WRC Flood Protection and Drainage Schemes
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Waikato District Council
WAIKATO DISTRICT COUNCIL Report and Decisions of the Waikato District Plan Hearings Panel REPORT 2 Ohinewai Rezoning 24 May 2021 Commissioners Dr Phil Mitchell (Chair) Mr Paul Cooney (Deputy Chair) Mr Dynes Fulton Mr Weo Maag Page | 1 Decision Report 2: Ohinewai Rezoning Report and Decisions of the Waikato District Plan Hearings Panel Page | 2 Decision Report 2: Ohinewai Rezoning Report and Decisions of the Waikato District Plan Hearings Panel TABLE OF CONTENTS 1 Introduction ................................................................................................................................... 5 2 The APL submission ...................................................................................................................... 9 3 Statutory and planning framework ............................................................................................ 15 4 Site suitability and physical characteristics ............................................................................... 18 5 Three Waters Infrastructure ...................................................................................................... 20 6 Natural hazards ........................................................................................................................... 24 7 Transport and traffic ................................................................................................................... 26 8 Economic effects ......................................................................................................................... -
2016 Pilot Waikato River Report Card: Methods and Technical Summary
2016 Pilot Waikato River Report Card: Methods and Technical Summary Prepared for Waikato River Authority March 2016 2016 Pilot Waikato River Report Card: Methods and Technical Summary Prepared by: Bruce Williamson (Diffuse Sources) John Quinn (NIWA) Erica Williams (NIWA) Cheri van Schravendijk-Goodman (WRRT) For any information regarding this report please contact: National Institute of Water & Atmospheric Research Ltd PO Box 11115 Hamilton 3251 Phone +64 7 856 7026 NIWA CLIENT REPORT No: HAM2016-011 Report date: March 2016 NIWA Project: WRA14203 Quality Assurance Statement Reviewed by: Dr Bob Wilcock Formatting checked by: Alison Bartley Approved for release by: Bryce Cooper Photo: Waikato River at Wellington Street Beach, Hamilton. [John Quinn, NIWA] 2016 Pilot Waikato River Report Card: Methods and Technical Summary Contents Summary ............................................................................................................................ 9 Reflections from the Project Team ..................................................................................... 12 1 Introduction ............................................................................................................ 18 1.1 Report Cards ........................................................................................................... 18 1.2 2015 Pilot Waikato River Report Cards .................................................................. 20 1.3 Purpose of this Technical Summary ....................................................................... -
Mercer Airport – Submitter #921 – Hearing Highlights Package
Mercer Airport – Submitter #921 – Hearing Highlights Package Chris Dawson - Planning 1.1 The correct approach under the RMA is to determine what district plan provisions (or zone) most appropriately assist Waikato District Council to carry out its functions to achieve the purpose of the Act. The critical evaluation is set out in s32 of the Act which determines determine the efficiency and effectiveness of the proposed provisions in achieving the objectives of the Proposed Waikato District Plan (PDP). 1.2 Mercer Airport requires a special zone to recognise that it is already a regionally significant aviation resource and should be formally protected in the District Plan as such. The rezoning, plus Obstacle Limitation Surfaces1 and Air Noise Boundary2 provisions are required to protect that facility and provide it with the operational certainty to grow over time in the future. 1.3 The most appropriate time to provide the statutory protection for the airport and the surrounding community is now before the Mercer area gets more developed than it already is. The implementation of a Special Zone for Mercer Airport is essential to ensure that the Proposed Waikato District Plan is consistent with the relevant higher order documents, specifically the Operative Waikato Regional Policy Statement Policy 6.3 and Method 6.3.1. 1.4 The policy direction of the Rural Zone is a relevant consideration under s32 of the Act, and Lens 2 of the s42A Framework report because that zone informs the existing environment and will continue to be applied over the -
Historic Overview - Pokeno & District
