In and Around Launceston Walks, Runs and Rides for All Ages
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Natural History and Values of the Kanamaluka/Tamar Estuary Formation, Function and Ecology
TAMAR ESTUARY AND ESK RIVERS PROGRAM EDUCATION SERIES - FACT SHEET 2 nrmnorth.org.au Natural history and values of the kanamaluka/Tamar estuary Formation, function and ecology The kanamaluka/Tamar estuary is unique in South and North Esk rivers met at the mouth many ways. Fed by five major river systems, it of Corra Lynn Gorge. drains the largest catchment in Tasmania, and Between 35 and 47 million years ago, several the estuary itself is the longest navigable large lava flows occurred in the north, middle estuary in Australia. Home to many unique and southern parts of the valley. The lava and sometimes threatened plant and animal cooled to form basalt. In the middle sections species, it is truly a special place. the basalt capped the old lake sediments, HOW WAS IT FORMED? preserving them from further erosion. This can be seen at Grindelwald, Windermere, and In the early geological history of Tasmania, the north of Hillwood. Tamar Valley didn’t exist and was instead a large peneplain, or dolerite capped lowland Basalt at Rowella and Bell Bay forced the river area, that had been worn down by millions of to keep to its channel, preventing it from years of erosion. From 95 to 65 million years eating sideways into the old sediments and ago, stretching of the earth’s crust created blocking the river for some time at Whirlpool earthquakes that split this peneplain apart, Reach and Bell Bay, creating new lakes in the creating the highland areas of Mt Arthur, Mt valley again, which were eventually breached Barrow and Ben Lomond to the east and the and the Tamar resumed its old course. -
Land of Tasmania Report by the Surveyor-General
(No. 18.) 18 6 4. TASMAN I A. LANDS OF TASMANIA. REPORT BY THE SURVEYOR-GENERAL. Laid upon the Table by Mr. Colonial Treasurer, and ordered by the House to he printed, 29 June, I 864. LANDS OF TASTh1ANIA; . COMPILED FROM THE OFFICIAL RECORDS OF THE SURVEY DEPARTMENT, DY ORDER OF THE HONORABLE THE COLONIAL TREASURER. Made up to the 31st December, 1862. '««f,man ta: JAMES BARNARD, GOVERNMENT PRINTER, HOBART TOWN. 186 4. T A B L E OF C O N T E N T S. PAGE PREFACE •••••••••• , • • • • • • • • • . • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • • 3 Area of Tasmania, with alienated and unalienated Lands . • . • • • • . • . 17 Population of Tasmania ...............••..• ,........................... ib. Ditto of Towns . • • . • • • . • . • . • . • • . • . ] 8 Country Lands granted and sold since 1804 ..• , • • • • . • • • • • . • • • . • . • • • • • . 19 Town· Lands sold . • • • • • . • . • . • • • • • . • • • . • . • • • . • . • . 20 'fown Lands sold for Cash under " The Waste Lands Act" ·• . • • • • • • • • • • . • . 21 Deposits forfeited- on ditto •.••• , . • . • • • . • • . • • • . • . • . .. • . • . • • . • 40 Town Lands sold on Credit . • • • . • . • • • • . • • . • • • • . • . • . • . • • • • 42 Agricultural Lands sold for Cash, under 18th Sect. of" The Waste Lands Act". 45 Ditto on Credit, ditto .•.•• , • . • • • • . • . • . • . • • • • • . • . • • • . • • • • . • . 46 Ditto for Cash, under 19th Sect. of" The Waste Lands Act" • . • . 49 Ditto on Credit, ditto . • . • • • • • • • • • . • . • . • . • . • • • • • -
Assessment of Juvenile Eel Resources in South Eastern Australia and Associated Development of Intensive Eel Farming for Local Production
ASSESSMENT OF JUVENILE EEL RESOURCES IN SOUTH EASTERN AUSTRALIA AND ASSOCIATED DEVELOPMENT OF INTENSIVE EEL FARMING FOR LOCAL PRODUCTION G J. Gooley, L. J. McKinnon, B. A. Ingram, B. Larkin, R.O. Collins and S.S. de Silva. Final Report FRDC Project No 94/067 FI SHERIE S RESEARCH & DEVELOPMENT Natural Resources CORPOR ATIO N and Environment AGRICULTURE RESOURCES COIISERVAT/Otl ASSESSMENT OF JUVENILE EEL RESOURCES IN SOUTH-EASTERN AUSTRALIA AND ASSOCIATED DEVELOPMENT OF INTENSIVE EEL FARMING FOR LOCAL PRODUCTION G.J Gooley, L.J. McKinnon, B.A. Ingram, B.J. Larkin, R.O. Collins and S.S. De Silva Final Report FRDC Project No 94/067 ISBN 0731143787 Marine and Freshwater Resources Institute, 1999. Copies of this document are available from: Marine and Freshwater Resources Institute Private Bag 20 Alexandra. VIC. 3714. AUSTRALIA.. This publication may be of assistance to you but the State of Victoria and its officers do not guarantee that the publication is without flaw of any kind or is wholly appropriate for your particular purposes and therefore disclaims all liability for error, loss or other consequence which may arise from you relying on any information in this publication. 