Galena occurs in a range of deposit contexts, often in metalliferous veins, such as Broken Hill, Australia; Coeur d’Alene, Idaho, United States.; Clausthal Zellerfeld, Germany; and Cornwall, England. Large deposits also replace limestone, dolomite, or occasionally organic matter, or have a contact-metamorphic origin. Galena is additionally found in cavities, brecciated (fractured) zones in limestone and chert, and in coal beds. This specimen was recovered from Broken Hill NSW and is 60% lead with 8-12 oz/silver to the ton.Galena or 'lead glance' is a grey lead sulfide and the chief ore mineral of lead. It forms isometric crystals in which the ionic lattice is similar to sodium chloride. Galena is brittle and easily weathers to secondary lead minerals, with the upper part of mineral deposits often containing cerussite, anglesite, and pyromorphite. It usually contains silver, which is mined along with its lead content. Other commercially important minerals that form in close association with galena are antimony, copper, and 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 small-sized solid specimen containing one mineral with a sparkly silver metallic lustre exterior and pastel-grey interior.geological specimen, geology, geology collection, burke museum, beechworth, galena, lead sulphide, alfred selwyn, broken hill

It is not known where this opal originated. Common Opal is formed from silica-rich water entering the earths crust and hardening into a gel of water and silica-spheres, layered through the specimen. Common opal differs from precious opal in colouration and appearance, with precious opal including more colours, and having a translucent or glossy appearance, where common opal shows less colour and is typically opaque. It scores high on the Mohs hardness scale, and is common throughout the world, especially in Australia, where it is far more prevalent than the highly-prized precious opal. Australia is also the highest producer of opals in the modern world. 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, silica-based mineral specimen of Common Opal in shades of grey, green, and yellow, with a thick grey vein running through the centre. geological specimen, geology, geology collection, burke museum, beechworth, opal, common opal, gemstone, mining

Map of the Counties of Dundas, Berung, and Riponcounty of dundas, county of berung, county of ripon, map, geology, ararat, stawell, hamilton, grampians

Typed sheets listing departments, staff and developmentsstaffing, ballarat school of mines, civil engineering, electrical engineering, mechanical engineering, geology, mathematica, humanities, time allocations

Red covered booklet of 12 pages. Back and front covers are written onapplied chemistry, metallurgy, geology, electrical engineering, mecanical engineering, civil engineering, mining engineering, applied physics, art

Digital images showing Middle Island and Merri Island, Warrnambool.landscape, seascape, geology, warrnambool, middle island, merri island, coast, coastal, thunderpoint

Water flowing through the tunnel at The Blowhole, Hepburnhepburn, landscape, heritage, hepburn regional park, mining, blowhole, floods, weather, geology

Colour photograph of wind turbines at Cape Bridgewater.cape bridgewater, geology, ocean, coastal, landscape, seascape, petrified forest, wind farm, wind turbine

cape bridgewater, geology, ocean, coastal, landscape, seascape, petrified forest, wind farm, wind turbine

Digital image of the mouth of the Merri River at Stingray Bay. landscape, seascape, geology, warrnambool, coast, coastal, stingray bay, merri river, mouth

The Bendigo School of Mines was opened in 1873 following the first report of the Technological Commission in 1869 which recommended the establishment of schools of design and science to meet the scientific and technical needs of the mining industry on the local gold fields. Initially mining, chemistry, geology, metallurgy and art were taught while a separate school of design was established in c. 1870 but incorporated into the School of Mines around 1883 when it was renamed as the School of Mines and Industry. In 1904 The Mechanics Institute was liquidated and its assets and buildings acquired by the School of Mines. Around 1907 a Junior Technical School commenced to operate at the School of Mines and Industry but ceased operating in 1961 with that function being transferred to the White Hills and Kangaroo Flat Technical Schools.Obverse; Ornate relief design made up of a coat of arms with mining icons in each quarter flanked by flags on either side. Per varios usus artem experientia fecit written in scroll underneath. Translation: Practice has brought skill through different exercises. (Manilius) Reverse; Outer wheel Bendigo School of Mines and Industries. Inner; 1873 /Jubilee /1923Obverse; Per varios usus artem experientia fecit Reverse; Outer wheel Bendigo School of Mines and Industries. Inner; 1873 /Jubilee /1923city of greater bendigo education, bendigo school of mines

E560 N5 Dec 1979 A43 Boring mole pit near big box tree in 39 Burlock Avenue backyard Part of a 43-photo record of the MMBW�s engineering feat in drilling a 12 inch pipe line up to 40 feet deep through rock hardened by volcanic action associated with geological fault that occurs along the line. The work took place from October 1979 to May 1980 on the southern boundary of Hubbard Reserve, North Ringwood. The collection was presented to the Ringwood Historical Research Group by J Clarke on 9th June 1980.

