Structore and Petrology of the Raglan Range
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TWWHA Walking Track Management Strategy 1994 Vol 1
Walking Track Management Strategy for the Tasmanian Wilderness World Heritage Area Volume I Main Report January 1994 1 Summary The Walking Track Management Strategy is a strategy developed by the Tasmanian Parks & Wildlife Service for the management of walking tracks and walkers in and adjacent to the Tasmanian Wilderness World Heritage Area (WHA), in accordance with the recommendations of the World Heritage Area Management Plan. Key management issues in the region include the extensive deterioration of existing walking tracks and the unplanned development of new walking tracks in many areas. Campsite impacts, crowding, pollution and broadscale trampling damage to vegetation and soils are also creating serious problems in some areas. The Strategy has been prepared on the basis of an extensive literature survey and an inventory of tracks and track conditions throughout the WHA. Research has also been undertaken to assess usage levels, usage trends and user attitudes and characteristics throughout the WHA. The three-volume document includes: • a summary of the findings of the literature survey (section 2 and appendix B); • a description of the method used to compile the inventory of tracks and track conditions, and a summary of the findings of the inventory (section 3); • a summary of available information on usage levels, usage trends, user characteristics and attitudes and social impacts throughout the WHA (section 4 and appendix C); • an assessment of the opportunity spectrum for bushwalking in and adjacent to the WHA (section 5 and appendix -
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 -
Explanatory Notes for the Time–Space Diagram and Stratotectonic Elements Map of Tasmania
Tasmanian Geological Survey TASMANIA DEVELOPMENT Record 1995/01 AND RESOURCES Tasgo NGMA Project Sub-Project 1: Geological Synthesis Explanatory notes for the Time–Space Diagram and Stratotectonic Elements Map of Tasmania by D. B. Seymour and C. R. Calver Tasmanian Geological Survey Record 1995/01 1 CONTENTS INTRODUCTION ..................................................................................................................... 4 KING ISLAND.......................................................................................................................... 5 ?Mesoproterozoic ............................................................................................................... 5 Neoproterozoic orogenesis and granitoid intrusive rocks ................................................ 5 ?Neoproterozoic sequences ................................................................................................ 5 Early Carboniferous granitoid intrusive rocks ................................................................ 6 ROCKY CAPE ELEMENT....................................................................................................... 7 ?Mesoproterozoic: Rocky Cape Group ............................................................................... 7 Burnie and Oonah Formations ........................................................................................ 7 Smithton Synclinorium .................................................................................................... 7 Ahrberg Group ................................................................................................................. -
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. -
TWWHA Wilderness Value Assessment 2015.Pdf
Tasmanian Wilderness World Heritage Area Assessment of Wilderness Value Stage 2: Entire TWWHA Martin Hawes & Roger Ling September 2015 TWWHA Wilderness Value Assessment Stage 2: Entire TWWHA Summary Two computer-based methodologies, the National Wilderness Inventory (NWI) methodology and a revised version of this, were used to assess wilderness value across the Tasmanian Wilderness World Heritage Area (TWWHA) and contiguous wild areas based on input geodata that was (mostly) current in 2015. The results were used to assess the current status of wilderness across the region and the changes in wilderness value relative to the results of similar studies undertaken in 1995 and 2005. The 2015 results were broadly similar to those obtained in 2005, although substantial losses due to post-2005 roading were