4. Hygarth Gaffneys Finalvol. 17
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Australian Hualong Pty Ltd 1 Fowler Street Zeehan Tasmania 7469 Australia; Ph: 03 6471 6613; ACN 131 800 934
Australian Hualong Pty Ltd 1 Fowler Street Zeehan Tasmania 7469 Australia; Ph: 03 6471 6613; ACN 131 800 934 13 November 2019 The Chairperson Board of Environmental Protection Authority Department of Primary Industries, Parks, Water and Environment GPO Box 44 Hobart, TAS 7001 Via email "Mulligan, Helen (EPA)" <[email protected]> Dear Sir/Madam: Re: Tenth Legion Iron Ore Mine; DRAFT 3 Notice Of Intent - Level 2 Extractive Industries 1 Proponent This submission is made by Australian Hualong Limited (AHL). Contact details are; Dr Joe Xie Australian Hualong Pty Ltd. Tel/Fax: 02 8197 6518 ABN 96131800934 ACN 131 800 934. Operations: 1 Fowler Street Zeehan Tasmania 7469. PO Box 231 Zeehan Tasmania 7469 Ph: 03 6471 6613 Registered Address: 41 Kambala Road, Bellevue Hill, NSW 2023 Mr. Zhian Zhang, sole owner of Australian Hualong, has extensive experience in iron ore, tin and base metal mining, processing and smelting, mostly through his operations in Yunnan, China. More details about Mr. Zhang's operation under Zhida Industry in China are provided in the document attached, if required. Zhida in China is also owned and controlled by Mr. Zhang. 2 Project name and location The project name is the Tenth Legion Iron Ore Mine. The Project is located approximately 10km west of the township of Zeehan on the west coast of Tasmania (Figure 1). Australian Hualong Magnetite Mine – Draft NOI Revised 3 2 FIGURE 1 PROJECT LOCATION – Zeehan Western Tasmania AHL also owns the nearby Comstock plant site, which is being rehabilitated. AHL is applying for a mining lease over the propose project area, as shown in Figure 2. -
Groundwaters in Wet, Temperate, Mountainous,Sulphide-Mining Districts
Groundwaters in wet, temperate, mountainous, sulphide-mining districts: delineation of modern fluid flow and predictive modelling for mine closure (Rosebery, Tasmania). by Lee R. Evans B.App.Sci.(Hons) Submitted in fulfilment of the requirements for the degree of Doctor of Philosophy UNIVERSITY OF TASMANIA September 2009 Cover Image: Elevated orthogonal view of the 3D Rosebery groundwater model grid looking towards the northeast. i Declaration This thesis contains no material that has been accepted for a degree or diploma by the University or any institution, except by way of background information and duly acknowledged in the thesis, and to the best of the candidate’s knowledge and beliefs, contains no material previously published or written by another person, except where due acknowledgement is made in the text of the thesis. Three co-authored conference publications written as part of the present study (Evans et al., 2003; Evans et al., 2004a; and Evans et al., 2004b) are provided in Appendix Sixteen. Lee R. Evans Date: This thesis is to be made available for loan or copying in accordance with the Copyright Act 1969 from the date this statement was signed. Lee R. Evans Date: ii Abstract There are as yet few studies of the hydrogeology of sulphide-mining districts in wet, temperate, mountainous areas of the world. This is despite the importance of understanding the influence of hydrogeology on the evolution and management of environmental issues such as acid mine drainage (AMD). There is a need to determine whether the special climatic and geological features of such districts result in distinct groundwater behaviours and compositions which need to be considered in mining impact studies. -
Mount Heemskirk, West Coast
(No. 89.) l 8 8 2. -TASMAN I A. HOUSE OF ASSEMBLY •. MOUNT HEEMSKIRK, WEST COAST: REPORT ON TIN MINES BY G. THUREAU, ESQ., F.G.S. Laid upon the Table by the Minister of Lands, and ordered by the House to be printed, August 16, 1882. Lands and Works Office, Hobart, 5th June, 1882. :Srn, I HAVE the honor to instruct you to visit the West Coast, Mount Heemskirk, to report on the mineral prospects and permanency of the Tin deposits, whether lode or alluvial ; and also as to the progress. that has been made in the development of the mining industry in that locality since your former visit. · · I may also state that it is left to your own option whether you proceed to Heemskirk per steamer Amy, returning vid. Long Plain to report on the gold-fields in · that locality, or, if you prefer it, travel viit Mount Bischoff to Long Plain and Heemskirk, returning per steamer. It is very desirable that you proceed to the West Coast at your earliest possible convenience. I have the honor to be, Sir, Your obedient Servant, C. O'REILLY, Minister of Lands and Works. •G. THuREAU, Esq., F.G.S. Mount Heemskirk, 10th July, 1882. :Srn, I HAVE the honor to inform you that, since my arrival at Trial Harbour on Saturday last, I have decided upon the manner in which I shall proceed with the examinations of the Mmes and mineral deposits in this vicinity in compliance with your instructions. To-morrow I shall visit the Orient and Mount Agnew Mines, returning next day; then the .Cumberland and West Cumberland; the Gap Mines to follow, concluding with the Mines in the vicinity of the Montagu, Cliff, and along the north-western sea shore. -
