Outstanding Natural Landscapes & Features
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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 -
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. -
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. -
Very Wet in Many Parts and an Extremely Cold Snap for the South
New Zealand Climate Summary: June 2015 Issued: 3 July 2015 Very wet in many parts and an extremely cold snap for the south. Rainfall Rainfall was above normal (120-149%) or well above normal (> 149%) for much of the Manawatu-Whanganui, Taranaki, Westland, Tasman, Nelson, Marlborough, Canterbury, Otago, and Southland regions. Rainfall was well below normal (< 50%) or below normal (50-79%) for parts of Northland, Auckland, Waikato, Bay of Plenty, Gisborne, Hawke’s Bay, and north Canterbury. Temperature June temperatures were near average across much of the country (within 0.5°C of June average). Below average temperatures were recorded in inland Canterbury, Wairarapa, western Waikato (0.5-1.2°C below June average) and above average temperatures experienced in northern, eastern, and western parts of the North Island and northern, western, and south-central parts of the South Island (0.5-1.2°C above June average). A polar outbreak in late June led to the 4th-lowest temperature ever recorded in New Zealand. Soil Moisture As of 1 July 2015, soil moisture levels were below normal for this time of year for East Cape, around and inland from Napier, coastal Wairarapa, coastal southern Marlborough and eastern parts of Canterbury north of Christchurch. It was especially dry about north Canterbury where soils were considerably drier than normal for this time of year. Sunshine Well above normal (>125%) or above normal (110-125%) sunshine was recorded in Northland, Auckland, western Waikato, Wellington, Marlborough, north Canterbury, and Central Otago. Near normal sunshine (within 10% of normal) was recorded elsewhere, expect in Franz Josef and Tauranga where below normal sunshine was recorded. -
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. -
Otaki.Net.Nz CONTRIBUTORS: Pera Barrett (Good Thinking) • Fraser Carson (Media & • PLUNKET 0800 933 922
Māoriland Hear marae Frosty mornings Covid-19: festival voices for Get to know remounts from whitebaiters your enemy p3 1950 p13 p16 p19 otakitoday.com ŌTAKI TODAY • MAHURU SEPTEMBER 2020 Ngā Kōrero o Ōtaki Rangatahi seek support Already rocked by two young people taking their own life in the past four years, Ōtaki College is saying its counselling services are stretched to the limit. As at many other schools throughout the country, the number of rangatahi (teenagers) seeking help is unprecedented. The pressure increased with the onset of Covid-19 and the return to school in May. Issues have included increased anxiety, depression, family separation, impacts of family mental health needs, stress about exams and future plans. College counsellor Jo McInerney says she’s pleased to see that students are seeking support, but she’s “holding” the safety of many while they wait for therapy. Community mental health and counselling services are also stretched, so the wait can be 4-6 weeks. “Once significant issues have come to the surface it can be difficult for students WHEN HUMANS to manage their emotions,” Jo says. “I am needing to help students to make safety plans for themselves and to have increased contact with home as required.” LET CATS DOWN The college has applied to the Ministry By Ian Carson of Education Covid- 19 Urgent Response The grey tabby had roamed North Manakau Sad case of the Manakau Mauler Fund to increase counsellor resource – it’s for months, scrapping with local cats and he was a former house cat. He was clearly It can’t have been a great home, because waiting for a response. -
Ohau Loop Phase 1 Existing Status and Recommendations for Improvement
Ohau Loop Phase 1 Existing Status and Recommendations for Improvement Manaaki Taha Moana: Enhancing Coastal Ecosystems for Iwi MTM Report No. 5 November 2011 ŌHAU LOOP PHASE 1: EXISTING STATUS AND RECOMMENDATIONS FOR IMPROVEMENT CRAIG ALLEN, KATI DOEHRING, ROGER YOUNG, JIM SINNER Manaaki Taha Moana: Enhancing Coastal Ecosystems for Iwi and Hapū SBN 978-0-9876535-4-3 ISSN 2230-3332 (Print) ISSN 2230-3340 (Online) Published by the Manaaki Taha Moana Research Team Funded by the Ministry for Science and Innovation MAUX 0907 Contract Holder: Massey University www.mtm.ac.nz APPROVED FOR RELEASE REVIEWED BY: BY: John Hayes MTM Science Leader Cawthron Institute Professor Murray Patterson ISSUE DATE: November 2011 RECOMMENDED CITATION: Allen C, Doehring K, Young R, Sinner J 2011. Ōhau Loop Phase 1: Existing Status and Recommendations for Improvement. Manaaki Taha Moana Research Report No. 5. Cawthron Report No. 2041. 