The Kew Historical Society has an extensive collection of maps and plans; most relating to the former City of Kew (1860-1994). Within this collection, this hand-drawn map is unique.The most important and earliest original map of Kew in the collection, showing places of interest in early Kew.Hand-coloured map on heavy paper, depicting from Kew in 1875 from memory by Jesse Dannock. The map includes the names of local institutions and old residents. These, and many of the street names are very faded and have been overwritten with biro at a later date.maps - kew (vic), mrs dannock's map, cartography

Gwen McWilliam is well known as an authority on the history of Boroondara and the author of a large number of books and pamphlets about the City. She was awarded the medal of the Order of Australia in 2001 ‘for service to the community of Hawthorn and district, particularly through the research, documentation and publication of its history.’ This map from her collection was donated to the Kew Historical SocietyPlan of Heidelberg, annotated with details about the occupancy pre and post European settlement. The plan also contains geological references. The plan is included and analysed in volume 2 of the Heidelberg Conservation Study (1985). The original plan was published created in 1982. Printed annotationscity of heidelberg, yarra valley, historic plans -- heidelberg

Set of 9 sheets containing a map of the "Sorrento Tramway", and 8 sheets of photographs including one of the horse tram from the collections of Norm Wadeson, A R Lyell, A Winzenried collections. The Map is dated 5/1983 by SM.Yields information the Sorrento tramway line and some of its operations.Set of 9 A4 sheets, printed or copied from a publication.tramways, maps, sorrento, horse tram

Information - on front cover - "CENTENARY EDITION/ BEERSHEBA/ TRAVELS THROUGH A FORGOTTEN AUSTRALIAN VICTORY/ PAUL DALEY/. A full-bodied, human telling of the deeds of the AUSTRALIAN LIGHT HORSEMAN/ TONY WRIGHT" On back cover. "It was a glorious triumph of arms for Australian/ Forces, a romantic moment of dash and bravura that/ stood out in the tragedy of World War 1. Yet it barely/ registers in Australia's national consciousness."Soft cover book. Cover - cardboard; black, gold and white print on front, spine and back. White background. Illustrated - front - black and white photograph of a trooper mounted on a horse with full kit. 339 pages, cut, plain, white paper. Illustrated - black and white diagrams of maps and centrefold collection of photographs. Inscription - front end paper.Front end paper - handwritten, black ink - donor's name and date, "Donated by Joy Wellings/ 16-8-2023".books, ww1, beersheba, australian army, light horse regiment.

Document. KELLY & ALLSOP COLLECTION. Map of the Hustlers Line of Reef, Bendigo (South portion). Issued by Wood & McNair, Sharebrokers, Beehive Chambers, Bendigo and High St., Eaglehawk. Mines shown on map are Fortuna Hustler's Co., Hustler's Royal Reserve No.2, Great Extended Hustlers Co., Hustlers Reef Co., Hustler's Reef No.1 Co., United Hustler's & Redan Co. Number of shares is listed against each of these mines.Wood & McNairbusiness, stockbroker, kelly & allsop, kelly & allsop collection, hustlers line of reef map, wood & mcnair.

Joan O'Shea Collection. Goldfield Maps Dunolly 3 Sheets 1980. Page 1: Mines in Dunolly, Whistling Flat, Painswick and Surrounds. Page 2: Mines in Goldsborough, McKinnons Gap, Bealiba Range, Stewarts Flat and Surrounds. Page 3: Mines in Dunolly, Emu Creek, Bet Bet, Bromley & Surrounds. Scale in Chains and Kilometres.GoldField Maps 1980 based on Dunolly 7624 by Division of National Mappinggold, goldfields, goldfield maps dunolly & surrounds

Warrnambool Tourist Maps collected over the years by Warrnambool Historical Society membersPreservation of local maps for historical purposesEnclosed in A4 size plastic envelopes in an A4 size archival box and numbered and catalogued according to the date of acquisition.This collection has 16 pamphlets containing maps of Warrnambool and district and some accompanying printed materialwarrnambool tourism, city of warrnambool, shipwreck coast tourismwarrnambool tourism, city of warrnambool, shipwreck coast tourism

