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

Dolomite is a mineral, calcium magnesium carbonate, with the chemical formula CaMg(CO3)2. It is a principle component of various rock types sometimes also referred to as dolomite, including dolostone, dolomitic marble and dolomitic limestone (according to the composition of each type). Dolomite rock is found in sedimentary basins throughout the world, comprising approximately 2% of the Earth's crust. It is formed when lime mud or limestone encounters groundwater containing magnesium. Dolomite can contain elements such as lead, zinc and copper. Dolomite and limestone are used in various construction, landscaping and agricultural processes. This specimen was donated to the Burke Museum in 1868 by Alfred Selwyn as part of 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. Dolomite and limestone are mined at several locations in Victoria, including sites in the North-East of the state in Bindi and Limestone Creek. There are notable dolomite deposits in most Australian states. The dolomitised form of the mineral tends to come from older limestone deposits, formed during the palaeozoic era in marine settings, so this specimen may have come from a deposit located along a coastline in Victoria or another state. The specimen is significant as an example 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. 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 piece of pale pink dolomite (calcium magnesium carbonate) with dark grey rim and hollowed centre. geological specimen, geology, geology collection, burke museum, beechworth, dolomite, mineralogy, geological survey, alfred selwyn, limestone, calcium magnesium carbonate

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

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

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

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

Agate occurs when amygdales (gas pockets) form in the upper levels of basaltic lava flows. If these pockets or bubbles are iniltrated by water bearing silica in solution, the fluid dries and hardens in layers, forming round or egg shaped nodules or geodes within the rocky matrix. Agate is formed of a silica mineral chalcedony similar to quartz. Although relatively common and semi-precious, agate has been prized since at least 1450 BC - an intricately carved agate seal was found in the 2015 excavation of a grave belonging to a Mycenaeum priest or warrior near Pylos in Greece. Agate is also used in jewellery and other decorative or ritual purposes due to its often striking appearance. These specimens originated in North Queensland, which contains noted agate-fossicking regions such as in the area surrounding Forsayth. They were collected in approximately 1852 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 specimens are significant as 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. Two solid egg-sized pieces of peach/orange toned agate (a common semi-precious chalcedony, similar to quartz) with a striped pattern, embedded in a light and dark brown matrix. geological specimen, geology, geology collection, burke museum, beechworth, agate, north queensland agate, 1852 geological survey of victoria, l. hufer - donor, mineralogy, agate specimen, indigo shire

The Ballarat School of Mines Annual Report 1891. Annual Report, Crown Grant, Affiliation Statute, Constitution, Examination Statutes, Associateship of The School, Certificates Granted by the Council, Clunes Branch Report, Departmental Expenditure, 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, Practical Treatment of Ores, 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 Lecturer on Electrical Engineering and Telegraphy, Report of the Lecturer on Botany, Report of the Lecturer on Geometrical and Freehand Drawing, Report of the Lecturer on Materia Medica and Physiology, Report of University Classes, Report on Mining Laboratory, Examinations Held, Scale of Charges for Assays and Analyses, Statement of Receipts and Expenditure for the year 1891 and Special Trust Funds, Statistics - Students attending Lectures, Subjects and Lecturers, Subjects and Examiners, Subscriptions and Donations from 1st January to 31st December 1891, Syllabus of Lecture CoursesThe Ballarat School of Mines Industries and Science Annual Report, 1891. Cover is browning around the edges, front cover has small tear on bottom of cover, 132 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, c. eyres - honorary treasurer, charles kent - auditor, andrew berry - registrar, f. m. krause - professor of mineralogy and geology, and curator of the museum, alf. mica. smith - chemistry, metallurgy, natural philosophy, f. m. krause - geology, mineralogy, geological surveying, j. h. horwood - lecturer on engineering and surveying, h. j. hall - lecturer free-hand and model drawing, george day - botany, j. f. usher - materia medica and physiology, c. w. wilson - university classes, isaac jaques jones j.p., mr e. wattis - manager, mining laboratory, j. a. dawson - electrical engineering and telegraphy, elder gray, harry e. sando, charles matthews - auditor, j. h. daley - auditor, henry crone - assistant registrar of titles, henry b. loch, isaac jacques jones, charles eyres, j.a, j.a. dawson, statistics, university classes, bella guerin, c.w. wilson, clunes branch of the ballarat school of mines, w.e. burbridge, h.j. hall, museum, state school students, daniel walker, a.j. higgins, state school science classes

