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The Beechworth Burke Museum
Geological specimen - Anthracite crystal, Unknown
... . This specimen is part of a larger collection of geological and mineral ...Anthracite typically occurs in geologically deformed areas due to extreme heating – with temperatures ranging from 170 to 250 °C – caused by igneous intrusions or high geothermal gradients. It is most commonly found in northeastern Pennsylvania in the United States; however, smaller amounts are also found in Australia, China, eastern Ukraine, South Africa, western Canada, and other countries. This specimen was recovered from Tasmania and is 85-95% carbon.Anthracite is the mineral name for hard coal and is the least plentiful of all coal types. It is clean to the touch and, when polished, is used for decorative purposes. Before natural gas and electricity, anthracite was used for domestic heating as it produces little dust, burns slowly, and gives off a minor amount of smoke. However, it is also limited in abundance and expensive. 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 highly metamorphosed coal mineral with a black/steel-grey shiny metallic lustre.geological specimen, geology, geology collection, burke museum, beechworth, indigo shire, geological, mineralogy, victoria, alfred selwyn, anthracite -
The Beechworth Burke Museum
Geological specimen - Selwynite, Unknown
... of geological and mineral specimens collected from around Australia ...Selwynite is a fine-grained, compact green rock made primarily of chromian muscovite (fuchsite) and diaspore. Corundum and fuchsite can occur together in the form of massive aggregates or nodules. Often, copper carbonates are found as earthy films or tiny crystals in joint planes. The mineral name honours the late A. R. C. Selwyn, founding Director of the Geological Survey of Victoria. The particular specimen, a mottled green stone suitable for carving was recovered and found in Heathcote, Victoria, Australia. The rarity and qualities of this mineral attracted commercial mining, which was not successful, but traces of the mine shafts still exist today, and it is still highly valued by mineral collectors.Selwynit is considered to be one of the rare forms of rock because it is composed of phosphate minerals containing zirconium. This is an extremely rare combination found in nature. 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 fine grained rock composed of mainly of chromian muscovite (fuchsite) diaspore and corundum.geological specimen, geology, geology collection, burke museum, beechworth, mineralogy, heathcote, mineral collectors, selwynite, green rock, rock specimen -
The Beechworth Burke Museum
Geological specimen - Marble, Unknown
... of a larger collection of geological and mineral specimens collected ...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 -
The Beechworth Burke Museum
Geological specimen - Fluorite (purple)
Fluorite comes in a variety of natural colours and crystal formations and glows under ultraviolet light (the word 'fluorescence' comes from the same etymological source). In its pure form, calcium fluoride, it is a colourless combination of the elements calcium and fluorine, but gains its colour from trace elements that infiltrate or replace calcium within its crystal structure during its formation. Although fluorite crystals polish well and can achieve a high level of lustre, the mineral is very soft (4 on MOHS hardness scale) so it is unsuitable for use in rings and must be handled and stored carefully if used in other forms of jewellery. Most crystals of the mineral are too coarse for decorative purposes but have been mined under the name fluorspar for a variety of commercial and industrial purposes. These include the production of hydrofluoric acid, smelting metal alloys, producing glazes and ceramic finishes and use in medical and dental products. An existing label for this specimen indicates that its origin or collection-point was 'probably USA.' Fluorspar, the form of fluorite used commercially and industrially, was mined in significant quantities in the counties of Hardin and Pope in South-Eastern Illinois throughout the Nineteenth and Twentieth Centuries. Fluorite was made Illinois' state mineral in recognition of its contribution to the state's identity and economy. The specimens are significant as examples of surveying activity undertaken to assess and direct the development of the mineral resource industries, as well as the movement to expand human knowledge of earth sciences such as mineralogy and geology in the nineteenth century.The specimen is a piece of purple shaded fluorite (also known as fluorspar), the mineral form of calcium fluoride. The unpolished specimen presents a dark purple interior with a substantial dark grey crust representing the matrix from which the specimen was obtained. Existing label: Flourite / (purple) / probably / USA / BB /burke museum, beechworth, geological, geological specimen, fluorite, flourite, calcium fluoride, hydrofluoric acid, jewellery, indigo shire, north-east victoria, mining, illinois, usa, united states, fluorine, gemstones, purple stones -
The Beechworth Burke Museum
Geological specimen - Bituminous Coal, Unknown
... . This specimen is part of a larger collection of geological and mineral ...Bituminous coal is the most common type of coal, abundantly found in ancient coal deposits which can be dated back millions of years. Often referred to as soft or black coal, this specimen exhibits a high carbon content, ranging from 76-86%. It also holds a relatively high energy density (27 MJ/kg) meaning that it releases significant amounts of energy when burned. Bituminous coal is most commonly used for electricity generation, as well as in the production of steel. This particular piece of coal was collected as part of the Geological Survey of Victoria in the nineteenth century. It originates from Cape Paterson, a seaside village located in South Gippsland, Victoria (located on Bunurong Country). The discovery of bituminous coal in this locality was first made in 1826 by explorer William Hovell. More discoveries were gradually made over the following decades and in 1859 the Victorian Coal Company commenced the first active coal mining operations in the state by sinking a number of shafts and bores near the area of Cape Paterson. Evidence of this coal-focused past can be found today at the State Coal Mine Museum in the nearby town of Wonthaggi. This specimen is significant as it was collected from the locality of Cape Paterson in Victoria, an area that has since become historically instrumental in the mining of coal and other substances in the state 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 hand-sized piece of bituminous coal with a shiny black-grey surface and jagged edges.Existing Label: BITUMINOUS COAL / Locality: Cape / Patterson, VIC. burke museum, beechworth, geological, geological specimen, state coal mine museum, wonthaggi coal mine, victorian coal company, bituminous coal, coal victoria, coal energy generation, william hovell, cape paterson, coal specimen -
The Beechworth Burke Museum
Geological specimen - Malachite, Unknown
... of geological and mineral specimens collected from around Australia ...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 -
The Beechworth Burke Museum
Geological specimen - Montmorillonite
... . This specimen is part of a larger collection of geological and mineral ...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 -
