SGP-Alps 2 Ocean Trail-Tripnotes
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FT6 Aviemore
GEOSCIENCES 09 Annual Conference Oamaru, NZ FIELD TRIP 6 AVIEMORE – A DAM OF TWO HALVES Wednesday 25 November 2009 Authors: D.J.A Barrell, S.A.L. Read, R.J. Van Dissen, D.F. Macfarlane, J. Walker, U. Rieser Leaders: David Barrell, Stuart Read & Russ Van Dissen GNS Science, Dunedin and Avalon BIBLIOGRAPHIC REFERENCE: Barrell, D.J.A., Read, S.A.L., Van Dissen, R.J., Macfarlane, D.F., Walker, J., Rieser, U. (2009). Aviemore – a dam of two halves. Unpublished field trip guide for "Geosciences 09", the joint annual conference of the Geological Society of New Zealand and the New Zealand Geophysical Society, Oamaru, November 2009. 30 p. AVIEMORE - A DAM OF TWO HALVES D.J.A Barrell 1, S.A.L. Read 2, R.J. Van Dissen 2, D.F. Macfarlane 3, J. Walker 4, U. Rieser 5 1 GNS Science, Dunedin 2 GNS Science, Lower Hutt 3 URS New Zealand Ltd, Christchurch 4 Meridian Energy, Christchurch 5 School of Geography, Environment & Earth Sciences, Victoria Univ. of Wellington ********************** Trip Leaders: David Barrell, Stuart Read & Russ Van Dissen 1. INTRODUCTION 1.1 Overview This excursion provides an overview of the geology and tectonics of the Waitaki valley, including some features of its hydroelectric dams. The excursion highlight is Aviemore Dam, constructed in the 1960s across a major fault, the subsequent (mid-1990s – early 2000s) discovery and quantification of late Quaternary displacement on this fault and the resulting engineering mitigation of the dam foundation fault displacement hazard. The excursion provides insights to the nature and expression of faults in the Waitaki landscape, and the character and ages of the Waitaki alluvial terrace sequences. -
Great Southern Steam Train Tour
Great Southern Steam Train Tour • SOUTH ISLAND RAIL TOUR • DEPARTING WELLINGTON TO INVERCARGILL 22 APRIL - 29 APRIL 2021 | 8-DAY TOUR OPTION Experience the adventure, the nostalgia, the romance of Steam Train travel. Pounamu Tourism Group invites you to take a step back in time to a bygone era for an epic steam train journey exploring the majestic South Island of Aotearoa. GREAT SOUTHERN TOUR OPTIONS STEAM TRAIN TOUR TOUR OPTION 1: Journey with us into the deep south of New 13-DAY TOUR Departing Wellington Zealand and experience the postcard perfect vistas from 22 April – 4 May 2021 ** and dramatic scenery that this part of the world is renowned for. TOUR OPTION 2: You will spend the week travelling the entire 8-DAY TOUR Departing Wellington to length of the South Island (visiting Marlborough, Invercargill from 22 April – 29 April 2021 ** Christchurch, Oamaru, Dunedin and Invercargill), in the comfort of vintage carriages hauled by the ** option to begin tour in Blenheim on 23 April 2021 historic WW1 memorial steam locomotive Ab608 Passchendaele, (named in honour of our fallen soldiers at The Battle of Passchendaele in 1917). South Island 8-Day Steam Train Tour • 22 April 2021 - 29 April 2021 2 CONTENTS 8-DAY TOUR DEPARTING WELLINGTON TO INVERCARGILL DAY 1 DAY 2 Wellington – Blenheim – Blenheim Kaikoura page 6 page 6 DAY 3 DAY 4 Kaikoura – Christchurch Christchurch ANZAC DAY page 7 page 7 DAY 5 DAY 6 Christchurch – Oamaru – Oamaru Dunedin page 8 page 8 DAY 7 DAY 8 Dunedin – Invercargill Invercargill page 9 page 9 South Island 8-Day Steam Train Tour • 22 April 2021 - 29 April 2021 3 8-DAY TOUR WELLINGTON – INVERCARGILL 22 APRIL - 29 APRIL 2021 Steam Train South Island 8-Day Steam Train Tour • 22 April 2021 - 29 April 2021 4 8-DAY TOUR FROM The tour is escorted by a fleet of luxury coaches that provide seamless transfers from the train to your WELLINGTON TO accommodation each evening. -
Cultural Value Report Arrow and Cardrona
