Showing 287 items
matching geological survey.
-
Federation University Historical Collection
Letter, S.G. Turrell, Letter from S.G Turrell of the Brownhill Consols Ltd to the Ballarat School of Mines, 28/3/1911 (exact)
... and Geology in 1903 and Chemistry II, Metallurgy II, Steam and Gas... and Geology in 1903 and Chemistry II, Metallurgy II, Steam and Gas ...S. G. Turrell was a student at the Ballarat School of Mines and passed the Chemistry, Assaying, Metallurgy, Mineralogy and Geology in 1903 and Chemistry II, Metallurgy II, Steam and Gas Engines, Technical Chemistry, Mine Surveying, Electricity, Mining Geology and Engineering Drawing in 1904Two quarto pages. One from S.G. Turrell on Brownhill Consols Ltd letterhead asking Fred Martell of the Ballarat School of Mines for details on obtaining certificats. The second page is a list of the subjects passed by S.G. Turrell in 1903 and 1904university of ballarat, ballarat school of mines, fred martell, s g turrell, f j martell -
Federation University Historical Collection
Document, Robert S. Brain, Report on Rapid Surveys of the Gold-fields, Report on Parish of Mannibadar
One printed page.mannibadar, ernest lidget, geology, j. travis -
Kiewa Valley Historical Society
Book - Bogong High Plains x2, Early History and Discovery of the Bogong High Plains, 1968
The State Electricity Commission of Victoria constructed the Kiewa Hydro Electric Scheme in the north east of Victoria. Mr R.M. Duncan prepared the notes. He was a member of the S.E.C. Kiewa Branch from 1949 - 1966. This book was commissioned by the State Electricity Commission of Victoria. It consists of the early history of the Bogong High Plains and the origin of names of places and creeks in the area.This book was researched in 1968 by Mr R.M. Duncan who worked for the S.E.C. on the Kiewa Hydro Electric Scheme from 1949 to 1966. His sources were the Melbourne Public Library, the Victorian Historical Society, the North Eastern Victorian Historical Society and the Dept. of Crown Lands & Survey, Melbourne. The book is an accurate history of the Bogong High Plains given the available records at the time. Yellow cardboard covered book with black sketches and green print. 9 one-sided pages held together by 3 staples and taped over the staples. One - has sheets enclosed "The Three Floras of Bogong" and "General Geology of the Kiewa Area". 6 copies including 1 that is a photocopyDDTS hand written on front cover "Early History and Discovery / of the / Bogong High Plains" on cover top centre. "Settlement / of the / Kiewa-Valley" on cover towards the top slightly to the right. "Published by the / State Electricity Commission / of Victoria / July, 1968" on cover bottom left. "TR-K 596-4" on cover bottom left.bogong high plains. state electricity commission of victoria. kiewa. aborigines. kiewa valley. mullindollingong pastoral run. flora. geology -
The Beechworth Burke Museum
Geological specimen - Malachite, Unknown
... of a larger collection of geological and mineral specimens collected ...Malachite is a green copper carbonate hydroxide mineral and was one of the first ores used to make copper metal. Malachite has been utilised as a gemstone and sculptural material in the past as its distinctive green color does not fade when exposed to light or after long periods of time. Malachite is formed at shallow depths in the ground, in the oxidizing zone above copper deposits. The material has also been used as a pigment for painting throughout history. This particular specimen was recovered from the Burra Burra Copper Mine in Burra, South Australia. Otherwise known as the 'Monster Mine', the Burra Burra Copper Mine was first established in 1848 upon the discovery of copper deposits in 1845. Within a few short years, people from around the world migrated to Burra to lay their claim in the copper economy. By April 1848 the mine was employing over 567 people and supporting a population of 1,500 in the local township. Up until 1860, the mine was the largest metals mine in Australia, producing approximately 50,000 tonnes of copper between 1845 to its closure in 1877. The Burra Burra Mine was also famous for a number of other specimens, including; crystalline azurite, cuprite, and botryoidal and malachite.Malachite is considered a rare gemstone in that the original deposits for the stones have been depleted leaving behind very few sources. In addition, the use of Malachite as gemstones and sculptural materials remains just as popular today as they were throughout history. It is quite common to cut the stone into beads for jewellery. The fact that Malachite has such a rich colour and one that does not fade with time or when exposed to light makes it particularly rare. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study. A solid hand-sized copper carbonate hydroxide mineral with shades of yellow, blue, and light green throughout.geological, geological specimen, burke museum, indigo shire, malachite, malachite specimen, burra burra mine, burra, south australia, australian mines, mines, monster mine -
The Beechworth Burke Museum
Geological specimen - Galena Chalcopyrite, Unknown
... collected in Victoria as part of the Geological Survey of Victoria ...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 -
The Beechworth Burke Museum
Geological specimen - Feldspathic Sandstone
... were collected in Victoria as part of the Geological Survey ...Feldspathic arenites are sandstones that contain less than 90% quartz, and more feldspar than unstable lithic fragments, and minor accessory minerals.Feldspathic sandstones are commonly immature or sub-mature.These sandstones occur in association with cratonic or stable shelf settings. Feldspathic sandstones are derived from granitic-type, primary crystalline, rocks. If the sandstone is dominantly plagioclase, then it is igneous in origin Sandstone features prominently in public buildings throughout Victoria. Most of the sandstone used as dimension stone in the State came from three sources: the Heatherlie quarry in the Grampians (Silurian), the Bacchus Marsh area (Permian), and the Barrabool Hills near Geelong (Cretaceous).Sandstone features prominently in public buildings throughout Victoria, making this specimen special as it shows the materials used by Victorian building companies. Sandstone can also be crushed, crushed stone is used in the construction of roadways and road structures such as bridges, and in buildings, both commercial and residential. