PEAK-BAGGERS GUIDE 2013 Area Peak 1:100 000 1:25 000 Ref
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CLIMBING FEDERATION PEAK, SOUTH WEST TASMANIA Macquarie (University) Mountaineering Club Trip 1972 by Barbara Cameron Smith June 5, 2014
CLIMBING FEDERATION PEAK, SOUTH WEST TASMANIA Macquarie (University) Mountaineering Club trip 1972 By Barbara Cameron Smith June 5, 2014 Our anti clockwise route towards and up Federation Peak is depicted in orange above, with the exception of our detour off the loop to climb Burgess Bluff. We subsequently camped at Pineapple Flat, scrub bashed our way to Mount Picton, and eventually walked out to Blakes Opening along an unexpectedly civilized track. Map credit: Bill Filson 7 January 1972 We packed all our gear and then went shopping. We expect to be out for 7-10 days, and after packing the necessary food and excess, the food bill tallied 26 dollars for four, quite a lot of money. We went to local camping stores and got some extra equipment, then called in to chat with a few guys who could tell us something about the walk. We repacked everything after a counter lunch in a pub and off we went. We walked quite a way out of the main street of Hobart. Greg and I started hitching and were lucky, getting a lift with a guy who was going camping himself. I guess I was rather forward but I asked him if he’d mind picking up our two friends who were on the road already. He didn’t seem to mind, so we were all driven down to Geeveston. Had a few refreshments there and left details at the police station and gear at the council chambers. It was rather late to get a lift, it being 4.30 pm, but a local housewife drove all of us a few miles out of town. -
LATE WISCONSIN GLACIATION of TASMANIA by Eric A
Papers and Proceedings of the Royal Society of Tasmania, Volume 130(2), 1996 33 LATE WISCONSIN GLACIATION OF TASMANIA by Eric A. Calhoun, David Hannan and Kevin Kiernan (with two tables, four text-figures and one plate) COLHOUN, E.A., HANNAN, D. & KIERNAN, K., 1996 (xi): Late Wisconsin glaciation of Tasmania. In Banks, M. R. & Brown, M.F. (Eds): CLIMATIC SUCCESSION AND GLACIAL HISTORY OF THE SOUTHERN HEMISPHERE OVER THE LAST FIVE MILLION YEARS. Pap. Proc. R. Soc. Tasm. 130(2): 33-45. https://doi.org/10.26749/rstpp.130.2.33 ISSN 0080-4703. Department of Geography, University of Newcastle, Callaghan, NSW, Australia 2308 (EAC); Department of Physical Sciences, University of Tasmania at Launceston, Tasmania, Australia 7250 (DH); Forest Practices Board ofTasmania, 30 Patrick Street, Hobart, Tasmania, Australia 7000 (KK). During the Late Wisconsin, icecap and outlet glacier systems developed on the West Coast Range and on the Central Plateau ofTasmania. Local cirque and valley glaciers occurred in many other mountain areas of southwestern Tasmania. Criteria are outlined that enable Late Wisconsin and older glacial landforms and deposits to be distinguished. Radiocarbon dates show Late Wisconsin ice developed after 26-25 ka BP, attained its maximum extent c. 19 ka BP, and disappeared from the highest cirques before 10 ka BP. Important Late Wisconsin age glacial landforms and deposits of the West Coast Range, north-central and south-central Tasmania are described. Late Wisconsin ice was less extensive than ice formed during middle and earlier Pleistocene glaciations. Late Wisconsin snowline altitudes, glaciological conditions and palaeodimatic conditions are outlined. Key Words: glaciation, Tasmania, Late Wisconsin, snowline altitude, palaeoclimate. -
A Review of Natural Values Within the 2013 Extension to the Tasmanian Wilderness World Heritage Area
A review of natural values within the 2013 extension to the Tasmanian Wilderness World Heritage Area Nature Conservation Report 2017/6 Department of Primary Industries, Parks, Water and Environment Hobart A review of natural values within the 2013 extension to the Tasmanian Wilderness World Heritage Area Jayne Balmer, Jason Bradbury, Karen Richards, Tim Rudman, Micah Visoiu, Shannon Troy and Naomi Lawrence. Department of Primary Industries, Parks, Water and Environment Nature Conservation Report 2017/6, September 2017 This report was prepared under the direction of the Department of Primary Industries, Parks, Water and Environment (World Heritage Program). Australian