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To Arthur River To Moina To Sheffield (7km); (75km) Burnie A10 Devonport (38km) (50km) Arthur Pieman C123 Deloraine Conservation B12 Area r River e C249 te Mole Creek A5 y River Riv C247 h Cradle Karst National ld ey W Valley Park Corinna atfie Lake Pieman H Mackintosh Cradle Mers River Lake Mountain State Reserve Reece C252 Rosebery (1545m) Tullah Dam Lake Bastyan The Overland Pieman Dam Mt Farrell Lake Rosebery Breona Montezuma Murchison Rowallan Mt Jerusalem C249 Falls Mt Murchison Dam (1458m) (1275m) Lake Renison Bell Murchison Williamsford Great Granville Lake Harbour Lake Johnston Track Nature Reserve Cradle Mountain– Mt Ossa Zeehan B28 (1617m) Lake St Clair Walls of Jerusalem Trial C248 National Park Harbour Mt e National Park g Zeehan River n a R Eildon Peak Central (1439m) B27 t Plateau Miena s Henty Conservation a o Area Henty T ully Queenstown C Nelson Mt Olympus Dunes Falls (1449m) River t B24 s e Derwent A10 Bridge The Wall Ocean y W Macquarie Strahan Crotty In The Heads Beach Lake Hw Dam Lake Wilderness (Hells Gates) er Burbury Echo Lyell Riv Donaghy's West Coast Cape Sorell Hill Lake King Wilderness King Railway King Teepookana William Forest Macquarie Mt King Mt Sorell Frenchmans Cap Wi (1443m) William III Sloop Point (1144m) ll (1359m) R Tarraleah Harbour ia iver Sarah m Island Derwent Franklin R a River Franklin-Gordon nge iver A10 Heritage Wild Rivers R Landing National Park n o Birthday is Bay Birchs Kutikina Den Inlet Gordon Cave River s D'Aguilar le Range Sir John a The Lake C608 Hibbs Bay Falls W e Pleiades Gordon f g o n a Florentine e Mt Field c R Valley n National Westerway i r Park P Gordon Giants' Table Dam Lake & Cottages To Hobart Gordon (59km) Olga Strathgordon Serpentine B61 Maydena Dam Teds Wedge River Beach Nature Mt Sprent Trail Frodshams (1058m) Pass Styx & the Upper Mt Wedge Creepy Crawly Florentine Valleys Lake (1145m) Nature Trail F C607 Mt Anne r Mt an (1425m) k Solitary Mt W la Pedder eld nd Eliza Lake R Riv ang Scotts Judd er Elliot e Peak Low Rocky Bay Edgar Mt Weld Point Camping (1338m) Tahune Huon Forest Ground Reserve River Camping Scotts Ground Peak Dam Elliot Point To Geeveston A Art r hu ck (4km) th r Tra Davey u P r R lains ange S O U T H E R N Hartz Port Federation Peak Mountains O C E A N (1224m) National Payne Park Bay Southwest D a National Park Adamson v Port e Peak y Point Davey Bathurst (1226m) S Track Harbour St Vincent o u t h Hilliard w Head e Melaleuca s Precipitous Bluff 0 20 km t South (1120m) Mt La 0 10 miles C a p Coast Perouse e New (1157m) R Track a River Pindars n g Cox Lagoon Peak e Bight Prion Cox Bay Southwest Cape Bluff De Witt Island.

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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.
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Macquarie Harbour
Tasmanian West Coast Foray Part 1 Macquarie Harbour 100nm. Add another 22 when your Gale force winds, driving rain, cold temperatures, a small starting point is at Three Hummock Island. So one or even two stops can sprinkling of sunny days, and all this in late summer… Any be made along the way. takers for a foray down the West Coast of Tasmania? This is We studied two anchorage guides where CHRISTINE DANGER is sailing us over two issues. which are our bibles: Cruising Tasmania by J Brettingham-Moore, and Tasmanian Anchorage Guide published by the Royal Yacht Club of oming down the west coast, Our expedition started from So over two articles, we will share Tasmania. We talked to Tasmanian even during the so-called Melbourne in late February. We with you the sites we visited and friends who know the area well and C best season, is not for the sailed west to Apollo Bay, then south impressions we formed. The first picked the brains of cray fishermen to faint hearted. It is committal, it is to King Island and the Hunter Group, focuses on Macquarie Harbour, the find out about anchorages they use The coast is quite scenic: a mix of TOP: Strahan with its old buildings challenging, but when it all goes and there we waited for the right second on Port Davey. along the coast. There is a wealth of scrub, sand dunes, rocky outcrops … a welcome sight after many smoothly on a well-equipped boat, conditions to start our descent. It did knowledge out there and people are hours at sea.
