Feilding Manawatu Palmerston North City
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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. -
Full Article
NOTORNIS QUARTERLY JOURNAL of the Ornithological Society of New Zealand Volume Sixteen, Number Two, lune, 1969 NOTICE TO CONTRIBUTORS Contributions should be type-written, double- or treble-spaced, with a wide margin, on one side of the paper only. They should be addressed to the Editor, and are accepted o?, condition that sole publication is being offered in the first instance to Notornis." They should be concise, avoid repetition of facts already published, and should take full account of previous literature on the subject matter. The use of an appendix is recommended in certain cases where details and tables are preferably transferred out of the text. Long contributions should be provided with a brief summary at the start. Reprints: Twenty-five off-prints will be supplied free to authors, other than of Short Notes. When additional copies are required, these will be produced as reprints, and the whole number will be charged to the author by the printers. Arrangements for such reprints must be made directly between the author and the printers, Te Rau Press Ltd., P.O. Box 195, Gisborne, prior to publication. Tables: Lengthy and/or intricate tables will usually be reproduced photographically, so that every care should be taken that copy is correct in the first instance. The necessity to produce a second photographic plate could delay publication, and the author may be called upon to meet the additional cost. nlastrutions: Diagrams, etc., should be in Indian ink, preferably on tracing cloth, and the lines and lettering must be sufficiently bold to allow of reduction. Photographs must be suitable in shape to allow of reduction to 7" x 4", or 4" x 3f". -
Businessevents.Newzealand.Com Te Puia, Rotorua
Te Puia, Rotorua businessevents.newzealand.com PULL-UP BANNERS Wellington newzealand.com AsCA CRYSTAL December - | Auckland, New Zealand Royal Wellington Golf Club Graeme Murray WELCOME TO AUCKLAND Viaduct Harbour, Auckland . HRS . HRS NORTH AMERICA EUROPE HRS HRS NORTH ASIA HRS MIDDLE EAST HRS INDIA HRS AGCSA SOUTH EAST ASIA SOUTH AMERICA HRS HRS AUSTRALIA HRS . HRS AUCKLAND NEW ZEALAND DISCOVER Oriental Bay, Wellington Rob Suisted Rob Wellington Oriental Bay, NEW ZEALAND Hobbiton, Waikato Sara Orme Sara Waikato Hobbiton, Julian Apse TM Wellington Harbour Wellington Jet Shotover River Shotover Bridge to Nowhere, Whanganui National Park Hobbiton Movie set, Waikato Bleed Area A4 BANNERS WellingtonMilford Sound, Fiordland DunedinMilford Sound, Fiordland newzealand.com newzealand.com ChristchurchMilford Sound, Fiordland WaitomoMilford Sound, Glowworm Fiordland Caves newzealand.com newzealand.com EMAIL NEWSLETTERS BEYOND THE OFFICIAL PROGRAMME Te Puia, Rotorua newzealand.com GETTING HERE EUROPE HRS NORTH ASIA HRS NORTH AMERICA Arthurs Point, Queenstown Te Puia, Rotorua Hobbiton™ Movie Set, Waikato HRS Hokitika Gorge, West Coast In New Zealand, you are never far from something incredible. SOUTH EAST SOUTH ASIA AMERICA There’s no better place for adventure, rejuvenation, or inspiration. HRS HRS AUSTRALIA HRS Expand your horizons beyond your conference programme AUCKLAND HRS and explore the amazing experiences on offer. NEW ZEALAND In a short span of travelling time, our diverse landscape changes from snowcapped mountains to golden beaches, bubbling geothermal pools and lush rainforests. Waiheke Island, Auckland New Zealand is the only place you’ll find unique Māori culture, Tongariro Alpine Crossing, Ruapehu Wellington from facing a haka (ancestral war challenge) to eating from a hāngī (traditional pit oven). -
Feilding Manawatu Palmerston North City
