Coastal Stability Report V9 Phase 1 FINAL
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Additions to Taranaki Inventory of Key Native Ecosystems January 2018
Campbells Bush At a glance TRC Reference: BD/9576 LENZ: C1.1a Chronically threatened Ecological District: Matemateaonga National: Priority 1 – Threatened Land Land Tenure: District Environment Regional: Key Native Ecosystem Area(ha): 1.4 Regional At risk 20-30% left GPS: 1720227X & 5633703Y Ecosystem Loss: Bioclimate Zone: Lowland Protection Status: Local Government Habitat: Forest Remnant Catchment: Tangahoe (348) Ecosystem Type MF7.3: Tawa, pukatea, podocarp forest General Description Campbell's Bush is located on Sangster Road, Rawhitiroa, approximately 8kms east of Eltham in central Taranaki. The forest remnant is located within the Matemateaonga Ecological District and lies in the Tangahoe River catchment. Campbell's Bush is a small (1.4ha) lowland forest remnant owned by the South Taranaki District Council as a Scenic Reserve. The bush remnant is only 900 metres west of the Rotokare Scenic Reserve and is within the Rotokare Reserve Trust 'halo' management area. Ecological Features Flora The high canopy at Campbell’s Bush is dominated by pukatea, tawa and swamp maire with occasional rewarewa and titoki. The understory is recovering well including species such as kawakawa, kanono, pigeonwood, mahoe and turepo and has become dense in places. Native ferns are well established in places and are establishing wider including shining spleenwort, sickle spleenwort, hen and chicken fern etc. Swamp maire (Regionally Distinctive) is present in good numbers and is notable for this site. Fauna The reserve will definitely be receiving spill over from the predator fenced Lake Rotokare Scenic Reserve and also benefiting from the halo pest animal control programme in this area. Tui were generally in numbers higher than usual for a small site. -
Circulation and Mixing in Greater Cook Strait, New Zealand
OCEANOLOGICA ACTA 1983- VOL. 6- N" 4 ~ -----!~- Cook Strait Circulation and mixing Upwelling Tidal mixing Circulation in greater Cook S.trait, Plume Détroit de Cook Upwelling .New Zealand Mélange Circulation Panache Malcolm J. Bowrnan a, Alick C. Kibblewhite b, Richard A. Murtagh a, Stephen M. Chiswell a, Brian G. Sanderson c a Marine Sciences Research Center, State University of New York, Stony Brook, NY 11794, USA. b Physics Department, University of Auckland, Auckland, New Zealand. c Department of Oceanography, University of British Columbia, Vancouver, B.C., Canada. Received 9/8/82, in revised form 2/5/83, accepted 6/5/83. ABSTRACT The shelf seas of Central New Zealand are strongly influenced by both wind and tidally driven circulation and mixing. The region is characterized by sudden and large variations in bathymetry; winds are highly variable and often intense. Cook Strait canyon is a mixing basin for waters of both subtropical and subantarctic origins. During weak winds, patterns of summer stratification and the loci of tidal mixing fronts correlate weil with the h/u3 stratification index. Under increasing wind stress, these prevailing patterns are easily upset, particularly for winds b1owing to the southeasterly quarter. Under such conditions, slope currents develop along the North Island west coast which eject warm, nutrient depleted subtropical water into the surface layers of the Strait. Coastal upwelling occurs on the flanks of Cook Strait canyon in the southeastern approaches. Under storm force winds to the south and southeast, intensifying transport through the Strait leads to increased upwelling of subsurface water occupying Cook Strait canyon at depth. -
Taranaki-Whanganui Conservation Board Notice of Appeal
To The ReGistrar of the HiGh Court at WellinGton and To The Respondent and To The Applicant and To Other submitters This document notifies you that: 1 The appellant, being the Taranaki-WhanGanui Conservation Board (Conservation Board), will move the HiGh Court at WellinGton by way of appeal against the decision of the majority decision of the decision making committee of the Environmental Protection Authority (DMC), dated 3 AuGust 2017, public notice #EEZ000011, in which a marine consent and marine discharge consent was granted to Trans-Tasman Resources Limited (TTRL). The Application and Decision 2 TTRL applied for marine consents and marine discharge consents to enable it to mine iron sands in the South Taranaki BiGht, 22-36km offshore (Application). Up to 50 million tonnes of seabed material could be mined and processed each year, for up to 35 years. 