CULTURAL VALUES REPORT Arrow River / Wakatipu Basin Aquifers Cardrona River Intellectual Property Rights This report has been prepared for Otago Regional Council on behalf of Te Rūnanga o Moeraki, Kāti Huirapa Rūnaka ki Puketeraki, Te Rūnanga o Ōtākou and Hokonui Rūnanga (Kāi Tahu ki Otago) and Te Rūnanga o Waihōpai, Te Rūnanga o Awarua and Te Rūnanga o Ōraka-Aparima (Kāi Tahu ki Murihiku). Intellectual property rights are reserved by these rūnanga. Acknowledgement The preparation of this report was undertaken with the assistance of: Te Rūnanga o Moeraki Kāti Huirapa Rūnaka ki Puketeraki Te Rūnanga o Ōtākou Hokonui Rūnanga Te Rūnanga o Waihōpai Te Rūnanga o Awarua Te Rūnanga o Ōraka-Aparima Key informants and site evaluation participants. Peter Petchey and Brian Allingham. Front Cover: The confluence of the Cardrona and Clutha rivers. Photograph: Maree Kleinlangevelsloo Version: October 2017 KTKO Ltd Prepared by: Level 1 Maree Kleinlangevelsloo 258 Stuart Street Literature Review: Rosemary Clucas PO Box 446 Reviewed By: Dunedin Te Rūnanga o Moeraki Tel: 03-477–0071 Kāti Huirapa Rūnaka ki Puketeraki Te Rūnanga o Ōtākou Hokonui Rūnaka Te Rūnanga o Awarua Te Rūnanga o Waihōpai Te Rūnanga o Ōraka-Aparima Tim Vial (KTKO Ltd) 1 Executive Summary The Arrow and Cardrona catchments and the Wakatipu Basin are highly valued by the whānau of Kāi Tahu ki Otago and Murihiku (Kāi Tahu). Ara tawhito (trails), ran through these catchments, bringing whānau into the southern lakes and rivers on their seasonal pursuit of resources. Today the rivers are used for recreation, and are valued for their landscape qualities and the species residing in them. -
The Wrybill <I>Anarhynchus Frontalis</I>: a Brief Review of Status, Threats and Work in Progress
The Wrybill Anarhynchus frontalis: a brief review of status, threats and work in progress ADRIAN C. RIEGEN '1 & JOHN E. DOWDING 2 •231 ForestHill Road, Waiatarua, Auckland 8, NewZealand, e-maih riegen @xtra.co. nz; 2p.o. BOX36-274, Merivale, Christchurch 8030, New Zealand, e-maih [email protected]. nz Riegen,A.C. & Dowding, J.E. 2003. The Wrybill Anarhynchusfrontalis:a brief review of status,threats and work in progress.Wader Study Group Bull. 100: 20-24. The Wrybill is a threatenedplover endemic to New Zealandand unique in havinga bill curvedto the right.It is specializedfor breedingon bareshingle in thebraided riverbeds of Canterburyand Otago in the SouthIsland. After breeding,almost the entirepopulation migrates north and wintersin the harboursaround Auckland. The speciesis classifiedas Vulnerable. Based on countsof winteringflocks, the population currently appears to number4,500-5,000 individuals.However, countingproblems mean that trendsare difficult to determine. The mainthreats to theWrybill arebelieved to be predationon thebreeding grounds, degradation of breeding habitat,and floodingof nests.In a recentstudy in the MackenzieBasin, predation by introducedmammals (mainly stoats,cats and possibly ferrets) had a substantialimpact on Wrybill survivaland productivity. Prey- switchingby predatorsfollowing the introductionof rabbithaemorrhagic disease in 1997 probablyincreased predationrates on breedingwaders. A recentstudy of stoatsin the TasmanRiver showedthat 11% of stoat densexamined contained Wrybill remains.Breeding habitat is beinglost in somerivers and degraded in oth- ers,mainly by waterabstraction and flow manipulation,invasion of weeds,and human recreational use. Flood- ing causessome loss of nestsbut is alsobeneficial, keeping nesting areas weed-free. The breedingrange of the speciesappears to be contractingand fragmenting, with the bulk of the popula- tion now breedingin three large catchments. -
Harsh Winter Likely As Recession Bites by GILLIAN VINE Vouchers to Rise
THE MON T HLY MAGAZINE FOR T HE CA T HOLI C S OF T HE DUNE D IN DIO C ESE HE ABLE T MayT 2009 T Issue No 143 Singing for Mum … Five-year-old Ted Nelson (left) leads fellow pupils of St Joseph’s School, Balclutha, in singing You Are My Shepherd after the May 5 Mass at which his mother, Annie Nelson, was commissioned as principal of the school� Beside Ted is Tamara-Lee Rodwell� At the Mass, parish priest Fr Michael Hishon noted it was Good Shepherd Sunday and said a challenge to Mrs Nelson was “to be like the shepherd … and do her best to lead” the school� Fr Hishon spoke of Mrs Nelson’s love of and commitment to her calling and expressed his confidence that the roll, now standing at 53, would continue to rise under Mrs Nelson’s leadership� – Gillian Vine Harsh winter likely as recession bites By GILLIAN VINE vouchers to rise. demand will certainly be higher than ST VINCENT de Paul branches in the Dunedin area manager Ken Fahey last year,” he said. diocese are bracing themselves for also predicted a rise in requests for He attributed higher demand post- higher demand this winter as the assistance, saying: “Winter could be the Christmas to the tougher economic recession takes its toll. critical period.” climate, as overtime and even basic “I would expect it to get busier, In January and February, Dunedin’s St hours for workers were cut. Food bank especially with recent redundancies in Vincent de Paul food bank had recorded donations from Dunedin parishes were the town,” Oamaru St Vincent de Paul 25 per cent increases in demand on “solid” and he was “just so happy and shop manager Jeanette Verheyen said. -
