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Regional Plan for the Tarawera River Catchment
Environment Bay of Plenty P O Box 364 Whakatane NEW ZEALAND Environmental Publication 2003/24 ISSN: 1175-9372 REGIONAL PLAN FOR THE TARAWERA RIVER CATCHMENT 1 February 2004 Environment Bay of Plenty Bay of Plenty Regional Council 1 February 2004 Tarawera River Catchment Plan Reader’s Guide READER’S GUIDE There may be some parts of this regional plan that you are interested in reading. To find these parts quickly, the following guide gives a brief summary of what each chapter is about. Chapter 1 - Introduction: Names the regional plan, outlines its purpose and aims, discusses topics and issues to be managed, the geographical area of the plan, and sets its duration. Chapter 2 - Preparation of the Regional Plan for the Tarawera River Catchment: Provides a summary of how the regional plan was prepared, research undertaken and the people and organisations consulted. Chapter 3 - Statutory Framework: Outlines the primary parts or sections of the Resource Management Act 1991 relevant to the preparation of the regional plan. It also includes definitions of “Issues”, “Objectives”, “Policies”, and “Methods”. Chapter 4 - Policy Framework: Establishes how this regional plan relates to other planning documents at the national, regional and district level. Chapter 5 - Responsibilities: Identifies the principle local body and governmental organisations with resource management responsibilities, and gives a brief resume of their primary functions and duties. Chapter 6 - Physical Description of the Tarawera Catchment: Provides background information on the area covered by the regional plan. Discusses the Tarawera River catchment in four sub-areas, namely the Tarawera Lakes and their catchments, the catchment of the Upper Reach of the Tarawera River, the catchment of the Lower Reach of the Tarawera River, and the Tarawera River mouth. -
Effects of Industry on Maori Cultural Values: the Case of the Tarawera River
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Research Commons@Waikato Effects of Industry on Maori Cultural Values: The Case of the Tarawera River: Materoa Dodd Abstract The research is a case study of the relationship between three tribes; Te Arawa, Tuwharetoa ki Kawerau and Ngāti Awa and the Tarawera River during the second half of the 20th century when the river was polluted with effluent from pulp and paper mills. It involves the cultural story of the Tarawera River as told by the iwi (tribes) of the river informed by Maori epistemologies and what has come to be known as a ‗kaupapa Maori research' approach. Reference is made to the history, legends, customs and lifestyle that have arisen from the Materoa Dodd is of Ngati Awa and Ngai Te Rangi descent. relationship between iwi and the river. It includes comments on the pollution of the river from My background is political, socio-cultural and economic members of each iwi. The world views, experiences, and perceptions reported on here have development. I specialise in monitoring international forced a fundamental change on the iwi, a change that has affected their cultural and social development trends and their impact on nation-state relationship to the river. The price of economic development on the river has been cultural economies and indigenous populations. and ecological genocide. The cultural voice echoes a familiar story in indigenous communities. In the Maori context I work as a Senior Lecturer in Development Studies at Waikato the research provides opportunities for further inquiry into determining the socio-cultural, University and conduct Nation Building research about post - economic and political future of the iwi of the river. -
The Ngati Awa Raupatu Report
THE NGATI AWA RAUPATU REPORT THE NGAT I AWA RAUPATU REPORT WA I 46 WAITANGI TRIBUNAL REPORT 1999 The cover design by Cliä Whiting invokes the signing of the Treaty of Waitangi and the consequent interwoven development of Maori and Pakeha history in New Zealand as it continuously unfolds in a pattern not yet completely known A Waitangi Tribunal report isbn 1-86956-252-6 © Waitangi Tribunal 1999 Edited and produced by the Waitangi Tribunal Published by Legislation Direct, Wellington, New Zealand Printed by PrintLink, Wellington, New Zealand Text set in Adobe Minion Multiple Master Captions set in Adobe Cronos Multiple Master LIST OF CONTENTS Letter of transmittal. ix Chapter 1Chapter 1: ScopeScopeScope. 1 1.1 Introduction. 1 1.2 The raupatu claims . 2 1.3 Tribal overlaps . 3 1.4 Summary of main åndings . 4 1.5 Claims not covered in this report . 10 1.6 Hearings. 10 Chapter 2: Introduction to the Tribes. 13 2.1 Ngati Awa and Tuwharetoa . 13 2.2 Origins of Ngati Awa . 14 2.3 Ngati Awa today . 16 2.4 Origins of Tuwharetoa. 19 2.5 Tuwharetoa today . .20 2.6 Ngati Makino . 22 Chapter 3: Background . 23 3.1 Musket wars. 23 3.2 Traders . 24 3.3 Missionaries . 24 3.4 The signing of the Treaty of Waitangi . 25 3.5 Law . 26 3.6 Principles of the Treaty of Waitangi. 28 Chapter 4: The Central North Island Wars . 33 4.1 The relevance of the wars to Ngati Awa. 33 4.2 Conclusion . 39 Chapter 5: The Völkner And Fulloon Slayings . -
