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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. -
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, -
World Heritage Values and to Identify New Values
FLORISTIC VALUES OF THE TASMANIAN WILDERNESS WORLD HERITAGE AREA J. Balmer, J. Whinam, J. Kelman, J.B. Kirkpatrick & E. Lazarus Nature Conservation Branch Report October 2004 This report was prepared under the direction of the Department of Primary Industries, Water and Environment (World Heritage Area Vegetation Program). Commonwealth 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 Department of Primary Industries, Water and Environment or those of the Department of the Environment and Heritage. ISSN 1441–0680 Copyright 2003 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, Water and Environment. Published by Nature Conservation Branch Department of Primary Industries, Water and Environment GPO Box 44 Hobart Tasmania, 7001 Front Cover Photograph: Alpine bolster heath (1050 metres) at Mt Anne. Stunted Nothofagus cunninghamii is shrouded in mist with Richea pandanifolia scattered throughout and Astelia alpina in the foreground. Photograph taken by Grant Dixon Back Cover Photograph: Nothofagus gunnii leaf with fossil imprint in deposits dating from 35-40 million years ago: Photograph taken by Greg Jordan Cite as: Balmer J., Whinam J., Kelman J., Kirkpatrick J.B. & Lazarus E. (2004) A review of the floristic values of the Tasmanian Wilderness World Heritage Area. Nature Conservation Report 2004/3. Department of Primary Industries Water and Environment, Tasmania, Australia T ABLE OF C ONTENTS ACKNOWLEDGMENTS .................................................................................................................................................................................1 1. -
Papers of Theroyal Society of Tasmania 1927
lll ,- <> PAPERS OF THE ROYAL SOCIETY OF TASMANIA 1927 THE SOUTH COAST AND PORT DAV·EY, TASMANIA, By CLIVE LoRD, F .L.S. (Director of the Tasmanian Museum). CORRIGENDA (Plates I.-XII. and Five Text figures.) (Read 11th April, 1927.) Page 187, line six-Early in 1850 sho1tld read Early INTRODUCTORY. in 1853. On 13th September, 1875, the late Hon. J. R. Scott read Page 193-The Paragraph b~ginning "The coast line'' a paper (Scott, P. & P. Roy. Soc. Tas., 1875) before this should come before "(b) Stratigraphy" ~n page 192. Society describing Port Davey. The facts contained in Scott's paper are of value at the present time to those in search of information concerning the early history of the south-western portion of Tasmania, and as in years to come information may be desired concerning the condition of the south-western regi-on half a century after Scott's account was written, the writer desires to place on record certain brief general obser vations concerning this interesting area. The remarks made in the present instance are the out come of two brief visits to this area. In January, 1926, I visited the South Coast as far as New Harbour in my own yacht Telopea. Again, in January, 1927, at the kind invi tation of Mr. M. R. Freney, I visited the S-outh C-oast and Port Davey in the ketch Len'IUL (S. Purdon, Skipper). Messrs. P. B. Nye and F. Blake of the Mines Department were also members of this latter excursion. During the recent visit to this area we landed at Cox Bight, and camped for some days before walking across and rejoining our !boat at Port Davey. -
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. -
Conservation of Natural Wilderness Values in the Port Davey Marine and Estuarine Protected Area, South-Western Tasmania
AQUATIC CONSERVATION: MARINE AND FRESHWATER ECOSYSTEMS Aquatic Conserv: Mar. Freshw. Ecosyst. 20: 297–311 (2010) Published online 3 December 2009 in Wiley InterScience (www.interscience.wiley.com). DOI: 10.1002/aqc.1079 Conservation of natural wilderness values in the Port Davey marine and estuarine protected area, south-western Tasmania GRAHAM J. EDGARa,b,Ã, PETER R. LASTc, NEVILLE S. BARRETTb, KAREN GOWLETT-HOLMESc, MICHAEL DRIESSENd and PETER MOONEYe aAquenal Pty Ltd, GPO Box 828, Hobart, Tasmania, Australia 7001 bTasmanian Aquaculture and Fisheries Institute, University of Tasmania, GPO Box 252-49, Hobart, Tasmania, Australia 7001 cCSIRO Divison of Marine and Atmospheric Research, Castray Esplanade, Hobart, Tasmania, Australia 7000 dDepartment of Primary Industries and Water, Hobart, Tasmania, Australia 7000 eParks and Wildlife Service, Hobart, Tasmania, Australia 7000 ABSTRACT 1. Port Davey and associated Bathurst Harbour in south-western Tasmania represent one of the world’s most anomalous estuarine systems owing to an unusual combination of environmental factors. These include: (i) large uninhabited catchment protected as a National Park; (ii) ria geomorphology but with fjord characteristics that include a shallow entrance and deep 12-km long channel connecting an almost land-locked harbour to the sea; (iii) high rainfall and riverine input that generate strongly-stratified estuarine conditions, with a low-salinity surface layer and marine bottom water; (iv) a deeply tannin-stained surface layer that blocks light penetration to -
Eroding Landforms Within the Port Davey Ria Estuary Complex: Wave Wake Or Sea Level Rise?