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study. A feldspar-rich sandstone, a sandstone intermediate in composition between an arkosic sandstone and a quartz sandstone, containing 10% to 25% feldspar and less than 20% matrix material of clay, sericite, and chlorite. Feldspathic arenite containing less than 90 percent of the composition of quartz. Feldspar is the main composition. Feldspathic arenite may contain fragments of unstable rock, and a little amount of other minerals such as mica and heavy minerals. Some feldspathic arenite have pink or red color because of the presence of potassium feldspar or iron oxide. There are also colored light gray to white. These sandstones are usually medium to coarse grained and can contain a high percentage of granules with angular until subangular roundness. The content of the matrix can appear as the rest up to more than 15 percent, and sorting of grains can present as moderate to poorly sorted. Feldspathic sandstones are generally immature in textural maturity. Feldspathic arenite can not be judged from the structure of the sediment. Bedding can emerge from the laminate parallel to the crossbed. Fossils may appear in the layer deposited on the sea. Feldspathic arenites usually appear on the craton or the continental shelf, which can be associated with conglomerate, quartz lithic arenite, carbonate rock, or evaporites. This sandstone may also appear on the succession of sedimentary basins deposited on an unstable or deep sea, and moving arc setting. According to Pettijohn (1963) Arkose make up about 15 percent of all sandstones. Some Arkose formed in situ when the granite and related rocks disintegrate and generate granular sediments. Most of the material feldspathic sandstones derived from primary crystalline granitic rocks, such as granite or metasomatic rocks containing abundant potassium feldspar. Mineral contained in sandstones is mostly a form of plagioclase feldspar derived from quartz diorite or volcanic rock. Feldspar contained on this sandstone comes from arid to cool climates when the chemical weathering process is reduced.sandstone, natural stone, feldspathic sandstone, burke museum, geology, geological, geological specimen -
The Beechworth Burke Museum
Geological specimen - Ilvaite
... is part of a larger collection of geological and mineral specimens ...Ilvaite has acquired its name from Ilva (Latin for Elba) Island, Greece, where Ilvaite is most commonly found. The geological setting in which Ilvaite occurs is through contact with magnetite, zinc and copper ore deposits, along with contact metamorphic deposits and zeolite zones. llvaite crystallizes in the form of black prismatic crystals and columns . This specimen was retrieved from Broken hill, known as the world's richest and largest zinc-lead ore deposit. Because of Ilvaite's often unaesthetic crystal formations compared to other minerals, Ilvaite is uncommon in most rock collections, particularly specimens that are not well formed, such as this one. Ilvaite is also a member of the Sorosilicate subclass of the silicate minerals, which have an unusual basic unit of Si2O7, making Ilvaite a unique mineral. Given that Ilvaite is not commonly found in Australia, it marks a unique contribution to an Australian collection of minerals. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A solid hand-sized ferrous iron analogue mineral with of black with shades of beige Ilvaite is a brittle, opaque rock formation that has acquired its name from Ilva (Latin for Elba) Island, Greece, where Ilvaite is most commonly found. The geological setting in which Ilvaite occurs is through contact with magnetite, zinc and copper ore deposits, along with contact metamorphic deposits and zeolite zones. llvaite crystallizes in the form of black prismatic crystals and columns rock, mineral, ilvaite, ilvaite specimen -
The Beechworth Burke Museum
Geological specimen - Copper Ore
... collected in Victoria as part of the Geological Survey of Victoria ...This specimen was recovered from Silverton Mine in Broken Hill, New South Wales. Otherwise known as the 'Day Dream Mine', the Silverton Mine was first established in 1883, when silver and lead deposits where discovered. Within a few short years, the population of Broken Hill reached 3000 people. As of today the Silverton Mine is still open, and has produced over 200 million tonnes of ore, which has generated over $100 billion. The Silverton Mine was also famous for a number of specimens such as silver, iron and zinc.Copper is considered to be a rare ore in that finding it in its pure form is rare. Nowadays when mining for Copper it is often found in mixed in with other minerals or it is recycled from use. Moreover, Copper is found in a range of everyday uses such as coins, cookware, pipes, heating conductors and anything that generate electricity. The fact that Copper is heat a heat conductor, electricity conductor and it does not corrode easily, makes this ore a versatile and useful. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A solid hand-sized cube-shaped sulfide and oxide with shades of green, grey and brown throughout. Copper is typically found as nuggets in the ground. It can be found in a range of forms such as its native state; mixed with other ores, such as zinc and iron; as porphyry copper deposits; and as major deposits. Porphyry deposits are when the mineral is scattered evenly throughout the rock. Major deposits are when the mineral is scattered amongst other minerals.burke museum, beechworth, indigo shire, beechworth musum, geological, geological specimen, mineraology, copper, copper ore, copper ore speciment, broken hill, new south wales -
The Beechworth Burke Museum
Geological specimen - Brown coal
... collected in Victoria as part of the Geological Survey of Victoria ...This particular specimen was recovered from the Lal Lal Coal and Iron Mine in Victoria, 19km from Ballarat. Brown Coal was discovered here in 1857, just alongside the Geelong to Ballarat Railway line. This discovery of lignite (brown coal) was the first in Victoria, which would bring important benefits to the region and state, both of which had previously been reliant on coal imports. In the 1860s, iron ore was found just 5km from Lal Lal, and the area was converted into an Iron Ore Mine. The Lal Lal Iron Mining Company took over operations in 1874, who then peaked iron production in 1884. This mine continued operations until June 1884, when the blast furnace was extinguished and never recommenced. The blast furnace at Lal Lal is considered one of the most important and highly significant sites ion early industrial history in Australia, as it is the only remaining best furnace from the nineteenth century in the Southern Hemisphere. The furnace ruins are 17 metres high, and are clearly visible today on Iron Mine Road, Lal Lal, near the Bungal Dam. This specimen of Lignite (brown coal) is significant, as it was mined from the area where brown coal was first discovered in Victoria, leading to an important and controversial future of the mining and use of brown coal in this State. The Victorian Heritage Database has listed the Lal Lal Coal Mine with local significance, with their Statement of Significance stating: "The Lal Lal coal