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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,
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Western Explorer
Travelling times and distances, based on safe speed and good road conditions Due to the remote and rugged Experience Tasmania’s Smithton – Marrawah: terrain of this region, some unique western wilderness roads are narrow and winding. 45 minutes / 49 km / 90 kmh / sealed The Western Explorer route links Stanley in the North West WESTERN Marrawah – Arthur River: Many of these roads are to Strahan on the West Coast and takes you through some 10 minutes / 12 km / 80 kmh / sealed unsealed and therefore of the State’s most beautiful and isolated areas. susceptible to the varying EXPLORER Road travellers can expect a unique experience, exploring Arthur River – Couta Rocks: weather conditions. 20 minutes / 18 km / 70 kmh / unsealed a region steeped in early mining history, surrounded by wilderness and remarkable scenery. The landscape is wild Couta Rocks – Blackwater Road: West Coast Wilderness Drive Smithton to Strahan and rugged with a climate that can vary from snow to 15 minutes / 16km / 70 kmh / unsealed brilliant sunshine in one day. Blackwater Road – Lindsay River: During wet weather, roads This guide provides you with valuable information about 20 minutes / 21 km / 70 kmh / unsealed can become slippery, flooded or potholed. Unsealed roads the road conditions between Stanley and Strahan, however Lindsay River – Corinna: can become extremely dusty be prepared: If you break down, the roads are isolated and 90 minutes / 57 km / 40 kmh / unsealed during dry periods. you may experience a long delay before another traveller or assistance comes. Arthur River – Corinna: For your safety and comfort 2 hrs 15 minutes. it is wise to check road and Arthur River – Zeehan: weather conditions before 3 hrs 15 minutes.
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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].
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A Review of Geoconservation Values
Geoconservation Values of the TWWHA and Adjacent Areas 3.0 GEOCONSERVATION AND GEOHERITAGE VALUES OF THE TWWHA AND ADJACENT AREAS 3.1 Introduction This section provides an assessment of the geoconservation (geoheritage) values of the TWWHA, with particular emphasis on the identification of geoconservation values of World Heritage significance. This assessment is based on: • a review (Section 2.3.2) of the geoconservation values cited in the 1989 TWWHA nomination (DASETT 1989); • a review of relevant new scientific data that has become available since 1989 (Section 2.4); and: • the use of contemporary procedures for rigorous justification of geoconservation significance (see Section 2.2) in terms of the updated World Heritage Criteria (UNESCO 1999; see this report Section 2.3.3). In general, this review indicates that the major geoconservation World Heritage values of the TWWHA identified in 1989 are robust and remain valid. However, only a handful of individual sites or features in the TWWHA are considered to have World Heritage value in their own right, as physical features considered in isolation (eg, Exit Cave). In general it is the diversity, extent and inter-relationships between numerous features, sites, areas or processes that gives World Heritage significance to certain geoheritage “themes” in the TWWHA (eg, the "Ongoing Natural Geomorphic and Soil Process Systems" and “Late Cainozoic "Ice Ages" and Climate Change Record” themes). This "wholistic" principle under-pinned the 1989 TWWHA nomination (DASETT 1989, p. 27; see this report Section 2.3.2), and is strongly supported by the present review (see discussion and justification of this principle in Section 2.2).
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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).
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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.
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Reimagining the Visitor Experience of Tasmania's Wilderness World
Reimagining the Visitor Experience of Tasmania’s Wilderness World Heritage Area Ecotourism Investment Profile Reimagining the Visitor Experience of Tasmania’s Wilderness World Heritage Area: Ecotourism Investment Profile This report was commissioned by Tourism Industry Council Tasmania and the Cradle Coast Authority, in partnership with the Tasmanian Government through Tourism Tasmania and the Tasmanian Parks and Wildlife Service. This report is co-funded by the Australian Government under the Tourism Industry Regional Development Fund Grants Programme. This report has been prepared by EC3 Global, TRC Tourism and Tourism Industry Council Tasmania. Date prepared: June 2014 Design by Halibut Creative Collective. Disclaimer The information and recommendations provided in this report are made on the basis of information available at the time of preparation. While all care has been taken to check and validate material presented in this report, independent research should be undertaken before any action or decision is taken on the basis of material contained in this report. This report does not seek to provide any assurance of project viability and EC3 Global, TRC Tourism and Tourism Industry Council Tasmania accept no liability for decisions made or the information provided in this report. Cover photo: Huon Pine Walk Corinna The Tarkine - Rob Burnett & Tourism Tasmania Contents Background...............................................................2 Reimagining the Visitor Experience of the TWWHA .................................................................5