Government funds were contributed to the project through the World Heritage Area program. The views and opinions expressed in this report are those of the authors and do not necessarily reflect those of the Tasmanian or Australian Governments. ISSN 1441-0680 Copyright 2017 Crown in right of State of Tasmania Apart from fair dealing for the purposes of private study, research, criticism or review, as permitted under the Copyright act, no part may be reproduced by any means without permission from the Department of Primary Industries, Parks, Water and Environment. Published by Natural Values Conservation Branch Department of Primary Industries, Parks, Water and Environment GPO Box 44 Hobart, Tasmania, 7001 Front Cover Photograph of Eucalyptus regnans tall forest in the Styx Valley: Rob Blakers Cite as: Balmer, J., Bradbury, J., Richards, K., Rudman, T., Visoiu, M., Troy, S. and Lawrence, N. 2017. A review of natural values within the 2013 extension to the Tasmanian Wilderness World Heritage Area. Nature Conservation Report 2017/6, Department of Primary Industries, Parks, Water and Environment, Hobart. -
IUCN S07: TASMANIAN WILDERNESS (Revision to Existing
WORLD HERITAGE NOMINATION - IUCN S07: TASMANIAN WILDERNESS (Revision to existing Property inscribed in 1982) Summary prepared by IUCN (April 1989) based on the original nomination submitted by the Government of Australia. This original and all documents presented in support of this nomination will be available for consultation at the meeting of the Bureau and the Committee. Note: In the light of the Bureau's concurrence with proposals to further extend the nominated site, the State Party's nomination of 1,374,000 ha in total, further revised in September 1989, is discussed in the IUCN Technical Evaluation. 1. LOCATION Comprises a contiguous network of reserved lands that extends over much of south-western Tasmania. including five national parks (Cradle Mountain-Lake St Clair, Franklin-Lower Gordon Wild Rivers, Southwest, Walls of Jerusalem and Hartz Mountains), four state reserves (Devils Gullet, Marakoopa Cave, Exit Cave and Port Davey) and part of Liffey Falls State Reserve, four conservation areas (Central Plateau, Oakleigh Creek, Southwest and St. Clair Lagoon), and"a number of protected areas, forest reserves as well as land verted in the Hydro-Electric Commission. Several outliers are included in the nominated area: Sarah Island Historic Site .in Macquarie Harbour; and lIe du Golfe, De Witt Island, Flat Witch Island and Maatsukyer Island off the south coast of Tasmania. Lake Gordon and some land adjoining it in the centre of this network has been developed for hydro-electric purposes and is excluded. 41°3S'-43°40'S, l4S02S'-l46°55'E. 2. JURIDICAL DATA Apart from approximately 330ha of privately-owned land in the Vale of Rasselas, on the Central Plateau and at Pillinger, land is publicly owned and includes 773,215ha under national parks, 2074h under state reserves, c. -
Review of the Upper Parmeener Supergroup
IJRJ981_0i .M Tasmania Department of Mines - Report 1987/01 Review of the Upper Parmeener Supergroup by S. M. Forsyth INTRODUCTION intrude Parmeener Strata, largely as transgressive sheets and dykes several hundred metres thick (Schmidt and Strata of Late Carboniferous to Late Triassic age are McDougall, 1977; Leaman, 1975) Metamorphism caused widespread in Tasmania. The strata are essentially by the intrusions is minimal, but disruption of the host flat -lying and were named the Panneener Supergroup by strata particularly above feeders and at steeply Banks (1973). The Panneener Supergroup has been transgressive sheet segments and at junctions of intrusion formally subdivided into a Lower division that includes segments, caused significant breaks in the continuity of all known glaciomarine strata and an Upper division that lithological units. Further disruption of the strata has been consists of freshwater strata (Forsyth et al.,1974). caused by subsequent block faulting. Erosion has Strata of the Parmeener Supergroup rest (commonly with completely removed the Parmeener strata from some area. pronounced landscape unconformity) or granitic and The uppennost strata tend to be preserved only in graberts folded rocks. They obtain a maximum composite or