mine is historically significant as the site of the first discovery of lignite (brown coal) in Victoria, and one that promised important benefits to regional and state industries that were reliant on coal imports at the time. The significance of the stie is reduced by the poor state of preservation of the coal mining and processing fabric". This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A hand-sized light-weight, soft and combustable sedimentary rock specimen, that is dark brown in colour. The specimen has jagged edges, as though parts of the rock have crumbled away. Brown coal, or Lignite, is formed naturally from compressed peat, and is typically found in natural basins. The stages to the formation of coal ('coalification') begin with plant material and wood, which will decay if it is not subjected to deep burial or heating, and turn into Peat. Peat, when sufficiently compressed naturally, will turn into Brown Coal (Lignite), and finally into Black Coal (sub-bituminous, bituminous and anthracite). Each successive stage has a higher energy content and lower water content. It is brownish-black in colour. Brown Coal has a high moisture content, between 50 and 75 percent, and a low carbon content. Some Brown Coals may be stratified, with layers of plant matter, which means little coalification has occurred beyond the peat natural processing stage. When Brown Coal is submerged in dilute nitric acid or boiling potassium hydroxide solution, it reacts to produce a reddish solution, of which higher-ranked coals do not. When brown coal is pulverised and burned in boilers, the steam is used to drive turbines, which generates electricity. It is the lowest rank of coal, as when burned, it creates a relatively low heat content, which in turn does not create a great output of steam. burke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, mineralogy, brown coal, brown coal specimen, lignite, lal lal, lal lal coal mine, lal lal iron mine, ballarat, blast furnace -
The Beechworth Burke Museum
Geological specimen - Granite
... -country Granite Geological specimen A solid palm-sized mineral ...Gabo Island sits off the coast of East Gippsland in Victoria, with cliffs of granite in a relatively unique red/pink colour. Early attempts to build a lighthouse on the island were abandoned due to poor foundations, but when a ship ran aground on the nearby Tullaberga Island in 1853 and led to the death of 37 people, efforts were reignited. Construction of a new lighthouse was completed by 1858, using Gabo Island granite. The lighthouse is Australia's second tallest in Australia and continues to play an important role in guiding boats around the coast as they journey between Melbourne and Sydney. The distinct pink colour from the granite means the lighthouse continues to be a defining feature of the island. Gabo Island granite was also used to construct the Treasury Building at 117 Macquarie Street in Sydney, now the Intercontinental Hotel.Granite in the pink colour of this specimen is relatively rare. The connection to the lighthouse on Gabo Island also gives the specimen historic significance and social significance regarding the maritime history of Victoria. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A solid palm-sized mineral, coloured by flecks of pink, red, and grey. Granite is formed by the slow crystallisation of magma below the earth's surface. It is typically composed of a mix of quartz, feldspar, and other minerals, though syenitic granite like this sample has a smaller amount of quartz than typical granite. This different mineral composition leads to the more distinct pink and red colouring.First sticker: [torn]logical survey / R........ S........ / Loc Gabo Island / 1/4 Sheet / Second Sticker: 15 Third Sticker: Syenitic Graniteburke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, mineralogy, gabo island, gabo island lighthouse, lighthouse, granite, coast, coastal, granite specimen, victoria, coastal cliffs -
The Beechworth Burke Museum
Geological specimen - Precious Opal
... of a larger collection of geological and mineral specimens collected ...In Australia, precious opal is found in Cretaceous age sandstones and mudstones. These sedimentary rocks were deeply weathered and this weathering released silica into the groundwater.Australia is the only part of the world where opalised animal and plant fossils have been found. Opal artefacts several thousands of years old have been discovered in East Africa. As early as 250 BC the Romans prized opals, thought to have come from mines in Eastern Europe, the ancient world's main source of opals. There are many aboriginal dreamtime stories that feature opal. Australian opals discovered during the late 1800's found little favour with European markets but their commercial value increased in the 1900's and in 1932 Australia took over as the major producer of opals in the world and remains the largest producer to this day. Opal is found around the world (Brazil, Mexico, Honduras and the western US) however Australia produces 95% of the world's precious opal and it is our official national gemstone. Opal was first mined commercially at Listowel Downs in Queensland in 1875 and later at White Cliffs in NSW. Today, Coober Pedy (SA) is the main producer of white opal, though in recent years this field has expanded and all types of opals are found. Other centres in SA include Andamooka and Mintabe. Lightning Ridge (NSW) is renowned for black opal and formerly White Cliffs was a large producer of high quality opal. Boulder opals (opals in concretionary ironstone) are mined in Queensland from numerous localities in a zone extending from the Eulo and Cunnamulla district in the south and northwest for a distance of over 700 km to Kynuna in the north. The towns of Quilpie, Yowah and Winton are the main opal mining and wholesale centres. Opals are considered gemstones and have been used in jewellery for thousands of years.Throughout much of history, opals were actually believed to be good luck. The Romans thought that opals were one of the luckiest gemstones and a symbol of hope. In the Middle Ages, opals were believed to be bestowed with all the positive properties of coloured gemstones due to its rainbow-like play of colour. Finally, there is a superstition that you should not wear an opal unless it is your birthstone otherwise misfortune will befall you. This, of course, is far-fetched, but the notion could have been promoted in the late 19th and early 20th Centuries by diamond traders who were trying to increase sales of diamonds and deter people from buying opals. Possibly related to this is the thought that you should set opal jewellery with diamonds as their powers of good fortune will override any negativity held by the opal. The great majority of opal does not show play of colour and is called common opal or potch however this is not the case with a precious opal. Opal is a precious gemstone, like rubies, emeralds or diamonds. Opal is rare, and it is expensive to prospect and mine for.Silica is one of the most common minerals on the planet, but precious opal is very rare – far more rare than diamonds. Precious opal is rare because the natural processes that create it rarely occur.Most (at least 95%) of the opal found by miners is common opal without gem colour. In Australia we call it potch. It can be white, grey, black or amber coloured. Even when a miner finds gem-coloured opal, most of it can’t be cut into gemstones because it’s too thin, or sandy. