DOCSLIB.ORG

Te Ara Ahi — NZ Walking Access Commission Ara Hīkoi Aotearoa

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Te Ara Ahi — NZ Walking Access Commission Ara Hīkoi Aotearoa 9/25/2021 Te Ara Ahi — NZ Walking Access Commission Ara Hīkoi Aotearoa Te Ara Ahi Walking Cycling Difculties Easy , Medium Length 46.7 km Journey Time 2 days Region Bay of Plenty Part of the Collection Nga Haerenga - The New Zealand Cycle Trail Rotorua — Waikite Valley (2 days, 48km) https://www.walkingaccess.govt.nz/track/te-ara-ahi/pdfPreview 1/5 9/25/2021 Te Ara Ahi — NZ Walking Access Commission Ara Hīkoi Aotearoa This trail offers a 48km adventure through a thermal wonderland of steaming vents, bubbling mud pools and spectacular geysers. Between the trail heads at Rotorua and the Waikite Valley Thermal Pools, this cycle trail takes riders to four signicant geothermal elds: Whakarewarewa, Waimangu Volcanic Valley, Wai-O- Tapu Thermal Wonderland and Waikite Valley Thermal Springs. Each has its own unique geothermal features, including rare ora and fauna, and is rich in Maori history and folklore. Possibly the most famous of these is the Whakarewarewa Thermal Reserve, located next to Te Puia (the New Zealand Maori Arts & Crafts Institute). Here you will also nd Whakarewarewa Village, which has existed for over 700 years and is home to many families of the survivors of the 1886 eruption of Mt Tarawera. Other unique features along the trail include the Lake Okaro restoration project (re-established wetland), Rainbow Mountain, Te Ranga Hot Pools and the Waikite Geothermal Field. Most of the geothermal areas are well established tourist attractions, with a wide range of amenities such as cafés, souvenir shops, toilets and bike storage facilities. We recommend you take at least two days to ride this trail. And if you want more after that, Rotorua is a mountainbiking mecca, with a range of worldclass cycle trails to explore. Whakarewarewa – The Living Maori Village Whakarewarewa Thermal Valley incorporates a living, breathing Maori village that relies on geothermal power for the ease of everyday living. Throughout the day local residents act as village guides, providing a tour with a difference – from relaying village stories, to cooking meals and explaining how they use the natural landscape for bathing, washing clothes and predicting weather patterns. You can also see spine-tingling cultural performances including the haka, and taste delicious traditional Maori food. Lake Rotorua This picturesque lake is the second biggest in the North Island and is perfect for windsurng, sailing and shing. Tours are available to Mokoia Island, in the middle of the lake. https://www.walkingaccess.govt.nz/track/te-ara-ahi/pdfPreview 2/5 9/25/2021 Te Ara Ahi — NZ Walking Access Commission Ara Hīkoi Aotearoa Conditions: MOBILE PHONE COVERAGE: Good coverage from the start of the trail at Princes Gates through to Waiotapu. No coverage on Waikite Valley Rd. DRINKING WATER: Available at cafés at the Rotorua Mountain Bike car park in the Waipa Valley, Waimangu Volcanic Valley, Wai-O-Tapu Thermal Wonderland, Waikite Valley Thermal Pools and at Lake Okaro and the Waiotapu Tavern. https://www.walkingaccess.govt.nz/track/te-ara-ahi/pdfPreview 3/5 9/25/2021 Te Ara Ahi — NZ Walking Access Commission Ara Hīkoi Aotearoa How to get here Rotorua to Waimangu Volcanic Valley, (Grades 2-3, Easy to Intermediate) 30km From the Rotorua i-SITE, ride east on Queen St to the start of the trail at the Princes Gate Archway a few hundred metres away. Follow the trail signs around the edge of Lake Rotorua for 6km to the historic Whakarewarewa Maori Village (the village entrance is 200m off the trail on your left). Guided tours are regularly held through this historical village. From