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Haast Regional Walks Brochure
Mäori first settled here at least 800 years ago, the sea, Haast Visitor Centre Introduction coast and navigable rivers providing main points of access. Mäori settlement and activity was centred around Information on the Te Wähipounamu - South West New The Haast area is more than a collection of small gathering, carving and trading precious jade, known as Zealand World Heritage Area, other lands administered by settlements near the main highway or along the road to pounamu (greenstone). Jackson Bay Okahu. It is a diverse region, stretching the Department of Conservation, tracks, accommodation European settlement was attempted at Jackson Bay Okahu from Knights Point to the Cascade Valley and inland to the and advice on recreational opportunities in the Haast area during the 1870s. The pioneers’ attempt to “tame” the forest-lined Haast Pass. The area offers a wide variety of can be obtained from the Haast Visitor Centre at Haast landscape was largely unsuccessful but their efforts left scenery, chances to view wildlife and many recreational (situated on the corner of SH6 and the Jackson Bay Road). a tradition of South Westland residents as being tough, opportunities. Hut tickets, hunting permits, maps, conservation souvenirs resilient and independent. and publications can also be obtained from the visitor The region is famous for it’s dramatic coastline - the This brochure should help visitors find their way around the centre. EFTPOS is available. sweeping curves of beaches, the rugged cliff tops, and Haast area. Displays at the Department of Conservation’s the striking rock formations at Knights Point south of Lake Haast Visitor Centre and at other sites within the World Moeraki. -
West Coast Visitor Waste Management Strategy
WEST COAST VISITOR WASTE MANAGEMENT STRATEGY AS AMENDED BY 2ND STAKEHOLDER MEETING IN GREYMOUTH ON 4TH OCTOBER 2006 PREPARED FOR : W EST COAST WASTE MANAGEMENT GROUP PREPARED BY : T OURISM RESOURCE CONSULTANTS , IN ASSOCIATION WITH LINCOLN UNIVERSITY EXECUTIVE SUMMARY This strategy has been developed to manage waste generated by visitors to the West Coast. It has been prepared for several parties: the West Coast Waste Management Working Group, an inter-agency working group consisting of: West Coast Regional Council; Buller District Council; Grey District Council; Westland District Council; Transit New Zealand; Department of Conservation; and the Ministry for Environment. Other parties also have an interest in the project, including Tourism West Coast and the Ministry of Tourism. The strategy has been prepared by Tourism Resource Consultants in association with Lincoln University. It has been prepared following meetings with council staff, Transit New Zealand, Opus and various community, waste management and visitor industry representatives on and off the West Coast. Relevant information on visitor sites and facilities were integrated into a database and ‘Hot-Spots’ (areas under substantial pressure from visitors) were identified. Our goal with this strategy is to: Minimise effects of waste generated by visitors to the West Coast. Our objectives to achieve this, are to: Provide a level of infrastructure and service that is cost-effective, integrated and of the right capacity to cope with present and future growth in the visitor industry; Provide effective information and education so that visitors use waste management facilities; Discourage non-complying activities and enforce financial consequences for visitors who are not using waste management facilities. -
West Coast Crimson Trail
WEST COAST CRIMSON TRAIL The West Coast is the rata capital of New Zealand. In the North, from the Heaphy Track to Greymouth, northern rata often dominates the forest landscape, mainly near the coast and on limestone faces. Huge trees festooned with climbing and perching plants billow above the forest canopy. On higher ground southern rata is scattered on bluffs and through beech forest. Northern rata South of Hokitika in the valleys and slopes of the beech-free main divide, Northern rata (Metrosideros robusta) is one of New Zealand’s tallest flowering trees and grows from southern rata becomes a dominant canopy tree reaching high into the Alps. Hokitika northwards. It usually