The Ballarat School of Mines Annual Report 1893. Annual Report, Examination Papers, Associateship of The School of Mines, Syllabus for Technical Schools, Crown Grant, Affiliation Statute, Certificates Granted by the Council, Clunes Branch Report, Departmental Expenditure, Fees, Form of Bequest, General Balance Sheet and Liabilities and Assets, Honorary Correspondents, Life Governors, Meteorological Observations, Number of Students attended The School of Mines, Office Bearers, Practical Treatment of Ores, 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 Lecturer in Mechanical Drawing, Machine Construction and Design, Report of the Lecturer on Electrical Engineering and Telegraphy, Report of the Lecturer on Botany, Report of the Lecturer on Biology, Pharmacy, Materia Medica, Report on Mining Laboratory, Examinations Held, Scale of Charges for Assays and Analyses, Statement of Receipts and Expenditure for the year 1892 and Special Trust Funds, Statistics - Students attending Lectures, Subjects and Lecturers, Subjects and Examiners, Subscriptions and Donations from 1st January to 31st December 1892, Syllabus of Lecture Courses6188: The Ballarat School of Mines Industries and Science Calendar and Annual Report, 1893. Red soft cover is browning around the edges, spine is tattered, 156 pages. 6188.2: Red soft covered booklet of 26 pages, Office Copyballarat 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, alf. mica. smith - chemistry, metallurgy, f. m. krause - geology, mineralogy, mining, j. h. horwood - mechanical engineering, machine drawing and design, theoretica and applied mechanics, mathematics, henry j. hall - freehand and model drawing, j. a. dawson - electricity and magnetism, george day - botany, e. gutheil - biology, materia medica, pharmacy, a. e. c. kerr - mechanical drawing, machine construction and design, e. gutheil - biology, pharmacy, materia medica, henry crone - assistant registrar of titles, henry b. loch, elder gray - president, clunes branch, harry e. sando - registrar, clunes branch, w. y. witherden - hon. treasurer, clunes branch

Actinolite is usually found in metamorphic rocks, such as contact aureoles surrounding cooled intrusive igneous rocks. It also occurs as a product of the metamorphism of magnesium-rich limestones. Pyrite is usually found with other sulfides or oxides in quartz veins, sedimentary rock, and metamorphic rock, as well coal beds, and as a replacement mineral in fossils. Actinolite is an amphibole silicate mineral. It is named after the Greek word "aktinos" meaning “ray” in allusion to the mineral's fibrous nature. Fibrous actinolite is a type of asbestos and was once mined along Jones Creek at Gundagai, New South Wales. Pyrite or "Fool's Gold" is the most common sulfide mineral. It is named after the Greek "pyr" meaning "fire" because it can be used to create sparks needed for a fire if struck against metal or a hard surface. Due to its gold colour, pyrite can be mistaken for gold and often forms alongside it, causing small amounts of gold to be present in rocks containing pyrite. Most importantly, pyrite is an ore of gold. Pyrite is sometimes used as a gemstone but is not great for jewellery as it easily tarnishes. In some fossils of ammonites – shelled cephalopods that died ~66 million years ago – pyrite also replaces the shell. 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-medium-sized solid specimen with the minerals actinolite (dark green fibrous) and pyrite (brassy) with shades of brown, black/grey, and white. Actinolite is an amphibole mineral in the tremolite-actinolite series of calcium, magnesium, and iron silicates. Pyrite is an iron disulfide mineral.geological specimen, geology, geology collection, burke museum, beechworth, indigo shire, geological, mineralogy, pyrite, actinolite, victoria, sewyln, alfred selwyn

The Thames School of Mines is in Thames, New Zealand.Printed sylabus for the Thames School of Mines, New Zealand. It includes a scale of charges.thames school of mines, schools of mines, new zealand, james park, f.b. allen, geology, metallurgy, ventilation, explosives, surveying, mineralogy, assaying, physics, astronomy

