Water Quality of Rivers in the North Esk Catchment

Total Page:16

File Type:pdf, Size:1020Kb

Water Quality of Rivers in the North Esk Catchment Water Quality of Rivers in the North Esk Catchment A Report Forming Part of the Requirements for State of Rivers Reporting PART 1 Authors; Katrina Berry 1 Christopher Bobbi 2 Abigail Foley 1 Water Assessment and Planning Branch DPIWE. 1 Water Assessment and Planning Branch, Water Resources Division. 2 Environmental and Resource Analysis, Hydro Tasmania. December 2003 Copyright Notice: Material contained in the report provided is subject to Australian copyright law. Other than in accordance with the Copyright Act 1968 of the Commonwealth Parliament, no part of this report may, in any form or by any means, be reproduced, transmitted or used. This report cannot be redistributed for any commercial purpose whatsoever, or distributed to a third party for such purpose, without prior written permission being sought from the Department of Primary Industries, Water and Environment, on behalf of the Crown in Right of the State of Tasmania. Disclaimer: Whilst DPIWE has made every attempt to ensure the accuracy and reliability of the information and data provided, it is the responsibility of the data user to make their own decisions about the accuracy, currency, reliability and correctness of information provided. The Department of Primary Industries, Water and Environment, its employees and agents, and the Crown in the Right of the State of Tasmania do not accept any liability for any damage caused by, or economic loss arising from, reliance on this information. Preferred Citation: DPIWE (2003) State of Rivers Report for the North Esk Catchment. Water Assessment and Planning Branch, Department of Primary Industries, Water and Environment, Hobart. Technical Report No. WAP 03/06 ISSN: 1449-5996 The Department of Primary Industries, Water and Environment The Department of Primary Industries, Water and Environment provides leadership in the sustainable management and development of Tasmania’s resources. The Mission of the Department is to advance Tasmania’s prosperity through the sustainable development of our natural resources and the conservation of our natural and cultural heritage for the future. The Water Resources Division provides a focus for water management and water development in Tasmania through a diverse range of functions including the design of policy and regulatory frameworks to ensure sustainable use of the surface water and groundwater resources; monitoring, assessment and reporting on the condition of the State’s freshwater resources; facilitation of infrastructure development projects to ensure the efficient and sustainable supply of water; and implementation of the Water Management Act 1999, related legislation and the State Water Development Plan. ii State of Rivers Water Quality of the North Esk Catchment TABLE OF CONTENTS EXECUTIVE SUMMARY .......................................................................................................V A GLOSSARY OF TERMS ..................................................................................................VII Units and Conversions........................................................................................................................................ ix Acronyms............................................................................................................................................................. ix B SUMMARY OF NATIONAL GUIDELINES FOR WATER QUALITY.......................................................... x Primary contact ......................................................................................................................................................... xi Secondary contact...................................................................................................................................................... xi WATER QUALITY OF THE NORTH ESK CATCHMENT 1 1 HISTORICAL AND OTHER DATA .................................................................................... 1 1.1 Chimney Saddle & Distillery Creek Water Quality ......................................................................................... 1 1.2 Tamar River Sediment Study ............................................................................................................................. 5 1.3 Launceston City Council monitoring................................................................................................................. 7 1.3.1 Time series Analysis……………………………………………………………………………………….. 7 1.4 Analysis of Water Quality in Response to Forest Harvesting in the Musselboro Creek Catchment. ........ 10 1.5Historical Data from the State database HYDROL.......................................................................................... 11 1.6 Launceston Waterwatch – St Patricks River Monitoring .............................................................................. 16 2 CURRENT STUDY........................................................................................................... 20 2.1 Physico-chemical properties ............................................................................................................................. 23 2.1.1Water Temperature…………………………………………………………………………………………. 23 2.1.2 In-stream pH……………………………………………………………………………………………….. 25 2.1.3 Electrical Conductivity……………………………………………………………………………………. 26 2.1.4 Turbidity……………………………………………………………………………………………………. 28 2.1.5 Dissolved Oxygen…………………………………………………………………………………………..30 2.2 General Ionic Composition ............................................................................................................................... 33 2.2.1 Sulphate……………………………………………………………………………………………………...36 2.2.2 Apparent Colour…………………………………………………………………………………………….36 2.2.3 Suspended Solids…………………………………………………………………………………………...37 2.3 Nutrients............................................................................................................................................................. 