MOLE CREEK and GUNNS PLAINS HAPPENINGS - Cathie Plowman
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6. Annual Review and Significant Events
6. Annual Review and Significant Events January-April: wet in the tropics and WA, very hot in central to eastern Australia For northern Australia, the tropical wet season (October 2005 – April 2006) was the fifth wettest on record, with an average of 674 mm falling over the period. The monsoon trough was somewhat late in arriving over the Top End (mid-January as opposed to the average of late December), but once it had become established, widespread heavy rain featured for the next four months, except over the NT and Queensland in February. One particularly noteworthy event occurred towards the end of January when an intense low (central pressure near 990 hPa) on the monsoon trough, drifted slowly westward across the central NT generating large quantities of rain. A two-day deluge of 482 mm fell at Supplejack in the Tanami Desert (NT), resulting in major flooding over the Victoria River catchment. A large part of the central NT had its wettest January on record. Widespread areas of above average rain in WA were mainly due to the passages of several decaying tropical cyclones, and to a lesser extent southward incursions of tropical moisture interacting with mid-latitude systems. Severe tropical cyclone Clare crossed the Pilbara coast on 9t h January and then moved on a southerly track across the western fringes of WA as a rain depression. Significant flooding occurred around Lake Grace where 226 mm of rain fell in a 24-hour period from 12 t h to 13 t h January. Tropical cyclone Emma crossed the Pilbara coast on 28 th February and moved on a southerly track; very heavy rain fell in the headwaters of the Murchison River on 1s t March causing this river’s highest flood on record. -
Edition 2 from Forest to Fjaeldmark the Vegetation Communities Highland Treeless Vegetation
Edition 2 From Forest to Fjaeldmark The Vegetation Communities Highland treeless vegetation Richea scoparia Edition 2 From Forest to Fjaeldmark 1 Highland treeless vegetation Community (Code) Page Alpine coniferous heathland (HCH) 4 Cushion moorland (HCM) 6 Eastern alpine heathland (HHE) 8 Eastern alpine sedgeland (HSE) 10 Eastern alpine vegetation (undifferentiated) (HUE) 12 Western alpine heathland (HHW) 13 Western alpine sedgeland/herbland (HSW) 15 General description Rainforest and related scrub, Dry eucalypt forest and woodland, Scrub, heathland and coastal complexes. Highland treeless vegetation communities occur Likewise, some non-forest communities with wide within the alpine zone where the growth of trees is environmental amplitudes, such as wetlands, may be impeded by climatic factors. The altitude above found in alpine areas. which trees cannot survive varies between approximately 700 m in the south-west to over The boundaries between alpine vegetation communities are usually well defined, but 1 400 m in the north-east highlands; its exact location depends on a number of factors. In many communities may occur in a tight mosaic. In these parts of Tasmania the boundary is not well defined. situations, mapping community boundaries at Sometimes tree lines are inverted due to exposure 1:25 000 may not be feasible. This is particularly the or frost hollows. problem in the eastern highlands; the class Eastern alpine vegetation (undifferentiated) (HUE) is used in There are seven specific highland heathland, those areas where remote sensing does not provide sedgeland and moorland mapping communities, sufficient resolution. including one undifferentiated class. Other highland treeless vegetation such as grasslands, herbfields, A minor revision in 2017 added information on the grassy sedgelands and wetlands are described in occurrence of peatland pool complexes, and other sections. -
Description Distribution and Habitat Mole Creek Cave Beetle
THREATENED SPECIES LISTING STATEMENT Mole Creek Cave Beetle, Tasmanotrechus cockerilli Moore 1972 Status Commonwealth Environment Protection and Biodiversity Conservation Act 1999.............................…...........…………………………………....Not listed Tasmanian Threatened Species Protection Act 1995…………………....Rare Description The Mole Creek cave beetle is found only in caves; Tasmanotrechus cockerilli such species are referred to as ‘troglobites’. Troglobitic beetles show varying degrees of adaptation to a cave existence, including loss of body colouring, a reduction or complete loss of eyes, and a lengthening of legs and other appendages. The Mole Creek cave beetle is small (body length approximately 6 mm), with an elongated head and vestigial eyes. For a full description refer to Moore (1972). Distribution and Habitat Tasmanotrechus cockerilli is known only from the 5mm Mole Creek karst system in central north Tasmania. Within this cave system it is fairly widely distributed, Illustration: Karen Richards having so far been located in nine caves, however, the species is extremely rare in the caves where it has been found (Eberhard et al. 1991). A number of specimens of a beetle very similar to the Mole Creek cave beetle were also collected by Eberhard (2000) from six new cave sites within the Mole Creek karst system. These have been tentatively assigned to the same species. However, the specimens have yet to be formally identified as belonging to the species T. cockerilli. The species is confined mostly to the deep cave zone, where it is found under stones, in or near flood litter, and on moist surfaces near water. Occasionally the species has also been found some distance from permanent water. -
