Leslie–Karamea Track Brochure
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Statement of Evidence: Paul Williams: Proposed Mokihinui Hydro
BEFORE THE ENVIRONMENT COURT AT CHRISTCHURCH ENV-2010-CHC-115, 123, 124 AND 135 IN THE MATTER of Appeals pursuant to Section 120 of the Resource Management Act 1991 BETWEEN WEST COAST ENT INC Appellant AND ROYAL FOREST AND BIRD PROTECTION SOCIETY OF NEW ZEALAND INC Appellant AND WHITE WATER NEW ZEALAND INC Appellant AND DIRECTOR GENERAL OF CONSERVATION Appellant AND WEST COAST REGIONAL COUNCIL AND BULLER DISTRICT COUNCIL Respondents ....Continued over leaf _____________________________________________________ STATEMENT OF EVIDENCE OF PAUL WORTHING WILLIAMS FOR DIRECTOR-GENERAL OF CONSERVATION Dated: 13 May 2012 _____________________________________________________ _____________________________________________________ Department of Conservation, West Coast Tai o Poutini Conservancy Private Bag 701, Sewell Street HOKITIKA Ph 03 756 9100 Fax 03 756 9188 Counsel Acting: A Cameron, D van Mierlo 2 AND MERIDIAN ENERGY LIMITED Applicant AND FRIDA INTA Section 274 Party AND WHANAU PIHAWAI WEST – RICHARD WAYNE BARBER AND IRI MAY BARBER MILNER Section 274 Party AND J MacTAGGART Section 274 Party AND ORION ENERGY NZ LTD, ALPINE ENERGY LTD, MAIN POWER NZ LTD AND ELECTRICITY ASHBURTON LTD Section 274 Party AND NZ RAFTING INC Section 274 Party AND ANN SHERIDAN Section 274 Party AND BULLER ELECTRICITY Section 274 Party 3 TABLE OF CONTENTS 1. QUALIFICATIONS AND EXPERIENCE...............................4 2. SCOPE OF EVIDENCE............................................................5 3. EXPLANATION OF TERMS...................................................7 -
Communications Lifeline Assets
West Coast Lifelines Vulnerability and Interdependency Assessment Supplement 7: Communications Lifeline Assets West Coast Civil Defence Emergency Management Group August 2017 IMPORTANT NOTES Disclaimer The information collected and presented in this report and accompanying documents by the Consultants and supplied to West Coast Civil Defence Emergency Management Group is accurate to the best of the knowledge and belief of the Consultants acting on behalf of West Coast Civil Defence Emergency Management Group. While the Consultants have exercised all reasonable skill and care in the preparation of information in this report, neither the Consultants nor West Coast Civil Defence Emergency Management Group accept any liability in contract, tort or otherwise for any loss, damage, injury or expense, whether direct, indirect or consequential, arising out of the provision of information in this report. This report has been prepared on behalf of West Coast Civil Defence Emergency Management Group by: Ian McCahon BE (Civil), David Elms BA, MSE, PhD Rob Dewhirst BE, ME (Civil) Geotech Consulting Ltd 21 Victoria Park Road Rob Dewhirst Consulting Ltd 29 Norwood Street Christchurch 38A Penruddock Rise Christchurch Westmorland Christchurch Hazard Maps The hazard maps contained in this report are regional in scope and detail, and should not be considered as a substitute for site-specific investigations and/or geotechnical engineering assessments for any project. Qualified and experienced practitioners should assess the site-specific hazard potential, including the potential for damage, at a more detailed scale. Cover Photo: Telecommunications cabinet hit by fallen power pole, Kaikoura earthquake 2016. Photo from Chorus. West Coast Lifelines Vulnerability and Interdependency Assessment Supplement 7: Communications Lifeline Assets Contents 1 OVERVIEW ................................................................................................................................. -
Come Join Us in “New Zealand's Happiest Place”*