3 The Environmental Protection Authority (EPA) made its decision on the application through its DMC (Decision). The DMC’s Decision was split. Two of the DMC’s members considered that the consents should be refused. They took the view that: … overall the localised adverse environmental effects on the Patea Shoals and tangata whenua existing interests are unacceptable, and are not avoided, remedied or mitigated by the conditions imposed. We also have concerns reGardinG uncertainty and the adequacy of environmental protection within the coastal marine area (CMA).1 4 However, the Chair held the castinG vote, and exercised it in favour of granting consent. Accordingly, the “majority decision” was to grant consent. 5 The DMC made its Decision on 3 August 2017. -
Blue Whale Ecology in the South Taranaki Bight Region of New Zealand
Blue whale ecology in the South Taranaki Bight region of New Zealand January-February 2016 Field Report March 2016 1 Report prepared by: Dr. Leigh Torres, PI Assistant Professor; Oregon Sea Grant Extension agent Department of Fisheries and Wildlife, Marine Mammal Institute Oregon State University, Hatfield Marine Science Center 2030 SE Marine Science Drive Newport, OR 97365, U.S.A +1-541-867-0895; [email protected] Webpage: http://mmi.oregonstate.edu/gemm-lab Lab blog: http://blogs.oregonstate.edu/gemmlab/ Dr. Holger Klinck, Co-PI Technology Director Assistant Professor Bioacoustics Research Program Oregon State University and Cornell Lab of Ornithology NOAA Pacific Marine Environmental Laboratory Cornell University Hatfield Marine Science Center 159 Sapsucker Woods Road 2030 SE Marine Science Drive Ithaca, NY 14850, USA Newport, OR 97365, USA Tel: +1.607.254.6250 Email: [email protected] Collaborators: Ian Angus1, Todd Chandler2, Kristin Hodge3, Mike Ogle1, Callum Lilley1, C. Scott Baker2, Debbie Steel2, Brittany Graham4, Philip Sutton4, Joanna O’Callaghan4, Rochelle Constantine5 1 New Zealand Department of Conservation (DOC) 2 Oregon State University, Marine Mammal Institute 3 Bioacoustics Research Program, Cornell Lab of Ornithology, Cornell University 4 National Institute of Water and Atmospheric Research, Ltd. (NIWA) 5 University of Auckland, School of Biological Sciences Research program supported by: The Aotearoa Foundation, The National Geographic Society Waitt Foundation, The New Zealand Department of Conservation, The Marine Mammal Institute at Oregon State University, The National Oceanographic and Atmospheric Administration’s Cooperative Institute for Marine Resources Studies (NOAA/CIMRS), Greenpeace New Zealand, OceanCare, Kiwis Against Seabed Mining, and an anonymous donor. -
Retrieval of Suspended Sediment Concentration in Near-Shore Coastal Waters Using MODIS Data
Copyright is owned by the Author of the thesis. Permission is given for a copy to be downloaded by an individual for the purpose of research and private study only. The thesis may not be reproduced elsewhere without the permission of the Author. Retrieval of suspended sediment concentration in near-shore coastal waters using MODIS data A thesis presented in partial fulfilment of the requirements for the degree of Master of Philosophy In Earth Science At Massey University, Palmerston North New Zealand Di Zhou 2012 1 Abstract: This study focuses on using remote sensing satellite data to retrieve water suspended sediment concentration (SSC) of near-shore coastal waters. Aqua/Terra Satellite MODIS 250m data of the south-western coast of the North Island, New Zealand was used. Two methods of analysis are used in this study to obtain an SSC map; non-liner optimisation and quasi-analytical. The non-linear optimisation method was used to fit an exponential function between reflectance and SSC, with SSC replaced by a linear relationship between SSC and reflectance in the near infrared domain. The optimisation result was used to convert Aqua/Terra MODIS images to SSC maps. The quasi-analytical method, a backscattering coefficient at 645nm is first derived from Aqua/Terra MODIS 250m Band 1 data using a quasi-analytical algorithm after applying a simple atmospheric correction routine. An empirical relationship was derived from laboratory experiments. Finally SSC maps were obtained by applying the empirical relationship to convert the backscattering coefficient to SSC. 2 Acknowledgements I would firstly like to thank my supervisor Mike Tuohy for his time and thoughtful advice throughout the preparation of this thesis. -
