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Mount Rouse Reserve Management Plan 1/08/2016
Trim atDevelop Disclaimer This management plan has been drafted by RMIT University and Regional Advance to guide the future management of Mount Rouse Reserve by the Committee of Management (Southern Grampians Shire Council). The plan articulates management priorities for the reserve that have been identified through desktop research, a basic site investigation and consultation with a number of the reserve’s stakeholders. While care has been taken in identifying management priorities and strategies for the reserve, the accuracy and comprehensiveness of this document may not be without limitation. RMIT University and Regional Advance shall not be responsible in any way to any person in respect to the document, including errors or omissions contained, regardless of cause. 1 Mount Rouse Reserve Management Plan 1/08/2016 Contents 1 Context ................................................................................................ 3 3.2 Community and Amenity Values ............................................... 12 2 Reserve Overview ............................................................................... 3 3.2.1 Public Amenity ...................................................... 12 2.1 Reserve Description .................................................................... 3 3.2.1 Public Amenity (Continued) .................................. 13 3.2.2 Tourism and Recreational Uses ............................. 14 2.2 Boundaries and Allotments Map ................................................ 4 3.2.3 Access ................................................................... -
The Harmans Valley Lava Flow and Its Tortuous Path
The Harmans Valley lava flow and its tortuous path John Brush Canberra Speleological Society Inc, Chairman, IUS Commission on Volcanic Caves Email: [email protected] Abstract as the most significant damage was in areas that are visible from a public viewing point, the landscape The Harmans Valley lava flow, south of Hamilton in significance has diminished. Western Victoria, originates at the Mt Napier volcano and meanders its way across the landscape along a In October 2016, the Victorian Government imposed pre-existing valley. The renowned Byaduk lava caves a Significant Landscape Overlay (SLO), in effect a occur within the flow. The flow itself is about 40,000 landscape protection control, on those parts of the years old and is regarded by many experts to be the flow that lie on private land within the Southern best example of a lava flow constrained by a valley Grampians Shire. Unless replaced by a permanent and having one of the most intact and significant SLO, the interim SLO will expire on 31 October collections of young volcanic features in Australia. 2018. The flow also has aboriginal and early-European This paper reviews efforts to protect the flow and its cultural heritage significance as well as dramatic important geological, landscape, ecological and landscape values. While the meandering route of the cultural features and considers the likelihood of flow could be described as tortuous, the path to achieving effective permanent protection. protecting this iconic feature has been, and continues to be, even more tortuous. Introduction The Mount Napier volcano and the upper part of the The Harmans Valley basalt lava flow in Western flow, containing many of the Byaduk caves, are Victoria originated at Mt Napier and flowed down a protected as they are in the Mount Napier State Park. -
SOUTH WEST VICTORIA LANDSCAPE ASSESSMENT STUDY Significant Views of South West Victoria June 2013
