF THIS NOTICE 1.1 This Anglers’ Notice sets out the conditions under which a current licence holder may fish for sports fish in the area to which the notice relates, being conditions relating to— a.) the size and limit bag for any species of sports fish: b.) any open or closed season in any specified waters in the area, and the sports fish in respect of which they are open or closed: c.) any requirements, restrictions, or prohibitions on fishing tackle, methods, or the use of any gear, equipment, or device: d.) the hours of fishing: e.) the handling, treatment, or disposal of any sports fish. 1.2 This Anglers’ Notice applies to sports fish which include species of trout, salmon and also perch and tench (and rudd in Auckland /Waikato Region only). 1.3 Perch and tench (and rudd in Auckland /Waikato Region only) are also classed as coarse fish in this Notice. 1.4 Within coarse fishing waters (as defined in this Notice) special provisions enable the use of coarse fishing methods that would otherwise be prohibited. 1.5 Outside of coarse fishing waters a current licence holder may fish for coarse fish wherever sports fishing is permitted, subject to the general provisions in this Notice that apply for that region. -
Heading/Title Aquatic Pest Report 2019
Aquatic Pest Report 2019 Bay of Plenty Regional Council Environmental Publication 2019/03 FebruaryHeading/title 2019 PreparedSubheading by Freya Ewing and Thomas Bailey (Summer Students) 5Month Quay YearStreet P O Box 364 WhakatānePrepared by NEW ZEALAND ISSN: 1175-9372 (Print) ISSN: 1179-9471 (Online) Cover photo: Rowan Wells (NIWA) Acknowledgements We would like to thank Hamish Lass, Biosecurity Officer for his support and guidance, and Lucas MacDonald, Biosecurity Officer for his assistance and advice across all advocacy work. Our acknowledgements also go to Greg Corbett and the remainder of the Biosecurity Team at the Bay of Plenty Regional Council, we are grateful for the encouragement and support we received from all of you. We would also like to show our gratitude to Geoff Ewert for his continued commitment to the Rotorua Lakes, in particular with fixing weed cordons and the running of the boat wash station. We are also immensely grateful to Sarah Van Der Boom from Freshwater Biosecurity Partnership Program for her help with data collection. Lastly, we would like to thank Sam Beaumont and the remainder of the team at Ministry for Primary Industries, for the supplying of merchandise and collateral, signage and guidance. BAY OF PLENTY REGIONAL COUNCIL TOI MOANA 1 Executive summary Many of New Zealand’s most well-known lakes and rivers can be found in the Bay of Plenty region and are therefore known to attract significant visitor numbers annually. The preservation and protection of these waterways are what attracts so many international and domestic tourists to them. Due to the close proximity of the Bay of Plenty lakes and rivers, and their popularity, they are extremely susceptible to invasive pest species. -
The Sedimentation and Drainage History of Haroharo Caldera and the Tarawera River System, Taupo Volcanic Zone, New Zealand
The Sedimentation and Drainage History of Haroharo Caldera and The Tarawera River System, Taupo Volcanic Zone, New Zealand Prepared by K A Hodgson and I A Nairn Environment Bay of Plenty Operations Publication 2004/03 August 2004 5 Quay Street P O Box 364 Whakatane NEW ZEALAND ISSN 1176 - 5550 Working with our communities for a better environment Environment Bay of Plenty i Acknowledgements The Department of Conservation (Rotorua Lakes Office) permitted our studies in lake and river reserves. Fletcher Challenge Forests (and its successors) provided detailed contour maps and aerial photographs. Bryan Davy and Hugh Bibby (GNS) provided a pre- publication copy of their paper on seismic imaging in Lake Tarawera. PGSF Contract IANX0201 funded this study. Sedimentation and Drainage History, Tarawera River System Operations Publication 2004/03 Environment Bay of Plenty iii Executive Summary Haroharo caldera has been formed by the coalescence of multiple collapse structures over the last 350 kyr, the latest major collapse accompanying voluminous rhyolite pyroclastic eruptions at ~50 ka. The caldera