E560 N24 Jan 1980 A43 Cover of mole pit near big box tree in 39 Burlock Avenue backyard Part of a 43-photo record of the MMBW�s engineering feat in drilling a 12 inch pipe line up to 40 feet deep through rock hardened by volcanic action associated with geological fault that occurs along the line. The work took place from October 1979 to May 1980 on the southern boundary of Hubbard Reserve, North Ringwood. The collection was presented to the Ringwood Historical Research Group by J Clarke on 9th June 1980.

The Chinese Imperial Commissioner, Hwang How Cheng, visited Australia at the request of the Chinese Emperor for the purpose of establishing Chinese consulates in the Commonwealth. He visited Ballarat at the request of Ballarat’s Chinese community. The newspaper reported that it was hoped the Commissioner would visit the Ballarat School of Mines “where the knowledge he would get would probably be of the utmost usefulness in the development of the great resources of China.” The Commissioner was accompanied by interpreter Ah Ket (Melbourne barrister and solicitor), and met by members of Ballarat’s Chinese community, including Dr Wong Chock Son. Apparently the Chinese Commissioner wanted to visit SMB because of its international fame relating to education in mining. From the SMB Letter book (Cat. No. 436) comes the following which suggests the Commissioner was based in Adelaide) '17th November 1906 His Excellency, Hwang How Cheng Chinese Commission Adelaide May it please your Excellency By this post I have the pleasure in forwarding for your Excellency's kind acceptance (and one for Mr. When) copies of the photograph taken of your recent visit to the School of Mines. I trust they will serve a pleasing memento of what, I hope, was a pleasant visit to our Golden City. Yours Faithfully Fredk Martell Director' The visit was reported in the Ballarat Star in 14 November 1906:- The Chinese Imperial Commissioner, Hwang Hon Cheng, who recently arrived in Victoria on behalf of the Chinese Government, paid a visit to Ballarat last evening, and was entertained by his fellow countrymen at a dinner at the Bow Leong rooms, Main street. The commissioner, who came up by the express, was accompanied by his secretary and Mr Ah Ket, the well-known Chinese barrister, of Melbourne; but some disappointment was expressed by the fact that he did not wear his official robes, being attired in the more sombre European dress. Mr W. D. M’Kee presided at the dinner, on the invitation of the Bow Leong Society, and in addition to representative Chinese residents, three were also present the mayor of the city (Cr. J. J. Brokenshire), Crs. R. Pearse, G. Crocker (City), J. R. Elsworth, A. Mackenzie, J. A. M’Neil, A. Levy, G. Bunting, F. Penhalluriack (Town), Col. Williams, Mr. J. Gent, Messrs. F. J. Martell (director of the School of Mines), A. W. Hager (president of the Orphan Asylum), A. Kenny (superintendent), R. G. Fitzgerald (clerk of courts at Ballarat East), J. Trethowan, A. A. Buley, Serg Dalton, and others. Apologies were received from the mayor of the town Revs. J. West Lau, Dr Cairns, Hon. J. Y. M’Donald, L. Lederman, C. C. Shoppee and others. The gathering was a very cordial one, and the hospitality of the Chinese was greatly appreciated. After the loyal toasts, “The King” and “The Emperor of China,” had been honoured, the chairman extended a hearty welcome on behalf of the society and others to the commissioner. Mr M’Kee said he was privileged to speak in behalf of the Chinese. There was a warm feeling of friendship between them and himself, and his services were always at their command. If he were in China he would desire that a similar compliment would be extended to him. They were all pleased the Emperor of China had sent the commissioner to establish consulates in Australia with a view of the empire understanding the feelings of Australasia better than they did at present. He hoped the commissioner would have opportunity of visiting some of their industries, as they desired him to gain all the scientific and practical knowledge of those industries that he could. The toast of “The Commissioner” was proposed by Col. Williams who expressed pleasure at the visit of