Agenda of Environment Committee
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Schedule D Part3
Schedule D Table D.7: Native Fish Spawning Value in the Manawatu-Wanganui Region Management Sub-zone River/Stream Name Reference Zone From the river mouth to a point 100 metres upstream of Manawatu River the CMA boundary located at the seaward edge of Coastal Coastal Manawatu Foxton Loop at approx NZMS 260 S24:010-765 Manawatu From confluence with the Manawatu River from approx Whitebait Creek NZMS 260 S24:982-791 to Source From the river mouth to a point 100 metres upstream of Coastal the CMA boundary located at the seaward edge of the Tidal Rangitikei Rangitikei River Rangitikei boat ramp on the true left bank of the river located at approx NZMS 260 S24:009-000 From confluence with Whanganui River at approx Lower Whanganui Mateongaonga Stream NZMS 260 R22:873-434 to Kaimatira Road at approx R22:889-422 From the river mouth to a point approx 100 metres upstream of the CMA boundary located at the seaward Whanganui River edge of the Cobham Street Bridge at approx NZMS 260 R22:848-381 Lower Coastal Whanganui From confluence with Whanganui River at approx Whanganui Stream opposite Corliss NZMS 260 R22:836-374 to State Highway 3 at approx Island R22:862-370 From the stream mouth to a point 1km upstream at Omapu Stream approx NZMS 260 R22: 750-441 From confluence with Whanganui River at approx Matarawa Matarawa Stream NZMS 260 R22:858-398 to Ikitara Street at approx R22:869-409 Coastal Coastal Whangaehu River From the river mouth to approx NZMS 260 S22:915-300 Whangaehu Whangaehu From the river mouth to a point located at the Turakina Lower -
Geology of the Wairarapa Area
GEOLOGY OF THE WAIRARAPA AREA J. M. LEE J.G.BEGG (COMPILERS) New International NewZOaland Age International New Zealand 248 (Ma) .............. 8~:~~~~~~~~ 16 il~ M.- L. Pleistocene !~ Castlecliffian We £§ Sellnuntian .~ Ozhulflanl Makarewan YOm 1.8 100 Wuehlaplngien i ~ Gelaslan Cl Nukumaruan Wn ~ ;g '"~ l!! ~~ Mangapanlan Ql -' TatarianiMidian Ql Piacenzlan ~ ~;: ~ u Wai i ian 200 Ian w 3.6 ,g~ J: Kazanlan a.~ Zanetaan Opoitian Wo c:: 300 '"E Braxtonisn .!!! .~ YAb 256 5.3 E Kunaurian Messinian Kapitean Tk Ql ~ Mangapirian YAm 400 a. Arlinskian :;; ~ l!!'" 500 Sakmarian ~ Tortonisn ,!!! Tongaporutuan Tt w'" pre-Telfordian Ypt ~ Asselian 600 '" 290 11.2 ~ 700 'lii Serravallian Waiauan 5w Ql ." i'l () c:: ~ 600 J!l - fl~ '§ ~ 0'" 0 0 ~~ !II Lillburnian 51 N 900 Langhian 0 ~ Clifdenian 5e 16.4 ca '1000 1 323 !II Z'E e'" W~ A1tonian PI oS! ~ Burdigalian i '2 F () 0- w'" '" Dtaian Po ~ OS Waitakian Lw U 23.8 UI nlan ~S § "t: ." Duntroonian Ld '" Chattian ~ W'" 28.5 P .Sll~ -''" Whalngaroan Lwh O~ Rupelian 33.7 Late Priabonian ." AC 37.0 n n 0 I ~~ ~ Bortonian Ab g; Lutetisn Paranaen Do W Heretauncan Oh 49.0 354 ~ Mangaorapan Om i Ypreslan .;;: w WalD8wsn Ow ~ JU 54.8 ~ Thanetlan § 370 t-- §~ 0'" ~ Selandian laurien Dt ." 61.0 ;g JM ~"t: c:::::;; a.os'"w Danian 391 () os t-- 65.0 '2 Maastrichtian 0 - Emslsn Jzl 0 a; -m Haumurian Mh :::;; N 0 t-- Campanian ~ Santonian 0 Pragian Jpr ~ Piripauan Mp W w'" -' t-- Coniacian 1ij Teratan Rt ...J Lochovlan Jlo Turonian Mannaotanean Rm <C !II j Arowhanan Ra 417 0- Cenomanian '" Ngaterian Cn Prldoli -
The 1934 Pahiatua Earthquake Sequence: Analysis of Observational and Instrumental Data
221 THE 1934 PAHIATUA EARTHQUAKE SEQUENCE: ANALYSIS OF OBSERVATIONAL AND INSTRUMENTAL DATA Gaye Downes1' 2, David Dowrick1' 4, Euan Smith3' 4 and Kelvin Berryman1' 2 ABSTRACT Descriptive accounts and analysis of local seismograms establish that the epicentre of the 1934 March 5 M,7.6 earthquake, known as the Pahiatua earthquake, was nearer to Pongaroa than to Pahiatua. Conspicuous and severe damage (MM8) in the business centre of Pahiatua in the northern Wairarapa led early seismologists to name the earthquake after the town, but it has now been found that the highest intensities (MM9) occurred about 40 km to the east and southeast of Pahiatua, between Pongaroa and Bideford. Uncertainties