has formed a sink for precipitation on surrounding catchments, with overflow via the Tarawera River through the Whakatane graben to the sea at ~30 km to NE. Lakes have probably always occupied at least part of the caldera floor, but the early lacustrine history is largely obscured by younger eruptives. Since 26 ka, the Haroharo, Okareka, Rotoma and Tarawera volcanic complexes have grown within the caldera during eleven eruption episodes, confining ten lakes on the caldera margins. Growth of the volcanic complexes has greatly altered drainage paths and ponding areas within and marginal to the caldera, so that the present ~700 km2 caldera catchment area is about half the ~1400 km2 area that drained into the caldera between 26 ka and 9.5 ka. -
THE NEW ZEALAND GAZETTE No
1384' THE NEW ZEALAND GAZETTE No. 39 In Bankruptcy-Supreme Court Rogers, Hugh Arthur, 87 Clinkard Avenue, Rotorua, NOTICE is hereby given that dividends are payable at my workman. B. 64/74. office on all proved claims in the under-mentioned estate: Rowley, Henry Byers, 7 Pukeko Street, Rotorua, con crete worker. B. 62/76. Paaka Joe Teoti, formerly of 30 Chesney Court, Inver Sale, Graham John, 18 Brents Road, Rotorua, builder. cargill, labourer, now of 254 Crinan Street, Invercargill, B. 12/75. first and final dividend of I 00 cents in the dollar. Sale, William Hall, 18 Brents Road, Rotorua, builder. W. E. OSMAND, Official Assignee. B. 29/74. Saunders, Barry Francis, 753 Main Road, Mount Maun Supreme Court, Invercargill. ganui, dredgehand. B. 37 /75. Snowden, William, 61 Bellingham Crescent, Rotorua, millhand. B. 4/75. IN BANKRUPTCY-IN THE SUPREME COURT AT Tapu, Kenneth Daniel, 18 Seymour Place, Tauranga, ROTORUA driver. B. 25 /74. Te Torno, Leonard Robert Puhanga, 61 Wallace Crescent, NOTICE is hereby given that statements of accounts in respect Rotorua, unemployed commercial cleaner. B. 60/75. of the under-mentioned estates together with the report of the Thomas, William Halsey, 121 Oregon Drive, Murupara, Audit Office thereon, have been duly filed in the above bush supervisor. B. 19/74. Court; and I hereby further give notice that at the sitting of the Court, to be held on Friday, the 19th day of May 1978, Dated at Hamilton, this 3rd day of May 1978. I intend to apply for an order releasing me from the admin A. -
REPOROA, NEW ZEALAND Gregory Bignall
251 Proc 12th New Zealand Geothermal Workshop 1990 Bignall HYDROLOGY AND HYDROTHERMAL ALTERATION, REPOROA WELL (1), REPOROA, NEW ZEALAND Gregory Bignall Geothermal Institute, University of Auckland, Private Bag, Auckland ABSTRACT The Opaheke-Reporoa thermal system has surface activity that consists of hot, neutral alkali chloride-bicarbonatepools; minor sinter, mudpools; steaming ground and hot water seepage. Regional resistivity measurements and fluid chemistry surveys suggest that the Reporoa system is a lateral outflow of hot water from the Waiotapu Geothermal System to the north-east. A deep exploratory drillhole, encountered a sequence of lacustrine sediments, volcanic, tuffaceous and ignimbritic rocks. The well was discharged in October 1966, but was shut down after 5 hours during which time wellhead pressure fell from to Downhole temperatures in were measured after 47 days of heating and showed a significanttemperature inversion between and which is interpreted to be caused by hot water at about depth flowing above a cooler water influx. The temperature interpretation from clay and calc-silicate mineralogy and calculated chemical geothermometers is consistent with the bore hole temperatures. A minor maximum of occurred at 305m (interlayered illite-smectite encountered),a minimum of at 549m (smectite),and a maximum of at 853m to 975m (illite + rare epidote), o : bottom hole temperaturewas /a A Intensity of hydrothermal alteration generally increases with depth below about with the mineral assemblage of quartz, albite, adularia, titanite, illite, chlorite and calcite 40 produced by near neutral chloride-bicarbonate fluid. The scarcity of epidote and absence of wairakite and other calc- Figure 1 Location of the Reporoa geothermal area, Taupo silicate minerals is consistent with alteration by a geothermal Volcanic Zone, North Island, New Zealand. -