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

This particular geological specimen was found in Mount Franklin or Lalgambook in Djadjawurrung, located between Daylesford and Newstead, approximately ninety minutes drive from Melbourne. The mountain is an example of a breached scoria cone (a steep conical hill of loose pyroclastic fragments) which was created by a volcanic eruption about 470,000 years ago, a date which may indicate the age of this geological specimen. The volcanic eruptions of Mount Franklin were most likely witnessed by members of the Dja Dja Wurrung Aboriginal tribe, who referred to this country as the 'smoking grounds'. Mount Franklin and the surrounding area appears to have been a place of considerable religious significance to Aboriginal people, there is evidence which indicates that frequent large ceremonial gatherings took place in the area. Basalt is the most common rock on Earth’s surface, more than 90% of all volcanic rock on Earth is basalt. Basalt is an aphanitic extrusive igneous rock formed from the rapid cooling of low-viscosity lava exposed at or very near the surface of a rocky planet or moon. Specimens are black in colour and weather to dark green or brown. Basalt is rich in iron and magnesium and is mainly composed of olivine, pyroxene, and plagioclase. Olivine is the name of a group of rock-forming silicate minerals with compositions ranging between Mg2SiO4 and Fe2SiO4. Unlike other minerals, Olivine has a very high crystallisation temperature which makes it the first of the minerals to crystallise from magma. As magma cools, the crystals begin to form and settle on the bottom of the lava and form basalts that are abnormally enriched in olivine in the lower part of lava flows. According to H. M. King (on geology.com) "Olivine is thought to be an important mineral in Earth's mantle. Its presence as a mantle mineral has been inferred by a change in the behaviour of seismic waves as they cross the boundary between Earth's crust and mantle". Lava from Mount Franklin and other volcanoes in the area filled valleys and buried the gold bearing streams that became the renowned ‘deep leads’ of the gold mining era. In 1852, as part of the Victorian gold rush, gold was discovered in the immediate area, this gold was created by lava flows during the Newer Volcanic period, which were mined intensively during the nineteenth century. Around 1865 the presence of a deep lead in Mount Franklin was established. Deep lead mining was initially unsuccessful, and it was not until the late 1870s that the Franklinford Gold Mining Company mined at Mount Franklin on a significant scale. A few years later the Mount Franklin Estate Gold Mining Company also struck gold, followed by the Shakespeare and Great Western companies in the mid-1880s. By the late 1880s, however, deep lead mining had ceased in the area. Soon after gold was discovered in 1851, Victoria’s Governor La Trobe wrote to the Colonial Office in London, urging ‘the propriety of selecting and appointing as Mineral Surveyor for this Colony a gentleman possessed of the requisite qualifications and acquaintance with geological science and phenomena’. Alfred Selwyn was appointed geological surveyor in Australia in 1852 which began the Geological Survey of Victoria. In 1853-69 the Geological Survey issued under Selwyn's direction sixty-one geological maps and numerous reports; they were of such high standard that a writer in the Quarterly Journal of the Geological Society of London bracketed the survey with that of the United States of America as the best in the world. During his years spent in Australia, Selwyn collected numerous significant geological specimens, examples of which are held in collections such as the Burke Museum.This geological specimen is an example of basalt and olivine which shows the volcanic lava activity and geographical specific nature of Mt Franklin as a significant volcanic site. According to Agriculture Victoria 'The crater is one of the deepest in the Central Highlands area. It is a major megacryst site with some of the largest known Victorian examples of megacrysts of augite and an orthoclase. The small parasitic mound of Lady Franklin on the western flanks adds to the geological interest of the site'. This specimen also highlights the locality as a significant place for both indigenous activity and Victorian gold rush era mining practices. 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.An angular, solid hand-sized piece of grey volcanic Basalt with green/brown Olivine phenocrysts along one flat edge.Olivine in basalt / - label is probably / correct. / C. Willman / 15/4/21burke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, mineralogy, basalt, igneous rock, igneous-volcanic, volcanic geology, volcanic, olivine, olivine specimen, basaltoid

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 ship was built in 1953 by Ferguson Shipbuilders of Port Glasgow, Scotland for the Port Phillip Sea Pilots organisation as a pilot cutter. Her role as a pilot cutter was to sail with pilots on board to meet ships entering Port Phillip Bay. Pilots would be transferred by the Wyuna's workboat to the vessel requiring pilotage while it was stopped dead in the water, with shelter provided by the vessel itself. In the early 1970s the pilot service started using fast launches to allow pilots to board while ships were still underway, and in 1979 the Wyuna was sold to the Australian Maritime College in Launceston, Tasmania as a training vessel. She continued in that role until 2004 when sold to Mineralogy Pty Ltd as an accommodation vessel. In September 2013 she was donated to the Western Port Oberon Association for the Victorian Maritime Centre currently at Crib Point. For a time she was docked at Beauty Point, Tasmania, and after being refurbished for 18 months she was to be moved to Docklands in Melbourne, Victoria. After this berth became unavailable the vessel was docked at Inspection Head Wharf in Beauty Point. After a period there it was towed into Bell Bay where she lays at anchor as of January 2016. When funding becomes available the Western Port Oberon Association has plans to display the vessel in a wet berth alongside the former Royal Australian Navy Oberon-class submarine HMAS Otama.Mr Henry HudsonBlack and white photograph of the Pilot Tender MV Wyuna partially obscured by a large wave at the rip, entrance to Port Phillip Bay.mv wyuna, port phillip pilot service, the rip, the heads, queenscliff, point lonsdale

