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Cradle Coast Natural Resource Management
CRADLE COASTNRMANNUAL REPORT 2015-16 22015015 22016016 ANNUAL REPORT MANAGEMENT NATURAL RESOURCE CRADLE COAST 1 Cradle Coast NRM Annual Report 2015-2016 Copyright © Cradle Coast Authority 2016 No part of this publication may be reproduced without the express prior permission of the publisher. Published by: Cradle Coast Authority PO Box 338 Burnie TAS 7320 Ph: 03 6433 8400 [email protected] www.cradlecoastnrm.com www.facebook.com/cradlecoastnrm This report is produced to fulfi l the statutory reporting obligations of the Cradle Coast NRM Committee under the Tasmanian Natural Resource Management Act 2002. The Committee is required to report on its activity to the Minister for Primary Industries, Parks, Water and Environment. This report covers the period from 1 July 2015 to 30 June 2016. The Cradle Coast NRM Committee acknowledges the fi nancial support provided to it by the Australian and Tasmanian Governments. CONTENTS 4 Foreword 7 Introduction 8-10 Cradle Coast NRM Staff and Committee 12 Executive Off icer Report 14 Cradle Coast NRM Strategy Summary Cradle Coast NRM 2015/2016 Program Overview Sustainable Environment 16-17 Restoring and Maintaining Urban Waterways and Coastal Environments 18-19 Conserving and Protecting Species and Eco-Systems 20-21 Community Skills, Knowledge and Engagement Sustainable Agriculture 25 Regional Landcare Facilitator 26-27 Productive Landscapes 28 Building Indigenous People’s Capacity in NRM 29-33 Cradle Coast NRM Financial Statements 34 Thank You CRADLE COAST NRM ANNUAL REPORT 2015-16 3 FOREWORD I present the Annual Report clear that there is a crucial role for on our committee and staff , whose for 2015/16 on behalf of the regional NRM in supporting the impact experience, knowledge and passion Cradle Coast Natural Resource assessment and recovery actions. -
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 -
Geochemistry of Darwin Glass and Target Rocks from Darwin Crater, Tasmania, Australia
Meteoritics & Planetary Science 43, Nr 3, 479–496 (2008) AUTHOR’S Abstract available online at http://meteoritics.org PROOF Geochemistry of Darwin glass and target rocks from Darwin crater, Tasmania, Australia Kieren T. HOWARD School of Earth Sciences, University of Tasmania, Hobart, Tasmania 7000, Australia Present address: Impacts and Astromaterials Research Centre, Department of Mineralogy, The Natural History Museum, Cromwell Road, London SW7 5BD, UK Corresponding author. E-mail: [email protected] (Received 1 March 2007; revision accepted 25 July 2007) Abstract–Darwin glass formed about 800,000 years ago in western Tasmania, Australia. Target rocks at Darwin crater are quartzites and slates (Siluro-Devonian, Eldon Group). Analyses show 2 groups of glass, Average group 1 is composed of: SiO2 (85%), Al2O3 (7.3%), TiO2 (0.05%), FeO (2.2%), MgO (0.9%), and K2O (1.8%). Group 2 has lower average SiO2 (81.1%) and higher average Al2O3 (8.2%). Group 2 is enriched in FeO (+1.5%), MgO (+1.3%) and Ni, Co, and Cr. Average Ni (416 ppm), Co (31 ppm), and Cr (162 ppm) in group 2 are beyond the range of sedimentary rocks. Glass and target rocks have concordant REE patterns (La/Lu = 5.9–10; Eu/Eu* = 0.55–0.65) and overlapping trace element abundances. 87Sr/86Sr ratios for the glasses (0.80778–0.81605) fall in the range (0.76481–1.1212) defined by the rock samples. ε-Nd results range from −13.57 to −15.86. Nd model ages range from 1.2–1.9 Ga (CHUR) and the glasses (1.2–1.5 Ga) fall within the range defined by the target samples. -
The Philosophers' Tale
1 Photo: Ollie Khedun Photo: THE VISION THE CONCEPT THE PROPOSAL The Philosophers’ Tale is The West Coast Range consists The Next Iconic Walk – The of 6 mountains on a north south Philosophers’ Tale 2019 proposal more than just an iconic walk, ridge. The ridge is trisected by the – Chapter One: Owen, takes it is made up of a series of Lyell Highway (between Mt Lyell people on a journey over 28km in iconic walks to be developed and Mt Owen) and the King River 3 days and 2 nights experiencing Gorge (between Mt Huxley and Mt mountain peaks, incredible views, over a period of time. There Jukes). This makes for three distinct button grass plains, cantilever are an abundance of coastal regions, each with their own part platforms and suspension bridges walks – the Overland Track to play in telling the bigger story. over deep river gorges down into All areas have been impacted cool temperate rainforest, majestic is now mature, and people by mining exploration or other waterfalls along the tranquil King are looking for the next development in the past 100 years. River on the incredible West Coast of Tasmania. With the option to option – The Philosophers’ The area is naturally divided into finish via train, hi-rail, raft, kayak, four zones, or in story telling Tale is just that. People will helicopter or jet boat, making it a parlance, ‘Chapters’. The Chapters be drawn locally and across truly unforgettable experience. (outlined on page 8), let’s call them the globe to experience these Owen, Jukes, Lyell and Tyndall lead View West Coast video iconic walks, returning time easily to the staged construction of any proposed track works. -