the turn-off to the village, continue following signs south past Te Puia, theNew Zealand Maori Arts and Crafts Institute, through Hemo Gorge to the entrance to the Whakarewarewa Forest for mountain biking (100m off the trail on your left). Here you will nd a café and bike hire, etc. From the mountain bike carpark, ride 150m towards the highway to the start of a concrete bike path, which runs alongside the highway for several kilometres of smooth easy riding. The trail then follows Waimangu Rd to the Waimangu Volcanic Valley, which is 31km from Rotorua. At Waimangu Volcanic Valley you can relax in the café or pay to go for a walk on a number of walking trails through one of the world’s youngest thermal areas. Waimangu Volcanic Valley to Waikite Valley ThermalPools, (Grade 3 Intermediate) 18km From Waimangu Volcanic Valley, continue along Waimangu Rd, past the Lake Okaro picnic area (camping sites available) and onto SH 38. Take care crossing the highway and follow the off-road cycle path around Rainbow Mountain. After passing a roadside picnic area the trail climbs further around the mountain and drops down to cross the gravel Old Waiotapu Rd. Here you can turn left to go to Te Ranga (a thermally heated stream locally known as Kerosene Creek) or you can carry on straight ahead on an off-road trail all the way to Waiotapu. Parts of the trail are steep here and may require walking. At Waiotapu you will nd a hotel with accommodation, petrol station and a honey factory with a café and shop. Only 2km from Waiotapu is the Waiotapu Mud Pool and the Wai-OTapu Thermal Wonderland (paid entry).From Waiotapu follow the Waikite Valley Rd for 6km to the Waikite Valley Thermal Pools – there is camping and a café here. https://www.walkingaccess.govt.nz/track/te-ara-ahi/pdfPreview 4/5 9/25/2021 Te Ara Ahi — NZ Walking Access Commission Ara Hīkoi Aotearoa Track Elevation and Map Page last updated: Sep 8, 2020, 3:41 PM https://www.walkingaccess.govt.nz/track/te-ara-ahi/pdfPreview 5/5.
Load more

Recommended publications
  • Rotorua District Perceptions of Safety Survey 2007
    ROTORUA DISTRICT PERCEPTIONS OF SAFETY SURVEY 2007 PREPARED BY APR CONSULTANTS FOR ROTORUA DISTRICT COUNCIL JUNE 2007 Rotorua District Safety Perception Survey 2007 FOREWORD Over 500 local residents participated in the 2007 Rotorua District Perceptions of Safety Survey undertaken during the first half of 2007. The survey process followed that of the 2005 and 2006 Perceptions of Safety Surveys on current perceptions held by local Rotorua residents in regard to safety in the district. The survey is part of an ongoing monitoring tool for Rotorua District Council and provides residents with an opportunity to have their say on matters of personal safety, safety in neighbourhoods, and safety in public places like the Central Business District. Council is committed to creating a safe and caring community for our residents and visitors. Let’s continue to work together to achieve this goal. Kevin Winters Mayor of the Rotorua District APR Consultants Ltd 2 Rotorua District Safety Perception Survey 2007 EXECUTIVE SUMMARY This report presents the results of the Rotorua District Perceptions of Safety Survey undertaken within the Rotorua District of New Zealand, during April and May 2007. A total of 511 local residents were surveyed via telephone to establish: perceptions of general safety in the Central Business District (CBD); perceptions of general safety in the local neighbourhood and the home during the day-time and night-time; perceptions of vehicle safety when parked unattended both in the CBD and around the district; actual incidents of crime and the frequency of alcohol consumption by offenders; and residents’ awareness of initiatives currently in place to reduce crime.