Material relating to the Shire of Eltham War Memorial located at Garden Hill, Kangaroo Ground. Also known as The Eltham Shire War Memorial Tower, Shire of Eltham Soldiers' Memorial and Kangaroo Ground War Memorial Park. Includes photocopies, newspaper clippings, correspondence and more beginning from early history 1919-2009. Contents: Archive Box 1 Folder 1 (Publication Proofs) The Tower of Remembrance and War Memorial Park On Garden Hill at Kangaroo Ground, Victoria 1919-2010 Folder 2 (Up to 1960) 1. Binder with plastic pockets. Photocopies. Minutes of the Kangaroo Ground War Memorial Bazaar Committee, 1922-1926 EDHS Newsletter No. 123 November 1998 PRESIDENT'S REPORT ACQUISITION FROM NILLUMBIK SHIRE'S MEMORABILIA Recently found in a storage box of old Shire of Eltham items was a school size, blue lined black covered writing book. It is recognized as the minute book and cash receipt book of the period 1922-1926 when the Memorial Park Committee, who it seems were part of the Shire of Eltham Soldier's Memorial League, was requested to raise funds for building the Shire of Eltham War Memorial Tower at Kangaroo Ground. History tells us that the tower, which is currently being refurbished, was officially opened by the Governor General of Australia, Lord Stonehaven on 11.11.26. The ladies invited to the first meeting at the Shire Hall did so on 21st September 1922. The minutes book reads: Present: Mesdames Bell, Bourchier, McMahon, Gosling, Cockcroft, Wraight, E Coutie, R Rogers, A Jones, AH White, Davies, Everitt and the Misses Lacey, Harris, N Weller, Gosling, Bell and D and G J Bourchier. These people became the Kangaroo Ground Memorial Bazaar Committee along with others named at further meetings. They conditionally accepted the role of raising funds, their condition being that the Bazaar Committee be given representation on any committee empowered to deal with the memorial in proportion to the amount of money raised by the bazaar'. The Andrew Ross Museum has the original book. We at Eltham District Historical Society have two photocopies for public perusal. 2. Transcriptions of newspaper articles 1919-1920. 6 pages. 3. Photocopy of program for thanksgiving service July 6th, 1919 held at Public Hall, Panton Hill. 4. Photocopies: a. Kangaroo Ground, The Advertiser, 17 Oct 1919 (working bee) b. The Advertiser August 1920 – advertisement for coach between Eltham and KG. c. Anzac Memorial Service, The Eltham & Whittlesea Shires Advertiser & Diamond Creek Advertiser, April 14, 1922 and April 28, 1922 d. Anzac Day services. April 27, 1923 e. Photocopy Anzac Commemoration, local newspaper, May 2, 1924 f. Shire of Eltham Memorial Service, The Advertiser April 23, 1926 g. Eltham Shire War Memorial Advertiser August 13,1926 h. Eltham Shire War Memorial The Advertiser October 26, 1926 i. Eltham The Advertiser, December 17, 1926 j. Kangaroo Ground April 26, 1929 5. Photocopy. Eltham War Memorial Tower article, The Advertiser, November 19, 1926 6. Typed transcription of parts of newspaper articles for three titles, November 1926 7. Transcription. Public Notice, October 16, 1926 8. Photocopy Kangaroo Ground Armistice Day local newspaper, November 25, 1927 9. Photocopy Kangaroo Ground Armistice Day local newspaper, November 16, 1928 10. Photocopy Kangaroo Ground, local newspaper, April 26 1929 11. 3 Original Copies. One Hardback. Dedication of memorial official brochure, 1951 original but damaged 12. Photocopy with notes from G.G. relating to the land transfer/acquisition/contract via White and Gepp. Folder 3 (1961-1970) 1. Original newspaper article: Place with a view at Kangaroo Ground, The Age, May 11, 1963, p18 Folder 4 (1981-1990) 1. Newspaper article, Memorial a fire watch. Diamond Valley News, March 16, 1982, 2 original copies. 2. Newspaper article. An Obvious Monument by Russell Yeoman article with photo: Network Nov/Dec 1984, p14. Folder 5 (1991-2000) 1. Original newspaper article: “Kangaroo Ground Tower is top spot”. Thought to be from a tourist information free newspaper, Mountain Country, Summer [1993] p39. 2. Newspaper article with reference to quoins – a contrasting edging or corner stone on the façade of a stone or brick house. Age August 2000 3. Program. Service program for Remembrance Day commemoration ceremony, 1996. 4. Speech by Harry Gilham for Remembrance Day commemoration ceremony, 1996 5. Newspaper article: Remembrance, Diamond Valley News, 20 November 1996 6. Word Document. A Tower of Strength by Dean Stewart April 1997 7. Newspaper articles: Tower group needed, Diamond Valley News, September 17, 1997, p3 and advertisement “Nillumbik, Nominations for Kangaroo Ground Memorial Tower and Grounds Advisory Committee”, Diamond Valley News, September 17, 1997 8. Newspaper article: Council apology; scaling new heights, 1997 about Aboriginal Reconciliation. Probably Diamond Valley News ca 1997. 9. Photocopy / Newspaper Article: Two newspaper clippings, “Memorial with a view” 30 April 1997 and “Funds boost to restore tower to its former glory”, Diamond Valley News, 3 December 1997. 10. Newspaper article: Kangaroo Ground Tower of Remembrance Nillumbik Mail, 9th August 2000 and Research notes (July 2000) by Harry Gilham pertaining to photo in August 2000 newspaper article. 11. Photocopy. Newspaper article: New lease of life for tower (Concept plan) Nillumbik Mail, September 27, 2000 12. Photocopy: 4 pages, War Memorials of Victoria; a pictorial record, c.1994 Folder 6 (2001-2010) 1. Newspaper article: $10,000 to start refurbishment, Nillumbik Mail, Feb 21, 2001 2. Circular. KG War Memorial Advisory committee circular August 2001 3. Newspaper article: Tower group retained 4. Program for re-dedication of the Kangaroo Ground War Memorial Tower 8th November 2001 with copies of pages 65-70 of from The Tower of Remembrance and War Memorial Park 1919-2001 (see Folder 1) - Speaking notes from the day from Nillumbik Shire Mayor, Cr. Sigmund Jorgensen and Harry Gilham and Speech by John Landy, Governor of Victoria 5. 2 pages of Harry Gilham notes – Draft of ‘book’ notes ‘Thank you’ for rededication ceremony to be held Thursday, Nov 8, 2001 - list of invitations, notifications and acknowledgements. 6. Proposed running sheet. Re-dedication of KGT. November 8, 2001 7. Newspaper article (2 copies) Century of war service, DVL November 14, 2001 page 6 8. Letter. Gov. John Landy to Harry Gilham. Thank you for visit. [2001] 9. Newsletter Clipping: Governor of Victoria re-dedicates KG War memorial Tower, Nillumbik News (NSC) Christmas 2001 10. Newspaper article: War Memorial to be restored: DVL November 19, 2003 11. Newspaper article: Memorial Facelift Sept 29 2004. 12. Folder. Collection of maps and context Yarra Water proposal to build water tanks 13. Newspaper clipping. Pressure on with new tank. Re installation of water tank near site. DVL March 2, 2005 14. Folder of emails and designs from Dennis Ward re poppies and prostrate rosemary for formal garden around base of tower April 2005 15. Folder. Letters and paperwork re the Victorian Government “Community Cabinet” and invitation for community groups to speak directly with a government minister. Actual submission not included in folder. 16. Newspaper clipping. Time to remember among the poppies, Diamond Valley Leader, 9 November 2005, p1 and 17. Newspaper clipping. Lone pine company for souls. DVL 9 November 2005 18. Folder. Restoring Community War Memorials Grants Program. Application and associated paperwork 2005/2006 January 2006 19. Newspaper article. Shared views. Valley Weekly, June 21 2006 20. Newspaper article: Kangaroo Ground, Restoration on schedule, DVL October 2006? 21. Newspaper article. Towering over the terrain. The Age August 8, 2009 22. Photocopy. Nillumbik Shire Council. Policy and service report re lease of land to Victoria Police for police radio communications and re-building of radio tower. December 9, 2009 23. Schematics: A3 photocopies, Kangaroo Ground memorial Tower, front and rear view, Tom Manley, 17 Apr 2001 Folder 7 (2011 on) 1. Magazine article and cover. Cover story – The Kangaroo Ground Memorial Tower, The Genealogist, March 2010 2. Newspaper article. (2 copies) Photo and caption. Diamond Valley Leader, July 14, 2010 3. Newspaper notice: Notice of application for a planning permit to construct radio communications tower, DVL, October 10, 2012 4. Copy. Reference enquiry to National Film and Sound Archive. 10 September 2012 5. Copy letter. Quotation/estimate for Shire of Nillumbik on renovation and underpinning of old care takers cottage, KG. 30 September, 2012 6. Story. The Kangaroo Ground Tower of Remembrance by Amy Shaw. Yarrambat Primary School Year 6 History speech, 2014. 7. Program: Remembrance Day service, 11th November 2014 8. Newspaper article. Tribute to bravery DVL, November 19, 2014. 9. Minutes. MAC meeting. 2 September 2016. Folder 8 (Interpretative Signs Grant 2000-2001) 1. Folder. Various including Letters. EDHS Grant project: Kangaroo Ground Park and Tower of Remembrance interpretative signage from Parks Victoria 2000-2001. Folder 9 (Miscellaneous) 1. Folder Gilham collection. Google earth images of Tower, Extract describing history of Tower, including honour roll for WW1 and WW2, 8 pages, Extract describing history of Tower, including honour roll for WW1 and WW2, 3 pages, 2002 and 2004; Kangaroo Ground Tower; Southwell-Keely M.; WAR MEMORIALS IN AUSTRALIA; 8 pages, https://web.archive.org/web/20080722161554/http://www.skp.com.au/memorials2/pages/30054.htm) 2. Letter. Undated, unsigned re application to council to proposed work to police radio masts behind caretaker’s cottage. 3. Brochure: Heritage Nillumbik. Includes cover photo and other information about site. Published by Nillumbik Shire Council. About 2006. 4. Folder of notes and photocopies of various Certificates of Title for property 5. Inward loan documents. Two. Andrew Ross Museum inward loan for collection items from “War Memorial Tower” 2003 6. Photocopies of postcards of Soldiers War Memorial: One taken c.1926 before completion around base, on colour print on paper (enlarged) of Soldiers War Memorial postcard c.1930s prior to gun placements with typed text pasted on and additional detail version mounted on card with handwritten explanatory notes by Harry Gilham. 7. Photocopy of photo of tower 1944 with guns in place from Gordon and explanatory notes plus A4 photo paper print of image (photoshopped cleaned up). 8. Miscellaneous photocopies of photos taken by Harry Gilham of Memorial Park entrance, model tower in font of tower entrance, caretaker’s cottage, spiral staircase, Menin Gate sign and possibly planting of Lone Pine. Folder 10 (Fire Spotting Operations) 1. Biographical notes on Herman Motschall 1969-1981 2. Newspaper article, Memorial Tower top site for fire spotter, Diamond Valley News, May 15, 1973. 3. Proper Officer's report on an addition to the Kangaroo Ground Memorial Tower for Fire Spotting purposes: "This report covers the history of the tower, its uses, and reasons why it should be put to greater use, benefiting the Shire Council and ratepayers" Includes detailed commentary around the proposal to use the Shire of Eltham War Memorial at Kangaroo Ground for fire spotting. From Shire of Eltham archives. H. J. Masefield Property Officer. 4. Eltham Shire Council meetings 14 and 24 September 1973 references to fire watching facilities. Summary of end of season reports from spotters 1965-1973. 5. Newspaper clipping; Memorial a fire watch by Marguerite Marshall Diamond Valley News 16 March 1982 6. Letter: Cover letter from Dennis Ward 20 Feb 2006 architect for CFA Cabin design and Proposal to upgrade the fire spotting cabin, 2007 including a cost and concept plan dated 7 February 2009. 7. Newspaper article. From that first puff of smoke – horror. Diamond Valley Leader, Feb 25, 2009, p. 7 8. Invitation: State Government announcement of refurbishment of KGWM Fire spotting tower 19 October 2009 9. Newspaper article. Tower– up, Black Saturday watch. Cover and page. Diamond Valley Leader, October 28, 2009 10. Invitation. Opening of newly upgraded fire spotting tower, 11 April 2010 11. Newspaper article. Incredible luxury at fire spotting tower, Diamond Valley Leader, April 21, 2010, p, 5 12. Printout of plan of base of tower including comms cabinet and ladder to CFA cabin. Dated 17/6/2010   Archive Box 2 Folder 11 (Moor-rul Viewing Platform) 1. Agenda. Planning and building committee 12 March 2003 Application for construction of a viewing platform and road entry refurbishment and coach parking bay. 2. Envelope. Letters, paperwork and emails, mainly from Dennis Ward re roof design for the viewing platform and order for poppy seeds. 2005 3. Newspaper article (enlarged and laminated). Stolen Red gum seats sap new project’s momentum. (Local paper), April 3, 2007 4. Convenor’s Notes – Opening of the Viewing Platform at Kangaroo Ground, Shire of Nillumbik 5. Folder. Nillumbik Reconciliation Charter. Opening of the Moor-rul viewing platform 17.4.2008. Compiled by Harry Gilham. Includes newspaper clipping, speech, photocopy of photos with captions. 6. Newspaper article. View from the hill is a thrill. Heidelberg and Diamond Valley Weekly, April 22, 2008 7. Newspaper article. A platform towards reconciliation. Diamond Valley Leader, 23 April 2008. 8. Newspaper article: 6 reasons to visit Hurstbridge, The Age, Jun 6 2012 9. Article: Aboriginal cultural values and heritage management issues 10. Folder: Material relating to design and construction of viewing platform Folder 12 - Shire of Nillumbik Advisory Committee 1. 2011 Diary, Harry Gilham, Kangaroo Ground Advisory Committee 2. Photocopy. Newspaper clipping. Nillumbik Council seeking nominations for new Kangaroo Ground Memorial Tower and grounds advisory committee. DVN 17 Sept 1997 3. Letter. From NSC to Dean Stewart re heritage listing status. 12 July 1998. 4. Business paper for NSC Council meeting: KG Memorial Tower and Grounds advisory committee, 12 March 2002. Includes Terms of Reference Folder 13 - Friends of Kangaroo Ground War Memorial Park Inc. 1. KG Tower and land occupational health & Safety (guidelines) for volunteers 2. Supplementary notes (not related to fire spotting) from Friends group or advisory group of Kangaroo Ground War Memorial Park including design of seating, proposed budget for works, hand written notes from meeting by H.G. about 1999. Folder 14 - Soldiers. 1. Folder of material pertaining to men from the Shire of Eltham who enlisted in WW1 and for whom the Shire of Eltham War Memorial was dedicated. 2. Folder on residents from Shire of Eltham who died in WW2 1939-1945 with listings of each from Commonwealth War Graves Commission, WW2 Nominal Roll for Eltham 3. Newspaper article: Mates join to recall past, Diamond Valley News, November 16, 1994 4. Newspaper article: Board replaced, Diamond Valley News, September 2, 1998 about Hurstbridge RSL Honour Roll Board 5. Newspaper article: Keeping the memories alive; VP Day honoured, Valley Weekly, August 17, 2005 6. Newspaper article: In our hearts; Tributes for war heroes, Diamond Valley Leader, November 9, 2005, p1 7. Newspaper article: Service honoured, Diamond Valley News, Leader, April 23, 2008 8. Newspaper article: Salute to last men standing, Diamond Valley Leader, April 20, 2011, p1 and Last of the world warriors, pp8-9 9. Newspaper article: We will remember, Diamond Valley Leader, April 25, 2012, p3 10. Newspaper article: Family legacy builds whole town, Diamond Valley Leader, Oct, 2013, p15 11. Photos and details of Honour Boards in the shire 12. Miscellaneous notes by Harry Gilham Folder 15 – Welcome Home Committee Meeting Minutes. 1. Extracts from Welcome Home Committee Meeting Minutes 18 August 1917 to 14 August 1919. Folder 16 – World War One Local Enlistments. 1. Lever arch binder containing records of local enlistments by name from the Diamond Valley including extracts from Commonwealth War Graves Commission records. Includes Newspaper article clipping "Digger's marker of respect: Temporary cross a poignant find after eight decades in dusty garage"; Sunday Herald Sun, November 10, 2024, p33 concerning Private Harry Conway who died April 1918 and whose tempory grave marker cros now housed at Montmorency-Eltham RSL. Archive Box with documentsharry gilham collection, fire spotting, kangaroo ground, shire of eltham war memorial, masefield h. j., cfa, kangaroo ground war memorial park, shire of eltham soldiers' memorial, eltham shire war memorial tower, harry conway, montmorency-eltham rsl sub-branch

