Back-Country Huts: More Than a Roof Over Your Head
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Fluctuation in Opossum Populations Along the North Bank of the Taramakau Catchment and Its Effect on the Forest Canopy C
212 Vol. 9 FLUCTUATION IN OPOSSUM POPULATIONS ALONG THE NORTH BANK OF THE TARAMAKAU CATCHMENT AND ITS EFFECT ON THE FOREST CANOPY C. J. PEKELHARING Forest Research Institute, New Zealand Forest Service. Christchurch (Received for publication 10 August 1979) ABSTRACT Fluctuations in density patterns of opossum populations were studied by faecal pellet counts, along the North Bank of the Taramakau catchment from 1970 to 1977. The study area contained two major vegetation associations, rata/kamahi forest and red beech forest. Variations in density patterns over the years indicated that peak population numbers in the beech forests were approxi mately half those in the rata/kamahi forests. The upper transitional forests above both major forest types, however, reached similar peak densities. Canopy defoliation was studied by aerial photography in 1980 and in 1973. Within 13 years over 40% of the canopy in these protection forests was defoliated. This large-scale defoliation coincided with a build-up and peaking of the opossum population. In the winter of 1974 the whole area was poisoned by air with 1080 (sodium monofluoroacetate) impregnated carrot. Approximately 85% of the opossum population was removed by this operation. The greatest decline in pellet densities was recorded in the lower and mid-forest strata. INTRODUCTION A study on the dynamics of opossum populations was initiated by Bamford in 1970 along the north bank of the Taramakau River, Westland (Bamford, 1972). Faecal pellet lines established by Forest Research Institute staff in April 1970 were remeasured in April 1974, 1975 and 1977. The area was aerially poisoned by the Forest Service in June 1974. -
Ïg8g - 1Gg0 ISSN 0113-2S04
MAF $outtr lsland *nanga spawning sur\feys, ïg8g - 1gg0 ISSN 0113-2s04 New Zealand tr'reshwater Fisheries Report No. 133 South Island inanga spawning surv€ys, 1988 - 1990 by M.J. Taylor A.R. Buckland* G.R. Kelly * Department of Conservation hivate Bag Hokitika Report to: Department of Conservation Freshwater Fisheries Centre MAF Fisheries Christchurch Servicing freshwater fisheries and aquaculture March L992 NEW ZEALAND F'RESTTWATER F'ISHERIES RBPORTS This report is one of a series issued by the Freshwater Fisheries Centre, MAF Fisheries. The series is issued under the following criteria: (1) Copies are issued free only to organisations which have commissioned the investigation reported on. They will be issued to other organisations on request. A schedule of reports and their costs is available from the librarian. (2) Organisations may apply to the librarian to be put on the mailing list to receive all reports as they are published. An invoice will be sent for each new publication. ., rsBN o-417-O8ffi4-7 Edited by: S.F. Davis The studies documented in this report have been funded by the Department of Conservation. MINISTBY OF AGRICULTUBE AND FISHERIES TE MANAlU AHUWHENUA AHUMOANA MAF Fisheries is the fisheries business group of the New Zealand Ministry of Agriculture and Fisheries. The name MAF Fisheries was formalised on I November 1989 and replaces MAFFish, which was established on 1 April 1987. It combines the functions of the t-ormer Fisheries Research and Fisheries Management Divisions, and the fisheries functions of the former Economics Division. T\e New Zealand Freshwater Fisheries Report series continues the New Zealand Ministry of Agriculture and Fisheries, Fisheries Environmental Report series. -
FT1 Australian-Pacific Plate Boundary Tectonics
