Maritime Times of Tasmania
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Cape Wickham Lighthouse 150 Anniversary Event Programme
Cape Wickham Lighthouse 150th Anniversary Event Programme 3 – 7 November 2011 www.kingislandlight150.com A project of King Island Tourism Inc, King Island Council & the Australian Maritime Safety Authority (AMSA) Final Version 26 October 2011 The Story of the Lighthouse King Island‟s “Beacon of Bass Strait” is about to come-of-age! The Cape Wickham Lighthouse on the northernmost tip of King Island started service on 1st November 1861 – 150 years ago. King Island, located at the western entrance to Bass Strait, is an island rich in history with shipwrecks, lighthouses and jagged reefs. It is blessed with an abundance of long stretching sandy beaches and lush green pasture. From this little paradise are produced some of Australia's finest natural foods for which the Island is probably best known including grass fed beef, cheese, crayfish & abalone and yet there is more to this 64km long by 27km wide stretch of land than first meets the eye. The 48m tall Cape Wickham Lighthouse began operating 150 years ago on November 1st 1861 and has been in continuous operation since that first night providing - 150 years of saving lives. 150 years of guidance and direction for shipping 150 years of community capacity building 150 years of very unique history. Cape Wickham is at the northernmost tip of King Island and the 88km gap between Cape Otway (Victoria) and Cape Wickham was often a trap for the unwary Ship‟s Master seeking entry into Bass Strait. The Western entrance has become the graveyard to at least 18 ships nearing the end of their long voyages. -
Tasman Peninsula
7 A OJ? TASMAN PENINSULA M.R. Banks, E.A. Calholln, RJ. Ford and E. Williams University of Tasmania (MRB and the laie R.J. Ford). b!ewcastle fo rmerly University of Tasmama (EAC) and (ie,a/Ogle,Cl; Survey of Tasmania (E'W) (wjth two text-figures lUld one plate) On Tasman Peninsula, southeastern Tasmania, almost hOrizontal Permian marine and Triassic non-marine lOcks were inllUded by Jurassic dolerite, faulted and overiain by basalt Marine processes operating on the Jurassic and older rocks have prcl(iU!ced with many erosional features widely noted for their grandeur a self-renewing economic asset. Key Words: Tasman Peninsula, Tasmania, Permian, dolerite, erosional coastline, submarine topography. From SMITH, S.J. (Ed.), 1989: IS lllSTORY ENOUGH ? PA ST, PRESENT AND FUTURE USE OF THE RESOURCES OF TA SMAN PENINSULA Royal Society of Tasmania, Hobart: 7-23. INTRODUCTION Coal was discovered ncar Plunkett Point by surveyors Woodward and Hughes in 1833 (GO 33/ Tasman Peninsula is known for its spectacular coastal 16/264·5; TSA) and the seam visited by Captain scenery - cliffs and the great dolerite columns O'Hara Booth on May 23, 1833 (Heard 1981, p.158). which form cliffs in places, These columns were Dr John Lhotsky reported to Sir John Franklin on the first geological features noted on the peninsula. this coal and the coal mining methods in 1837 (CSO Matthew Flinders, who saw the columns in 1798, 5/72/1584; TSA). His thorough report was supported reported (1801, pp.2--3) that the columns at Cape by a coloured map (CSO 5/11/147; TSA) showing Pillar, Tasman Island and Cape "Basaltcs" (Raoul) some outcrops of different rock This map, were "not strictlybasaltes", that they were although not the Australian not the same in form as those Causeway Dictionary of (Vol. -
Volume 42 No 2 March 2016
