Very Wet in Many Parts and an Extremely Cold Snap for the South
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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. -
Wairarapa Train Services: Survey Results
Wairarapa train services: survey results Introduction Greater Wellington Regional Council carried out a survey of passengers on the north-bound Wairarapa trains on 22 June 2011 as part of the Wairarapa Public Transport Service Review. A total of 725 completed forms were returned. We would like to thank passengers and train-staff for your help with this survey. A summary of the results are shown below. The full survey report is available at www.gw.govt.nz/wairarapareview Where people live and how they get to the station About 25% of passengers live in each of Masterton, Carterton or Featherston. A further 13% of passengers live in Greytown and 6% in Martinborough. Sixty-eight percent of passengers travel to the station by car (57% parking their car at the station and 11% being dropped off). A further 23% of passengers walk or cycle to the station and 7% use the bus. Origin and destination The main boarding station in Wairarapa is Featherston (33%), followed by Masterton (28%), Carterton (25%) and Woodside (12%). Most passengers (85%) are going to Wellington, with the rest (15%) going to the Hutt Valley. Why people use the train, and purpose and frequency of travel The main reason people said they use the train is because it is cheaper than taking the car (56% of passengers) and a significant number also said it is quicker than driving (29% of passengers). Comfort (45% of passengers) and ability to work on the train (47% of passengers) were also important. Twenty-six percent of passengers also indicated that it’s environmentally responsible and 20% said they had no other transport option. -
Cultural Value Report Arrow and Cardrona
CULTURAL VALUES REPORT Arrow River / Wakatipu Basin Aquifers Cardrona River Intellectual Property Rights This report has been prepared for Otago Regional Council on behalf of Te Rūnanga o Moeraki, Kāti Huirapa Rūnaka ki Puketeraki, Te Rūnanga o Ōtākou and Hokonui Rūnanga (Kāi Tahu ki Otago) and Te Rūnanga o Waihōpai, Te Rūnanga o Awarua and Te Rūnanga o Ōraka-Aparima (Kāi Tahu ki Murihiku). Intellectual property rights are reserved by these rūnanga. Acknowledgement The preparation of this report was undertaken with the assistance of: Te Rūnanga o Moeraki Kāti Huirapa Rūnaka ki Puketeraki Te Rūnanga o Ōtākou Hokonui Rūnanga Te Rūnanga o Waihōpai Te Rūnanga o Awarua Te Rūnanga o Ōraka-Aparima Key informants and site evaluation participants. Peter Petchey and Brian Allingham. Front Cover: The confluence of the Cardrona and Clutha rivers. Photograph: Maree Kleinlangevelsloo Version: October 2017 KTKO Ltd Prepared by: Level 1 Maree Kleinlangevelsloo 258 Stuart Street Literature Review: Rosemary Clucas PO Box 446 Reviewed By: Dunedin Te Rūnanga o Moeraki Tel: 03-477–0071 Kāti Huirapa Rūnaka ki Puketeraki Te Rūnanga o Ōtākou Hokonui Rūnaka Te Rūnanga o Awarua Te Rūnanga o Waihōpai Te Rūnanga o Ōraka-Aparima Tim Vial (KTKO Ltd) 1 Executive Summary The Arrow and Cardrona catchments and the Wakatipu Basin are highly valued by the whānau of Kāi Tahu ki Otago and Murihiku (Kāi Tahu). Ara tawhito (trails), ran through these catchments, bringing whānau into the southern lakes and rivers on their seasonal pursuit of resources. Today the rivers are used for recreation, and are valued for their landscape qualities and the species residing in them. -
2021 Annual Report
LION FOUNDATION 2021 ANNUAL REPORT Our aim is to be New Zealand’s leading charitable trust, nationally recognised and respected for helping New Zealanders achieve great things in the community. We value integrity, compelling us to act honestly, ethically and transparently. For 36 years we have been working with NZ communities to make a difference. During this time we have granted over $985 million to support community projects across the country. In the last financial year we distributed more than $35 million to community-based organisations. We’re here to make a difference. Barnardos NZ “We can’t do the work we do without the help of generous supporters like The Lion Foundation.” – Dr Claire Achmad, General Manager Advocacy, Fundraising, Marketing & Communications THETHETHE LION LION LION FOUNDATION FOUNDATIONFOUNDATION | CHAIRMAN | CHAIRMAN AND AND CEO CEO REPORT REPORT Chairman and CEO Report CHAIRMAN’SCHAIRMAN’S REPORT REPORT CHIEFCHIEF EXECUTIVE’S EXECUTIVE’S REPORT REPORT Chairman’sThe LionThe FoundationLion Report Foundation has continued has continued its proud its proudthan inthan March in March 2020, 2020, when, when,as a nationas a nationwe weWhat anWhatChief interesting an interestingExecutive’s end to end our to2019/2020 our Report 2019/2020 financial financial year asyear as record of community fundraising over the past experienced a life changing pandemic. the Covid-19 pandemic presented unprecedented challenges I have had therecord privilege of community of writing thisfundraising message over to the the pastplatforms experienced disappear a lifeoverseas changing and pandemic.no resulting funding theWell, Covid-19 our 2020/21 pandemic financial presented year unprecedentedhas certainly beenchallenges an year, withyear, $38,296,847with $38,296,847 being beingdistributed distributed to Despiteto these unchartered times, The Lion - not only- not for only The for Lion The Foundation, Lion Foundation, our venue our venueoperators operators and and Lion Foundationsupport community forprojects several throughoutyears. -