1 TABLE OF CONTENTS 1 TABLE OF CONTENTS...............................................................................................................................i 2 ACKNOWLEDGMENTS.......................................................................................................................... iii 3 NON-TECHNICAL SUMMARY................................................................................................................! -
B South Esk Catchment
B SOUTH ESK CATCHMENT 1.0 Hydrology The South Esk River rises in the North Eastern highlands near Mathinna initially travelling southwards before passing through the Fingal Valley and finally turning northwards and draining into the Tamar River estuary at Launceston. Upstream of the confluences with the Macquarie and Meander rivers the major tributaries include the Break O’Day, St Pauls and Nile rivers. Many smaller streams contribute water to the South Esk mainly from the North- East highlands around Ben Lomond (eg Storeys Creek and Buffalo Brook). 1.1 Historical Background Measurement of river heights in the South Esk River has a long history. Unfortunately these measurements are not always useful indicators of flow due to changes in the channel such as growth and destruction of vegetation, aggradation and scouring of river beds, etc. Such changes provide unstable relationships between gauge height and flow. Nevertheless, many of the gauge height stations continue to be maintained and in many instances are the major tools used for flood warning. The South Esk is a relatively flat river for much of its length and there are often large areas where natural backwaters occur. There are therefore limited opportunities along the river to collect stream flow information and it was not until the 1950's that two reasonable locations were instrumented. These two sites - one at Llewellyn and the other at Perth - have collected streamflow information for around 40 years and are therefore invaluable in assessing the water yields, flood and drought behaviour of the river system. Unfortunately the early record at Llewellyn (prior to 1973) is subject to a major review by the Hydro-Electric Commission and could not be used for this study. -
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June 1946 MEM. NAT. Mus. V1cT., 14, PT. 2, 1946. https://doi.org/10.24199/j.mmv.1946.14.06 THE SUNKLANDS OF PORT PHILLIP BAY AND BASS STRAIT By R. A. Keble, F.G.S., Palaeontologist, National Jiiiseurn of Victoria. Figs. 1-16. (Received for publication 18th l\fay, 1945) The floors of Port Phillip Bay and Bass Strait were formerly portions of a continuous land surface joining Victoria with Tasmania. This land surface was drained by a river system of which the Riv-er Y arra was part, and was intersected by two orogenic ridges, the Bassian and King Island ridges, near its eastern and western margins respectively. \Vith progressive subsidence and eustatic adjustment, these ridges became land bridges and the main route for the migration of the flora and fauna. At present, their former trend is indicated by the chains of islands in Bass Strait and the shallower portions of the Strait. The history of the development of the River Yarra is largely that of the former land surface and the King Island land bridge, and is the main theme for this discussion. The Yarra River was developed, for the most part, during the Pleistocene or Ice Age. In Tasmania, there is direct evidence of the Ice Age in the form of U-shaped valleys, raised beaches, strandlines, and river terraces, but in Victoria the effects of glaciation are less apparent. A correlation of the Victorian with the Tasmanian deposits and land forms, and, incidentally, with the European and American, can only be obtained by ascertaining the conditions of sedimentation and accumulation of such deposits in Victoria, as can be seen at the surface1 or as have been revealed by bores, particularly those on the N epean Peninsula; by observing the succession of river terraces along the Maribyrnong River; and by reconstructing the floor of Port Phillip Bay, King Bay, and Bass Strait, and interpreting the submerged land forms revealed by the bathymetrical contours. -