Brown Coal is typically found as rocks. During formation the Brown Coal starts as peats, which is an acidic brown deposit resembling soil, and over time when subjected to pressure and heat these peats form the Coal. Brown Coal is the lowest rank of coal as it has a low carbon (energy) content, and a high moisture content. This high moisture content makes Brown Coal unsuitable for overseas exports. This particular specimen was recovered from the Yallourn Mine in Latrobe Valley, Victoria as part of the geological survey of Victoria being carried out by Alfred Selwyn. Otherwise known as the 'Yallourn Power Station', the Yallourn Mine is Australia's second largest mine. Yallourn Mine was first built in 1920, and since then it has been providing over 1 billion tonnes of Brown Coal to Australia every year. The Yallourn Mine is responsible for 22% of Victoria's electricity and 8% of Australia's electricity. As of 2021 the mine employs around 500 people. Due to ongoing maintenance issues and Australia's move to cleaner energy, the Yallourn Mine intends to shut down permanently as of 2028. Soon after gold was discovered in 1851, Victoria’s Governor La Trobe wrote to the Colonial Office in London, urging ‘the propriety of selecting and appointing as Mineral Surveyor for this Colony a gentleman possessed of the requisite qualifications and acquaintance with geological science and phenomena’. Alfred Selwyn was appointed geological surveyor in Australia in 1852 which began the Geological Survey of Victoria. In 1853-69 the Geological Survey issued under Selwyn's direction sixty-one geological maps and numerous reports; they were of such high standard that a writer in the Quarterly Journal of the Geological Society of London bracketed the survey with that of the United States of America as the best in the world. During his years spent in Australia, Selwyn collected numerous significant geological specimens, examples of which are held in collections such as the Burke Museum.Brown coal is considered to be an essential rock to Australia's energy consumption. Although plentiful in sources, Brown Coal is not able to be exported overseas due to its high moisture content. As Australia moves towards cleaner energy, Brown Coal is going become less used. 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 sedimentary rock that is a dark shade of brown.13 / BROWN COAL / Showing Woody structure / Locality: Yallourn, Vic. | Label probably / correct but / can't find reference / no. 13 to match in / registers. / C Willman / 15/4/21burke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, mineralogy, yallourn, yallourn mine, victoria, coal, brown coal, brown coal specimen, alfred selwyn, geological survey of victoria, geological survey, yallourn power station