The Beechworth Burke Museum
Geological specimen - Cassiterite
... of geological and mineral specimens collected from around Australia ...This specimen is Cassiterite in Quartz. Cassiterite is a tin oxide metal that forms in thin crystals which can have a beautiful lustre. Quartz is made of silicon dioxide, also known as silica, and is one of the most common minerals on earth. Cassiterite has been a fundamental source of tin ore for humans throughout history, including today. Tin is an important metal that has a wide variety of human uses in different areas, from dying fabric, to making mirrors, and their most well-known use ‘tin’ cans. Tin cans are primarily made of steel and are coated with tin in order to take advantage of tin’s property of being non-corroding. This is a massive step in the history of food preservation. Tinned food first reached Australia in 1815 with early settlers, and it began to be manufactured here in the 1840s. It was incredibly popular, and was a highly exported product, which would be a contributing factor to the ‘tin mining boom’ of the early 1880s. This specimen was collected at Jingellic, New South Wales, in about 1852. Although the Goldfields of the 1800s are much more well-known, tin mines existed alongside the gold mines which began in the mid 19th century and extended almost one hundred years, to the mid 20th century. Specimens like this would have been used as evidence to justify tin mining operations in the region as an investment. 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. The Geological Survey of Victoria was headed by British geologist, Alfred Richard Cecil Selwyn (1824-1902), who was responsible for issuing over 60 geological maps during his 17 years as director. These maps were all hand-drawn and coloured and became the benchmark for accuracy for geological mapping. 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 fist-sized solid geological specimen made on one half of tin oxide, which is dark grey, and on the other side of silica, which is brown and cream.burke museum, beechworth, geological, geological specimen -
The Beechworth Burke Museum
Geological specimen - Chiastolite
... of geological and mineral specimens collected from around Australia ...It is made up of andalusite. Andalusite is a rock-forming mineral, sometimes found in granite or schist. It is often used to make glass, ceramic products, chemicals, and heat-resistant bricks as it can withstand high temperatures without changing. The chiastolite contains particles of graphite, which arranges in geometric patterns. When crystal growth occurs in the rock, the granite particles concentrate at crystal interfaces and can result in cross shapes. These ‘cross stones’ have been valued and used for their spiritual or religious meaning and used as charms, gems, or amulets. Chiastolite was first discovered in 1754, seen in a description in a published book by a palaeontologist, Franciscan priest, and Spanish author, Jose Torrubia. Deposits have been found in Australia, France, the USA, Chile, Canada, Spain, Brazil, Sri Lanka, and Russia. Deposits have been found in Western Australia and South Australia. This particular specimen was found in Bimbowrie, South Australia. Other chiastolite specimens have been found in Bimbowrie, along with jasper, quartz, and aventurine in the form of rolled pebbles or schist. This chiastolite specimen is socially and historically significant. It is a very rare sort of andalusite mineral. It is from one of only two locations where it is regularly found in Australia. The carbon cross has made it an important religious symbol in the past. Its ability to withstand high temperatures has made it a common ingredient in heat-resistant bricks and ceramics today. 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 metamorphic mineral consisting of andalusite, with a cross shaped graphite pattern in colours of grey, brown and yellowburke museum, beechworth, geological, geological specimen, andalusite, chiastolite, geometric, cross stone, spiritual, religious, australia, south australia, bimbowrie, quartz, jasper, aventurine, schist -
The Beechworth Burke Museum
Geological specimen - Cerussite, Unknown c.1890s
Named in 1845 by Wilhelm Karl von Haidinger cerussite takes its name from the Latin cerussa, meaning 'white lead'. When viewed under certain lighting conditions cerussite gives of fire and rainbow-like colours (due to its high dispersion) and it is quite sought after by geological collectors for this very reason. Cerussite is usually found in the oxidised zone of lead ore deposits. It is a very common weathering product of galena and other lead ore minerals. It is a secondary mineral, meaning it forms as a result of the alteration of pre-existing minerals in the Earth’s crust. The presence of lead in cerussite makes it potentially toxic. Historically, it has been an important source of lead, which has numerous industrial applications, including in batteries, construction materials, and radiation shielding. Cerussite has a crystal structure that belongs to the orthorhombic crystal system. Its crystal structure is characterized by a three-dimensional arrangement of atoms in a repeating pattern. The crystal lattice of cerussite consists of interconnected lead (Pb) and carbonate (CO3) ions. This crystal structure is visible in the specimen. This specimen was found in Dundas (formerly Mount Dundas), a historical mining locality, mineral field and railway located on the western foothills of the West Coast Range in Western Tasmania. During the 1890s Dundas swelled in numbers however it is now lost in a temperate rainforest and its population is now 2. The present Dundas Extended mine, about 1.5 km east of Dundas is presently worked for specimen material.Faceted cerussite gems are considered rare and valuable, given the softness of the mineral. This item is not a faceted gem however its historical and scientific research potential give it significance; mined in an Australian township, this cerussite could shed light on the now lost history of Dundas and the mining that occurred there. Additionally, the uses of this mineral in historical industrial processes give it scientific significance. Such knowledge can add to understandings of the geographical and geological nature of Western Tasmania and allow for further study of Australian geological specimens. A small lead carbonite mineral with shades of cream, white and brown throughout, flaky shards of white at base. CERUSSITE / (lead carbonite) / Locality: Dundas, W. Tasmaniadundas, tasmania, cerussite, lead, orthorhombic, geology, minerals, mining -
Federation University Historical Collection
Rocks, Mica Schist With Form of Mineral Included
From the Ballarat School of Mines.Geological specimenrocks, geology, mica schist -
Federation University Historical Collection
Booklet, The Ballarat School of Mines and Industries 1870-1920 Jubilee Booklet, 1920 (estimated)