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. -
An Introductory Review
1 Citation: Lowe, D.J. 2010. Quaternary volcanism, tephras, and tephra-derived soils in New Zealand: an introductory review. In: Lowe, D.J.; Neall, V.E., Hedley, M; Clothier, B.; Mackay, A. 2010. Guidebook for Pre-conference North Island, New Zealand „Volcanoes to Oceans‟ field tour (27-30 July). 19th World Soils Congress, International Union of Soil Sciences, Brisbane. Soil and Earth Sciences Occasional Publication No. 3, Massey University, Palmerston North, pp. 7-29. Quaternary volcanism, tephras, and tephra-derived soils in New Zealand: an introductory review David J. Lowe Department of Earth and Ocean Sciences, University of Waikato, Hamilton Introduction This two-part article comprises brief introductions to (1) volcanism and its products in general and to the broad pattern of Quaternary volcanism and tephrostratigraphy in North Island, and (2) the ensuing tephra-derived soils of North Island. Part 1 derives mainly from Smith et al. (2006), Leonard et al. (2007), and Lowe (2008a). Other useful reviews include those of Neall (2001), Graham (2008: Chapter 7), Wilson et al. (2009), and Cole et al. (2010). Recent reviews on tephras include Shane (2000), Alloway et al. (2007), Lowe (2008b, 2011), and Lowe et al. (2008a, 2008b). A history of tephra studies in New Zealand was reported by Lowe (1990). Part 2 describes the distribution and character of the main tephra-derived soils, these being Entisols and Andisols (mostly Vitrands and Udands) and Ultisols (Lowe and Palmer, 2005). Books on these and other soils in New Zealand include NZ Soil Bureau (1968), Gibbs (1980), McLaren and Cameron (1996), Cornforth (1998), and Molloy and Christie (1998). -
Scanned Using the Fujitsu 6670 Scanner and Scandall Pro Ver 1.7
Ngati Awa Claims Settlement Bill Government Bill Explanatory note General policy statement This Bill . records the acknowledgements and apology given by the Crown to Ngati Awa in the deed of settlement dated 27 March 2003 between the Crown and Ngati Awa; and . gives effect to the deed of settlement in which the Crown and Ngati Awa agree to a final settlement of all the Ngati Awa historical claims. Scope of settlement Ngati Awa are located in Eastern Bay of Plenty and have approxi- mately 13 000 members. In the deed of settlement, and in this Bill, Ngati Awa have been defined as the descendants of- • Awanuiarangi II; and • people who exercised customary interests at any time after 6 February 1840 in the Ngati Awa area of interest. The settlement settles all of the historical claims of Ngati Awa. Those claims include all claims that are, or are founded on, a right arising- • from the Treaty of Waitangi (Te Tiriti o Waitangi) or the principles of the Treaty of Waitangi (Te Tiriti o Waitangi): • under legislation or at common law (including in relation to aboriginal title or customary law): • from fiduciary duty: • otherwise; and 175-1 2 Ngati Awa Claims Settlement Explanatory note that arise from, or relate to, acts or omissions before 21 September 1992-- • by, or on behalf of, the Crown; or • by, or under, legislation. The Crown is released and discharged from all obligations and liabilities in respect of those claims. History of the claim In 1988 the Crown, in accordance with its policy of devolution to iwi authorities and at the request of Ngati Awa, enacted Te Runanga o Ngati Awa Act 1988 establishing the Te Runanga o Ngati Awa. -
Part 2 Geological History.Indd
2. Geological History Activities Curriculum Curriculum Environmental Page Activity title level link education aspect 2a Formation of the L 3–5 Science 37 Rotorua lakes 2b Silent Card Shuffl e L 3–5 Science 39 2c Mt Ngongotaha L 3–5 Science About, In 42 2d Looking at Sediment Any level Science About, In 53 2e How Wet is your Any level Science 55 Sediment? 