Zeehan Mountain Bike (MTB) Trail Design Plan
Heemskirk MTB Trails- Design Plan West Coast,Heemskirk Tasmania Mountain Bike Trail Design Plan – West Coast, Tasmania Dirt Art Pty Ltd 1 West Coast Council October 2020 Table of Contents 1 Executive Summary 6 2 Introduction 8 2.1 Project Overview 8 2.2 Key Objectives 8 2.3 Project Background 8 2.4 Establishing the West Coast as a Mountain Bike Destination 9 3 Methodology 10 3.1 Background Analysis 10 3.2 Stage 1 Consultation 10 3.3 Desktop Analysis 10 3.4 Field Analysis 11 3.5 Detailed Trail Design 11 3.6 Stage 2 Consultation 11 3.7 Report Preparation 11 4 Site Analysis 12 4.1.1 Overview 12 4.1.2 Topography 12 4.1.3 Climate 12 4.1.4 Geology 13 4.1.5 Vegetation 13 4.1.6 Environmental and Cultural Values 13 4.1.7 Land Tenure 14 4.1.8 Land Lease and License Considerations 14 5 Consultation 15 5.1 Overview 15 5.2 Key Stakeholders 15 5.2.1 West Coast Council 15 5.2.2 Tasmanian Parks and Wildlife Service 15 5.2.3 Mining and Minerals Tasmania (MMT) 15 5.2.4 Destination West Coast (DWC) 15 5.2.5 West Coast Mountain Bike Club (WCMTBC) 15 5.2.6 Police and Emergency Services 15 5.2.7 Business Community 16 5.2.8 West Coast MTB Reference Group 16 5.2.9 Community Consultation 16 6 Proposed Development 17 6.1 Overview 17 6.1.1 Project Staging 17 6.1.2 Location Map 17 6.2 Trail Head Developments 19 6.2.1 Primary Trail Head 19 Heemskirk Mountain Bike Trail Design Plan – West Coast, Tasmania Dirt Art Pty Ltd 2 6.3 Functional Trail Head 21 6.3.1 Overview 21 6.3.2 Infrastructure Development 21 6.4 Proposed Trail Network 23 6.4.1 Overview 23 6.4.2 Trail -
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. -
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, -
Papers and Proceedings of the Royal Society of Tasmania
PAPERS AND PROCEEDINGS 01' THII ROYAL SOCIETY 01' TASMANIA, JOB (ISSUED JUNE, 1894.) TASMANIA: PJUl'TBD .&.T «TO XBROUBY" OJ'lPIOE, JUOQUUIE BT., HOBART. 1894. Googk A CATALOGUE OF THE MINERALS KNOWN TO OCCUR IN TASMANIA, WITH NOTES ON THEIR DISTRIBUTION• .Bv W. F. PETTERD. THE following Catalogue of the Minerals known to occur and reeortled from this Island is mainly prepared from specimen~ contained in my own collection, and in the majority of instances I have verified the identifications by careful qualitative analysis. It cannot claim any originality of research, 01' even accluac)" of detail, but as the material has been so rapidly accumulating during the past few )'ears I bave thoug-ht it well to place on record the result of my personal observation and collecting, wbich, with information ~Ieaned from authentic sources, may, I trust, at least pave tbe way for a more elaborate compilation by a more capable authority. I have purposely curtailed my remarks on the various species 80 Rs to make them as concise as possible, and to redulle the bulk of the matter. As an amateur I think I may fairly claim tbe indulgence of the professional or otber critics, for I feel sure tbat my task has been very inadequately performed in pro portion to the importance of the subjeot-one not only fraugbt with a deep scientific interest on account of tbe multitude of questions arisin~ from the occurrence and deposition of the minerals them selves, but also from the great economic results of our growing mining indu.try. My object has been more to give some inform ation on tbis subject to the general student of nature,-to point out tbe larg-e and varied field of observation open to him,- than to instruct the more advanced mineralo~ist. -
Papers and Proceedings of the Royal Society of Tasmania