SOUTH WEST VICTORIA LANDSCAPE ASSESSMENT STUDY Significant Views of South West Victoria June 2013 1 Significant Views of South West Victoria NATIMUK HORSHAM 5.1 Mount Arapiles STAW ELL EDENHOPE 6.1 Grampians Lookouts HALLS GAP 3.1 Pioneer Lookout ARARAT 1.9 Berry Deep Lead Gold Mine DAYLESFORD 2.3 Robertsons Hill BALLARAT 2.1 Mount 1.10 Mount Warrenheip Blackwood 2.2 Lal Lal Falls 4.1 Mickle Lookout COLERAINE 1.10 Mount Buninyong CASTERTON DUNKELD BACCHUS MARSH HAMILTON 1.4 Lake Linlithgow 1.1 Mount Rouse DERRINALLUM 1.2 Harmans Valley DARTMOOR MORTLAKE 1.3 Lake Surprise GEELONG 1.8 Lake Keilambete HEYW OOD CAMPERDOW N Coastal Spaces Landscape Assessment Study, 2006 1.5 Mount Leura 1.6 Red Rocks Coastal Spaces Landscape 1.7 Lakes Gnotuk Assessment Study, 2006 & Bullen Merri PORTLAND Great Ocean Road Region Landscape Assessment Study, 2003 PORT FAIRY © 2013 Logo is at twice the size for the footer Significant Views of South West Victoria 1. WESTERN VOLCANIC PLAIN 4.O THE R LLING TABLELANDS 1.1 Mount Rouse State 4.1 Mickle Lookout, Casterton Regional 1.2 Harmans Valley State 1.3 Lake Surprise Regional 5. THE WIMMERA PLAINS 1.4 Lake Linlithgow Regional 5.1 Mount Arapiles State 1.5 Mount Leura State 1.6 Red Rocks State 6. The Grampians (Gariwerd) & surrounds 1.7 Lakes Gnotuk & Bullen Merri State 1.8 Lake Keilambete Regional 6.1 Grampians Lookouts State 1.9 Berry Deep Lead Gold Mine Views Regional 1.10 Mount Buninyong & Mount 7. VEGETATED RISES Regional Warrenheip (No State or Regionally Significant 2. -
Does Early Colonial Art Provide an Accurate Guide to the Nature and Structure of the Pre-European Forests and Woodlands of South
Does early Colonial Art provide an accurate guide to the nature and structure of the pre-European forests and woodlands of South-Eastern Australia? A study focusing on Victoria and Tasmania By Michael Francis Ryan B For Sei, University of Melbourne Submitted in fulfilment of the requirement for the degree of: Master of Forestry Australian National University November 2009 Candidate’s Declaration I declare that this is the original work of Michael Francis Ryan of 84 Somerville Rd Yarraville, Victoria submitted in fulfilment of the requirement for the degree of Master of Forestry at the Australian National University. 2 Acknowledgements I am very grateful for the assistance and patience especially of Professor Peter Kanowski of the Australian National University for overseeing this work and providing guidance and advice on structure, content and editing. I would also like to acknowledge Professor Tim Bonyhady also of the Australian National University, whose expertise in the artwork field provided much inspiration and thoughtful analysis understanding early artwork. Bill Gammage, also from the ANU, provided excellent critical analysis using his extensive knowledge of the artists of the period to suggest valuable improvements. Ron Hateley from the University of Melbourne has an incredible knowledge of the early history of Victoria and of the ecology of Australia’s forests and woodlands. Ron continued to be a great sounding board for ideas and freely shared his own thoughts on early artwork in Western Victoria and the nature of the pre-European forests and I thank him for his assistance. Pat Groenhout, formally from VicForests, provided detailed comments and proof reading of manuscripts and this has considerably improved the readability and structure. -
Umberatana Wall Part of a (The?) Wall on Umberatana Was Washed Away, Presumably Early in Its Life, in Unusual Storms in August 1865
The Flag Stone Issue No. 40, October 2017 Patron: Lyn Allison ISSN 2204-8316 Editor: Bruce Munday T A Problem to Ponder by Colin Murdoch Dry stone wall across ridge-top at Umberatana is just visible on the skyline he last few kilometres of the drive in to the Approaching the wall from the southern side it was Thomestead at Umberatana Station, at the consistently 1500-1700 millimetres high with significant north end of the Gammon Ranges (SA), is domi- foundation rocks which pass all the way through. Some- nated by a dry stone wall on the hill-top to the times these are “found” as in utilised in their original position without moving them for the wall. The next south. Umberatana caretaker/managers, John layer most often has three rocks lying in the direction of and Sue Mengersen, have lived in the area for over the wall next to each other; that is one on the north 50 years and believe that there is an Afghan link, side, one in the middle and one on the south side. These suggesting that perhaps it was built for camels, are topped by a layer two rocks thick, again generally but there is little hard evidence to support this. laid with their long axis in the direction of the length of Checking on Google Earth, and having walked it, I feel the wall. Finally, there are the copes where rocks lie the wall is about 1.6 to 2 kilometres long. On the ground across the wall and on their narrow side to create great- it is clear that it runs until there is no more building er pressure on the wall below. -
