Thomson River Environmental Flows and Management Review Flow Recommendations Paper
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Thomson River-Rainbow Creek
WEST GIPPSLAND CATCHMENT MANAGEMENT AUTHORITY Thomson River-Rainbow Creek Waterway Management Plan 2020 Acknowledgements The Thomson Rainbow Waterway Management Plan was co-developed through the collective effort of a number of individuals and organisations, including: • Project Working Group members: Cr. Carolyn Crossley (Chair), Trevor Astbury, Norm Drew, Beverly Hookey, Merv Whittaker, Phil Taylor, Malcolm Stewart and representatives from Gippsland Water, Wellington Shire Council, Gunaikurnai Land and Waters Aboriginal Corporation, Southern Rural Water and the West Gippsland Catchment Management Authority • Project Steering Committee members: Southern Rural Water and the West Gippsland Catchment Management Authority • Project Team: Natural Decisions (Geoff Park and Anna Roberts), Blue Sense Consulting (Michelle Dickson), Professor Ian Rutherfurd, and Water Technology (consulting support) • Interested community members and landholders who participated in community forums and the supporting studies for this plan. Acknowledgement of Country The West Gippsland Catchment Management Authority would like to acknowledge and pay our respects to the Traditional Land Owners of the Thomson – Rainbow Creek area, the Gunaikurnai people. We also recognise the contribution of Aboriginal and Torres Strait Islander people and organisations in land and natural resource management. Disclaimer This publication may be of assistance to you but the West Gippsland Catchment Management Authority (WGCMA) and its consultants and employees do not guarantee that the publication is without flaw of any kind or is wholly appropriate for your particular purpose. The mapping and modelling outputs represented in this Plan are not definitive and provided for indicative purposes only. It therefore disclaims all liability for any error, loss or other consequence which may arise from you relying on any information in this publication. -
Rivers and Streams Special Investigation Final Recommendations
LAND CONSERVATION COUNCIL RIVERS AND STREAMS SPECIAL INVESTIGATION FINAL RECOMMENDATIONS June 1991 This text is a facsimile of the former Land Conservation Council’s Rivers and Streams Special Investigation Final Recommendations. It has been edited to incorporate Government decisions on the recommendations made by Order in Council dated 7 July 1992, and subsequent formal amendments. Added text is shown underlined; deleted text is shown struck through. Annotations [in brackets] explain the origins of the changes. MEMBERS OF THE LAND CONSERVATION COUNCIL D.H.F. Scott, B.A. (Chairman) R.W. Campbell, B.Vet.Sc., M.B.A.; Director - Natural Resource Systems, Department of Conservation and Environment (Deputy Chairman) D.M. Calder, M.Sc., Ph.D., M.I.Biol. W.A. Chamley, B.Sc., D.Phil.; Director - Fisheries Management, Department of Conservation and Environment S.M. Ferguson, M.B.E. M.D.A. Gregson, E.D., M.A.F., Aus.I.M.M.; General Manager - Minerals, Department of Manufacturing and Industry Development A.E.K. Hingston, B.Behav.Sc., M.Env.Stud., Cert.Hort. P. Jerome, B.A., Dip.T.R.P., M.A.; Director - Regional Planning, Department of Planning and Housing M.N. Kinsella, B.Ag.Sc., M.Sci., F.A.I.A.S.; Manager - Quarantine and Inspection Services, Department of Agriculture K.J. Langford, B.Eng.(Ag)., Ph.D , General Manager - Rural Water Commission R.D. Malcolmson, M.B.E., B.Sc., F.A.I.M., M.I.P.M.A., M.Inst.P., M.A.I.P. D.S. Saunders, B.Agr.Sc., M.A.I.A.S.; Director - National Parks and Public Land, Department of Conservation and Environment K.J. -
Environmental Condition of Rivers and Streams in the Latrobe, Thomson and Avon Catchments
ENVIRONMENTAL CONDITION OF RIVERS AND STREAMS IN THE LATROBE, THOMSON AND AVON CATCHMENTS Publication 832 March 2002 1 INTRODUCTION activities have contributed to a significant change in the quantity and quality of water delivered to Lake This publication provides an overview of the Wellington and there is a significant amount of environmental condition of the rivers and streams in public concern regarding impacts on the health of the Latrobe, Thomson and Avon catchments1 (Figure the Gippsland Lakes. 1). The Latrobe and Thomson river systems, for The Latrobe, Thomson and Avon catchments contain example, contribute approximately twice the some of Victoria’s most significant river systems. nutrient inputs to the Gippsland Lakes than all other Located in the Gippsland region of Victoria, these riverine inputs. The most significant nutrient loading three river systems form the total catchment of Lake is associated with high flow events and reflects the Wellington, the western-most of the Gippsland increased surface runoff and erosion caused Lakes. The demands on these freshwater resources through land clearance and urbanisation. are considerable. Australia’s largest pulp and paper It is commonly agreed that the only long-term mill, most of the State’s power industry, much of solution for improving the condition of Lake Melbourne’s water supply and the State’s second Wellington is to significantly reduce the nutrient largest irrigation district fall within their catchment loads from the Latrobe and Thomson river systems. boundaries. Restoration of the catchments to a more sustainable Much change has occurred in these catchments land use, revegetating riparian zones and reducing since early settlement. -