Eroding landforms within the Port Davey ria estuary complex: wave wake or sea level rise? Monitoring report for the decade 2000 – 2010 Jason Bradbury Geodiversity Conservation and Management Resource Management and Conservation Division Department of Primary Industries, Parks, Water and Environment 15 April 2011 Eroding ria estuaries of Port Davey Summary The Port Davey region and its catchment area lie entirely within the Tasmanian Wilderness World Heritage Area and are in largely natural condition. Several discrete sub-estuaries contain a complex assemblage of depositional Holocene landforms that, due to their intimate genetic association with flora (and possibly fauna) of Gondwanan affinity, are probably globally unusual if not unique. Despite the depositional context a monitoring programme first established in 1992 has consistently recorded widespread erosion at a rate of a few millimetres per year. This paper reports some monitoring results and geomorphological observations collected over the past decade and makes the following recommendations with respect to management of vessel wave wake: • maintain the existing five knot speed limit in Melaleuca Inlet and Creek; • introduce a five knot speed limit on the Davey River upstream of Brookes Reach, • close Manwoneer Inlet to motorised boating, While many of the bank types present are susceptible to vessel wave wake the distribution of erosion indicates that wake is not the principle cause of the erosion recorded. It is concluded that sea level rise presents the most likely mechanism to effect the observed erosion and that in the otherwise essentially undisturbed Port Davey catchment estuarine change from a depositional to erosional regime is a clear marker of the onset of the Anthropocene epoch (in which the geological record is characterised by significant human influence). -
Constitution Act 1934 (Tas) [Transcript
[Received from the Clerk of the Legislative Council the 10th day of January 1935 A.G. Brammall Registrar Supreme Court] TASMANIA. _________ THE CONSTITUTION ACT 1934. _________ ANALYSIS. PART I. – PRELIMINARY. Division III. – The Assembly. 1. Short title. 22. Constitution of the Assembly. 2. Repeal. 23. Triennial Parliaments. 3. Interpretation. 24. Election of Speaker. 25. Quorum of the Assembly. PART II. – THE CROWN. Division IV. – Electoral Divisions and 4. Parliament not dissolved by demise Qualifications Of Electors. of the Crown. 5. Demise of the Crown not to affect 26. Council Divisions. things done before proclamation 27. Assembly Divisions. thereof. 28. Qualification of electors for the 6. All appointments, &c., by the Gover- Legislative Council. nor to continue in force notwith- Joint tenants. standing demise of the Crown. 29. Assembly electors. 7. All civil or criminal process, and all contracts, bonds, and engagements Division V. – Disqualification; Vacation with or on behalf of His Majesty Of Office; Penalty. to subsist and continue notwith- standing demise. 30. Oath to be taken by members. 8. Deputy-Governor’s powers. 31. Commonwealth membership. Interpretation. 32. Office of profit. Exercise of powers by Deputy- 33. Contractors. Governor. 34. Vacation of office for other causes. Provision as to deputy of Lieutenant- 35. Penalty for sitting when disqualified. Governor or Administrator. Act to be retrospective. PART IV. – MONEY BILLS; POWERS OF HOUSES PART III. – PARLIAMENT. 36. Interpretation. Division I. – Both Houses. 37. Money bills to originate in the Assembly. 9. Continuation of existing Houses. 38. All money votes to be recommended Continuance in office of existing by the Governor. -
The Construction of Wilderness in the Work of John Watt Beattie (1859-1930)
Macquarie University Faculty of Arts Department of Modern History, Politics and International Relations An orientation to nature: The construction of wilderness in the work of John Watt Beattie (1859-1930) Jarrod Ray Hore Bachelor of Arts (Macquarie University) A thesis submitted in fulfilment of the requirements for the degree Masters of Research Acknowledgements I am taking this opportunity to express my gratitude to all those who supported me throughout this Masters of Research thesis. I am particularly indebted to Doctor Alison Holland for her indispensable direction and helpful feedback throughout 2014 and to Doctor Leigh Boucher for his guidance and encouragement over a number of years. I would like to thank the staff of the Department of Modern History, Politics and International Relations at Macquarie University for the welcoming and supportive environment that has encouraged me since I began university in 2009. I would like to thank the University of Tasmania Library Special and Rare Collections, the National Library of Australia and the Mitchell Library of New South Wales for the access I was granted to the material necessary for the completion of this thesis. I am grateful for all the friendship, inspiration and support of the first cohort of Masters of Research candidates in Modern History at Macquarie University and I appreciate all the assistance, advice and criticism that my peers and family have provided. I would like to thank Miss Alice Robinson for her consistent dedication to the development of my writing and her confidence in my ability. Finally, I express my warm thanks to Miss Olivia Lynch for her corrections, comments and suggestions on the draft of this paper. -