    [Show full text]
  • The Origin of Radon Anomalies Along Normal Faults in an Active Rift and Geothermal Area GEOSPHERE; V
    Research Paper GEOSPHERE The origin of radon anomalies along normal faults in an active rift and geothermal area GEOSPHERE; v. 12, no. 5 Jonathan Robert Joseph Davidson1, Jerry Fairley2, Andrew Nicol1,3, Darren Gravley1, and Uwe Ring1,4 1Department of Geological Sciences, University of Canterbury, Private Bag 4800, Christchurch 8140, New Zealand doi:10.1130/GES01321.1 2Department of Geological Sciences, University of Idaho, 875 Perimeter Drive, MS 3022, Moscow, Idaho 83844, USA 3GNS Science, PO Box 30368, Lower Hutt, New Zealand 10 figures; 4 tables 4Department of Geological Sciences, Stockholm University, Svante Arrhenius väg 8, SE-106 91 Stockholm, Sweden CORRESPONDENCE: jrjdavidson@ gmail .com ABSTRACT Katsanou et al., 2010). The preponderance of evidence suggests that these CITATION: Davidson, J.R.J., Fairley, J., Nicol, A., anomalies can provide reliable information about the locations of faults and the Gravley, D., and Ring, U., 2016, The origin of radon anomalies along normal faults in an active rift and Radon anomalies are widely reported in the vicinity of active faults, where spatial distribution of fluid flow within fault zones; however, the actual mecha- geothermal area: Geosphere, v. 12, no. 5, p. 1656– they are often inferred to result from upward migration of fluids along fault nism responsible for the observed radon anomalies is unclear. Local increases 1669, doi:10.1130/GES01321.1. zones. We examine the up-fault flow hypothesis by measuring radon 220( Rn in radon emanation along faults could be caused by a number of processes, and 222Rn) in soil gas above two active normal fault zones within the central including coprecipitation of parent nuclides in groundwater mixing zones re- Received 27 January 2016 Taupo rift, New Zealand.
    [Show full text]
  • Ngāti Tahu- Ngāti Whaoa Iwi Environmental Management Plan PART I : TIROHANGA WHĀNUI Overview
    1 IMAGE CREDITS Cover image: Charles Blomfield. Orakei Korako on the Waikato 1885. Museum of New Zealand Te Papa Tongarewa. Registration No 1994-0012-1 Historic photographs of Orākei Kōrako Ngāwhā p 26: Courtesy of Trevor Hunt Photograph of Aratiatia Rapids p 90: Aratiatia Rapids 25025; Hocken Collections, Uare Taoka o Hākena, University of Otago. Copy negative No. c/nE6143/26. Photograph of Orākei Kōrako p 46-47: Whites Aviation Ltd : Photographs. Orakei Korako [Geyserland]. Alexander Turnbull Library, Wellington, New Zealand. Ref: WA-62646-G Historical painting on p 5: Charles Barraud. Orakei Korako 1877. Auckland Art Gallery Toi o Tamaki. Accession No 1985/53/1 2 3 Ngāti Tahu- Ngāti Whaoa Iwi Environmental Management Plan PART I : TIROHANGA WHĀNUI Overview PART II: NGA TAONGA O TAIAO Treasured resources 2 3 CONTENTS PART I : TIROHANGA WHĀNUI - OVERVIEW Mihi ........................................................................................................................ 6 Acknowledgements ................................................................................................... 8 Statements of support ............................................................................................... 9 Foreword ................................................................................................................ 11 Whakatakinga – Introduction ..................................................................................... 12 How this plan was developed ................................................................................
