Kaolin is also known as china clay. This specimen came from Dunolly, Victoria and was donated to the Museum in 1868 as part of the Geological Survey of Victoria. This survey helped map and study the geology of Victoria. In Victoria, Kaolin is particularly used as a filler and coating material in paper manufacture. It can also be used in paints, ceramics, rubbers and plastics. There are many kaolin deposits in Victoria but many of these have been mined out and there is not much Kaolin left. Rocks that have a high amount of Kaolinite and it can be formed through the decomposition of other materials. There are two types of Kaolin; hard and soft kaolin. Soft kaolin's are coarse but have a soapy texture. It can also break easily. The hard kaolins have an earthly texture and are finer grained. This means that they are harder to break, unlike the soft kaolin. Hard kaolin's are formed by flocculation in salt water, a process that in basic terms, bonds particles together. Kaolin is a common material in Victoria and that is why it is significant. While this specimen was mined in Dunolly, Victoria Kaolin can also be found Pittong, Pakenham, Bulla, Hallam and Ballarat as well as many other places throughout Victoria. This specimen represents the presence of Kaolin deposits in this region of Australia. It is also significant because Kaolin has many uses and is largely beneficial to many manufacturing processes in 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.Two pieces of Kaolinite mineral with shades of white and graygeological specimen, geology, geology collection, burke museum, beechworth, kaolin, china clay, dunolly, geological survey of victoria, kaolinite, victoria, mining, mining deposits, geology of victoria, australia, filler, coating material, paper manufacture, paint, ceramics, rubbers, plastics, decomposition, materials, soft kaolin, hard kaolin, flocculation, particles, salt water

The context in which the hat was made and worn assists in establishing its potential historic significance. 'Bailliere's Victorian Gazetteer and Road Guide containing the most recent and accurate information as to every place in the Colony' (1870), describes the village of Vaughan as being located on the road from Daylesford to Castlemaine. In 1870 the Vaughan was deemed to be entirely a gold mining area, gold having been discovered in the district in 1853. Intriguingly the entry in the Gazetteer claims that the electoral division of Vaughan began at the junction of the Middleton Creek and the Loddon River, so perhaps the cap might have belonged to a member of a significant local family. In 1870, Vaughan had a population of about 1000 persons and included almost 300 dwellings. Articles from newspapers, published on Trove refer frequently to a Mr Middleton as a litigant in court cases before the Vaughan Court in the 1860s. By the 1870s, the Mt Alexander Mail, in an article on ‘Mining: The Pioneer Wheel’ describes the success of Mr Middleton and his Middleton’s Reef Gold Quartz Mining Company, which had built the largest water wheel in the Colony. The wheel was 20’ in diameter and 2’ wide. Quartz mining as practiced by companies such as Middleton’s had become necessary after the exhaustion of alluvial quartz mining deposits in the 1860s. So we can probably establish a link between the cap and a significant mining identity in the period in which the article was made. The historical significance of the cap is only one part of the story. Caps such as the Middleton example can also be items of aesthetic significance as they were typically, examples of women’s work, using published patterns in magazines such as the Ladies Home Magazine. While women might follow or adapt a published pattern, their choice of materials reflected what was available locally. The fine hand stitching on this example is evidence of high quality domestic needlework. The maker crafted the cap from five triangular pieces of cotton cloth, each piece lined with a faded yellow net. The net provides some stiffening for the cap and has a functional purpose in that it anchors the hand-stitched, looped design of yellow silk ribbon that decorates the surface of the cap. Gentleman’s smoking (lounging) cap believed to have been made in c.1860-69. The conical hat is made of a dark green cotton fabric embroidered with narrow ribbon of a paler green silk. The unlined rimless hat is made of four pieces of fabric. There is no evidence of the hat at one stage featuring a tassle. The original donation record noted that the cap had been made for, and was worn by, a Mr Middleton, of Vaughan in Central Victoria. Nilhats, smokers hats, men's clothing

Blue/black hard covered book of 234 pages including index and photographic reproductions. Contents include Uses of Water in Mining; Geology of Placer Deposits; Gold Recovery; Flumes, ditches, dams, pipes; Giants, valaves, gates, weirs, miner's inch, pressure box, dams; gravel elvators; exploiting. mining, hydraulics, water, dredge, dredging, gold mining