The first school of Mines in Australia was established at Ballarat in 1870. At the time of its jubilee (1930) the following people were members of the School Council: W.H. Middleton (President), W.T. Humphreys (VP), J.S. Vickery (VP), F. Barrow, Col. W.K. Bolton, William Baragwanath, A.E. Cutter, J.N. Dunn, G. Fitches, W.H. Fleay, F. Herman. W.D. Hill, T. Hurley, K. Kean. J. Kelly, L. Lederman, Mayor of Ballarat, Mayour of Ballarat East, D. Maxwell, M. Martin, R. Maddern, D. Ronaldson, F. Saunders, R. Stephenson, A.O. Stubbs, R.E. Tunbridge. The School Staff in 1920 comprised: Herbert H. Smith, Walter Rowbotham, Reginald L. Cutter, M.C. Young, Hilda Wardle, M. Wiliamson, P.S. Richards, L.H. Archibald, J. Woods, Ken Moss, W. Kenneth, Mrs McIlvena. B. Robinson, S. Rowe, E. Hope-Jones, Miss Abrams, L.St.G.P. Austin, Alfred Mica Smith, J.R. Pound, Herbert R. Murphy, N.H. Junner, Maurice Copland, L.H. Archibald, E.J.A. McConnon, Newton King, D.m. Hull, T.R. Gordon, John M. Sutherland, T.K. Jebb, Dick Richards, C. Tonkin, A.W. Steane, J. Paterson, H.W. Malin, R.V. Maddison, S.M. Mayo, F.A. King, W.H. Steane, T.R. Gordon, T.A. Williams, H. Waldron, G. Black, E.J. McConnon, R.V. Duncan. R. Cutter, E.G. Vawdrey, Hilda WardleWhite stapled booklet - landscape format - 20pp + soft covers with blue writing. Includes an historical sketch of the Ballarat School of Mines. Contains images of the school from around 1920. The history outlined in the booklet follows: 'Ballarat has helped to influence the life and destinies of Australia in many ways, the recital of which would perhaps prove tedious to the citizens of less favoured localities! However, it can be said, without much fear of contradiction, that only less known thought Australia than its fame as a gold field is the reputation won for it by its school of Mines, ... Ballarat was still quite a new place when the School was founded, but a very propserous and popular place all the same, with a go-ahead lot of citizens brim full of the spirit of enterprise which seemsto animate mining populations generally. Money was plentiful, and they launched out into ventures, which later, were to develop and take the place of the gold mines, while what is more to the point, they understood the value of education. the old digging days were passing away. So far as Ballarat itself was concerned the day of the cradle and tin dish had already passed into an antiquity "as dead and distant as the age of the Tubal Caon," said dir redmond Barry on declaring the School open. Mining had become a serious business, and the mining engineer, the metallurgist, and the geologist had become a power in the land. In these circumstances the suggestions to found a School of Mines met with ready acceptance. The late Mr James M. Bickett had the honor of bringing forward the proposition at a meeting of the Ballarat Mining Board in October, 1869. it was agreed to, and the Government, having been approached for assistance, granted a lease of the old Supreme Court buildings at a nominal reantal. A modest sum, including 100 pounds from the Borough Council of Ballarat West, was subscribed by a number of sympathisers, and on the 26th October, 1870, the inaugural address was delivered by Sir Redmond Barry, the first President of the School. Classes were commenced on the 23rd January, 1871. The students at first were mostly adults. They were chiefly men emloyed at the mines, who had the wisdom and energy to devote their spare time to study, and, though their attendance was somewhat irregular, they made very good progress. Old prints which have been preserved show them at work at furnaces, big bearded men of the old-fashioned type of miner. It is interesting to note that among those who gave evidence and encouragement was Sir Roderick Murchison, who many years before had advised Cornish miners to emigrate to Australia to search for gold, and who in 1848 was in possession of gold ore sent from this country. Sir Roderick sent a parcel of books for the library, and gave useful advice as to the curriculum which should be adopted. The Museum, which now contains a most valuable collection of minerals, was one of the first things attended to, and the reports presented to the Council from time to time speak of additions being made from all parts of the world. New equipment was constantly being added to the School, a good deal of assay work was done, and some specimens were sent from the East Indies for examination as far back as 1873. By this time there was a difficulty in providing accomodation for the students who wished to enrol, and the number of instructors had grown from two to four. In 1882 the first building was being erected on what was then part of the gaol reserve. A little more than ten years afterwards a buildnig formerly serving as a Methodist Church was absorbed, while later on, the demand for accomodation increasing, the attack upon the gaol was renewed. The School continued to grow in reputation and size, and became the science centre of the district, and in 1889 a learge new building was opened by Sir Alexander Peacock. Students came from over seas as well as from all the States of Australia, and after going through their courses they took with them the name and fame of the old School to all parts of the globe. School of Mines boys have played a great part in developing the mining fields of Western Australia, South Australia, and africa, while old students who have made a name in their profession are constantly dropping in to see how the old place is getting along. It was not to be expected, however, that the Ballarat School would be left without rivals, its very success inspiring competition. Mining Schools were started in other parts of Australia, and, at the same time, Victoria ceased to hold first place as a mining state. On the other hand there was a great advance in manufacturing, and the demand for technicaly trained men became a great and as insistent as ever it had been for trained mining men. The Council was quick to adapt the school to the new conditions, and the result is seen in the institution, which is one of Ballarat's proudest possession. Instruction is given in all branches of technical work, and the classes are filled with students who are building up for Ballarat a reputation as an industrial centre, which promises to equal that which it formerly held as a mining town. Owing to its bracing climate, its abundant opportunities for recreations, and its accessibilty, Ballarat as a city is an ideal place for educational purposed, and is yearly becoming more and more appreciated throughout the State. The chairman of one of Ballarat's biggests industries claims that the workman can do twice the day's work here that he can do in Melbourne. he was a little enthusiastic over it, perhaps, but it is a well-known fact that the healthy and invigourating Ballarat climate is conducive to both physical and mental activity, and the records of the School provide ample proof of it. One of the most interesting and successful branches of the School of Mines and Industries - if the name be enlarged with the enlargement of its scope - is the Technical Art School. "The City of Statues" has from its earliest days been a stronghold of art. Art schools have flourised here, and in 1905 the Education Department came to the conclusion that the best thing to do with them was to place them under the management of the School of Mines Council. A magnificent new Technical Art School was built at a cost of some 12,000 pounds on the site of the old Supreme Court building, and was formally opened on the 23rd July, 1915. The results have not only been justified but surpassed all anticipations. The most comprehensive list of subjects is taught, and this list is constantly added to. Students have flocked to the art School, which may be said to occupy a unique position in Australia, and its record of success is really astonishing. Its students supply art teachers for the newer schools that are being built, and many occupy leading positinos in important business houses. So well is its reputation known that orders are