begins life as an epi- And, in the far South, it forms emergent giants on the flood plains, or gnarled phyte (perching plant) high in the forest’s canopy. groups around the precipitous shores of the fiords. As its roots descend to the ground, the rata smoth- ers its host. Grows to 25m or more in height with a This Crimson Trail is a journey from the north to south on the West coast of trunk up to 2.5m in diameter. Prefers warm moist New Zealand’s South Island. As you travel some 500 kilometres you will see areas such as north-west Nelson and Northland. significant glaciers, wild coastline and large tracts of primeval forest. Northern rata grows from sea level to a maximum of 900m above sea level. Southern rata Southern rata (Metrosideros umbellata) is the most widespread rata, growing throughout New Zealand as well as in the sub-antarctic Auckland Islands. -
NEW ZEALAND NOTES·, 1954-5 by DAVID HALL
• NEW ZEALAND NOTES, 1954-5 39 1 . NEW ZEALAND NOTES·, 1954-5 By DAVID HALL HE last climbing season was notable for two things : first, the early disappearance of snow providing in early January conditions which might have been expected six weeks later ; second, the high death roll in accidents. A consequence of the lack of snow was that much rock was exposed which would have been concealed at a normal Christmas season and many slopes were uncompromisingly hard ice which would normally · have been steep, firm snow; everyone in fact had to work fairly hard for the climbs they did. But some very good climbs were done. The existence (or should one say the ' invention ') of new ten thousanders must be a perpetual menace to the peace of mind of those few choice spirits who have achieved what they hoped was an unfading garland with the ascent of all the peaks in New Zealand over 1o,ooo ft. However, Mount ' Magellan ' is not positively claimed as definitely 1o,ooo ft., although it must closely approximate to it. (Throughout these notes names cited in inverted commas have yet to receive the approval of the Geographic Board.) ' Magellan ' lies on the Balfour Range spur of Mount Teichelmann, and its first ascent was made in February by Guide Harry Ayres with B. S. Gillies and Sir Edmund Hillary and D. G. Herron; the two parties climbed some of the day on one rope. They ieft the Haast Hut at 2 A.M., were· at the summit of Teichelmann by way of Clarke Saddle by 10.45 A.M., reached their objective, after traversing a long teetery crest of snow interrupted by a formidable rock tower, at 4 P.M., and returned to the Haast Hut by the route of ascent twenty-four hours after setting forth. -
Chemical Weathering in Highsedimentyielding Watersheds
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 110, F01008, doi:10.1029/2003JF000088, 2005 Chemical weathering in high-sediment-yielding watersheds, New Zealand W. Berry Lyons and Anne E. Carey Department of Geological Sciences and Byrd Polar Research Center, Ohio State University, Columbus, Ohio, USA D. Murray Hicks NIWA Research, Christchurch, New Zealand Carmen A. Nezat1 Byrd Polar Research Center, Ohio State University, Columbus, Ohio, USA Received 3 September 2003; revised 14 September 2004; accepted 30 November 2004; published 15 February 2005. [1] We have determined the chemical erosion yields for fifteen watersheds in New Zealand, ranging in size from 12.2 to 2928 km2. These rates, coupled with previously measured physical erosion yields, allow us to compare these two modes of landscape denudation. The physical erosion yields are some of the highest measured in the world. Although in most instances the chemical erosion yields are only a small fraction of the total erosion yields, the absolute values are very high. Our data strongly support the notion that chemical erosion rates are greatly influenced by the yield of physical erosion and that the rapid production of fresh surfaces as a result of high physical erosion rates and subsequent denudation is critical to the high chemical erosion yields observed. Citation: Lyons, W. B., A. E. Carey, D. M. Hicks, and C. A. Nezat (2005), Chemical weathering in high-sediment-yielding watersheds, New Zealand, J. Geophys. Res., 110, F01008, doi:10.1029/2003JF000088. 1. Introduction Vance et al., 2003]. In general, the net, large-scale erosional potential of a landscape is thought to increase with precip- [2] Over the past decade, a debate has occurred regard- itation, drainage area and slope [Montgomery et al., 2001]. -