Documents: September 1943 issue of the West Australian Mining and Commercial Review Magazine - 32 Pages plus cover. It has a photo of the Australian Prime Minister, Hon John Curtin P.C. and the cost is 9d dated September, 1943. The back cover is advertising for Goodyear V-Belt Drivers. Articles on Municipal Finance, Port War Radio, W.A. Mining Industry, Ore Deposits, Rand Gold Producers. Advertising for Mobil Oil, Fibrolite, Bromet Alloy Tungsten Carbide, Steel Machinery Covers, Dept.., of Industrial Development, Hume Steel Ltd, State Saw Mills etc.MCCOLL RANKIN AND STANSISTREETorganization, business, gold mining magazine, mccoll rankin and stansistreet

The author, Bennett H. Brough was an associate of theRoyal School of Mines, a member of the COuncil of the Institution of Mining Engineers, a fellow of the geological society and of the Institute of Chemistry, a member of the Mining Institute of Cornwall, and a former instructor of mine-surveying at the Royal School of MinesRed had covered book 372 pages - part of Griffin's Mining Series. Contents include general explanatinos of surveying, an historical sketch, mineral deposits, mining terms, measures of length, measurement distances, the chain, rods, steel bands, measuring wheel, Miner's Dial, Magnetic needle, Fixed needle, German Dial, theodolite, traversing underground. Surface-surveys. plotting the survey, calculation of area, leveling, Telescope, Setting out, Mine-Surveying Problems, Mine Plans, Photographic Surveying, examination Surveying. Illustrations include: Whitelaw's Dial (Fig 22), Theodolite of the American Type with Hoffman tripod head, (fig 37a)mining, surveying, miner's dial, chain, survey, theodolite, scientific instruments

This candle holder has a sharpened point to push or hammer into soft rock and a hook to hang on a ledge or piece of rock. It is intended to be used in a mine and many residents of Warrnambool and district went to the gold mining districts in the 19th century. But it could have been used in the Warrnambool district if a small night light was required in one of the many local quarries or even in the search for coal deposits in the region. It could also have been used in a household.This miner’s candle holder has no known local provenance but it is retained as an interesting example of a candle holder used in the past.This is a thin piece of metal tapering to a point at one end and curving around in a loop at the other end to make a handle. Along the straight metal piece is attached a curved metal hook. At the end of the loop is an open-ended circular piece with a serrated top. The circular piece has a rectangular-shaped end piece which enables the hole in the curved piece to be pushed out or pulled in to make the hole smaller or bigger. The metal is much rusted. 19th century mining, history of warrnambool

Panning dishes were used for washing fine gold from river sediments or from the residue trapped in cradles and puddling tubs. They were often used on the edge of streams/rivers to sift gold from alluvial soil or crushed quartz. This simple pan would have been filled with sand and gravel which might have contained gold. The pan was submerged in the water and shaken to sort the gold from the gravel and other material, with the lighter material gradually being washed over the lip until only the heavy deposits, such as gold, remained at the bottom. (ref. Museum Victoria) This pan was used by George Henry Douglas Russell Snr. As a young man prior to his enlistment in WW1 he panned for gold using this dish. During the war he became a vet sergeant in charge of horse lines.Gold panning is the oldest and simplest method of extracting gold. Gold pans had widespread use in alluvial gold fields where water is available. This item is an example of the type of pan commonly used on Victorian gold fields.A circular dull metal panning dish which has a wide rolled top lip which tapers down to a smaller diameter for the base which is flat. The pan has been made from ironmetal which has a coating of another metal with a matte grey finish. It has a small hanging hole and a reinforcing ring all around the top.russell-doug gold-panning mining