Malachite is typically found as crystalline aggregates or crusts, often banded in appearance, like agates. It is also often found as botryoidal clusters of radiating crystals, and as mammillary aggregates as well. Single crystals and clusters of distinguishable crystals are uncommon, but when found they are typically acicular to prismatic. It is also frequently found as a pseudomorph after Azurite crystals, which are generally more tabular in shape. This particular specimen was recovered from the Burra Burra Copper Mine in Burra, South Australia. Otherwise known as the 'Monster Mine', the Burra Burra Copper Mine was first established in 1848 upon the discovery of copper deposits in 1845. Within a few short years, people from around the world migrated to Burra to lay their claim in the copper economy. By April 1848 the mine was employing over 567 people and supporting a population of 1,500 in the local township. Up until 1860, the mine was the largest metals mine in Australia, producing approximately 50,000 tonnes of copper between 1845 to its closure in 1877. The Burra Burra Mine was also famous for a number of other specimens, including; crystalline azurite, cuprite, and botryoidal and malachite. Malachite is considered a rare gemstone in that the original deposits for the stones have been depleted leaving behind very few sources. In addition, the use of Malachite as gemstones and sculptural materials remains just as popular today as they were throughout history. It is quite common to cut the stone into beads for jewellery. The fact that Malachite has such a rich colour and one that does not fade with time or when exposed to light makes it particularly rare. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study. A solid hand-sized copper carbonate hydroxide mineral with shades of blue and light green throughout. burke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, mineralogy, burra, burra burra mine, south australia, malachite, malachite specimen