Heritage Rivers Act 1992 No
Version No. 014 Heritage Rivers Act 1992 No. 36 of 1992 Version incorporating amendments as at 7 December 2007 TABLE OF PROVISIONS Section Page 1 Purpose 1 2 Commencement 1 3 Definitions 1 4 Crown to be bound 4 5 Heritage river areas 4 6 Natural catchment areas 4 7 Powers and duties of managing authorities 4 8 Management plans 5 8A Disallowance of management plan or part of a management plan 7 8B Effect of disallowance of management plan or part of a management plan 8 8C Notice of disallowance of management plan or part of a management plan 8 9 Contents of management plans 8 10 Land and water uses which are not permitted in heritage river areas 8 11 Specific land and water uses for particular heritage river areas 9 12 Land and water uses which are not permitted in natural catchment areas 9 13 Specific land and water uses for particular natural catchment areas 10 14 Public land in a heritage river area or natural catchment area is not to be disposed of 11 15 Act to prevail over inconsistent provisions 11 16 Managing authority may act in an emergency 11 17 Power to enter into agreements 12 18 Regulations 12 19–21 Repealed 13 22 Transitional provision 13 23 Further transitional and savings provisions 14 __________________ i Section Page SCHEDULES 15 SCHEDULE 1—Heritage River Areas 15 SCHEDULE 2—Natural Catchment Areas 21 SCHEDULE 3—Restricted Land and Water Uses in Heritage River Areas 25 SCHEDULE 4—Specific Land and Water Uses for Particular Heritage River Areas 27 SCHEDULE 5—Specific Land and Water Uses for Particular Natural Catchment Areas 30 ═══════════════ ENDNOTES 31 1. -
Walhalla Visitor Guide 3
WALHALLA Visitor Guide visitwalhalla.com Australia’S valley Of the gods HIDDEN IN A DEEP VALLEy IN THE VICTORIAN ALPS, WALHALLA HISTORIC TOWNSHIP WAS A BOOM TOWN Of THE 1880S THAT WENT BUST IN THE EARLy 1900S AND WAS DESERTED fOR MOST Of THE 20TH CENTURy. Just a short drive east of Melbourne you’ll Exotic trees and cute miner’s cottages line the discover a village that time has passed by. meandering street and twisting creek in the From 1863 until 1914, Walhalla was one of the steep valley. Walhalla’s unique topography in a richest gold areas in Australia with a population narrow mountain gorge meant that the early of over 3,000 people. There were 10 hotels, townsfolk needed to think vertically. 7 churches, several dance halls, a school with Walhalla’s iconic cemetery clings to the side of more than 500 students and over 30 shops. the hill at a 45 degree angle and the slopes are Walhalla’s picturesque location in the Gippsland dotted with cottages built on narrow ledges mountains combines the wild Australian bush cut into the steep hillsides. When gold mining environment with a colonial style reminiscent became unprofitable in 1914 and the mines of the gold era. closed, Walhalla’s decline was rapid. 2 www.visitwalhalla.com WALHALLA VISITOR GUIDE 3 things to see and do Most of the houses and buildings were pulled down and shipped to other towns LONG TUNNEL EXTENDED on the newly opened railway, while GOLD MINE others were simply abandoned. Discover a golden past on an informative 45 minute tour of an original gold mine The structures that remained were with a local guide. -
And Hinterland LANDSCAPE PRIORITY AREA
GIPPSLAND LAKES and Hinterland LANDSCAPE PRIORITY AREA Photo: The Perry River 31 GIPPSLAND LAKES AND HINTERLAND Gippsland Lakes and Hinterland AQUIFER ASSET VALUES, CONDITION AND KEY THREATS Figure 25: Gippsland Lakes and Hinterland Landscape Priority Area Aquifer Asset Shallow Aquifer The Shallow Alluvial aquifer includes the Denison and Wa De Lock Groundwater Management Areas. It has high Figure 24: Gippsland Lakes and Hinterland Landscape connectivity to surface water systems including the provision Priority Area location of base flow to rivers, such as the Avon, Thomson and Macalister. The aquifer contributes to the condition of other Groundwater Dependent Ecosystems including wetlands, The Gippsland Lakes and Hinterland landscape priority area estuarine environments and terrestrial flora. The aquifer is characterised by the iconic Gippsland Lakes and wetlands is also a very important resource for domestic, livestock, Ramsar site. The Gippsland Lakes is