The booklet comprises of a series of papers published in the Ballarat Star, with some revisions. The Administrative Council hoped the publication would increase interest in Technical Education, especially the Art of Mining. He would also hope the public would recognise the Ballarat School of Mines as an institution adapted to supply technical education. The Ballarat School of Mines Council listed at the front of the book includes: Redmond Barry (President and Trustee), Judge Rogers (Vice-President), Somerville Livingstone Learmonth (Trustee), Rivett Henry Bland (Trustee), Charles Gavan Duffy, John A. MacPherson (MLA), William McLellan (MLA), Duncan Gillies (MLA), F. McCoy (University of Melbourne), John I. Bleasdale, W.H. Barnard, James M. Bickett, Henry Richards Caselli, P. Chauncy, J.M. Davey, Joseph Flude, R.F. Hudson, Robert Lewis, James Oddie, Robert M. Serjeant, J. F. Usher, John Walker, J. Williamson, Mayor of the City of Ballaarat, chairman (for the time being) of each of the seven Mining Boards of Victoria. The President of Examiners was Judge Rogers, and the Honorary Auditor was Richard Ford.Stapled, brown soft covered booklet of 48 pages. Section I outlines the establishment of the Ballarat School of Mines, the buildings and land used by the school, describes in detail the former Ballarat Circuit Court and describes the lecture rooms. Section II describes the Ballarat School of Mines Museum, including a description of exhibits. Section III describes the lecture hall, and the apartments on either side of the hall, including the office of the registrar W.H. Barnard, mathematical classroom, chemical laboratory, and metallurgical laboratory. Section IV outlines the subjects offered by the Ballarat School of Mines, including Mathematics taught by John Victor of Grenville College, who had been educated at Trinity College Dublin. Mining and Land Surveying was taught by C.W. Thomas. Mr Croll taught mechanical drawing, followed by Jonathan Robinson of the Union Foundry, and finally S. Keast. It then lists some text books used in the school. Section V mentions the School Council, lack of funds, future directions, mining laboratory. Vi- Describes the land and out buildings, and the proposed building for metal and wood turning, brass foundry, blacksmith, working engine, etc. This section describes some large donations to the school - 50 pounds from the Misses Meglin of Melbourne, 10 pounds 10 shillings to the 'Pyrites fund' by the Walhalla and Long Tunnel Companies in Gippsland. Section VII covers the teaching of chemistry by Joseph Flude. Section VIII outlines the metallurgy classes and the process of assaying. Section IX covers telegraphy taught by Mr Bechervaise Section X describes the examination process at the Ballarat School of Mines. Examiners in mathematics were G.J. Russell (Buninyong) and John Lynch (Smythesdale), mining and land surveying John Lynch and P.C. Fitzpatrick (Ballarat), Principles and Practice of Mining R.M. Serjeant (Band and Albion Consols), Mechanical Engineering John Lewis (New North Company Clunes, Mineralogy and Geology G.H. F. Ulrich, Assayign and Chemistry J. Cosmo Newberry, and Telegraphy R.L.J. Ellery (government astronomer) and Sam W. Macgowan. Underground managers and captains in quart mining was examined by Henry Rosales (Walhalla Company), and alluvial mines by Messrs Bockett, Kent, Martin and Mitchell. Engineers and Engine driving was examined by W.H. Keast,Peter Matthews, Jonathan Robinson and J.M. Troup. Section XI - Covers Annual reports of the school, and honorary correspondents of the school including: John Day (Geelong); R. Evan Day (London); W.W. Evans, M.J.C.E. of New York; J.Y. Fishburne, M.B. of Ararat; Felice Giordano, Inspector of Mines, Italy; Julius Von Haast, Ph. D.F.R.S., Government Geologist of Canterbury; James Hector, M.D., F.R.S., Government Geologist of Wellington, New Zealand, W.F. Hopkins (Grant); Charles A. La Trobe, C.E. (Engineer-in-Chief International Railway Plant, London); Archibald Liversidge, F.G.S. (Professor of Mineralogy and Reader in geology at Sydney University; J.J. Macgregor, M.D. (Creswick); J.T. McKenna (1st class of SMB underground management - Northern Territory); Henry Rosales, M.E. and M. (Walhalla); Harrie Wood (SMB founder and Under-secretary for Mines, Sydney); John Walthew (Stockport, England) .2) Signed 'E.J. Tippett', former President of the Ballarat School of Mines Council melbourne, mla, ballarat school of mines, redmond barry, j f usher, james bickett, w f hopkins, rivett henry bland, s m b, judge rogers, somerville learmonth, charles gavan duffy, gavan duffy, john macpherson, william mclellan, duncan gillies, f mccoy, university, john bleasdale, henry richards caselli, henry caselli, p chauncy, j m davey, joseph flude, r f hudson, robert lewis, james oddie, robert m serjeant, john walker, j williamson, richard ford, ballarat court house, assay, john victor, grenville college, trinity college dublin, c w thomas, jonathan robinson, union foundry, s keast, blessdale, john day, r evan day, w w evans, j y fishburne, felice giordano, julius von haast, james hector, charles a la, trobe, archibald liversidge, j j macgregor, j t mckenna, henry rosales, harrie wood, john walthew, fees, frederick mccoy, w.h. barnard