Volume 42 No 2 March 2016 PO Box 605 Sandy Bay TAS 7006 cyct.org.au Committee Members Commodore Andrew Boon M 0400 651 532 Juliet Vice Commodore Lew Garnham M 0417 589 008 Minerva Rear Commodore Catrina Boon H 6243 9268 Dalliance Treasurer Alex Papij H 6223 4639 Rusalka Secretary Mike Ponsonby H 6247 1409 Rubicon Editor Albatross Fiona Preston M 0435 542 247 Samos Committee Richard Philpot H 6267 4551 Heather Anne Leigh Miller H 6229 9078 Fleur de Lys Alan Butler M 0457 000 434 Membership Officer Julie Macdonald H 6247 9569 Westerly Warden & Albatross mailing Chris Creese H 6225 2806 Neptune Quartermaster Elizabeth Helm H 6229 3932 Intrepid Webmaster Dave Davey H 6267 4852 Windclimber Life Members Erika Shankley Dave Davey Chris Creese Send all material for publication in ‘Albatross’ to the Editor - [email protected]. Cover page: Dogs who sail. Photographer: Lizzie Garnham Albatross March 2016 Contents CYCT CALENDAR .................................................................................................. 2 Editorial ....................................................................................................................... 3 Commodore’s Report ............................................................................................. 4 Vice Commodore’s Report .................................................................................... 5 Rear Commodore’s Report ................................................................................... 6 Women on Boats ..................................................................................................... -
Beacon to Beacon Guide—Capricorn Coast
Maritime Safety Queensland Rosslyn Bay Boat Harbour Beacon to Beacon Guide Capricorn Coast Published by For commercial use terms and conditions Maritime Safety Queensland Please visit the Maritime Safety Queensland website at www.msq.qld.gov.au © Copyright The State of Queensland (Department of Transport and Main Roads) 2014 ‘How to’ use this guide Use this Beacon to Beacon Guide with To view a copy of this licence, visit the ‘How to’ and legend booklet available from http://creativecommons.org/licenses/by/3.0/au www.msq.qld.gov.au Capricorn Coast Key Sheet Mag P P P P P P P P P P P P P P Corio Bay P P P P ¶AP P North Keppel Island SOUTH Yeppoon Rosslyn Bay !A !1 Boat PACIFIC Harbour Great Keppel Island OCEAN Emu Park Fitzroy Keppel !2 Sands !B ROCKHAMPTON !3 River Keppel Bay !C Port Alma Curtis Island !D T h e N a r r o w s Marine rescue services !1 CG Yeppoon !2 CG Keppel Sands !3 CG Rockhampton !4 VMR Gladstone !4 GLADSTONE Enlargements ! A Rosslyn Bay Boat Harbour See Gladstone ! B Rockhampton series ! C Port Alma ! D The Narrows CG Yeppoon (0600-1800 Fri--Mon) (88-86, 16-21-22, 4125-6215-8291-2182-2524) ph 4933 6600 CG Keppel Sands (0600-1800 Tues-Thurs) (88-86, 16-21-22, 4125-6215-8291-2182-2524) ph 4934 4906 CC-1 See charts AUS 820, 426, 367 Mag nautical miles (nM) Sloping Island P P 0 1 2 P P P P P ! P Barlows Hill P P Yeppoon Inlet P P ! 0 1 2 3 4 P KEPPEL P Meikleville Hill P P kilometres P P FG ISLES AP P FG ¶ YEPPOON Fi g T n Inlet ree o po Ck k ep e Y e r C See Inset 1 s s Cooee Bay o R Inset 1 Fl(2) 6s TARANGANBA Claytons -
The Effects of Fire on Burrow-Nesting Seabirds Particularly Short-Tailed Shearwaters
Papers and Proceedings of the Royal Society of Tasmania, Volume 133(1), 1999 15 THE EFFECTS OF FIRE ON BURROW-NESTING SEABIRDS PARTICULARLY SHORT-TAILED SHEARWATERS (PUFF/NUS TENUIROSTR/5) AND THEIR HABITAT IN TASMANIA by Nigel Brothers and Stephen Harris (with three text-figures, four plates and an appendix) BROTHERS, N. & HARRJS, S., 1999 (31 :x): The effects of fire on burrow-nesting seabirds particularly short-tailed shearwaters (Puffinus tenuirostris) and their habitat in Tasmania. Pap. Proc. R. Soc. Tasm. 133(1 ): 15-22. https://doi.org/10.26749/rstpp.133.1.15 ISSN 0080-4703. Parks and Wildlife Service, Department of Primary Industries, Water and Environment, GPO Box 44A, Hobart, Tasmania, Australia 7001. The synchronised breeding habit of many seabird species makes them particularly vulnerable to fires in the nesting area. Post-fire recolonisation and soil formation were studied on Albatross Island, and observations from island rookeries of shearwaters, fairy prions and fairy penguins in eastern Bass Strait and elsewhere were used with a view to understanding the long-term impact of fires on seabird colonies in Tasmania. Key Words: island vegetation, flora, Tasmania, fire, coast, rookeries, seabirds, soil depth, Puffinus tenuirostris, Bass Strait, habitat monitoring. INTRODUCTION and it is in such circumstances chat burrow-nesting seabirds are found in greatest abundance. Short-tailed shearwaters, Large populations of seabirds breed on islands around Puffinustenuirostris, are most abundant in chis habitat, Tasmania and it is on these islands chat wildfires frequencly with small numbers of liccle penguin, Eudyptes minor, occur, moscly through vandalism, sometimes by accident. scattered throughout. Figure 2 indicates the location of colony Deliberate burning by land managers also occurs. -