a gentleman of education and attainments to look into the condition of the scions of China in Australia. He hoped the commissioner would carry away a correct impression. In Australia they had nothing to conceal; they hoped to be understood. (Applause.) No intelligent man had the temerity to condescend to patronise China, one of the richest countries in the world, with a civilisation dating back thousands of years. In the matter of population alone it was equal to one-third of the world. They heard a lot about the “awakening of China.” They hoped it would be humane, just, and considerate if it had power. He hoped the commissioner would be satisfied with what he saw. The law of filial relation to the children was strictly observed in China, and he did not know whether it would not be a good thing if they had a little more of that religion here. It would be a fair thing to tell the commissioner that while he might inquire into the labour laws, the basis of these laws was not a desire to oppress but to enable every man to obtain the same conditions they expected from their own people. If he gained that impression he felt they would be fairly treated. (Applause.) Mayor Brokenshire supported the toast. They had, he said, in the Chinese a most law-abiding people. Their behaviour was an example to the British citizens. They were quiet, inoffensive men, and they toiled hard, even on Sundays. (Laughter.) Mr Ah Ket; That is what the government does with the railway employees. (Laughter.) The Commissioner replied through Mr Ah Ket, who in a graceful speech acknowledged the toast. The commissioner had, he said been delighted with what he had seen of the country – he believed it to be one of the finest in the world – and he greatly appreciated the hospitality extended to him. (Applause.) The Chairman proposed the toast of “The health of Mr Ah Ket,” and paid a tribute to his ability. It was satisfactory to see that he had risen to such a position, and it might be that in the future he would be asked to occupy a position on the bench. (Applause.) Mr Ah Ket, in response, said he had not come prepared to make a speech. He had come to Ballarat to have a quiet evening with his friends, and as soon as he arrived he had been whirled away in a motor car to a place where he found an aggregation of East and West. He was pleased to see them commingled at the festive board. That suggested the idea that East and West could meet together without friction. Misunderstandings arose only because men were superficial. If they threw off outer garments they would know each other better. He looked forward to the time when nations would understand each other. It was by an interchange of visits that such things could be accomplished, and nations would then live at peace with each other. (Applause.) Other toasts were also honored. Twelve men pose for a photograph on the stairs of a building at the Ballarat School of Mines. Back row left to right: A.D. Gilchrist (Prof. of Engineering), B. Whittington (Mathematics, Physics), Thomas S. Hart (Prof. of Geology and Mining), J.M. Sutherland (Electrical Engineering) Front row left to right: Dr Wong Chock Son (Ballarat), Fred. J. Martell, Alfred Mica Smith, Ah Ket esq (Melbourne Barrister), His Excellency Hwang How Cheng (Chinese Commissioner), Wen Esq (Secretary), Alderman Grase (mayor of Brisbane), Grase Esq (Ballarat).ballarat school of mines, alfred mica smith, fred martell, j m sutherland, a d gilchrist, b whittington, thomas hart, wong chock son, ah ket, hwang how cheng, chinese, chinese commissioner, international, new classrooms, administration building, a building

Book; Brown paper containers with plates (& maps) to accompany bulletin No49 of geological survey of Victoria. V Oswalds G.M. Plan of lease. VI. Oswalds G. M. Plan of workings. VII. Oswalds G. M. Transverse Sect. VIII. Oswalds G. M. Longit. Section. IX. Oswalds G. M. Plan & Sect. 500ft. Level. X. Northey's Reef plan & sections. XI. Carlisle and Whittaker's Mine Plan & Sections.XII. Goldsborough G. M. Co. Gordon's Reef, Plan & Section. XIII. Mount Tarrengower Tunnel Plan & Section.MCCOLL RANKIN & STANISTREETorganisation, industry, surveys, mccoll rankin & stanistreet