A Lady's Visit to the Gold Diggings of Australia in 1852-53
A Lady’s Visit to the Gold Diggings of Australia in 1852-53 Clacy, Ellen (Mrs. Charles) University of Sydney Library Sydney 1997 http://setis.library.usyd.edu.au/ © University of Sydney Library. The texts and Images are not to be used for commercial purposes without permission Source Text: Prepared from the print edition published by Hurst and Blackett London, 1853 Trailer: "LONDON: Printed by Schulze and Co., 13, Poland Street." All quotation marks retained as data All unambiguous end-of-line hyphens have been removed, and the trailing part of a word has been joined to the preceding line. First Published: 1853 919.45F8280 Australian Etexts goldrush diaries women writers 1840-1869 prose nonfiction 7th February 1999 Creagh Cole Coordinator Final Checking and Parsing A Lady’s Visit to the Gold Diggings of Australia in 1852-53 London Hurst and Blackett 1853 A LADY'S VISIT TO THE GOLD DIGGINGS OF AUSTRALIA. IN 1852–53 Chapter I. Introductory Remarks IT may be deemed presumptuous that one of my age and sex should venture to give to the public an account of personal adventures in a land which has so often been descanted upon by other and abler pens; but when I reflect on the many mothers, wives, and sisters in England, whose hearts are ever longing for information respecting the dangers and privations to which their relatives at the antipodes are exposed, I cannot but hope that the presumption of my undertaking may be pardoned in consideration of the pleasure which an accurate description of some of the Australian Gold Fields may perhaps afford to many; and although the time of my residence in the colonies was short, I had the advantage (not only in Melbourne, but whilst in the bush) of constant intercourse with many experienced diggers and old colonists — thus having every facility for acquiring information respecting Victoria and the other colonies. -
Volcanic Caves of Western Victoria Ken G
Volcanic Caves of Western Victoria Ken G. Grimes RRN 795 Morgiana Rd., Hamilton, 3300, Australia ([email protected]). Abstract The Western District Volcanic Province extends from Melbourne across to the Mount Gambier area and has been erupting basalt lavas for at least the last 5 million years. Lava caves have formed in several areas across the region, but the best concentrations are in the ~30,000 year-old lavas from Mt. Eccles and Mt. Napier. There are a variety of volcanic caves, including large feeder tubes that are responsible for the long lava flows (60 km in the case of a flow from Mt Rouse), but also smaller but more complex shallow subcrustal lava caves and one example of a still-open volcanic vent or large hornito. Lava tubes form in two main ways. The first is by the roofing of narrow surface lava channels, which happens in several ways. This type tends to form linear and simply-branching or anastomosing tubes. The second way is by draining from beneath the crust of a set of spreading lava lobes near the leading edge of a lava flow - these tend to form more complex mazes of shallow, low-roofed chambers and passages, but over time they may evolve by solidification of the more stagnant areas and erosional enlargement of the fastest moving routes to form simpler linear tubes that are difficult to distinguish from the roofed channels. Both types of tube contain liquid lava flowing beneath a solid crust. At the end of the eruption some of that lava drains out to leave empty caves, but most tubes remain filled with solidified lava. -
Buninyong Botanic Gardens Conservation Study