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.It is not known where this opal originated, except that it is probably from Victoria, as it has been recorded from many localities in the State. Common Opal is formed from silica-rich water circulating through rocks near the Earth’s surface. It consists of minute spheres of silica arranged in different ways. In common opal, the spheres are of different sizes and randomly arranged, unlike in precious opal where the spheres are of similar size and uniformly arranged in three dimensions. These differences account for common opal generally being translucent to opaque and without the play of colours, or opalescence, displayed by precious opal. Common opal is found in many localities and different geological environments throughout Australia and the world. Precious opal requires special conditions to form and is much less common. Australia produces most to the world’s precious opal. burke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, precious opal, opal, brazil, mexico, honduras, queensland, coober pedy, gemstones, jewellery, play-of-colour, light blue -
The Beechworth Burke Museum
Geological specimen - Gold-Sulphide Ore
... as part of the Geological Survey of Victoria that begun in 1852 ...This particular specimen was recovered from two hundred feet down in the Golden Mile in Kalgoorlie, Western Australia. The Golden Mile, named after the estimated sixty million ounces of gold worth around one hundred billion dollars, was the birthplace of the largest gold rush in Australia almost one hundred and thirty years ago when William Brookman and Samuel Pearce leased the Great Boulder mine. The Golden Mile is also the home of the Super Pit, Australia's most well-known mine.The majority of gold deposits will form as a native metal, however, on occasion, it can form a compound with another element, in this case, sulphur. Therefore, this specimen is a rare example of gold naturally forming into a compound mineral with sulphur. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A small gold-sulphide ore mineral specimen in shades of silver and grey with flecks of gold. Precious metals are often found in Sulphide Ores, as sulphides usually bind to these metals. They are also extremely symmetrical in crystaline form. Gold-Sulphide Ore occurs when gold forms a natural compound with other elements. In this form, gold can be present in one of two ways. It can be fully immersed in the sulphide, or a portion may be partially free. This specimen has minimal gold visible, with only a few flecks being partially visible.burke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, mineralogy, gold-sulphide ore -
The Beechworth Burke Museum
Geological specimen - Chalcedony
... as part of the Geological Survey of Victoria that begun in 1852 ...This specimen was recovered from Philip Island in Victoria. Chalcedony is composed of Quartz and Silicon Dioxide represented as SIO2. It has and is still used as a gemstone for thousands of years. This is an excellent specimen Chalcedony that shows its aesthetic properties. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study. Uniquely shaped piece of Chalcedony with opening in the centerburke museum, beechworth, geological, geological specimen -
The Beechworth Burke Museum
Geological specimen - Gold Telluride Ore
... is part of a larger collection of geological and mineral specimens ...Gold usually is found as a native metal, but it also forms minerals with tellurium, sulphur, or selenium. The gold-bearing minerals that contain tellurium are called tellurides. Kalgoorlie, Western Australia contains greater than 1500 tonnes of gold.Seventy to seventy-five percent of the deposit occurs as native gold, but a further twenty percent appears as tellurides. What remains is in the form of 'invisible' gold. Extracting gold from telluride minerals, such as calaverite, which contains around forty-two percent gold, has produced approximately three hundred tonnes of gold. Prior to 1896, rocks containing tellurides were not recognised as rich gold ores, and were discarded.This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A hand-sized silvery to pyrite-yellow striated mineral containing tellurium and goldburke museum, beechworth, beechworth museum, geological, geological specimen, mineralogy, telluride, tellurite, gold-bearing, kalgoorlie, tellurium -
The Beechworth Burke Museum
Geological specimen - Rhodonite with Galena and Sphalerite
... collected in Victoria as part of the Geological Survey of Victoria ...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 -
The Beechworth Burke Museum
Geological specimen - Mangan Hedenbergite
... of a larger collection of geological and mineral specimens collected ...This specimen was recovered from Broken Hill, NSW. It was given the name Mangan Hedenbergite in 1819 by Jöns Jakob Berzelius in honor of Mr. Anders Ludvig of Hedenberg who was the first to define hedenbergite as a mineral. Hedenbergite, belongs in the pyroxene group having a monoclinic crystal system. The mineral is extremely rarely found as a pure substance. Mangan Hedenbergite is a manganese bearing variety of Hedenbergite. Manganese is the world’s fourth most used mineral after iron, aluminium, and copper primarily because it has no satisfactory substitute in its major applications. Globally, the steel industry is the primary user of manganese metal, utilizing it as an alloy to enhance the strength and workability of steel and in the manufacture of tin cans. Manganese is a key component of certain widely used aluminium alloys and, in oxide form, dry cell batteries used in electric vehicles. These batteries are in high demand. Another potential use for manganese may as an additive to help coat and protect a car’s engine. Manganese is also used for non-metallurgical purposes such as plant fertilizers, animal feed, and colorants for bricks. 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 mineral specimen in shades of silver and blackmanganese, open cut mine, manganese ore processing, bell bay, tasmania, northern territory, steel industry, zinc-carbon batteries, alkaline batteries, tin cans -
The Beechworth Burke Museum
Geological specimen - Fossiliferous Mudstone, Unknown