Appendix C – Geotechnical Assessment
Appendix C – Geotechnical Assessment Whanganui District Council Mill Road Structure Plan Geotechnical Assessment October 2017 Table of contents 1. Introduction ............................................................................................................................... 3 1.1 Introduction ..................................................................................................................... 3 1.2 Scope of this report ......................................................................................................... 3 1.3 General Site Setting ........................................................................................................ 3 2. Published Geological Information .............................................................................................. 4 2.1 Geology .......................................................................................................................... 4 2.2 Earthquakes .................................................................................................................... 5 2.3 Known Active Faults ........................................................................................................ 6 2.4 Liquefaction Susceptibility ............................................................................................... 6 2.5 Slope Stability ................................................................................................................. 6 2.6 Site Sub-Soil Class ......................................................................................................... -
Seabed Mining (KASM), Posted a Facebook Page Inviting People to Turn up at the Stadium When Hearings Began
MINING MINEFIELD A company called Trans-Tasman Resources is having a second go at setting up a world-first project to mine iron ore from the seabed off South Taranaki’s coast. The company (TTR) has spent a decade and about $70 million to hone its case for Environmental Protection Authority (EPA) consent to take more than a billion tonnes of iron- bearing sand off the sea floor over 25 or so years. The process – which will return 90 percent of what’s extracted back to the seabed - will bring in about $400 million a year in off-shore ore sales, with our government getting about $6 million in annual royalties. The project is expected to increase Taranaki’s gross domestic product by about $220 million a year (half that of Methanex) and create about 300 jobs. Sound like a good deal? Somewhere between 13,733 and about 17,000 people (the total is disputed) don’t think so. Many people living in South Taranaki and further afield, local iwi, most of the fishing industry, and a close-neighbour oil company are worried about what it might do to the environment and local communities. That uncertainty has prompted their representative organisations and many individuals to fight the company to the bitter end. The case will be a precedent-setter under the Exclusive Economic Zone (EEZ) Act. Environmentalists don’t like the law, partly because it excludes climate change-causing emissions as grounds for objection, and partly because they reckon it’s the National government’s way of opening up our 200 kilometre-wide continental shelf to big overseas business. -
The Evolution of the Rural Settlement Pattern Of
THE EVOLUTION OF THE RURAL SETTLEMENT PATTERN OF LOWLAND SOUTH TARAN.AKI 1860 - 1920 BEING A THESIS presented to UNIVERSITY OF CANTERBURY IN PARTIAL FULFILMENT of the requirements for the Degree of MASTER OF ARTS in Geography By G.I. RAWSON 1967 CONTENTS Page CHAPTER ONE: INTRODUCTION 1 Aim Sources Method Physical Setting References CHAPTER TWO: THE BEGININGS OF SETTLEMENT 11 (a) The Settlement Pattern 1868-1870 The Need For Security The ITilTllaturity Of Settlement The Pattern Was A Simple One (b) The 1870's - Some Continuing Themes Settlement Characteristics The Position Of The Maori Government Influence Increased Regional Identity References CHAPTER THREE: THE OCCUPATION OF THE BUSHLANDS 25 The Demand For Land Government Assistance The Prog+ess of Settlement References CHAPTER FOUR: SOUTH TARANAKI 1884-1886 33 (a) Where The People Were (b) The Farming