Farming in North Otago
FARMING IN NORTH OTAGO J. D. CURRIE Ministry of Agriculture and Fisheries, Oarnaru Abstract North Otago is a well-established, efficiently farmed district. Primary production, which grossed an estimated $20 million in the 1973-4 season, will continue to be the major source of regional revenue. The geographic character and the soil resources of the district are described with a comprehensive coverage of historical development, current farming practices and future opportunities for pastoral development. The principal factor limiting agriculture in North Otago is a climate characterized by low, variable rainfall. Pastoral potential is closely tied to investment in oversowing, lucerne and irrigation. Successful farming under difhcult environmental conditions demands above-average ability. The managerial skill of North Otago’s farmers is an outstanding regional resource that augurs well for the future. GEOGRAPHIC DESCRIPTION NORTH OTAGO is a well-defined region. The northern, Canterbury, boundary follows the Waitaki River to its snowfield source in the Southern Alps beyond Lake Ohau. Above Kurow are the hydro dams, below Kurow the river remains as a broad natural boundary, flowing in swift braided channels down a bouldery bed to the sea. The southern boundary that isolates North Otago from its parent province is a mountain wall running north-west from Shag Point to the Lindis Pass and on to the Alps. A fork in the mountains that sweep round from Danseys Pass to Kurow divides North Otago into two districts that are distinct in nature and development. Inland, at Omarama, the sparsely populated run country is similar to Central Otago. Below Kurow is the more closely settled country, The moun- tains and foothills are only suited to extensive grazing, but most of the lower country is made up of rolling loessial downs, good natural grassland, much of it arable. -
Alps 2 Ocean Cycle Trail Visitor Survey 2020
LEAP Research Report No. 52 Alps 2 Ocean Cycle Trail Visitor Survey 2020 Lena Mkwara David Simmons Geoffrey Kerr November 2020 Alps 2 Ocean Cycle Trail Visitor Survey 2020 Lena Mkwara David Simmons Geoffrey Kerr Land Environment and People Research Report Report No. 52 November 2020 ISSN 1172-0859 (Print) ISSN 1172-0891 (PDF) ISBN 978-0-86476-452-2 (Print) ISBN 978-0-86476-455-3 (PDF) Lincoln University, Canterbury, New Zealand Abstract This report presents the findings from a 2020 survey of Alps 2 Ocean Cycle Trail (A2O) cyclists. COVID-19 cancelled fieldwork before data collection was complete. The limited data indicate that cyclists are extremely satisfied with the A2O and associated services, and make substantial expenditures associated with their ride. The A2O was a strong attractant to cyclists, the large majority of whom would not have visited the districts in the absence of the trail. Keywords A2O Cycle Trail, tourist attractions, tourism spending, economic attribution model, Mackenzie District, Waitaki District Acknowledgements This project benefitted immensely from the contributions of others. We wish to thank the following people for their generosity and assistance. Waitaki District Council, Tourism Waitaki and Cycle Journeys for their guidance and support. Accommodation providers and visitor centre operators who assisted with the distribution of survey cards. Lincoln University colleagues who peer reviewed the survey instrument. Dr Sally Driml, University of Queensland, for peer review of the survey instrument and the economic attribution model. Dr Yvonne Mathews, University of Waikato/Waikato Regional Council, for structuring the interactive mapping inputs. Dr Bentry Mkwara for GIS mapping assistance. -
Phaedra Upton1, Rachel Skudder2 and the Mackenzie Basin Lakes