where Jurassic dolerite sheets or Tertiary basalt flows thickness of about 2 Ian. Most of the initial basement have slowed erosion. irregularities were buried during deposition of the Lower This review deals largely with the stratigraphy and Parmeener Supergroup. Local disconfonnities, very palaeontology of the Upper Parmeener Supergroup and is slightly angular erosive unconformities and condensed an expanded version of the section on the stratigraphy of sequences indicate surface subsidence was not entirely the Upper Parmeener Supergroup in the Geology and unifonn during deposition of the Parmeener Supergroup MineraIDepositsofTasmania(BurrettandMartin,1989). -
3966 Tour Op 4Col
The Tasmanian Advantage natural and cultural features of Tasmania a resource manual aimed at developing knowledge and interpretive skills specific to Tasmania Contents 1 INTRODUCTION The aim of the manual Notesheets & how to use them Interpretation tips & useful references Minimal impact tourism 2 TASMANIA IN BRIEF Location Size Climate Population National parks Tasmania’s Wilderness World Heritage Area (WHA) Marine reserves Regional Forest Agreement (RFA) 4 INTERPRETATION AND TIPS Background What is interpretation? What is the aim of your operation? Principles of interpretation Planning to interpret Conducting your tour Research your content Manage the potential risks Evaluate your tour Commercial operators information 5 NATURAL ADVANTAGE Antarctic connection Geodiversity Marine environment Plant communities Threatened fauna species Mammals Birds Reptiles Freshwater fishes Invertebrates Fire Threats 6 HERITAGE Tasmanian Aboriginal heritage European history Convicts Whaling Pining Mining Coastal fishing Inland fishing History of the parks service History of forestry History of hydro electric power Gordon below Franklin dam controversy 6 WHAT AND WHERE: EAST & NORTHEAST National parks Reserved areas Great short walks Tasmanian trail Snippets of history What’s in a name? 7 WHAT AND WHERE: SOUTH & CENTRAL PLATEAU 8 WHAT AND WHERE: WEST & NORTHWEST 9 REFERENCES Useful references List of notesheets 10 NOTESHEETS: FAUNA Wildlife, Living with wildlife, Caring for nature, Threatened species, Threats 11 NOTESHEETS: PARKS & PLACES Parks & places, -
Characteristics of Interstate and Overseas Bushwalkers in the Arthur Ranges, South West Tasmania
CHARACTERISTICS OF INTERSTATE AND OVERSEAS BUSHWALKERS IN THE ARTHUR RANGES, SOUTH-WEST TASMANIA By Douglas A. Grubert & Lorne K. Kriwoken RESEARCH REPORT RESEARCH REPORT SERIES The primary aim of CRC Tourism's research report series is technology transfer. The reports are targeted toward both industry and government users and tourism researchers. The content of this technical report series primarily focuses on applications, but may also advance research methodology and tourism theory. The report series titles relate to CRC Tourism's research program areas. All research reports are peer reviewed by at least two external reviewers. For further information on the report series, access the CRC website [www.crctourism.com.au]. EDITORS Prof Chris Cooper University of Queensland Editor-in-Chief Prof Terry De Lacy CRC for Sustainable Tourism Chief Executive Prof Leo Jago CRC for Sustainable Tourism Director of Research National Library of Australia Cataloguing-in-Publication Data Grubert, Douglas. Characteristics of interstate and overseas bushwalkers in the Arthur Ranges, South West Tasmania. Bibliography. ISBN 1 876685 83 2. 1. Hiking - Research - Tasmania - Arthur Range. 2. Hiking - Tasmania - Arthur Range - Statistics. 3. National parks and reserves - Public use - Tasmania - Arthur Range. I. Kriwoken, Lorne K. (Lorne Keith). II. Cooperative Research Centre for Sustainable Tourism. III. Title. 796.52209946 © 2002 Copyright CRC for Sustainable Tourism Pty Ltd All rights reserved. No parts of this report may be reproduced, stored in a retrieval system or transmitted in any form or by means of electronic, mechanical, photocopying, recording or otherwise without the prior permission of the publisher. Any enquiries should be directed to Brad Cox, Director of Communications or Trish O’Connor, Publications Manager to [email protected]. -
A Fascination with a Cartoon Animal and a Class V River Lured Her to The