Buninyong Botanic Gardens Conservation Study Dr David Jones, School of Architecture, Landscape Architecture & Urban Design, Adelaide University With Fifth Creek Studio For City of Ballarat Final Version June 2004 Buninyong Botanic Gardens Conservation Plan The draft documenbt was prepared by Dr David Jones, School of Architecture, Landscape Architecture & Urban Design, The University of Adelaide, for the City of Ballarat. Photographs taken by Dr Jones or from the photograph collection held by the Buninyong & District Historical Society, unless otherwise stated. Historical advice has been provided by Beth Ritchie and Derick Leather, Buninyong, Vic. Landscape design advice has been provided by Graeme Hopkins and Christine Goodwin of Fifth Creek Studio, Montacute, SA. Technical tree advice has been provided by JAE Whitehill of Tree Advisory Services, Glengowrie, SA. All plans and drawings by Dr Jones. © Dr David Jones Dr David Jones Senior Lecturer in Landscape Architecture School of Architecture, Landscape Architecture, and Urban Design The University of Adelaide Adelaide SA 5005 Phone 08 8303 4589 Fax 08 8303 4377 Email [email protected] Following public consultation and submissions the Bunincyong Botanic Gardens Conservation Study Steering Committee recommended a number of changes to the historical details of this report. As the consultant was unable to produce a revised document with these amendments within the timescale required by Council, the draft document was adopted by Council at its meeting held 9 June 2004 with the following resolutions: 1. That Council adopts the “Buninyong Botanic Gardens Conservation Study and Masterplan with text modifications as pr attachement 4 2. That Counil acknowledeges and thanks the members of the Steering Committee for their involvement in development of the plan. -
GDTA POST Reg
GDTA POST Reg. AOO27059N Newsletter of the Great Dividing Trail Association http://www.gdt.org.au Volume 2013 Issue 4 December 2013 Wow! What happened next? –See the report on the St Georges Lake to White Swan Rd Walk by Gib Wettenhall, page 8 President’s report GDTA president Barry Golding has commissioned the following message from our special envoy at the North Pole: And Best Wishes for 2014 2014 Guided Walks Program – The BIG GDT CIRCUIT The BIG GDT CIRCUIT comprises one to three circuit walks near each of the GDT townships of Buninyong, Creswick, Daylesford, Castlemaine and Bendigo; followed by four circuits near Blackwood, Bacchus Marsh and in the Wombat State Forest. FIFTEEN walks in total! All described in this issue of POST. Walks will be graded generally as Medium because of the length or the terrain, although there are some Hard and some Easy sections. For insurance purposes, each visitor will need to become a GDTA Temporary Member (for one day only). In the one calendar year: . Financial Members can have as many walks as they like, at no cost other than their annual subscription. GDTA is a member of Bushwalking Victoria www.bushwalkingvictoria.org.au GDTA POST DECEMBER 2013 . Visitors can have up to three walks as Temporary Members at a fee of $5.00 per walk. After that they must become Financial Members before they walk again with GDTA. Temporary Member fees will count towards payment of the first year’s subscription. Register with the walk leader by Thursday 8.00pm before the walk. NOTE: Give your phone number so we can contact you if walk arrangements change. -
Heritage Landscapes Selected Forum Papers 2004–08
Heritage landscapes Selected forum papers 2004–08 Editors Dr John Dwyer QC Dr Janet Schapper Heritage landscapes Selected forum papers 2004–08 Editors Dr John Dwyer QC Dr Janet Schapper Production Editor Pauline Hitchins, Heritage Victoria Published by the Heritage Council of Victoria 2009, Melbourne References throughout to the heritage website or Heritage Victoria website refer to: www.heritage.vic.gov.au which includes the searchable Victorian Heritage Database. Published by the Heritage Council of Victoria, Melbourne, October 2009. Also published at www.heritage.vic.gov.au © State of Victoria, Heritage Council of Victoria 2009. This publication is copyright. No part may be reproduced by any process except in accordance with the provisions of the Copyright Act 1968. ISBN 978 0 9806217 2 3 (print), 978 0 9806217 4 7 (CD Rom), 978 0 9806217 3 0 (online) Disclaimer This publication may be of assistance to you but the State of Victoria and its employees do not guarantee that the publication is without fl aw of any kind or is wholly appropriate for your particular purposes and therefore disclaims all liability for any error, loss or other consequence which may arise from you relying on any information in this publication. Heritage Victoria / Heritage Council of Victoria, Level 4, 55 Collins St, Melbourne 3000 GPO Box 2392, Melbourne, Victoria 3001 Phone: (03) 8644 8800 Fax: (03) 8644 8811 Email: [email protected] Web: www.heritage.vic.gov.au Cover images: From left ( back cover) to right Spray Farm estate on the Bellarine Peninsula. Image Mark Chen, Tourism Victoria The former Carlo Gervasoni homestead at Yandoit Hills is a reminder of early Italian settlement in the area. -