WDC District Plan Review – Built Heritage Assessment Historic Overview - Pokeno & District Pokeno The fertile valley floor in the vicinity of Pokeno has most likely been occupied by Maori since the earliest days of their settlement of Aotearoa. Pokeno is geographically close to the Tamaki isthmus, the lower Waikato River and the Hauraki Plains, all areas densely occupied by Maori in pre-European times. Traditionally, iwi of Waikato have claimed ownership of the area. Prior to and following 1840, that iwi was Ngati Tamaoho, including the hapu of Te Akitai and Te Uri-a-Tapa. The town’s name derives from the Maori village of Pokino located north of the present town centre, which ceased to exist on the eve of General Cameron’s invasion of the Waikato in July 1863. In the early 1820s the area was repeatedly swept by Nga Puhi war parties under Hongi Hika, the first of several forces to move through the area during the inter-tribal wars of the 1820s and 1830s. It is likely that the hapu of Pokeno joined Ngati Tamaoho war parties that travelled north to attack Nga Puhi and other tribes.1 In 1822 Hongi Hika and a force of around 3000 warriors, many armed with muskets, made an epic journey south from the Bay of Islands into the Waikato. The journey involved the portage of large war waka across the Tamaki isthmus and between the Waiuku River and the headwaters of the Awaroa and hence into the Waikato River west of Pokeno. It is likely warriors from the Pokeno area were among Waikato people who felled large trees across the Awaroa River to slow Hika’s progress. -
Waikato District Plan Review Archaeological Heritage Project Phase V
Waikato District Plan Review Archaeological Heritage Project Phase V Dr Alexy Simmons Simmons & Associates Ltd. November 2016 Executive Summary Waikato District Council is currently drafting a new District Plan and is required to recognise and provide for the protection of New Zealand's historic heritage under the Resource Management Act 1991. To accomplish this task a multi-phased WDC Archaeological Heritage Project was commissioned. The information included in this report relates to Phase V of the project. Phase V of the project entails the review and updating of ten archaeological sites that have been scheduled in the operative Waikato District Plan and the Franklin District Plan. The sites are reviewed using the Waikato Regional Council heritage criteria included in the Regional Policy Statement. The other task addressed in this Phase V report is the review of the three ‘Battlefield Viewshafts’ in Appendix C2 of the operative Waikato District Plan. 1 Simmons & Associates Ltd. November 2016 Contents Executive Summary ................................................................................................................ 1 Introduction ............................................................................................................................. 5 Background Information on the Archaeological Heritage Project .................................. 5 Definition of an Archaeological Site ................................................................................. 6 Purpose of Phase V ................................................................................................................ -
Mapping the Socio- Political Life of the Waikato River MARAMA MURU-LANNING
6. ‘At Every Bend a Chief, At Every Bend a Chief, Waikato of One Hundred Chiefs’: Mapping the Socio- Political Life of the Waikato River MARAMA MURU-LANNING Introduction At 425 kilometres, the Waikato River is the longest river in New Zealand, and a vital resource for the country (McCan 1990: 33–5). Officially beginning at Nukuhau near Taupo township, the river is fed by Lake Taupo and a number of smaller rivers and streams throughout its course. Running swiftly in a northwesterly direction, the river passes through many urban, forested and rural areas. Over the past 90 years, the Waikato River has been adversely impacted by dams built for hydro-electricity generation, by runoff and fertilisers associated with farming and forestry, and by the waste waters of several major industries and urban centres. At Huntly, north of Taupiri (see Figure 6.1), the river’s waters are further sullied when they are warmed during thermal electricity generation processes. For Māori, another major desecration of the Waikato River occurs when its waters are diverted and mixed with waters from other sources, so that they can be drunk by people living in Auckland. 137 Island Rivers Figure 6.1 A socio-political map of the Waikato River and catchment. Source: Created by Peter Quin, University of Auckland. As the Waikato River is an important natural resource, it has a long history of people making claims to it, including Treaty of Waitangi1 claims by Māori for guardianship recognition and management and property rights.2 This process of claiming has culminated in a number of tribes 1 The Treaty of Waitangi was signed by the British Crown and more than 500 Māori chiefs in 1840. -
Waikato and Waipā River Restoration Strategy Isbn 978-0-9922583-6-8
