West Coast Landowners Information
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THE FATAL ACCIDENT in OTIRA TUNNEL. . Before 1864 Maori
THE FATAL ACCIDENT IN OTIRA TUNNEL. Stephen WOOD, killed during construction of the Otira Tunnel Before 1864 Maori travelled through the Bealey and Otira valleys on their journeys to Westland in search of greenstone though they chose a less steep route, often through the Harper Pass, for the return journey. Arthur's Pass is 920 metres above sea level, and there is a steep descent to Otira in the west. Arthur's Pass is named after Arthur Dudley Dobson, an explorer/surveyor who discovered the pass in 1864. In 1865 a tent camp was set up for surveyors to prepare for the construction of the road to the West Coast where gold had been discovered in 1864. In 1866 the road was opened for coach traffic, and Cobb and Co coaches began to take passengers and mail over this hazardous road. The coaches set out from Christchurch, crossing the unbridged Waimakariri River, following the Bealey River up to the Arthur's Pass Village, climbing to the top of the Pass, descending through the Otira Gorge to the village of Otira, and then continuing to Hokitika. The journey took thirty six hours with an overnight stop at Bealey. In 1901 the Arthur's Pass National Park was established on the suggestion of Dr Leonard Cockayne. 72,000 hectares around the headwaters of the Waimakariri, Arthur's Pass and Otira were reserved for national park purposes under the provisions of the Land Act 1892. It was New Zealand's third National Park and now encompasses an area of 114.000 hectares. In 1883 a Royal Commission had decided that the Arthur's Pass route was the best for the railway to link the east and west coasts. -
May 2019, Issue 4
THE NEWS MAY 2019 S ISSUE 5 REDUCTION READINESS RESPONSE RECOVERY IN THIS ISSUE > Westland bears the brunt of heavy rainfall > AF8 Roadshow > Understanding the risk > New Zealand ShakeOut 2019 > Kid's time! Welcome to our Autumn newsletter! Looking after yourself and your family in an emergency | Readiness plans Many disasters will affect A household emergency plan will help you work out: essential services and possibly n What you will each do in the event n How and when to turn off the water, disrupt your ability to travel or of disasters such as an earthquake, electricity and gas at the main communicate with each other. tsunami, volcanic eruption, flood or switches in your home or business. storm. You may be confined to your home or Turn off gas only if you suspect a n How and where you will meet up during forced to evacuate your neighbourhood. leak, or if you are instructed to do so and after a disaster. In the immediate aftermath of a disaster, by authorities. If you turn the gas off emergency services may not be able to get n Where to store emergency survival you will need a professional to turn it help to everyone as quickly as needed. items and who will be responsible for back on and it may take them weeks to maintaining supplies. This is when you are likely to be most respond after an event. n vulnerable, so it is important to plan to What you will each need to have in your n What local radio stations to tune in to look after yourself and your loved ones getaway kits and where to keep them. -
The New Zealand Gazette. 497
MAR. 4.] THE NEW ZEALAND GAZETTE. 497 MILITARY DISTRICT No. 9 ,(NELSON)--oontmued. MILITARY DISTRICT No. 9 (NELSON)--oontinued. 383641 Home, Earl Reid, religious worker, Greenwood St., Motueka. 284958 Johnston, John Marcus, herd-tester, Budge St., Blenheim. 271736 Hooper, Vernon Graham, grocer's assistant, Wakefield, 287372 Johnstone, John Murdoch Sidney Merewether, engineer and Nelson. fitter, North Revell St., Hokitika. 427329 Hope, Harry Beresford, stores labourer, Public Works De 265106 Johnstone, John Smith, orchard worker, Haslep Rd., Tasman partment, Bruce Bay, South Westland. RurA.1 Mail Delivery, Upper Moutere. 261221 Hope, Pat McKellar, shepherd and drover, Deep Bay, French 425997 Jones, Edward Lloyd, miner, 17 Richmond St., Cobden, Pass. Greymouth. 