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 -
Introduction Getting There the Hurunui River the Waiau River
Introduction The Hurunui and Waiau Rivers offer a more relaxed fishing experience than the bigger braided rivers further south. They are home to North Canterbury’s best populations of brown trout in addition to seasonal populations of sea run salmon. The Hurunui and Waiau Rivers flow through hills for most of their length and are Canterbury’s most scenic braided rivers. In places, the presence of hills on the riverbanks make access challenging but anglers who put in the effort should be well rewarded. Getting There The Waiau River The Hurunui and Waiau Rivers lie around 90 and 130 kilometres north clears after a fresh. The section of river on either side of the State The Waiau River runs through a series of gorges from the Alps to the of Christchurch City respectively. The lower reaches are accessed from Highway 7 (Balmoral) Bridge is the easiest to access. Mid January until sea. Access can be difficult in places but is more than made up for by roads leading off State Highway 1. Both rivers benefit from a number mid March is the best time to fish for salmon in the Hurunui River. the stunning scenery on offer. The Waiau Mouth is a popular spot for of bridges which are the principle access points for anglers wishing to salmon fishing but can only be accessed by launching a jet boat at fish the middle reaches. In the upper reaches of the Hurunui, access is Populations of brown trout can be found anywhere from the mouth up Spotswood and boating downstream for ten minutes. -
East Coast Inquiry District: an Overview of Crown-Maori Relations 1840-1986
OFFICIAL Wai 900, A14 WAI 900 East Coast Inquiry District: An Overview of Crown- Maori Relations 1840-1986 A Scoping Report Commissioned by the Waitangi Tribunal Wendy Hart November 2007 Contents Tables...................................................................................................................................................................5 Maps ....................................................................................................................................................................5 Images..................................................................................................................................................................5 Preface.................................................................................................................................................................6 The Author.......................................................................................................................................................... 6 Acknowledgements............................................................................................................................................ 6 Note regarding style........................................................................................................................................... 6 Abbreviations...................................................................................................................................................... 7 Chapter One: Introduction ...................................................................................................................... -
Print PDF Trip Notes
Central Otago Trail Trip Notes A collection of cycle trails alongside the rivers and lakes of the stunning Central Otago district including Arrowtown, Cromwell, Wanaka, Clyde and Roxburgh. Incredible scenery and excellent cycle trails. Tour Highlights Tour Details + Cycle 187km of cycle trails around Central Otago’s stunning lakes & rivers + 6 days + Ride the stunning purpose built Gibbston Valley Trail; Lake Hawea Trail; Lake Dunstan Cycle + Grade 2 Trail; Roxburgh Gorge and Clutha Gold Cycle Trails + 187km+ cycling with full vehicle support + Experience the colours of the seasons [100% gravel cycle trail] + Take in the spectacular scenery and relaxed vibe of the Central Otago + Starts/Ends in Queenstown or + Explore the small communities of Arrowtown, Cromwell & Clyde Christchurch + Travel through the stunning Roxburgh