Mangaweka Adventure Company (G1) Rangiwahia Scenic Reserve (H2) Location: 143 Ruahine Road, Mangaweka. Phone: +64 6 382 5744 (See Manawatu Scenic Route) OFFICIAL VISITOR GUIDE OFFICIAL VISITOR GUIDE Website: www.mangaweka.co.nz The best way to experience the mighty Rangitikei River is with these guys. Guided kayaking and rafting Robotic Dairy Farm Manawatu(F6) trips for all abilities are on offer, and the friendly crew will make sure you have an awesome time. Location: Bunnythorpe. Phone: +64 27 632 7451 Bookings preferred but not essential. Located less than 1km off State Highway 1! Website: www.robotfarmnz.wixsite.com/robotfarmnz Take a farm tour and watch the clever cows milk themselves in the amazing robotic milking machines, Mangaweka Campgrounds (G1) experience biological, pasture-based, free-range, sustainable, robotic farming. Bookings are essential. Location: 118 Ruahine Road, Mangaweka. Phone: +64 6 382 5744 Website: www.mangaweka.co.nz An idyllic spot for a fun Kiwi camp experience. There are lots of options available from here including The Coach House Museum (E5) rafting, kayaking, fishing, camping or just relaxing under the native trees. You can hire a cabin that Location: 121 South Street, Feilding. Phone: +64 6 323 6401 includes a full kitchen, private fire pit and wood-burning barbecue. Website: www.coachhousemuseum.org Discover the romance, hardships, innovation and spirit of the early Feilding and Manawatu pioneers Mangaweka Gallery and Homestay (G1) through their stories, photos and the various transportation methods they used, all on display in an Location: The Yellow Church, State Highway 1, Mangaweka. Phone: +64 6 382 5774 outstanding collection of rural New Zealand heritage, showcasing over 140 years of history. -
The Late Quaternary Geomorphology of the Lower Manawatu
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. THE LATE QUATERNARY GEOMORPHOLOGY OF THE LOWER MANAWATU A thesis presented in partial fulfilment of the requirements for the Degree of Master of Arts in Geography at Massey University by PATRICK ALAN HESP 1975 ABSTRACT The geomorphology of the present Lower Manawa tu floodplain and the valleys that exit at the margin of the floodplain, is presented. An introduction to the geology and geomorphology of the study area is given, and previous studies are reported where relevant. Two types of tributary valleys have been recognised in the study area. These valleys have been cut into the Tokomaru Marine Terrace. The first type recognised are predominantly gravel-floored, box-shaped valleys with headwaters in the Tararua Ranges. The second and major type recognised are box-shaped valleys without gravel floors. The first type have been formed by normal fluvial processes, while the second type were originally V-shaped, and have been infilled by estuarine sedimentation processes. The latter occurred as a direct result of the Flandrian Transgression. The morphology of the Tokoma ru Marine Terrace margin is examined, and it is concluded that the margin is predominantly river-cut. The Manawatu floodplain was originally an estuary. As the Flandrian Transgression began the lower reaches of the Manawatu and eventually the Oroua Rivers were drowned. As the Transgression progressed, the Lower Manawatu became an estuary. -
Application and Evaluation of Sediment Fingerprinting Techniques in the Manawatu River Catchment, New Zealand
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. Application and Evaluation of Sediment Fingerprinting Techniques in the Manawatu River Catchment, New Zealand A thesis presented in partial fulfilment of the requirements for the degree of Doctor of Philosophy in Geography at Massey University, Palmerston North, New Zealand Simon Vale 2016 ii Abstract Suspended sediment is an important component of the fluvial environment, contributing not only to the physical form, but also the chemical and ecological character of river channels and adjacent floodplains. Fluvial sediment flux reflects erosion of the contributing catchment, which when enhanced can lead to a reduction in agricultural productivity, effect morphological