Kanamaluka Tamar River Headwaters Natural Restoration Plan 2021 - 2025
kanamaluka Tamar River Headwaters Natural Restoration Plan 2021 - 2025 Tamar River Headwaters Natural Restoration Plan 1 This Restoration Plan. The Tamar Yacht Club, on behalf of other stakeholders, has developed this restoration Definition - The Headwaters of the Tamar plan based on the best available engineering River (kanamaluka) are defined by the area of and academic bodies of work that primarily the confluence of the South Esk with the focus on a return to the natural conditions of Tamar, forming the Yacht Basin from the the Tamar River (kanamaluka) headwaters that Kings Bridge to the North Esk confluence as existed prior to the construction of the well as the contiguous zone known as Home Trevallyn Dam and Power Station. Reach from Home Point to Ti Tree Bend. Tamar River Headwaters Natural Restoration Plan 2 The Tamar Yacht Club (TYC) is one of the oldest Yacht Clubs in the southern hemisphere and is amongst the longest existing landholders in the headwaters of the Tamar River. POSITION STATEMENT 1. The TYC has taken the decision to enter and lead the community debate regarding the future of the Tamar River. 2. The TYC will now focus on the overdue return of the Tamar River to its fully natural state as existed prior to the hydro development. Tamar River Headwaters Natural Restoration Plan 3 OUR PLAN The TYC Plan is to facilitate the first step in the restoration of the Tamar River headwaters area to its natural state, as existed prior to the Trevallyn hydro development. This Plan... 3. Is proposed following the public announcement that the Tasmanian and 1. -
191 Launceston Tasmania 7250 State Secretary: [email protected] Journal Editors: [email protected] Home Page
Tasmanian Family History Society Inc. PO Box 191 Launceston Tasmania 7250 State Secretary: [email protected] Journal Editors: [email protected] Home Page: http://www.tasfhs.org Patron: Dr Alison Alexander Fellows: Dr Neil Chick, David Harris and Denise McNeice Executive: President Anita Swan (03) 6326 5778 Vice President Maurice Appleyard (03) 6248 4229 Vice President Peter Cocker (03) 6435 4103 State Secretary Muriel Bissett (03) 6344 4034 State Treasurer Betty Bissett (03) 6344 4034 Committee: Judy Cocker Jim Rouse Kerrie Blyth Brian Hortle Leo Prior John Gillham Libby Gillham Helen Stuart Judith Whish-Wilson By-laws Officer Denise McNeice (03) 6228 3564 Assistant By-laws Officer Maurice Appleyard (03) 6248 4229 Webmaster Robert Tanner (03) 6231 0794 Journal Editors Anita Swan (03) 6326 5778 Betty Bissett (03) 6344 4034 LWFHA Coordinator Anita Swan (03) 6394 8456 Members’ Interests Compiler John Gillham (03) 6239 6529 Membership Registrar Muriel Bissett (03) 6344 4034 Publications Coordinator Denise McNeice (03) 6228 3564 Public Officer Denise McNeice (03) 6228 3564 State Sales Officer Betty Bissett (03) 6344 4034 Branches of the Society Burnie: PO Box 748 Burnie Tasmania 7320 [email protected] Devonport: PO Box 587 Devonport Tasmania 7310 [email protected] Hobart: PO Box 326 Rosny Park Tasmania 7018 [email protected] Huon: PO Box 117 Huonville Tasmania 7109 [email protected] Launceston: PO Box 1290 Launceston Tasmania 7250 [email protected] Volume 29 Number 1 June 2008 ISSN 0159 0677 Contents Editorial .................................................................................................................. -
The Sum of Us