    [Show full text]
  • Mamaku Messenger June Editor:- Lyn Fleet Next Deadline 2017 Email:- [email protected] 26Th June, 2017 Printed with the Support of NMF Rotorua Lakes Council
    Mamaku Messenger June Editor:- Lyn Fleet Next Deadline 2017 Email:- [email protected] 26th June, 2017 Printed with the support of NMF Rotorua Lakes Council Mamaku School Possum Challenge. 20 teams rose to the challenge and braved the elements on what could only be called a typical winter weekend. Showing all the elements in a maer of 3 days. Cold, wind, rain, frost and the eventual, sunshine. Some waited with sausage in hand for the ute loads of possums, hares, rabbits, wallabies, stoats, ferrets, 4 blind mice. ( not in the count but a rodent all the same) and a couple of turkeys. As they arrived hunt- ers produced their largest possums weighed, had their lots categorised, counted and recorded to produce a total of 298 as well as a trailer of rabbits, wallabies, stoats, and a ferret As well as the challenge there was a lively and hilarious aucon of goods (supplied many local business- es) by Charles Sturt which raised an extra $920 to the amount raised on the day. Special thanks to:- Pol- ynesian Spa, First Naonal, Vet Plus, Bike Force, Mamaku Garage, Ngo. Pharmacy, Ngo. Books, Chaffco, The Warehouse, Mitre 10, Count Down, Farmlands, DOC, Killwell Sports, Reading Cinema, Skyline Rotorua, Gull Ngo. Gold’s Fitness, Palmers Rotorua, The Adventure Room, Buried Village, Mamaku Takeaways, Aquac Centre, Piako Tractors, Mamaku Blue, Paerson O’Connor, Rail Cruising, Rainbow Springs, Extra Mile Auto, Animal Health Services, Off Road NZ, Waikite Valley Pools, Capers, Hikoi Pro- ducons, Serious Shooters, Agrodome, Pig n Whistle, OGO, Agroventures, Gun Supplies Ltd, Stoney Creek, Moon Entertain- ment, BOP Regional Council, Hamurana Lodge, Mokia Downs B & B, Hells Gate, W & R Services, The Novotel, Gourmet Foods Ltd, Macs Steakhouse, Huntaway Farm Trek, Volcanic Air, Wealleans, Tyre Works, Chaan Farm camping, Rydes Rotorua, Flipout, Duck Tours, Amaze Me, Clayton Rd Mobil, Kings Commericals, Marlene Badger, Global Velocity, Paul Gee, CLAAS Trac- tors, Carson Taylor, RD 1 , Okere Falls Store, Blackman Spargo Law, ZORB, Burger Fuel.
    [Show full text]
  • 1. Kerosene Creek 2. Wairua Stream
    1. Kerosene Creek First on our list of hot pools in Rotorua is the world-famous Kerosene Creek. 35 minutes from Rotorua and down a gravel road will take you to the thermal pool and waterfall at Kerosene Creek. The creek is popular not just for its geothermal activity but its beautiful surroundings. Location: 28km south of Rotorua. Take State Highway 5, then travel about 2km down Old Waiotapu Road. 2. Wairua Stream Wairua Stream is a bit harder to get to as you have to get a boat across Lake Tarawera, making it a local’s paradise. It is near Te Rata Bay and is one of the most picturesque hot pools near Rotorua. Location: About 25 minutes out of Rotorua down Spencer Road, Lake Tarawera. By boat, launch at Stoney Point and head straight across Lake Tarawera to the headlands on the right of Mt Tarawera. Go straight through these headlands to where the lake opens. Steer gently to starboard and make for the only beach in this area. 3. Wai-o-Tapu / The Bridge / The Secret Spot When it comes to Rotorua hot pools, it does not get more popular thank this one. Funnily enough, it is supposed to be a secret. Get the remnants from the Wai-O-Tapu geothermal attraction by bathing in the hot pool formed by the hot Wai-O-Tapu stream meeting the cool river. It’s a thermal pool, completely natural and completely free! Location: Just outside the Wai-O-Tapu geothermal park (under the bridge). 30km south of Rotorua just off State Highway 5.