Geosciences 2016 Annual Conference of the Geoscience Society of New Zealand, Wanaka Field Trip 1 25-28 November 2016 Tectonics of the Pacific‐Australian Plate Boundary Leader: Virginia Toy University of Otago Bibliographic reference: Toy, V.G., Norris, R.J., Cooper, A.F., Sibson, R.H., Little, T., Sutherland, R., Langridge, R., Berryman, K. (2016). Tectonics of the Pacific Australian Plate Boundary. In: Smillie, R. (compiler). Fieldtrip Guides, Geosciences 2016 Conference, Wanaka, New Zealand.Geoscience Society of New Zealand Miscellaneous Publication 145B, 86p. ISBN 978-1-877480-53-9 ISSN (print) : 2230-4487 ISSN (online) : 2230-4495 1 Frontispiece: Near-surface displacement on the Alpine Fault has been localised in an ~1cm thick gouge zone exposed in the bed of Hare Mare Creek. Photo by D.J. Prior. 2 INTRODUCTION This guide contains background geological information about sites that we hope to visit on this field trip. It is based primarily on the one that has been used for University of Otago Geology Department West Coast Field Trips for the last 30 years, partially updated to reflect recently published research. Copies of relevant recent publications will also be made available. Flexibility with respect to weather, driving times, and participant interest may mean that we do not see all of these sites. Stops are denoted by letters, and their locations indicated on Figure 1. List of stops and milestones Stop Date Time start Time stop Location letter Aim of stop Notes 25‐Nov 800 930 N Door Geol Dept, Dunedin Food delivery VT, AV, Nathaniel Chandrakumar go to 930 1015 N Door Geology, Dunedin Hansens in Kai Valley to collect van 1015 1100 New World, Dunedin Shoping for last food supplies 1115 1130 N Door Pick up Gilbert van Reenen Drive to Chch airport to collect other 1130 1700 Dud‐Chch participants Stop at a shop so people can buy 1700 1900 Chch‐Flockhill Drive Chch Airport ‐ Flockhill Lodge beer/wine/snacks Flockhill Lodge: SH 73, Arthur's Pass Overnight accommodation; cook meal 7875. -
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. -
Supplement 9: Regional Flood Control Assets
West Coast Lifelines Vulnerability and Interdependency Assessment Supplement 9: Regional Flood Control 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: Greymouth Floodwall, Grey River, Greymouth West Coast Lifelines Vulnerability and Interdependency Assessment Supplement 9: Regional Flood Control Assets Contents 1 INTRODUCTION ........................................................................................................................ -
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]. -
The First Crossing of the Southern Alps of New Zealand Author(S): Edward A
The First Crossing of the Southern Alps of New Zealand Author(s): Edward A. Fitz Gerald Source: The Geographical Journal, Vol. 7, No. 5 (May, 1896), pp. 483-499 Published by: geographicalj Stable URL: http://www.jstor.org/stable/1773992 Accessed: 24-06-2016 18:50 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]. Wiley, The Royal Geographical Society (with the Institute of British Geographers) are collaborating with JSTOR to digitize, preserve and extend access to The Geographical Journal This content downloaded from 137.99.31.134 on Fri, 24 Jun 2016 18:50:23 UTC All use subject to http://about.jstor.org/terms THE FIRST CROSSING OF THE SOUTHERN ALPS OF NEW ZEALAND. 483 :fixed by observation; 200 miles further west the dead reckoning agreed within half a mile of the longitude obtained by an occultation observed by Mr. Littledale, and compiled by Mr. Coles; and at Shushal, near the Ladak frontier, where the survey terminated, there was, after a traverse of 1700 miles, only a difference of 1J mile between Mr. Littledale's position and that given by the Trignometrical Survey of India. We not only have to thank Mr. -
PART ONE This Management Plan