The Sum of Us The Sum Of Us | 1 4 | The Sum Of Us Jeanneret The Sum Of Us | 5 Janneret Jeannerat Jeannerot Jeannotat, Jeannottat Jeanneney Jeannenez Jeannesson, Jonneret Johannot Johannes Jeanneret- Gris Jeanneret-Grosjean Jeanjean Jeanpierre Jampierre Jeanperrin Jeangirard Jeanjaquet Jeanhenry Jeanclaude Jeanrenaud Jean-Gueninn Jeanguenin Jeanguenat Jean-Richard JeanRichard Jeanrichard Jean-Mairet Jeanmairet Jeanneret Jeanmonod Jeanmonnot Jeangros Jeangroz Jeanningros Grosjean Grandjean Petitjean Jean-Cartier Jean-Quartier Jeanquartier Jeanbourquin Jeanbourgquin Jean- Prêtre Jeanmaire Jeanclerc Jeancier Jeanfavre Jeandrevin Jeanbrun Jeandroz Jeandupeux Jeanloz Jehanneret Jonerey Jennerick Generette Jeneret Genrett Janerette 6 | The Sum Of Us HISTORY OF THE FAMILY JEANNERET ORIGINATING FROM LE LOCLE SWITZERLAND Genealogical search, or more exactly the search of the surname can hardly be made beyond the 15th century. At that time the shortage of personnel, the shortage of documentation and the lack of their text do not make it possible to establish with certainty affiliation. One must be often satisfied with probability and limited data. During the 14th Century, amongst subjects of the Princes of Valangin we find in year 1350, the name of Yermin which becomes Small Jehan then Jehanneret then Jeanneret. In 1447, the population of valley-I-Ruz becoming more numerous, the lord of Valangin supports the colonists who from there in the High Jura will call themselves as clearer- ploughman. At the 14th Century they are established in Segue, with the Between-two-Mounts, Locle the Lime of Bottoms. A family of the name of Jeanneret is installed with the hamlet of Crozot on Locle, an official letter going back to 1612, addressed to Jean-Jacques Jeanneret, Bourgois of Valangin. -
A City on a Floodplain Protecting Launceston from a 1 in 200 Ari Flood
LAUNCESTON - A CITY ON A FLOODPLAIN PROTECTING LAUNCESTON FROM A 1 IN 200 ARI FLOOD A Fullard 1 1Launceston Flood Authority, Launceston, TAS Introduction Launceston is a city of some 70,000 people, with a portion of its CBD and major northern suburb, Invermay, situated on the natural floodplain at the confluence of the Tamar River estuary and the North and South Esk Rivers. Much of Invermay is below the high tide level and is reliant upon levees for its sustainability. Refer Figure 1 for extent of Launceston's flooding if levee were not present. The Invermay area is now considered a desirable inner city suburb populated by a large number of young and middle-aged people indicating its potential for growth. Much of Launceston's cultural centre, including Launceston's Museum, Aurora Sports Stadium, and campuses of the University of Tasmania, are located there. The flood prone area of the CBD is a mixture of residential and commercial enterprises and is home to Boags Brewery and historic buildings associated with Launceston's port history. Launceston has been subject to 35 significant floods since records began, with the 1929 flood reputedly being the worst, displacing over 4000 residents and rendering many buildings uninhabitable. Much of the lower CBD was also inundated during this flood. Two floods in 1852 and 1863 are recorded to be higher than the 1929 flood; however the 1929 flood had the most severe consequences and is etched into the history of Launceston. Figure 1 - Launceston's CBD and suburb of Invermay inundation area without levees. 1 Following a significant design report by the Launceston Flood Protection Authority in 1959 (Munro, 1959), a levee system was constructed during the following decade to protect the CBD and Invermay. -
Tracer Analysis of Sediment Redistribution of Tamar AMC Search and Estuary for Launceston Flood Authority ETS Worldwide Ltd