A fascination with a cartoon THE animal and a Class V river lured her to the empty wilderness of Tasmania. Turns out the raw side of Down devil Under offers an made me amazing number of pristine places to camp, surf, hike, mountain bike, and kayak. STEPHANIE PEARSON goes all in. Bruny Island, off Tasmania’s southern coast DO IT 68 OUTSIDE MAGAZINE Cocooned in my sleeping bag, I stare a foot by the Franklin. Fewer than 500 people per vish that zoomed around like a tornado, above me at whorls of coral and register that year attempt it, and some don’t come out the slicing through boulders and trees. In 2000, I’m lying under thousands of tons of over other end. In 1822, eight convicts fled into the I cycled and roadtripped for six weeks hanging rock. We’re camping alongside the Franklin watershed to escape Sarah Island through mainland Australia while reading Franklin River at the Newlands Cascades rap prison, the British Empire’s version of the Robert Hughes’s The Fatal Shore, a history ids, in the shallow caves that form the base of Gulag Archipelago, on Tasmania’s west coast. of Oz’s settling, in which Tasmania played a aThe limestone wall 100 feet high.cave I can make out Only oneis man, Alexander like Pearce, walked out acritical and darkwomb. role. In 1803, the British cap a delicate web on the ceiling, likely the work alive—after killing and eating five of his fel italized on the island’s isolation, colonizing it of a Tasmanian cave spider, and wonder if a low escapees. -
CHANGES in SOUTHWESTERN TASMANIAN FIRE REGIMES SINCE the EARLY 1800S
Papers and Proceedings o/the Royal Society o/Tasmania, Volume 132, 1998 IS CHANGES IN SOUTHWESTERN TASMANIAN FIRE REGIMES SINCE THE EARLY 1800s by Jon B. Marsden-Smedley (with five tables and one text-figure) MARSDEN-SMEDLEY, ].B., 1998 (31:xii): Changes in southwestern Tasmanian fire regimes since the early 1800s. Pap.Proc. R. Soc. Tasm. 132: 15-29. ISSN 0040-4703. School of Geography and Environmental Studies, University of Tasmania, GPO Box 252-78, Hobart, Tasmania, Australia 7001. There have been major changes in the fire regime of southwestern Tasmania over the past 170 years. The fire regime has changed from an Aboriginal fire regime of frequent low-intensity fires in buttongrass moorland (mostly in spring and autumn) with only the occasional high-intensity forest fire, to the early European fire regime of frequent high-intensity fires in all vegetation types, to a regime of low to medium intensity buttongrass moorland fires and finally to the current regime of few fires. These changes in the fire regime resulted in major impacts to the region's fire-sensitive vegetation types during the early European period, while the current low fire frequency across much of southwestern Tasmania has resulted in a large proportion of the region's fire-adapted buttongrass moorland being classified as old-growth. These extensive areas of old-growth buttongrass moorland mean that the potential for another large-scale ecologically damaging wildfire is high and, to avoid this, it would be better to re-introduce a regime oflow-intensity fires into the region. Key Words: fire regimes, fire management, southwestern Tasmania, Aboriginal fire, history. -
Paradoxes of Protection Evolution of the Tasmanian Parks and Wildlife Service and National Parks and Reserved Lands System
Paradoxes of Protection Evolution of the Tasmanian Parks and Wildlife Service and National Parks and Reserved Lands System By Dr Louise Crossley May 2009 A Report for Senator Christine Milne www.christinemilne.org.au Australian Greens Cover image: Lake Gwendolen from the track to the summit of Frenchmans Cap, Tasmanian Wilderness World Heritage Area Photo: Matt Newton Photography Table of Contents EXECUTIVE SUMMARY .................................................................................................. 1 1. THE INITIAL ESTABLISHMENT OF PARKS AND RESERVES; UTILITARIANS VERSUS CONSERVATIONISTS 1915-1970....................................................................... 3 1.1 The Scenery Preservation Board as the first manager of reserved lands ............................................................ 3 1.2 Extension of the reserved lands system ................................................................................................................... 3 1.3The wilderness value of wasteland ........................................................................................................................... 4 1.4 Inadequacies of the Scenery Protection Board ...................................................................................................... 4 2. THE ESTABLISHMENT AND ‘GLORY DAYS’ OF THE NATIONAL PARKS AND WILDLIFE SERVICE 1971-81 ........................................................................................... 6 2.1 The demise of the Scenery Preservation Board and the Lake Pedder controversy -