Scene The Established Farms1 The Bush Farms First Attempts At Dairying (c) Some Continuing Themes References CHAPTER FIVE: THE GROWTH OF DAIRYING 1886-1920 49 Initial Difficulties Initiative Taken By The Farmers The Role Of The Entrepreneur Progress To 1893 1893-1920 - The Final Developments References CHAPTER SIX: THE PATTERN COMPLETED - SOUTH TA.RA.NAKI 64 In 1920 CHAPTER SEVEN: SUMMARY AND CONCLUSIONS 69 ANNOTATED BIBLIOGRAPHY 73 FIGURES: Following Page Fig. 1 SOUTH TARAN.AKI 1868 - 1870 14 Fig. 2 SOUTH TARAN.AKI 1884 - 1886 34 Fig. 3 THE EXPANSION OF DAIRYING - 1888 - 1920 54 Fig. 4 SOUTH TARAN.AKI 1920 65 Fig. 5 TOPOGRAPHICAL MAPS In End Pocket J;>LATES: Following Page PLATE ONE: The Waimate Plains 6 PLATE TWO: The Waingongoro Valley 6 PLATE THREE: Undulating Land near Eltham 7 PLATE FOUR: The Hurleyville area 7 PLATE FIVE: The Fringes of The Hill Country 39 PLATE SIX: A Raupo Whare In The 1880 1 s 39 PLATE SEVEN: The Manutahi Area 58 PLATE EIGHT: Kakaramea 58 PLATE NINE: The Fraser Road Dairy Factory 67 PLATE TEN: Unimproved Land Near Eltham 67 Unless otherwise acknowledged all photographs were taken by the author. -
Lake Rotorangi Water-Quality and Biological State of the Environment Report
State of the Environment Monitoring of Lake Rotorangi water quality and biological programme Annual Report 2013-2014 Technical Report 2014-22 ISSN: 0114-8184 (Print) Taranaki Regional Council ISSN: 1178-1467 (Online) Private Bag 713 Document: 1420188 (Word) STRATFORD Document: 1460601 (Pdf) March 2015 Executive summary Consents 0488 and 0489, originally granted to Egmont Electricity Ltd (then held by Powerco Ltd and more recently transferred to TrustPower Ltd) for the Patea Dam, required water quality and biological monitoring of Lake Rotorangi and lake level monitoring. At the time of granting the consents (1978) a Tribunal recognised that a recreational lake resource of regional importance would be formed but at the same time the potential existed for a range of adverse environmental impacts to occur. Monitoring programmes and reports had continued since 1984. The report covering the 2010-2011 period (the twenty-first annual report) was the final report in this format, with subsequent lake water quality monitoring reported as a state of the environment annual report, in part financed by TrustPower. The consent holder lodged renewal applications in late 2007. The renewal process which continued through the 2008-2009 period, culminated in a formal hearing in June 2009 followed by appeals with subsequent, on-going, mediation during 2009-2010. The new consents became operative in mid December 2010 with considerable changes in conditions and associated monitoring requirements. A NIWA consultant's report concerning trends in Lake Rotorangi water quality, commissioned by Council during the 1995-96 monitoring year, confirmed earlier monitoring reports' conclusions and identified minor adjustments and additions to future programmes to enable long term trend monitoring to be performed in accordance with State of the Environment monitoring requirements. -
Consents & Regulatory Committee Agenda October 2017
Consents and Regulatory Committee Tuesday 17 October 2017 9.30am Taranaki Regional Council, Stratford Consents and Regulatory Committee - Agenda Agenda for the meeting of the Consents and Regulatory Committee to be held in the Taranaki Regional Council chambers, 47 Cloten Road, Stratford, on Tuesday 17 October 2017 commencing at 9.30am. Members Councillor M P Joyce (Committee Chairperson) Councillor M J Cloke Councillor M G Davey Councillor C L Littlewood Councillor M J McDonald Councillor B K Raine Councillor N W Walker Councillor D L Lean (ex officio) Councillor D N MacLeod (ex officio) Representative Mr H Eriwata (Iwi Representative) Members Mr K Holswich (Iwi Representative) Ms F Mulligan (Iwi Representative) Apologies Notification of Late Items Opening Karakia Item Page Subject Item 1 5 Confirmation of Minutes Item 2 11 Resource consents issued under delegated authority and applications in progress Item 3 32 Report on five applications for notified consents - Fonterra Limited Whareroa Site Item 4 157 Appointment of Hearing Commissioner - New Zealand Transport Agency Item 5 160 Consent monitoring annual reports and case study 'Live Water Quality Monitoring' - moving forward with the latest technology 2 Consents and Regulatory Committee - Agenda Item 6 191 Incident, Compliance, Monitoring Non-compliances and Enforcement Summary Item 7 223 Public Excluded Item 8 224 Confirmation of Confidential Minutes 3 Consents and Regulatory Committee - Opening Karakia Whakataka te hau Karakia to open and close meetings Whakataka te hau ki te uru Cease the winds from the west Whakataka te hau ki tonga Cease the winds from the south Kia mākinakina ki uta Let the breeze blow over the land Kia mātaratara ki tai Let the breeze blow over the ocean Kia hī ake ana te atakura Let the red-tipped dawn come with a sharpened air He tio, he huka, he hauhu A touch of frost, a promise of glorious day Tūturu o whiti whakamaua kia tina. -