of high social, economic, irrigation and urban (Briagolong) water supply. The shallow environmental and cultural value and is a major drawcard aquifer of the Avon, Thomson, Macalister and lower Latrobe for tourists. A number of major Gippsland rivers (Latrobe, catchments is naturally variable in quality and yield. In many Thomson, Macalister, Avon and Perry) all drain through areas the aquifer contains large volumes of high quality floodplains to Lake Wellington and ultimately the Southern (fresh) groundwater, whereas elsewhere the aquifer can be Ocean, with the Perry River being one of the few waterways naturally high in salinity levels. Watertable levels in some in Victoria to have an intact chain of ponds geomorphology. areas have been elevated due to land clearing and irrigation The EPBC Act listed Gippsland Red Gum Grassy Woodland recharge. -
West Gippsland Region
Powlett River. Courtesy WGCMA The West Gippsland region is diverse and characterised by areas of natural forest, West areas of high conservation value, fertile floodplains for agriculture, as well as having Gippsland major coal deposits and the Loy Yang, Hazelwood and Yallourn power stations. Region Three river basins form the region – Thomson (basin 25), Latrobe (basin 26) and South Gippsland (basin 27). West Gippsland Region In the north of the region is the Thomson basin, Hydrology characterised by the naturally forested Eastern Highlands. At the foot of the highlands are two major dams - Lake The hydrological condition of streams across the West Glenmaggie and the Thomson dam. Over half (55%) of Gippsland region reflects the varied land use - from natural the stream length in the Thomson basin was found to be and near natural flow regimes in headwater streams in in good or excellent condition. Of the remainder, 41% of forested areas of the region to flow regimes under immense stream length was in moderate condition and just 3% stress in areas dependent on water supply for domestic and 1% in poor and very poor condition respectively. and agricultural use. In the centre of the region is the Latrobe basin. The basin Thomson Dam provided 12,046 ML of environmental water features vast tracts of forest through the Strezlecki Ranges in 2011-12 for six reaches on the Thomson River (reaches and the Great Dividing Range, where streams rise and flow 1-5) and Rainbow Creek (reach 17) and Lake Glenmaggie to Lake Wellington in the east. Although much of the land provided 14,018 ML of environmental water to two reaches has been cleared for agriculture, the dominant land use is on the Macalister River (reaches 7 and 8). -
Water Supply Options for Melbourne
Submission to the Environment and Natural Resources Committee Inquiry into Melbourne’s Water Supply Water supply options for Melbourne An examination of costs and availabilities of new water supply sources for Melbourne and other urban areas in Victoria Alan Moran Director, Deregulation Unit, Institute of Public Affairs Institute of Public Affairs Occassional Paper, revised August 2008 Water supply options for Melbourne Summary greenfield developments. Recycling Eastern Treatment Plant (ETP) water appears to be prohibitively costly, while Melbourne’s water supply is suffering from a combination releasing treated water and substituting it for other sources of drought and a failure to build new storage facilities over is also expensive. Some variations of household rainwater the past 23 years when the population has increased by tanks rival the Wonthaggi desalination plant proposal in over 30 per cent. These matters may be aggravated by providing the most expensive solutions. Less expensive is long term climate change diminishing the precipitation to the government’s Sugarloaf approach, but this still entails the traditional sources in the Melbourne catchment. water costing two and a half times that from a new dam in The government policy of matching supply and the Melbourne catchment. demand has been, and largely remains, directed at The table below summarises the estimated costs measures that curtail demand; supply side measures and potential additional water supplies from the more have focused on tapping local sources, mainly through realistic options available. A major new Gippsland dam household water tanks. Additional supply sources have is the lowest cost option, though a river diversion into the been proposed over the past year or so. -
Benefits of Environmental Water – Spawning of Australian Grayling in Four Coastal Rivers Fact Sheet 3 - Spawning Success of Australian Grayling