observed in several areas, particularly the Counsel River area. Gains in wilderness value due to the closure, downgrading or revegetation of roads and vehicle tracks were observed in the area west of Macquarie Harbour, the middle Hansons River area and the area north of Victoria Pass. Numerous apparent changes (mainly losses) in wilderness value were observed due the inclusion in the 2015 data set of features such as residences and areas of disturbed land that were overlooked in the 2005 analysis. Comparison using the NWI methodology of current wilderness value with the results obtained in 1995 revealed numerous gains and losses, some of which had already been observed in 2005. Substantial gains in wilderness value, mostly due to the closure, downgrading or revegetation of roads and vehicle tracks, were observed in the area southwest of Macquarie Harbour, Moores Valley, Alma Valley, the northern half of the Jane River Track and Little Fisher Valley. -
Brand Voice, Marketing Framework, Key Audiences, Journeys & Messaging, Go-To-Market Strategy, Recommended Brand Activations
Work / Digital platform For The People x Snowy Valleys Marketing Strategy Brand voice, marketing framework, key audiences, journeys & messaging, go-to-market strategy, recommended brand activations, leveraging key events and partnerships, indicative marketing executions, implementation recommendations What’s inside Following this page, you’ll find a marketing strategy for driving visitation to the Snowy Valleys. This is not about simply planting the message: visit Snowy Valleys. It’s about defining the product that is the Snowy Valleys for and finding a market for it. The Snowy Valleys isn’t one singular experience or attraction that will draw visitors, but rather a combination of experiences across the region - so a key component of the strategy is how to package these experiences in a way that makes sense to outside visitors. Changing behaviour (driving visitation) is no small task, and this strategy won’t be successful unless this effort is bigger than individual businesses, and bigger than the council - a true partnership of community, council, and neighbouring regions. The destination brand strategy positioned the Snowy Valleys. This marketing framework about helping make decisions that allow council to facilitate and experiences that are quintessentially Snowy Valleys, guide visitors from one experience to another, and helping council and community reach the right people who’d be excited about the kind of experience the Snowy Valleys can offer. As a result of this positioning this document defines: who will we speak to, what touchpoints will we reach them on, and what will we say to them? • Key audiences, journeys and messages • Go-to-market strategy incorporating media mix — owned (website, signage, print etc) • Recommendations for brand and marketing activations • Recommendations for leveraging key events and partnerships Contents 1. -
Part-3---A-Review-Of-The-Geoconservation-Values-Of-The-Tasmanian-WWHA.Pdf
Recommendations and Issues Arising 4.0 RECOMMENDATIONS & ISSUES ARISING 4.1 Introduction This final section briefly draws out conclusions arising from the descriptions and discussions of the World Heritage geoconservation values of the TWWHA that have been provided in Section (3.0). In most cases, issues are only briefly highlighted or dot-pointed in this section, so as to provide a simple "check list" of key issues arising. Section (3.0) (and references therein) should be referred to for background details of the various issues and recommendations listed here. 4.2 Recommended Additions to the TWWHA Based on Geoconservation Values, and Areas for Further Consideration All of the 21 new reserves adjoining the TWWHA, as listed and described in Section (3.3) above, contain features or systems contributing substantially to one of more of the recognised TWWHA World Heritage geodiversity themes (see Section 3.3), and hence they are all recommended for inclusion in an extended Tasmanian Wilderness World Heritage Area (TWWHA) boundary on this basis. It is additionally recommended that the Hastings Caves State Reserve – which immediately adjoins the Hastings Cave reserve extension that is one of the 21 new reserves recommended for inclusion in the TWWHA - be also incorporated within the TWWHA boundary owing to its possession of dolomite karst systems that are physically continuous with, as well-developed, and more accessible than those contributing to the Karst World Heritage geoconservation themes within the existing (and now contiguous) Southwest National Park / TWWHA (see Section 3.4). Significantly, this proposal would also add an important ongoing hydrothermal karst system to the TWWHA (see Section 3.4), which is a karst process that is at present poorly represented within the TWWHA, yet is an important element of Tasmania's karst geodiversity. -