2f What is in your L 5 Science 58 Sediment? Relevant resources: • Rotorua’s Volcanic Past – video – hire from Rotorua Public Library • Rotorua Museum Education Resources » Te Arawa – Mai Maketu ki Tongariro » Legends, Landforms and Learning » Tarawera photo kit » Tarawera Resource kit • Pollution Busters newsletter # 5 Volcanoes • Learning Media - Building Science Concepts • Book 12 – Volcanoes: Hot Rock in a Cool World Levels: 3–4 • Book 52 – The Land Changes: Keeping Earth’s Systems in Balance: Levels: 3–4 • Learning Media – Readers » The Changing Land, Jane Buxton, ISBN 0478214162, explores how the elements can affect Earth and change its shape The Rotorua Lakes Education Resource 35 Activity 2a Formation of the Rotorua Lakes Curriculum links Science Any level 2 Resources required Science • PowerPoint presentation by Will Esler, University of Waikato (on CD) • The Life and Times of Lake Rotorua and Lake Rotoiti (see background notes) • Graphic of Rotorua lake edge 9000 years ago Method 1 View the PowerPoint (ppt) before using it with the class, or set a small group this responsibility. Identify good stopping places for discussion or questions. Have some questions already identifi ed e.g. What was the signifi cant event during this time? Why was it signifi cant? Who/what was responsible for this event occurring? If a small group has previewed the ppt then they can act as a lead questioner/facilitator for one of the groups below. -
Aspects of the Chronology, Structure and Thermal History of the Kawerau Geothermal Field
Aspects of the Chronology, Structure and Thermal History of the Kawerau Geothermal Field By Sarah Dawn Milicich A thesis submitted to Victoria University of Wellington in fulfilment of the requirements for the degree of Doctor of Philosophy in Geology Victoria University of Wellington School of Geography, Environment and Earth Sciences Wellington, New Zealand 2013 ii „It is what it is‟ id est quod est J.L. Wooden (pers. comm. 2010) iii iv ABSTRACT The development and management of high-temperature geothermal resources for electrical power generation requires accurate knowledge of the local geological conditions, particularly where they impact on the hydrology of the resource. This study is an integrated programme of work designed to develop new perspectives on the geological and structural framework of the Kawerau geothermal resource as a sound basis for field management. Although the geological approaches and techniques utilised in this study have previously been used, their application to an integrated study of a geothermal system in New Zealand has not been previously undertaken. Correlating volcanic and sedimentary stratigraphy in geothermal areas in New Zealand can be challenging due to similarities in lithology and the destruction of distinctive chemical, mineralogical and textural characteristic by hydrothermal alteration. A means to overcoming these issues is to utilise dating to correlate the stratigraphy. Zircons are resistant to the effects of typical hydrothermal conditions and were dated using SIMS techniques (SHRIMP-RG) to retrieve U–Pb ages on zircons. These age data were then used to correlate units across the field, in part aided by correlations to material that had previously been dated from fresh rock by 40Ar/39Ar techniques, and used to redefine the stratigraphic framework for the area. -
The Tarawera Forest Report
Downloaded from www.waitangi-tribunal.govt.nz THE TARAWERA FOREST REPORT Downloaded from www.waitangi-tribunal.govt.nz Downloaded from www.waitangi-tribunal.govt.nz Downloaded from www.waitangi-tribunal.govt.nz Downloaded from www.waitangi-tribunal.govt.nz THE TARAWERA FOREST REPORT WA I 4 11 WAITANGI TRIBUNAL REPORT 2003 Downloaded from www.waitangi-tribunal.govt.nz Downloaded from www.waitangi-tribunal.govt.nz The cover design by Cliff Whiting invokes the signing of the Treaty of Waitangi and the consequent interwoven development of MaoriandPakehahistoryinNewZealandasitcontinuously unfolds in a pattern not yet completely known A Waitangi Tribunal report isbn 1-86956-268-2 www.waitangi-tribunal.govt.nz Typeset by the Waitangi Tribunal Published by Legislation Direct, Wellington, New Zealand Printed by SecuraCopy, Wellington, New Zealand Set in Adobe Minion and Cronos multiple master typefaces Downloaded from www.waitangi-tribunal.govt.nz Downloaded from www.waitangi-tribunal.govt.nz CONTENTS Letter of transmittal . xiii Chapter1:TheClaims,Issues,andTreatyPrinciples 1.1 Introduction . 1 1.2 Claims’ relationship with eastern Bay of Plenty inquiry . 4 1.3 Wai 411 . 7 1.4 Wai 46. 12 1.5 Wai 872 . 13 1.6 The Crown’s response to the claims . 15 1.7 Issues for the Tribunal . 19 1.8 Relevant Treaty principles . 20 1.9 Summary . 32 Chapter2:TheContextfortheClaims 2.1 Introduction . 33 2.2 Crown policy for Maori land development . 33 2.3 Crown forestry development policy . 44 2.4 Tasman Pulp and Paper Company Limited . 49 2.5 Summary . 53 Chapter3:DevelopingtheJoint-Venture Proposal from 1960 to 1964 3.1 Introduction . -
Kawerau District Council