THE BULLER GUIDE TO LIVING WELL Come join us in “New Zealand’s Happiest Place”* * The Happiness of New Zealand Report – UMR Research 2012 Top 10 reasons why people move here • Easy lifestyle and quality of life • We’re kid-safe and family focused • A strong sense of community and caring • So much to see and do right on your doorstep • World-renowned scenery • Get a great house on an average wage • Getting to work, school or play takes just minutes • An unbeatable range of sport and recreation • Great retail, support services and cafes • Great transport links to main centres Click on our interactive menu and links throughout to go directly to the section you would like to see. 0 1 2 3 4 5 6 7 10 great Housing, Perfect Place Education & Sports, Health and Culture, Relocation reasons Living for the Active Community Recreation, Wellbeing The Arts, Support Intro Essentials Retiree Learning Entertainment Heritage & Useful & Climate contacts SPACE & freedom The Buller district covers Reefton just less than 8600 square – gateway to the Buller from the Lewis Pass route from kilometers with 84% in Christchurch - born from gold in the 1860’s and now a conservation land and National modern goldmining town with a wonderfully preserved Park. All of this wonderful play heritage main street. Entry way to the magnificent Victoria Conservation Park. area for a population of around 10,000 people! Westport Choose your town – – our biggest little town of around 5,500 with all mod cons. The service centre for the Buller sited at the mouth or go country of the Buller River. -
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Date Printed: 04/22/2009 JTS Box Number: 1FES 67 Tab Number: 123 Document Title: Your Guide to Voting in the 1996 General Election Document Date: 1996 Document Country: New Zealand Document Language: English 1FES 10: CE01221 E II~I6 866 ~II~II~II C - -- ~,~,- - --:- -- - 11 I E14c I· --- ---~--.~~ ~ ---~~ -- ~-~~~ = 'I 1 : l!lG,IJfi~;m~ I 1 I II I 'DURGUIDE : . !I TOVOTING ! "'I IN l'HE 1998 .. i1, , i II 1 GENERAl, - iI - !! ... ... '. ..' I: IElJIECTlON II I i i ! !: !I 11 II !i Authorised by the Chief Electoral Officer, Ministry of Justice, Wellington 1 ,, __ ~ __ -=-==_.=_~~~~ --=----==-=-_ Ji Know your Electorate and General Electoral Districts , North Island • • Hamilton East Hamilton West -----\i}::::::::::!c.4J Taranaki-King Country No,", Every tffort Iws b«n mude co etlSull' tilt' accuracy of pr'rty iiI{ C<llldidate., (pases 10-13) alld rlec/oralt' pollillg piau locations (past's 14-38). CarloJmpllr by Tt'rmlilJk NZ Ltd. Crown Copyr(~"t Reserved. 2 Polling booths are open from gam your nearest Polling Place ~Okernu Maori Electoral Districts ~ lil1qpCli1~~ Ilfhtg II! ili em g} !i'1l!:[jDCli1&:!m1Ib ~ lDIID~ nfhliuli ili im {) 6m !.I:l:qjxDJGmll~ ~(kD~ Te Tai Tonga Gl (Indudes South Island. Gl IIlllx!I:i!I (kD ~ Chatham Islands and Stewart Island) G\ 1D!m'llD~- ill Il".ilmlIllltJu:t!ml amOOvm!m~ Q) .mm:ro 00iTIP West Coast lID ~!Ytn:l -Tasman Kaikoura 00 ~~',!!61'1 W 1\<t!funn General Electoral Districts -----------IEl fl!rIJlmmD South Island l1:ilwWj'@ Dunedin m No,," &FJ 'lb'iJrfl'llil:rtlJD __ Clutha-Southland ------- ---~--- to 7pm on Saturday-12 October 1996 3 ELECTl~NS Everything you need to know to _.""iii·lli,n_iU"· , This guide to voting contains everything For more information you need to know about how to have your call tollfree on say on polling day. -
The Signature of an Extreme Erosion Event on Suspended Sediment Loads: Motueka River Catchment, South Island, New Zealand
184 Sediment Dynamics in Changing Environments (Proceedings of a symposium held in Christchurch, New Zealand, December 2008). IAHS Publ. 325, 2008. The signature of an extreme erosion event on suspended sediment loads: Motueka River catchment, South Island, New Zealand D. M. HICKS1 & L. R. BASHER2 1 National Institute of Water and Atmospheric Research, PO Box 8602, Christchurch, New Zealand [email protected] 2 Landcare Research, Private Bag 6, Nelson Mail Centre, Nelson 7042, New Zealand Abstract Five years of continuously monitoring turbidity and suspended sediment (SS) at four sites in the Motueka River catchment, northern South Island, New Zealand, has characterised the downstream and temporal dispersion of high SS inputs from an extreme rainfall event. The rainstorm, of >50 year recurrence interval, was concentrated in the upper Motueka and Motupiko tributaries and delivered high sediment outputs from re-activated gully complexes and landslides. These only appear to activate when a rainfall threshold is exceeded. Monitoring stations in these tributaries captured a ~20- to 30-fold increase in SS concentrations and event sediment yields, whereas the monitoring station at the coast recorded only a 2- to 5-fold increase. The high concentrations and event yields decayed exponentially back towards normal levels over ~2–3 years at both upstream and downstream sites. Field observations suggest that this erosion recovery trend relates more to the exhaustion/stabilisation of transient riparian sediment storage than to “healing” of the primary erosion sites by surface-armouring and/or re-vegetation. The downstream decay relates both to dilution (from other tributaries carrying lower SS concentrations) and dispersion processes. -