constantly being received, not only from Victoria, but from other States, for honor boards and challenge shields to be designed and made. The most recent addition to the School of Mines and Industries is the Junior Technical School, for which a new building is now being erected on a portion of the gaol site, transferred to the School of Mines Counci by the Government. At the present moment temporary quarters are being occupied. Some students after passing through the Junior School go straight to employment, continuing perhaps to attend the evening trade classes, while others move on to the senior School. In a review of the work of the School of Mines mention must be made of a series of industrial research carried out under supervision of the Principal. One in particular, regarding the suitability of the local ores for the manufacture of pigments attracted much attention, while the experiemtns on the manufacture of white potery from Victorian clayes were considered of sufficient importance by the Federal Advisory Council of Science and Industry to warrant the appointment of a special investigator. The results of these have been most encouraging, and may have far-reaching consequences. The vocational training of returned soldiers also should not be overlooked. The work was taken in hand from the first, before the Repatriation Department gave assistance, and now with the help of the department of the School has become one of the largest vocational training centres in Victoria outside of Melbourne. The soldiers, trained in a variety of occupations, have made remarkable progress, and already considerable numbers have found employment in local workshops and factories. To sum up, the School is divided into the following departments, each well staffed and equipped: - The School of Mines, science, and Engineering; the Techncial Art School, the Boys' Junior Technical School, the Girl's Preparatory Technical Classes, Trade Classes, and the Commercial School. The school of Mines, science and Engineering, comprises the following branches: - Mining, Metallurgy, Geology, Electrical Engineering, Civil Engineering, Mechanical Engineering, Applied Chemistry, and Pharmacy. Battery treatments, Cyanide Testing, Smelting, Assays, and Clay Testing from a regular part of the School's work. Students gaining qualifications obtain concession in their courses at the university, should they proceed there to continue their studies. The technical Art school curriculum includes training in all branches of pictorial and applied art, an Architectural Diploma Course, a Draughtman's Course, technical Art teachers' Course, Photography,Ticket Writing, Art Metal Work, Woodcarving, Needlework, and Leather work. The Trade Classes give instruction in Telephone Mechanics, telegraphy, Carpentry, Cabinet Making, Plumbing, Blacksmithing, Fitting, Electric Wiring, and Printing. Numerous Scholarships are offered every year, and altogether students will find few places to equal the Ballarat School of Mines and Industries as a training place for their life's work. One of the first in the continent to be established, its Jubilee finds it still in the front rank, keeping pace with the times, and offering to the youths of this country the means of taking advantage of Australia's teeming opportunities. william, battery, smith, herbert, drawing from the antique, ballarat school of mines botanical gardens, ballarat school of mines, redmond barry, alfred mica smith, james bickett, museum, dick richards, ballarat junior technical school, s m b, ballarat school of mines and industries, ballarat technical art school, model mine, james m bickett, j m bickett, roderick murchison, vocational training rooms, wesley church, methodist church, alexander peacock, lathes, repatriation, repatriatin department, war service, school council, baragwanath, gold mining, mining laboratory, plaster cast, r.w. richards, anniversary, jubilee -
Federation University Historical Collection
Book, A Descriptive Catalogue of the Minerals in the Museum of the School of Mines, Ballaarat, 1882, 1882
The Museum of the Ballarat School of Mines was established in 1872. The curator in 1882 was Ferdinand M. Krause. Prefatory Notice by James Oddie). The want of a guide through the technical collections of The School Mines has long been felt by visitors and students - a guide , not so much to those who merely 'look' at the various exhibits in the Museum, but an instructor to those who desire to take away with them some practical information on the natural occurrence and economical value of the objects exhibited. This want is being filled by the labour of Mr. Krause, whose first installment - 'A Descriptive Catalogue of the Minerals' - is herewith represented to the visiting public." Introduction to the catalogue: " The collection is still in its early growth, and far from being a complete representation of the Mineral Kingdom; many varieties, species, and even whole groups are absent. This state of incompleteness will, no doubt, be adjusted in the sequence, and progressive lists issued from time to time. 'Ad interin' the present catalogue will, be found useful to students and visitors of the School. As far as practicable, the classifications of the minerals accords with that adopted at the Royal School of Mines, London. The numbers prefixed to the species in the catalogue agree with those on the descriptive labels which accompany each specimen, and also with those attached to the specimens themselves. On the descriptive labels the chemical composition of the minerals is expressed in formulae usually employed in standard mineralogical works. Students who have note paid attention to mineralogical chemistry will note that each dot over a symbol is equivalent to one atom of oxygen, .... A bar through a symbol denotes a double atom of the base, .... " In 1882 the collection was housed in 33 cases. The catalogue outlines the specimen types housed in each case. The classification of minerals accords with that adopted at the Royal School of Mines, London. Leather covered book of 94 pages with gold lettering on the front, including "F.M. Krause". The book includes a plan of the museum layout, plan of the grounds and buildings of the Ballarat School of Mines and a prefatory notice by James Oddie.ballarat school of mines, ballarat school of mines museum, museum, krause, ferdinand krause, fm krause, oddie, james oddie, geology, mineralogy, charles boyd, f.m. krause, minerals, curator -
Federation University Historical Collection
Booklet, The Ballarat School of Mines and Industries 1870-1920 Jubilee Booklet, 1920 (estimated)