... collected in Victoria as part of the Geological Survey of Victoria ...This specimen was found in Cape Patterson, Vic. Cape Paterson is a cape and seaside village located near the town of Wonthaggi, 132 kilometres southeast of Melbourne, in the Bass Coast Shire of Gippsland, Victoria, Australia. These dark, fossiliferous Mudstones were deposited in slow-moving water associated with sedimentary basins & continental shelves. They are rich in carbon which makes them almost black. This is typical of an anoxic, reducing environment such as deep water or stagnant conditions where carbon-rich material would remain unoxidised during subsequent deposition & diagenesis. it has an imprint of a leaf in the rock itself, displaying the fossil of the plant. This specimen is unique due to the leaf impression within the stone itself. Imprint fossils are formed from an organism moving in some way, leaving behind a trace or track. These tracks are preserved when the clay/silt dries slowly and is covered by other sediment. Plants can also leave imprint fossils when they are covered by sediment. The leaf tissue degrades, leaving an imprint of where the leaf once was. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.These dark, fossiliferous Mudstones were deposited in slow moving water associated with sedimentary basins & continental shelves. They are rich in carbon which makes them almost black. This is typical of an anoxic, reducing environment such as deep water or stagnant conditions where carbon rich material would remain unoxidised during subsequent deposition & diagenesis. FOSSILIFEROUS MUDSTONE / Locality: Cape Patterson, Victoria | Descriptive catalogue / Pg 27 No 95 / "Grey Clay, / Cape Paterson with leaf impressions' / 15/4/21 C. William /mudstone, cape patterson, leaf imprint, fossilised leaf, fossiliferous mudstone -
The Beechworth Burke Museum
Geological specimen - Spotted Slate, Unknown
... as part of the Geological Survey of Victoria that begun in 1852 ...This specimen was recovered from Sedgwick, VIC. Spotted slate is a fine-grained porphyroblastic metamorphic rock with a number of compounds including muscovite, quartz, graphite with cordierite poikiloblasts and more. The cordierite poikiloblasts are rounded crystals that size up to 2.5 mm. the growth of these crystals is in response to metamorphism of low to medium intensity. The town Sedgwick was named after British geologist Adam Sedgwick 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 rectangular hand-sized spotted slate specimen in a shade of light grey with darker flecks throughout Spotted Slate / Locality: Sedgwick Victoria | This is an early specimen / from the Quarter sheet / map. See sample 62 / page 18. Described as 'Spotted Slate' but these / days we would call it spotted hornfels / C. William 15/4/21 slate, spotted slate, victoria, beechworth, burke museum, geological specimen, mineralogy, sedgwick, sedgwick victoria, spotted slate specimen -
The Beechworth Burke Museum
Geological specimen - Chalcopyrite, Unknown
... of a larger collection of geological and mineral specimens collected ...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 - Slate with Iron pyrites
... collected in Victoria as part of the Geological Survey of Victoria ...This specimen was recovered from Moonambel, Donkey Hill, Victoria. Established in the early 1860's, Moonambel is a small town in the Pyrenees region of the Australian state of Victoria. In the 1850s the location of Moonambel was part of the ‘Mountain Creek’ pastoral run, but in 1860 reports began to appear of a gold-rush at McKinnon’s ‘Mountain Creek’ station. By 1861, a township had developed on the diggings site, and on 21 October 1861 the “municipal district of Moonambel, on Mountain Creek” was proclaimed. The name 'Moonambel' is believed to be an aboriginal word meaning 'hollow in the hills'. Slate is a stone with a fine grain that is noted for its persistent strength and ability to naturally split into slabs. It forms under low temperatures and is most often created from clay. Pyrite is a crystallising compound that occurs naturally in grey and blue-black slate that is colloquially referred to as slate-rust as it resembles regular rust. 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.Pyrite is iron sulphide (also known as “fool's gold”) which is commonly found in slates.Existing label: 53 /moonambel, slate, pyrite, burke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, mineralogy, victoria -
The Beechworth Burke Museum
Geological specimen - Pyrite
... were collected in Victoria as part of the Geological Survey ...This specimen was recovered from Adelong, NSW. The initial discovery of gold at Adelong by a Mr Williams took place in 1857. Much of the area is underlain by granitic rocks, while at Adelong itself a prominent norite intrusive body occurs. To the west of Adelong is a belt of intermediate to mafic igneous rocks and sediments which extends from Batlow in the south to at least as far north as the Snowy Mountains Highway. Around 26 tonnes of gold was found at the Adelong goldfield from its discovery in the 1850s until the last miners left in the 1940s. Pyrite has the formula of FeS2 and forms as an isometric (cube) form. It is a common occurring material and is often mistaken for gold, now colloquially known as ‘fool’s gold’. Pyrite that has strongly crystallised is considered stable, but the mineral has the potential to oxidise and decay. 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.Pyrite is iron sulphide (also known as “fool's gold”) which is commonly found in slates.Existing Label: 104 /burke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, mineralogy, pyrite, adelong -
The Beechworth Burke Museum
Geological specimen - Ropy Lava
... collected in Victoria as part of the Geological Survey of Victoria ...‘Ropy lava’ is known for its sculptural and layered qualities. It occurs in specific lava flows that are slow moving and slow cooling, allowing for unique formations to be created out of the motion. Ropy Lava is a flow that has a hardened crust with molten material underneath, the tension between these states is what creates its characteristic form. The brown/red hue of the stone is an indication of age, as it is oxidised iron deposits. This rock deposit is thought to be sourced from the area by Talbot, in western Victoria. This area has a rich mineral history and experienced the gold rush in the 1850's. The traditional owners of this area are the Dja Dja Wurrung people.This geological specimen shows the conditions in which the Australian landscape was created as well as provides an indication as to how these events occurred. It is representative of a common natural process that contextualises the formation of Australia with the formation of other landmasses. 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.Hand sized specimen in brown/red hues42 / victoria, talbot, lava, ropy, ropy lava, mineral, geological specimen, geological, geological heritage, natural stone, natural history -