    [Show full text]
  • Details of Certified Inspectors Available to Do Inspections on Non DECA
    Details of certified Inspectors available to do inspections on Non DECA Holders Post Code Name Region City Phone Cell Email 110 Alex Svela Whangarei Maunu 09 433 6511 021 1127845 [email protected] 112 Peter Alexander Whangarei Tikipunga 022 1211 221 [email protected] 173 John Beauregard Ngunguru, Kiripaka, Kaiatea 09 437 5506 [email protected] 173 James Clueard Whangarei Matapouri / Tutukaka Coast / Ngunguru / Whangarei 09 434 4341 027 358 9096 [email protected] 174 Carter Lifshutz Whangarei District 022 1880871 [email protected] 178 Trevor Clifton WHANGAREI PUWERA MAUNGAKARAMEA 09 4329511 027 4330155 [email protected] 178 Judith Mabbott Whangarei Maungakaramea Whangarei lwbudd@Xtra. Co. nz 179 George Walkinshaw Whangarei Maunu Whangarei 027 4843018 [email protected] 179 Linda Wilkinson Whangarei Poroti 09-4346654 021 919966 [email protected] 179 Keith Fitzpatrick Whangarei Whangarei (021) 2358283 [email protected] 192 Ross Cook Whangarei Parua Bay Pataua South 09 4365749 027 2812984 [email protected] 204 Zareth Karena Northland Auckland upwards, mid north Bay of Islands, Whangarei, Kaiataia, far north 020 409 45175 [email protected] 230 Mike Smith Bay of islands KERIKERI 021 2734891 [email protected] David Spiers Kerikeri 021 2775228 [email protected] 245 Robert Corden Northland Kerikeri 021 0336009 [email protected] 241 John McEntee Opua Northland 021 2145564 [email protected] 272 Neil Davidson Opua Northland Paihia Russell Kerikeri kawakawa (shift worker) 0274 379368 [email protected]
    [Show full text]
  • Over the Years
    OVER THE YEARS A HISTORY OF THE RURAL COMMUNITY HALLS IN THE ROTORUA DISTRICT FOREWORD Nau mai, Haere mai, There are nine rural community halls in the Rotorua District, at Broadlands, Kaharoa, Mamaku, Ngakuru, Ngongotaha, Okareka, Reporoa, Rerewhakaaitu, and Waikite. Volunteers have driven the development and maintenance of these vital community facilities, which have been the focus for community functions and gatherings for many years. In 2001, Rotorua District Council awarded certificates of appreciation to many of these volunteers for their tireless efforts to sustain the upkeep of their local halls. This booklet was commissioned by the District Council to record the history of Rotorua’s rural halls, for both archival and community interest. Information was compiled in the latter months of 2002 by Marlana Maru, a Year 2 Bachelor of Applied Social Science student from the Waiariki Institute of Technology. RDC Social Research Officer Paul Killerby undertook additional editing and formatting. Marlana and I would like to thank the many local informants whose memories and impressions contributed to this booklet. In particular we would like to thank Barbara Blackburn, Peter Blackburn, Andy Burnett, Mary Burnett, David Fleet, Lyn Fleet, Maxine Greenslade, Triss Hill, Wally Hope, Marie Jepsen, Noeleen Martelli, Verna Martelli, Pam Murray, Jim Nicholson, Norman Reichardt, Rei Reichardt, Arthur Roe, Don Sandilands, and Chris Stevens. We would welcome any further background information on the halls listed in this booklet, which will be recorded and utilised in any further update of the publication. Tom Baker RDC Community Services Officer Cover photos, clockwise from top: 1. Mamaku War Memorial Hall, date unknown.