Geological Timeline - Tasmania
GEODIVERSITY Geological Timeline - Tasmania Tasmania’s spectacular geodiversity has contributed Chains of volcanoes form across Tasmania, including Mt directly to the islands’ biodiversity. The State’s Read Volcanic Belt, a highly significant mineralised belt. geodiversity is a result of continental drift, ice ages, humid, hot conditions and earthquakes occurring over 443 - 408 Million Years Ago more than a billion years. Extensive erosion and subsequent deposition form the sandstones and conglomerates of West Coast Range and A very brief and summarised account of Tasmania’s Denison Range. geological history is outlined below. Although Tasmania is referred to frequently, it was not until about 45 Tasmania partly covered by a warm tropical sea and part million years ago that Tasmania began to look anything of a much larger land mass of Gondwana situated near like it does today. the equator. Gordon Limestone formed from the debris of marine life. Today this limestone outcrops in parts of 4600 - 635 Million Years Ago the Franklin and Gordon River valleys and around Mole The Earth formed about 4600 million years ago. Creek, where subsequent disolving by water has formed many karst and cave systems. Little is known about the Precambrian, despite it making up roughly seven-eighths of the Earth’s history. This is 408 - 360 Million Years Ago because traces of the geological heritage of Precambrian Warm shallow continental seas provide a hospitable times have been erased by relentless subsequent erosion. environment for marine life of all kinds. Coral reefs made First evidence of simple life forms, cyanobacteria, the their first appearance during this time, and first bony fish building blocks for stromatolites, are among the oldest appear. -
South-East Marine Region Profile
South-east marine region profile A description of the ecosystems, conservation values and uses of the South-east Marine Region June 2015 © Commonwealth of Australia 2015 South-east marine region profile: A description of the ecosystems, conservation values and uses of the South-east Marine Region is licensed by the Commonwealth of Australia for use under a Creative Commons Attribution 3.0 Australia licence with the exception of the Coat of Arms of the Commonwealth of Australia, the logo of the agency responsible for publishing the report, content supplied by third parties, and any images depicting people. For licence conditions see: http://creativecommons.org/licenses/by/3.0/au/ This report should be attributed as ‘South-east marine region profile: A description of the ecosystems, conservation values and uses of the South-east Marine Region, Commonwealth of Australia 2015’. The Commonwealth of Australia has made all reasonable efforts to identify content supplied by third parties using the following format ‘© Copyright, [name of third party] ’. Front cover: Seamount (CSIRO) Back cover: Royal penguin colony at Finch Creek, Macquarie Island (Melinda Brouwer) B / South-east marine region profile South-east marine region profile A description of the ecosystems, conservation values and uses of the South-east Marine Region Contents Figures iv Tables iv Executive Summary 1 The marine environment of the South-east Marine Region 1 Provincial bioregions of the South-east Marine Region 2 Conservation values of the South-east Marine Region 2 Key ecological features 2 Protected species 2 Protected places 2 Human activities and the marine environment 3 1. -
Discover a World of Family History SAVE the GSV from HISTORY!