Berry Street School Annual Report 2019
2019 ANNUAL REPORT CONTENTS 01 OPENING ACKNOWLEDGEMENT “ We will strive to provide a service 02 OUR VISION 03 CONTACT DETAILS where reconciliation lives in 03 MINIMUM STANDARDS ATTESTATION the hearts, minds and actions 04 DEMOCRATIC PRINCIPALS STATEMENT of all our teams. We commit to 05 OUR BOARD OF DIRECTORS 07 CEO REPORT transparency on our journey and 08 DIRECTOR OF EDUCATION GOVERNING AUTHORITY REPORT recognise Aboriginal and Torres 09 PRINCIPAL’S REPORT Strait Islander perspectives 11 OUR SCHOOL 12 ATTENDANCE DATA and leadership is critical to our 13 INTERVIEW WITH SARAH DAWSON success.” 15 OUR LEARNING CEO Michael Perusco 15 CHARACTERISTICS OF STUDENT POPULATION 15 TEACHING AND LEARNING REPORT and Board President Jo Flynn 17 INTERVIEW WITH KATE 19 EXTRA CURRICULARS 21 LITERACY AND NUMERACY GROWTH 22 STUDENT WELLBEING 23 SETH’S STORY 25 OUR STAFF 25 STAFF WELLBEING 27 CHILD SAFE STANDARDS 29 STAFF AT BERRY STREET SCHOOL 2019 31 SCHOOL PERFORMANCE DATA SUMMARY 32 FINANCIAL REPORT 33 OUR FUTURE 33 FUTURE FOCUS 34 ALUMNI STORIES 35 ABOUT THE ARTIST 36 CLOSING ACKNOWLEDGEMENT 01 BERRY STREET SCHOOL 2019 ANNUAL REPORT ACKNOWLEDGEMENT Berry Street School acknowledges Aboriginal and Torres Strait Islander peoples as the Traditional Vision Our Custodians of the lands, skies, and waterways across Australia. We acknowledge that sovereignty was never ceded, and we recognise the impact School Our colonisation has had and continues to have. We appreciate the knowledge, wisdom and learnings of the longest living cultures and we are guided by their strength and resilience. The Berry Street Learning Our School pays our respect and we acknowledge Elders as holders, protectors and educators of Aboriginal and Torres Strait Islander cultures. -
The Moyjil Site, South-West Victoria, Australia: Stratigraphic and Geomorphic Context
CSIRO Publishing The Royal Society of Victoria, 130, 14–31, 2018 www.publish.csiro.au/journals/rs 10.1071/RS18004 THE MOYJIL SITE, SOUTH-WEST VICTORIA, AUSTRALIA: STRATIGRAPHIC AND GEOMORPHIC CONTEXT STEPHEN P. CAREY1, JOHN E. SHERWOOD2, MEGAN KAY1, IAN J. MCNIVEN3 AND JAMES M. BOWLER4 1School of Science, Engineering and Information Technology, Federation University Australia, PO Box 663, Ballarat, Victoria 3353, Australia 2School of Life and Environmental Sciences, Deakin University, PO Box 423, Warrnambool, Victoria 3280, Australia 3ARC Centre of Excellence for Australian Biodiversity and Heritage, Monash Indigenous Studies Centre, Monash University, Melbourne, Victoria 3800, Australia 4School of Earth Sciences, The University of Melbourne, Victoria 3010, Australia Correspondence: Stephen Carey, [email protected] ABSTRACT: Shelly deposits at Moyjil (Point Ritchie, Warrnambool), Victoria, together with ages determined from a variety of techniques, have long excited interest in the possibility of a preserved early human influence in far south-eastern Australia. This paper presents a detailed analysis of the stratigraphy of the host Bridgewater Formation (Pleistocene) at Moyjil and provides the context to the shelly deposits, evidence of fire and geochronological sampling. We have identified five superposed calcarenite–palaeosol units in the Bridgewater Formation, together with two prominent erosional surfaces that may have hosted intensive human activity. Part of the sequence is overlain by the Tower Hill Tuff, previously dated as 35 ka. Coastal marine erosion during the Last Interglacial highstand created a horizontal surface on which deposits of stones and shells subsequently accumulated. Parts of the erosional surface and some of the stones are blackened, perhaps by fire.