Touring the West Coast - Ross to Hawea — NZ Walking Access Commission Ara Hīkoi Aotearoa
9/27/2021 Touring the West Coast - Ross to Hawea — NZ Walking Access Commission Ara Hīkoi Aotearoa Touring the West Coast - Ross to Hawea Difculty Hard Length 399.8 km Journey Time 6-8 days cycling Region West Coast Part of the Collection Nga Haerenga - The New Zealand Cycle Trail ROSS TO WHATAROA (75KM, 4–6 HOURS) From Ross, head south on Highway 6 for 5km and turn right down Bold Head Road. Then, head south on the highway to tranquil Lake Ianthe (26 km from Ross and good spot for a break). Continue down the highway to a small town called Harihari. About 75km from Ross is another small town called Whataroa, which is a good stopping place for the rst night. https://www.walkingaccess.govt.nz/track/touring-the-west-coast-ross-to-hawea/pdfPreview 1/5 9/27/2021 Touring the West Coast - Ross to Hawea — NZ Walking Access Commission Ara Hīkoi Aotearoa WHATAROA TO FOX GLACIER (53KM, 3–4 HOURS) Continue south, past Lake Wahapo and Lake Mapourika to Franz Josef township (30km from Whataroa). This tourist town has many services, and is a good base for a visit to the glacier. From Franz Josef township, the 23km journey south to Fox crosses three tough hills. Fox township is a similar size to Franz Josef. The DOC visitor centres at both towns are valuable sources of information. There are two excellent cycle paths leading to each glacier. Both are easy and about 10km long. They are signposted from just south of Franz Josef, and Fox townships. -
Westland District Council Lifelines Assets
West Coast Lifelines Vulnerability and Interdependency Assessment Supplement 12: Westland District Council Lifelines Assets West Coast Civil Defence Emergency Management Group August 2017 IMPORTANT NOTES Disclaimer The information collected and presented in this report and accompanying documents by the Consultants and supplied to West Coast Civil Defence Emergency Management Group is accurate to the best of the knowledge and belief of the Consultants acting on behalf of West Coast Civil Defence Emergency Management Group. While the Consultants have exercised all reasonable skill and care in the preparation of information in this report, neither the Consultants nor West Coast Civil Defence Emergency Management Group accept any liability in contract, tort or otherwise for any loss, damage, injury or expense, whether direct, indirect or consequential, arising out of the provision of information in this report. This report has been prepared on behalf of West Coast Civil Defence Emergency Management Group by: Ian McCahon BE (Civil), David Elms BA, MSE, PhD Rob Dewhirst BE, ME (Civil) Geotech Consulting Ltd 21 Victoria Park Road Rob Dewhirst Consulting Ltd 29 Norwood Street Christchurch 38A Penruddock Rise Christchurch Westmorland Christchurch Hazard Maps The hazard maps contained in this report are regional in scope and detail, and should not be considered as a substitute for site-specific investigations and/or geotechnical engineering assessments for any project. Qualified and experienced practitioners should assess the site-specific hazard potential, including the potential for damage, at a more detailed scale. Cover Photo: Franz Josef Oxidation Ponds, March 2016. Photo from West Coast Regional Council West Coast Lifelines Vulnerability and Interdependency Assessment Supplement 12: Westland District Council Lifeline Assets . -
The Last Interglacial Sea-Level Record of Aotearoa New Zealand (Aotearoa)
The last interglacial sea-level record of Aotearoa New Zealand (Aotearoa) Deirdre D. Ryan1*, Alastair J.H. Clement2, Nathan R. Jankowski3,4, Paolo Stocchi5 1MARUM – Center for Marine Environmental Sciences, University of Bremen, Bremen, Germany 5 2School of Agriculture and Environment, Massey University, Palmerston North, New Zealand 3 Centre for Archeological Science, School of Earth, Atmospheric and Life Sciences, University of Wollongong, Wollongong, Australia 4Australian Research Council (ARC) Centre of Excellence for Australian Biodiversity and Heritage, University of Wollongong, Wollongong, Australia 10 5NIOZ, Royal Netherlands Institute for Sea Research, Coastal Systems