changes in the riparian environment and alter aquatic ecosystems by elevating turbidity levels and degrading water quality. It is therefore important to identify catchment-scale erosion processes and understand rates of sediment delivery, transport and deposition into the fluvial system to be able to mitigate such adverse effects. Sediment fingerprinting is a well-used tool for evaluating sediment sources, capable of directly quantifying sediment supply through differentiating sediment sources based on their inherent geochemical signatures and statistical modelling. Confluence-based sediment fingerprinting has achieved broad scale geochemical discrimination within the 5870 km2 Manawatu catchment, which drains terrain comprising soft-rock Tertiary and Quaternary sandstones, mudstones, limestones and more indurated greywacke. Multiple sediment samples were taken upstream and downstream of major river confluences, sieved to < 63 μm and analysed through step-wise discrimination, principle component analysis and a range of geochemical indicators to investigate and identify the sub- catchment geochemical signatures. -
Riparian Sites of Significance Based on the Habitat Requirements of Selected Bird Species : Technical Report to Support Policy Development
MANAGING OUR ENVIRONMENT Riparian Sites of Signifi cance Based on the Habitat Requirements of Selected Bird Species : Technical Report to Support Policy Development Riparian Sites of Significance Based on the Habitat Requirements of Selected Bird Species : Technical Report to Support Policy Development April 2007 Author James Lambie Research Associate Internally Reviewed and Approved by Alistair Beveridge and Fleur Maseyk. External Review by Fiona Bancroft (Department of Conservation (DoC)) and Ian Saville (Wrybill Birding Tours). Acknowledgements to Christopher Robertson (Ornithological Society of New Zealand), Nick Peet (DoC), Viv McGlynn (DoC), Jim Campbell (DoC), Nicola Etheridge (DoC), Gillian Dennis (DoC), Bev Taylor (DoC), John Mangos (New Zealand Defence Force), and Elaine Iddon (Horizons). Front Cover Photo Royal Spoonbill on Whanganui River tidal flats Photo: Suzanne Lambie April 2007 ISBN: 1-877413-72-0 Report No: 2007/EXT/782 CONTACT 24hr Freephone 0508 800 800 [email protected] www.horizons.govt.nz Kairanga Palmerston North Dannevirke Cnr Rongotea & 11-15 Victoria Avenue Weber Road, P O Box 201 Kairanga-Bunnythorpe Rds Private Bag 11 025 Dannevirke 4942 Palmerston North Manawatu Mail Centre Palmerston North 4442 Levin 11 Bruce Road, P O Box 680 Marton T 06 952 2800 Levin 5540 Hammond Street F 06 952 2929 SERVICE REGIONAL P O Box 289 DEPOTS Pahiatua CENTRES Marton 4741 HOUSES Cnr Huxley & Queen Streets Wanganui P O Box 44 181 Guyton Street Pahiatua 4941 Taumarunui P O Box 515 34 Maata Street Wanganui Mail Centre Taihape P O Box 194 Wanganui 4540 Torere Road, Ohotu Taumarunui 3943 F 06 345 3076 P O Box 156 Taihape 4742 EXECUTIVE SUMMARY The riparian zone represents a gradation of habitats influenced by flooding from a nearby waterway. -
Totara Reserve REGIONAL PARK
Totara Reserve REGIONAL PARK Totara Reserve Regional Park Guide to Tracks, Trails and Walks Camping Grounds Welcome to Fern Walk Totara Reserve The Fern Walk, opened in 2000, leads you through the most intact REGIONAL PARK part of the Reserve. You will enjoy kahikatea stands, nikau palm groves, and stunning examples of ancient totara, rimu and rata. Required fitness level – Moderate Walk duration – 3-4 hours Pettifar & Gilchrist Loop Tracks The Pettifar and Gilchrist Loop Tracks lead you down a series of terraces to the Pohangina River. You will pass through kahikatea- dominated forest in the wetter areas, and totara-dominated forest in drier areas. Both walks make use of the Old Coach Road, a section of the original horse and cart track along the Pohangina Valley. An abandoned tree nursery on the Gilchrist Loop Track was the source of most of the large poplars now visible