Malachite is a green copper carbonate hydroxide mineral and was one of the first ores used to make copper metal. Malachite has been utilised as a gemstone and sculptural material in the past as its distinctive green color does not fade when exposed to light or after long periods of time. Malachite is formed at shallow depths in the ground, in the oxidizing zone above copper deposits. The material has also been used as a pigment for painting throughout history. This particular specimen was recovered from the Burra Burra Copper Mine in Burra, South Australia. Otherwise known as the 'Monster Mine', the Burra Burra Copper Mine was first established in 1848 upon the discovery of copper deposits in 1845. Within a few short years, people from around the world migrated to Burra to lay their claim in the copper economy. By April 1848 the mine was employing over 567 people and supporting a population of 1,500 in the local township. Up until 1860, the mine was the largest metals mine in Australia, producing approximately 50,000 tonnes of copper between 1845 to its closure in 1877. The Burra Burra Mine was also famous for a number of other specimens, including; crystalline azurite, cuprite, and botryoidal and malachite.Malachite is considered a rare gemstone in that the original deposits for the stones have been depleted leaving behind very few sources. In addition, the use of Malachite as gemstones and sculptural materials remains just as popular today as they were throughout history. It is quite common to cut the stone into beads for jewellery. The fact that Malachite has such a rich colour and one that does not fade with time or when exposed to light makes it particularly rare. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study. A solid hand-sized copper carbonate hydroxide mineral with shades of yellow, blue, and light green throughout.geological, geological specimen, burke museum, indigo shire, malachite, malachite specimen, burra burra mine, burra, south australia, australian mines, mines, monster mine

Galena Chalcopyrite is the earth's primary ore of lead and is mined from a large number of deposits in many countries. It is also an important source of silver. Galena Chalcopyrite is one of the most abundant and widely distributed sulfide minerals across the world. The mineral is found in igneous and metamorphic rocks in medium- to low-temperature hydrothermal veins. This specific specimen was recovered from the mines in Broken Hill, New South Wales. The mines in Broken Hill were first established after Charles Rasp discovered a large amount of silver-lead-zinc ore-body in the area in 1883. BHP (Broken Hill Proprietary) mining company was then established in 1885 and quickly became the lead in Australia's mining industry after they began excavating and exporting the country's largest amount of lead, silver, and zinc. This feat generated over $100 billion in wealth for the company.Galena Chalcopyrite is signifiant as it represents the catalyst for the rise of Australia's most influential mining companies - BHP. The mineral was one of the first to be mined in the country and after being made into lead, was used for a variety of things such as paint, batteries, ammunition, and plumbing materials before it was known to be harmful to humans. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study. A grey, solid hand-sized lead sulfide mineral with a silver metallic luster.burke museum, beechworth, geological, geological specimen, galena, galena chalcopyrite, chalcopyrite, broken hill, bhp, bhp mining, broken hill mine, mine, australia mine, lead, lead mine