Department, and Utrecht University, PO Box 59 1790 AB Den Burg (Texel), The Netherlands Correspondence to: Deirdre D. Ryan ([email protected]) Abstract: This paper presents the current state-of-knowledge of the Aotearoa New Zealand (Aotearoa) last interglacial (MIS 5 sensu lato) sea-level record compiled within the framework of the World Atlas of Last Interglacial Shorelines (WALIS) 15 database. Seventy-seven total relative sea-level (RSL) indicators (direct, marine-, and terrestrial-limiting points), commonly in association with marine terraces, were identified from over 120 studies reviewed. Extensive coastal deformation around New Zealand has prompted research focused on active tectonics, which requires less precision than sea-level reconstruction. The range of last interglacial paleo-shoreline elevations are resulted in a significant range of elevation measurements on both the North Island (276.8 ± 10.0 to -94.2 ± 10.6 m amsl) and South Island (173.1165.8 ± 2.0 to -70.0 ± 10.3 m amsl) and 20 prompted the use of RSL indicators tohave been used to estimate rates of vertical land movement; however, indicators in many instances lackk adequate description and age constraint for high-quality RSL indicators. -
Regional Relief Characteristics and Denudation Pattern of the Western Southern Alps, New Zealand
Geomorphology 71 (2005) 402–423 www.elsevier.com/locate/geomorph Regional relief characteristics and denudation pattern of the western Southern Alps, New Zealand Oliver Korupa,*, Jochen Schmidtb, Mauri J. McSaveneyc aWSL Swiss Federal Institute for Snow and Avalanche Research SLF, CH-7260 Davos, Switzerland bNational Institute for Water and Atmospheric Research, Christchurch, New Zealand cInstitute for Geological and Nuclear Sciences, Lower Hutt, New Zealand Received 7 June 2004; received in revised form 1 April 2005; accepted 27 April 2005 Available online 5 July 2005 Abstract The Southern Alps of New Zealand are the topographic expression of active oblique continental convergence of the Australian and Pacific plates. Despite inferred high rates of tectonic and climatic forcing, the pattern of differential uplift and erosion remains uncertain. We use a 25-m DEM to conduct a regional-scale relief analysis of a 250-km long strip of the western Southern Alps (WSA). We present a preliminary map of regional erosion and denudation by overlaying mean basin relief, a modelled stream-power erosion index, river incision rates, historic landslide denudation rates, and landslide density. The interplay between strong tectonic and climatic forcing has led to relief production that locally attains ~2 km in major catchments, with mean values of 0.65–0.68 km. Interpolation between elevations of major catchment divides indicates potential removal of l01–103 km3, or a mean basin relief of 0.51–0.85 km in the larger catchments. Local relief and inferred river incision rates into bedrock are highest about 50–67% of the distance between the Alpine fault and the main divide. -
Quaternary Geomorphology, Stratigraphy, and Paleoclimate of the Central Southern Alps, South Island, New Zealand
"""-'r-Tlnrl () » Ii z .t" INQUA 2007 (fJ ~~~"~laCial~4"~laCial Field Tour oI\) ~ New Zealand o.... Quaternary Geomorphology, Stratigraphy, and Paleoclimate of the central Southern Alps, South Island, New Zealand INQUA 2007 Post Conference Field Trip Authors: Peter Almond, David Barrell, Olivia Hyatt, Henrik Rother, James Shulmeister & Marcus Vandergoes ueU IVERSITYw Of' Lincoln UN IVERSIT Y Of' CACANTE TERBURYRBU RY University Editor & Compiler: Olivia Hyatt T.r. wit..,..wI".. .. IVWill....... ...",," 0D W",II"'"W.. I, ..,I, .. Tfr~ w"wll ..... , .~ WoIw ..... .. /i tl ../i 0" AO'.!'AO"'~' CllllITCHUaCHCI I I ISTl:H UaCH I'll"Inw UALAN&UAL .. NII' © P.C. Almond, D.J.A. Barrell, O.M. Hyatt, H. Rother, J. Shulmeister and M.J. Vandergoes 2007 ISBN 978-0-86476-189-7 Published by Lincoln University PO Box 84, Lincoln 7647, Canterbury, New Zealand 2 Authors and Leaders: Peter C. Almond, Agriculture and Life Sciences Division, Lincoln University, Canterbury, NZ. David J.A. Barrell, GNS Science, Dunedin, NZ. Olivia M. Hyatt, Department of Geological Sciences, University of Canterbury, Christchurch, NZ. Henrik Rother, ANSTO, Institute for Environmental Research, Menai, NSW, Australia. James Shulmeister, Department of Geological Sciences, University of Canterbury, Christchurch, NZ. Marcus J. Vandergoes, GNS Science, Lower Hutt, NZ. Organisers: Peter C. Almond. Fiona L. Shanhun, Agriculture and Life Sciences Division, Lincoln University, Canterbury, NZ. Editor & Compiler: Olivia M. Hyatt. Cover images, Jamie Shulmeister, Olivia Hyatt and Andrew Wells Contents Introduction 5 Day 1. Christchurch to Twizel, with stops in the Rakaia Valley and Mackenzie Basin 8 Christchurch to Glentunnel 8 Glentunnel to Rakaia Gorge 9 Stop 1-1. -
