Latrobe River Basin January 2014
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Victorian Catchment Management Almanac 2019
Victorian Catchment Management Almanac 2019 Our approach to catchment management is continuously developing in response to many initiatives and events. This Almanac identifies key happenings and lists them in chronological order. We welcome input to help improve the accuracy and scope of this document. Please forward suggestions to [email protected] Almanac: Victoria's Catchment Management Framework Year Event Background Imperative Consequence -100000 Climate similar to that of present Continuing climate till about year -60000 -63000 Humans move into Australia Humans originally migrating out of Inexorable spread of Human colonisation . Timing is becoming less contentious. Recent work at Africa. The origins of the first Australians humans Madjedbede (Northern Australia) dated grinding stones, and ground axe heads is not clear (but presumably through SE at -63,000BC. (Clarkson et al (2017) Human occupation of Northern Australia by Asia rather than Polynesia). They are 65 000 years ago . Nature 547 306-310). There is evidence of change in fire believed to be amongst the earliest regimes occurring up to about 100 000 years ago. migrations out of Africa. -60000 Colder and dryer climate phase Continuing climate till about year -10000. Known as the last glacial age. -50000 Megafauna / human/climate This relationship of this interaction with Extinction related to any, Megafauna extinction but dating of when this occurred is controversial. Peak of interaction megafauna extinction is fraught. or all, of climate change, extinctions calculated by various sources at about -45000 to -40000 years (see Some evidence that megafauna became human land management Van der Kaars et al (2017) Nature Communication 8 Article 14142)- intriguing as extinct within a rapid timeframe. -
West Gippsland Floodplain Management Strategy 2018
WEST GIPPSLAND CATCHMENT MANAGEMENT AUTHORITY West Gippsland Floodplain Management Strategy 2018 - 2027 Disclaimer Acknowledgements This publication may be of assistance to you but The development of this West Gippsland the West Gippsland Catchment Management Floodplain Management Strategy has involved Authority (WGCMA) and its employees do not the collective effort of a number of individuals guarantee that the publication is without flaw and organisations. of any kind or is wholly appropriate for your Primary author – Linda Tubnor (WGCMA) particular purpose. It therefore disclaims all Support and technical input – WGCMA liability for any error, loss or other consequence Board (Jane Hildebrant, Ian Gibson, Courtney which may arise from you relying on any Mraz), Martin Fuller (WGCMA), Adam Dunn information in this publication. (WGCMA), Catherine Couling (WGCMA), Copyright and representatives from VICSES, Bass Coast Shire Council, Baw Baw Shire Council, Latrobe © West Gippsland Catchment Management City Council, South Gippsland Shire Council, Authority Wellington Shire Council, East Gippsland First published 2017. This publication is Shire Council, East Gippsland Catchment copyright. No part may be reproduced by any Management Authority, DELWP, Bunurong process except in accordance with the provisions Land Council, Gunaikurnai Land and Waters of the Copyright Act 1968. Aboriginal Corporation and Boon Wurrung Foundation. Accessibility Acknowledgement of Country This document is available in alternative formats upon request. We would like to acknowledge and pay our respects to the Traditional Land Owners and other indigenous people within the catchment area: the Gunaikurnai, The Bunurong and Boon Wurrung, and the Wurundjeri people. We also recognise the contribution of Aboriginal and Torres Strait Islander people and organisations in Land and Natural Resource Management. -
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. -
Victorian Recreational Fishing Guide 2021
FREE TARGET ONE MILLION ONE MILLION VICTORIANS FISHING #target1million VICTORIAN RECREATIONAL FISHING A GUIDE TO FISHING RULES AND PRACTICES 2021 GUIDE 2 Introduction 55 Waters with varying bag and size limits 2 (trout and salmon) 4 Message from the Minister 56 Trout and salmon regulations 5 About this guide 60 Year-round trout and salmon fisheries 6 Target One Million 61 Trout and salmon family fishing lakes 9 Marine and estuarine fishing 63 Spiny crays 10 Marine and estuarine scale fish 66 Yabbies 20 Sharks, skates and rays 68 Freshwater shrimp and mussels 23 Crabs INTRODUCTION 69 Freshwater fishing restrictions 24 Shrimps and prawns 70 Freshwater fishing equipment 26 Rock lobster 70 Using equipment in inland waters 30 Shellfish 74 Illegal fishing equipment 33 Squid, octopus and cuttlefish 74 Bait and berley 34 Molluscs 76 Recreational fishing licence 34 Other invertebrates 76 Licence information 35 Marine fishing equipment 78 Your fishing licence fees at work 36 Using equipment in marine waters 82 Recreational harvest food safety 40 Illegal fishing equipment 82 Food safety 40 Bait and berley 84 Responsible fishing behaviours 41 Waters closed to recreational fishing 85 Fishing definitions 41 Marine waters closed to recreational fishing 86 Recreational fishing water definitions 41 Aquaculture fisheries reserves 86 Water definitions 42 Victoria’s marine national parks 88 Regulation enforcement and sanctuaries 88 Fisheries officers 42 Boundary markers 89 Reporting illegal fishing 43 Restricted areas 89 Rule reminders 44 Intertidal zone -
