Hump Ridge Feb 25 - March 1, 2021 5 Days 4 Nights
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FIORDLAND NATIONAL PARK 287 ( P311 ) © Lonely Planet Publications Planet Lonely ©
© Lonely Planet Publications 287 Fiordland National Park Fiordland National Park, the largest slice of the Te Wahipounamu-Southwest New Zealand World Heritage Area, is one of New Zealand’s finest outdoor treasures. At 12,523 sq km, Fiordland is the country’s largest park, and one of the largest in the world. It stretches from Martins Bay in the north to Te Waewae Bay in the south, and is bordered by the Tasman Sea on one side and a series of deep lakes on the other. In between are rugged ranges with sharp granite peaks and narrow valleys, 14 of New Zealand’s most beautiful fiords, and the country’s best collection of waterfalls. The rugged terrain, rainforest-like bush and abundant water have kept progress and people out of much of the park. Fiordland’s fringes are easily visited, but most of the park is impenetrable to all but the hardiest trampers, making it a true wilderness in every sense. The most intimate way to experience Fiordland is on foot. There are more than 500km of tracks, and more than 60 huts scattered along them. The most famous track in New Zealand is the Milford Track. Often labelled the ‘finest walk in the world’, the Milford is almost a pilgrimage to many Kiwis. Right from the beginning the Milford has been a highly regulated and commercial venture, and this has deterred some trampers. However, despite the high costs and the abundance of buildings on the manicured track, it’s still a wonderfully scenic tramp. There are many other tracks in Fiordland. -
Download Itinerary
HUMP RIDGE TRACK ITINERARY Situated on the south-west corner of New Zealand’s South Island, the Tuatapere Hump Ridge Track is 3-day loop walk that takes hikers along the south coast of New Zealand, up to the sub-alpine zone of the Hump Ridge, and over historic viaducts in the heart of native forest. There are commanding views of the south coast, Lake Poteriteri, Lake Hauroko and mountain ranges deep in Fiordland National Park. Walk through 13 marine coastal terraces in the Waitutu Forest, which Dr David Bellamy described as “probably the most important forest in the world”. This ancient terraced forest rises out of the sea with each level being 100,000 years older than the last. It remains pristine and unspoiled. Experienced guides will provide you with an intimate knowledge of the area, enriching your vacation. All the organising will be done for you and your gear helicoptered on day 1 so that you can focus on the delights and make the most of your walking holiday. LENGTH 3.5 days GRADE C (some alpine hiking and uneven terrain) START Day 1: Pre-track briefing, 5:30pm, at Tuatapere Hump Ridge office, 31 Orawia Rd, Tuatapere. (transfers available from Queenstown/Te Anau) FINISH Tuatapere 3pm (transfers available to Te Anau arriving 4:45pm and Queenstown 7:30pm) DEPARTURES 2021 Nov: 1, 4, 15, 18 | Dec: 2, 9, 13, 16 | 2022 Jan: 6, 13, 20 | Feb: 10, 17, 28 | Mar: 3, 6, 24, 31 | Apr: 7 2022 Oct: 31 | Nov: 10, 14, 24, 28 | Dec: 8, 12, 15, 19 2023 Jan: 5, 9, 19, 23 | Feb: 2, 6, 20 | Mar: 2, 6, 16, 20, 23, 30 | Apr: 3, 6 PRICE 1 Nov 2021 - 31 May 2023 Adult ex Tuatapere NZD $1,795.00 Private room upgrade (per room, for both nights) NZD $250.00 Transfer from Te Anau (return, per person) NZD $75.00 Transfer from Invercargill (return, per person) NZD $95.00 Transfer from Queenstown (return, per person) NZD $150.00 Single supplement (individual travellers - pre night accommodation) NZD $50.00 Minimum age: 10 years. -
California State University, Northridge Strain Localization Within Arc Crust