The photo depicts one shift of mine hands at Hanlon Consols Mine Rokewod in 1901. ist on the left is George Edgar Yung. George was born in Ararat the son of Yohann Godlip and Christina (b Weller)Yung. They lived at Happy Valley near Linton. and Piggoreet. Yohann was a miner and died in the All Nations Mine collapse at Derwnt Jack's in 1877. Interesting to note in the following information that the Hanlon Consol mamager, William Maughan was also the manager of the Try Again Mine in Piggoreet. He was also on the six man school committee of Piggoreet Common School No. 726. (Is this why George Yung ended up working in Rokewood because of a previous connection at Piggoreet? George married Clara Emma Smith from Happy Valley and worked in a mine at Allendale. They later moved to Yendon) About the Hanlon gold mining company near Rokewood. 1901 - Information Bendigo Prospecting Club, 21/08/2020. Information provided once again by Peter McCarthy. Christopher Hanlon had put down a line of bores south of the Rokewood main street, looking for a continuation of the Break O’Day lead which had been worked for two or three miles with highly payable results, though in a primitive manner. Ground was being paddocked 30 feet deep and made to pay. The bores suggested the sinking would be about 70 feet and a shaft site was selected at the back of Stanbrook’s Hotel. The Hanlon Gold Mining Company was formed in March 1895 and the shaft was bottomed at 68 feet, getting just over an ounce of gold from the shaft bottom. By January 1896, the poppet heads were up, and steam plant was nearly ready. The mine produced 846 oz by September, which was not as good as expected, but they installed a second puddling machine. The mine was profitable for the next three years, with periods of prospecting and the need to install steam pumps in 1897. A second shaft was sunk in 1899, which bottomed at 86 feet on good wash and was sunk on to 109 feet. 1743 oz of gold had been produced in six months to September 1899, but the No1 shaft was let on tribute as the No2 workings were opened and machinery installed the following year. The No1 shaft tributors broke even in 1900 and in 1901 the shaft was shut down, with the No1 shaft machinery sold late in 1902. By September 1901, the mine had produced gold worth £66,124 and the No2 shaft main drive was in 346 feet, with gold being found mainly in crevices in the hard floor. Mining continued, but once the No2 shaft workings met up with the old No1 shaft workings at the end of 1902 there was not much wash remaining. The mine was let on tribute in June 1903 and a drive was put in to test deeper ground. The company was wound up in February 1904 and the plant sold. From what they discovered, the manager concluded that the mine sat at the edge of an ancient coastline and the gold was in a beach deposit. The total gold production from the mine was worth £73,294. J Lee Archer JP, shareholder, was the manager of the Bank of Victoria in Ballarat. Born in Tasmania, he came to Victoria with his parents and first came to Ballarat in 1855 as a junior clerk with the bank. He died in 1902 aged 64. Alexander J. Peacock was a legal manager and a share broker. In 1897 Peacock, born in Creswick, had been elected as one of the Victorian delegates to the Constitutional Convention which wrote the Australian Constitution. He later became a politician, state treasurer and three times state premier of Victoria and was knighted KCGM. He died in 1933 aged 72. William Maughan, director, was an English miner who came to Victoria in the 1850s and became a mine manager, managing the Try Again at Piggoreet, Ryan’s Freehold and the Madam Berry, among others. He died in Williamstown in 1915 aged 85. Sepia photographRhs front of photo: R. Millist Phto & Lanternist Geelong Verso (upside down): ONE SHIFT OF MINE HANDS HANLON CONSOLS MINE ROKEWOOD 1901 Grandfather Yung 1st on left rokewood, hanlon consols mine, shift of mine workers 1901, gold mines, george edgar godlip yung, william maughan

Newspaper article, Friday 3, 2017, Bendigo Weekly. titled 'Gold win for mine' by Sharon Kemp. Fosterville Gold Mine has hit the jackpot intercepting some of the richest gold mineralisation in the world. Article describes richness of Fosterville deposit. Fosterville started operating in 2005 and has been mining underground for 10 years. 'At the current Australian dollar gold price, the three month haul is worth $70 million'bendigo, mining, fosterville gold mine

Documents: Brown wrapping paper held closed with string, Documents from the Royal Mint: Melbourne Branch, Deposit buts: The English Scottish & Australian Bank Limited, The School of Mines and Industries, Bendigo J.R.V. Anderson, B.M.E. Licensed Gold Smelter.organization, business, industrial - mining, mccoll rankin & stanistreet, mining, gold mining, central napoleon