Feldspathic arenites are sandstones that contain less than 90% quartz, and more feldspar than unstable lithic fragments, and minor accessory minerals.Feldspathic sandstones are commonly immature or sub-mature.These sandstones occur in association with cratonic or stable shelf settings. Feldspathic sandstones are derived from granitic-type, primary crystalline, rocks. If the sandstone is dominantly plagioclase, then it is igneous in origin Sandstone features prominently in public buildings throughout Victoria. Most of the sandstone used as dimension stone in the State came from three sources: the Heatherlie quarry in the Grampians (Silurian), the Bacchus Marsh area (Permian), and the Barrabool Hills near Geelong (Cretaceous).Sandstone features prominently in public buildings throughout Victoria, making this specimen special as it shows the materials used by Victorian building companies. Sandstone can also be crushed, crushed stone is used in the construction of roadways and road structures such as bridges, and in buildings, both commercial and residential. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study. A feldspar-rich sandstone, a sandstone intermediate in composition between an arkosic sandstone and a quartz sandstone, containing 10% to 25% feldspar and less than 20% matrix material of clay, sericite, and chlorite. Feldspathic arenite containing less than 90 percent of the composition of quartz. Feldspar is the main composition. Feldspathic arenite may contain fragments of unstable rock, and a little amount of other minerals such as mica and heavy minerals. Some feldspathic arenite have pink or red color because of the presence of potassium feldspar or iron oxide. There are also colored light gray to white. These sandstones are usually medium to coarse grained and can contain a high percentage of granules with angular until subangular roundness. The content of the matrix can appear as the rest up to more than 15 percent, and sorting of grains can present as moderate to poorly sorted. Feldspathic sandstones are generally immature in textural maturity. Feldspathic arenite can not be judged from the structure of the sediment. Bedding can emerge from the laminate parallel to the crossbed. Fossils may appear in the layer deposited on the sea. Feldspathic arenites usually appear on the craton or the continental shelf, which can be associated with conglomerate, quartz lithic arenite, carbonate rock, or evaporites. This sandstone may also appear on the succession of sedimentary basins deposited on an unstable or deep sea, and moving arc setting. According to Pettijohn (1963) Arkose make up about 15 percent of all sandstones. Some Arkose formed in situ when the granite and related rocks disintegrate and generate granular sediments. Most of the material feldspathic sandstones derived from primary crystalline granitic rocks, such as granite or metasomatic rocks containing abundant potassium feldspar. Mineral contained in sandstones is mostly a form of plagioclase feldspar derived from quartz diorite or volcanic rock. Feldspar contained on this sandstone comes from arid to cool climates when the chemical weathering process is reduced.sandstone, natural stone, feldspathic sandstone, burke museum, geology, geological, geological specimen

Ilvaite has acquired its name from Ilva (Latin for Elba) Island, Greece, where Ilvaite is most commonly found. The geological setting in which Ilvaite occurs is through contact with magnetite, zinc and copper ore deposits, along with contact metamorphic deposits and zeolite zones. llvaite crystallizes in the form of black prismatic crystals and columns . This specimen was retrieved from Broken hill, known as the world's richest and largest zinc-lead ore deposit. Because of Ilvaite's often unaesthetic crystal formations compared to other minerals, Ilvaite is uncommon in most rock collections, particularly specimens that are not well formed, such as this one. Ilvaite is also a member of the Sorosilicate subclass of the silicate minerals, which have an unusual basic unit of Si2O7, making Ilvaite a unique mineral. Given that Ilvaite is not commonly found in Australia, it marks a unique contribution to an Australian collection of minerals. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A solid hand-sized ferrous iron analogue mineral with of black with shades of beige Ilvaite is a brittle, opaque rock formation that has acquired its name from Ilva (Latin for Elba) Island, Greece, where Ilvaite is most commonly found. The geological setting in which Ilvaite occurs is through contact with magnetite, zinc and copper ore deposits, along with contact metamorphic deposits and zeolite zones. llvaite crystallizes in the form of black prismatic crystals and columns rock, mineral, ilvaite, ilvaite specimen

This specimen was recovered from the Nigretta Falls (previously named the Upper Wannon Falls), Victoria. The falls are fed by the Wannon River that has its head waters in the Grampians mountains. Approx. 10km upstream of the Wannon Falls, Nigretta is a multi-channel segmented cascade of smaller drops and bounces guided by patterns of joints in a much older (Devonian) rhyolitic volcanic rock. Both the Wannon and Nigretta Falls are iconic landscape features, entrenched in the history and identity of the region. These falls are particularly rare as they are the product of volcanic activity, which is unique in the context of the Volcanic Plain of Victoria. Waterfalls of this capacity are generally associated with the Uplands areas of Victoria, rather than the edges of the Volcanic Plain. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study. A solid, dark grey mineral specimen with pale terracotta coloured inclusions. Rhyodacite is a volcanic rock intermediate in composition between dacite and rhyolite. Rhyodacites form from rapid cooling of lava relatively rich in silica and low in alkali metal oxides.GEOLOGICAL SURVEY / R / S 55 FELSTONE PORPHYburke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, porphyritic rhyodacite, lava, nigretta falls, upper wannon falls, dacite, rhyolite, volcanic geology

Rhodonite is a reddish-pink manganese silicate material and often contains iron, magnesium and calcium. It is usually found in metamorphic rocks (rocks which have been altered by heat, pressure or chemical process). It can range in size from tiny to massive. Because of their composition they are not suitable for use in jewellery because they are hard enough. It is quite rare to find, though has been found in Australia, North America, South America and Europe.This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study. This specimen is a palm shaped piece of loellingite within rhodonite. It is mostly reddish-pink coloured, with flecks of light and dark grey. Loellingite is a grey iron arsenide which often forms into crystal shapes. It is mostly found in mesothermal veins (caused by immense heat) with sulfides or in limestone. It is toxic when heated or struck. rhodonite, loellingite, burke museum, beechworth, geological survey of victoria

This specimen was recovered from Silverton Mine in Broken Hill, New South Wales. Otherwise known as the 'Day Dream Mine', the Silverton Mine was first established in 1883, when silver and lead deposits where discovered. Within a few short years, the population of Broken Hill reached 3000 people. As of today the Silverton Mine is still open, and has produced over 200 million tonnes of ore, which has generated over $100 billion. The Silverton Mine was also famous for a number of specimens such as silver, iron and zinc.Copper is considered to be a rare ore in that finding it in its pure form is rare. Nowadays when mining for Copper it is often found in mixed in with other minerals or it is recycled from use. Moreover, Copper is found in a range of everyday uses such as coins, cookware, pipes, heating conductors and anything that generate electricity. The fact that Copper is heat a heat conductor, electricity conductor and it does not corrode easily, makes this ore a versatile and useful. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A solid hand-sized cube-shaped sulfide and oxide with shades of green, grey and brown throughout. Copper is typically found as nuggets in the ground. It can be found in a range of forms such as its native state; mixed with other ores, such as zinc and iron; as porphyry copper deposits; and as major deposits. Porphyry deposits are when the mineral is scattered evenly throughout the rock. Major deposits are when the mineral is scattered amongst other minerals.burke museum, beechworth, indigo shire, beechworth musum, geological, geological specimen, mineraology, copper, copper ore, copper ore speciment, broken hill, new south wales