In 1917 Bendigo Amalgamated Goldfield Ltd was formed from the amalgamation of 35 companies with operations on the Garden Gully, Sheepshead, Deborah and Derby lines of reef hoping to increase profits of these existing operations through economies of scale. This was difficult to achieve as the shafts involved were spread throughout the goldfield. Diamond drilling and good geological practices were introduced (Pabst was Chief Geologist) leading to some exploration success. However costs were rising rapidly and in 1923 the directors, deciding that mining would soon become unprofitable, dissolved the company returning assets to the original vendors. J.H. Lenten, Mine Manager, received his second class Mine Manager's certificate in September, 1914 at an examination held at the Bendigo Law Courts. One hundred pages of fortnightly manager's reports for Bendigo Amalgamated Goldfields N.L., Sheepshead Shaft. Reports consist of two pages for each fortnight, signed by J.H. Lenten, Mine Manager. Dates of reports range from November 20th, 1917 to 5th May 1920. Categories reported on include: development, stoping, tons from tributors, tons Company's stone, plant and machinery, underground workings, number of rock drill shifts, firewood used, coal burnt, and general remarks. charcoal burnt., lifting waterbendigo, margaret roberts, , goldmining, bendigo amalgamated goldfields, sheepshead shaft, j.h. lenten, mine manager

Common Opal is a mineraloid that is non crystallising and is classed as an amorphous silicate, the chemical composition for Opal is SiO2 nH2O. Opals can develop in weathered sedimentary rock typical in arid regions where limited water enters small gaps in the rock, and the silicate is hydrated. Common opals, unlike precious opals, do not exhibit ‘play of colour’ in which the colour appears to change depending on the angle of view. While precious opals are highly valuable and cut as gemstones for jewellery, common opals can be cut into inexpensive gemstones and are also mined for various uses including as ingredients in ceramics, insulation, fillers, and abrasives. The source of this common opal specimen is unknown, but common opals are found around the world, notable deposits are found in Queensland, South Australia, New South Wales, Peru, Kenya, Nevada, Oregon, and Mexico. This common opal specimen is of historic and scientific significance due to its donation in 1868 as part of the Geological Survey of Victoria and as a typical example of uncut common opal. 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 palm-sized amorphous (non-crystallising) hydrated silicate mineraloid specimen in shades of brown, orange, and white.Existing label: Common Opal / Locality unknowngeological specimen, geology, geology collection, burke museum, beechworth, common opal, opal, mineraloid, amorphous silicates, hydrated silicate

New Zealand Greenstone, also called Pounamu is found on New Zealand’s South Island in riverbeds and boulders, and colours vary depending on the source, but always include green tones. It is a form of the mineral nephrite, also known as jade, and is a tough stone with a crystalline structure, made up of calcium magnesium and iron silicate. Its hardness means it is ideal for carving, and has been used for this purpose throughout history, especially by the Maori people of New Zealand. Greenstone features heavily in Maori mythology, and the traditional name for the South Island, Te-Wai-Pounamu, literally translates to waters of greenstone. Wearing of Greenstone pendants with different carvings is practiced by Maori to represent connection to land and ancestors, or to endow the wearer with certain attributes. The sticker on the base of the specimen identifies it as a product of Hokitika Jade Company. The company, which was active in the 1970s, sold jade and greenstone specimens and ornaments. Hokitika, which started life as an 1860s gold rush town, is the origin of most nephrite found in New Zealand, and the centre of the Greenstone carving industry. The object has scientific and research potential as part of the Burke Museum's Geology Collection, and as and example of New Zealand Greenstone. It also has spiritual significance for it's role in Maori beliefs and communities, where it is both traditionally worn and features in mythology. As a valuable stone regularly used in carving and jewellery, it has aesthetic significance. Sticker on base: "N.Z. Greenstone/ a product of/ Hokitika Jade Coy."geological specimen, geology, geology collection, burke museum, beechworth, new zealand, greenstone, hokitika, nephrite, jade