Gorge by bicycle and jet boat + Indulge in fresh Central Otago produce and local wines + Dial out and enjoy a week away in this most stunning part of NZ Tour Cost Departure Dates Tour Price: from $2,250 Refer to our website for current departure Deposit: $400 dates and tour availability. What's included? + 5 nights twin-share ensuite accommodation + 5 evening meals; 4 lunches; 5 continental breakfasts Grade 2 + fruit, snacks & morning teas on the trail + the services of a tour leader who provides vehicle support & information + cycle repair support + all transport from/to Christchurch + Roxburgh Gorge jet boat shuttle + Goods & Services Tax of 15% Not included: + wine; beer; espresso coffees + lunch on Days 1 & 6 + wine tasting fees + bike hire (standard $200; e-bike $515) + single accommodation ($400) + transfers from Clyde to Queenstown on Day 6 (from $55 approx; bikes additional) _________________________________________________________________________________ Questions? Call us Phone worldwide: +64 21 178 8287 www.puretrailsnewzealand.co.nz 1 Central Otago Trail Trip Notes A collection of cycle trails alongside the rivers and lakes of the stunning Central Otago district including Arrowtown, Cromwell, Wanaka, Clyde and Roxburgh. -
Secondary Schools of New Zealand
All Secondary Schools of New Zealand Code School Address ( Street / Postal ) Phone Fax / Email Aoraki ASHB Ashburton College Walnut Avenue PO Box 204 03-308 4193 03-308 2104 Ashburton Ashburton [email protected] 7740 CRAI Craighead Diocesan School 3 Wrights Avenue Wrights Avenue 03-688 6074 03 6842250 Timaru Timaru [email protected] GERA Geraldine High School McKenzie Street 93 McKenzie Street 03-693 0017 03-693 0020 Geraldine 7930 Geraldine 7930 [email protected] MACK Mackenzie College Kirke Street Kirke Street 03-685 8603 03 685 8296 Fairlie Fairlie [email protected] Sth Canterbury Sth Canterbury MTHT Mount Hutt College Main Road PO Box 58 03-302 8437 03-302 8328 Methven 7730 Methven 7745 [email protected] MTVW Mountainview High School Pages Road Private Bag 907 03-684 7039 03-684 7037 Timaru Timaru [email protected] OPHI Opihi College Richard Pearse Dr Richard Pearse Dr 03-615 7442 03-615 9987 Temuka Temuka [email protected] RONC Roncalli College Wellington Street PO Box 138 03-688 6003 Timaru Timaru [email protected] STKV St Kevin's College 57 Taward Street PO Box 444 03-437 1665 03-437 2469 Redcastle Oamaru [email protected] Oamaru TIMB Timaru Boys' High School 211 North Street Private Bag 903 03-687 7560 03-688 8219 Timaru Timaru [email protected] TIMG Timaru Girls' High School Cain Street PO Box 558 03-688 1122 03-688 4254 Timaru Timaru [email protected] TWIZ Twizel Area School Mt Cook Street Mt Cook Street -
Auckland Regional Office of Archives New Zealand
A supplementary finding-aid to the archives relating to Maori Schools held in the Auckland Regional Office of Archives New Zealand MAORI SCHOOL RECORDS, 1879-1969 Archives New Zealand Auckland holds records relating to approximately 449 Maori Schools, which were transferred by the Department of Education. These schools cover the whole of New Zealand. In 1969 the Maori Schools were integrated into the State System. Since then some of the former Maori schools have transferred their records to Archives New Zealand Auckland. Building and Site Files (series 1001) For most schools we hold a Building and Site file. These usually give information on: • the acquisition of land, specifications for the school or teacher’s residence, sometimes a plan. • letters and petitions to the Education Department requesting a school, providing lists of families’ names and ages of children in the local community who would attend a school. (Sometimes the school was never built, or it was some years before the Department agreed to the establishment of a school in the area). The files may also contain other information such as: • initial Inspector’s reports on the pupils and the teacher, and standard of buildings and grounds; • correspondence from the teachers, Education Department and members of the school committee or community; • pre-1920 lists of students’ names may be included. There are no Building and Site files for Church/private Maori schools as those organisations usually erected, paid for and maintained the buildings themselves. Admission Registers (series 1004) provide details such as: - Name of pupil - Date enrolled - Date of birth - Name of parent or guardian - Address - Previous school attended - Years/classes attended - Last date of attendance - Next school or destination Attendance Returns (series 1001 and 1006) provide: - Name of pupil - Age in years and months - Sometimes number of days attended at time of Return Log Books (series 1003) Written by the Head Teacher/Sole Teacher this daily diary includes important events and various activities held at the school. -
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.