Using coupled models to place constraints on fluvial input into Lake Ohau, New Zealand Phaedra Upton1, Rachel Skudder2 and the Mackenzie Basin Lakes Team3 [email protected], 1GNS Science, 2Victoria University of Wellington, 3GNS Science + Otago University + Victoria University of Wellington 2004: no large storms 0 2000 kg/sec 1/1/10 daily rainfall Godley River modelled suspended sediment load Tasman River LakeTekapo 1/1/00 0 200 mm Lake Pukaki 1995: large summer storm 0 2000 kg/sec Hopkins River Box core #1 1/1/90 daily rainfall modelled suspended Lake Ohau Box core #2 Raymond Film Services sediment load Ahuriri River Figure 2: Lake Tekapo following a large rainfall event in its catchment. A sediment laden inflow plunges into the lake and leaves the surface waters clear. We use HydroTrend (Kettner and Syvitski 2008, Computers and 6 m core Daily Rainfall (mm) 0 200 mm Geoscience, 34) to calculate the overall sediment influx into the lake and 1/1/80 couple it to a conceptual model of how this sediment might be distributed 1969: large winter storm through the lake basin depending on the season to produce model cores. 0 2000 kg/sec 0 3 6 12 18 24km Figure 1: Located east of the main divide in the central Southern Alps, the Mackenzie Lakes; Ohau, Pukaki and Tekapo, occupy fault Figure 3: Map of Lake Ohau showing the location of the three cores we controlled glacial valleys and contain high resolution sedimentary compare our models to. daily rainfall records of the last ~17 ka. These sediments potentially contain a 1/1/70 modelled suspended record of climatic events and transitions, earthquakes along the Alpine sediment load Fault to the northwest, landscape response during and following deglaciation and recent human-influenced land use changes. -
NIWA Lake Benmore Model Assessment Nutrient Load Effects
Updated model assessment of the effects of increased nutrient loads into Lake Benmore Prepared for Environment Canterbury August 2015 Prepared by : Bob Spigel (NIWA) David Plew (NIWA) David Hamilton (University of Waikato) Donna Sutherland (NIWA) Clive Howard-Williams (NIWA) For any information regarding this report please contact: Bob Spigel Scientist Hydrodynamics +64-3-343 8020 [email protected] National Institute of Water & Atmospheric Research Ltd PO Box 8602 Riccarton Christchurch 8011 Phone +64 3 348 8987 NIWA CLIENT REPORT No: CHC2015-089 Report date: August 2015 NIWA Project: ENC14506 Quality Assurance Statement Reviewed by: Sandy Elliot Approved for release John Quinn by: Ohau C Canal inflow entering Haldon Arm, Lake Benmore. [Donna Sutherland, NIWA] © All rights reserved. This publication may not be reproduced or copied in any form without the permission of the copyright owner(s). Such permission is only to be given in accordance with the terms of the client’s contract with NIWA. This copyright extends to all forms of copying and any storage of material in any kind of information retrieval system. Whilst NIWA has used all reasonable endeavours to ensure that the information contained in this document is accurate, NIWA does not give any express or implied warranty as to the completeness of the information contained herein, or that it will be suitable for any purpose(s) other than those specifically contemplated during the Project or agreed by NIWA and the Client. Contents Extended summary ............................................................................................................ -
Project River Recovery Bibliography
Project River Recovery bibliography 1991–July 2007 CANTERBURY SERIES 0208 Project River Recovery bibliography 1991 – JULY 2007 Project River Recovery Report 2007/02 Susan Anderson Department of Conservation, Private Bag, Twizel July 2007 Docdm-171819 - PRR Bibliography 2 INTRODUCTION Since its inception in 1991, Project River Recovery has undertaken or funded numerous research projects. The results of these investigations have been reported in various reports, theses, Department of Conservation publications, and scientific papers. Results of all significant research have been published, can be found through literature searches, and are widely available. Internal reports that do not warrant publication are held at the Twizel Te Manahuna Area Office and at the main Department of Conservation library in Wellington. All unpublished Project River Recovery reports produced since 1998 have been assigned report numbers. In addition to reports