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. -
Lake Ōkareka 21
Contents Purpose 1 Overview 1 Lake Rotorua 2016-2017 1 Lake Rotoehu 2016-2017 3 Lake Rotoiti 2016-2017 3 Lake Ōkāreka 2016-2017 3 Key achievements 5 Rotorua Te Arawa Lakes Annual Water Quality Results 10 Lake Rotorua 13 Lake Rotoehu 17 Lake Rotoiti 19 Lake Ōkareka 21 Actions and Outcomes for Non Deed Lakes 23 Communications and stakeholder engagement update 26 Science update 27 Land Technical Advisory Group 27 Water Quality Technical Advisory Group 27 Rotorua Te Arawa Lakes Programme – DRAFT Annual Report 2016-2017 i Environmental modelling 28 Action Plans and sewage reticulation 28 Financials 29 Rotorua Te Arawa Lakes Programme – DRAFT Annual Report 2016-2017 ii Purpose The purpose of this document is to report progress against the 2016-2017 Annual Work Programme of the Rotorua Te Arawa Lakes Programme (the Programme), for the year ending 30 June 2017. This report is in accordance with Clause 5.1 and 5.2 of Deed of Funding with the Crown, for the Programme. In this report, progress made on individual interventions is reported against the Annual Work Programme commitments. The overarching goal of the Deed of Funding Agreement is to meet community aspirations for water quality in the four Deed Funded lakes: Rotoiti, Rotorua, Ōkāreka and Rotoehu. Each of these lakes has a target water quality set by the community in the Bay of Plenty Regional Water and Land Plan. This target water quality is set by Trophic Level Index (TLI) and this report provides an update on the status of water quality across the Rotorua Te Arawa Lakes, against the targets set for all lakes, Deed and non-Deed funded. -
Water Flow Between Ohau Channel and Lake Rotoiti Following Implementation of the Diversion Wall Part B
Water flow between Ohau Channel and Lake Rotoiti following implementation of the diversion wall Part B CBER Contract Report 116 Prepared for Bay of Plenty Regional Council By David P. Hamilton, Wendy Paul, Chris McBride and Dirk Immenga Centre for Biodiversity and Ecology Research The University of Waikato Private Bag 3105 Hamilton, 3240 New Zealand 2010 1 Table of contents Figures ................................................................................................................................. 3 Tables .................................................................................................................................. 5 Executive Summary ............................................................................................................ 6 Background ..................................................................................................................... 9 Water temperature ........................................................................................................ 13 Discussion ......................................................................................................................... 27 Acknowledgments ............................................................................................................. 29 References ......................................................................................................................... 30 Front cover – Photo of diversion wall taken by Wendy Paul 2 Figures Figure 1. ........................................................................................................................... -
Silvicultural Proposals for Radiata Pine on High Quality Sites R
SILVICULTURAL PROPOSALS FOR RADIATA PINE ON HIGH QUALITY SITES R. T. FENTON and W. R. J. SUTTON* SYNOPSIS An evaluation of current production thinning in radiata pine grown on high quality sites indicates that it has failed to increase realizable volumes, provide adequate intermediate returns (suf ficient to compensate for the loss of growth on the final crop trees) or significantly improve selection and quality of the final crop trees. An alternative, and potentially more profitable regime is pro posed which eliminates any production thinning for major produce by reducing the stand to the final crop in two stages (to 150 s.p.a. at 35 ft, and to 80 s.p.a, at 55 ft). This regime, designed to maintain near-maximum growth on the final