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

Used at the Ballarat School of Mines and the Ballarat Technical Art SchoolThis collection of examinations is significant because of its completeness with the full range of examinations between 1914 and 1950.Large leather bound books, with leather spine, containing all examinations held at the Ballarat School of Mines (including the Ballarat Technical Art School and Ballarat Junior Technical School). The examination papers were supplied and printed by the Education Department, Victoria. Examinations include: Agriculture, Algebra, Architecture, Arithmetic, Applied Mechanics, Assaying, Biology, Botany, Boilermaking, Building Design, Blacksmithing, Bricklaying, Carpentry and Joinery, Coachbuilding, Cabinet Making, Civil Engineering, Cabinet Making, Commercial, Chemistry, Engineering Drawing, Economics, English, Electrical technology, Electricity and Magnetism, Electric Wiring, Electric Welding, Electrical Fitting, Electrical Trades, Food Analysis, Geology, Geological Mapping, Graphics, Geometry, Heat Engines, Heat Treatment, Hydraulics, Hand Railing, Instrument Making, Millinery, Milling and Gearouting, Machine Shop Practice. Metal Founding, Mining, Metallurgy, Mineralogy, Mathematics, Motor Mechanics, Mine Surveying, Mining Mechanics, Petrology, Physics, Painting and Decorating, Pattern Making, Plastering, Plumbing and Gasfitting, Printing, Refrigeration, Spelling, Science , Shorthand, Surveying. Signwriting. Sheet Metalwork, Toolmaking, Ladies Tailoring, Trigonometry, Typewriting, Welding, Commercial Geography. Millinery, Dressmaking, Needlework, Decorative Needlework, Architecture, Building Design and Construction, Art (Composition in Form and Colour), Art (Casting Clay MOdels) Art (Drapery), Art (Drawing the Human Figure From Casts), Art (Drawing the Antique from Memory), Art (Drawing from Memory); Art (Drawing Plant Forms from Nature, Art (Drawing Plant Forms From Memory), Art (Drawing from Models and Objects), (Drawing From a Flat Example). Art (Drawing in Light and Shade from a Cast of Ornament or Lower Nature), Art (Drawing Ornament from the Cast), Art (Drawing from Models or Objects), Art (Drawing fro Dressmakers' and Milliners' Fashions), Art (Drawing With the Brush), Art (Drawing from a Flat Example); Art (Modelled Design), Art (General Design), Art (Embossed Leatherwork), Art (Practical Plane Geometry), Art (Practical Solid Geometry), Art (Geometrical Drawing), Carpentry and Joinery, Art (Human Anatomy), Art (Historic Ornament), Art (House Decoration), Art (LEttering), Signwriting, Art (Light Metalwork), Art (Modelling), Art (Modelling the Human Figure from a Life), Art (Stencilling); Art (Wood Carving) Refrigeration, Teaching, Boilermaking, Blacksmithing, Carpentry and Joinery, Coachbuilding and Carriage Drafting, Electric Wiring, Electrical Fitting, Graining and Marbling, Instrument Making , Machine Shop Practice, Metal Founding, Milling and Gear Cutting, Motor Mechanics, Painting and Decorating, Sheet Metalwork, Toolmaking, Printing, Pattern Making, Plumbing and gasfitting, examinations, ballarat school of mines, ballarat technical art school, trades, education department victoria, agriculture, algebra, architecture, arithmetic, applied mechanics, assaying, biology, botany, boilermaking, building design, blacksmithing, bricklaying, carpentry and joinery, coachbuilding, cabinet making, civil engineering, commercial, chemistry, engineering drawing, economics, english, electrical technology, electricity and magnetism, electric wiring, electric welding, electrical fitting, electrical trades, food analysis, geology, geological mapping, graphics, geometry, heat engines, heat treatment, hydraulics, hand railing, instrument making, millinery, milling and gearouting, machine shop practice, metal founding, mining, metallurgy, mineralogy, mathematics, motor mechanics, mine surveying, mining mechanics, petrology, physics, painting and decorating, pattern making, plastering, plumbing and gasfitting, printing, refrigeration, spelling, science, shorthand, surveying, signwriting, sheet metalwork, toolmaking, ladies tailoring, trigonometry, typewriting, welding., dressmaking, needlework, decorative needlework, architecture, building design and construction, art (composition in form and colour), art (casting clay models), art (drapery), art (drawing the human figure from casts), art (drawing the antique from memory), art (drawing from memory), art (drawing plant forms from nature, art (drawing plant forms from memory), art (drawing from models and objects), (drawing from a flat example), art (drawing in light and shade from a cast of ornament or lower nature), art (drawing ornament from the cast), art (drawing from models or objects), art (drawing for dressmakers' and milliners' fashions), art (drawing with the brush), art (drawing from a flat example), art (modelled design), art (general design), art (embossed leatherwork), art (practical plane geometry), art (practical solid geometry), art (geometrical drawing), art (human anatomy), art (historic ornament), art (house decoration), art (lettering), art (light metalwork), art (modelling), art (modelling the human figure from a life, art (stencilling), art (wood carving), teaching, coachbuilding and carriage drafting, graining and marbling, milling and gear cutting, commercial geography, exams, examination book