on original research, Project River Recovery has produced magazine articles and newspaper feature articles, various annual reports, progress reports, discussion documents, and plans. It has also commissioned some reports from consultants. This bibliography updates the bibliography compiled in 2000 (Sanders 2000) and lists all reports, theses, diplomas, Department of Conservation publications, and scientific papers that were produced or supported by Project River Recovery between 1991 and July 2007. It does not list brochures, posters, fact sheets, newsletters, abstracts for conference programmes, or minor magazine or newspaper articles. Docdm-171819 - PRR Bibliography 3 BIBLIOGRAPHY Adams, L.K. 1995: Reintroduction of juvenile black stilts to the wild. Unpublished MSc thesis, University of Canterbury, Christchurch. 108 p. Anderson, S.J. 2006: Proposal for black-fronted tern nest monitoring and predator trapping at the Ruataniwha Wetlands: 2006-2007 breeding season. -
Nohoanga Site Information Sheet Waianakarua (Glencoe Reserve)
Updated August 2020 NOHOANGA SITE INFORMATION SHEET WAIANAKARUA (GLENCOE RESERVE), NORTH OTAGO Getting there • The site is just west of Herbert, approximately 30 minutes south of Oamaru. • From Herbert township on State Highway 1, take Cullen Street to Monk Street, then head south to the end of Monk Street and west onto Glencoe Road. • Follow Glencoe Road, it will run onto Tulliemet Road. • Turn left at Camp Iona and follow the gravel road to the nohoanga site which is within the Department of Conservation camping site. The nohoanga site is on the right side of the entrance. • There is signage on site. For further information phone 0800 NOHOANGA or email [email protected] Page 1 of 5 Updated August 2020 Physical description • The nohoanga is not as large as other sites, but is flat and well-sheltered. • The site is an excellent area for camping. Vehicle access and parking • The site has excellent two wheel drive vehicle access right onto the site and is suitable for caravan and campervan use. • All vehicles should be parked on the nohoanga site and not the adjacent public camping area. Facilities and services • Nohoanga site users have permission to use the toilets and water located on the adjoining Department of Conservation camping area. As these facilities are shared with the public, always show consideration in accordance with the general information sheet. • The are no other facilities on the Waianakarua (Glencoe Reserve) nohoanga site. Site users need to provide their own shower facilities. • Water should be boiled at all times. • There is limited cell phone reception on this site. -
General Distribution and Characteristics of Active Faults and Folds in the Mackenzie District, South Canterbury D.J.A
General distribution and characteristics of active faults and folds in the Mackenzie District, South Canterbury D.J.A. Barrell D.T. Strong GNS Science Consultancy Report 2010/147 Environment Canterbury Report No. R10/44 June 2010 DISCLAIMER This report has been prepared by the Institute of Geological and Nuclear Sciences Limited (GNS Science) exclusively for and under contract to Environment Canterbury. Unless otherwise agreed in writing by GNS Science, GNS Science accepts no responsibility for any use of, or reliance on, any contents of this report by any person other than Environment Canterbury and shall not be liable to any person other than Environment Canterbury, on any ground, for any loss, damage or expense arising from such use or reliance. The data presented in this report are available to GNS Science for other use from June 2010 BIBLIOGRAPHIC REFERENCE Barrell, D.J.A., Strong, D.T. 2010. General distribution and characteristics of active faults and folds in the Mackenzie District, South Canterbury. GNS Science Consultancy Report 2010/147. 22 p. © Environment Canterbury Report No. R10/44 ISBN 978-1-877574-18-4 Project Number: 440W1435 2010 CONTENTS EXECUTIVE SUMMARY .........................................................................................................II 1. INTRODUCTION ..........................................................................................................1 2. INFORMATION SOURCES .........................................................................................2 3. GEOLOGICAL OVERVIEW