WAIKATO AND WAIPĀ RIVER RESTORATION STRATEGY ISBN 978-0-9922583-6-8 ISBN 978-0-9922583-7-5 (online) Printed May 2018. Prepared by Keri Neilson, Michelle Hodges, Julian Williams and Nigel Bradly Envirostrat Consulting Ltd Published by Waikato Regional Council in association with DairyNZ and Waikato River Authority The Restoration Strategy Project Steering Group requests that if excerpts or inferences are drawn from this document for further use by individuals or organisations, due care should be taken to ensure that the appropriate context has been preserved, and is accurately reflected and referenced in any subsequent spoken or written communication. While the Restoration Strategy Project Steering Group has exercised all reasonable skill and care in controlling the contents of this report, it accepts no liability in contract, tort or otherwise, for any loss, damage, injury or expense (whether direct, indirect or consequential) arising out of the provision of this information or its use by you or any other party. Cover photo: Waikato River. WAIKATO AND WAIPĀ RIVER RESTORATION STRATEGY TE RAUTAKI TĀMATA I NGĀ AWA O WAIKATO ME WAIPĀ RESTORATION STRATEGY FOREWORD HE KUPU WHAKATAKI MŌ TE RAUTAKI TĀMATA FROM THE PARTNERS MAI I TE TIRA RANGAPŪ Tooku awa koiora me oona pikonga he kura tangihia o te maataamuri. The river of life, each curve more beautiful than the last. We are pleased to introduce the Waikato and Waipā River Restoration Strategy. He koanga ngākau o mātou nei ki te whakarewa i te Rautaki Tāmata i ngā Awa o Waikato me Waipā. This document represents an exciting new chapter in our ongoing work to restore and protect the health and wellbeing of the Waikato and Waipā rivers as we work towards achieving Te Ture Whaimana o Te Awa o Waikato, the Vision & Strategy for the Waikato River. -
Notes on the Hydrology of the Waikato River
EARTH SCIENCE JOURNAL, Vol. 1, No. 1, 1967 NOTES ON THE HYDROLOGY OF THE W AIKATO RIVER G. T. Ridall Hydrologist, Waikato Valley Authority GENERAL The catchment area of the Waikato River is 5,500 square miles. If its source is accepted as being the Upper Waikato, then its distance to the sea at Port Waikato including its journey through Lake Taupo is 266 miles. It rises, together with the Whangaehu, the Rangitikei and the Wanganui, between the volcanic region of Ruapehu 9,000 ft. above sea level and the Kaimanawa Ranges 5,000 ft. above sea level. The river flows northwards for 34 miles into Lake Taupo, losing its identity into the Tongariro for the last 26 miles to the lake. It emerges from Lake Taupo resuming its proper name and, still flowing northwards, passes for more than 100 miles through a series of lakes formed by hydro- electric dams to Cambridge. From here it continues through a deeply incised channel to Ngaruawahia where it is joined by its major tributary, the Waipa River. From Ngaruawahia to the mouth, a distance of 60 miles, shallow lakes and peat swamps predominate on both sides of the river, many of them protected and drained and developed into rich dairy farms. From Mercer, 35 miles downstream of Ngaruawahia, where slight tidal effects are discernable at low flows, the river changes its general northerly direction to a westerly one and, still 9 miles from the mouth, enters the delta. Here it is fragmented into many channels before emptying into the broad expanse of Maioro Bay and finally emerges by two fairly narrow channels into the sea on the west coast, 25 miles south of Manukau Heads. -
Notice Concerning Copyright Restrictions
NOTICE CONCERNING COPYRIGHT RESTRICTIONS This document may contain copyrighted materials. These materials have been made available for use in research, teaching, and private study, but may not be used for any commercial purpose. Users may not otherwise copy, reproduce, retransmit, distribute, publish, commercially exploit or otherwise transfer any material. The copyright law of the United States (Title 17, United States Code) governs the making of photocopies or other reproductions of copyrighted material. Under certain conditions specified in the law, libraries and archives are authorized to furnish a photocopy or other reproduction. One of these specific conditions is that the photocopy or reproduction is not to be "used for any purpose other than private study, scholarship, or research." If a user makes a request for, or later uses, a photocopy or reproduction for purposes in excess of "fair use," that user may be liable for copyright infringement. This institution reserves the right to refuse to accept a copying order if, in its judgment, fulfillment of the order would involve violation of copyright law. A GIA, pe Agenda item II.A.2 (b) GEOTHERMAL POWER DEVELOPMENT AT WAIRAKEI, NEW ZEALAND H. Christopher H. Armstead * New Zealand's goethermal power scheme at an earlier project, now abandoned, to install a Wairakei has been generating power since November chemical distillation plant at Wairakei, taking steam 1958. The load carried is 65 MW or more, and outputs at 50 lb/sq in. gauge and exhausting at * lb/sq in. up to 101 million kWh per week have been generated, gauge. This plant, which was to have been combined equivalent to about 12 per cent of the total energy with topping sets on the upstream side and condens- production in North Island. -
Sedimentation