No 14, 19 March 1947
)aumb. 14 321 NEW ZEALAND SUPPLEMENT TO THE NEW ZEALAND GAZETTE OF THURSDAY, MARCH 13, 1947 WELLINGTON, WEDNESDAY, MARCH 19, 1947 Notice of a Scheme of Development and Reconstruction in Westland I (2) The establishment, development, and improvement of· and Buller industry on lands drained or otherwise reclaimed. (3) Development and improvement of the. c~al-mi~ing industry URSUANT to subsection (2) of section 29 of the Finance Act throughout the area, including particularly the Stockton State P (No. 3), 1944, I, Robert Semple, the Minister of Works, Mine, Burke's Creek Colliery, Garvey's Creek Mine, Liverpool hereby give notice of the nature of the work to be included in the Colliery, Mount Davey Coalfields, the Dobson Colliery, Strongman scheme of development and reconstruction described in the First Colliery, and the Tyneside Mine. Schedule hereto, and that the approximate boundaries of the area (4) The processing of coals, utilizing slack coals ai1d lignites of hereby affected are as described in the Second Schedule hereto, the West Coast and Buller regions, in particular the slack coals such area being hereinafter referred to as " the area." This notice of Westport District and the Charleston lignites. shall remain in force until the 30th day of September, 1956. FIRST SCHEDULE 3. Commercial NATURE OF WORK (1) The establishment of commercial areas, and the provision THE improvement of the lands and the development of the area and development of sites'and buildings for commerce in conjunction for industrial, commercial, residential, and recreational purposes, with residential and industrial areas. including, in particular, the provision of:- (2) The provision of accommodation and other facilities for 1. -
ICM Report FINAL.Pmd
2. Literature review and synthesis 2.1 PHYSICAL SETTING The Motueka Catchment is situated at the Moutere gravels, and from the west by a series western margin of the Moutere Depression of generally much larger tributaries, which drain and drains an area of 2180 km2 – the largest both hilly terrain on Moutere gravels (Motupiko, catchment in the Nelson region (Fig. 1). It flows Tadmor) and mountainous terrain underlain by a into Tasman Bay, a shallow but productive complex assemblage of sedimentary and coastal water body of high economic, igneous rocks (Wangapeka, Baton, Pearse, ecological and cultural significance. The Graham, Pokororo, Rocky River and Brooklyn Riwaka River drains a 105 km2 catchment that Stream). Similarly, the Riwaka River drains flows into Tasman Bay 3 km north of the dominantly mountainous terrain underlain by Motueka River mouth (Fig. 1 and Photo 1a). sedimentary and igneous rocks. The major subcatchments and their areas are listed in Table The main stem4 of the Motueka River rises in 1. Elevation ranges from sea level up to 1600– the Red Hills and flows north for about 110 1850 metres on the catchment divide in the km to the sea (Fig. 1). The river is joined from upper reaches of the Motueka, Baton and the east by a series of small and medium-sized Wangapeka rivers. Most of the catchment lies at tributaries (Stanley Brook, Dove, Orinoco, and relatively low elevation, with more than 50% Waiwhero) draining hilly terrain underlain by being between sea level and 500 m. 4 This is the main stem of the Motueka only in a geographical sense; hydrologically the Wangapeka is more important as it drains a larger area and contributes more water. -
Catchment Channel Characteristics and Riverbed Substrate Assessment – a Review and Trial of a Method of Fine Sediment Assessment in the Motueka River