276659 Hopgood, Walter Francis, lime-worker, Cape Foulwind. 276757 Jones, Frederick; loco-driver, Granity. 426079 Hopley, William James, coal-miner, Dawson's Hotel, 249413 Jones, George William, bus-driver, Premier Garage, Grey Reefton. mouth. 286081 Hornal, Robert James, miner, Wallsend, Brunnerton. 285309 Jones, Innes Ralph Rutland, dairy-farm!'r, Havelock, Marl- 177942 Hornby, William Charles, sawmiller, Ruru, West Coast. borough. 287125 Horne, Douglas Louis, builder, care of Hannah and Dyer, 238937 Jones, Jack, yard hand, Moorehouse St., Ross. Builders, Mental Hospital, Hokitika. 287458 Jones, Lemuel David, labourer, Jackson's Bay. 427260 Hornell, Arthur Thomas, timber-worker, Karangarua, South 264592 Jones, 'William Peter, farm labourer, Kokatahi. · Westland. 426688 Jope, George Edwa.rd, lorry-driver, Cape Foulwind. 050884 Horner, James Muir, farm-assistant, Murchison. 426061 Jope, Thomas Richard, labourer, care of Mr. A. E. Taylor, 233611 Horrell, Norman Nelson, sawmill hand, Upper Moutere Disraeli St., Westport. Rural Delivery. 373503 Jordan, Frederick Williams, constable, Hokitika. -
GNS Science Miscellaneous Series Report
NHRP Contestable Research Project A New Paradigm for Alpine Fault Paleoseismicity: The Northern Section of the Alpine Fault R Langridge JD Howarth GNS Science Miscellaneous Series 121 November 2018 DISCLAIMER The Institute of Geological and Nuclear Sciences Limited (GNS Science) and its funders give no warranties of any kind concerning the accuracy, completeness, timeliness or fitness for purpose of the contents of this report. GNS Science accepts no responsibility for any actions taken based on, or reliance placed on the contents of this report and GNS Science and its funders exclude to the full extent permitted by law liability for any loss, damage or expense, direct or indirect, and however caused, whether through negligence or otherwise, resulting from any person’s or organisation’s use of, or reliance on, the contents of this report. BIBLIOGRAPHIC REFERENCE Langridge, R.M., Howarth, J.D. 2018. A New Paradigm for Alpine Fault Paleoseismicity: The Northern Section of the Alpine Fault. Lower Hutt (NZ): GNS Science. 49 p. (GNS Science miscellaneous series 121). doi:10.21420/G2WS9H RM Langridge, GNS Science, PO Box 30-368, Lower Hutt, New Zealand JD Howarth, Dept. of Earth Sciences, Victoria University of Wellington, New Zealand © Institute of Geological and Nuclear Sciences Limited, 2018 www.gns.cri.nz ISSN 1177-2441 (print) ISSN 1172-2886 (online) ISBN (print): 978-1-98-853079-6 ISBN (online): 978-1-98-853080-2 http://dx.doi.org/10.21420/G2WS9H CONTENTS ABSTRACT ......................................................................................................................... IV KEYWORDS ......................................................................................................................... V KEY MESSAGES FOR MEDIA ............................................................................................ VI 1.0 INTRODUCTION ........................................................................................................ 7 2.0 RESEARCH AIM 1.1 — ACQUIRE NEW AIRBORNE LIDAR COVERAGE .............. -
Download Manuscript (Pdf)
DEVELOPING BEST MANAGEMENT GUIDELINES FOR EFFLUENT APPLICATION IN HIGH RAINFALL REGIONS S. Laurenson1, D.J. Houlbrooke2, R. Monaghan1 T. Wilson3, S. Morgan4 1AgResearch, Invermay Agriculture Centre, Private Bag 50034, Mosgiel, New Zealand 2AgResearch, Ruakura, Private Bag 3123, Hamilton 3240 3DairyNZ, Private Bag 3221, Hamilton 3240 4Westland Milk Products, PO Box 96 Hokitika E-mail: [email protected] Abstract Two- (or more) pond treatment systems discharging to water have traditionally been used for managing farm dairy effluent (FDE) on the West Coast. Many existing systems continue to discharge FDE directly into high volume, short reach rivers. This practice has come under recent scrutiny due to the potential effects of soluble P on the water quality of Lake Brunner. Application of FDE to land at a suitable irrigation depth (mm) and rate (mm/hr) is an alternative option with potential to curtail surface water pollution associated with direct discharge and recycle valuable nutrients for agronomic benefit. However, this approach does present some challenges because high annual rainfall (i.e. approx 4.8m per annum) results in a large volume of water collected from the dairy shed catchment areas while and also limits the development of soil water deficits that are large enough to safely apply FDE to land with high risk soils. The West Coast Regional Council (WCRC) intends to develop regulatory options for the management of FDE in the Lake Brunner Catchment that employ a decision support framework for application to land. Many West Coast soils would be defined as ‘high risk’ due to poor natural drainage or the hump and hollow drainage systems. -
Waiho River Flooding Risk Assessment MCDEM 2002.Pdf
Report 80295/2 Page i WAIHO RIVER FLOODING RISK ASSESSMENT For MINISTRY OF CIVIL DEFENCE & EMERGENCY MANAGEMENT AUGUST 2002 Report 80295/2 Page ii PROJECT CONTROL Consultant Details Project Leader: Adam Milligan Phone: 04 471 2733 Project Team: Fax: 04 471 2734 Organisation: Optimx Limited Postal Address: P O Box 942, Wellington Peer Reviewer Details Reviewer: David Elms Phone: 03 364 2379 Position: Director Fax: 03 364 2758 Organisation: Optimx Limited Postal Address: Department of Civil Engineering University of Canterbury Private Bag 4800, Christchurch Client Details Client: Ministry of Civil Defence & Emergency Postal Address: PO Box 5010 Management Wellington Client contact: Richard O’Reilly Phone: 04 473 7363 Project Details Project: Waiho River Flooding Risk Assessment Project No.: 80295 Version Status File Date Approval signatory 1 Draft 80295 MCDEM Waiho River Risk Assessment Report - Aug 2002 David Elms Version 1.doc 2 Final Draft 80295 MCDEM Waiho River Risk Assessment Report - Aug 2002 David Elms Version 2.doc 3 Final 80295 MCDEM Waiho River Risk Assessment Report - Aug 2002 David Elms FINAL.doc This report has been prepared at the specific instructions of the Client. Only the Client is entitled to rely upon this report, and then only for the purpose stated. Optimx Limited accept no liability to anyone other than the Client in any way in relation to this report and the content of it and any direct or indirect effect this report my have. Optimx Limited does not contemplate anyone else relying on this report or that it will be used for any other purpose. Should anyone wish to discuss the content of this report with Optimx Limited, they are welcome to contact the project leader at the address stated above. -
WEST COAST STATUS REPORT Meeting Paper for West Coast Tai Poutini Conservation Board
WEST COAST STATUS REPORT Meeting Paper For West Coast Tai Poutini Conservation Board TITLE OF PAPER STATUS REPORT AUTHOR: Mark Davies SUBJECT: Status Report for the Board for period ending 15 April 2016 DATE: 21 April 2016 SUMMARY: This report provides information on activities throughout the West Coast since the 19 February 2016 meeting of the West Coast Tai Poutini Conservation Board. MARINE PLACE The Operational Plan for the West Coast Marine Reserves is progressing well. The document will be sent out for Iwi comment on during May. MONITORING The local West Coast monitoring team completed possum monitoring in the Hope and Stafford valleys. The Hope and Stafford valleys are one of the last places possums reached in New Zealand, arriving in the 1990’s. The Hope valley is treated regularly with aerial 1080, the Stafford is not treated. The aim is to keep possum numbers below 5% RTC in the Hope valley and the current monitor found an RTC of 1.3% +/- 1.2%. The Stafford valley is also measured as a non-treatment pair for the Hope valley, it had an RTC of 21.5% +/- 6.2%. Stands of dead tree fuchsia were noted in the Stafford valley, and few mistletoe were spotted. In comparison, the Hope Valley has abundant mistletoe and healthy stands of fuchsia. Mistletoe recruitment plots, FBI and 20x20m plots were measured in the Hope this year, and will be measured in the Stafford valley next year. KARAMEA PLACE Planning Resource Consents received, Regional and District Plans, Management Planning One resource consent was received for in-stream drainage works. -