3 page document. Letterhead 'Edward Dyason & Co., member of the stock exchange of Melbourne, Safe Deposit building, 92 Queen St., Melbourne, dated November 7th, 1935. Document is an analysis of the 'world situation' and discusses the economic and political situation of the world . In particular, the equipment industries by ' re-arming programme's 'There is little doubt that the great activity in metal manufactures is partly for war purposes. Despite the building of armaments, nobody really wants war .....'business, mining, mccoll, rankin & stanistreet, metalliferous industries, dyason & co., stock exchange, shares

This photograph was taken in approximately 1870 and depicts four male miners standing in mining sluice at the Three Mile Goldfields. These men are wearing typical attire for 1870s gold miners. They wear white shirts, tan coloured pants with water proof shoes and most of the men are wearing an apron to prevent their clothing from becoming too dirty from the mud. Each man is wearing a wide brim hat and hold large wooden tools used for sorting through the sluice. Three of the four men have full beards. The photograph was donated to the Burke Museum by R. Ziegenbein before 2001 but the photographer and the individuals captured in the photo are unknown. The image depicts the landscape of the Three Mile Goldfields during a period when open cut sluicing was undertaken to reach gold. Open cut sluicing is a method used to extract gold and other precious metals from beneath the surface of the earth. This technique involved the use of high-powered hoses which broke down the soil enabling miners to come along and search this soil for gold. After the gold rush of the early 1850s, diggers had to enlist the assistance of heavy machinery and techniques like hydraulic sluicing in order to reach gold because the surface alluvial gold had already been discovered and removed. This heavy machinery was not used until after 1853. The Three Mile Goldfields was a site of rich alluvial gold deposits located about 5 km south of Beechworth in Victoria. Today, the location of this gold deposit is called Baarmutha. It was a popular area for gold mining in the 1850s but became largely abandoned by the following decade. In 1865, a man named John Pund recognized that the area could be potentially rich if a better water supply could be obtained. He secured a 15 year license with three other miners. Within the next five years, these men had constructed 19 km of water race going from Upper Nine Mile Creek to Three Mile Creek. By 1881, these four men had delivered 950,000 gallons to the Three Mile Sluicing area which is depicted in this photograph. Pund was later go into partnership with John Alston Wallace who would become owner of the Star Hotel in Beechworth. The Three Mile sluicing location continued to be operational until 1950. Sluice box workers were a vital part of gold mining regardless of how inefficient they were in the recovery of gold. After using hydraulic sluicing to cut away the earth, miners would use the big wooden boxes depicted in the image to catch the earth which would then be sifted for gold. However, accidents would occur often which would result in the gold washing away and unable to be recovered. It was not a very efficient system because the gold, which was alluvial and thus very fine, would often pass through the sluice box undetected.The search for gold is ingrained into the history of Victoria and therefore, images like this one which portray an open cut sluicing site can reveal important information for society and technology for the date when the photograph was taken. This image is of important historical significance for its ability to convey information about sluicing and the methods used to find gold in the late 1800s and early 1900s. It also shows a location where sluicing was undertook which provides insight into the impact of sluicing on the environment at a time when it was done. Images, like this one, of Australian gold rush history can reveal important information about the social and environmental impact of this period. This image depicts diggers standing in a mining location and therefore, this image has the capacity to reveal or support significant information for researchers studying the fashion and social status of diggers in Australia in approximately 1870. It can also provide information on the landscape of Australia in this period and the impact of mining for gold on both society and the Australian landscape. The Burke Museum is home to a substantial collection of Australian mining photographs which can be used to gain a deeper understanding into life on the gold fields, technology used in mining, the miners themselves and the impact of the gold digging on the environment.Sepia toned rectangular photograph printed on matte photographic paper and mounted on board.[illegible] about 1870 / 97 2514.1 / 2594 30three mile goldfields, goldfields, 1870, 1870 gold, australia, australian landscape, miners, gold miners, diggers, gold diggers, beechworth, victoria, sluice box workers, sluicing, sluice, mining