The first school of Mines in Australia was established at Ballarat in 1870. At the time of its jubilee (1930) the following people were members of the School Council: W.H. Middleton (President), W.T. Humphreys (VP), J.S. Vickery (VP), F. Barrow, Col. W.K. Bolton, William Baragwanath, A.E. Cutter, J.N. Dunn, G. Fitches, W.H. Fleay, F. Herman. W.D. Hill, T. Hurley, K. Kean. J. Kelly, L. Lederman, Mayor of Ballarat, Mayour of Ballarat East, D. Maxwell, M. Martin, R. Maddern, D. Ronaldson, F. Saunders, R. Stephenson, A.O. Stubbs, R.E. Tunbridge. The School Staff in 1920 comprised: Herbert H. Smith, Walter Rowbotham, Reginald L. Cutter, M.C. Young, Hilda Wardle, M. Wiliamson, P.S. Richards, L.H. Archibald, J. Woods, Ken Moss, W. Kenneth, Mrs McIlvena. B. Robinson, S. Rowe, E. Hope-Jones, Miss Abrams, L.St.G.P. Austin, Alfred Mica Smith, J.R. Pound, Herbert R. Murphy, N.H. Junner, Maurice Copland, L.H. Archibald, E.J.A. McConnon, Newton King, D.m. Hull, T.R. Gordon, John M. Sutherland, T.K. Jebb, Dick Richards, C. Tonkin, A.W. Steane, J. Paterson, H.W. Malin, R.V. Maddison, S.M. Mayo, F.A. King, W.H. Steane, T.R. Gordon, T.A. Williams, H. Waldron, G. Black, E.J. McConnon, R.V. Duncan. R. Cutter, E.G. Vawdrey, Hilda WardleWhite stapled booklet - landscape format - 20pp + soft covers with blue writing. Includes an historical sketch of the Ballarat School of Mines. Contains images of the school from around 1920. The history outlined in the booklet follows: 'Ballarat has helped to influence the life and destinies of Australia in many ways, the recital of which would perhaps prove tedious to the citizens of less favoured localities! However, it can be said, without much fear of contradiction, that only less known thought Australia than its fame as a gold field is the reputation won for it by its school of Mines, ... Ballarat was still quite a new place when the School was founded, but a very propserous and popular place all the same, with a go-ahead lot of citizens brim full of the spirit of enterprise which seemsto animate mining populations generally. Money was plentiful, and they launched out into ventures, which later, were to develop and take the place of the gold mines, while what is more to the point, they understood the value of education. the old digging days were passing away. So far as Ballarat itself was concerned the day of the cradle and tin dish had already passed into an antiquity "as dead and distant as the age of the Tubal Caon," said dir redmond Barry on declaring the School open. Mining had become a serious business, and the mining engineer, the metallurgist, and the geologist had become a power in the land. In these circumstances the suggestions to found a School of Mines met with ready acceptance. The late Mr James M. Bickett had the honor of bringing forward the proposition at a meeting of the Ballarat Mining Board in October, 1869. it was agreed to, and the Government, having been approached for assistance, granted a lease of the old Supreme Court buildings at a nominal reantal. A modest sum, including 100 pounds from the Borough Council of Ballarat West, was subscribed by a number of sympathisers, and on the 26th October, 1870, the inaugural address was delivered by Sir Redmond Barry, the first President of the School. Classes were commenced on the 23rd January, 1871. The students at first were mostly adults. They were chiefly men emloyed at the mines, who had the wisdom and energy to devote their spare time to study, and, though their attendance was somewhat irregular, they made very good progress. Old prints which have been preserved show them at work at furnaces, big bearded men of the old-fashioned type of miner. It is interesting to note that among those who gave evidence and encouragement was Sir Roderick Murchison, who many years before had advised Cornish miners to emigrate to Australia to search for gold, and who in 1848 was in possession of gold ore sent from this country. Sir Roderick sent a parcel of books for the library, and gave useful advice as to the curriculum which should be adopted. The Museum, which now contains a most valuable collection of minerals, was one of the first things attended to, and the reports presented to the Council from time to time speak of additions being made from all parts of the world. New equipment was constantly being added to the School, a good deal of assay work was done, and some specimens were sent from the East Indies for examination as far back as 1873. By this time there was a difficulty in providing accomodation for the students who wished to enrol, and the number of instructors had grown from two to four. In 1882 the first building was being erected on what was then part of the gaol reserve. A little more than ten years afterwards a buildnig formerly serving as a Methodist Church was absorbed, while later on, the demand for accomodation increasing, the attack upon the gaol was renewed. The School continued to grow in reputation and size, and became the science centre of the district, and in 1889 a learge new building was opened by Sir Alexander Peacock. Students came from over seas as well as from all the States of Australia, and after going through their courses they took with them the name and fame of the old School to all parts of the globe. School of Mines boys have played a great part in developing the mining fields of Western Australia, South Australia, and africa, while old students who have made a name in their profession are constantly dropping in to see how the old place is getting along. It was not to be expected, however, that the Ballarat School would be left without rivals, its very success inspiring competition. Mining Schools were started in other parts of Australia, and, at the same time, Victoria ceased to hold first place as a mining state. On the other hand there was a great advance in manufacturing, and the demand for technicaly trained men became a great and as insistent as ever it had been for trained mining men. The Council was quick to adapt the school to the new conditions, and the result is seen in the institution, which is one of Ballarat's proudest possession. Instruction is given in all branches of technical work, and the classes are filled with students who are building up for Ballarat a reputation as an industrial centre, which promises to equal that which it formerly held as a mining town. Owing to its bracing climate, its abundant opportunities for recreations, and its accessibilty, Ballarat as a city is an ideal place for educational purposed, and is yearly becoming more and more appreciated throughout the State. The chairman of one of Ballarat's biggests industries claims that the workman can do twice the day's work here that he can do in Melbourne. he was a little enthusiastic over it, perhaps, but it is a well-known fact that the healthy and invigourating Ballarat climate is conducive to both physical and mental activity, and the records of the School provide ample proof of it. One of the most interesting and successful branches of the School of Mines and Industries - if the name be enlarged with the enlargement of its scope - is the Technical Art School. "The City of Statues" has from its earliest days been a stronghold of art. Art schools have flourised here, and in 1905 the Education Department came to the conclusion that the best thing to do with them was to place them under the management of the School of Mines Council. A magnificent new Technical Art School was built at a cost of some 12,000 pounds on the site of the old Supreme Court building, and was formally opened on the 23rd July, 1915. The results have not only been justified but surpassed all anticipations. The most comprehensive list of subjects is taught, and this list is constantly added to. Students have flocked to the art School, which may be said to occupy a unique position in Australia, and its record of success is really astonishing. Its students supply art teachers for the newer schools that are being built, and many occupy leading positinos in important business houses. So well is its reputation known that orders are constantly being received, not only from Victoria, but from other States, for honor boards and challenge shields to be designed and made. The most recent addition to the School of Mines and Industries is the Junior Technical School, for which a new building is now being erected on a portion of the gaol site, transferred to the