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Walking Track List - PWS Class Wl to T4
PWS Commercial Visitor Services - Walking Track List - PWS class Wl to T4 Track Name FieldCentre PWS class AS2156 Length - Kms and Days PWS Management Region: Southern PWS Track Class: VV1 Overview: Wheelchair Standard Nature Trail Hastings Platypus Track Huonville W1 Class 1 0.290 less than 2 hrs Hastings Pool access track Huonville W1 Class 1 0.077 less than 2 hrs Mount Nelson Signal Station Tracks Derwent W1 Class 1 0.059 less than 2 hrs Russell Falls Nature Walk Mount Field W1 Class 1 0.649 less than 2 hrs PWS Management Region: Southern PWS Track Class: W2 Overview: Standard Nature Trail Arve Falls Huonville W2 Class 2 0.614 less than 2 hrs Blowhole circuit Tasman W2 Class 2 0.248 less than 2 hrs Cape Bruny lighthouse Bruny Island W2 Class 2 0.252 less than 2 hrs Cape Deslacs Seven Mile Beach W2 Class 2 0.154 less than 2 hrs Cape Deslacs Beach Seven Mile Beach W2 Class 2 0.345 less than 2 hrs Coal Point Bruny Island W2 Class 2 0.124 less than 2 hrs Creepy Crawly NT Mount Field W2 Class 2 0.175 less than 2 hrs Crowther Point Track Huonville W2 Class 2 0.248 less than 2 hrs Garden Point to Carnarvon Bay Tasman W2 Class 2 3.138 less than 2 hrs Gordons Hill fitness track Seven Mile Beach W2 Class 2 1.331 less than 2 hrs Hot Springs NT Huonville W2 Class 2 0.839 less than 2 hrs Kingston Heights Derwent W2 Class 2 0.344 less than 2 hrs Lake Osbome Huonville W2 Class 2 1.042 less than 2 hrs Maingon Bay lookout Tasman W2 Class 2 0.044 less than 2 hrs Needwonnee Walk Huonville W2 Class 2 1.324 less than 2 hrs Newdegate Cave - Main access
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Recent Wildfires in the Tasmanian Wilderness
Recent wildfires in the Tasmanian Wilderness The 2016 and 2019 Tasmanian wildfires burnt upwind of the most important Gondwanan refuges that remain - Mt Anne, Mt Bobs, Federation Peak and the Eastern Arthurs, New River headwaters, the Du Cane Range, the Walls of Jerusalem, Mt Read, the Tyndall Range, the lower Gordon River and the entire Tarkine rainforest (Huskisson River in the south and the Rapid River in the north). Aerial documentation of the south-eastern part of the Tasmanian Wilderness World Heritage Area (TWWHA) in March 2019 shows that fire damage to sensitive vegetation, although not wholly catastrophic, was extensive and locally extremely severe. For many areas the consequences will be permanent. A small selection of images from the flight is included below. Of even greater concern than the damage done, however, was that, with uncontrolled fire widespread through the landscape in 2016 and 2019, a brief period of severe or catastrophic fire conditions would have obliterated Tasmania’s most important stands of Gondwanic vegetation. In hot, dry, windy conditions rainforest does burn – the Southern Ranges, Mt Picton, the Raglan Range, Frenchmans Cap, Mt Murchison, Algonkian Mountain, the upper Jane River, the Meredith Range and many other places bear grim testament to that. The effects of climate change, combined with the absence of an effective means of immediately suppressing remote wildfires, pose a catastrophic threat to irreplaceable Gondwanan flora. This vegetation forms a major component of the Outstanding Universal Value of the TWWHA. Important tracts of these ancient life forms also occur outside the TWWHA. Climate change is creating unprecedented levels of dry-lightning strikes and resultant wildfires in the Tasmanian wilderness.
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A Review of Geology and Exploration in the Macquarie Harbour–Elliott Bay Area, South West Tasmania
Mineral Resources Tasmania Tasmanian Geological Survey Tasmania DEPARTMENT of INFRASTRUCTURE, Record 2003/04 ENERGY and RESOURCES Western Tasmanian Regional Minerals Program Mount Read Volcanics Compilation A review of geology and exploration in the Macquarie Harbour–Elliott Bay area, South West Tasmania K. D. Corbett Contents Summary ………………………………………………………………………………… 2 Introduction ……………………………………………………………………………… 3 Scope of study ………………………………………………………………………… 3 Conditions related to working in South West Tasmania …………………………………… 3 Acknowledgements …………………………………………………………………… 4 Major elements of the geology …………………………………………………………… 5 Introduction …………………………………………………………………………… 5 Mesoproterozoic Rocky Cape Group on Cape Sorell ……………………………………… 5 Neoproterozoic rift-related sequences of central Cape Sorell peninsula area ………………… 5 Early Cambrian allochthonous sequences ………………………………………………… 6 Middle Cambrian post-collisional sequences ……………………………………………… 7 Sequences present and their correlation …………………………………………………… 7 Eastern Quartz-Phyric Sequence correlate (Lewis River Volcanics) …………………………… 8 Western Volcano-Sedimentary Sequence (‘Wart Hill Pyroclastics’) …………………………… 8 Andesite-bearing volcano-sedimentary sequences—Noddy Creek Volcanics ………………… 8 Late Cambrian to Ordovician Owen Group and Gordon Group rocks ……………………… 10 Permo-Carboniferous and Jurassic rocks ………………………………………………… 12 Tertiary sedimentary rocks ……………………………………………………………… 12 Outline of proposed tectonic–depositional history ………………………………………… 13 Notes on aeromagnetic features from the WTRMP
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