2004-05/01 Catchment channel characteristics and riverbed substrate assessment – a review and trial of a method of fine sediment assessment in the Motueka River Prepared for Stakeholders of the Motueka Integrated Catchment Management Programme June 2005 Landcare ICM Report No. Motueka Integrated Catchment Management Programme Report Series: June 2005 2004-05/01 Catchment channel characteristics and riverbed substrate assessment – a review and trial of a method of fine sediment assessment in the Motueka River Catchment channel characteristics and riverbed substrate assessment – a review and trial of a method of fine sediment assessment in the Motueka River Motueka Integrated Catchment Management (Motueka ICM) Programme Report Series by Chris Phillips1 and Les Basher2 1 Landcare Research, P.O. Box 69, Lincoln 2 Landcare Research, Private Bag 6, Nelson Email: [email protected] [email protected] Information contained in this report may not be used without the prior consent of the client Cover Photo: Fine sediment infilling pool following Easter 2005 storm - upper Motueka River at Gorge. ii Landcare ICM Report No. Motueka Integrated Catchment Management Programme Report Series: June 2005 2004-05/01 Catchment channel characteristics and riverbed substrate assessment – a review and trial of a method of fine sediment assessment in the Motueka River PREFACE An ongoing report series, covering components of the Motueka Integrated Catchment Management (ICM) Programme, has been initiated in order to present preliminary research findings directly to key stakeholders. The intention is that the data, with brief interpretation, can be used by managers, environmental groups and users of resources to address specific questions that may require urgent attentin or may fall outside the scope of ICM research objectives. -
The Climate and Weather of the West Coast
THE CLIMATE AND WEATHER OF WEST COAST 2nd edition G. R. Macara © 2016. All rights reserved. The copyright for this report, and for the data, maps, figures and other information (hereafter collectively referred to as “data”) contained in it, is held by NIWA. This copyright extends to all forms of copying and any storage of material in any kind of information retrieval system. While NIWA uses all reasonable endeavours to ensure the accuracy of the data, NIWA does not guarantee or make any representation or warranty (express or implied) regarding the accuracy or completeness of the data, the use to which the data may be put or the results to be obtained from the use of the data. Accordingly, NIWA expressly disclaims all legal liability whatsoever arising from, or connected to, the use of, reference to, reliance on or possession of the data or the existence of errors therein. NIWA recommends that users exercise their own skill and care with respect to their use of the data and that they obtain independent professional advice relevant to their particular circumstances. NIWA SCIENCE AND TECHNOLOGY SERIES NUMBER 72 ISSN 1173-0382 Note to Second Edition This publication replaces the first edition of New Zealand Meteorological Service Miscellaneous Publication 115 (10), written in 1982 by J. W. D. Hessell. It was considered necessary to update the first edition, incorporating more recent data and updated methods of climatological variable calculation. THE CLIMATE AND WEATHER OF WEST COAST 2nd edition G. R. Macara SUMMARY West Coast is New Zealand’s wettest region, and this may be attributed to its exposure to the predominant westerly airflow over the country, combined with the orographic effect of the Southern Alps. -
Sherry Catchment Case Study
A SENSITIVITY ANALYSIS OF UNCERTAINTY IN THE SPATIAL RESOLUTION OF THE UNDERLYING DATA USED FOR ESTIMATING SOIL EROSION SUSCEPTIBILITY IN NEW ZEALAND A thesis submitted in partial fulfilment of the requirements for the Degree of Master of Science in Environmental Science by James B. Skurupey University of Canterbury 2013 Dedicated to my Grandfather and Grandmother Nehring, as well as my Uncle Loran Nehring and cousin Ann Collins, who all passed away while I was studying abroad in New Zealand. TABLE OF CONTENTS Table of Contents Table of Contents ....................................................................................................................... i List of Figures .......................................................................................................................... vi List of Tables ............................................................................................................................ ix List of Abbreviations ................................................................................................................ x Abstract ................................................................................................................................... xii Acknowledgments ................................................................................................................... xv Chapter 1 Introduction ...................................................................................................... 