Temporal and Spatial Lags Between Wind, Coastal Upwelling, and Blue Whale Occurrence Dawn R
www.nature.com/scientificreports OPEN Temporal and spatial lags between wind, coastal upwelling, and blue whale occurrence Dawn R. Barlow1*, Holger Klinck2,3, Dimitri Ponirakis2, Christina Garvey4 & Leigh G. Torres1 Understanding relationships between physical drivers and biological response is central to advancing ecological knowledge. Wind is the physical forcing mechanism in coastal upwelling systems, however lags between wind input and biological responses are seldom quantifed for marine predators. Lags were examined between wind at an upwelling source, decreased temperatures along the upwelling plume’s trajectory, and blue whale occurrence in New Zealand’s South Taranaki Bight region (STB). Wind speed and sea surface temperature (SST) were extracted for austral spring–summer months between 2009 and 2019. A hydrophone recorded blue whale vocalizations October 2016-March 2017. Timeseries cross-correlation analyses were conducted between wind speed, SST at diferent locations along the upwelling plume, and blue whale downswept vocalizations (D calls). Results document increasing lag times (0–2 weeks) between wind speed and SST consistent with the spatial progression of upwelling, culminating with increased D call density at the distal end of the plume three weeks after increased wind speeds at the upwelling source. Lag between wind events and blue whale aggregations (n = 34 aggregations 2013–2019) was 2.09 ± 0.43 weeks. Variation in lag was signifcantly related to the amount of wind over the preceding 30 days, which likely infuences stratifcation. This study enhances knowledge of physical-biological coupling in upwelling ecosystems and enables improved forecasting of species distribution patterns for dynamic management. A central pursuit of ecology is to decipher and understand the complex relationships between biological organ- isms and their physical environment. -
Trustpower Ltd Patea Hydro Scheme Monitoring Report
Trustpower Limited Patea Hydroelectric Power Scheme Monitoring Programme Report 2011-2014 Technical Report 2014-88 ISSN: 0144-8184 (Print) Taranaki Regional Council ISSN: 1178-1467 (Online) Private Bag 713 Document: 1459012 (Word) STRATFORD Document: 1480530 (Pdf) April 2015 Executive summary Trustpower Limited (the Company) operates a hydroelectric power station located on the Patea River on Maben Road, near Hurleyville. Water is impounded behind the 82m high Patea Dam to form Lake Rotorangi. This water is diverted through the 30 MW power station, the largest in Taranaki. This report for the period July 2011–June 2014 describes the monitoring programme implemented by the Taranaki Regional Council (the Council) to assess the Company’s environmental performance during the period under review, and the results and environmental effects of the Company’s activities. The Company holds 10 resource consents, which include a total of 146 conditions setting out the requirements that the Company must satisfy. The Company holds three consents to allow it to dam, take and/or use water, two consents to discharge water into the Patea River, three consents for structures associated with the scheme and two consents to discharge emissions into the air at this site. During the monitoring period, Trustpower Limited demonstrated an overall level of environmental performance that required improvement. The Council’s monitoring programme for the period under review included seven inspections and two hydrological gaugings. In addition, analysis of generation data, lake level data, Patea River flow and groundwater abstraction data, provided by the Company, was conducted. The Council also reviewed numerous reports submitted in accordance with consent conditions.