57 p. plus appendices. © COPYRIGHT: Apart from any fair dealing for the purpose of study, research, criticism, or review, as permitted under the Copyright Act, this publication must not be reproduced in whole or in part without the written permission of the Copyright Holder, who, unless other authorship is cited in the text or acknowledgements, is the commissioner of the report. Mihi Te ngākau pūaroha ki ngā ōhākī ‘E kore koe e ngaro- te kākano i ruia mai i Rangiātea Puritia! Puritia! Puritia! E ngā atua Māori, mō ōu whakaaro whānui mā a tātou, tēnā koutou. E ngā mana, e ngā reo, e ngā iwi o te motu, tēnā koutou. E ngā matāwaka, whītiki! Whītiki! Whītiki! Te hunga ora ki te hunga ora, te hunga mate ki te hunga mate. -
State of Ecological/Cultural Landscape Decline of the Horowhenua Coastline Between Hokio and Waitohu Streams
State of Ecological/Cultural Landscape Decline of the Horowhenua Coastline Between Hokio and Waitohu Streams Manaaki Taha Moana: Enhancing Coastal Ecosystems for Iwi MTM Report No. 2 June 2011 State of Ecological/Cultural Landscape State Declineof Ecological/Cultural of the Horowhenua Coastline LandscapeBetween Decline Hokio and ofWaitohu Horowhenua Streams Coastline Between Hokio and Dr Huhana Smith WaitohuAroha Streams Spinks Tipene Hoskins ! Moira Poutama ! "#!$%&'('!)*+,&! !!!!!! ISBN 978-0-9876535-1-2 !!!!!! ISSN-#.&'!)/+(01! 2230-3332 (Print) !!!!!! 2+/3(3!$.10+(1!ISSN 2230-3340 (Online) 4.+#'!5.%,'*'! Published by the Manaaki Taha Moana (MTM) Research Team FundedISBN by the978-0-9876535-1-2 Ministry for Science and Innovation Contract MAUX0907 MainISSN Contract 2230-3332 Holder: Massey(Print) University www.mtm.ac.nz ISSN 2230-3340 (Online) 5%67+1&38!69!,&3!4'(''0+!2'&'!4.'('!:424;!<313'#=&!23'*! >%(838!69!,&3!4+(+1,#9!?.#!)=+3(=3!'(8!@((.A',+.(! B.(,#'=,!4-CDEFEG! 4'+(!B.(,#'=,!$.783#H!4'1139!C(+A3#1+,9! IIIJ*,*J'=J(K! Peer reviewed by: !!!!!!!!! Approved for release by: Te Waari Carkeek and Dennis Emery!!!!!!!!!!! <3A+3I38!69H!! 23!L''#+!B'#0330! -//#.A38!?.#!#373'13!69H! ! !!"3((+1!M*3#9!!!!!!!!!! ! 424!)=+3(=3!N3'83#! ! !!!!!!!!!!! MTM5#.?311.#!4%##'9!5',,3#1.(! Science Leader !!!!!!!!!!! Professor Murray Patterson @11%3!"',3H!O%79!PEQQ! Recommended citation: <3=.**3(838!=+,',+.(H! )*+,&R!$JR!)/+(01R!-JR!$.10+(1R!2J!S!5.%,'*'R!4J!:PSmith, H., Spinks, A., Hoskins, T. & Poutama, EQQ;J!!),',3!.?!M=.7.T+='7UB%7,%#'7!N'(81='/3!"3=7+M. (2011). State of Ecological/Cultural Landscape Decline(3!.?!$.#.I&3(%'!B.'1,7 of Horowhenua Coastline+(3! V3,I33(!$.0+.!'(8!L'+,.&%!),#3'*1J!!4'(''0+!2'&'!4.Between Hokio and Waitohu Streams. -
Waiwiri Lake, Stream & Environs: He Taonga
20.3.18 (Collins, 2018 D4) Waiwiri Lake, Stream & Environs: He Taonga Cultural Impact Assessment report for the three affected Ngāti Raukawa hapū – Ngāti Kikopiri, Ngāti Pareraukawa, Ngāti Hikitanga By Heeni Collins, with support from the Ngāti Kikopiri Māori Marae Committee Society, the Kikopiri Marae Reservation Trustees, Ngāti Pareraukawa & Ngāti Hikitanga. Funded by the Horowhenua District Council March 2018 1 20.3.18 Contents Contents ..................................................................................................................................... 2 1. Introduction ........................................................................................................................... 3 2. Treaty of Waitangi Claims - Context ...................................................................................... 4 3. Steps towards Cultural Impact Assessment Report ............................................................... 7 4. Cultural Values – Ngāti Kikopiri, Ngāti Pareraukawa, Ngāti Hikitanga ................................ 10 4.1 Mauri .............................................................................................................................. 10 4.2 Wairuatanga - ngā atua & ngā tupuna .......................................................................... 10 4.3 Ngāti Kikopiri Environmental Management Report ...................................................... 11 4.4 Ngāti Kikopiri Oral and Traditional report ..................................................................... 13 -
Recent Spread of Tuberculosis in the Kapiti and Horowhenua Districts