Quarterly Journal of The Genealogical Society of Victoria Inc Getting it write Research Corner Creating a sense of tension, integrating confl ict Understanding Victoria's Legal System or struggle in a story for Genealogists VOLUME 35 ISSUE 2 JUNE 2020 $15.00 ISSN 0044-8222 Walter Hon, Beekeeper of Seventy Foot Diggings Learning from my Mistakes Henry Woodroffe: Much more than a seaman Cissie, Who Are You? Waterloo and Brexit How to: Irish Research Discover a world of family history SAVE THE GSV FROM HISTORY! For nearly 80 years the GSV has helped you find your histories, but we don’t want to be part of history! The GSV needs your help. We have lost almost all income from events and other sources for 2020 (see 'Pen of the President' in this issue). To continue with the high level of member services we need your donations. Please help us reach our target of $10,000 by the end of October. Your targeted donations to the GSV will also help stimulate our economy by multiplying its spending effect to keep our wheels turning. It is not being saved for a rainy day! You can donate via the 'Donate' button on the website, by email to [email protected], by mail using PayPal, bank transfer or cheque. All donations over $2.00 are tax deductable. Access to Records at Home Permission has been given for GSV Members to access these databases from home. For instructions on how, please email gsv@ gsv.org.au. Allow time for these instructions to be sent to you as emails are replied to on Monday to Friday, 10am to 4pm. -
Shipwrecks: Images and Perceptions of Nineteenth Century Maritime Disasters
4 Shipwrecks: Images and Perceptions of Nineteenth Century Maritime Disasters Mark Staniforth In the nineteenth century the long sea voyage across thousands of miles of open ocean to Australia was a step into the unknown. International migration at this time usually involved travel by sea, as it had in previous centuries. Ships were the primary long distance transportation method and the movement of passengers was one of their most important functions. It has been estimated that more than 1.6 million immigrants travelled to Australia by ship between 1788 and 1900, nearly half of these people were assisted immigrants of one type or another and they came primarily from Great Britain with smaller numbers from Europe (Barrie 1989:121). In the popular imagination the ocean represented hazard and uncertainty - an alien environment in which the possibility of shipwreck loomed large. Passengers felt themselves to be at the mercy of the elements and being directly exposed to the extremes of the weather in a moving structure was a new and disconcerting experience. This fear of shipwreck can be seen in a letter from P. Harnett to his brother from Cape Town in 1832 who writes that: 'you and the family must have been frequently tormented by anxious hopes and fears of my safety or probably have heard that the vessel was wrecked and as a matter of course that I was lost' (Harnett 1832). In most respects shipwrecks, like other tragedies involving transportation, are civil or 'man made' disasters yet they also exhibit some of the 45 46 Disasters: Images and Contexts characteristics of natural disasters.l These include evoking in the victims feelings of powerlessness in the face of overwhelming natural forces and a timeframe which sometimes extends over a period of hours or even days. -
Australia's Worst Civil Maritime Disaster Meet
AUSTRALIA’S WORST CIVIL MARITIME DISASTER MEET LOCAL MAKERS BIRDS OF KING ISLAND EDITION_37 WELCOME BACK! RESERVATIONS I am very pleased to welcome you In response to COVID-19, Sharp Airlines is back on board! actively monitoring government and agency & ENQUIRIES recommendations and we have developed During the past 12 months we have a COVID Control Framework which has CALL 1300 55 66 94 had our challenges and with a new been implemented across our business and year comes new hope. network. This has been established using sharpairlines.com.au industry standards. We look forward to continuing to deliver crucial tourism and In line with this, airlines and airports have worked together on a set of protocols to business opportunities to the minimise the risks of COVID-19 at each stage HEAD OFFICE Bass Strait Island communities. of your journey, the next time you fly. We 44 Gray Street want you to travel with confidence, and