in the location of the epicentre that have existed for sixty years are now resolved with the epicentre determined in this study lying midway between those calculated in the 1930' s by Hayes and Bullen. Damage and intensity summaries and a new isoseismal map, derived from extensive newspaper reports and from 1934 Dominion Observatory "felt reports", replace previous descriptions and isoseismal maps. A stable solution for the epicentre of the mainshock has been obtained by analysing phase arrivals read from surviving seismograms of the rather small and poorly equipped 1934 New Zealand network of twelve stations (two privately owned). The addition of some teleseismic P arrivals to this solution shifts the location of the epicentre by less than 10 km. It lies within, and to the northern end of, the MM9 isoseismal zone. Using local instrumental data larger aftershocks and other moderate magnitude earthquakes that occurred within 10 days and 50 km of the mainshock have also been located. -
Classifications
Classifications rt.code.desc Classifications Code Classifications rt.code.base Akitio River Scheme - River Maintenance RC Direct Benefit AREA Akitio River Scheme - Contributor CN Contributor AREA Ashhurst Scheme - Flood Protection AC Flooding Urban CAPITAL Ashhurst Scheme - Flood Protection SUIP AN Annual Charge TARGET Ashhurst Scheme - Lower Stream Maintenance AL Channel Maintenance High AREA Ashhurst Scheme - Upper Stream Maintenance AU Channel Maintenance Low AREA Eastern Manawatu - Lower River Maintenance EL Channell Maintenane High AREA Eastern Manawatu - Upper River Maintenance EU Channell Maintenance low AREA Eastern Manawatu River Scheme - Contributor CN Contributor AREA Eastern Manawatu River Scheme - Indirect IN Indirect Benefit TARGET Forest Road Drainage Scheme A High Benefit AREA Forest Road Drainage Scheme B Medium Benefit AREA Forest Road Drainage Scheme C Moderate Benefit AREA Forest Road Drainage Scheme D Low Benefit AREA Forest Road Drainage Scheme E Minor Benefit AREA Forest Road Drainage Scheme F Indirect Benefit AREA Foxton East Drainage Scheme D1 High Benefit AREA Foxton East Drainage Scheme D2 Medium Benefit AREA Foxton East Drainage Scheme D3 Moderate Benefit AREA Foxton East Drainage Scheme D4 Minor Benefit AREA Foxton East Drainage Scheme D5 Low Benefit AREA Foxton East Drainage Scheme SUIP AC Annual Charge TARGET Foxton East Drainage Scheme Urban U1 Urban CAPITAL Haunui Drainage Scheme A Direct Benefit CAPITAL Himatangi Drainage Scheme A High Benefit AREA Himatangi Drainage Scheme B Medium Benefit AREA Himatangi -
Te Kāuru Taiao Strategy
TE KĀURU EASTERN MANAWATŪ RIVER HAPŪ COLLECTIVE Te Kāuru Taiao Strategy TE KĀURU For The Eastern Manawatū River Catchment NOVEMBER 2016 First Edition: November 2016 Published by: Te Kāuru Eastern Manawatū River Hapū Collective 6 Ward Street PO Box 62 Dannevirke New Zealand Copyright © 2016 Te Kāuru Eastern Manawatū River Hapū Collective Acknowledgments The development of the ‘Te Kāuru Taiao Strategy’ is a tribute to all those who have been and those who are still collectively involved. This document provides strategies and actions for caring for the land, rivers, streams, all resident life within our environment, and our people in the Eastern Manawatū River Catchment. TE KĀURU EASTERN MANAWATŪ RIVER HAPŪ COLLECTIVE Te Kāuru Taiao Strategy Endorsements This strategy has been endorsed by the following 11 hapū of Te Kāuru who are shown with their respective tribal affiliation. A two tier rationale has been used (where required) to identify the Te Kāuru hapū members in terms of their customary connections with regards to their locality, occupation and connection with the Manawatū River and its tributaries: 1. Take ahikāroa 2. Tātai hono Ngāti Mārau (Rangitāne, Kahungunu) Ngāi Te Rangitotohu (Rangitāne, Kahungunu) Ngāi Tahu (Rangitāne, Kahungunu) Ngāti Ruatōtara (Rangitāne) Ngāti Te Opekai (Rangitāne) Ngāti Parakiore (Rangitāne) Ngāti Pakapaka (Rangitāne) Ngāti Mutuahi (Rangitāne) Ngāti Te Koro (Rangitāne) Te Kapuārangi (Rangitāne) Ngāti Hāmua (Rangitāne) Te Kāuru has hapū mana whenua membership of the Manawatū River Leaders’ Forum and will continue to support the ongoing efforts to restore and revitalise the mauri of the Manawatū River. Te Kāuru further support the integration of the Taiao Strategy into the wider Iwi/Hapū Management Plans. -