Franz Josef Glacier Township
Mt. Tasman Mt. Cook FRANZ JOSEF IMPORTANT PHONE NUMBERS www.glaciercountry.co.nz EMERGENCY Dial 111 POLICE (Franz Josef) 752 0044 D Franz Josef Health Clinic 752 0700 GLACIER TOWNSHIP Glacier The Visitor Centre at Franz Josef is open 7 days. I After hours information is available at the front I I entrance of the Visitor Centre/DOC offi ce. H Times given are from the start of track and are approximate I 1 A A. GLACIER VALLEY WALK 1 1 hour 20 mins return following the Waiho riverbed 2 20 G B to the glacier terminal. Please heed all signs & barriers. 14 B. SENTINEL ROCK WALK Condon Street 21 C 3 15 24 23 20 mins return. A steady climb for views of the glacier. 5 4 Cron Street 16 C. DOUGLAS WALK/PETERS POOL 25 22 43 42 12 26 20 mins return to Peter’s Pool for a fantastic 13 9 6 31 GLACIER E refl ective view up the glacier valley. 1 hour loop. 11 7 17 30 27 45 44 10 9 8 Street Cowan 29 28 ACCESS ROAD F D. ROBERTS POINT TRACK 18 33 32 Franz Josef 5 hours return. Climb via a rocky track and 35 33 State Highway 6 J Glacier Lake Wallace St Wallace 34 19 Wombat swingbridges to a high viewpoint above glacier. 40 37 36 Bus township to E. LAKE WOMBAT TRACK 41 39 38 Stop glacier carpark 40 State Highway 6 1 hour 30mins return. Easy forest walk to small refl ective pond. 46 is 5 km 2 hour F. -
Download the Fox Glacier Township
Mt. Tasman Mt. Cook FOX GLACIER TOWNSHIP www.GLACIERCOUNTRY.CO.NZ North to: FRANZ JOSEF GLACIER (30 mins drive) Hokitika, Greymouth CAMPING IS ONLY PERMITTED AT Health Clinic COMMERCIAL & DOC SITES Fox Glacier 1 2 6 GLACIER ACCESS 17 7 Sullivan3 Road Fox Glacier Airstrip 8 4 ROAD D 5 Fox Glacier township to 10 glacier carpark is 6 km LAKE MATHESON 18 11 13 (10 minutes drive). Fox Glacier township to Lake 26 i Matheson carpark is 6km, a 2 hour 27 20 12 14 return walk or 5 minute drive. 19 23 21 15 A C FIRE 29 22 24 Pekanga Drive State Highway 6 30 Glacier Access Road E Frames Road Lake Matheson 31 Glacier View Road Kerrs Road Fox B School N River 32 33 MAP NOT TO SCALE South to: F 34 Bruce Bay, Lake Paringa, Haast, Wanaka and Lake Matheson35 Road Cook Flat Road Queenstown 37 Williams Drive 36 G - Peak 39 (46 km) Viewpoint 10 Fox General Store 751 0829 The Visitor Centre at Franz Josef (open 7 days) and the DOC Office at Fox Glacier (open Mon-Fri, closed weekends and public Mahitahi Lodge 23 The Hobnail Shop - Gifts and Souvenirs 751 0825 holidays) offers information about Westland Tai Poutini National 35 ReflectioNZ Gifts & Gallery 751 0753 Park and Te Wahipounamu South West New Zealand World West to: SHOPS Heritage Area. Hut tickets and hunting permits are issued. After 40 (60 km) Gillespies Beach hours information is available outside the front entrance to both (21 km drive) The Salmon Farm from Fox township. -
Overview of the Westland Cultural Heritage Tourism Development Plan 1
Overview of the Westland Cultural Heritage Tourism Development Plan 1. CULTURAL HERITAGE THEMES DEVELOPMENT • Foundation Māori Settlement Heritage Theme – Pounamu: To be developed by Poutini Ngāi Tahu with Te Ara Pounamu Project • Foundation Pākehā Settlement Heritage Theme – West Coast Rain Forest Wilderness Gold Rush • Hokitika - Gold Rush Port, Emporium and Administrative Capital actually on the goldfields • Ross – New Zealand’s most diverse goldfield in terms of types of gold deposits and mining methods • Cultural Themes – Artisans, Food, Products, Recreation derived from untamed, natural wilderness 2. TOWN ENVIRONMENT ENHANCEMENTS 2.1 Hokitika Revitalisation • Cultural Heritage Precincts, Walkways, Interpretation, Public Art and Tohu Whenua Site • Wayfinders and Directional Signs (English, Te Reo Māori, Chinese) 2.2 Ross Enhancement • Enhancement and Experience Plan Development • Wayfinders and Directional Signs (English, Te Reo Māori, Chinese) 3. COMMERCIAL BUSINESS DEVELOPMENT • Go Wild Hokitika and other businesses at TRENZ 2020 • Chinese Visitor Business Cluster • Mahinapua Natural and Cultural Heritage Iconic Attraction 4. COMMUNITY OWNED BUSINESSES AND ACTIVITIES • Westland Industrial Heritage Park Experience Development • Ross Goldfields Heritage Centre and Area Experience Development 5. MARKETING • April 2020 KUMARA JUNCTION to GREYMOUTH Taramakau 73 River Kapitea Creek Overview of the Westland CulturalCHESTERFIELD Heritage 6 KUMARA AWATUNA Londonderry West Coast Rock Tourism Development Plan Wilderness Trail German Gully -