F I S H AND GAME NEW ZEALAND WEST COAST REGION SPORTS FISH AND GAME MANAGEMENT PLAN To manage, maintain and enhance the sports fish and game resource in the recreational interests of anglers and hunters AIRPORT DRIVE PO BOX 179 HOKITIKA 1 2 FOREWORD FROM THE CHAIRMAN I am pleased to present the Sportsfish and Game Management Plan for the West Coast Fish and Game Council. This plan has been prepared in line with the statutory responsibilities of Fish and Game West Coast following extensive consultation with a wide range of stakeholders. It identifies issues and establishes goals, objectives, and implementation methods for all output classes. While it provides an excellent snapshot-in-time of Fish and Game West Coast it should be noted that, as well as ongoing issues, there are likely to be further challenges in the future which will have the potential to impact on angler/hunter opportunities and satisfaction. To this extent, this plan must be seen as a document designed to be capable of addressing changing requirements by way of the annual workplan and in response to ongoing input from anglers and hunters, as well as other users of fish and game habitat. The West Coast Fish and Game Council welcomes such input. Andy Harris Chairman 3 SPORTS FISH AND GAME MANAGEMENT PLAN To manage, maintain and enhance the sports fish and game resource in the recreational interests of anglers and hunters CONTENTS Foreword from the chairman ................................................. 3 Contents .................................................................................... 4 Executive summary .................................................................. 5 PART ONE This management plan ............................................................ 6 Introduction .............................................................................. 8 PART TWO Goals and objectives ............................................................ -
THE IMPORTANCE of INFREQUENT EARTHQUAKES ALONG the ALPINE FAULT by Andrew Wells
LANDSCAPE DISTURBANCE HISTORY IN WESTLAND, NEW ZEALAND: THE IMPORTANCE OF INFREQUENT EARTHQUAKES ALONG THE ALPINE FAULT A thesis submitted in partial fulfilment of the requirements for the Degree of Doctor of Philosophy at Lincoln University by Andrew Wells Lincoln University 1998 ii ABSTRACT Abstract of a thesis submitted in partial fulfilment of the requirements for the Degree of Doctor of Philosophy LANDSCAPE DISTURBANCE HISTORY IN WESTLAND, NEW ZEALAND: THE IMPORTANCE OF INFREQUENT EARTHQUAKES ALONG THE ALPINE FAULT by Andrew Wells This thesis investigates landscape disturbance history in Westland since 1350 AD. Specifically, I test the hypothesis that large-magnitude regional episodes of natural disturbance have periodically devastated portions of the landscape and forest, and that these were caused by infrequent earthquakes along the Alpine Fault. Forest stand history reconstruction was used to determine the timing and extent of erosion and sedimentation events that initiated new forest cohorts in a 1412 ha study area in the Karangarua River catchment, south Westland. Over 85 % of the study area was disturbed sufficiently by erosion/sedimentation since 1350 AD to initiate new forest cohorts. During this time four episodes of catchment-wide disturbance impacted the study area, and these took place about 1825 AD ± 5 years (Ruera episode), 1715 AD ± 5 years (Sparkling episode), 1615 AD ± 5 years (McTaggart episode), and 1445 AD ± 15 years (Junction episode). The three most recent episodes disturbed 10 %, 35-40 % and 32-50 % respectively of the study area. The Junction episode disturbed at least 6 % of the study area, but elimination of evidence by more recent disturbances prevented an upper limit being defined. -
Coqqlstxtrtu>
coQQlstxtrtu> Name Address_-----_ no,o iltlilfi{ ffiil l. we wish to see March 79gg n Community Contact continue Ross June ZSS 41 76 2. We support Community Contact's Annie 755 4t45 application for a C.O.G.S. Grant Hari Hari Seonaid 753 s0t 2 Avis 753 3080 Wataroa Anne 753 4138 Ross Annie 755 1145 3. we do not wish to see community contact Franz Josef Sury 75 2 0717 Continue Jone 753 1083 Fox Glacier Sue 75t 08t8 and south Brenda 75 0837 I :<------Grr-rr Eleanor 751 07t6 Haast Trisha 750 0847 Please send to the mailing address on the opposite FAX(new number) 751 0715 side of the page urgently oh -and while you are doing it throw a story, poem, recipe, anecdote, tip Mailing address;- c/- Lake paringa postal Agency