02 Whole.Pdf (9.122Mb)
Copyright is owned by the Author of the thesis. Pennission 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 pennission of the Author. PALEOENVIRONMENTAL ANALYSIS OF QUATERNARY STRATA IN THE LEVIN AREA A thesis presented in partial fulfilment of the requirements for the degree of Master of Science in Quaternary Science at Massey University ALAN HENRY SEWELL 1991 ·-~-. - - ,.-.··,_·.:·.-· Frontispiece: Pencil sketch looking north from the Tararua foothills, south-east of Potts Hill, across the Tokomaru Marine Terrace and Manawatu River flood plain beyond. ABSTRACT Marine transgression during the Last Interglacial resulted in widespread inundation of the southern Manawa tu area. The Otaki Formation constitutes the relatively thick blanket of predominantly marine sand deposited at the height of the transgression and is now exposed in a partially dissected marine terrace abutting the Tararua Range. Sedimentation was controlled by basement block faulting related to a regional strike-slip tectonic regime on the south eastern margin of the South Wanganui Basin. Wave-induced longshore currents from the north-west supplied abundant sediment to the coast. North-east of Levin the Kairanga Trough, occupying a north-east-trending structural depression between uplifted basement blocks, formed the centre of an embayment during the transgression. Tide-dominated depositional processes predominated around the margins of the embayment. In the Forest Lakes area, the absence of seaward barriers resulted in an open wave-dominated coastline. Between Ohau and Shannon mixed wave/tide processes predominated. Stabilisation of sea level resulted in shoreline progradation which was especially marked south of Levin where a dune belt formed, mantling the coastal cliff and later migrating inland. -
Regional Land Transport Plan 2015 - 2025
Regional Land Transport Plan 2015 - 2025 Contents INTRODUCTION FROM THE CHAIRMAN ..................................................................................................................................... 1 SECTION 1: CONTEXT OF THE REGIONAL LAND TRANSPORT PLAN ...................................................................................... 2 1.1 Purpose of the Plan ........................................................................................................................................... 3 1.2 Responsibilities of Transport Organisations ..................................................................................................... 3 1.2.1 Central Government .......................................................................................................................... 3 1.2.2 Regional and Local Government ....................................................................................................... 3 1.3 The National and Regional Policy Context ........................................................................................................ 4 1.3.1 Government Policy Statement on Land Transport 2015 .................................................................. 4 1.3.2 New Zealand Energy Efficiency and Conservation Strategy 2011-2016 .......................................... 4 1.3.3 The One Plan ...................................................................................................................................... 4 1.4 Process for the Development of the -
A Record of Natural and Human-Induced Environmental