Derwent Catchment Review
Derwent Catchment Review PART 1 Introduction and Background Prepared for Derwent Catchment Review Steering Committee June, 2011 By Ruth Eriksen, Lois Koehnken, Alistair Brooks and Daniel Ray Table of Contents 1 Introduction ..........................................................................................................................................1 1.1 Project Scope and Need....................................................................................................1 2 Physical setting......................................................................................................................................1 2.1 Catchment description......................................................................................................2 2.2 Geology and Geomorphology ...........................................................................................5 2.3 Rainfall and climate...........................................................................................................9 2.3.1 Current climate ............................................................................................................9 2.3.2 Future climate............................................................................................................10 2.4 Vegetation patterns ........................................................................................................12 2.5 River hydrology ...............................................................................................................12 2.5.1 -
1 Deborah Hunter President, Friends of Great Western Tiers Kooparoona Niara Conservation Officer, Mole Creek Caving Club. Corres
Deborah Hunter President, Friends of Great Western Tiers Kooparoona Niara Conservation Officer, Mole Creek Caving Club. Correspondence: Submission for the Senate inquiry 15th April 2016 The response to, and lessons learnt from, recent fires in remote Tasmanian wilderness affecting the Tasmanian Wilderness World Heritage Area, with particular reference to: a. the impact of global warming on fire frequency and magnitude; b. the availability and provisions of financial, human and mechanical resources; c. the adequacy of fire assessment and modelling capacity; d. Australia’s obligations as State Party to the World Heritage Convention; e. world best practice in remote area fire management; and f. any related matter. 1 Preamble This submission concerns the fire known as the Lake Mackenzie, Tasmanian Fire Service (TFS) incident number 236227. It later became known as the Mersey Forest complex of fires. We welcome any opportunity to make further representation should there be hearings into the fires. The catastrophic losses incurred elsewhere in the Tasmanian Wilderness World Heritage Area (TWWHA) and high conservation value areas of recognised World Heritage status, 1 such as the Tarkine forests (takayna) are acknowledged but are beyond the scope of this submission. In making this submission, we express the greatest respect for all personnel involved in the dangerous and protracted effort to control and contain the fires. We make this submission in the spirit of helping to understand, address and prevent such devastation in the future. The first Tasmanians are respectfully acknowledged as traditional owners of this land, as is the name kooparoona niara. 2 Summary It is submitted that • Research on climate change and fire response must be restored and increased including CSIRO. -
Liawenee Flume Project
Liawenee Flume Project of consumables by boat over 12,000 miles from Barnsley in the United Kingdom to Hobart. On arrival in Hobart, we were met by Hydro Tasmania repre- sentative Norm Cribbin, whose help, local knowledge and sup- port were to prove invaluable, plus he carried the snakebite kits! Also there were representatives of JDP Coatings, a potential new installer for Australia. We hired a small truck and a large station Liawenee flume is situated high in the mountains north of Ho- wagon, loaded up and set off up the mountain. bart, capital city of Tasmania, an island 180 miles south of Aus- At site we unloaded the preparation equipment and set about tralia. Hobart is Australia’s second oldest and southernmost city, removing the moss, growths and unsound areas from the sur- next stop Antarctica. face with a high-pressure jet washer and in more difficult areas Fernco Environmental Ltd. is an U.K. company that markets a with a pneumatic scabbler. For the next stage we sprayed the unique range of products targeted at the preservation, conserva- whole area to be coated with a dilute bleach as a mild biocide tion, harvesting and recycling of water assets. We presented Fernco Ultracoat, an epoxy coating system de- The challenges were a remote site, no facilities veloped by Warren Environmental, to Tasmania Hydro, highlight- whatsoever, in a national park, an area of conservation, ing its special qualities as a no VOCs, high build in one coat, conditions varied from freezing to +20 degrees Celsius. structurally reinforcing and rapidly applied epoxy coating system with over 15 years of successful in ground history. -