California State University, Northridge Strain Localization within Arc Crust: Microstructural Investigation of the Grebe Mylonite Zone in Fiordland, New Zealand A thesis submitted in partial fulfillment of the requirements For the degree of Master of Science in Geological Sciences By Lonnie Hufford August 2018 The thesis of Lonnie Hufford is approved: _________________________________________ ______________ Dr. Keith Klepeis Date _________________________________________ ______________ Dr. Joshua Schwartz Date _________________________________________ ______________ Dr. Elena Miranda, Chair Date California State University, Northridge ii ACKNOWLEDGMENTS I would like to thank the following people for their help and support with this thesis: Dr. Miranda’s ability to explain microstructural concepts in an understandable way was critical to my completion of this thesis. The professionalism and desire she had for me to produce the best work I could is something I deeply appreciate and have used to grow as a scientist. Dr. Schwartz’s geochemical knowledge and patience when I was trying to interpret my data is extremely appreciated. Dr. Klepeis’ ideas prompted me to think about how the Grebe Mylonite Zone compares to other regions which helped me focus on large-scale Fiordland geology. My family for their love and support. It is a blessing to have a mother, stepfather, and sisters who are always there for you. Dr. Peng for saving the SEM, even on the weekends. Dr. Andrew Cross for his help with MTEX code. Dr. Turnbull for her help with interpreting geochemistry data. Dr. Hielscher for his help with MTEX code. All the faculty and staff at CSUN for their help and support. Caroline, Courtney, Luisa, and Solishia for being such amazing research team peers. -
Section 6 Schedules 27 June 2001 Page 197
SECTION 6 SCHEDULES Southland District Plan Section 6 Schedules 27 June 2001 Page 197 SECTION 6: SCHEDULES SCHEDULE SUBJECT MATTER RELEVANT SECTION PAGE 6.1 Designations and Requirements 3.13 Public Works 199 6.2 Reserves 208 6.3 Rivers and Streams requiring Esplanade Mechanisms 3.7 Financial and Reserve 215 Requirements 6.4 Roading Hierarchy 3.2 Transportation 217 6.5 Design Vehicles 3.2 Transportation 221 6.6 Parking and Access Layouts 3.2 Transportation 213 6.7 Vehicle Parking Requirements 3.2 Transportation 227 6.8 Archaeological Sites 3.4 Heritage 228 6.9 Registered Historic Buildings, Places and Sites 3.4 Heritage 251 6.10 Local Historic Significance (Unregistered) 3.4 Heritage 253 6.11 Sites of Natural or Unique Significance 3.4 Heritage 254 6.12 Significant Tree and Bush Stands 3.4 Heritage 255 6.13 Significant Geological Sites and Landforms 3.4 Heritage 258 6.14 Significant Wetland and Wildlife Habitats 3.4 Heritage 274 6.15 Amalgamated with Schedule 6.14 277 6.16 Information Requirements for Resource Consent 2.2 The Planning Process 278 Applications 6.17 Guidelines for Signs 4.5 Urban Resource Area 281 6.18 Airport Approach Vectors 3.2 Transportation 283 6.19 Waterbody Speed Limits and Reserved Areas 3.5 Water 284 6.20 Reserve Development Programme 3.7 Financial and Reserve 286 Requirements 6.21 Railway Sight Lines 3.2 Transportation 287 6.22 Edendale Dairy Plant Development Concept Plan 288 6.23 Stewart Island Industrial Area Concept Plan 293 6.24 Wilding Trees Maps 295 6.25 Te Anau Residential Zone B 298 6.26 Eweburn Resource Area 301 Southland District Plan Section 6 Schedules 27 June 2001 Page 198 6.1 DESIGNATIONS AND REQUIREMENTS This Schedule cross references with Section 3.13 at Page 124 Desig. -
Tuatapere-Community-Response-Plan
NTON Southland has NO Civil Defence sirens (fire brigade sirens are not used as warnings for a Civil Defence emergency) Tuatapere Community Response Plan 2018 If you’d like to become part of the Tuatapere Community Response Group Please email [email protected] Find more information on how you can be prepared for an emergency www.cdsouthland.nz Community Response Planning In the event of an emergency, communities may need to support themselves for up to 10 days before assistance arrives. The more prepared a community is, the more likely it is that the community will be able to look after themselves and others. This plan contains a short demographic description of Tuatapere, information about key hazards and risks, information about Community Emergency Hubs where the community can gather, and important contact information to help the community respond effectively. Members of the Tuatapere Community Response Group have developed the information contained in this plan and will be Emergency Management Southland’s first point of community contact in an emergency. Demographic details • Tuatapere is contained within the Southland District Council area; • The Tuatapere area has a population of approximately 1,940. Tuatapere has a population of about 558; • The main industries in the area include agriculture, forestry, sawmilling, fishing and transportation; • The town has a medical centre, ambulance, police and fire service. There are also fire stations at Orepuki and Blackmount; • There are two primary schools in the area. Waiau Area School and Hauroko Primary School, as well as various preschool options; • The broad geographic area for the Tuatapere Community Response Plan includes lower southwest Fiordland, Lake Hauroko, Lake Monowai, Blackmount, Cliften, Orepuki and Pahia, see the map below for a more detailed indication; • This is not to limit the area, but to give an indication of the extent of the geographic district. -
RESEARCH the Tempo of Continental Arc Construction in the Mesozoic
RESEARCH The tempo of continental arc construction in the Mesozoic Median Batholith, Fiordland, New Zealand Joshua J. Schwartz1,*, Keith A. Klepeis2, Joseph F. Sadorski1, Harold H. Stowell3, Andy J. Tulloch4, and Matthew A. Coble5 1DEPARTMENT OF GEOLOGICAL SCIENCES, CALIFORNIA STATE UNIVERSITY NORTHRIDGE, 18111 NORDHOFF STREET, NORTHRIDGE, CALIFORNIA 91330, USA 2DEPARTMENT OF GEOLOGY, UNIVERSITY OF VERMONT, 180 COLCHESTER AVENUE, BURLINGTON, VERMONT 05405, USA 3DEPARTMENT OF GEOLOGICAL SCIENCES, UNIVERSITY OF ALABAMA, 201 7TH AVENUE, ROOM 2003 BEVILL BUILDING, TUSCALOOSA, ALABAMA 35487, USA 4GNS SCIENCE, 764 CUMBERLAND STREET, DUNEDIN 9016, PRIVATE BAG 1930, DUNEDIN 9054, NEW ZEALAND 5SCHOOL OF EARTH, ENERGY & ENVIRONMENTAL SCIENCES, STANFORD UNIVERSITY, 397 PANAMA MALL, MITCHELL BUILDING 101, STANFORD, CALIFORNIA 94305, USA ABSTRACT We investigate the temporal record of magmatism in the Fiordland sector of the Median Batholith (New Zealand) with the goal of evaluating models for cyclic and episodic patterns of magmatism and deformation in continental arcs. We compare 20 U-Pb zircon ages from >2300 km2 of Mesozoic lower and middle crust of the Western Fiordland Orthogneiss to existing data from the Median Batholith to: (1) document the tempo of arc construction, (2) estimate rates of magmatic addition at various depths during arc construction, and (3) evaluate the role of cyclical feedbacks between magmatism and deformation during high and low magma addition rate events. Results from the Western Fiordland Orthogneiss indicate that the oldest dates are distributed in northern and southern extremities: the Worsley Pluton (123–121 Ma), eastern McKerr Intrusives (128–120 Ma), and Breaksea Orthogneiss (123 Ma). Dates within the interior of the Western Fiordland Orthogneiss (Misty and Malaspina Plutons, western McKerr Intrusives) primarily range from 118 to 115 Ma and signify a major flux of mafic to interme- diate magmatism during which nearly 70% of the arc root was emplaced during a brief, ~3 m.y., interval. -
Percy Burn Hut, Fiordland National Park
Percy Burn Hut, Fiordland National Park WILD FILE Access 28km west of Tuatapere Grade Easy-moderate Times Rarakau to Port Craig 5-7hr; Port Craig to Percy Burn Hut 1½-2hr; Percy Burn Hut to Wairaurahiri Hut 2.5-3hr Distance 33km to Wairaurahiri River Accommodation Port Craig School Hut, 20 bunks; Wairaurahiri Hut, 14 bunks; Percy Burn Hut, 18 bunks Map CG07, CG06 Description Head through regrowth forest along the clifftop before a steep descent takes you on to Bluecliffs Beach. It takes a good hour to get from the Waikoau River to the western end of the beach, and then a short walk on the remains of the road to the boundary of Fiordland National Park and the start of the track proper. As much of the South Coast Track is now part of the Hump Ridge Track, it’s seen quite a bit of development in recent years, and the legendary mud is largely no more. So, a quick walk takes you to the bridge over Pipi Tuariki Stream (known locally as Flat Stream), past the turnoff to the ascent to Okaka Hut and down onto Blowhole Beach. The track crosses a couple of small headlands, which can be bypassed at low tide, before reaching O Hoka Stream. This is the decision point for choosing a low tide route along the stunning beach or the slightly longer inland route to Port Craig. From here, it’s a little over an hour to the Sand Hill Viaduct, and another 10 minutes to Percy Burn, the site of probably the largest surviving wooden viaduct in the world. -