Unbroken Meteorite Rough Draft
Space Visitors in Kentucky: Meteorites and Asteroid “Ida.” Most meteorites originate from asteroids. Meteorite Impact Sites in Kentucky Meteorite from Clark County, Ky. Mercury Earth Saturn Venus Mars Neptune Jupiter William D. Ehmann Asteroid Belt with contributions by Warren H. Anderson Uranus Pluto www.uky.edu/KGS Special thanks to Collie Rulo for cover design. Earth image was compiled from satellite images from NOAA and NASA. Kentucky Geological Survey James C. Cobb, State Geologist and Director University of Kentucky, Lexington Space Visitors in Kentucky: Meteorites and Meteorite Impact Sites in Kentucky William D. Ehmann Special Publication 1 Series XII, 2000 i UNIVERSITY OF KENTUCKY Collie Rulo, Graphic Design Technician Charles T. Wethington Jr., President Luanne Davis, Staff Support Associate II Fitzgerald Bramwell, Vice President for Theola L. Evans, Staff Support Associate I Research and Graduate Studies William A. Briscoe III, Publication Sales Jack Supplee, Director, Administrative Supervisor Affairs, Research and Graduate Studies Roger S. Banks, Account Clerk I KENTUCKY GEOLOGICAL SURVEY Energy and Minerals Section: James A. Drahovzal, Head ADVISORY BOARD Garland R. Dever Jr., Geologist V Henry M. Morgan, Chair, Utica Cortland F. Eble, Geologist V Ron D. Gilkerson, Vice Chair, Lexington Stephen F. Greb, Geologist V William W. Bowdy, Fort Thomas David A. Williams, Geologist V, Manager, Steven Cawood, Frankfort Henderson office Hugh B. Gabbard, Winchester David C. Harris, Geologist IV Kenneth Gibson, Madisonville Brandon C. Nuttall, Geologist IV Mark E. Gormley, Versailles William M. Andrews Jr., Geologist II Rosanne Kruzich, Louisville John B. Hickman, Geologist II William A. Mossbarger, Lexington Ernest E. Thacker, Geologist I Jacqueline Swigart, Louisville Anna E. -
Physical Distribution Trends in Darwin Glass
Physical distribution trends in Darwin glass Item Type Article; text Authors Howard, Kieren T. Citation Howard, K. T. (2009). Physical distribution trends in Darwin glass. Meteoritics & Planetary Science, 44(1), 115-129. DOI 10.1111/j.1945-5100.2009.tb00722.x Publisher The Meteoritical Society Journal Meteoritics & Planetary Science Rights Copyright © The Meteoritical Society Download date 11/10/2021 08:24:44 Item License http://rightsstatements.org/vocab/InC/1.0/ Version Final published version Link to Item http://hdl.handle.net/10150/656530 Meteoritics & Planetary Science 44, Nr 1, 115–129 (2009) Abstract available online at http://meteoritics.org Physical distribution trends in Darwin glass Kieren T. HOWARD Impacts and Astromaterials Research Centre (IARC), Mineralogy Department, The Natural History Museum, Cromwell Road, London SW7 5BD, UK Corresponding author. E-mail: [email protected] (Received 25 January 2008; revision accepted 26 September 2008) Abstract–Darwin glass formed by impact melting, probably during excavation of the 1.2 km diameter Darwin crater, Tasmania, Australia. The glass was ejected up to 20 km from the source crater and forms a strewn field of >400 km2. There is at least 11,250 m3 of glass in the strewn field and relative to the size of the crater this is the most abundant ejected impact glass on Earth. The glass population can be subdivided on the basis of shape (74% irregular, 20% ropy, 0.5% spheroid, 6% droplet, and 0.7% elongate) and color (53% dark green, 31% light green, 11% black, and 5% white). The white glasses contain up to 92 wt% SiO2 and are formed from melting of quartzite. -
Aboriginal Society in North West Tasmania:Dispossession And