Listing Statement
THREATENED SPECIES LISTING STATEMENT ORCHID L iawenee greenhood Pterostylis pratensis D. L. Jones 1998 Status Tasmanian Threatened Species Protection Act 1995 ……………………………….……..………..………………..vulnerable Commonwealth Environment Protection and Biodiversity Conservation Act 1999 ……………………..….….…...............Vulnerable Hans & Annie Wapstra Description December. In flower, the plants are 7 to 15 cm tall, Pterostylis pratensis belongs to a group of orchids with many closely sheathing stem leaves. They commonly known as greenhoods because the dorsal have 2 to 12 densely crowded white flowers with sepal and petals are united to form a predominantly dark green stripes. The hood apex curves down green, hood-like structure that dominates the abruptly and terminates with a short tip. The two flower. When triggered by touch, the labellum flips lateral sepals hang down and are fused to form a inwards towards the column, trapping any insect pouch below the labellum though the tips may inside the flower, thereby aiding pollination as the remain free. The labellum, which also hangs down, insect struggles to escape. Greenhoods are is whitish green, oblong with a shallowly notched deciduous terrestrials that have fleshy tubers, which tip and has an appendage that points out with a dark are replaced annually. At some stage in their life green, knob-like apex with a short, broad, blunt cycle all greenhoods produce a rosette of leaves. beak about 0.5 mm long. In all, the flowers are 7 to 8.5 mm long and 4.5 mm wide. The rosette of Pterostylis pratensis encircles the base of the flower stem. The 4 to 8 rosette leaves Its darker green and white flowers and larger leaves are dark green, crowded, and oval to circular can distinguish Pterostylis pratensis, which grows shaped with the broadest part in the middle, 25 to in montane and subalpine regions on the Central 35 mm long and 14 to 22 mm wide. -
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, -
GREAT WESTERN TIERS and MEANDER VALLEY Destination Action Plan 2017-2020 June 2017 Acknowledgments
GREAT WESTERN TIERS AND MEANDER VALLEY Destination Action Plan 2017-2020 June 2017 Acknowledgments The development of the Great Western Tiers and Meander Valley Destination Plan has been facilitated by Tourism Northern Tasmania with the support of the Department of State Growth. The process brought together representatives from all stakeholder groups that benefit from the visitor economy; local government, state government agencies, industry and the community, to develop a plan. This Plan seeks to identify the challenges and opportunities facing the Great Western Tiers and Meander Valley – and to establish achievable affordable priorities that if delivered would increase the competiveness of the destination. Facilitator Chris Griffin, CEO, Tourism Northern Tasmania Coordinator Gillian Miles, Industry Liaison, Tourism Northern Tasmania Destination Action Plan Leadership Group Lindi Dornauf Frank Horton Hayden Stedman Christmas Hills Raspberry Farm Kooparoona Niara Cultural Trail Parks & Wildlife Service Jonathon Harmey Androo Kelly Maria Tassone Meander Valley Council Trowunna Wildlife Park Arcoona Mark Flanigan Mick Kelly John Temple Empire Hotel MVC Councillor MVC Councillor Michal Frydrych Toni & Rob Mehigan Berice Van Der Aa Springfield Deer Farm Mole Creek Guest House Trade Training Centre Alfred Franssen Rosemary Norwood Deb White Seppenfelts Emporium Forest Walks Lodge MVC Councillor Barbara Harvey Roger Nutting Deb Willis Deloraine Deli Mountain Huts Preservation Society Deloraine Jewellers Martin Hay Vicki Pryer Kooparoona Niara Cultural Trail Visitor Information Centre Ben Harker Ross Quick Field Rabbit Mole Creek Progress Association Images used within this document are courtesy of Tourism Tasmania, Queen Victoria Museum and Art Gallery, Kathryn Leahy, Rob Burnett, Pete Mattila, Geoffrey Lea, N.R. Goldsmith, Knox Photographic Society, Lap Fung Lam, Chris Crerar, Masaaki Aihara, Meander Valley Council, Brian Dullaghan, Paul Flood, Joe Shemesh. -
399 a ABC Range 269-72 Aboriginal Peoples
