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Natural History and Values of the Kanamaluka/Tamar Estuary Formation, Function and Ecology
TAMAR ESTUARY AND ESK RIVERS PROGRAM EDUCATION SERIES - FACT SHEET 2 nrmnorth.org.au Natural history and values of the kanamaluka/Tamar estuary Formation, function and ecology The kanamaluka/Tamar estuary is unique in South and North Esk rivers met at the mouth many ways. Fed by five major river systems, it of Corra Lynn Gorge. drains the largest catchment in Tasmania, and Between 35 and 47 million years ago, several the estuary itself is the longest navigable large lava flows occurred in the north, middle estuary in Australia. Home to many unique and southern parts of the valley. The lava and sometimes threatened plant and animal cooled to form basalt. In the middle sections species, it is truly a special place. the basalt capped the old lake sediments, HOW WAS IT FORMED? preserving them from further erosion. This can be seen at Grindelwald, Windermere, and In the early geological history of Tasmania, the north of Hillwood. Tamar Valley didn’t exist and was instead a large peneplain, or dolerite capped lowland Basalt at Rowella and Bell Bay forced the river area, that had been worn down by millions of to keep to its channel, preventing it from years of erosion. From 95 to 65 million years eating sideways into the old sediments and ago, stretching of the earth’s crust created blocking the river for some time at Whirlpool earthquakes that split this peneplain apart, Reach and Bell Bay, creating new lakes in the creating the highland areas of Mt Arthur, Mt valley again, which were eventually breached Barrow and Ben Lomond to the east and the and the Tamar resumed its old course. -
Smart Decisions. Strong Partnerships. Stronger Communities
2025 smart decisions. strong partnerships. stronger communities. With Funding support from Australian Government through Primary Health 2 WEST COAST COMMUNITY PLAN 2025 contents the plan 03 Our Future 05 Our Place Our Lifestyle 11 Our Community Plan 20 Future Directions 23 What We Said our plan for action Our People Our Community 29 Our Economy 32 Our Infrastructure 34 Our Environment 36 Our Partnerships Our Leadership 37 3 WEST COAST COMMUNITY PLAN 2025 from the Mayor & General Manager our future t is with great pride that we present the We look forward to continuing these West Coast Community Plan 2025, a valued partnerships and connections, as the vision for the West Coast which will guide community moves forward with a whole-of- the Region over the next 10 years and community response to the vision provided Ibeyond. for the West Coast. West Coast’s Community Plan provides an The community embraced the opportunity opportunity to strategically plan a future that to be part of a vision for the Region, and the community, Council, government, non- that is reflected through the engagement government organisations, businesses and process and reflected in the Plan. West stakeholders can work towards together. Coast Council would like to sincerely thank the community for their enthusiasm The Community Plan has been developed and responsiveness to the West Coast by the West Coast community, for the Community Plan engagement process. community. More than 2,000 people were The visions, suggestions, and comments involved in some way in the development provided by the community have resulted of this plan, and it is the culmination of the in the development of the first West Coast ideas, vision, and concerns of our community. -
A Biological Monitoring Survey of Reef Biota Within Bathurst Channel, Southwest Tasmania 2010 Neville Barrett, Elizabeth Oh, Lisa Meyer, Dane Jones and Graham Edgar
A BIOLOGICAL MONITORING SURVEY OF REEF BIOTA WITHIN BATHURST CHANNEL, SOUTHWEST TASMANIA 2010 NEVILLE BARRETT, ELIZABETH OH, LISA MEYER, DANE JONES AND GRAHAM EDGAR Executive Summary The benthic reef communities of Bathurst Channel represent an important feature for the ongoing management of Tasmania‟s marine ecology and diversity. Containing a number of fragile deep-water invertebrate species growing at accessibly shallow depths, the reef habitats are both susceptible to impacts and of scientific importance. The foundation for this study was the continuing need for a practical, quantitative monitoring program which will provide information on species composition, species distribution throughout the channel, and detect any changes occurring over time. The survey, conducted in March 2010, collected digital image data from depth intervals ranging from the intertidal zone to 20 metres depth at 13 monitoring sites extending throughout Bathurst channel, and compared it to baseline imagery taken in 2002. The high resolution imagery collected in 2010 was used to create a descriptive catalogue of the biota observed, which can be used for future monitoring and species referencing. Species and substrate percentage cover in the photos was analysed using an easily repeatable point count method (CPCe) where data files can be stored and reanalysed. The information collected described the changes in species composition along Bathurst Channel, and thus provided some insight into the relevant environmental and biological factors limiting the distribution of algal and invertebrate species throughout the estuary. Results were consistent with previous descriptions of the community types within the Channel, showing that this system is inherently stable over these time frames. -
Background Report