    [Show full text]
  • Lake Rotorua Catchment Landscape Assessment
    LAKE ROTORUA CATCHMENT LANDSCAPE ASSESSMENT :: JUNE 2010 WEB VERSION Rotorua District Council Contact Details Email: [email protected] Phone: +64 7 348 4199 After hours: +64 7 348 4195 Fax: +64 7 346 3143 Post: Rotorua District Council Private Bag 3029 Rotorua Mail Centre Rotorua 3046 New Zealand Street Address: Rotorua District Council, Civic Centre 1061 Haupapa Street Rotorua New Zealand Prepared for by Rotorua DistrictWEB Council VERSIONBoffa Miskell Limited A07141_RdL_Rotorua_Southern_Lakes_Landscape_Assessment\Graphics\A07141_001_[prev_T05132_050]_Lake_Rotorua_Catchment_Lsc_Assessmt.indd WEB VERSION WEB VERSION Contents Executive Summary Introduction 1 250 EasterN Rural Terrace ������������������������������������������������������������������������������������������������������������������������������63 Uses of Landscape Character Assessment ����������������������������������������������������������������������������������������������������������������2 25.1: Eastern Rural Terrace 63 260 EasterN Rural Hills ������������������������������������������������������������������������������������������������������������������������������������65 What is “Landscape”? �������������������������������������������������������������������������������������������������������������������������������������������������2 26.1: Eastern Rural Hills 65 Landscape Change in the Lake Rotorua Catchment2 270 MOUNT NGONGOtaHA ���������������������������������������������������������������������������������������������������������������������������������67
    [Show full text]
  • REPOROA, NEW ZEALAND Gregory Bignall
    251 Proc 12th New Zealand Geothermal Workshop 1990 Bignall HYDROLOGY AND HYDROTHERMAL ALTERATION, REPOROA WELL (1), REPOROA, NEW ZEALAND Gregory Bignall Geothermal Institute, University of Auckland, Private Bag, Auckland ABSTRACT The Opaheke-Reporoa thermal system has surface activity that consists of hot, neutral alkali chloride-bicarbonatepools; minor sinter, mudpools; steaming ground and hot water seepage. Regional resistivity measurements and fluid chemistry surveys suggest that the Reporoa system is a lateral outflow of hot water from the Waiotapu Geothermal System to the north-east. A deep exploratory drillhole, encountered a sequence of lacustrine sediments, volcanic, tuffaceous and ignimbritic rocks. The well was discharged in October 1966, but was shut down after 5 hours during which time wellhead pressure fell from to Downhole temperatures in were measured after 47 days of heating and showed a significanttemperature inversion between and which is interpreted to be caused by hot water at about depth flowing above a cooler water influx. The temperature interpretation from clay and calc-silicate mineralogy and calculated chemical geothermometers is consistent with the bore hole temperatures. A minor maximum of occurred at 305m (interlayered illite-smectite encountered),a minimum of at 549m (smectite),and a maximum of at 853m to 975m (illite + rare epidote), o : bottom hole temperaturewas /a A Intensity of hydrothermal alteration generally increases with depth below about with the mineral assemblage of quartz, albite, adularia, titanite, illite, chlorite and calcite 40 produced by near neutral chloride-bicarbonate fluid. The scarcity of epidote and absence of wairakite and other calc- Figure 1 Location of the Reporoa geothermal area, Taupo silicate minerals is consistent with alteration by a geothermal Volcanic Zone, North Island, New Zealand.
    [Show full text]
  • Wood Calderas and Geothermal Systems in The
    WOOD CALDERAS AND GEOTHERMAL SYSTEMS IN THE TAUPO VOLCANIC ZONE, NEW ZEALAND C Peter Wood Institute of Geological Nuclear Sciences Ltd, Wairakei Research Centre Taupo, New Zealand Key Words: Calderas, Geothermal Systems, Taupo Volcanic Zone. New Zcaland 2. TAUPO VOLCANIC ZONE The Taupo Volcanic Zone Fig. 1) is the consequence of plate subduction beneath the North Island of New Zcaland. ABSTRACT The thin continental crust (-15 km, Stem and Davey, 1987) spreads at rates up to 18 (Darby and Williams, 1991) Silicic calderas and geothermal systems in Taupo Volcanic in active rifting and subsidence. Since c. 1.6 Ma, the Zone (TVZ) of New Zealand are spatially related. Eight calderas, central TVZ has been the most frequently active and productive active since 1.6 Ma, occupy 45% of the Boundaries of region of rhyolitic volcanism on earth (Houghton et al., 1994). calderas arc often speculative, but of 20 geothermal systems producing an estimated 10 - 15 of rhyolite, and considercd, 15 occur on or next to a caldera margin where there is subordinate dacite, andesite and basalt. Debate continues whether enhanced deep permeability: the best examples are at Haroharo TVZ is a migrating andesitic arc and zone of asymmetric crustal where systems occur at the intersection of volcanic lineations and spreading (eg. Stem, or an andesite-dacite arc with bimodal caldera embayments, and at Rotorua. Drillhole evidence supports rhyolite-basalt back arc (eg. Cole, 1990). Whichever is the case, a realignment of caldera margin through the Wairakei- it is a matter of observation that most geothermal fields are geothermal field. Four geothermal systems have no known contained within the area of rhyolite volcanism.