38 2.3.1 Total Nitrogen……………………………………………………………………………………………….38 2.3.2 Nitrate Nitrogen…………………………………………………………………………………………….39 2.3.3 Ammonia Nitrogen………………………………………………………………………………………….41 2.3.4 Phosphorus………………………………………………………………………………………………….42 2.4 Catchment Surveys............................................................................................................................................. 44 2.4.3 Catchment Survey – Total Nitrogen………………………………………………………………………..44 2.4.4 Catchment Survey – Total Phosphorus……………………………………………………………………..47 2.4.2 Catchment Survey – Heavy Metals…………………………………………………………………………51 2.4.5 Catchment Survey – Bacteria………………………………………………………………………………..57 2.5 Nutrient Load Estimates .................................................................................................................................... 61 2.5.1 North Esk at Ballroom……………………………………………………………………………………... 61 2.5.2 North Esk at Corra Linn……………………………………………………………………………………. 66 2.5.3 ‘Snapshot’ Flood Sampling………………………………………………………………………………….70 2.6 Diurnal Water Quality Variations .................................................................................................................... 73 2.6.1 Temperature…………………………………………………………………………………………………73 iii State of Rivers Water Quality of the North Esk Catchment 2.6.2 Dissolved oxygen……………………………………………………………………………………………75 2.6.3 pH……………………………………………………………………………………………………………79 2.6.3 Conductivity…………………………………………………………………………………………………81 3 SUMMARY AND COMMENTS ........................................................................................ 83 4 REFERENCES................................................................................................................. 86 APPENDIX 1. ....................................................................................................................... 88 iv State of Rivers Water Quality of the North Esk Catchment Executive Summary The North Esk Catchment is used extensively for agriculture and forestry and provides domestic water supply for Launceston. The catchment is approximately 1,065 km² and is composed of two major drainage systems, the North Esk River and the St Patricks River. The North Esk River originates in the foothills of the Ben Nevis and Ben Lomond Ranges travelling south though forestry plantations until it reaches the confluence of the Ford River where it turns west draining dispersed agricultural pastures. The smaller tributaries of Burns Creek, Musselboro Creek, Weavers Creek, Pig Run Creek and River O’Plain Creek contribute flow to the North Esk River before it reaches the confluence of the St Patricks River where flow dramatically increases. The offtake for the Esk Waters Chimney Hill Water Treatment Plant is located upstream of the confluence with the St Patricks River. The North Esk River then continues in a westerly direction through a predominantly agricultural landscape receiving flows from Roses Rivulet. As the North Esk continues west through the city of Launceston it receives flow from the partially urbanised Distillery Creek region and the heavily urbanised region of Kings Meadows Rivulet before it discharges into the Tamar River. The head waters f the St Patricks River originate between the foot hills of Mount Maurice and Ben Nevis. The St Patricks River flows through a landscape dominated by forestry operations and dispersed grazing picking up contributing flows from Camden Rivulet. Travelling in a north westerly direction the river hooks around the foothills of Mount Barrow and flows in a south westerly direction through primarily
Recommended publications
  • 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.
    [Show full text]
  • 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 . • . • • • • • • • • • . • . • . • . • . • • • • •
    [Show full text]
  • 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................................................................................................................!
    [Show full text]
  • 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.
    [Show full text]
  • Download Full Article 2.9MB .Pdf File
    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.
    [Show full text]
  • Water Management Plan Meeti
    Water Management Planning Report Series Consultative Group Water Resources Information Package for the South Esk Catchment (above Macquarie) Water Management Plan Meeting Two August 2008 Water Resources Information Package for the South Esk River Catchment Water Management Plan Copyright Notice Material contained in the report provided is subject to Australian copyright law. Other than in accordance with the Copyright Act 1968 of the Commonwealth Parliament, no part of this report may, in any form or by any means, be reproduced, transmitted or used. This report cannot be redistributed for any commercial purpose whatsoever, or distributed to a third party for such purpose, without prior written permission being sought from the Department of Primary Industries and Water, on behalf of the Crown in Right of the State of Tasmania. Disclaimer Whilst DPIW has made every attempt to ensure the accuracy and reliability of the information and data provided, it is the responsibility of the data user to make their own decisions about the accuracy, currency, reliability and correctness of information provided. The Department of Primary Industries and Water, its employees and agents, and the Crown in the Right of the State of Tasmania do not accept any liability for any damage caused by, or economic loss arising from, reliance on this information. Preferred Citation DPIW (2008). Water Resources Information Package for the South Esk catchment (above Macquarie) Water Management Plan Technical Report No. WMP 08/03. Water Resources Division, Department of Primary Industries and Water, Hobart. The Department of Primary Industries and Water (DPIW) The Department of Primary Industries and Water provides leadership in the sustainable management and development of Tasmania’s natural resources.