According to the 1912 Department of Mines Bulletin of the Geological Survey of Victoria, basalt covers a considerable portion of the Macedon area including Mount Macedon. Basalt is the most common form of rock underlying the earth's surface and is found in three kinds of rock forming environments: ocean divergent boundaries, oceanic hotspots, and mantle plumes and hotspots beneath continents.This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A solid mass, geological specimen in shades of grey and white. Hyalite is a colourless variety of opal. It occurs as globular and botryoidal masses and irregular crusts in volcanic and pegmatite environments where the silica deposits from the gas phase. Basalt is dark in colour, fine-grained igneous rock composed of plagioclase and pyroxene minerals. It is commonly formed as an extrusive rock, such as lava flow. It is one of the most common forms of rock underlying the earth's surface.burke museum, geological specimen, department of mines, geological survey of victoria, basalt, mount macedon, beechworth

This particular specimen was recovered from the Lal Lal Coal and Iron Mine in Victoria, 19km from Ballarat. Brown Coal was discovered here in 1857, just alongside the Geelong to Ballarat Railway line. This discovery of lignite (brown coal) was the first in Victoria, which would bring important benefits to the region and state, both of which had previously been reliant on coal imports. In the 1860s, iron ore was found just 5km from Lal Lal, and the area was converted into an Iron Ore Mine. The Lal Lal Iron Mining Company took over operations in 1874, who then peaked iron production in 1884. This mine continued operations until June 1884, when the blast furnace was extinguished and never recommenced. The blast furnace at Lal Lal is considered one of the most important and highly significant sites ion early industrial history in Australia, as it is the only remaining best furnace from the nineteenth century in the Southern Hemisphere. The furnace ruins are 17 metres high, and are clearly visible today on Iron Mine Road, Lal Lal, near the Bungal Dam. This specimen of Lignite (brown coal) is significant, as it was mined from the area where brown coal was first discovered in Victoria, leading to an important and controversial future of the mining and use of brown coal in this State. The Victorian Heritage Database has listed the Lal Lal Coal Mine with local significance, with their Statement of Significance stating: "The Lal Lal coal mine is historically significant as the site of the first discovery of lignite (brown coal) in Victoria, and one that promised important benefits to regional and state industries that were reliant on coal imports at the time. The significance of the stie is reduced by the poor state of preservation of the coal mining and processing fabric". This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A hand-sized light-weight, soft and combustable sedimentary rock specimen, that is dark brown in colour. The specimen has jagged edges, as though parts of the rock have crumbled away. Brown coal, or Lignite, is formed naturally from compressed peat, and is typically found in natural basins. The stages to the formation of coal ('coalification') begin with plant material and wood, which will decay if it is not subjected to deep burial or heating, and turn into Peat. Peat, when sufficiently compressed naturally, will turn into Brown Coal (Lignite), and finally into Black Coal (sub-bituminous, bituminous and anthracite). Each successive stage has a higher energy content and lower water content. It is brownish-black in colour. Brown Coal has a high moisture content, between 50 and 75 percent, and a low carbon content. Some Brown Coals may be stratified, with layers of plant matter, which means little coalification has occurred beyond the peat natural processing stage. When Brown Coal is submerged in dilute nitric acid or boiling potassium hydroxide solution, it reacts to produce a reddish solution, of which higher-ranked coals do not. When brown coal is pulverised and burned in boilers, the steam is used to drive turbines, which generates electricity. It is the lowest rank of coal, as when burned, it creates a relatively low heat content, which in turn does not create a great output of steam. burke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, mineralogy, brown coal, brown coal specimen, lignite, lal lal, lal lal coal mine, lal lal iron mine, ballarat, blast furnace

Gabo Island sits off the coast of East Gippsland in Victoria, with cliffs of granite in a relatively unique red/pink colour. Early attempts to build a lighthouse on the island were abandoned due to poor foundations, but when a ship ran aground on the nearby Tullaberga Island in 1853 and led to the death of 37 people, efforts were reignited. Construction of a new lighthouse was completed by 1858, using Gabo Island granite. The lighthouse is Australia's second tallest in Australia and continues to play an important role in guiding boats around the coast as they journey between Melbourne and Sydney. The distinct pink colour from the granite means the lighthouse continues to be a defining feature of the island. Gabo Island granite was also used to construct the Treasury Building at 117 Macquarie Street in Sydney, now the Intercontinental Hotel.Granite in the pink colour of this specimen is relatively rare. The connection to the lighthouse on Gabo Island also gives the specimen historic significance and social significance regarding the maritime history of Victoria. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A solid palm-sized mineral, coloured by flecks of pink, red, and grey. Granite is formed by the slow crystallisation of magma below the earth's surface. It is typically composed of a mix of quartz, feldspar, and other minerals, though syenitic granite like this sample has a smaller amount of quartz than typical granite. This different mineral composition leads to the more distinct pink and red colouring.First sticker: [torn]logical survey / R........ S........ / Loc Gabo Island / 1/4 Sheet / Second Sticker: 15 Third Sticker: Syenitic Graniteburke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, mineralogy, gabo island, gabo island lighthouse, lighthouse, granite, coast, coastal, granite specimen, victoria, coastal cliffs