2012 Gippsland Flood Event - Review of Flood Warnings and Information Systems
2012 Gippsland Flood Event - Review of Flood Warnings and Information Systems TRIM ID: CD/12/522803 Date: 21 November 2012 Version: Final OFFICE of the EMERGENCY SERVICES COMMISSIONER Page i MINISTERIAL FOREWORD In early June this year, heavy rain and widespread flooding affected tens of thousands of Victorians across the central and eastern Gippsland region. The damage to towns and communities was widespread – particularly in the Latrobe City, Wellington and East Gippsland municipalities. Homes, properties and businesses were damaged, roads and bridges were closed, and more than 1500 farmers were impacted by the rains. A number of people were rescued after being trapped or stranded by the rising waters. Following the floods, some communities had a perception that telephone-based community warnings and information had failed them. As the Minister for Police and Emergency Services, I requested Victoria’s Emergency Services Commissioner to review the effectiveness, timeliness and relevance of the community information and warnings. This report has met my expectations and has identified the consequences and causes for the public’s perception. I welcome the review’s findings. I am confident these will, in time, lead to better and more effective arrangements for community information and warnings and contribute to a safer and more resilient Victoria. PETER RYAN Minister for Police and Emergency Services Page ii Contents Glossary ......................................................................................................................... v Executive Summary....................................................................................................... 1 1. June 2012 Gippsland flood.................................................................................3 1.1 Key physical aspects of the 2012 Gippsland flood event 3 1.2 Key aspects of information and warnings in the incident response 6 1.2.1 Key information and warnings from Bureau of Meteorology 6 1.2.2 Key information and warnings through incident management 7 2. -
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. -
Friends of Latrobe Water
26th August 2020 National Water Reform 2020 Productivity Commission Lodgement online at [email protected] Dear Commissioners RE: National Water Reform Inquiry - Submission from Friends of Latrobe Water Friends of Latrobe Water (FLoW) welcomes this opportunity to provide input to the Productivity Commission to assist with its review of National Water Reform. FLoW advocates for the protection of Latrobe Valley’s water sources and safeguarding the protection of the Gippsland Lakes from industry activities, including coal mine rehabilitation and coal ash contamination. Threats include – • Declining water flows • Changes in flows • Overallocation of water sources • Priority sharing of water resources In consideration of the Commission’s 2017 recommendations that jurisdictions recommit to a renewed NWI, FLoW has concerns with, • policy settings for alternative water sources in entitlement and planning frameworks • other policy settings relating to: – urban water management – environmental water management – decision-making on building and supporting new infrastructure. In context to the regional area of Gippsland in Victoria, alignment of water policy on a statewide basis is challenging due to the dominance and current governance of mining in the Latrobe Valley in Gippsland’s central west. This has resulted in substantial impacts to water flow, quality and chemistry to all other beneficial users downstream including environmental water health. In responding to the Issues Paper on the scope of this inquiry FLoW will also address, • emerging challenges faced by Governments, water providers and water users, such as climate change or changes in economic circumstances • the interaction of water policy with other areas (such as land use planning and urban development) • the impacts of climate change on water resources • the provision of reliable water services to regional and remote communities • the principles to be satisfied for any Government investment in major water infrastructure. -
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). -
I • T • Maddern , Morwe1l E 1~[8/25 the First