    [Show full text]
  • 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.
    [Show full text]
  • 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 ..................................................................................................................
    [Show full text]
  • Listing Statement for Epacris Exserta (South Esk Heath) Ep Acris Exserta
    Listing Statement for Epacris exserta (south esk heath) Ep acris exserta south esk heath T A S M A N I A N T H R E A T E N E D S P E C I E S L I S T I N G S T A T E M E N T Image by Oberon Carter Scientific name: Epacris exserta R. Br., Prodr. 551 (1810) Common name: south esk heath (Wapstra et al. 2005) Group: vascular plant, dicotyledon, family Epacridaceae Status: Threatened Species Protection Act 1995 : endangered Environment Protection and Biodiversity Conservation Act 1999 : Endangered Distribution: Endemic status: Endemic to Tasmania Tasmanian NRM Region: North Figure 1 . The distribution of Epacris exserta Plate 1. Epacris exserta : flower detail (image by Oberon Carter) 1 Threatened Species Section – Department of Primary Industries, Parks, Water and Environment Listing Statement for Epacris exserta (south esk heath) IDENTIFICATION AND ECOLOGY [description from Crowden 2003] Epacris exserta is a woody shrub in the Epacridaceae family. It is a riparian species up Taxonomic issues to 1.5 m tall that is restricted to three rivers in The taxon referred to as Epacris exserta in the Tasmania’s north. Epacris exserta is best Recovery Plan – Tasmanian Forest Epacrids 1999– identified during its flowering period, 2004 (Keith 1998) consisted of ten September to late October. subpopulations in the north of the State. Epacris Known pollinators of Epacris taxa include a exserta as understood here ( sensu Crowden variety of adult carrion flies from the families 2003), includes only three of those Tabanidae, Muscidae and Calliphoridae (Keith subpopulations, the remainder being 1998).
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • In and Around Launceston Walks, Runs and Rides for All Ages
    Trails in and around Launceston Walks, runs and rides for all ages Developed by the Launceston City Council for locals and visitors, these trails aim to facilitate active and healthy lifestyles while you discover the beautiful city of Launceston. Grouped by colour, many of these trails are in the same area or can be linked together. TRAIL LENGTH PAGE River Edge Trail 1.8km 5 West Tamar Trail 2.1km 6 Cataract Walk 1.0km 7 Zig Zag Track 1.0km 8 First Basin Loop 900m 9 Duck Reach Trail 4.5km 10 Hardwicke Street Trail 2.2km 11 Dalrymple Street Trail 2.1km 12 Carr Villa Trail 3.1km 13 Youngtown Trail 2.0km 14 Glenwood Trail 2.5km 15 Kings Meadows Trail 900m 16 Punchbowl Trail 1.2km 17 North Esk Trail 2.2km 18 Henry Street Trail 1.5km 19 Black Bridge Trail 1.0km 20 Inveresk Trail 2.8km 21 Between Two Bridges Trail 500m 22 University Trail 3.9km 23 Heritage Forest Trail 2.9km 24 Rocherlea Old Rail Trail 3.2km 25 Newnham Trail 1.2km 26 Lilydale Falls Trail 500m 27 Merthyr Park Trail 2.6km 28 Waverley Lake Trail 1.3km 29 Trails Location Map 30-31 Welcome to the Launceston Trails Guide This guide is designed to help you navigate your way around Launceston’s Trail Network. The trails range from 500 metres to 4 kilometres in length. Nearby trails are also listed as they can be joined together. Each page features a new trail with a map and details. There is an overview map at the end of the Guide, which can also help you plan longer walks and rides by joining several trails.
    [Show full text]