In Australia, precious opal is found in Cretaceous age sandstones and mudstones. These sedimentary rocks were deeply weathered and this weathering released silica into the groundwater.Australia is the only part of the world where opalised animal and plant fossils have been found. Opal artefacts several thousands of years old have been discovered in East Africa. As early as 250 BC the Romans prized opals, thought to have come from mines in Eastern Europe, the ancient world's main source of opals. There are many aboriginal dreamtime stories that feature opal. Australian opals discovered during the late 1800's found little favour with European markets but their commercial value increased in the 1900's and in 1932 Australia took over as the major producer of opals in the world and remains the largest producer to this day. Opal is found around the world (Brazil, Mexico, Honduras and the western US) however Australia produces 95% of the world's precious opal and it is our official national gemstone. Opal was first mined commercially at Listowel Downs in Queensland in 1875 and later at White Cliffs in NSW. Today, Coober Pedy (SA) is the main producer of white opal, though in recent years this field has expanded and all types of opals are found. Other centres in SA include Andamooka and Mintabe. Lightning Ridge (NSW) is renowned for black opal and formerly White Cliffs was a large producer of high quality opal. Boulder opals (opals in concretionary ironstone) are mined in Queensland from numerous localities in a zone extending from the Eulo and Cunnamulla district in the south and northwest for a distance of over 700 km to Kynuna in the north. The towns of Quilpie, Yowah and Winton are the main opal mining and wholesale centres. Opals are considered gemstones and have been used in jewellery for thousands of years.Throughout much of history, opals were actually believed to be good luck. The Romans thought that opals were one of the luckiest gemstones and a symbol of hope. In the Middle Ages, opals were believed to be bestowed with all the positive properties of coloured gemstones due to its rainbow-like play of colour. Finally, there is a superstition that you should not wear an opal unless it is your birthstone otherwise misfortune will befall you. This, of course, is far-fetched, but the notion could have been promoted in the late 19th and early 20th Centuries by diamond traders who were trying to increase sales of diamonds and deter people from buying opals. Possibly related to this is the thought that you should set opal jewellery with diamonds as their powers of good fortune will override any negativity held by the opal. The great majority of opal does not show play of colour and is called common opal or potch however this is not the case with a precious opal. Opal is a precious gemstone, like rubies, emeralds or diamonds. Opal is rare, and it is expensive to prospect and mine for.Silica is one of the most common minerals on the planet, but precious opal is very rare – far more rare than diamonds. Precious opal is rare because the natural processes that create it rarely occur.Most (at least 95%) of the opal found by miners is common opal without gem colour. In Australia we call it potch. It can be white, grey, black or amber coloured. Even when a miner finds gem-coloured opal, most of it can’t be cut into gemstones because it’s too thin, or sandy. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.It is not known where this opal originated, except that it is probably from Victoria, as it has been recorded from many localities in the State. Common Opal is formed from silica-rich water circulating through rocks near the Earth’s surface. It consists of minute spheres of silica arranged in different ways. In common opal, the spheres are of different sizes and randomly arranged, unlike in precious opal where the spheres are of similar size and uniformly arranged in three dimensions. These differences account for common opal generally being translucent to opaque and without the play of colours, or opalescence, displayed by precious opal. Common opal is found in many localities and different geological environments throughout Australia and the world. Precious opal requires special conditions to form and is much less common. Australia produces most to the world’s precious opal. burke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, precious opal, opal, brazil, mexico, honduras, queensland, coober pedy, gemstones, jewellery, play-of-colour, light blue

Basalt is a common igneous rock that composes most of the Earth's surface and can be found on the Moon and other rocky planets of the Solar System. It is generally composed minerals such as calcic plagioclase, clinopyroxene and iron ore which form grains that are indistinguishable to the naked eye. It can be dark grey or black in colouring and sometimes may contain holes left by gas bubbles. Most of the Earth's basalt was produced in environments such as oceanic divergent boundaries, oceanic hotspots, and mantle plumes and hotspots beneath continents. Basalt is commonly used in construction where it is crushed and used for multiple purposes such as concrete aggregate, road base, or railroad ballast. Thin slabs of basalt can also be cut and used for floor tiles, stone monuments, and building veneer. This particular specimen was excavated from Talbot in Victoria, which was a small gold mining town established in 1852. As basalt is a common rock, it is not specific to Talbot. However, this specimen can be assumed to be of the Cainozoic age due to previous geomorphic surveys of the area. This particular type of Basalt was used mainly for roads due to the durability of the rock.Basalt holds significance due to the continued use of the rock from historic until present times. The rock has been utilised for many types of construction and is still used for the same purposes today. Basalt also has significance to the Earth and other rocky planets of the Solar System as it makes up most of the planet's surface. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A smaller than hand sized rock specimen which is dark grey in colour with small holes and white deposits across its surface.Geological survey / [illegible] /burke museum, beechworth, geological specimen, geology, basalt, basalt specemin, indigo shire, talbot, cainozoic, igneous rock

This specimen was recovered from Creswick in Victoria. Basalt is dark in colour, often black and has a fine grain. It is composed of plagioclase and pyroxene minerals and an igneous rock. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A cylindrical fine-grained piece of igneous rockburke museum, geological survey of victoria, geological specimen, geology

This specimen was recovered from Wonthaggi in Victoria. Coal is a sedimentary rock which is composed of peat after it has been exposed over millions of years. This is an example of Australian black coal which is used as either thermal or coking coal for electricity generation or manufacturing processes. It is predominantly composed of Carbon which is 'C' on the periodic table of elements. This early example of a coal sample, shows the important role that coal played/plays in Australia's energy generation and manufacturing processes. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.Small piece of black coal with museum original labelGeological survey / R..... S...../ Locality Cape Patterson coal specimen, burke museum, geological survey of victoria, geological specimen, geology

This particular specimen was recovered from two hundred feet down in the Golden Mile in Kalgoorlie, Western Australia. The Golden Mile, named after the estimated sixty million ounces of gold worth around one hundred billion dollars, was the birthplace of the largest gold rush in Australia almost one hundred and thirty years ago when William Brookman and Samuel Pearce leased the Great Boulder mine. The Golden Mile is also the home of the Super Pit, Australia's most well-known mine.The majority of gold deposits will form as a native metal, however, on occasion, it can form a compound with another element, in this case, sulphur. Therefore, this specimen is a rare example of gold naturally forming into a compound mineral with sulphur. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A small gold-sulphide ore mineral specimen in shades of silver and grey with flecks of gold. Precious metals are often found in Sulphide Ores, as sulphides usually bind to these metals. They are also extremely symmetrical in crystaline form. Gold-Sulphide Ore occurs when gold forms a natural compound with other elements. In this form, gold can be present in one of two ways. It can be fully immersed in the sulphide, or a portion may be partially free. This specimen has minimal gold visible, with only a few flecks being partially visible.burke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, mineralogy, gold-sulphide ore