~boriginal Society in North West Tasmania: Dispossession and Genocide by Ian McFarlane B.A. (Hons) submitted in fulfillment of the requirements for the degree of Doctor of Philosophy University of Tasmania October 2002 Statement of Authorship This thesis contains no material which has been accepted for a degree or diploma by the _University or any other institution, except by way of background information and duly acknowledged in the thesis and, to the best of my knowledge and belief, no material previously published or written by another person, except where due acknowledgment is made in the text of the thesis. 31 lf?~?.. Zoo-z.. Signed ...... /~ .. ~ .. 'f.-!~.. D at e ..............................t.,. .. Statement of authority of access This thesis may be made available for loan and limited copying in accordance with the Copyright Act 1968. stgne. d............................................... J._ ~~-1-- . 19 March 2002 Abstract Aboriginal Society in North West Tasmania: Dispossession and Genocide As the title indicates this study is restricted to those Aboriginal tribes1 located in the North West region of Tasmania. This approach enables the regional character and diversity of Aboriginal communities to be brought into focus; it also facilitates an . ex:a.miJ,lation of the QJlique process of dispossession that took place in the North West region, an area totally under the control of the Van Diemen's Land Company (VDL Co). Issues dealing with entitlement to ownership and sovereignty will be established by an examination of t~e structure and function of traditional. Aboriginal Societies in the region, as well as the, occupation and use they made of their lands. -
Northwest Tasmania Groundwater
300000mE 350000mE 400000mE 450000mE MINERAL RESOURCES TASMANIA CAPE WICKHAM Tasmania Disappointment DEPARTMENT of INFRASTRUCTURE Cape ENERGY and RESOURCES Farewell Bay 5600000mN NORTHWEST TASMANIA 5600000mN GROUNDWATER MAP PHOQUES Lavinia Pt BAY New Year Is Christmas Is PERCENT PERCENTAGE AVERAGE SALINITY PROSPECTIVITY NUMBER MAXIMUM IRRIGATION VULNERABILITY TO POLLUTION AQUIFER TYPE (Whole of Tasmania) ROCK GROUPS SUCCESSFUL YIELD (L/s) RANGE GENERAL AQUIFER CHARACTERISTICS OF BORES YIELD (L/s) SUCCESSFUL (mg/L) (YIELD >0.03) # (YIELD >=1.5) Whistler Pt Quaternary aeolian deposits marginal to the coast 60 95 0.65 (11) 1.3 0 270 - 980 These aquifers are contained in surface sand deposits of limited thickness - usually up to a maximum thickness of 10-15 metres, but often much less. Yields depend on grain High. consisting of fine to medium grain size sand. POROUS size, clay content and the thickness of saturated material. Yields decrease with an increase in the clay content. Groundwater is usually extracted from these aquifers using spear (INTERGRANULAR) HIGH bores installed to a depth of 7-8 metres. A single spear in a prospective area may yield 0.75 L/s (e.g. Currie area) which would be sufficient for domestic, garden, and stock use. A nest of spear bores (10-20) using a central pump may yield irrigation or small town supplies (7-15 L/s). Significant extraction from these deposits takes place at Currie, where the town supply comes from dune sand, and at Stanley where the golf club installed a system to water the course. Other areas including Woolnorth, Stanley, Arthur River and Peggs Beach have proved to have potential for useful supplies. -
A Survey of the Freshwater Fish Fauna of the Tarkine Region, North-West Tasmania
Bush Blitz – Tarkine Region North-West Tasmania, 27 January to 6 February 2015 A survey of the freshwater fish fauna of the Tarkine region, north-west Tasmania 27 January – 6 February 2015 Submitted: 26 March 2015 Scott Hardie Page 1 of 29 Bush Blitz – Tarkine Region North-West Tasmania, 27 January to 6 February 2015 Contents Contents .................................................................................................................................. 2 List of contributors ................................................................................................................... 3 Abstract ................................................................................................................................... 4 1. Introduction ...................................................................................................................... 4 2. Methods .......................................................................................................................... 6 2.1 Site selection ............................................................................................................. 6 2.2 Collection methods .................................................................................................... 6 2.2.1 General methods .................................................................................................... 6 2.2.2 Methods used at standard survey sites ................................................................... 8 2.3 Identifying the collections ......................................................................................... -
Economic Implications for Tasmania of the Proposed National Heritage Listing of the Tarkine Area