Benefits of environmental water – Spawning of Australian Grayling in four coastal rivers Fact sheet 3 - Spawning success of Australian Grayling Investigating how to use environmental water to Studying Australian Grayling protect and restore environmental values within rivers, floodplains, wetlands and estuaries. From 2008 to 2015, the Arthur Rylah Institute (ARI) studied the effects of flows on spawning of Australian Background Grayling. The objective was to identify key components of the flow regime (hydrograph) that could be provided Australian Grayling (Prototroctes maraena) is a annually to stimulate downstream spawning nationally threatened fish that lives in coastal rivers in migrations from March to May. south-eastern Australia. The species is amphidromous, meaning adults spawn in the lower freshwater reaches, Monitoring spawning success larvae then drift downstream to the sea, and juveniles migrate back upstream into freshwater. There has Eggs and larvae of Australian Grayling were collected in been a dramatic decline in abundance and distribution the lower Bunyip and Yarra rivers annually from 2008 of Australian Grayling, due largely to altered flow to 2015 using drift nets. This represents an important regimes and stream barriers, which block fish continuous dataset to analyse flow patterns and the migration. ecology of a nationally threatened species. Eggs and larvae were collected in the Thomson River from 2013 Managing environmental water releases to 2015 and in the Tarwin River in 2012. In Victoria, many agencies work to implement Monitoring results environmental watering programs. West Gippsland Catchment Management Authority and Melbourne Bunyip River Water have develop seasonal watering proposals The peak abundances of eggs and larvae which include key flow objectives to deliver within (about 70%) coincided with a within-channel channel flow pulses, known as 'freshes', to specifically flow pulse in late April. -
Prospecting in Victoria
PROSPECTING IN VICTORIA 1. What is a Miner’s Right? A Miner’s Right is a permit to prospect for minerals on unreserved Crown Land or Private Land where the permission of the landowner has been granted. 2. What is prospecting / fossicking? Prospecting involves the use of metal detectors, hand tools, pans or simple sluices in the search for gold and gemstones. 3. Why is a Miner’s Right required to prospect for minerals? All minerals belong to the Crown, even on private land. A Miner’s Right transfers the ownership of any minerals found whilst prospecting, to the holder of the Miners Right. 4. Who needs a Miner’s Right? Anyone searching for minerals needs to have an exploration licence, a mining licence or a Miner’s Right. 5. Does that mean that a Miner’s Right is required even if you are fossicking on your own land? Yes. 6. How much is a Miner’s Right? Refer to Earth Resources Fees and Charges 7. How long does a Miner’s Right last? You can purchase a Miner’s Right for 2 or 10 years, but not exceeding 10. 8. Do pensioners, people who are unemployed or people with disabilities receive any concessional discount if they purchase a Miner’s Right? No. 9. Do hobbyists or gemstone seekers require a Miner’s Right? Yes. 10. If a family goes away prospecting and fossicking does each family member need a Miner’s Right? All adults who intend to fossick must have a Miner’s Right. Children under supervision of an adult with a Miner’s Right do not need a Miner’s Right of their own. -
BAW BAW NATIONAL PARK (13 530 Hectares) Park Overview Baw Baw
BAW BAW NATIONAL PARK (13 530 hectares) Park overview Baw Baw National Park north of the Latrobe Valley consists of a distinctive sub-alpine plateau and surrounding forested uplands. It contains the headwaters of the Tyers River and tributaries of the Thompson and Aberfeldy Rivers, which provide water to Melbourne and towns surrounding the park. Although similar in some respects, the park is considerably isolated from the rest of Victoria’s high country and has similarities with Tasmania’s vegetation. The park is surrounded mostly by State forest and also by the Walhalla Historic area in the south-east (covering parts of the major goldfields of the Aberfeldy - Walhalla area) and the Baw Baw Alpine Resort. Park location and access Baw Baw National Park is located about 120 km east of Melbourne and 50 km north of the Latrobe Valley. The main access to the plateau is from the Mount Erica and St Gwinear carparks along signposted roads off the Thomson Valley Road, north of Erica. Access through the Thompson and Aberfeldy River valleys on the eastern side of the park is via the winding Walhalla Road. Many of the tracks in the Thomson and Aberfeldy Valleys are suitable for four-wheel drive vehicles only. and is typified by steep grades. Many roads and tracks are closed during the winter months. The Baw Baw Plateau itself is only accessible to walkers and skiers beyond the Mount Erica and St Gwinear carparks. Conservation attributes Baw Baw National Park contains a diverse array of vegetation types and plant species, extending over an elevation range of 1100 metres. -
Draft Gippsland Region Sustainable Water Strategy
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