etc. into the enveloppe if you have one. ThanksM SOUTH WESTI-AT{D , TOX GI}ICIERSCHOOL BOARD OF TRUSTEES EI.,ECTION Nominations are invited for the election of 5 parent representatives to the Board of Trustees. Nomination forms can be obtained from the Fox Glacier School Office or from the Returning H[lP Offioer. Nominations close at Noon Thursday 26th March 1998. A copy of the electoral roll is available for inspection at the school office during Hc nGGil yru hncrs cl silDnrn norrnal school hours. DlGasG!! Voting papers will be sent to eligible voters, Last month in Community Contact we asked The poll closes at noon 9th April 1998. you, the readens, if you wished us to continue publishing Community Contact - in light of the John Sullivan - Returning Officer fact that there are now two free newspapers circulating on the West Coast and also we needed letters to support our application for u C.O.G.S Grant . -
DATE: November 2019 Vol. 72 No. 10
DATE: November 2019 Vol. 72 No. 10 ARNOLD JOHN HEINE : QSM, ONZM, Polar Medal Please submit your December 2019/January 2020 H&V articles to the editor by 30th November 2019 HVTC Postal Address: PO Box 30-883, Lower Hutt: Clubrooms: Birch Street Reserve, Birch Street, Waterloo Internet: http://www.hvtc.org.nz E-mail: [email protected] President: Dennis Page 970 6901 Secretary: Murray Presland 562 8194 Trip Coordinator: Chris McMillan 569 9019 Treasurer: Jim Cousins 586 2135 Editor H&V: Bruce Miller 563 5966 [email protected] 1 BJFM/H&V/Vol72/No10 WEDNESDAY NIGHT PROGRAMME Starts 8.00 pm promptly 6 November : Andrew Robinson – Eye-Q Test 4 By popular demand Andrew brings you another quiz night that will test your powers of observation. There will be the usual spot-the-difference, there won't be hidden names, but beyond that, you'll have to wait and see (as it were). 13 November : Frank and Robyn Usmar– European Trip 2019 part. 2 The Czech Republic Following on from Pat Tristram’s talk in the Switzerland area Frank and Robyn will continue with the next leg of their travels with the Czech Castles Self-Guided Cycle Tour from Cesky Krumlov to Prague. The group visited medieval towns, castles and monasteries, while cycling through and along picturesque landscapes, forests and river trails. Sales Table run by Graeme Lythgoe. Bring your cash and your saleable items. 20 November : Owen Spearpoint – ‘The Great Unknown’ Owen will be launching his new book entitled ‘The Great Unknown; Mountain Journeys in the Southern Alps’. -
Peak Bagging and Mountain Adventures
2009–2015 Peak Bagging and Peak compiled by Colin & Jeni Bell Colin & Jeni compiled by Mountain Adventures Adventures Mountain SIMON’S TRIPS SIMON’S SIMON’S TRIPS PEAK BAGGING AND MOUNTAIN ADVENTURES 2009–2015 BELL SIMON’S TRIPS SIMON’S TRIPS Peak Bagging and Mountain Adventures 2009–2015 compiled by Colin & Jeni Bell Cover photo: Simon crossing Lake Stream on the way to Jagged Peak, October 2014. Nina Dickerhof Published 2015 by Colin & Jeni Bell ISBN 978-0-473-34051-3 © Copyright 2015 All rights reserved. The moral rights of all contributors are asserted. Please contact Colin & Jeni Bell for permission to use or reprint this material or for electronic or additional copies. Printed by The Copy Press, Nelson, New Zealand. www.copypress.co.nz Simon Colin Bell set out to climb Pikirakatahi / Mt Earnslaw on the 15th January 2015 and did not return. This work is to honour Simon, keep his memory alive and be a gift to his friends and family. It is also to introduce and thank some of the many people who enriched his life. Simon wrote most of this book and provided most of the photographs. His family, friends and fellow climbers contributed the rest. All that is gold does not glitter, Not all those who wander are lost; The old that is strong does not wither, Deep roots are not reached by the frost. J. R. R. Tolkien in Lord of the Rings. PREFACE On the 15th January this year, our son Simon left Esquilant Bivvy in the Mount Aspiring National Park alone and early in the morning to climb Mt Earnslaw.