A granular metamorphic rock, marble is derived from limestone or dolomite and composed of calcite or dolomite interlocking grains. Heat and pressure from overlying sediments form it from limestone buried deep in Earth's crust. Graphite, pyrite, quartz, mica, and iron oxides can affect rock texture and colour. This specimen was found in Carrara, Italy. Carrara marble is the most common marble found in Italy, and it gets its name from the region where it is located. The marble was also called Luna marble and was used as a decorative element in buildings and sculptures. It has been quarried since Roman times in the Lunigiana, the northernmost tip of Tuscany, just outside the city of Carrara in the province of Massa and Carrara.Marble is one of the most popular and expensive rocks used in sculpture, architecture, interior decorations, statues, table tops, and novelties. It is available in various colors and textures depending on the chemical composition. The strength of the rock and its ability to hold finer details have made it a favorite among designers. 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 Marble (metamorphic rock) predominantly white with specks light grey and ochre geological specimen, geology, geology collection, burke museum, beechworth, marble, carrara marble, italian marble, marble specimen, tuscany

A collection of eight large fold out coloured maps published in a bound book formnon-fictionThe Melbourne Study Report is a series of volumes describing the physical nature of the land and its environment, examines the likely forms of land use, and assesses the hazards associated with these uses. This is Volume 2 (coloured maps). The first page featues a black and white map described as "Shire of Diamond Valley" with public land marked in yellow. Followed by eight large fold out maps. Melbourne Study Area Public land and descriptive blocks, Population description, Geology, Physiography, topography and rainfall, vegetation and water supply. The Land Conservation Act 1970 established the Land Conservation Council whose functions is to "carry out investigations and make recommendations to the Minister with respect to the use of public land in order to provide for the balanced use of land in Victoria. This report sets out to describe and assess the natural resources of the public lands in the Melbourne area and provides a factual basis on which members of the community may base submissions to the [Land Conservation] Council of Victoria. maps, shire of diamond valley, population, geology, topography, rainfall, vegetation, water supply, land use, public lands

Three handwritten pages relating to gold discovery at Ballarat.ballarat, gold discovery, smythesdale, bunninyong, warrenheip, geology, archibald yuille, pyrenees, clunes, herbert swindles

Colour photograph of a metal fire brigade at Cape Bridgewater.cape bridgewater, geology, ocean, coastal, landscape, cfa, fire, station, fire brigade, cape bridgewater fire brigade

Native Sulphur in its solid form is a yellow crystalline mineral that forms near volcanic vents and fumaroles where it is the solid form of hot gases. It is also frequently found in the subsurface as a by-product of sulphide ore mineralization. In all its forms, sulphur is one of the most commonly occurring minerals on the planet, especially in natural gases, and is key to the make-up of a range of other minerals. It is essential to continuing life on earth, and was used in ancient societies as part of medical care, religious rites, and entertainment, and was key to the invention of gunpowder by the Chinese. Native Sulphur in its solid form is a yellow crystalline mineral that forms near volcanic vents and fumaroles where it is the solid form of hot gases. It is also frequently found in the subsurface as a by-product of sulphide ore mineralization. In all its forms, sulphur is one of the most commonly occurring minerals on the planet, especially in natural gases, and is key to the make-up of a range of other minerals. It is essential to continuing life on earth and was used in ancient societies as part of medical care, religious rites, and entertainment, and was key to the invention of gunpowder by the Chinese. The exact site of extraction for this specimen is unknown, but it was probably collected in New Zealand in the 1850s. Sulphur is significant both for its historical and current uses, and for its nature as one of the most abundant minerals on the planet. Sulphur's importance comes both from its abundance and its role in ensuring survival, creating other minerals, and daily human life. This specimen is significant as representative of sulphur's solid 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.A solid, small, crystalline mineral specimen that is largely bright yellow, with some darker spotting. geological specimen, geology, geology collection, burke museum, beechworth, sulphur, native sulphur, new zealand, native sulphur specimen, sulphur specimen

4 pages from the 'Mining and Geological Journal', July 1938. Front page is an index to figures in the graptolite collection. 'Numbers in brackets are taken from the Fossils Register of the Mines Department Museum, Melbourne, and refer to the specimens in the Museum.' Lancefieldian, Bendigonian, Chewtonian, Castlemainian, Yapeenian, Middle Ordovician, Upper Ordovician, Gisbornian, Estonian and Bolindian categories are described. The numbers on the BHS fossil collection relate to the numbers/names on the page. Two following pages illustrate the fossil types within the major categories. Small sign with pages ' 'Fossils, Bendigo & /surrounding Districts' was with the fossil display in a glass display cabinet, ex Museum of Mines Museum, Bendigo.