School of Mines Counci by the Government. At the present moment temporary quarters are being occupied. Some students after passing through the Junior School go straight to employment, continuing perhaps to attend the evening trade classes, while others move on to the senior School. In a review of the work of the School of Mines mention must be made of a series of industrial research carried out under supervision of the Principal. One in particular, regarding the suitability of the local ores for the manufacture of pigments attracted much attention, while the experiemtns on the manufacture of white potery from Victorian clayes were considered of sufficient importance by the Federal Advisory Council of Science and Industry to warrant the appointment of a special investigator. The results of these have been most encouraging, and may have far-reaching consequences. The vocational training of returned soldiers also should not be overlooked. The work was taken in hand from the first, before the Repatriation Department gave assistance, and now with the help of the department of the School has become one of the largest vocational training centres in Victoria outside of Melbourne. The soldiers, trained in a variety of occupations, have made remarkable progress, and already considerable numbers have found employment in local workshops and factories. To sum up, the School is divided into the following departments, each well staffed and equipped: - The School of Mines, science, and Engineering; the Techncial Art School, the Boys' Junior Technical School, the Girl's Preparatory Technical Classes, Trade Classes, and the Commercial School. The school of Mines, science and Engineering, comprises the following branches: - Mining, Metallurgy, Geology, Electrical Engineering, Civil Engineering, Mechanical Engineering, Applied Chemistry, and Pharmacy. Battery treatments, Cyanide Testing, Smelting, Assays, and Clay Testing from a regular part of the School's work. Students gaining qualifications obtain concession in their courses at the university, should they proceed there to continue their studies. The technical Art school curriculum includes training in all branches of pictorial and applied art, an Architectural Diploma Course, a Draughtman's Course, technical Art teachers' Course, Photography,Ticket Writing, Art Metal Work, Woodcarving, Needlework, and Leather work. The Trade Classes give instruction in Telephone Mechanics, telegraphy, Carpentry, Cabinet Making, Plumbing, Blacksmithing, Fitting, Electric Wiring, and Printing. Numerous Scholarships are offered every year, and altogether students will find few places to equal the Ballarat School of Mines and Industries as a training place for their life's work. One of the first in the continent to be established, its Jubilee finds it still in the front rank, keeping pace with the times, and offering to the youths of this country the means of taking advantage of Australia's teeming opportunities. william, battery, smith, herbert, drawing from the antique, ballarat school of mines botanical gardens, ballarat school of mines, redmond barry, alfred mica smith, james bickett, museum, dick richards, ballarat junior technical school, s m b, ballarat school of mines and industries, ballarat technical art school, model mine, james m bickett, j m bickett, roderick murchison, vocational training rooms, wesley church, methodist church, alexander peacock, lathes, repatriation, repatriatin department, war service, school council, baragwanath, gold mining, mining laboratory, plaster cast, r.w. richards, anniversary, jubilee -
Federation University Historical Collection
Book, A Descriptive Catalogue of the Minerals in the Museum of the School of Mines, Ballaarat, 1882, 1882
The Museum of the Ballarat School of Mines was established in 1872. The curator in 1882 was Ferdinand Krause. Prefatory Notice by James Oddie). The want of a guide through the technical collections of The School Mines has long been felt by visitors and students - a guide, not so much to those who merely 'look' at the various exhibits in the Museum, but an instructor to those who desire to take away with them some practical information on the natural occurrence and economical value of the objects exhibited. This want is being filled by the labour of Mr. Krause, whose first installment - 'A Descriptive Catalogue of the Minerals' - is herewith represented to the visiting public." Introduction to the catalogue: " The collection is still in its early growth, and far from being a complete representation of the Mineral Kingdom; many varieties, species, and even whole groups are absent. This state of incompleteness will, no doubt, be adjusted in the sequence, and progressive lists issued from time to time. 'Ad interin' the present catalogue will, be found useful to students and visitors of the School. As far as practicable, the classifications of the minerals accords with that adopted at the Royal School of Mines, London. The numbers prefixed to the species in the catalogue agree with those on the descriptive labels which accompany each specimen, and also with those attached to the specimens themselves. On the descriptive labels the chemical composition of the minerals is expressed in formulae usually employed in standard mineralogical works. Students who have note paid attention to mineralogical chemistry will note that each dot over a symbol is equivalent to one atom of oxygen, .... A bar through a symbol denotes a double atom of the base, .... " In 1882 the collection was housed in 33 cases. The catalogue outlines the specimen types housed in each case. Brown soft covered book of 94 pages with gold lettering on the front. The book includes a plan of the museum layout, plan of the grounds and buildings of the Ballarat School of Mines and a prefatory notice by James Oddie. It also includes handwritten notes by Curator Ferdinand Krause. .2) Business card of I.H. Barbery, engraver with F.W. Niven. The lithography of the plan of the Ballarat School of Mines at the back of the catalogue was undertaken by F.W. Niven.Handwritten inclusion of extra entries (probably by Ferdinand Krause).ballarat school of mines, ballarat school of mines museum, museum, krause, ferdinand krause, fm krause, oddie, james oddie, geology, mineralogy, charles boyd, royal school of mines london, london school of mines, classification -
Federation University Historical Collection
Photograph, Jack Barker and Phil Day with the Baragwanath Donation
William Baragwanath joined the Victorian Department of Mines in 1897, was director of the geological survey (1922-4), Chief Mining Surveyor (1924-43), Secretary for Mines (1932-34), consultant to the Department of Mines (1943-50) . He was born at Durham Lead on 1 August 1878 and was a former student of the Ballarat School of Mines. Baragwanath was president of the Royal society of Victoria (1943-44) and a councillor of the Ballarat School of Mines (1916-1950). After Baragwanath's death on 20 September 1966 the Department of Minerals and Energy (Geological Survey division) donated a number of Baragwanath's items to the Ballarat School of Mines, including this collection. Black and white photograph of E.J. Jack Barker (Ballarat School of Mines Principal) and Phil Day (Head of Geology) standing in front of a cabinet of geological specimens housed in a timber cabinet. ballarat school of mines, geology, ej barker, jack barker, phil day, baragwanath, william baragwanath, victorian mines department -
Bendigo Historical Society Inc.