1 1.1 Background ................................................................................................................... -
Geochemistry of the Karamea Batholith, New Zealand and Comparisons with the Lachlan Fold Belt Granites of SE Australia
LITHOS 0 ELSEVIER Lithos 39 ( 1996) l-20 Geochemistry of the Karamea Batholith, New Zealand and comparisons with the Lachlan Fold Belt granites of SE Australia R.J. Muir a,* , S.D. Weaver a, J.D. Bradshaw a, G.N. Eby ‘, J.A. Evans ‘, T.R. Ireland d a Department ofGeological Sciences, University of Canterbury, Priuate Bag 4800, Christchurch, New Zealand b Department of Earth Sciences, University of Massachusetts, Lowell, MA 01854, USA ’ NERC Isotope Geosciences Laboratory, British Geological Suruey, Keyworth, Nottingham NG12 5GG, UK d Research School of Earth Sciences, The Australian National University, 1 Mills Road, Canberra, ACT 0200, Australia Received 4 January 1996; revised 7 June 1996; accepted 7 June 1996 Abstract The Karamea Batholith in the Buller terrane of the South Island New Zealand forms part of an extensive Middle-Late Devonian belt of magmatic activity along, or close to, the Paleo-Pacific margin of Gondwana. The belt includes the I- and S-type granites of the Lachlan Fold Belt in SE Australia and coeval rocks in Antarctica. The northern half of the Karamea Batholith comprises five main intrusive phases: Zetland Diorite, Whale Creek Granite, Karamea Granite, O’Sullivans Granite and Dunphy Granite. To the east of the Karamea Batholith in the Takaka terrane, ultramafic-mafic Devonian igneous rocks are represented by the Riwaka Complex. The rocks forming the Karamea Batholith are a high-K talc-alkaline suite ranging in composition from metaluminous (AS1 for Zetland Diorite = 0.8) to strongly peraluminous (AS1 for Dunphy Granite = 1.2-1.3). Initial *‘Sr/ s6Sr ratios exhibit a large range from 0.705 in the Zetland Diorite to 0.719 in the Dunphy Granite. -
Headwater Trout Fisheries Ln New Zealand
Headwater trout fisheries ln New Zealand D.J. Jellyman E" Graynoth New Zealand Freshwater Research Report No. 12 rssN 1171-9E42 New Zealmtd, Freshwater Research Report No. 12 Headwater trout fïsheries in New Zealand by D.J. Jellyman E. Graynoth NI\ryA Freshwater Christchurch January 1994 NEW ZEALAND FRBSHWATER RESEARCH REPORTS This report is one of a series issued by NItilA Freshwater, a division of the National Institute of Water and Atmospheric Research Ltd. A current list of publications in the series with their prices is available from NIWA Freshwater. Organisations may apply to be put on the mailing list to receive all reports as they are published. An invoice will be sent for each new publication. For all enquiries and orders, contact: The Publications Officer NIWA Freshwater PO Box 8602 Riccarton, Christchurch New Zealand ISBN 0-47848326-2 Edited by: C.K. Holmes Preparation of this report was funded by the New Zealand Fish and Game Councils NIWA (the National Institute of Water and Atmospheric Research Ltd) specialises in meeting information needs for the sustainable development of water and atmospheric resources. It was established on I July 1992. NIWA Freshwater consists of the former Freshwater Fisheries Centre, MAF Fisheries, Christchurch, and parts of the former Marine and Freshwater Division, Department of Scientific and Industrial Research (Hydrology Centre, Christchurch and Taupo Research hboratory). Ttte New Zealand Freshwater Research Report series continues the New Zealand Freshwater Fßheries Report series (formerly the New Zealand. Ministry of Agriculture and Fisheries, Fisheries Environmental Repon series), and Publications of the Hydrology Centre, Chrßtchurch. CONTENTS Page SUMMARY 1.