© Lonely Planet Publications 399 Index A animals 27-30, see also individual Hazards Beach 244 ABCABBREVIATIONS Range 269-72 animals Injidup Beach 283 AboriginalACT peoplesAustralian Capital Arenge Bluff 325 Jan Juc beach 141 Territory Adnyamathana 267 Aroona Homestead 270 Kilcarnup Beach 286 NSW New South Wales Brataualung 175 Aroona Hut 270 Le Grand Beach 302 NT Northern Territory Daruk 65 Aroona Valley 270 Lion’s Head Beach 131 Qld Queensland Dharawal 58 Arthur’s Seat 133 Little Beach 58 SA South Australia Djab wurrung 150 ATMs 367 Little Marley Beach 59 Tas Tasmania INDEX Gamilaroi 110 Augusta 281 Little Oberon Bay 180 Vic Victoria Jandwardjali 150 Australian Alps Walking Track 157, 157 Marley Beach 59 WA Western Australia Krautungulung 181 Australian Capital Territory 84 Milanesia Beach 146 Malyankapa 123 Needles Beach 131 Pandjikali 123 B Norman Beach 180 Port Davey 236 B&Bs 358 Oberon Bay 180 Wailwan 110 Babinda 356 Osmiridium Beach 241 Western Arrernte 321 backpacks 393 Peaceful Bay 291-2, 296 Acacia Flat 73 Badjala Sandblow 347 Picnic Bay 179 accidents 385-6 Bahnamboola Falls 340 Prion Beach 240, 241 accommodation 357-60 Bald Head 302 Putty Beach 55-8 Acropolis, the 228 Baldry Crossing 133 Quininup Beach 284, 44 Adaminaby 95 Balor Hut 113 Redgate Beach 287 Adelaide 251-3 Banksia Bay 351 Safety Beach 132 Admiration Point 101 Banksia Creek 351 Seal Cove 186 Aeroplane Hill 118 banksias 45 Sealers Cove 178 agriculture 46 Bare Knoll 203-4 Secret Beach 186 air travel 372-5 Barn Bluff 220, 222 Smiths Beach 283 airports 372-3 Barrington -
Australian Orchidaceae: Genera and Species (12/1/2004)
AUSTRALIAN ORCHID NAME INDEX (21/1/2008) by Mark A. Clements Centre for Plant Biodiversity Research/Australian National Herbarium GPO Box 1600 Canberra ACT 2601 Australia Corresponding author: [email protected] INTRODUCTION The Australian Orchid Name Index (AONI) provides the currently accepted scientific names, together with their synonyms, of all Australian orchids including those in external territories. The appropriate scientific name for each orchid taxon is based on data published in the scientific or historical literature, and/or from study of the relevant type specimens or illustrations and study of taxa as herbarium specimens, in the field or in the living state. Structure of the index: Genera and species are listed alphabetically. Accepted names for taxa are in bold, followed by the author(s), place and date of publication, details of the type(s), including where it is held and assessment of its status. The institution(s) where type specimen(s) are housed are recorded using the international codes for Herbaria (Appendix 1) as listed in Holmgren et al’s Index Herbariorum (1981) continuously updated, see [http://sciweb.nybg.org/science2/IndexHerbariorum.asp]. Citation of authors follows Brummit & Powell (1992) Authors of Plant Names; for book abbreviations, the standard is Taxonomic Literature, 2nd edn. (Stafleu & Cowan 1976-88; supplements, 1992-2000); and periodicals are abbreviated according to B-P- H/S (Bridson, 1992) [http://www.ipni.org/index.html]. Synonyms are provided with relevant information on place of publication and details of the type(s). They are indented and listed in chronological order under the accepted taxon name. Synonyms are also cross-referenced under genus. -
The Glacial History of the Upper Mersey Valley
THE GLACIAL HISTORY OF THE UPPER MERSEY VALLEY by A a" D. G. Hannan, B.Sc., B. Ed., M. Ed. (Hons.) • Submitted in fulfilment of the requirements for the degree of Master of Science UNIVERSITY OF TASMANIA HOBART February, 1989 CONTENTS Summary of Figures and Tables Acknowledgements ix Declaration ix Abstract 1 Chapter 1 The upper Mersey Valley and adjacent areas: geographical 3 background Location and topography 3 Lithology and geological structure of the upper Mersey region 4 Access to the region 9 Climate 10 Vegetation 10 Fauna 13 Land use 14 Chapter 2 Literature review, aims and methodology 16 Review of previous studies of glaciation in the upper Mersey 16 region Problems arising from the literature 21 Aims of the study and methodology 23 Chapter $ Landforms produced by glacial and periglacial processes 28 Landforms of glacial erosion 28 Landforms of glacial deposition 37 Periglacial landforms and deposits 43 Chapter 4 Stratigraphic relationships between the Rowallan, Arm and Croesus glaciations 51 Regional stratigraphy 51 Weathering characteristics of the glacial, glacifluvial and solifluction deposits 58 Geographic extent and location of glacial sediments 75 Chapter 5 The Rowallan Glaciation 77 The extent of Rowallan Glaciation ice 77 Sediments associated with Rowallan Glaciation ice 94 Directions of ice movement 106 Deglaciation of Rowallan Glaciation ice 109 The age of the Rowallan Glaciation 113 Climate during the Rowallan Glaciation 116 Chapter The Arm, Croesus and older glaciations 119 The Arm Glaciation 119 The Croesus Glaciation 132 Tertiary Glaciation 135 Late Palaeozoic Glaciation 136 Chapter 7 Conclusions 139 , Possible correlations of other glaciations with the upper Mersey region 139 Concluding remarks 146 References 153 Appendix A INDEX OF FIGURES AND TABLES FIGURES Follows page Figure 1: Location of the study area.