    [Show full text]
  • Silvicultural Proposals for Radiata Pine on High Quality Sites R
    SILVICULTURAL PROPOSALS FOR RADIATA PINE ON HIGH QUALITY SITES R. T. FENTON and W. R. J. SUTTON* SYNOPSIS An evaluation of current production thinning in radiata pine grown on high quality sites indicates that it has failed to increase realizable volumes, provide adequate intermediate returns (suf­ ficient to compensate for the loss of growth on the final crop trees) or significantly improve selection and quality of the final crop trees. An alternative, and potentially more profitable regime is pro­ posed which eliminates any production thinning for major produce by reducing the stand to the final crop in two stages (to 150 s.p.a. at 35 ft, and to 80 s.p.a, at 55 ft). This regime, designed to maintain near-maximum growth on the final crop trees, is expected to produce trees of mean d.b.h. 22 to 23 inches in 25 to 26 years on sites of Index 95 ft. The regime aims to produce board grades only. PRODUCTION THINNING IN RADIATA PINE Management of both private companies and the Forest Service almost invariably prescribes production-thinning, and often, second-log pruning. The clearfelling of untended stands prescribed on steep country — for pulpwood of radiata pine (Pinus radiata D. Don) (Fenton and Grainger, 1965) and for Douglas fir (Pseudotsuga menziesii Mirb. Franco) (Fenton, 1967a) — were exceptions. (Another was the modification of Schedule B proposed by Bunn, Familton and Fenton to the Forest Research Institute meeting on Thinning and Pruning — Bunn, 1963). Pulpwood crops without production thinning — based on the assumption ". that little would be gained by planting at a greater rate than the sustained yield annual cut .
    [Show full text]
  • A Bathymetrical Survey of the Lakes of New Zealand Author(S): Keith Lucas Source: the Geographical Journal, Vol
    A Bathymetrical Survey of the Lakes of New Zealand Author(s): Keith Lucas Source: The Geographical Journal, Vol. 23, No. 5 (May, 1904), pp. 645-660 Published by: geographicalj Stable URL: http://www.jstor.org/stable/1776009 Accessed: 21-06-2016 04:12 UTC Your use of the JSTOR archive indicates your acceptance of the Terms & Conditions of Use, available at http://about.jstor.org/terms JSTOR is a not-for-profit service that helps scholars, researchers, and students discover, use, and build upon a wide range of content in a trusted digital archive. We use information technology and tools to increase productivity and facilitate new forms of scholarship. For more information about JSTOR, please contact [email protected]. The Royal Geographical Society (with the Institute of British Geographers), Wiley are collaborating with JSTOR to digitize, preserve and extend access to The Geographical Journal This content downloaded from 137.99.31.134 on Tue, 21 Jun 2016 04:12:15 UTC All use subject to http://about.jstor.org/terms A BATHYMETRICAL SURVEY OF THE LAKES OF NEW ZEALAND. 645 will probably have to be by taking numerous measurements with record- ing instruments (of which several have been invented), which will enable the complex wave disturbance to be analyzed into its component simple waves. I trust that the Admiralty may see their way to have this done.* I have to record my indebtedness first to the late Sir G. G. Stokes, who kindly explained to me points of mathematical theory; secondly, to Captain D. Wilson-Barker, who allowed me to examine some of his original notes of observations at sea; and, lastly, to the Editors of IKnowledge, who have lent the blocks for the figures, which were originally drawn by me for a series of articles in that journal (January to July, 1901).
    [Show full text]