This specimen originated from Mount Lyell on the west coast of Tasmania, where a large group of open cut and underground copper-silver-gold mines began operating in 1883. Between 1893-1994, the Mt Lyell Mining and Railway Company were responsible for operations. The Mt Lyell copper-gold mines produce some excellent crystallised specimens of chalcopyrite and other minerals. The deposits are generally considered to be of Cambrian volcanic origin, but there are indications of Devonian granitic influence on the ores, plus local remobilisation during Devonian deformation. Over 120 million tonnes of ore was produced from several workings, including the main Prince Lyell mine and the North Lyell mine, which was also of great importance. The Mount Lyell mines have a long history of human and environmental disasters, including the 1912 North Lyell fire that killed 42 miners, and two separate incidents in 2013 in which three people lost their lives. The environmental impacts from this complex of mines are extensive, with waste tailings and heavy metal contamination flowing directly into the King and Queen River catchments. In 1954, the eminent Australian historian, Geoffrey Blainey, published 'The Peaks of Lyell' which delves into the history of the 1912 North Mount Lyell Disaster.Chalcopyrite does not contain the most copper in its structure relative to other minerals, but it is the most important copper ore since it can be found in many localities and occurs in a variety of ore types. The brassy-yellow colours in Chalcopyrite mean it is often confused with pyrites and gold, leading to use of the term, "fool's gold." Chalcopyrite has been the primary ore of copper since smelting began five thousand years ago. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.This hand sized solid mineral specimen has shades of brass-yellow with spots of iridescent green-black tarnish. Chalcopyrite is a copper iron sulphide mineral and a major ore of copper common in sulphide veins and disseminated in igneous rocks. Chalcopyrite has a hardness of 3.5-4 on the Mohs Scale. It is a member of the tetragonal crystal system and has metallic lustre and opaque transparency.burke museum, beechworth, indigo shire, beechworth museum, geology, geological specimen, chalcopyrite, copper pyrites, copper mining, tasmanian geology, mount lyell, mount lyell mines, fools gold, mohs scale, crystals, minerals, historical geological collection, victorian geological survey, a.r.c selwyn, gold rush, van diemans land

This specimen is from Barefoot Hills, Victoria. Sandstones are economically important as major reservoirs for both petroleum and water, as building materials, and as valuable sources of metallic ores. Most significantly, they are the single most useful sedimentary rock type for deciphering Earth history. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A sedimentary rock composed mostly of quartz sand. Sandstone is the second most common sedimentary rock after shale. Sandstones consist of sand-sized grains principally quartz, feldspar and rock fragments. The two major classes of sandstone are arenite and wacke. the colour of sandstone varies from grey, yellow, red and white reflecting the variation in mineral content and cement and is gritty to touch (like sandpaper).Geological survey / R.... S 61 / Loc Bareboot Hills / Sheet / 24SE / 94 /burke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, mineralogy, sandstone, yellow sandstone, victoria, barefoot hills

This specimen was recovered from Philip Island in Victoria. Chalcedony is composed of Quartz and Silicon Dioxide represented as SIO2. It has and is still used as a gemstone for thousands of years. This is an excellent specimen Chalcedony that shows its aesthetic properties. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study. Uniquely shaped piece of Chalcedony with opening in the centerburke museum, beechworth, geological, geological specimen

Gold usually is found as a native metal, but it also forms minerals with tellurium, sulphur, or selenium. The gold-bearing minerals that contain tellurium are called tellurides. Kalgoorlie, Western Australia contains greater than 1500 tonnes of gold.Seventy to seventy-five percent of the deposit occurs as native gold, but a further twenty percent appears as tellurides. What remains is in the form of 'invisible' gold. Extracting gold from telluride minerals, such as calaverite, which contains around forty-two percent gold, has produced approximately three hundred tonnes of gold. Prior to 1896, rocks containing tellurides were not recognised as rich gold ores, and were discarded.This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A hand-sized silvery to pyrite-yellow striated mineral containing tellurium and goldburke museum, beechworth, beechworth museum, geological, geological specimen, mineralogy, telluride, tellurite, gold-bearing, kalgoorlie, tellurium

This specimen is from Broken Hill, NSW. Galena is a natural mineral form of lead sulphide and is often found associated with sphalerite, calcite, and fluorite. Galena is an important lead ore mineral, and, in some regions, it is also an important mineral associated with silver ore. Sphalerite is a sulphide mineral that is the main ore of zinc. Rhodonite is an uncommon mineral once used as an ore of manganese in India, however today the scarcity and fragility of the crystals mean it is primarily used as lapidary materials or mineral specimens. In 1883, Charles Rasp who was a boundary rider at the time, discovered what he thought were deposits of tin but were in fact samples of silver and lead. He and six others went on to set up the first mining company in Broken Hill (BHP). The ore body became the largest and richest of its kind in the world mining ore worth more than 42,000 pounds in its first year. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study. Galena contains lead and silver, Sphalerite contains zinc. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A hand-sized piece of Sphalerite and Galena with Rhodonite crystalsburke museum, beechworth, geological, geological specimen, galena, rhodonite, sphalerite, silver ore, manganese, lead sulphide, lead ore, zinc ore, lapidary, mineral specimen, broken hill, nsw

This specimen was found in Cape Patterson, Vic. Cape Paterson is a cape and seaside village located near the town of Wonthaggi, 132 kilometres southeast of Melbourne, in the Bass Coast Shire of Gippsland, Victoria, Australia. These dark, fossiliferous Mudstones were deposited in slow-moving water associated with sedimentary basins & continental shelves. They are rich in carbon which makes them almost black. This is typical of an anoxic, reducing environment such as deep water or stagnant conditions where carbon-rich material would remain unoxidised during subsequent deposition & diagenesis. it has an imprint of a leaf in the rock itself, displaying the fossil of the plant. This specimen is unique due to the leaf impression within the stone itself. Imprint fossils are formed from an organism moving in some way, leaving behind a trace or track. These tracks are preserved when the clay/silt dries slowly and is covered by other sediment. Plants can also leave imprint fossils when they are covered by sediment. The leaf tissue degrades, leaving an imprint of where the leaf once was. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.These dark, fossiliferous Mudstones were deposited in slow moving water associated with sedimentary basins & continental shelves. They are rich in carbon which makes them almost black. This is typical of an anoxic, reducing environment such as deep water or stagnant conditions where carbon rich material would remain unoxidised during subsequent deposition & diagenesis. FOSSILIFEROUS MUDSTONE / Locality: Cape Patterson, Victoria | Descriptive catalogue / Pg 27 No 95 / "Grey Clay, / Cape Paterson with leaf impressions' / 15/4/21 C. William /mudstone, cape patterson, leaf imprint, fossilised leaf, fossiliferous mudstone