Forest to Fjaeldmark: Rainforest and Related Scrub
Edition 2 From Forest to Fjaeldmark The Vegetation Communities Rainforest and related scrub Eucryphia lucida Edition 2 From Forest to Fjaeldmark (revised – May 2018) 1 Rainforest and related scrub Community (Code) Page Athrotaxis cupressoides-Nothofagus gunnii short rainforest (RPF) 10 Athrotaxis cupressoides open woodland (RPW) 12 Athrotaxis cupressoides rainforest (RPP) 15 Athrotaxis selaginoides-Nothofagus gunnii short rainforest (RKF) 17 Athrotaxis selaginoides rainforest (RKP) 19 Athrotaxis selaginoides subalpine scrub (RKS) 21 Coastal rainforest (RCO) 23 Highland low rainforest and scrub (RSH) 25 Highland rainforest scrub with dead Athrotaxis selaginoides (RKX) 27 Lagarostrobos franklinii rainforest and scrub (RHP) 29 Nothofagus-Atherosperma rainforest (RMT) 31 Nothofagus-Leptospermum short rainforest (RML) 34 Nothofagus-Phyllocladus short rainforest (RMS) 36 Nothofagus gunnii rainforest scrub (RFS) 39 Nothofagus rainforest (undifferentiated) (RMU) 41 Rainforest fernland (RFE) 42 General description Diselma archeri and/or Pherosphaera hookeriana. These are mapped within the unit Highland This group comprises most Tasmanian vegetation coniferous shrubland (HCS), which is included within dominated by Tasmanian rainforest species (sensu the Highland treeless vegetation section. Jarman and Brown 1983) regardless of whether the dominant species are trees, shrubs or ferns. Rainforests and related scrub vegetation generally Tasmanian cool temperate rainforest has been occur in high rainfall areas of Tasmania that exceed defined floristically -
2531 WHA Man Folder Cover
Tasmanian Wilderness Tasmanian World Heritage Tasmanian Wilderness World Heritage Area MANAGEMENT PLAN 1999 Area Wilderness MANAGEMENT World Heritage PLAN 1999 Area “To identify, protect, conserve, present and, where appropriate, rehabilitate the world heritage and other natural and cultural values of the WHA, and to transmit that heritage to future generations in as good or better condition than at present.” WHA Management Plan, Overall Objective, 1999 MANAGEMENT PLAN PARKS PARKS and WILDLIFE and WILDLIFE SERVICE 1999 SERVICE ISBN 0 7246 2058 3 Tasmanian Wilderness World Heritage Area PARKS MANAGEMENT PLAN and WILDLIFE 1999 SERVICE TASMANIAN WILDERNESS WORLD HERITAGE AREA MANAGEMENT PLAN 1999 This management plan replaces the Tasmanian Abbreviations and General Terms Wilderness World Heritage Area Management The meanings of abbreviations and general terms Plan 1992, in accordance with Section 19(1) of the used throughout this plan are given below. National Parks and Wildlife Act 1970. A glossary of technical terms and phrases is The plan covers those parts of the Tasmanian provided on page 206. Wilderness World Heritage Area and 21 adjacent the Director areas (see table 2, page 15) reserved under the National Parks and Wildlife Act 1970 and has been The term ‘Director’ refers to the Director of prepared in accordance with the requirements of National Parks and Wildlife, a statutory position Part IV of that Act. held by the Director of the Parks and Wildlife Service. The draft of this plan (Tasmanian Wilderness World Heritage Area Management Plan 1997 the Minister Draft) was available for public comment from 14 The ‘Minister’ refers to the Minister administering November 1997 until 16 January 1998. -
West Coast Municipality Map.Pdf