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. A record of natural and human- induced environmental change from Lake Horowhenua A thesis presented in partial fulfilment of the requirements for the degree of Master of Science in Earth Science School of Agriculture and Natural Environment, Massey University, Palmerston North, New Zealand Celeste Bevins 2019 Lake Horowhenua at sunset. Abstract Lake Horowhenua is a hypertrophic turbid lake located in the western coastal plain of the lower North Island of New Zealand. In order to effectively restore or manage modified systems such as Lake Horowhenua, an understanding of past environmental change and natural variability is essential to provide a benchmark for ‘natural’ conditions. Cores from the bed of Lake Horowhenua have been analysed to reconstruct a detailed environmental record for the last c. 4,200 cal yr BP. Prior to lake formation, the area now occupied by the lake was subject to fluvial deposition from the Ohau River sometime prior to 7,500 cal yr BP. Dune transgression began in the region c. 7,700 cal yr BP at the very earliest, and drainage of the small streams and springs was impeded, allowing for the formation of a proto lake. A tidal surge up the Hokio Stream may have occurred c. 7,100 cal yr BP. Clastic delivery into the lake from the inflowing streams was high from 4,200 cal yr BP until sometime around 3,200 cal yr BP. -
Minutes of Hastings District Rural Community Board
Monday, 30 November 2020 Te Hui o Te Kaunihera ā-Rohe o Heretaunga Hastings District Council: Hastings District Rural Community Board Meeting Ngā Miniti Open Minutes Te Rā Hui: Meeting date: Monday, 30 November 2020 Landmarks Room Ground Floor Venue Civic Administration Building Lyndon Road East Hastings Time start - end 2.00 pm - 4.40 pm Go to HASTINGS DISTRICT COUNCIL www.hastingsdc.govt.nz 207 Lyndon Road East, Hastings 4122 | Private Bag 9002, Hastings 4156 Phone 06 871 5000 | www.hastingsdc.govt.nz to see all documents TE KAUNIHERA O HERETAUNGA Monday, 30 November 2020 Te Hui o Te Kaunihera ā-Rohe o Heretaunga Hastings District Council: Hastings District Rural Community Board Meeting Ngā Miniti Open Minutes Te Rārangi Upoko Table of Contents Item Page No. 1. Apologies & Leave of Absence – Ngā Whakapāhatanga me te Wehenga ā-Hui 1 2. Conflicts of Interest - He Ngākau Kōnatunatu 2 3. Confirmation of Minutes - Te Whakamana i Ngā Miniti 2 4. Presentation: Hawke's Bay Forestry Association 2 5. Rural Transportation Activities Report 2 6. Rural Recycling Update and Management of Facilities 3 7. Rural CCTV Update 3 8. Minor Items - Ngā Take Iti 4 9. Urgent Items - Ngā Take WhakahihirI 4 <File No. CG-16-7-00027> Hastings District Council - Hastings District Rural Community Board Minutes | 30/11/2020 Page 1 Monday, 30 November 2020 Te Hui o Te Kaunihera ā-Rohe o Heretaunga Hastings District Council: Hastings District Rural Community Board Meeting Ngā Miniti Open Minutes Chair: Nick Dawson Kua Tae ā-tinana: Marcus Buddo, Sue Maxwell and Jonathon -
Manawatu-Whanganui Regional Sports Facility Plan Is to Provide a High Level Strategic Framework for Sport and Recreation Facility Planning Across the Region (Map 1)
MANAWATU - WHANGANUI REGIONAL SPORT FACILITY PLAN REFERENCE REPORT MARCH 2018 Foreword – Sport New Zealand Sport New Zealand aims to get more young people and adults into sport and active recreation and produce more winners on the worlds sporting stage. It does this through its strategic approach for Community Sport and High Performance Sport outcomes. Spaces, places, and facilities for sport is one of five strategic priorities in the Community Sport Strategy with a goal to develop and sustain a world leading community sport system where the need of the participant and athlete is the focus. With leadership from the network of Regional Sports Trusts, Sport NZ is actively supporting better decision making and investment for future sporting spaces and places through a collaborative regional approach with local and regional government, education, Iwi, funders, national and regional sports organisations. The drivers for taking a regional approach to facility planning can be one or more of the following: • The desire of funders to invest wisely