SUMMARY of RESOURCE CONSENT APPLICATIONS As at 13/10/15 Appln Applicant Description Location Date No
SUMMARY OF RESOURCE CONSENT APPLICATIONS As at 13/10/15 Appln Applicant Description Location Date No. Received 150090 Peter Black To use land described as Lot 1 DP 415563, at Ruatapu-Ross Road 06/10/15 Ruatapu-Ross Road, for residential purposes including a dwelling and accessory buildings as submitted in an application and plans received 6th October 2015. 150089 Cloud 9 To use land described as Lot 2 DP 458483, at 8 8 Greyhound Road 13/10/15 Enterprises Greyhound Road, to reduce front yard setback to 8 Limited metres to facilitate an accessory building as submitted in an application and plans received 13th October 2015. 150088 Westland Milk To use land described as Lot 3 DP 2695 at Town Town Belt East 07/10/15 Products Ltd Belt East, Hokitika, for general industrial activities including storage and informal parking. This consent proceeds to formalise the existing temporary on site activity as submitted in an application and plans received 7th October 2015. 150087 Spark NZ Ltd To use land described as Part Rural Section 5472, at Hokitika Airport 02/10/15 Hokitika Airport, to establish a telecommunication facility which has a tower that exceeds 25 metres in height and an accessory building with a ground coverage of more than 15m2. The proposal includes relocating the existing Spark tower and equipment container from the Seaview site. A 4.4 metre high mobile telephone service (MTS), a nine-panel antenna and associated equipment will be added to the tower. The maximum height of the antenna will be 33 metres as submitted in an application and plans received 2nd October 2015. -
South Island Fishing Regulations for 2020
Fish & Game 1 2 3 4 5 6 Check www.fishandgame.org.nz for details of regional boundaries Code of Conduct ....................................................................4 National Sports Fishing Regulations ...................................... 5 First Schedule ......................................................................... 7 1. Nelson/Marlborough .......................................................... 11 2. West Coast ........................................................................16 3. North Canterbury ............................................................. 23 4. Central South Island ......................................................... 33 5. Otago ................................................................................44 6. Southland .........................................................................54 The regulations printed in this guide booklet are subject to the Minister of Conservation’s approval. A copy of the published Anglers’ Notice in the New Zealand Gazette is available on www.fishandgame.org.nz Cover Photo: Jaymie Challis 3 Regulations CODE OF CONDUCT Please consider the rights of others and observe the anglers’ code of conduct • Always ask permission from the land occupier before crossing private property unless a Fish & Game access sign is present. • Do not park vehicles so that they obstruct gateways or cause a hazard on the road or access way. • Always use gates, stiles or other recognised access points and avoid damage to fences. • Leave everything as you found it. If a gate is open or closed leave it that way. • A farm is the owner’s livelihood and if they say no dogs, then please respect this. • When driving on riverbeds keep to marked tracks or park on the bank and walk to your fishing spot. • Never push in on a pool occupied by another angler. If you are in any doubt have a chat and work out who goes where. • However, if agreed to share the pool then always enter behind any angler already there. • Move upstream or downstream with every few casts (unless you are alone).