crop trees, is expected to produce trees of mean d.b.h. 22 to 23 inches in 25 to 26 years on sites of Index 95 ft. The regime aims to produce board grades only. PRODUCTION THINNING IN RADIATA PINE Management of both private companies and the Forest Service almost invariably prescribes production-thinning, and often, second-log pruning. The clearfelling of untended stands prescribed on steep country — for pulpwood of radiata pine (Pinus radiata D. Don) (Fenton and Grainger, 1965) and for Douglas fir (Pseudotsuga menziesii Mirb. Franco) (Fenton, 1967a) — were exceptions. (Another was the modification of Schedule B proposed by Bunn, Familton and Fenton to the Forest Research Institute meeting on Thinning and Pruning — Bunn, 1963). Pulpwood crops without production thinning — based on the assumption ". that little would be gained by planting at a greater rate than the sustained yield annual cut . -
Evolving Community Response to Tourism and Change in Rotorua
Evolving Community Response To Tourism and Change in Rotorua Chrys Horn Researcher, Human Sciences Division, Lincoln University. [email protected] David G Simmons Professor of Tourism, Human Sciences Division, Lincoln University. [email protected] John R Fairweather Principal Research Officer in the Agribusiness and Economics Research Unit, Lincoln University. [email protected] February 2000 ISSN 1174-670X Tourism Research and Education Centre (TREC) Report No. 14 Lincoln University Contents LIST OF TABLES vi LIST OF FIGURES viii ACKNOWLEDGEMENTS x SUMMARY xii CHAPTER 1 INTRODUCTION...................................................................................1 1.1 Introduction....................................................................................1 1.2 Report Structure .............................................................................3 CHAPTER 2 METHODS..............................................................................................5 2.1 Qualitative Methods.......................................................................5 2.2 Quantitative Survey........................................................................6 2.3 Weighting.......................................................................................9 2.4 Presentation....................................................................................9 2.5 Limitations of Research ...............................................................10 CHAPTER 3 THE ROTORUA CONTEXT: HISTORY AND SOCIAL PATTERNS..........................................................................................11 -
Formation of the Sport of Athletics in Rotorua
Lake City Athletic Club Inc A History by Pam Kenny Three clubs joined together in April 1991, to form the current Lake City Athletic Club Inc. A short history of the earlier clubs is shown first. Rotorua Amateur Athletic & Cycling Club / Rotorua Athletic Club 1931-1991 On the 13 November 1931 a meeting was convened at Brent’s Bathgate House to establish an athletic and cycling club in Rotorua. Thirty people were in attendance and the Rotorua Amateur Athletic and Cycling Club was formed, with the club achieving incorporated society status in 1938. Blue and gold were the club colours - blue singlet/blouse and shorts with gold “R” on the top. Weekly competitions were held at the Rotorua Boys High on a Friday evening, with the customary track and field events for the runners, with cyclists contesting both track and road races. Val Robinson winning an early ladies’ athletics meeting in the late 1940's The club went into recess during the Second World War, with activities resuming October 1944. Venues utilized between 1944 and 1960 were Harriers in the late 1940's - L to R; John Wild, Alex Kuirau Park, the old A&P Showgrounds near Uta Millar, Keith French, Harry Findon Street, Arawa Park, Pererika Street, and again Kuirau Park. 1961 saw the Club at Smallbone Park, its home until the 1983/84 season, when a move was made to the new International Stadium, though the inadequacy of the track led to a return to Smallbone Park for a season. 1986 it was back to the Stadium until sand carpeting of the ground prevented permanent lane markings and children being able to run barefooted.