This photograph was taken in 1911 at Three Mile Creek, about five kilometers south of Beechworth town. Significant digging took place at this location from late 1855, which led to a flood of workers and stores to follow, though daily earnings were slim compared to the nearby Woolshed site. This remained the case even after workers at Three Mile Creek attempted to protest around Beechworth during an election in November 1855. Three Mile Creek was one of seven significant divisions of the Beechworth Mining District formalised by the Governor-in-Council in 1858, though by the time this photograph was taken, the boundaries of the original seven districts had shifted to create seventeen divisions. The Three Mile Goldfields was a site of rich alluvial gold deposits located about 5km south of Beechworth in Victoria. Today, the location of this gold deposit is called Baarmutha. It was a popular area for gold mining in the 1850s but became largely abandoned by the following decade. In 1865, a man named John Pund (a man second from the left in the back row of this photograph shares this surname) recognized that the area could be potentially rich if a better water supply could be obtained. He secured a 15 year license with three other miners. Within the next five years, these men had constructed 19 km of water race going from Upper Nine Mile Creek to Three Mile Creek. By 1881, these four men had delivered 950,000 gallons to the Three Mile Sluicing area which is depicted in this photograph. Pund would later go into partnership with John Alston Wallace who would become owner of the Star Hotel in Beechworth. The Three Mile sluicing location continued to be operational until 1950. The eleven miners in this photograph are: Back row: Led Guthrie, P. Pund, F. Beel, [Unknown] Miller Front row: Paddy McNamara, J. King, W. Beel, [Unknown] Garland, J. Clarke, J. Ryan, H. Bartsh In the background of the photograph is a huge dirt wall that appears to suffer damage caused by hydraulic sluicing. Hydraulic sluicing is a specialised mining technique that involves directing high pressure water flows at dirt to uncover gold. The technique played a significant role in shaping Beechworth's landscape during the gold rush to create the topography seen today.The search for gold is ingrained into the history of Victoria and therefore, images like this one which portray an open cut sluicing site can reveal important information for society and technology for the date when the photograph was taken. This image is of important historical significance for its ability to convey information about sluicing and the methods used to find gold in the late 1800s and early 1900s. It also shows a location where sluicing was undertook which provides insight into the impact of sluicing on the environment at a time when it was done. Images, like this one, of Australian gold rush history can reveal important information about the social and environmental impact of this period. This image depicts diggers standing in a mining location and therefore, this image has the capacity to reveal or support significant information for researchers studying the fashion and social status of diggers in Australia in approximately 1911. It can also provide information on the landscape of Australia in this period and the impact of mining for gold on both society and the Australian landscape. The Burke Museum is home to a substantial collection of Australian mining photographs which can be used to gain a deeper understanding into life on the gold fields, technology used in mining, the miners themselves and the impact of the gold digging on the environment.Black and white / sepia rectangular reproduced photograph printed on glossy photographic paper mounted on board.beechworth, beechworth museum, mining, mining team, three mile creek, sluicing, hydraulic sluicing, photography, gold sluicing, gold mining, pund mining

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

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

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 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

A fossil refers to any remains or traces of past life that are preserved in the rock. It could be remains of plants or animals. Fossil leaves are commonly found on different types of rocks. These fossils can go as far back as the Triassic Age just like the series of fossil plants collected at Denmark Hill, Ipswich in Queensland. Fossils leaves are formed when dead plants get buried by sediments like mud, sand, or volcanic ash. Often, it gets detached cleanly from stems along a special layer of weak cells, then twigs, and, less commonly, cones of conifers and fruits and seeds of flowering plants. Over time, the leaves or pieces of leaves get buried by more sediments and eventually gets 'lithified' or hardened into a rock. Erosions and mining can cause the rocks to break and reveal the fossils buried in it. Fossilisation frequently takes place at sites in the lowlands where deposits of clay, silt, sand are found. This is usually due to weathering and erosion of rocks. Fossil leaves can provide information about ancient Australia's way of living. It contributes to Victorian biodiversity records and its botanical collections. It also contributes information on the geographical profile of Victoria as fossilisation usually occur at estuaries and deltas of rivers, river flood plains, ponds and lakes. 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.Piece of light brown rock with fossilised leaves in shades of golden yellow and brown.Existing label: Fossil Leaves / Locality unknown / might be worth checking if this is Glossopteris, a Permian age plant. / C. William 16/4/21 geological specimen, geology, geology collection, burke museum, beechworth, fossil leaves, fossilization, 1868 geological survey of victoria, lithified, rocks, fossilised leaf, rock, fossils, leaves