CAMPBELL NeaseySTRAHAN • QUEENSTOWN • ZEEHAN • ROSEBERY • TULLAH12 Plains 10 THE RANGE 6 Blue Peak 18 4 16 5 Mt 4 DAZZLER Hill 17 Duncan 10 3 5 17 16 12 Ri 13 ver 9 14 7 EUGENANA ARLETONT LATROBE Rive SOUT H River SPALFORD TAS HARFORD River 14 UPPER KINDREDMELROSE Horton R River RIANA 19 5 Guide NATONE River 45 HAMPSHIRE PALOONA ons GUNNS y SPRENT L BALFOUR R AUS 13PLAINS Rubicon Mt Balfour PRESTON 9 LOWER SASSAFRAS Mt CASTRA Mersey R 27 Mt Bertha Emu HEKA BARRINGTON Frankland r ARRINGAW Blythe River WESTKeith COAST Lake 22 17 13 River Paloona n Do Arthu River NOOK R Lindsay THE OFFICIAL iver 49 1106 ST VALENTINES PK River NIETTA SHEFFIELD Mt Hazelton GUIDEDeep TO GETTING CreeLOSTk WILMO T WEST SUNNYSIDE 5 Gully KENTISH PARKHAM Dempster SOUTH LAKE River Leven ROLAND River 78 Savage BARRINGTON 21 Ck NIETTA LOWER Pedder TOWN MAPS GUILDFORD DININGCLAUDEROAD BEULAH Mt Bischoff River Talbots 7 Mt Cleveland WARATAH 1339 BLACK BLUFF STAVERTON13 Lagoon River Lake C157 MOLTEMA 759 Mt Norfolk ATTRACTIONS zlewood 856 ACCOMMODATION1231 MT ROLAND Gairdner CETHANA ELIZABETH C136 GOWRIE PARK ARTHUR PIEMAN Hea 11 TOWN Mt Vero WALKS B23 43 MOINA SHOPS WEEGENA Mt Pearce Mt Claude r C138 CONSERVATION AREA e 1001 W 10 y a w Med v i 16 Mt Cattley River 13River DUNORLAN R River Mersey 19 LEMANA SAVAGE Lake 30 C137 RED HILLS r Rive Lea Iris LAKE River 26 LORINNA RIVER CETHANA LIENA KING 11 River River Middlesex NEEDLES C132 SOLOMONS 4 MOLE STANLEY BURNIE Plains C139 Interview CAVE MAYBERRY C169 Coldstream River Mt Meredith River Que River CREEK R C249 26 River -
The Geology of the West Coast Range of Tasmania
PAPERS AND PROCE'EDINGS OF THE ROYAL SOCIETY 01'''' TASMANIA, VOLUME 88 The Geology of the West Coast Range of Tasmania PART I: STRATIGRAPHY AND METASOMATISM By J. BRADLEY SenioT LedllTer "in Geology at Victoria Unive?"'sity College, FVellington, N.Z. (WITH 4 TEXT FIGURES AND 9 PLATES) ABSTRACT The 'Vest Coast Range is a monadnock mountain chain of Tremadocian and older rocks. The Tremadoc strata were fault angle conglomerates which were crushed in Devonian times between a Cambrian geanticline and the Precambrian core of Tasmania. Cambrian rocks are of spilitic lavas and macigno facies greywackes. The Tremadocian strata are of Flysch and Molasse-like facies. Devonian movement was largely on tbe line of upthrust of the Cambrian geanticline and aiong thIs same line intense metasomatic metanlOrphism dosely followed the Devonian orogeny. The juxtaposition of contemporaneous and later faulting with metamorphislP and volcanic sedimentary and metamorphic breccias, provides interest. The two most interesting problems concern metamorphic contacts which resemble unconformities, and the tectonic history of the area. The phenomena observed ean be welded into a eonsecutive story which is thought to be of world-wide application. INTRODUCTION This study is part of a wider programme of investigation into the mineral bearing region of Western Tasmania. The work, under the aegis of the University of Tasmania, has already resulted in descriptions of the stratigraphy and palaeontology of the Siluro-Devonian strata of the Zeehan district, by Gill and Banks (1950). The Ordovician strata form the subject of another study; this article is concerned with the rocks and structures of the West Coast Range; with rocks which are in general of Cambrian age, unfossiliferous, metamorphosed, and cast in complex forms. -
Picturesque Atlas of Australasia Maps
A-Signal Battery. I-Workshops. B-Observatory . K-Government House. C-Hospital. L-Palmer's Farm. .__4 S URVEY D-Prison. M-Officers ' Quarters. of E-Barracks . N-Magazine. F-Store Houses. 0-Gallows. THE SET TLEMENT ;n i Vh u/ ,S OUTN ALES G-Marine Barracks . P-Brick-kilns. H-Prisoners ' Huts. Q-Brickfields. LW OLLANI) iz /` 5Mile t4 2 d2 36 Engraved by A.Dulon 4 L.Poates • 1FTTh T i1111Tm»iTIT1 149 .Bogga 1 a 151 Bengalla • . l v' r-- Cootamundra Coola i r A aloe a 11lichellago 4 I A.J. SCALLY DEL. , it 153 'Greggreg ll tai III IJL. INDEX TO GENERAL MAP OF NE W SOUTH W ALES . NOTE -The letters after the names correspond with those in the borders of the map, and indicate the square in which the name will be found. Abercrombie River . Billagoe Mountain Bundella . J d Conjurong Lake . Dromedary Mountain. Aberdeen . Binalong . Bunda Lake C d Coogee . Drummond Mountain. Aberfoyle River . Binda . Bundarra . L c Cook (county) . Dry Bogan (creek) Acacia Creek . Bingera . Bunganbil Hill G g Coolabah . Dry Lake . Acres Billabong . Binyah . Bungarry Lake . E g Coolaburrag u ndy River Dry Lake Adelong Bird Island Bungendore J h Coolac Dry Lake Beds . Adelong Middle . Birie River Bungle Gully I c Coolah . Dry River . Ailsa . Bishop 's Bridge . Bungonia . J g Coolaman . Dubbo Creek Albemarle Black Head Bunker 's Creek . D d Coolbaggie Creek Dubbo Albert Lake . Blackheath Bunna Bunna Creek J b Cooleba Creek Duck Creek Albury . Black Point Bunyan J i Cooma Dudanman Hill . Alice Black Swamp Burbar Creek G b Coomba Lake Dudley (county) .