Gordonvale World Heritage Area Reserve Background Report www.tasland.org.au Tasmanian Land Conservancy (2015). Gordonvale World Heritage Area Reserve Background Report. Tasmanian Land Conservancy, Tasmania Australia 7005. Copyright ©Tasmanian Land Conservancy The views expressed in this report are those of the Tasmanian Land Conservancy and not the Commonwealth Government, State Government or any other entity. This work is copyright. It may be reproduced for study, research or training purposes subject to an acknowledgment of the sources and no commercial usage or sale. Requests and enquires concerning reproduction and rights should be addressed to the Tasmanian Land Conservancy. Front Image: Gordonvale homestead (archive photo) and the Vale of Rasselas landscape © Grant Dixon Contact Address Tasmanian Land Conservancy PO Box 2112, Lower Sandy Bay, 827 Sandy Bay Road, Sandy Bay Tasmania, AUSTRALIA 7005 | p: 03 6225 1399 | www.tasland.org.au | Contents Page Acknowledgments 2 Acronyms and Abbreviations 3 INTRODUCTION 4 Gordonvale Fundraising Campaign 4 Location and Access 5 BIOREGIONAL AND LANDSCAPE CONTEXT 7 WORLD HERITAGE AREA STATUS 7 IUCN Protected Area Management Category 7 Legal Status and Compliance 8 NATURAL VALUES 9 GEO-CONSERVATION VALUES 12 WILDERNESS VALUES 12 INDIGENOUS VALUES 12 EUROPEAN HERITAGE 13 INVASIVE PESTS, WEEDS AND DISEASES 13 SCIENTIFIC STUDIES 13 MANAGEMENT STRATEGY 14 REFERENCES 15 APPENDIX A – Gordonvale ‘For Sale’ 16 APPENDIX B - Bushwalking tracks into Gordonvale 18 APPENDIX C - History of Ernie Bond at Gordonvale 21 1 Acknowledgements The Gordonvale World Heritage Area Reserve was secured by the Tasmanian Land Conservancy (TLC) in 2013 after a successful public fundraising campaign to purchase this private freehold block of land. -
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. -
Assessment of Juvenile Eel Resources in South Eastern Australia and Associated Development of Intensive Eel Farming for Local Production
ASSESSMENT OF JUVENILE EEL RESOURCES IN SOUTH EASTERN AUSTRALIA AND ASSOCIATED DEVELOPMENT OF INTENSIVE EEL FARMING FOR LOCAL PRODUCTION G J. Gooley, L. J. McKinnon, B. A. Ingram, B. Larkin, R.O. Collins and S.S. de Silva. Final Report FRDC Project No 94/067 FI SHERIE S RESEARCH & DEVELOPMENT Natural Resources CORPOR ATIO N and Environment AGRICULTURE RESOURCES COIISERVAT/Otl ASSESSMENT OF JUVENILE EEL RESOURCES IN SOUTH-EASTERN AUSTRALIA AND ASSOCIATED DEVELOPMENT OF INTENSIVE EEL FARMING FOR LOCAL PRODUCTION G.J Gooley, L.J. McKinnon, B.A. Ingram, B.J. Larkin, R.O. Collins and S.S. De Silva Final Report FRDC Project No 94/067 ISBN 0731143787 Marine and Freshwater Resources Institute, 1999. Copies of this document are available from: Marine and Freshwater Resources Institute Private Bag 20 Alexandra. VIC. 3714. AUSTRALIA.. This publication may be of assistance to you but the State of Victoria and its officers do not guarantee that the publication is without flaw of any kind or is wholly appropriate for your particular purposes and therefore disclaims all liability for error, loss or other consequence which may arise from you relying on any information in this publication. 1 TABLE OF CONTENTS 1 TABLE OF CONTENTS...............................................................................................................................i 2 ACKNOWLEDGMENTS.......................................................................................................................... iii 3 NON-TECHNICAL SUMMARY................................................................................................................! -
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. -
Coastal Erosion Reveals a Potentially Unique Oligocene and Possible Periglacial Sequence at Present-Day Sea Level in Port Davey, Remote South-West Tasmania
Papers and Proceedings of the Royal Society of Tasmania, Volume 148, 2014 43 COASTAL EROSION REVEALS A POTENTIALLY UNIQUE OLIGOCENE AND POSSIBLE PERIGLACIAL SEQUENCE AT PRESENT-DAY SEA LEVEL IN PORT DAVEY, REMOTE SOUTH-WEST TASMANIA by Mike Macphail, Chris Sharples, David Bowman, Sam Wood & Simon Haberle (with two text-figures, five plates and two tables) Macphail, M., Sharples, C., Bowman, D., Wood, S. & Haberle, S. 2014 (19:xii): Coastal erosion reveals a potentially unique Oligocene and possible periglacial sequence at present-day sea level in Port Davey, remote South-West Tasmania. Papers and Proceedings of the Royal Society of Tasmania 148: 43–59. https://doi.org/10.26749/rstpp.148.43 ISSN 0080-4703 Department of Archaeology & Natural History, College of Asia and the Pacific, Australian National University, Canberra, ACT 0200, Australia (MM*, SH); School of Geography & Environmental Studies, Faculty of Science, Engineering & Technology, University of Tasmania, Hobart 7001, Tasmania, Australia (CS); School of Biological Sciences, Faculty of Science, Engineering & Technology, University of Tasmania, Hobart 7001, Tasmania, Australia (DB, SW). *Author for correspondence. Email: [email protected] Cut-back of a sea-cliff at Hannant Inlet in remote South-West Tasmania has exposed Oligocene clays buried under Late Pleistocene “collu- vium” from which abundant wood fragments protrude. The two units are separated by a transitional interval defined by mixed Oligocene and Pleistocene microfloras. Microfloras preserved in situ in the clay provide a link between floras in Tasmania and other Southern Hemisphere landmasses following onset of major glaciation in East Antarctica during the Eocene-Oligocene transition (c. 34 Ma). -
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