Malachite is a water soluble, crystalline, triphenyl methylene chloride salt. It has a close relationship to copper because it is common for Malachite and copper to come from the same ore. Malachite often has shades of green, making it also known as Malachite Green. As a result of it's colour, it is known for being a dye and has been used in the dye industry, the textile industry and in medical fields. Cobar in New South Wales is well known for it's mining. This is because of the number of important deposits present in the area and include three important mining belts where most of the materials are found. These are the 'Cobar belt', the 'Canbelego belt' and the 'Girilambone belt'. The 'Cobar belt' runs underneath the main town. Copper was first discovered in Cobar in 1869 and since then, many deposits of other materials have been found, including Malachite.This specimen is significant because it comes from Cobar, NSW and represents the many deposits of materials found there. Cobar has a long history of mining and is a source of Australia's copper minerals. Malachite is often found in copper deposits meaning that it is representative of Cobar's copper production. Malachite is known for it's vivid green colour and as a result, has many uses, such as meaning used as a dye. This makes it a valuable material and highly significant. 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 mineral with shades of brown , white and light green throughout.geological specimen, geology, geology collection, burke museum, beechworth, malachite, copper, water soluble, cobar, cobar mines, cobar mining, cobar nsw, nsw, new south wales, mining belts, ore, copper ore, malachite green, dye, green, dye industry, textile industry, desposits, canbelego, girilambone, alfred selwyn

Galena is the natural compound of lead and classed as a sulphide, it crystallises in a cubic pattern and its chemical formula is PbS. Galena is a primary source of both lead and silver. This specimen of Galena comes from Broken Hill. Broken Hill has one of the world’s largest and most significant deposit of ore for the production of lead. Mining of Galena at Broken Hill began with the staking of land by Charles Rasp in 1883. By the following year, in 1884, Rasp and six others had formed Broken Hill Mining Company. Broken Hill Mining Company eventually evolved into BHP group limited and is currently the largest mining company in the world and the largest company in Australia. There is archaeological evidence from artefacts discovered in Turkey that humans have been extracting lead from galena by the process of smelting since at least 6500 BCE. This specimen also has quartz on the top surface which is frequently discovered alongside Galena. This mineral specimen is of historic significance as a sample of Galena extracted from Broken Hill during the 19th century. Mining for Galena in Broken Hill begin in 1883 by Charles Rasp and evolved into the world’s largest mining company – BHP Group Limited. Broken Hill is one of the world’s most significant deposits of ore for the production of lead. 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 flat, hand-sized, grey sulphide specimen that is the natural compound of lead with a quartz formation on the top surface. Existing Label: GALENA / (with quartz) / Locality: Broken Hill / N.S.W 120 x 70 x 29geological specimen, geology, geology collection, burke museum, beechworth, galena, galena quartz, quartz, charles rasp, broken hill mining company, bhp group limited, bhp, lead, ore, lead sulphide, sulphide, silver, broken hill

Malachite is a copper carbonate hydroxide mineral. It has a chemical composition of Cu2(CO3)(OH)2. It often forms within limestone where a subsurface chemical environment favourable for the formation of carbonate minerals can occur. It is a substance that can be found in many different parts of the world including: Australia, USA, Russia and the Democratic Republic of Congo. Malachite has historically been used to produce copper, with mining of the mineral dating back over a period of four thousand years. Due to its beautiful green colourations, it is also commonly used for aesthetic purposes such as in the production of sculptures and jewellery. This particular specimen was collected from the town of Burra, South Australia as part of a geological survey undertaken during the nineteenth century. The locality (located on Ngadjuri Country) has a long history of mining, particularly in copper mining, as the area is rich in copper deposits. The first significant discovery of this was made in Burra (Burra Burra Mine) in 1845 and, at the time, the mine was the largest and richest of its kind in the world, producing nearly five percent of the total world copper output. This specimen is significant as it is considered to be a rare gemstone, as many of the original deposits for the stones are significantly depleted, leaving behind very few sources. 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 copper carbonate hydroxide mineral with patterns of green colourations Existing Label: MALACHITE / Locality: Burra / S. Aust. Other Label: Confirmed / as Malachite / C. Willman / 15/4/1 / + Bill Birch burke museum, beechworth, geological, geological specimen, malachite, gemstone, green gemstone, burra, burra burra mine, burra south australia, carbonate mineral, copper, copper mining, copper mining burra, carbonate hydroxide mineral, copper carbonate, malachite mining, malachite burra, monster mine