The Ecology of Whataroa Virus, an Alphavirus, in South Westland, New Zealand by J
J. Hyg., Camb. (1973), 71, 701 701 Printed in Great Britain The ecology of Whataroa virus, an alphavirus, in South Westland, New Zealand BY J. A. R. MILES Department of Microbiology, Medical School, University of Otago, Dunedin, New Zealand (Received 6 March 1973) SUMMARY The findings of a survey on the ecology of an alphavirus over the years 1964-9 are reviewed. Evidence is presented to show that wild birds constitute a vertebrate reservoir of the virus and that mosquitoes, primarily Culiseta tonnoiri and Gulex pervigilans, which are both endemic New Zealand species, are responsible for summer transmission. Serological evidence of infection was obtained in all years and evidence is presented to indicate that the virus is enzootic rather than being reintroduced each spring. The number of birds with antibody increased before mosquitoes became active in the spring and possible explanations of this are discussed. The mean temperature in the hottest month in the study area is substantially below that in other areas with enzootic mosquito-borne viruses and experimental studies showed that Whataroa virus was able to replicate more rapidly in mos- quitoes at low temperatures than any arboviruses previously studied. The main natural focus of infection appeared to be in a modified habitat and the introduced song thrush (Turdus philomelos) to be the main vertebrate reservoir host. INTRODUCTION In New Zealand a number of rural summer epidemics of influenza-like disease suggestive of an arbovirus aetiology have occurred. Because of this a serological survey covering a variety of climatic and biological zones throughout the country was initiated in 1959-60. -
An Unusual Plant Community on Some Westland Piedmont Moraines, by G. Rennison and J. L. Brock, P
223 AN UNUSUAL PLANT COMMUNITY ON SOME SOUTH WESTLAND PIEDMONT MORAINES by G. Rennison* and J.L. Brockf In South Westland there is an extensive area of piedmont moraines lying between the sea and the western scarp of the Southern Alps, and bounded by the Waiho River to the north and the Cook River to the south (Fig. 1). In the main the existing vegetation is podocarp-broadleaf forest, but with small pockets of a plant community which has definite alpine affinities. From the air these show up as light-coloured areas against the dark forest, and occupy areas of infertile terrace. For an explanation of their occurrence an outline of the recent geological history is pertinent. Late Pleistocene History of the Moraines Approximately two thirds of the moraines are mapped as Okarito Formation and the rest as Moana Formation (Warren, 1967; Fig. 2). Both were formed during the advance of the Otira Glaciation, the Okarito Formation being correlated with the Kumara-2 and early Kumara-3 advance, and the Moana Formation with the later Kumara-3 advance (Suggate, 1965). The Okarito Formation may also include remnants of moraines formed by the earlier Waimea Glaciation. From radio-carbon dating, Suggate suggests that the early Kumara-3 advance commenced approximately 16,000 years before present (BP). The late Kumara-3 advance commenced approximately 1,500 years later (14,500 BP) and resulted in the Fox and Franz Josef Glaciers being extended beyond the present coastline, with an extensive lateral moraine complex being formed along the periphery of the Okarito Formation. Vegetation Development on the Moraines The following is an outline of the possible mode of vegetation development on these piedmont moraines: 1.