Koorie Heritage Trust
Journal - Serials, Birdsell, Joseph B. et al, Records of the Queen Victoria Museum Launceston. Contents - The racial origins of the Extinct Tasmanians. A survey of possible sea routes available to the Tasmanian Aborigines. The Tasmanians - a summary, 1949
Some of the points raised seem rather dated, but an interesting set of theories historically.105-145P.; plates; refs. figs.Some of the points raised seem rather dated, but an interesting set of theories historically.tasmanians - racial origins., australian aboriginals - origins., migration theories - tasmanians., bass strait - geology. -
Flagstaff Hill Maritime Museum and Village
Freezer, circa 1930's
This ice cream freezer, manufactured in South Australia in the 1930's, was advertised to "keep the contents of the cream compartment frozen for many hours". It was promoted for use at picnics to keep salads cool. Its design is very similar to other freezers of The Frigid name which were made in 1939; those freezers were all one colour whereas this one is blue around the top and bottom of the barrel and cream in the centre with blue/green lettering. The process of making ice cream was to pack the outer chamber full with a combination of 3 parts ice cubes of about 1 inch (2.cm) to one part coarse salt, then pour into the chamber about 1 cup of cold water. After this, the ingredients for ice cream or sorbet were poured into the inner chamber, then attach the lid and turn The Frigid freezer upside down for about 40 minutes or until the right consistency is reached. Advice as given to open the freezer every 20 minutes and stir around the contents that were frozen against the sides of the inner chamber. The ingredients for the ice cream could include cream, sugar, vanilla and eggs. The label on the box of The Frigid shows the address of A Simpson and Son to be at Pirie Street, Adelaide. This address was used as early as 1876 and later catalogues, 1931 - 1960 still show this address. Alfred Simpson and his family emigrated from England, arriving in South Australia in 1849. He had already completed his apprenticeship as a tinplate worker but he tried various other occupations, including trying out the gold mines in Victoria, before he established himself as a tinsmith in 1853. His products included many agricultural items. His son, Alfred Muller Simpson, joined the business when he turned 21. In the 1860 Simpson's products included 'explosion proof' safes. In the late 1880's A Simpson and Son manufactured munitions and mines for the war. At the time of Alfred's death in 1891, A Simpson and Son had the largest metal manufacturing plant in Australia. From 1898 the company's reputation grew from the process of enamel plating with porcelain. During the First World War, Simpsons returned to the manufacture of munitions. Alfred M. Simpson's sons (Alfred Allen, known as Allen, and Fredrick Neighbour) joined the company when they finished their schooling. Allen was also associated with the Royal Geological Society over many years and when the CT Madigan surveyed Central Australia in 1929, the Simpson Desert was named in his honour. Cape Simpson in Antarctica is also named after him due to his assistance to Douglas Mawson. A new factory was opened at Dudley Park in the 1940s and the company began the manufacture of whitegoods. In 1963 A. Simpson and Son merged with Pope Industries to form Simpson Pope Holdings. Alfred Simpson became chairman of the board of Simpson Pope Holdings. The Simpson brand, now owned by Electrolux, continues to produce a variety of household appliances. (Reference: State Library of South Australia) A Simpson and Son was an early colonial business that has lasted well into the 20th century and the name Simpson is still associated with whitegoods. Freezer, 2 quart (1.8 litre) capacity, made by A Simpson and Son Ltd, marked "The Frigid". Cylinder shaped, constructed from enamelled sheet metal, has two catches one on the base and one on top. Inner cylinder for holding contents for freezing. Slightly rusted. Freezer is inside original cardboard box with yellow label showing manufacturer details. Circa 1930'sOutside of freezer is printed in blue"The Frigid". Box includes "THE "FRIGID" FREEZER" and branded "S & S" inside a circle.flagstaff hill, warrnambool, shipwrecked-coast, flagstaff-hill, flagstaff-hill-maritime-museum, maritime-museum, shipwreck-coast, flagstaff-hill-maritime-village, a. simpson & son limited, manufacturer, foundry, freezer, 2 quart freezer, portable freezer, kitchen appliance, the frigid, ice cream freezer, ice cream maker 1930's -
Federation University Historical Collection
Booklet, The School of Mines, Ballaarat, Annual Report 1881, 1882
The School of Mines Ballaarat Annual Report 1881. Annual Report, Additional Examination Statute, Certificates Granted by the Council, Copy of letter received from the Honble. Francis Ormond, M.L.C., Extracts from the Visitors' Book, Fees, Form of Bequest, Life Governors, Museum - open to Visitors', Office Bearers, Paper of Particulars, Report of the Curator of the Museum and Library (with plans), Report of the Superintendent of Laboratories, Report of the Lecturer in Telegraphy, Report of the Lecturer in Mechanical Engineering, Statement of Receipts and Expenditure for the year 1881, Subjects and Lecturers, Subjects and Examiners, Subscriptions and Donations from 1st January to 31st December 1881, The Lignite Deposit at Skipton (with Section and Plan)Soft covered pale green booklet of 63 pages.annual report, additional examination statute, certificates granted by the council, copy of letter received from the honble. francis ormond, m.l.c., extracts from visitors' book, fees, form of bequest, paper of particulars, life governors, museum, officer bearers, report of the curator of the museum and library, report of the lecturer in telegraphy, report of the lecturer in mechanical engineering, statement of receipts and expenditure for the year 1881, subjects and lecturers, subjects and examiners, subscriptions and donations from 1st january to 31st december 1881, the lignite deposit at skipton, james oddie, esq., j.p., alf. mica smith, lecturer in chemistry, natural philosophy and botany, f. m. krause, lecturer in geology, scientific mining, land, mining and engineering surveying, t. h. thompson, lecturer in practical mining, w. h. shaw, lecturer in mechanical engineering, h. reid, lecturer in mechanical engineering, a. a. buley, lecturer in mathematics, w. d. campbell, lecturer in telegraphy, j. f. usher, lecturer in materia medica, pharmacy and physiology, a.a. buley, w.d. campbell, j.f. usher, w.h. shaw, ferdinand krause, t.h. krause, skipton lignite deposit, skipton coal, ballarat school of mines annual report -