we all Hamilton Victoria 3300 Recently we have been able have a role to play in that. T: 1300 55 66 94 to support the Tasmania E: [email protected] Government’s aim of encouraging Please ensure when travelling you are aware intrastate visitation in the wake of of any government requirements that apply at your destination, including wearing face COVID-19 border restrictions. LIKE TO ADVERTISE? masks and coverings. Editorial & Advertising We have been able to offer return flight Please visit the government websites to Contact Heidi Jarvis services between Hobart and King Island, obtain up to date information on the relevant T: 0438 778 161 and Hobart and Flinders Island, which are E: [email protected] border controls and COVID requirements currently available until the end of May. -
Assessment of Australia's High Seas Permits
Assessment of Australia’s High Seas Permits May, 2013 © Commonwealth of Australia 2013 This work is copyright. Apart from any use as permitted under the Copyright Act 1968, no part may be reproduced by any process without prior written permission from the Commonwealth, available from the Department of Sustainability, Environment, Water, Population and Communities. Requests and inquiries concerning reproduction and rights should be addressed to: Assistant Secretary Marine Biodiversity and Biosecurity Branch Department of Sustainability, Environment, Water, Population and Communities GPO Box 787 Canberra ACT 2601 Disclaimer This document is an assessment carried out by the Department of Sustainability, Environment, Water, Population and Communities of a commercial fishery against the Australian Government ‘Guidelines for the Ecologically Sustainable Management of Fisheries – 2nd Edition’. It forms part of the advice provided to the Minister for Sustainability, Environment, Water, Population and Communities on the fishery in relation to decisions under Part 13A of the Environment Protection and Biodiversity Conservation Act 1999. The views expressed do not necessarily reflect those of the Minister for Sustainability, Environment, Water, Population and Communities or the Australian Government. While reasonable efforts have been made to ensure that the contents of this report are factually correct, the Australian Government does not accept responsibility for the accuracy or completeness of the contents, and shall not be liable for any loss or damage that may be occasioned directly or indirectly through the use of, or reliance on, the contents of this report. You should not rely solely on the information presented in the report when making a commercial or other decision. -
Glacial-Interglacial Sea Surface Temperture And
PLANKTIC FORAMINIFERA-BASED SEA SURFACE TEMPERATURE ESTIMATES AND LATE QUATERNARY OCEANOGRAPHY OFF NEW ZEALAND’S WEST COAST Andrew Peter Kolodziej A thesis submitted in partial fulfillment for the degree of Masters of Science in Geology School of Geography, Environment and Earth Sciences Victoria University 2010 i ii Abstract Planktic foraminiferal assemblages were used to investigate the paleoceanography of the Eastern Tasman Sea over the last 480 kyrs (Marine Isotope Stages 12-1). One hundred and sixty-two faunas (96 picked and identified as part of this project (MIS 12-6) added to 66 census counts from Dr. M. Crundwell (MIS 6-1)) have been assembled from Marion Dufresne piston core MD06-2986 (~43˚ S. off New Zealand‟s west coast, 1477 m water depth). Faunal changes through the last five glacial-interglacial cycles are used to track surface water mass movement. Glacial periods are dominated by the eutrophic species Globigerina bulloides, with significant contributions from the temperate species Globoconella inflata. Temperate species Neogloboquadrina incompta and Gc. inflata dominate interglacials, with the former dominating the warmer parts and the latter dominating the cooler parts of the interglacials. Modern Analogue Technique (MAT) and an Artificial Neural Network (ANN) were used to estimate past sea surface temperatures (SST) based on the foraminiferal census counts data (23 species, ~46,000 specimens). SSTs show that MIS 12 was the longest, sustained cold period, while the coldest temperature was recorded in MIS 5d (~8º C). Interglacials MIS 11 and 5e are the two warmest stages of the record, with SSTs reaching ~18.5º C, about ~2º C warmer than present day.