Montmorillonite is a type of clay composed of aluminium silicate that forms very small particles that are not well-bonded to one another. This is why it is so soft. When in the presence of water, all types of clay swell. Montmorillonite swells even more than most types of clay, which is why it is often chosen over other types of clay in its practical uses. Montmorillonite has many different practical uses, including in the mining industry, as a soil additive, as a sealant, as a desiccant to draw water out of the air, to clean ponds, to make kitty litter and in cosmetics. Montmorillonite is a common mineral and, despite being named after Montmorillon, France, can be found all over the world, including many deposits in Australia. It is not known where this particular specimen originates from. Montmorillonite is an economically and socially significant material with a wide variety of uses. Having samples of common and important minerals allows collections, like the Burke Museum, to have a more complete view of the land on which they are located, and therefore a more complete view of heritage. 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 tennis-ball sized chunk of aluminium silicate clay. It is primarily white, accented with orange and brown.burke museum, beechworth, geological, geological specimen, clay, montmorillonite

There are 17 opal fields in Australia. This opal bearing stone was found in Lightning Ridge, NSW over what is known as the Great Australian Basin. This basin was formed and covers an area of 1.7 million square kilometers in eastern Australia in the Cretaceous period. This basin used to contain an inland sea, which provided an environment where silcrete eventually formed when water levels changed. This eventually seeped into other structures, and eventually hardened and formed opal. Lightning Ridge has a population of around 2000 people, with about 80 000 visitors every year. It is a historic mining town, and is known for its deposits of a rare black opal. Mining started in the area in the late 1800s, early 1900s when the black opal was discovered. This opal-bearing stone is of social and historical significance. It is from Lightning Ridge, which is well-known for being a large producer of opal stones, most famously black opal. The history of the period dates back to 140 million years, with the discovery of black opal in the early 1900s causing interest in the area. 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 solid mineral specimen in shades of beige and light orange*** silica based? burke museum, beechworth, geological, geological specimen, opal, opal fields, australia, lightning ridge, new south wales, great australian basin, cretaceous, silcrete, black opal, mining

Alluvial deposits along with water were scooped into this pan and aggressively agitated to allow dense material, such as gold, sink to the bottom for easy extraction.Mining played an important role in the history of Beechworth, for the township was established in the mid-1850s after gold was discovered in the area. The success of goldmining lead to the growth and development of early Beechworth.A circular gold panning tin featuring sloped sides, a folded over rim, and handles.burke museum, beechworth, gold mining, alluvial mining

Feldspar, derived from the German word feldspat, is a group of minerals which is the most common mineral group found on Earth, making up more than half of the planet's crust. The major rock-forming minerals in the Feldspar group include albite, anorthite, orthoclase and microcline. (Mindat, Feldspar Group). Orthoclase is part of the Feldspar Group subgroup, Alkaline Feldspar, which are known to be poor in calcium, and mostly rich in potassium. It is further also considered to be a K Feldspar, a subgroup of Alkaline Feldspar that are Potassium-dominant with variable crystal symmetry and Al-Si ordering state. Orthoclase are most commonly Colorless to white, Greenish white, Grayish yellow, or Pale pink and transparent to translucent with slightly pearly cleavage. The mineral rates at a 6 on the Mohs Hardness Scale. (cannot be scratched with a knife, but scratches glass with difficulty). The stronger green colour of this particular specimen is distinctive to the Broken Hill region (where it was found), and due to a small amount of lead. (BB) Its qualities find it misidentified at times as as microcline variety amazonite. Broken Hill is one of the world’s richest lead-zinc-silver deposits. The huge, 300-million-tonne orebody was discovered in 1883 and the superb mineral specimens attract collectors from around the world. (Australian Museum, Minerals from Australia: Australian mining regions)While feldspar is not by any means rare, this particular specimen has qualities distinctive to the Broken Hill mining district, with these properties leading at times to the mineral's misidentification. This creates potential for further study and identification of these mineral deposits through methods such as microscopic twinning, or using the position of certain d values in XRD patterns to calculate the degree of disorder of a K-feldspar, as discussed on the Mindat website (Mindat.com, Orthoclase:About Orthoclase). 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 aluminosilicate mineral composition which is primarily pale green and blue-grey in colour with traces of beige and white throughout. Note: green plumbian orthoclase (aka green feldspar) is an indicator mineral for the Broken Hill style lead-zinc deposits.N/Abroken hill mine, geological specimen, minerology