Federation University Historical Collection
Booklet, A. A. Herberte, "STAR' Printing Works, The School of Mines, Ballaarat, Annual Report 1884, 1885
The School of Mines Ballaarat Annual Report 1884. Annual Report, Balance Sheet, Certificates Granted by the Council, Examination Papers - Elementary Science Classes (Appendix), Fees, Honorary Correspondents, Life Governors, Museum - open to Visitors', Office Bearers, Report of the Curator of the Museum and Library, Report of the Lecturer in Mathematics, Report of the Lecturer in Mechanical Engineering, Report of the Lecturer in Electricity and Magnetism, Report of the Lecturer in Telegraphy, Report of the Lecturer in Botany, Report of the Lecturer in Materia Medica and Physiology, Report of the Lecturer in Astronomy, Scale of Charges for Assays and Analyses, Examinations Held, Statement of Receipts and Expenditure for the year 1884, Statement of Receipts and Expenditure for Special Funds, Subjects and Lecturers, Subjects and Examiners, Subscriptions and Donations from 1st January to 31st December 1884, Time TableSoft covered pale green booklet of 67 pages. The Ballarat School of Mines Annual Report for 1984.annual report, balance sheet, certificates granted by the council, examination papers - elementary science, fees, honorary correspondents, life governors, museum, officer bearers, report of the curator of the museum and library, report of the lecturer in telegraphy, report of the lecturer in mechanical engineering, report of the lecturer in astronomy, scale of charges for assays and analyses, examinations held, statement of receipts and expenditure for the year 1884, statement of receipts and expenditure for special funds, subjects and lecturers, subjects and examiners, subscriptions and donations from 1st january to 31st december 1884, time table, james oddie, esq., j.p., alf. mica smith, lecturer in chemistry, natural philosophy and botany, f. m. krause, lecturer in geology, scientific mining, land, mining and engineering surveying, t. h. thompson, lecturer in practical mining, j. sommers, lecturer in mechanical engineering, h. sutton, lecturer in mechanical applied electricity and magnetism, a. a. buley, lecturer in mathematics, w. d. campbell, lecturer in telegraphy, j. f. usher, lecturer in materia medica, pharmacy and physiology, geo. day, lecturer in botany, john wall, lecturer in astronomy, subscriptions, fonations, telegraphy, henry sutton, usher, george day -
Federation University Historical Collection
Booklet, W. B. Macdonald, The Ballarat School of Mines, Industries and Science, Annual Report 1890, 1890
The Ballarat School of Mines Annual Report 1890. Annual Report, Crown Grant, Affiliation Statute, Constitution, Examination Statutes, Associateship of The School, Department of Agriculture, Certificates Granted by Council, Fees, Form of Bequest, Gauge-Testing Apparatus, General Balance Sheet and Liabilities and Assets, Honorary Correspondents, Life Governors, Meteorological Observations, Number of Students attended The School of Mines, Office Bearers, Report of the Professor of Mineralogy and Geology and Curator of the Museum, Report of the Superintendent of Laboratories, Report of the Lecturer on Engineering and Surveying, Report of the Lecturer on Geometrical and Freehand Drawing, Report of the Lecturer on Telegraphy, Report of the Lecturer on Botany, Report of the Lecturer on Materia Medica and Physiology, Report of University Classes, Examinations Held, Scale of Charges for Assays and Analyses, Statement of Receipts and Expenditure for the year 1890 and Special Trust Funds, Statistics - Students attending Lectures, Subjects and Examiners, Subscriptions and Donations from 1st January to 31st December 1890, Time TableThe Ballarat School of Mines annual Report, 1890. Cover is browning around the edges, back cover partly detached and is torn, 184 pages. ballarat school of mines, annual report, andrew anderson j.p. - president (acting) and vice president, rivett henry bland - trustee, the hon. sir w. j. clarke - trustee, the hon. john warrington rogers - trustee, james oddie - trustee, the hon. henry cuthbert - honorary solicitor, i. j. jones - honorary treasurer, chas. kent - auditor, andrew berry - registrar, f. m. krause - professor of mineralogy and geology, and curator of the museum, alf. mica. smith - superintendent of laboratories, mr e. wattis - manager, mining laboratory, j. h. horwood - lecturer on engineering and surveyin, h. j. hall - lecturer geometrical and free-hand drawing, george day - botany, j. f. usher - materia medica and physiology, miss bella guerin - university classes, charles kent - auditor, henry krone - assistant registrar of titles, henry b. loch, d. e. martin - secretary for agriculture, r. hedger wallace - department of agriculture -
Federation University Historical Collection
Booklet, Berry Anderson & Co, The Ballarat School of Mines, Calendar and Annual Report 1894, 1894
The Ballarat School of Mines Calendar and Annual Report 1894. Associateship of The School, Calendar for 1894, Certificates Granted by the Council 1893, Comparative Statement of Receipts and Expenditure, Departmental Expenditure, Examiners, Examination Papers, Examination Fees, Fees, Honorary Correspondents, Life Governors, Meteorological Observations, Mining Engineering Scholarship, Number of Certificates Granted since Inception, Number of Students attended The School of Mines, Office Bearers, Plant and Appliances, Practical Treatment of Ores, Professors and Lecturers, Report of the Professor of Mineralogy and Geology and Curator of the Museum, Report of the Superintendent of Laboratories, Report of the Lecturer on Engineering and Surveying, Report of the Lecturer on Mathematics, Report of the Instructor in Mechanical Drawing and Machine Construction and Design, Report of the Lecturer on Electrical Engineering and Telegraphy, Report of the Lecturer on Geometrical Model and Perspective Drawing, Report of the Lecturer on Botany, Report of the Lecturer on Biology, Pharmacy, Materia Medica, Scale of Charges for Assays and Analyses, State School Science Classes, Statement of Receipts and Expenditure for year 1893 and Serjeant Scholarship Fund, Statistics - Student attending Lectures, Subscriptions and Donations, Syllabus of Lecture Courses, Time TableThe Ballarat School of Mines Calendar and Annual Report, 1894. Green soft cover, 116 pages. ballarat school of mines, annual report, andrew anderson j.p. - president, f. j. martell - vice president, r. denham pinnock - vice president, rivett henry bland - trustee, the hon. sir w. j. clarke - trustee, the hon. john warrington rogers - trustee, james oddie - trustee, the hon. henry cuthbert - honorary solicitor, r. g. middleton - honorary treasurer, charles kent - auditor, andrew berry - registrar, professor alf. mica smith - chemistry, metallurgy, natural philosophy, professor krause - geology, mineralogy, principles of mining, professor j. h. horwood - mine and land surveying, mining mechanics, hydraulics, civil engineering, applied mechanics, j. a. dawson - electrical engineering, d. walker - chemistry and natural philosophy, w. e. bennetts - mathematics, henry j. hall - freehand and perspective drawing, a. e. c. kerr - mechanical drawing, george p. day - botany, e. gutheil - paleontology, zoology, materia medica, w. d. snowball - veterinary science -