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by University of Tasmania Open Access Repository ON MESOZOIC DOLERITP] AND DIABASE IN TASMANIA. By W. H. Twblvetrees, F.G.S., and W. F. Petterd, C.M.Z.S. The following Notes lay no claim to be an exhaustive description of our familiar '• diabase" or "dolerite" rock, which plays such an important part in the geology and physical configuration of our Island. The present object is rather to place upon record some inferences drawn from the examination of numerous microscopical sections of speci- mens collected or received from all parts of Tasmania. It is by accumulating the results of observations that stepping stones are formed to more complete knowledge. A glance at Mr. R. M. Johnston's geological map of Tasmania, issued by the Lands Office, will show the share this rock takes in the structure of the Island. It occupies the whole upland area of the Central Tiers. On the northern face of the Tiers—the Western Tiers as they are here called—there is a tongue of the rock prolonged northwards past IMount Claude. At their north-west corner it forms or caps mountains, such as Cradle Mountain (the highest in Tas- mania), Barn Bluff, Mount Pelion West. Eldon Blufi: forms a narrow western extension. Mount Sedgwick is a western out-lier ; Mount Dundas another. In that part of the island it is also found at Mount Heemskirk Falls, and on the Magnet Range, two miles north of the Magnet Mine. Mounts Gell and Hugel are also western out-liers. -
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. -
The Geology, Geochemistry and Structure of the Mount Darwin - South Darwin Peak Area, Western Tasmania
The Geology, Geochemistry and Structure of the Mount Darwin - South Darwin Peak Area, Western Tasmania. by Andrew Thomas Jones B.App.Sci.(RMIT) A thesis submitted in partial fulfihnent of the requirements for the degree ofBachelor of Science with Honours. CE:-iTRE FOR ORE DEPOSIT A:"/D EXPLORATION STUDIES Geology Department, University ofTasmania, November 1993. Abstract The Cambrian Darwin Granite intrudes calc-alkaline rhyolites of the Central Volcanic Complex on the Darwin Plateau, western Tasmania. Two distinct granite phases are recognised, an equigranular granite and a granodiorite. A biotite grade contact aureole is preserved in the Central Volcanic Complex immediate to the Darwin Granite. Debris flow deposits of volcaniclastic conglomerates and sandstones, and coherent dacite lavas of the Mid - Late Cambrian Tyndall Group unconformably overlie the Darwin Granite and Central Volcanic Complex, and are in turn overlain unconformably by pebble to boulder conglomerates of the siliciclastic Owen Conglomerate. Stratigraphic and structural evidence recognise three deformation periods within the Mt Darwin - South Darwin Peak area: the Mid - Late Cambrian, Late Cambrian - Early Ordovician, and the Devonian Tabberabberan Orogeny. Mid - Late Cambrian deformation, evidenced by granitic and foliated volcanic clasts in basal Tyndall Group conglomerate, indicates catastrophic uplift and subsequent unroofing of the granite prior to Tyndall Group deposition. This unconformity represents a significant Cambrian hiatus in the southern Mount Read Volcanics. A second unconformit)r between the Tyndall Group and the Owen Conglomerate marks cessation of Tyndall Group deposition with the onset of deposition of large volumes of siliceous detritus. The two Devonian Tabberabberan-related deformations are characterised by, NW and N trending dextral strike slip faulting and locally intense N-trending cleavage development. -
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. -
Report on Field Investigations Mt Darwin–Mt Murchison Region
Mineral Resources Tasmania Tasmanian Geological Survey Tasmania DEPARTMENT of Record 2002/18 INFRASTRUCTURE, ENERGYand RESOURCES Western Tasmanian Regional Minerals Program Mount Read Volcanics Compilation Report on field investigations Mt Darwin–Mt Murchison Region K. C. Morrison CONTENTS SUMMARY ……………………………………………………………………… 2 INTRODUCTION ………………………………………………………………… 3 SCOPE OF THE PROJECT ………………………………………………………… 3 ACKNOWLEDGMENTS ………………………………………………………… 3 FIELD TRAVERSES ……………………………………………………………… 4 DISCUSSION AND CONCLUSIONS ……………………………………………… 6 The Tyndall Group–Eastern Quartz-Phyric Sequence problem …………………… 6 Granite and related intrusive rocks — Exploration implications …………………… 7 Exploration potential of the region ……………………………………………… 9 REFERENCES …………………………………………………………………… 12 APPENDIX 1: Rock analyses ……………………………………………………… 14 FIGURES 1. Location of traverses …………………………………………………………… 16 2. Schematic cross section showing Cu-Au exploration potential of the Jukes–Darwin area, southern Mount Read Volcanics ……………………………… 10 While every care has been taken in the preparation of this report, no warranty is given as to the correctness of the information and no liability is accepted for any statement or opinion or for any error or omission. No reader should act or fail to act on the basis of any material contained herein. Readers should consult professional advisers. As a result the Crown in Right of the State of Tasmania and its employees, contractors and agents expressly disclaim all and any liability (including all liability from or attributable