Exploration of the Western Country Mr. Gould's Report
(No. 4.) 18 6 0. TASMAN I A. EXPLORATION OF THE WESTERN COUNTRY. MR. GOULD'S RE PORT. Laid upon the Table by Mr. Attorney-General, and ordered by the House to be printed, 25 July, 1860. Geological Survey Of!ic,e, 26tli June, 1860. Sm, I HAVE the honor to forward you an account of the exploration of the Western Country, conducted recently by myself according to your instructions; and to assist you in compre hending the physical structure and nature of the country explored, as well as the various routes pursued by the Expedition, I have prepared the accompanying Map, which embraces the whole of the country visited, and upon which, in addition to the topographical information a_cquired, I have expressed the geologi9al structure by the assistance of distinguishing colours. I have found it convenient to distribute the information obtained under several headings. In the first section of the Report, which is in the form of a brief narrative, I have confined myself to a g·eneral description of the progress of the Expedition, of the country visited, and of the steps taken for the purpose of testing its reput_ed richness in auriferous deposits. The second is devoted to a sketch of the geological structure of the district, and to the con sideration of its mineral capabilities; while, in the last, I have appended a few general remarks upon those portions which are available for settlement, together with meteorological tables which may be of interest as furnishing some information as to the nature of its clim'ate. I have the honor to remain, Sir, Your v~ry obedient Servant, CHARLES GOULD. -
Ben Lomond Management Plan 1998
Ben Lomond National Park Management Plan 1998 Parks and Wildlife Service DepartmentDepartment of Primaryof Environment Industries, Waterand Land and Management Environment Ben Lomond National Park - Management Plan, 1998 BEN LOMOND NATIONAL PARK MANAGEMENT PLAN 1998 This Management Plan for the Ben Lomond National Park has been prepared in accordance with the requirements of part IV of the National Parks and Wildlife Act 1970. A draft of this plan was released for public comment in accordance with statutory requirements from 7 June 1997 until 19 September 1997. This plan is a modified version of that draft, having been varied to take account of public input during that period and the views of the National Parks and Wildlife Advisory Council. Unless otherwise specified, this plan adopts the interpretation of terms given in Section 3 of the National Parks and Wildlife Act 1970. The term “Minister” when used in the plan means the Minister administering the Act. The term “Park” refers to the Ben Lomond National Park. In accordance with Section 23(2) of the National Parks and Wildlife Act 1970, the managing authority for the Park, in this case the Director of National Parks and Wildlife, shall carry out his or her duties in relation to the Park for the purpose of giving effect to, and in accordance with the provisions of, this Management Plan. The position of Director is held by the Director, Parks and Wildlife Service, Department of Primary Industries, Water and Environment. In accordance with Section 23(2) of the National Parks and Wildlife Act 1970, and with Section 6 and Section 23(5) of the Ben Lomond Skifield Management Authority Act 1995, the managing authority for the Skifield Development Area within the Park, the Ben Lomond Skifield Management Authority, shall carry out its duties in relation to that portion of the Park within the Skifield Development Area for the purposes of giving effect to, and in accordance with the provisions of, this Management Plan.