Candidate Info Pack Kawerau District Council Chief Executive Officer July 2017 Contents Page Number Background 3 The District & Getting There 4 Community Profile 5 Mayor & Councillors 6 The Council 7 2 Kawerau District Council Background Kawerau is the heart of the Bay of Plenty, is central to everything and nestles within the Tarawera valley at the foot of the dramatic Putauaki (Mt Edgecumbe), a volcano that became dormant about 1000 years ago. The town was founded in 1953 as a mill town, making it one of New Zealand’s youngest towns. The District has a total population of 6,800 and is renowned for its friendliness, great sense of community, a wonderful climate and a strong Maori heritage. The Kawerau District is home to some of the most pure natural resources in the country, with its fascinating geothermal activity, the beautiful Tarawera falls and river, and the wetlands which the town was built upon. These resources are embraced by the community, and have become the real strength in the District for both the industry and tourism sectors’. Although it contains a small population and land mass, Kawerau has a heritage of tenacity, innovation and progressiveness. The District’s economy continues to grow and thrive with the ongoing strength of the industrial sector, while tourism remains a real focus for the Council, showcasing the true beauties of Kawerau. Kawerau is known for its friendly people and strong community spirit. The strength of its multicultural background is a proud characteristic of the town, as is the richness of its Maori heritage. Although small on landmass, Kawerau is only a short drive away from some of New Zealand’s most picturesque places and attractions there is to offer. -
Ngati Rangitihi Story Chapter 3
Ngati Rangitihi Story Chapter 3 D R A F T October 2016 Chapter 3: Ngati Rangitihi Lands After 1840 ....................................................................... 1 3.1 The Ngati Rangitihi Rohe Potae .............................................................................. 1 3.2 The Te Ariki Fighting, 1853–1854 .......................................................................... 4 3.3 The Confiscation of Ngati Rangitihi Lands, 1866 ................................................. 11 3.3.1 Confiscated Lands Returned to Ngati Rangitihi, 1866–1872 .......................... 16 3.3.2 Ngati Rangitihi Grants for Military Service .................................................... 20 3.3.3 Crown Purchase of Pukeroa ............................................................................ 21 3.3.4 Other Ngati Rangitihi Titles in the Confiscation District ................................ 26 3.4 Ngati Rangitihi Inland Blocks ................................................................................ 28 3.4.1 Haehaenga ....................................................................................................... 30 3.4.2 Kaingaroa 1 ..................................................................................................... 40 3.4.2.1 Early Private Leasing of Kaingaroa ......................................................... 41 3.4.2.2 Crown Leasing of Kaingaroa ................................................................... 45 3.4.2.3 Title Investigation, 1878-1879 ................................................................ -
Walking and Hiking in Rotorua Bay of Plenty This Publication Is Produced by Department of Conservation and Destination Rotorua
Walking and hiking in Rotorua Bay of Plenty This publication is produced by Department of Conservation and Destination Rotorua February 2017 Editing and design: DOC Publishing Team This publication is produced using paper sourced from well-managed, renewable and legally logged forests. All photos, unless otherwise credited, are copyright DOC. Cover photo: Walkers enjoying Redwoods walk. Photo: Adrian Hodge Contents Introduction 1 Visitor information 2 Keeping you and the environment safe 2 Fire and other emergencies 2 Geothermal hazards 2 Aquatic pests 3 Information for walkers and hikers 4 Track classifications 4 Essential gear 5 Plan and prepare 5 Camping 6 Hunting 6 Fishing 6 Restrictions 7 Dog exercise areas 7 Maps 7 For the whole family ... 8 Close to the city 8 New Zealand birds a plenty 8 Magnificent water 8 Geothermal action 9 Native Ōkataina 9 Tracks and reserves 12 Lake Tikitapu Scenic Reserve 12 Lake Ōkareka 14 Mount Ngongotaha Scenic Reserve 15 Hamurana Springs Recreation Reserve 16 Okere Falls Scenic Reserve 17 Rainbow Mountain Scenic Reserve 20 Lake Rotoiti Scenic Reserve 23 Lake Rotoma Scenic Reserve 25 Lake Okataina Scenic Reserve 26 Longer walks in Lake Okataina Scenic Reserve 29 Lake Tarawera Scenic Reserve 31 Camping around Lake Tarawera 34 Walks and tracks around Tarawera 34 Lake Rotomahana Wildlife Refuge 38 Kaharoa Conservation Area 39 Mangorewa Ecological Area 40 Mokaihaha Ecological Area 43 Te Waihou 44 Nau mai, haere mai ki te rohe o Te Waiāriki Welcome to the Rotorua Lakes area. White water rafting at Okere Falls. Photo: Kaitiaki Adventures Introduction Rotorua is a paradise for walkers and hikers.