Hematite is an iron ore significant for its high iron content (70%) and as being one of the two main iron oxide minerals, the other being magnetite. Hematite has a rating of 5-6 on the Moh's hardness scale and is often found as an accessory mineral in many igneous rocks. (an accessory mineral being "any mineral in an igneous rock not essential to the naming of the rock" - Britannica) Hematite has historically been the mainstay of South Australia’s iron ore production. (Magnetite: South Australia’s potential) Making up the eastern section of the Gawler Rangers, the Middleback Range is a mountain range on the eastern side of Eyre Peninsula in South Australia that has been a source of iron ore (its main commodity in minerals) for over a century. (see https://www.mindat.org/loc-22576.html). "Large reserves of high-grade iron ore were identified in 1890 in the Middleback Range, west of Whyalla. From 1915 these ores were shipped to Newcastle and later to Port Kembla, both in New South Wales. Local production of pig iron began when the first blast furnace was opened at Whyalla in 1941, and construction of an integrated iron and steel plant began there in 1958." (Britannica, South Australia: Resources and power). This area is home to 24 mines/mineral deposits (according to mindat.org, thought the Sarig Map provided by SA gov on their Energy and Mining website indicates significantly more mining leases).This mineral specimen was collected from the Middleback Ranges before the area was identified as holding large reserves of iron ore and being commercially mined and is representative of South Australia's significant and ongoing history of iron ore mining, and its contribution to Australia's steel manufacturing industry of the early 20th century (this specimen being collected in the prelude to these events).A small ferric oxide mineral composition a mid-blue-grey in colour with specks of rust-brown throughout.HEMATITE / (iron oxide) / Locality: Middleback Ranges, S. Aust.middleback ranges, iron ore mining, mining, south australia

This specimen is a native copper specimen that is metallic. Copper is typically found in the earth's crust and is often found alongside other metals such as gold, zinc, lead and silver which all belong to the same group which is the Copper/Gold group. Copper is most commonly formed from large masses of molten lava rock which has solidified in the earth's crust and over time though different sizes and speeds of crystal growth has turned into large amounts of copper, stored in porphyry copper deposits. Copper has a distinctive colour, yet can sometime appear blue and greenish which is often caused by oxidisation or a mixture of copper and other metals. This specific specimen was recovered from Moonta, South Australia. The Moonta Mining Company was established in 1861, after a Shepard in the area noticed traces of copper. This lead to a rush in the copper mining industry which was relatively young in Australia at the time, making Moonta Mining Company one of the richest in Australia. By the 1860's, South Australia had been nicknamed the "Copper Kingdom" due to its vast amount of Large copper mines and resources. As of 2016, Australia was the second largest producer of Copper internationally, following behind Chile in first place. This copper specimen is significant historically and scientifically as it is such an important metal commonly used throughout the world in various ways. Copper is an invaluable recourse used in daily life, used in most electrical appliances as it is a great conductor of heat and electricity, as well as being soft and malleable, making it easy to bend and mould into delicate sheets and wires. Copper does not corrode and is therefore used in the production of water pipes among countless other significant necessities that are often overlooked in our society. Historically, Copper holds great significance as it was the first metal used by humans. It was discovered roughly 9000 years ago and was utilised by the Neolithic Man who learnt that heating the metal made it more malleable, thus tools and utensils were made which were far superior to the previous stone tools used by humans. This history and its connection to the current and ongoing relationship between humans and copper must be preserved and highlighted as it is integral to the history of all humankind. A small, palm-sized solid native copper mineral specimen with shades of browns, black and rustic tones throughout the specimen.NATIVE (metalic) COPPER / Locality: Moonta, South Australiabeechworth, burke museum, geological specimen, native specimen, geological, mineral, mineralogy, indigo shire, beechworth museum, copper, copper ore