Southland Trail Notes Contents
22 October 2020 Southland trail notes Contents • Mararoa River Track • Tākitimu Track • Birchwood to Merrivale • Longwood Forest Track • Long Hilly Track • Tīhaka Beach Track • Oreti Beach Track • Invercargill to Bluff Mararoa River Track Route Trampers continuing on from the Mavora Walkway can walk south down and around the North Mavora Lake shore to the swingbridge across the Mararoa River at the lake’s outlet. From here the track is marked and sign-posted. It stays west of but proximate to the Mararoa River and then South Mavora Lake to this lake’s outlet where another swingbridge provides an alternative access point from Mavora Lakes Road. Beyond this swingbridge, the track continues down the true right side of the Mararoa River to a third and final swing bridge. Along the way a careful assessment is required: if the Mararoa River can be forded safely then Te Araroa Trampers can continue down the track on the true right side to the Kiwi Burn then either divert 1.5km to the Kiwi Burn Hut, or ford the Mararoa River and continue south on the true left bank. If the Mararoa is not fordable then Te Araroa trampers must cross the final swingbridge. Trampers can then continue down the true left bank on the riverside of the fence and, after 3km, rejoin the Te Araroa opposite the Kiwi Burn confluence. 1 Below the Kiwi Burn confluence, Te Araroa is marked with poles down the Mararoa’s true left bank. This is on the riverside of the fence all the way down to Wash Creek, some 16km distant. -
I-SITE Visitor Information Centres
www.isite.nz FIND YOUR NEW THING AT i-SITE Get help from i-SITE local experts. Live chat, free phone or in-person at over 60 locations. Redwoods Treewalk, Rotorua tairawhitigisborne.co.nz NORTHLAND THE COROMANDEL / LAKE TAUPŌ/ 42 Palmerston North i-SITE WEST COAST CENTRAL OTAGO/ BAY OF PLENTY RUAPEHU The Square, PALMERSTON NORTH SOUTHERN LAKES northlandnz.com (06) 350 1922 For the latest westcoastnz.com Cape Reinga/ information, including lakewanaka.co.nz thecoromandel.com lovetaupo.com Tararua i-SITE Te Rerenga Wairua Far North i-SITE (Kaitaia) 43 live chat visit 56 Westport i-SITE queenstownnz.co.nz 1 bayofplentynz.com visitruapehu.com 45 Vogel Street, WOODVILLE Te Ahu, Cnr Matthews Ave & Coal Town Museum, fiordland.org.nz rotoruanz.com (06) 376 0217 123 Palmerston Street South Street, KAITAIA isite.nz centralotagonz.com 31 Taupō i-SITE WESTPORT | (03) 789 6658 Maungataniwha (09) 408 9450 Whitianga i-SITE Foxton i-SITE Kaitaia Forest Bay of Islands 44 Herekino Omahuta 16 Raetea Forest Kerikeri or free phone 30 Tongariro Street, TAUPŌ Forest Forest Puketi Forest Opua Waikino 66 Albert Street, WHITIANGA Cnr Main & Wharf Streets, Forest Forest Warawara Poor Knights Islands (07) 376 0027 Forest Kaikohe Russell Hokianga i-SITE Forest Marine Reserve 0800 474 830 DOC Paparoa National 2 Kaiikanui Twin Coast FOXTON | (06) 366 0999 Forest (07) 866 5555 Cycle Trail Mataraua 57 Forest Waipoua Park Visitor Centre DOC Tititea/Mt Aspiring 29 State Highway 12, OPONONI, Forest Marlborough WHANGAREI 69 Taumarunui i-SITE Forest Pukenui Forest -
Case Study Provides an Example of the Application of Some Individual Tools to Specific Issues
CASE STUDIES Hump Ridge Track1 Key issue(s) Well focussed facilitation and project management of community-based development initiatives can utilise local resources as a base for tourism development. Integration of feasibility studies, EIA and resource consent applications, concession applications, project development and marketing and operation is necessary to complete community-based projects. Development processes may require integration with the management of visitor facilities by third parties, as with Department of Conservation land and assets, and collaboration with Maori customary owners. Background Tuatapere is a township in Western Southland which has a long associations with indigenous and plantation