throughout the Pohangina Valley. Required fitness level – Low-Moderate Walk duration – 1-2 hours for each loop track Nature Trails A network of trails behind the camping areas winds through the most varied vegetation in the Reserve. Special features include the ancient totara and matai, and one of the largest trees in the Reserve, located right alongside Churchill Drive! Required fitness level – Low Walk duration – 10 minutes -1 hour Toilet To Ashhurst Track Entrance Fern Walk At 350 hectares Totara Reserve is one of the last and largest remaining stands of the extensive forest that once covered much of the Manawatu Plains. A network of tracks takes you on a journey through the mixed podocarp forest with its tall canopy trees, shrub and forest floor communities, wide variety of birds and animals, and wonderful views of the Ruahine Ranges and Pohangina Valley. -
Hands-On Farm Experience Top in Tourism
TUESDAY, JUNE 11, 2013 11 CUSTOM DAIRY BLENDERS & Animal Feed Brokers “Local Company Working for Local Farmers” 0800 002 201 www.onlinesupplements.co.nz 5146621AB Hands-on farm experience top in tourism Bird song fills the air and in every direction there are green hills and trees. The tranquil Rangitikei Farmstay Rustic charm: won a top tourism award in Kylie Stewart inside the main the Enterprising Rural Women bunk-house, which she and contest. Jill Galloway talks her husband Andrew have to Kylie Stewart about the renovated. initiative. t’s the quiet life that attracts New up the farmstay. Many of the walls in the Part of the rural womens tourist award Zealand city dwellers and overseas guest bunk-house are festooned with old was about community involvement. people to the Rangitikei Farmstay. wool stencils and cross-cut saws. ‘‘Andrew’s father was thrilled as we Just birds, green hills and trees Another room, with a double bed and kept so much of the history of the farm dominate the rural homestay land- two singles, was built. when we developed the farmstay.’’ scape and then there is a great The Stewarts host people who can cook She says they employ people if they Istarry night-sky with no city light pol- for themselves and may choose to pay for have to feed the visitors. lution. extra activities. ‘‘Farm staff sometimes help, and Kylie and Andrew Stewart run it and There are 19 beds in total, and they are friends and family.’’ the homestay has 19 beds in mostly rustic mostly all taken in summer. -
Wai-2180-3.3.60-Ngati-Kauwhata.Pdf
Wai 2180, #3.3.60 IN THE WAITANGI TRIBUNAL WAI 2180 TAIHAPE - RANGITĪKEI KI RANGIPŌ INQUIRY DISTRICT WAI 784 IN THE MATTER of the Treaty of Waitangi Act 1975 AND IN THE MATTER of Taihape - Rangitīkei ki Rangipō Inquiry (Wai 2180) AND IN THE MATTER of a claim by Rodney Graham and others on behalf of themselves and the Kauwhata Treaty Claims Komiti and Ngā Uri Tangata o Ngāti Kauwhata ki Te Tonga (Wai 784) CLOSING SUBMISSIONS FOR THE WAI 784 NGĀTI KAUWHATA CLAIM Dated: this 20th day of October 2020 Rainey Collins PO Box 689 Solicitors DX: SP20010 Level 19 Telephone (04) 473 6850 113-119 The Terrace Facsimile (04) 473 9304 Wellington 689 Counsel: P Johnston / E Martinez / D Chong 615801.7 1 MAY IT PLEASE THE TRIBUNAL INTRODUCTION What the Crown has done to Ngāti Kauwhata throughout the motu has destabilised us – society has been eroded, and we have been deprived of much of what it is to be Ngāti Kauwhata and to be Māori. Any loss of tikanga or kawa is detrimental to our people. The Crown has restricted us in so many ways. We have been left with almost no place to exist as Māori. Our ability to exercise rangatiratanga has been taken away from us. In Kauwhata, a resurgence has begun, but there is still a long way to go.1 - Rodney Graham 1. These are the closing submissions for Wai 784, a claim by Rodney Graham and others on behalf of themselves and the Kauwhata Treaty Claims Komiti and Ngā Uri Tangata o Ngāti Kauwhata ki Te Tonga (“Wai 784 Ngāti Kauwhata claim”).