Spreadsheet Listing Contents of All Recorded Issues
TFNC tasnatcontentslist — Index printed 10-07-16, Index page 1/22 Year Month Vol No Page To Title Author1 Author2 Author3 Author4 Author5 Author6 Author7 1907 April 1 1 1 1 Ourselves Anon. 1907 April 1 1 1 5 The Coccidea: a family of remarkable insects Lea, A.M. 1907 April 1 1 5 6 Club notes: January meeting; March meeting Anon. 1907 April 1 1 6 10 Swan shooting on the east coast of Tasmania Elliott, E.A. 1907 April 1 1 10 11 Club notes: list of members Anon. 1907 April 1 1 11 12 The breeding habits of bronzewing pigeons Roberts, M.G. Camp out of the Field Naturalists' Club on Bruni [sic] Island, 1907 September 1 2 1 3 Elliott, E.A. Easter, 1907 1907 September 1 2 3 8 Tasmanian quail and game propagation Reid, A.R. 1907 September 1 2 8 9 A parasite upon flies Nicholls, H.M. Club notes: April meeting; May meeting; August meeting; 1907 September 1 2 10 11 Anon. miscellaneous observations (beetle/bush-rats; ground thrush) An entomologist's cycling trip to Cloncurry (Queensland) (incl. 1907 September 1 2 12 13 Hacker, H. note by Arthur M. Lea) Club notes: excursion to Botanic Gardens; excursion to South 1907 September 1 2 14 14 Anon. Bridgewater; printing fund Notes on the amorpholithes of the Tasmanian aborigines. No. 1.- 1907 September 1 2 14 19 Noetling, F. the native quarry on Coal Hill, near Melton Mowbray Club notes: annual report; statement of receipts and expenditure 1907 September 1 2 19 20 Anon. -
Freshwater Systems Between 1997 and 2002, with the Addition of New Observations
Status of Trout-free Waters in the Tasmanian Wilderness World Heritage Area Report to Department of Primary Industries, and Water, Hobart. PE Davies, LSJ Cook, WR Robinson, T Sloane June 2009 82 Waimea Ave, Sandy Bay, FFrreesshhwwaatteerr Tasmania Australia 7005 Ph/Fax: 03 62254660 SSyysstteemmss [email protected] Aquatiic Enviironmentall Consulltiing Serviice Table of Contents Executive Summary ............................................................................................................................. 3 Acknowledgements ............................................................................................................................. 5 1. Aims and Background ..................................................................................................................... 6 1.1 Aims ........................................................................................................................................... 6 1.2 Alien fish in the Tasmanian Wilderness World Heritage Area .................................................. 6 1.3 Brown trout ............................................................................................................................... 7 1.4 Value of trout-free waters ........................................................................................................ 8 2. Mapping the Distribution of Trout-free Waters ........................................................................... 10 2.1 Fish distribution database ...................................................................................................... -
Structure of the Precaivibrian Rocks of the Davey River Area, South#Western Tasmania
IA1alluscript reech'ed 20lh October. J 970 STRUCTURE OF THE PRECAIVIBRIAN ROCKS OF THE DAVEY RIVER AREA, SOUTH#WESTERN TASMANIA By C. J ..MACLEAN AND E. A. BOWEN School of Earth Sciences, A1acqullrie Umversfty. Sydney. ABS1'RACl Phase Symbol Textural Event rhe Precambrian quartzites and schists of the Davey L1 There are several lineations in this River area are characterised hv subvertical foliations group, probably of different ages. and garnet grade metamorphism. Three metamorphic Vari'Otls tex.tural expressions are: events are fonowed by several episodes of flexural (a) Micro crellulations (in schists) rdolding. (b) Surface rodding on S1 in quartzites INTRODlJC'fION AND ACKNOWLEDGEMENTS (c) Crystallographic orienta (ion of Detailed lithological and structural mapping has been quartz made at the Davey River, between its junction with the (d) Colour streaking in quartzite. Crossing River and the Davey Saddle, a ridge over F2 S2 (a) In schists, axial planes t'O crenulated looking the sea at Bond Bay, in Southwest Tasmania, rnicas about 70 mites sOllth of Frenchman's Cap. (b) In quartzites, axial planes to crenu The field work was conducted as part 'Of a regional lations in the flat-quartz foliation survey for the Hydro-Electric Commission under the (SI), with a parallel mica foliation. general supervision of Mr G. F. A. Hale and Dr K. L (e) Mesoscopically, S2 is a crenulation Burns. The logistic alssistance of the Commission, cleavage with transposition of lith particularly in respect of transport and base facilities, ology C'onfined to small areas where made the work possible. The assista nee 'Of officers of S2 is intensely developed.