forestry, and sawmilling. The expansion of sawmilling around the beginning of the 20th century hastened the clearance of land for agriculture and opened up the district for settlement, so both mill work and farming defined the township’s role as a service centre for the district. The population grew rapidly over a short period in the early 1950's and then more slowly until 1966, peaking at 954. Then, with the exception of a short period of growth between 1976 and 1981, the population of the township declined to 681 in 2001. The state was heavily involved in the management of indigenous forests in Southland but after the reorganisation of the New Zealand Forest Service in 1987, plantation forests and stated-owned mills were sold to multinational companies. Local sawmilling operators were largely excluded and had to find alternative supplies of timber from private forest owners. Furthermore, some 100,000 ha of indigenous forests was moved from production to the conservation estate. -
Fiordland Day Walks Te Wāhipounamu – South West New Zealand World Heritage Area
FIORDLAND SOUTHLAND Fiordland Day Walks Te Wāhipounamu – South West New Zealand World Heritage Area South West New Zealand is one of the great wilderness areas of the Southern Hemisphere. Known to Māori as Te Wāhipounamu (the place of greenstone), the South West New Zealand World Heritage Area incorporates Aoraki/Mount Cook, Westland Tai Poutini, Fiordland and Mount Aspiring national parks, covering 2.6 million hectares. World Heritage is a global concept that identifies natural and cultural sites of world significance, places so special that protecting them is of concern for all people. Some of the best examples of animals and plants once found on the ancient supercontinent Gondwana live in the World Heritage Area. Left: Lake Marian in Fiordland National Park. Photo: Henryk Welle Contents Fiordland National Park 3 Be prepared 4 History 5 Weather 6 Natural history 6 Formation ������������������������������������������������������� 7 Fiordland’s special birds 8 Marine life 10 Dogs and other pets 10 Te Rua-o-te-moko/Fiordland National Park Visitor Centre 11 Avalanches 11 Walks from the Milford Road Highway ����������������������������� 13 Walking tracks around Te Anau ����������� 21 Punanga Manu o Te Anau/ Te Anau Bird Sanctuary 28 Walks around Manapouri 31 Walking tracks around Monowai Lake, Borland and the Grebe valley ��������������� 37 Walking tracks around Lake Hauroko and the south coast 41 What else can I do in Fiordland National Park? 44 Contact us 46 ¯ Mi lfor d P S iop ound iota hi / )" Milford k r a ¯ P Mi lfor -
Rob Greenaway & Associates
Rob Greenaway & Associates Proposed Manapouri Tailrace Amended Discharge: Recreation and Tourism Assessment of Effects Prepared for Meridian Energy Ltd February 2009. Final version www.greenaway.co.nz MTAD Recreation and Tourism Assessment RG&A 1 Proposed Manapouri Tailrace Amended Discharge Recreation and Tourism Assessment of Effects Contents 1 Summary ................................................................................................................................................... 4 1.1 Lakes Te Anau and Manapouri, and the Lower Waiau River ................................................................ 4 1.2 Deep Cove and Doubtful Sound ........................................................................................................... 4 2 Introduction .............................................................................................................................................. 6 2.1 Study aims ............................................................................................................................................ 6 2.2 Method .................................................................................................................................................. 7 2.3 Study area definitions ........................................................................................................................... 7 2.4 Author’s experience .............................................................................................................................. 7