Recent spread of tuberculosis in the Kapiti and Horowhenua districts The Kapiti, Horowhenua and Manawatu dis- proximity to Wellington, there are many Tuberculosis breakdowns tricts have traditionally been free of bovine subdivisions of small farming or lifestyle tuberculosis. lnvestigations of tuberculosis blocks whose owners commute to the The breakdowns that occurred are breakdowns before 1990 showed that the in- capital. Horticultural blocks, with accom- shown in Table I. fection couldgenerally be traced to cattle that panying shelter belts, are scattered be- Otaki Beach: In early 1992, a large had movedfrom tuberculosis endemic areas. tween the livestock farms as the climate town-supply dairy herd just north of the Most breakdowns in cattle herds involved is suitable for many enterprises such as Otaki River (Property A, see Table I) was only a single infected animal. Since 1990, pip and stone fruit. Generally the owners tuberculin tested following the finding outbreaks ofbovine tuberculosis have occurred of smaller 'lifestyle' blocks farm a few of a tuberculous lesion in a bull beef in herds in the Horowhenua and Kapiti Dis- cattle, sheep or horses and the properties animal at slaughter in December 1991. tricts. At the time of these breakdowns there change hands frequently. Thus stock and Investigations revealed no obvious source was no immediate obvious domestic animal human movement is commonplace and of infection. The whole herd test resulted source of infection so a tuberculous wildlife part of the farming culture. in 12 reactors, eight of which had visible source was considered. Subsequent surveys Before 1992, the endemic area to the lesions at slaughter. -
State and Trends of River Water Quality in the Manawatū-Whanganui Region
State and Trends of River Water Quality in the Manawatū-Whanganui Region November 2018 Horizons Report 2018/EXT/1619 Prepared for: Abby Matthews November 2018 Science & Innovation Manager Report No. 2018/EXT/1619 ISBN 978-1-98-853744-3 Prepared by: Caroline Fraser and Ton Snelder Client Report 2018-08 For any information regarding this report please contact: Caroline Fraser Phone: 022 049 1779 Email: [email protected] LWP Ltd, PO Box 70 Lyttelton 8092 CONTACT 24 hr Freephone 0508 800 800 [email protected] www.horizons.govt.nz Kairanga Taumarunui Levin Cnr Rongotea and 34 Maata Street 120–122 Hōkio Beach Road Kairanga-Bunnythorpe Roads SERVICE REGIONAL Palmerston North Taihape Palmerston North DEPOTS CENTRES HOUSES 11-15 Victoria Avenue Torere Road Ohotu Marton Whanganui Hammond Street 181 Guyton Street Woodville 116 Vogel Street POSTAL Horizons Regional Council, Private Bag 11025, Manawatū Mail Centre, Palmerston North 4442 F 06 9522 929 ADDRESS State and Trends of River Water Quality in the Manawatū-Whanganui Region For all records up to 30 June 2017 November 2018 Prepared By: Caroline Fraser Ton Snelder For any information regarding this report please contact: Caroline Fraser Phone: 022 049 1779 Email: [email protected] LWP Ltd PO Box 70 Lyttelton 8092 New Zealand LWP Client Report Number: LWP Client Report 2018-08 Report Date: November 2018 LWP Project: 2018-08 Quality Assurance Statement [Click here and type text] Version (2) 11.09.18 Version (1) 31.07.18 Reviewed By Ned Norton [Signature] Page 2 of 126 Table of Contents Executive Summary ................................................................................................... 9 1 Introduction .................................................................................................... -
Muhunoa East
Muhunoa East 1900-1907 1907 112 Ohau/Side School Feist Adolph M D1 Head Master £225.00 $30.00 1907 112 Ohau/Side School Tew Winifred E H D2 Assistant Female £105.00 1907 112 Ohau/Side School Atkinson Mary E Assistant Female £85.00 3rd May 1900 Wellington Education Board An application was received for the establishment of an aided school at Muhunoa, about three miles from the present Ohau School. The Ohau committee wrote objecting to the proposal, urging that it would tend to weaken the present school. It was decided to suggest to _ the committee that it should subsidise a cart for the conveyance to and from- the present school of children living at a distance. [An aided school is where the community pay all the costs and the Education Board pays the school a sum of money based on the roll.] 28th June 1900 It was reported that parents on the Muhunoa road declined to provide conveyances so that their children might attend the Ohau School. 4th March 1903 Wellington Education Board With regard to the Kimberley road and Upper Muhunoa schools, it was reported a new road was being made to connect the districts, in which case one school would serve the needs of both places. The department’s offer of a subsidy towards the cost of conveying children living at the extremity of the road, the report stated, was still available. The report was adopted. 5th October 1904 Wellington Education Board Inspector Bakewell reported in favour of a new side school at Muhunoa, three to four miles from Ohau.