Final Issue. The Monell HiJ:rtorica.l .Societ:y News .••.•••• 15th. , • • Augu§t, .•. '·,•····· .. ···.•· .. ····· . 19l5 This issue is merely a·repe.at of· voiume 2, published in 1963, supplies of which · .. hSr~ becont~~lili~µs ~~9-·•· _R.e~blioation.ofVolume 2 has now· given us reserve of 20 complete sets of the.l3volumes issued in yearly volu,m.esfrom 1962to1974 inclusive. These sets will be kep't in reserve for posterity. Volume. 2 •••• 19§2. Table of Contents. Chapter 1 •.•.• 21/ 1/6:;••• John Irving, 1856-1894, School Teacher. 9h'll)ter ·• ~· .·-~~~/ .l/63. ~ .• Cowm.ercia.lRoad stat.a School, Monell• Ohapte.r' 3;. ~··"41. 2/63.·; ~Charles Oxtoby.Gilb~rt t 1829-1888~ Q~~pter 4 ••• 11{ 2/63 ••• Percy A.still Gilbert, 1868-1951. ·on~~te,;t{: 5., ,.18/ 2!f?> ••• The First Page of the Morwell School Ree;ister. Chapter~ 6 ••• 25/ 2/6'3 ". ~ • Insp.ectors and Inspections. ·abapt~~~ 1.• • 4/ 3/63... Hotels and Houses. Chapter 8.·: .ll/ ''5/63••• Tlie Homes of the Settlers. Oha.pter 9 •. .,.:18/ 7>/6'3.· ••An .,"'J.nniversa~''. · Cha.~t:er 10.••• 25/ 3/6·;r. -,.Houses of Old Morwell. Chapter 11. • • 1/ 4/63. ~ .Houses of . Old Mo~ell . (continued) • . :)",'Oh~1-Ce:r· 12.. •.• • ·.$/ 4/63. •:•Moe and the Moe Swamp. ·'Chap~~- 13. •:•l5/. 4/63.~.The ;a.a.untedHills. Cfl,S.pter14 ••• ,22/ 4/63 ••• coal. Chayte::r 15 ••• 29/ 4/63 ••• William Tulloch and the Open Cut Mine~ C~~pter 16.• • 6/ 5/ 6; •• •A;t'Ohc~bald ~X:a!.' s Diaq. Cha1ter· 17••• r;/ 5/63 ••• The· Swiss Family, Na.denbousoh. -
Latrobe River Tin Mines: an 1870S Mining Scam
Journal of Australasian Mining History, Volume 15, October 2017 Latrobe River Tin Mines: An 1870s Mining Scam By ROBIN BAILEY n old miner once defined a mine, as a hole in the ground owned by a liar. This definition well defines an episode in the 1870’s when two very prominent A members of the Victorian Parliament, John Woods and Louis Lawrence Smith, aware of publicity surrounding early discoveries of tin at Mount Bischoff in Tasmania, decided to get into the act. One of the pair having previously heard of abandoned tin prospects in heavily timbered mountainous country 80 kilometers east of Melbourne, in the Upper Latrobe River, saw an opportunity not to be missed. As the locality was so remote and difficult to access, there was little chance of any investigation into the viability of the mining leases at the time. Subsequently, they formally took out mining leases using the old lease plans and then attempted to sell these worthless leases in London for £100,000. This is the story of incompetence and of their mining scam. The Early Discoveries In the 1860s parties of prospectors were working in the Upper Goulburn River, culminating in the major gold field discoveries of Woods Point, Matlock, Jordan and later Walhalla. Supply lines for the many thousands of miners working in the mountainous country were very long, and the cost of packing provisions and equipment in from Jamieson and later Sale was very great. Much time and money was spent in developing the Yarra Track through Healesville and Marysville to Matlock and Woods Point, and the effort of keeping it trafficable in winter proved beyond the maintenance resources of the day.1 From the south, in 1862, a track was cut from Drouin, effectively following the course of the present road through Neerim to Noojee, then up the Loch River to the Yarra – Latrobe Divide near Mt. -
River Channel Relocation: Problems and Prospects
water Review River Channel Relocation: Problems and Prospects Alissa Flatley 1,* , Ian D Rutherfurd 1 and Ross Hardie 2 1 School of Geography, University of Melbourne, 221 Bouverie Street, Carlton, VIC 3053, Australia; [email protected] 2 Alluvium Consulting, Level 1, 105–115 Dover Street, Cremorne, VIC 3013, Australia; [email protected] * Correspondence: alissa.fl[email protected]; Tel.: +61-408-708-940 Received: 28 August 2018; Accepted: 26 September 2018; Published: 29 September 2018 Abstract: River relocation is the diversion of a river into an entirely new channel for part of their length (often called river diversions). Relocations have been common through history and have been carried out for a wide range of purposes, but most commonly to construct infrastructure and for mining. However, they have not been considered as a specific category of anthropogenic channel change. Relocated channels present a consistent set of physical and ecological challenges, often related to accelerated erosion and deposition. We present a new classification of river relocation, and present a series of case studies that highlight some of the key issues with river relocation construction and performance. Primary changes to the channel dimensions and materials, alongside changes to flow velocity or channel capacity, can lead to a consistent set of problems, and lead to further secondary and tertiary issues, such as heightened erosion or deposition, hanging tributaries, vegetation loss, water quality issues, and associated ecological impacts. Occasionally, relocated channels can suffer engineering failure, such as overtopping or complete channel collapse during floods. Older river relocation channels were constructed to minimise cost and carry large floods, and were straight and trapezoidal.