Geological specimen - AMY HUXTABLE COLLECTION: MINERAL COLLECTION
... specimen AMY HUXTABLE COLLECTION: MINERAL COLLECTION ...Fifty three mineral samples collected by Amy Huxtable. Samples in two plastic partitioned boxes. Samples were originally housed in poor conditions in matchbox inserts and placed on cotton wool. Existing labels, hand printed on tan card: Cerussite, crystalline ore of silver lead Galena, ore of silver lead, fine grained Galena, ore of silver lead, coarse grained Native copper, wave like form Malachite, copper carbonate, ore of copper Chalcopyrite, copper iron sulphide, ore of copper lead Malachite, copper carbonate, ore of coppermining, sampling, mineral samples -
The Beechworth Burke Museum
Geological specimen - Chalcopyrite
... , this the specimen of this mineral can be used to reflect a wider history ...This specimen was recovered from Mica Schist, Canada. Chalcopyrite is a copper iron sulfide mineral with a chemical composition of CuFeS2. Its name derives from the Greek words for copper (chalco-) and brass (pyrite). It can be found in shades of yellow, green and grey, and, when exposed to acid, it can change to purple, blue, violet and yellow tones. Weathering can cause loss of its metallic luster and its brass-yellow colour. Chalcopyrite forms under various conditions, with the most significant deposits being hydrothermal in their origin. It is known globally as the most important ore of copper for thousands of years, and is thus considered a very important mineral formation. Given its golden appearance, it is often confused for the mineral gold, earning it the popular reputation as 'fool's gold' or 'yellow copper'. However, it can be straightforwardly distinguished from gold; the latter is soft, with higher specific gravity and a yellow streak, whereas chalcopyrite is brittle, easily scratched by a nail, and has a greenish grey streak. Copper was the first metal that was used by people. It was discovered by the Neolithic man about 9,000 years ago and it gradually replaced stone as it was easier to be shaped. In Australia, search for copper began after the European settlement, leading to the discovery of substantial deposits, like the one at the Olympic Dam in South Australia, which is regarded as one of the largest copper deposits in the world. Chalcopyrite has been used for copper since smelting processes began approximately five thousand years ago. Although by no means rare, this the specimen of this mineral can be used to reflect a wider history of industrial uses of copper for a significant portion of human 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 solid hand-sized copper iron sulfide mineral of brass yellow, often with an iridescent tarnish, with greenish-black streak and submetallic luster. Chalcopyrite can be formed in several ways, including crystalizing from accessory minerals in igneous rocks, or from magma or within volcano sulfide deposits. Most commonly, chalcopyrite are found in hydrothermal conditions, where it forms in hydrothermal veins. As a member of the tetragonal crystal system, it often takes the shape of tetra-headed crystals, often with striations along the sides of the crystals. #18 Copper pyrites/(chalcopyrite) in/Laurentian Slate/(page 315 of inventory)/page missing from/descriptive catalogue/ Other label: 81 /fool's gold, chalcopyrite, mineral, rock, geology, geological, hydrothermal, neolithic, european settlement, olympic dam, south australia, stone, deposits, specific gravity, greenish grey streak, brittle, mineral gold, metallic luster, cufes2, greek words -
The Beechworth Burke Museum
Geological specimen - Olivine Crystals, Unknown
... . This specimen is part of a larger collection of geological and mineral ...Olivine is mostly found on the Earth's surface in igneous rocks that are dark-coloured. It is common at divergent plate boundaries and at warm spots, such as volcanic areas. It crystalises and forms during the cooling of magma. Olivine is used in refractory sand, bricks, and gemstones. Olivine has been found on a number of meteorites, which might have originated from large asteroids or the mantle of a now-destroyed planet. This olivine crystal is thought to originate from Mount Noorat, with speculation that it could have originated from Mount Shadwell. Mount Noorat is a dormant volcano cone located in the Newer Volcanics Province of Victoria. Mount Noorat belongs to the Kirrae Wuurong people, who used the Mount as a place for meetings and gatherings prior to European settlement. Contact was first made between European settlers and the Indigenous people in 1841. The Mount has mostly been used for cattle and sheep grazing. Mount Shadwell is a well-known source of olivine and is the highest of a gathering of volcanic cones. The New Volcanic Province is located in South East Australia and covers 15000 square kilometres. It contains 400 explosive vents and small shield volcanoes. The last eruption is thought to have occurred 5000 years ago at Mount Gambier and Mount Schank. This olivine crystal has been identified as a volcanic bomb, which is a molten rock which was pushed out and ejected into the air when a volcano reupts. A rock needs to be larger than 65 mm in diameter to be classified as a volcanic bomb. This olivine volcanic bomb and its locality is historically and socially significant. The olivine was found in the Newer Volcanic Province, an area which contains over 400 dormant volcanoes. This olivine is one part of a volcanic bomb, which would have ejected when magma erupted out of a volcano. 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 iron-magnesium silicate mineral with shades of green and brownburke museum, beechworth, geological, geological specimen, olivine, igneous rock, volcanic, gemstones, volcanic bomb, meteorites, asteroids, plantes, mount noorat, mount shadwell, indigenous, kirrae wuurong people, newer volcanics province, victoria, european settlement, eruption -
The Beechworth Burke Museum
Geological specimen - Thunderegg agates, Unknown