Federation University Historical Collection
Booklet, Berry Anderson & Co, The Ballarat School of Mines, Calendar and Annual Report 1895, 1895
The Ballarat School of Mines Calendar and Annual Report 1895. Associateship of The School, Calendar for 1895, Certificates Granted by the Council 1894, Certificates Granted by the Education Department 1893, Comparative Statement of Receipts and Expenditure, Departmental Expenditure, Examiners, Examination Papers, Examination Fees, Fees, Honorary Correspondents, Life Governors, Meteorological Observations, Number of Students attended The School of Mines, Obituary, Office Bearers, Practical Treatment of Ores, Professors and Lecturers, Report of the Professor of Mineralogy and Geology and Curator of the Museum, Report of the Superintendent of Laboratories, Report of the Lecturer on Engineering and Surveying, Report of the Lecturer on Mathematics, Report of the Instructor in Engineering and Machine Construction and Design, Report of the Lecturer on Electrical Engineering, Report of the Lecturer on Geometrical Model and Perspective Drawing, Report of the Lecturer on Botany, Report of the Lecturer on Palaeontology, Materia Medica and Mining Ambulance, Scale of Charges for Assays and Analyses, Statement of Receipts and Expenditure for year 1894, Statistics - Student attending Lectures, Subscriptions and Donations, Syllabus of Lecture Courses, Time TableThe Ballarat School of Mines Calendar and Annual Report, 1895. Pale brown soft cover, 90 pages. ballarat school of mines, annual report, andrew anderson j.p. - president, f. j. martell - vice president, r. denham pinnock - vice president, the hon. sir w. j. clarke - trustee, the hon. john warrington rogers - trustee, the right reverend samuel thornton - trustee, andrew anderson - trustee, james millhinch - trustee, james oddie - trustee, the hon. henry cuthbert - honorary solicitor, r. g. middleton - honorary treasurer, charles kent - auditor, andrew berry - registrar, professor alf. mica smith - chemistry, metallurgy, natural philosophy, professor krause - geology, mineralogy, principles of mining, professor g. j. dawbarn - mine and land surveying, mining mechanics, hydraulics, civil engineering, applied mechanics, j. rowe - practical mining, j. a. dawson - electrical engineering, d. walker - chemistry and natural philosophy, w. e. bennett - mathematics, henry j. hall - freehand and perspective drawing, a. e. c. kerr - mechanical drawing (machine construction and design), george p. day - botany, e. gutheil - paleontology, zoology, materia medica, rivett henry bland - obituary, george gant scott - obituary, fiddian, bennett, r. allan, dawbarn, rosales, krause, joseph bryant, matthews, j. robinson, andrew robertson, john lynch, jonathan robinson, a.e.c. kerr, alfred mica smith, frederick mccoy, j. cosmo newberry, blackett, elelry, arnot, robert allan, bickett, kent, martin, mitchell, ferdinand von mueller, rivett henry bland, thomas bath, john rowe, museum, andrew anderson, george day, subscriptions and donations, examination papers -
Federation University Historical Collection
Book, New York Post, The School of Mine Quarterly: A Journal of Applied Science, 1889-1809
The School of Mines Quarterly was a jpournal of Applied Science from Columbia College, New York City.The Index to the School of Mines Quarterlu Volumes X1-XX (1900) and 32 green covered journals school of mines, new york, columbia college, schools of mines, columbia school of mines, witwatersrand goldfield, inter-continental railway, mine ropes, harbor improvememnts on the pacific coast, glycerine and artificial butter industry, transit factors for teh columbia college observatory, tables for the reducation of transit observations, ancienct methods for dividing and recoording time in japan, assay of tin, john strong newberry, standards of linnear measure, comparison of costs of electric lighting, huanchaca mine bolivia, el callao gold mine venezuela, john magnus adams, ores in saxony, hartz and rhenish prussia, hofmann apparatus, adjustment of trangulation, determination of carbonic acid in white lead, lower coals in western clearfield county pennsylvania, old telegraph mine ningham canon utah, mechanical preparation of ores, modern waterworks construction, curdling of milk, french regenerative gas furnace, irrication canals, peruvian salt mine, collection of metallurgic dust and fume, permeability of iron and steel, assay of silver, explosion in a zinc fume condenser, teaching archtectural history, liquid air, between the mine and the smelter, ballistic galvonometer, assay of telluride ores, analytical chemistry, theory and design of the masonry arch, silver pick mine wilson colorado, telegraphy and telephoney, mineralogy, morse code, michigan mining practices, titaniferous magnetites, paradox of the pantheon, rocks from wyoming, witwatersrand goldfields, gaseous sun, alternating current distribution, engineering tests on direct current electrical machinery, thomas egleston, ore dressing, frederick morgan watson, camp bird gold mine and mills, magnetic properties of iron and steel, morphology of organic compounds, antimony, structure of the starch molecule, cerrillos hills new mexico, geology, rossie lead veins, practical electrochemistry, lines of graphic statics, anistic acid by the ozidation of anniseed oil, bromate method for antimony, john krom rees, trust company of america building, helion lamp, frederick arthur goetze, mine surveying, pine wood oils, malleable cast iron, electrolytic treatment of galena, turpentine and pine oils, bluestone, ashokan dam bluestone, road resistances, oxy-gas blowtorch, mine dumps, segregation of steel ingots, masonry dam formulas, putnam county magnetic belts, gases, continuity of education, hydraulic diagrams, standardistion of potassium permanganate, sewerage discharge into sea water, modern waterworks, true column formula, slags from lead furnaces, missouri river, tempreture of gases, rocks, architectural history, modern dome, oil machine, undulations in railway tracks, irrigation engineering, cleps-tachymeters, electrical engineering, new york shales, fan pump, sucrose, isaac newton, french school of anstronomers, electrolytic polarization, benjamin bowden lawrence, diamond drilling, new york ciy water front, engineering profession ethics