Thesis: Strategies for Sustainable Morphological Remediation of the Tamar River Estuary and other Similarly Degraded Estuaries by Ian M Kidd, BSc, Grad. Dip. of Computing Institute for Marine and Antarctic Studies Submitted in fulfilment of the requirements for the degree of Doctor of Philosophy University of Tasmania October 2016 Table of Contents Abstract ………………………………………………………………………….…...I General Declarations………….……………………….………………………..……II Acknowledgements………………………………………………………………….III List of Figures……………………………………………………………………….IV List of Tables……………………………….……………………………………..…V List of symbols and abbreviations used in the thesis……………….………………VI Chapter One: Introduction 1. Research Question………………………………………………………….……1 1.1 Background………………………………………………………………1 2. Literature review………………………………………………………………...1 2.1 Definition and classification of estuaries……………………………...1 2.2 Water circulation…………………….………………………………... 2 2.2.1 Classification of estuaries by circulation mode………………..3 2.3 Tides, tidal constituents and harmonics……………………………….3 2.3.1Tidal constituent analysis……………………………………...4 2.4 Sediment dynamics……………………………………………..………..4 2.4.1 Turbidity maximum, flocculation……….……………………..4 2.4.2 Tidal asymmetry……………………………….………………4 2.4.3 Sediment transport……………………………….……………5 2.4.4 Tidal asymmetry ratio…………………………………………7 2.4.5 Net sediment flux…………………….………………………..7 2.4.6 Sediment supply……………..……..……………………….....9 2.4.7 Sediment management………………...………………………9 Dredging……………………………..…………………………9 Silt raking………………..……………………………………10 Catchment management……………….……………….…..…10 -
Lands of Tasmania. Returns
(No. 30.) 18 6 2 . .T A S, M A N I A. ' • \.. ,,., ••'l..- .• , d. t.,. .~ !.. : !, : :_ . " , '-• tt' .1 •• ~- LANDS OF TASMANIA. RETURNS. Laid upon the Table by Mr. Henty, and ordered by the Council to be printed, _ 7 August, 1862. CORRIGENDA. In Preface, line 5 from the top, for "since little influence," read "eome little influence;" :iud in the first note, line 2, for "1857," read, "1856." In page 91, seventh entry in the fifth column,_for "4001" read," 4000." TABLE OF CONTENTS. FAGE PREFACE. LAND GAZETTE •••••••••••••••••••••••••••••••••••••••••••••••••• ~ • • 1 Area of Tasmania, with alienated and unalienate<l Lands . • . · 33 Population of Tasmania • • . • . • . • • • • • • • • • • . • . • • • • . • . • • • • • . 33 Ditto of Towns . • • • • • . • • • • . .. • . • • • • • • • . • . • . • . 34 Country Lands g:ranted and solrl since 1804 .•••.•.•••....••••..... : . • . • 35 Town Lands sold • • • • . • . • . • . • • . • • • . • • • . • . • • • • • . 36 Town Lands sold for Cash under "The Waste Lands Act." .••..•.•·••..••.•.• 37 Deposits forfeited on ditto...... • . • • • • • • . • . • . • • • • • . • . • • . • • . • . • 54 Town Lands sold on Credit .• ·.•..•. ; • . • • . • • • . • . • • 56 Agricultural Lands sold for Cash, under 18th Sect. of" The Waste Lands Act".. 59 Ditto on Credit, ditto . • . • • . • • • • • • . • . • . • • . • • 60 Ditto for Cash, under 19th Sect. of "The Waste Lands Act" ·.•.•....••• 62. Ditto on Cr~dit, ditto . • . • . • • • • • •. • • • • . • . • • • . • • • • . 64 Ditto for Cash at Public Auction • • • • -
Tamar Valley
TAMAR VALLEY This route explores the majestic Tamar START: Launceston EXPLORE: Tasmania’s north River from Launceston to Bass Strait as it DURATION: 1-3 days meanders for nearly 60 kms through the NATIONAL PARKS ON THIS ROUTE: heart of vineyard country past orchards, > Narantawpu National Park scenic pastures and forests. From here If arriving by plane, the drive into Launceston will give you an insight into the Valley’s focus on great produce, you’ll travel east to Narawntapu National taking you close by famous vineyards, including Josef Chromy, Jingler’s Creek and Sharman’s North Park for panoramic views of Badger Esk Vineyard, plus Evandale Estate Olives and the Head and Bass Strait. Tasmanian Gourmet Sauce Company. If you’re arriving by ship from Melbourne, you can join the route at Exeter by taking the Frankford Highway from Devonport. LEG TIME / DISTANCE Launceston to George Town 39 min / 51 km George Town to Beauty Point 36 min / 41 km Beauty Point to Launceston 47 min / 48 km Launceston - George Town > Depart Launceston and take a 15 minute scenic drive through the beautiful Tamar Valley and turn to Hillwood. Visit the Meander Valley Dairy and sample beautiful cheeses, cream and strawberries. > Down the road is the Hillwood Berry Farm where you can pick your own, pick up some jam, quince, liqueur or wine just to name a few, as well as their beauty and relaxation products. > Fruit can be bought from Millers Orchards on your Hillwood travels. Famous for their cherries, apricots, apples, peaches and more, your providore experience has just begun.