IN THE MATTER of the Resource Management Act 1991 AND IN THE MATTER of a Board of Inquiry appointed under s149J of the Resource Management Act 1991 to determine an application for resource consents sought by Watercare Services Limited for its Waikato River Take and Discharge Proposal. STATEMENT OF EVIDENCE OF SELENE ALEXANDRA CONN ON BEHALF OF WATERCARE SERVICES LIMITED Sedimentation 1. Introduction, Qualifications and Experience 1.1 My name is Selene Alexandra Conn. I am a Technical Director for fluvial geomorphology and an ecologist (specialising in riparian and wetland vegetation) at Tonkin and Taylor Limited, based in Tauranga. I have been employed by Tonkin and Taylor Limited for three years and seven months. 1.2 I hold the following qualifications relevant to this assessment: (a) Bachelor of Science (Biology and Geography (2007), Bachelor of Science Honours (Geography (2008), Master of Science (Geography (2009) from the University of Auckland. (b) I have been a Certified Environmental Practitioner (#1219) since 2018, and received the Geomorphology Specialisation Accreditation (#001) in February 2021. I am currently the vice chair of the New Zealand Rivers Group, a technical interest group of Engineering New Zealand, and have been on the committee since 2017. 1.3 I have eleven years’ experience in the fields of ecology and fluvial geomorphology. Prior to my role at Tonkin and Taylor, I was a senior ecologist at Wildland Consultants based in Tauranga specialising in wetland and riparian vegetation surveys and stream habitat enhancement plans. Between 2012 and 2016, I was employed as an environmental scientist at Alluvium Consulting in Townsville, Australia specialising in riparian vegetation surveys, riparian planting plans for large scale waterway diversions and geomorphic assessments for a range of clients and project objectives. -
A Directory of Wetlands in New Zealand
A Directory of Wetlands in New Zealand WAIKATO CONSERVANCY Lower Waikato River and Estuary (10) Location: Rangiriri, 37°26'S, 175°08'E; centre of delta, 37°21'S, 174°46'E. The Lower Waikato River is approximately 34 km southwest of the city of Auckland at Port Waikato and 72 km south of the city of Auckland at Rangiriri, North Island. Area: Lower Waikato River, c.3,500 ha (56 km from Rangiriri to Port Waikato); estuary c.588 ha. Altitude: Sea level to 10 m at Rangiriri. Overview: The Waikato River, between Rangiriri and Port Waikato, passes through large areas of mineralised swamp and shallow lakes, and finally discharges through a diverse delta habitat to the sea. It provides habitat for a range of threatened bird species, and supports New Zealand's largest eel fishery. Physical features: The site comprises the Lower Waikato River from Rangiriri downstream for about 56 km to Port Waikato at its mouth. The basement rocks of the Waikato Region are comprised of Mesozoic "greywacke-type" rocks that have undergone extensive alteration to form dissected fault blocks around the perimeter of the Waikato catchment. During the early Tertiary, coal measures with associated freshwater and shallow marine sediments were laid down, although today many have been removed by erosion. Following this period, a series of several different phases of volcanism occurred. As a result of extensive sediment deposition at this time, the Waikato River, which previously flowed out to the Firth of Thames, changed course to flow out into the Hamilton Basin, bringing much sediment with it and causing extensive deposition and creating small lakes and swamps. -
Hearing 22 Infrastructure Waikato District Council Transpower Ne
BEFORE THE HEARINGS PANEL Under the Resource Management Act 1991 In the matter of The Proposed Waikato District Plan - Hearing 22 Infrastructure Between Waikato District Council And Transpower New Zealand Limited (Submission S576 and FS1350) Statement of Evidence in Chief of Dougall Campbell for Transpower New Zealand Limited dated 29 September 2020 Executive Summary 1. Transpower New Zealand Limited (Transpower) operates the National Grid, which transmits electricity throughout New Zealand. The National Policy Statement on Electricity Transmission 2008 (NPSET) requires the National Grid to be appropriately recognised in the Proposed Waikato District Plan (the “Proposed Plan”). The Proposed Plan must give effect to the NPSET. 2. This means that the Proposed Plan must include provisions to recognise and provide for the national significance of the National Grid, manage the effects of the National Grid, and manage effects of the National Grid. Transpower adopts a thorough and systematic approach to planning for and establishing new National Grid assets. While a resilient National Grid remains at the heart of New Zealand’s energy future, climate change has become a central issue for governments globally and hence for Transpower as a responsible owner and operator of the National Grid on behalf of New Zealanders. 3. With regard to managing the effects of land use and development on the National Grid, corridors around the National Grid are necessary to: a) Ensure the network can be efficiently operated, maintained, developed and upgraded by providing the working and access space to do this; b) Manage reverse sensitivity effects; c) Ensure sensitive activities are generally not provided for in the area directly under lines; and d) Protect the safety of both the National Grid and people working or living close to it.