... of geological and mineral specimens collected from around Australia ...Thunderegg Agates are formed within rhyolite volcanic ash layers. They are rough spherical shapes, varying in size from less than an inch to over a metre long. Thundereggs usually contain centres of chalcedony which may have been fractured followed by deposition of agate, jasper or opal, either uniquely or in combination. A unique characteristic that these specimens have is the fact that they often look like ordinary rocks on the outside, but slicing them in half and polishing them may reveal intricate patterns and colours. These particular specimens are examples of thunderegg agates. Agate is a variety of chalcedony, a cryptocrystalline form of quartz. The agate component contributes to the intriguing internal patterns of the specimens. The specific locality of these specimens is unknown but they can be found in flows of rhyolite lava. They are formed in gas pockets in the lava, which act as moulds. These specimens can be found globally, with specific locations in Germany being particularly abundant. 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 small solid specimens with pale, sandy-coloured exteriors and fractured internal patterns. burke museum, beechworth, geological, geological specimen, thundereggs, thundereggs agate, agate, rhyolite, rhyolite lava, volcanic ash, chalcedony, cryptocrystalline -
The Beechworth Burke Museum
Geological specimen - Fossil Leaves
... collection of geological and mineral specimens collected from around ...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 -
The Beechworth Burke Museum
Geological specimen - Garnet (red crystals) in galena (silvery metallic) and green feldspar, Unknown
... three specimens in one. Garnet Galnea Green Feldspar Minerals ...Garnet is a popular gemstone used in jewellery due to its hardness and durability. There are about 5 varieties of Garnet, which distinguish the colour of each stone. In Australia mostly Pyrope and Aimandine varieties are found; Pyrope, which is blood-red to black and Aimadine, which is brownish-red to black. Other varieties are rarely found in Australia. The garnets visible in this specimen are likely Pyrope. Galnea is the natural mineral form of lead sulphide and has had various uses throughout history; from makeup to car batteries. It was first mined in South Australia in 1841. Green feldspar is an amazonite mineral, a variety of the potassium feldspar called microcline. This particular mineral is considered uncommon. It has been used in jewellery throughout history. It is likely that this specimen was found in Broken Hill, NSW, presumed due to findings of specimens with similar combinations. Broken Hill is Australia’s longest-lived mining city. The city’s fortunes have come and gone against an extreme economic background of boom and bust which continues today.This geological specimen is a rarity, given that is formed of three distinct minerals and the richness of colour that remains visible in this item attests to the strength of each structure. As we cannot pinpoint exactly where this specimen was found further research can only strengthen what is known about mining within Australia. As such the item is significant due to its scientific rarity and its ability to represent three specimens in one. A solid palm-sized mineral that features shades of grey, red and green. garnet, galnea, green feldspar, minerals, mining, rare specimen -
The Beechworth Burke Museum
Geological specimen - Galena (with quartz), unknown
... of geological and mineral specimens collected from around Australia ...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 -
The Beechworth Burke Museum
Geological specimen - Sphalerite, Unknown
... A pipe-shaped specimen of sulfide-mineral zinc ore..., dodecahedrons. This specimen was collected in approximately 1852 ...Sphalerite or sphaelerite is named from the Greek word for 'treacherous' or 'deceiver' as specimens can vary widely in appearance, making them hard to visually identify. It is a zinc sulfide with the chemical composition (Zn,Fe)S, the most important ore of zinc. Specimens of sphalerite can contain iron as a substitute for up to 25% of the usual zinc present, as well as trace elements of gallium, cadmium, geranium and indium. Small amounts of arsenic and manganese may also be detected. Sphalerite is found in igneous, sedimentary and metamorphic rocks. It forms when carbonate rock encounters acidic, zinc-bearing fluid. It often forms in veins or in fissures of the existing rock, with colours and crystal shapes dependent on the composition of the the combining elements. It forms isometric crystal shapes including cubes, tetrahedrons, octahedrons, dodecahedrons. This specimen was collected in approximately 1852, in Broken Hill, NSW, as an adjunct to the Geological Survey of Victoria. It was donated to the Museum in 1868. Victoria and other regions of Australia were surveyed for sites of potential mineral wealth throughout the 19th Century. The identification of sites containing valuable commodities such as gold, iron ore and gemstones in a locality had the potential to shape the development and history of communities and industries in the area. The discovery of gold in Victoria, for instance, had a significant influence on the development of the area now known as 'the goldfields', including Beechworth; the city of Melbourne and Victoria as a whole.The specimen is significant as an examples of surveying activity undertaken to assess and direct the development of the mineral resource industries in Victoria and Australia, as well as the movement to expand human knowledge of earth sciences such as mineralogy and geology in the nineteenth century.A pipe-shaped specimen of sulfide-mineral zinc ore displaying patches of black, brown, beige and gold colouring. The main item has associated broken pieces. geological specimen, geology, geology collection, burke museum, beechworth, mineralogy, indigo shire, geological survey, sphalerite, sphaelerite, zinc ore, broken hill, nsw, victoria, galena, fluorite, chalcopyrite, lead, cadmium, gallium, germanium, indium, iron