Potential Socio- economic implications for Tasmania of the Proposed National Heritage listing of the Tarkine area Tasmanian Government submission to the Australian Government - Minister for Sustainability, Environment, Water, Population and Communities October 2011 Table of Contents Section Section Heading Page Number Number Executive Summary 3 Introduction 5 1 North-West Region – Economic Data 5 2 Sovereign Risk and Uncertainty 12 3 Existing Mining Projects and Developments 12 4 Review of Adverse Impacts on Future Value Adding 19 Projects (Mining) 5 Potential for New Mineral Discovery in the Area 20 Under Assessment for National Heritage Listing 6 Current Regulation of Mineral Exploration and Mining 22 in Tasmania 7 Tourism Overview 23 8 Forestry 24 Conclusion 25 Attachment Comments from Local Government Authorities 27 1 2 Potential Socio-economic implications for Tasmania of the Proposed National Heritage listing of the Tarkine area Executive Summary As outlined in the Tasmanian Government’s submission to the Australian Heritage Council on the Proposed National Heritage listing, the Tasmanian Government does not agree with the proposed National Heritage values and boundary listing of the area of North-West Tasmania referred to as the Tarkine. The Government has issues with the approach taken to identifying values within the proposed boundary. In addition, pursuant to section 324JJ (5)(b) of the Environmental Protection and Biodiversity Conservation Act, 1999, the Government wishes to draw to the attention of the Minister that it believes serious immediate and long term social impacts should be taken into account which would occur in an already depressed region of Tasmania resulting from the closure of key industries such as mining and forestry. -
15. Mt Jukes Lookout
15. Mt Jukes Lookout Key facts about this geosite: The eastward trending ridge-line extending from Mt Jukes shows a glacially carved moraine ridge made up of Owen Conglomerate boulders The area shows outcrops of the Mount Read Volcanics The skyline to the east shows jagged peaks (including Frenchmans Cap) which are made up of resistive, Precambrian quartzite The general location of the Darwin Crater, a meteorite impact feature is to the south east of this site How to get there: From Queenstown drive south along the Mt Jukes Road for approximately 18 kilometres (Figure 1). The lookout is located on the left hand side of the road about 1 kilometre east the Mt Huxley Lookout. Figure 1. Location of the Mt Jukes Lookout Geosite Geosite Description: From the Mt Jukes Lookout there are extensive views towards Frenchmans Cap in the east and Mt Jukes to the south. A schematic geological interpretation of the view to the east is shown in Figures 2 and 3. Mt Jukes East Jukes Peak Mt Jukes Owen East Jukes Peak Conglomerate Cambrian Mt. Read Volcanics Moraine ridgeGlacial crest deposits Quaternary till (glacial deposits) Figure 2. The photograph above looking east from the car park has a schematic geological interpretation of the view below it. Figure 3. The photograph above looking south east across man-made Lake Burbury to Frenchmans Cap with a schematic geological interpretation of the view below. The rocks behind you, on Mt Jukes and West Jukes Peak (Figure 4), comprise a sequence of pink coloured conglomerate, sandstone and siltstone, which geologists have named the Owen Conglomerate. -
Extinction of the Thylacine
bioRxiv preprint doi: https://doi.org/10.1101/2021.01.18.427214; this version posted January 19, 2021. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY-NC-ND 4.0 International license. 1 Main Manuscript title: Extinction of the Thylacine. 2 3 Authors: Barry W. Brook1,2*, Stephen R. Sleightholme3, Cameron R. Campbell4, Ivan Jarić5,6 4 and Jessie C. Buettel1,2. 5 6 Affiliations: 7 1 School of Natural Sciences, University of Tasmania, Hobart, Tasmania, 7001 Australia. 8 2 ARC Centre of Excellence for Australian Biodiversity and Heritage (CABAH). 9 3 Project Director - International Thylacine Specimen Database (ITSD), 26 Bitham Mill, 10 Westbury, BA13 3DJ, UK. 11 4 Curator of the online Thylacine Museum: http://www.naturalworlds.org/thylacine/ 8707 Eagle 12 Mountain Circle, Fort Worth, TX 76135, USA. 13 5 Biology Centre of the Czech Academy of Sciences, Institute of Hydrobiology, České 14 Budějovice, Czech Republic. 15 6 University of South Bohemia, Faculty of Science, Department of Ecosystem Biology, České 16 Budějovice, Czech Republic. 17 *Corresponding author: [email protected] 18 19 Author Contributions: B.W.B., S.R.S., C.R.C. and J.C.B. conceived the project and developed 20 the database, B.W.B. performed the data analysis and wrote the paper, B.W.B., I.J. and J.C.B. 21 created the display items. All authors discussed the draft structure, results, and interpretation, and 22 commented on the manuscript.