in identified priority projects that will make the most impact • An ageing network of facilities needing refurbishment, re-purposing, replacement or removal • Changing demographics within a community, such as an increase in the population. • Changing participation trends nationally and within a region requiring new types of facilities, or a new use of an existing facility • Increasing expectations of users and user groups • A growing acknowledgement that there is a hierarchy of facilities – regional, sub-regional and local – and that regional collaboration is the only fair and reasonable way to build and manage regional and sub-regional facilities. -
3619-Northern Ohariu Fault: Earthquake Hazard Assessment of A
wp?:4·i .2. 444"'ll,Im6%fi.j - , le..Ibd*di.I 5*fe NORTHERN OHARIU FAULT: 4 /2 ** 4 :ty Earthquake Hazird Assessment of a Newly I . 46. .;1/*if. Discovered Actlve Strike-Slip Fault in Horowhenua 4,2 83 Alan Palmerl & Russ¥an Dissen* 1Soil and Earth Sciences Group, Instii of Natural' 1€sour, Massey University, Private Bag 11-222, Palmerston NorthW a. [email protected] Institute of Geological & Nuclear Sciences, PO Box 30-368 Lower Hutt, NZ 1&6./AL'Ime [email protected] A#jPlibll+A '\ R Prepared for a EQC Research Foundation Project 97/263 April, 2002 1.0 TECHNICAL ABSTRACT The Ohariu fault, discovered about 100 years ago, extends northeastward from o ffshore o f the Wellington south coast near Tongue Point through Porirua towards Paraparaumu. It has long been thought that the Ohariu fault "dies out" to the north in the Waikanae/Otaki area as a series of splays. However, in 1996 we discovered that the pronounced, 60 km long, NNE- to NE-trending topographic lineation that runs just inland of, and parallel to, the western flank of the northern portion of the Tararua Range between Otaki and Palmerston North is an active, right-lateral strike-slip fault. We name this newly discovered fault the Northern Ohariu fault because it appears to be the northern, along-strike, continuation of the Ohariu fault. Collectively the Ohariu and Northern Ohariu faults define a major active strike-slip fault that has a total length in excess of 130 km. Offset geomorphic features such as alluvial terrace risers and valley margins, and estimated ages based on soil and loess stratigraphy are used to constrain the timing, amount, and rate of movement on the fault. -
Order Paper Monday 10 February 2020 at 6.30Pm Hunterville Town Hall, Bruce Street, Hunterville
Hunterville Community Committee Order Paper Monday 10 February 2020 at 6.30pm Hunterville Town Hall, Bruce Street, Hunterville Website: www.rangitikei.govt.nz Email: [email protected] Telephone: 06 327-0099 Facsimile: 06 327-6970 Chair Karen Kennedy Deputy Chair Kelsey Smith Membership Sandra Carroll, Mariata Couch, Lynette Thompson, Jane Watson His Worship the Mayor, Andy Watson Councillor Fi Dalgety and Cr Richard Lambert Please Note: Items in this agenda may be subject to amendments or withdrawal at the meeting. It is recommended therefore that items not be reported upon until after adoption by the Council. Reporters who do not attend the meeting are requested to seek confirmation of the agenda material or proceedings of the meeting from the Chief Executive prior to any media reports being filed. Rangitīkei District Council Hunterville Community Committee Meeting Agenda – Monday 10 February 2020 – 6:30 p.m. Contents 1 Welcome.................................................................................................................2 2 Public Forum ...........................................................................................................2 3 Apologies.................................................................................................................2 4 Member’s conflict of interest .................................................................................2 Agenda note 5 Confirmation of order of business ..........................................................................2 Agenda note