.2) Timetable book of the Ballarat School of Mines, associated with H.H. Smith, and student fees.ballarat school of mines, trades, h.h.smith, sheet metalwork, plumbing, gasfitting, carpentry, joinery, cabinet making, manuel training, photography, architecture, engineering drawing, dressmaking, assaying, chemistry, electricty and magnetism, fitting and turning, electrical calculations, geology, geometrical drawing, hydraulics, applied mechanics, mining geology, metallurgy, mineralogy, printing, physics, petrology, surveying, steam and gas engineers, turning and fitting, trigonometry, telegraphy, telephone fitters, woolclassing

The Ballarat School of Mines was established in 1970 and was the first school of Mines in Australia.A number of Ballarat School of Mines Annual General reports bounds in a dark blue hardcover with black leather spine. Includes some illustrations such as the Ballarat School of Mines Senior Staff.mining, mining alumni, geometry, steam, botany, ballarat school of mines, alfred mica smith, j f usher, andrew anderson, chemistry, metallurgy, a e c kerr, henry j hall, veterinary science, robert e weir, assaying, mineralogy, petrography, algebra, trigonometry, applied, mechancis, land surveying, mine surveying, dynamics and heat, sound and light, magnetism and electricity, carpentry and joinery, architecture, photography, john warrington rogers, james bickett, thomas wanliss, henry cuthbert, museum, william huey, steele, and, gas, engines, mine managers certificate, john m sutherland, charles e campbell, cyanide plant, mining laboratory, samuel thornton, daniel walker, percy osborne, robert allan, hubert murphy, charles deane, ernest trend, thomas evans, alfred johnston, boer war, richard maddern, underground, ferdinand krause

John Kennedy was born on 04 April 1862, the son of ship carpenter Robert Kennedy and his wife Florinda (Aitken), and the brother of Malcolm and Colin Kennedy. In 1860 the family migrated to Melbourne where Kennedy senior set up as a shipwright. In 1879 Malcolm and John, who trained as a naval architect, joined their father as Robert Kennedy & Sons, shipbuilders and shipsmiths. On 27 December 1883 at North Melbourne, Malcolm married Ann White with Presbyterian forms. Next year Robert Kennedy & Sons removed to Hobart where with John W. Syme and W. J. Duffy, partners until 1889, they took over the Derwent Ironworks & Engineering Co., a foundry formerly owned by the (Alexander) Clark family. The Kennedys also acquired the patent slipyard, formerly Ross's, at Battery Point. After the shipbuilding industry in Hobart began to flag John also turned to mining: he attended the Ballarat School of Mines, and reopened the Hobart smelters which had been an adjunct of the Derwent Ironworks in the 1870s. He made several voyages overseas on smelting business and as mining promoter, and was a member of the London Stock Exchange. In 1913-14 he was manager of Tongkah Compound (1910); Robert Kennedy & Sons was reputed to have contributed to the success of the Hobart-run Tongkah Harbour, Thailand, tin mines by developing a suitable dredge. The brothers also held shares in the Irrawaddy Burma Co. John was a member of the Australasian Institute of Mining Engineers and from 1932 an honorary life member of the American Institute of Mining & Metallurgical Engineers. John died in Hobart on 10 January 1937. (Ann G. Smith, 'Kennedy, John (1862–1937)', Australian Dictionary of Biography, National Centre of Biography, Australian National University, http://adb.anu.edu.au/biography/kennedy-john-7092/text11963, published first in hardcopy 1983, accessed online 24 April 2020.) A book covered in black leather with 'John Kennedy' embossed on the front in gold. The book contains notes from the time he studies at the Ballarat School of Mines. The beginning of the book has an alphabetical section where John Kennedy has created an index.Inside front cover 'John Kennedy Nena Wharf Hobart Tasmania.' john kennedy, australasian institute of mining engineers, ausimm, american institute of mining metallurgical engineers, ballarat school of mines, lecture notes, lecture notebook, antinomy, brick clay, carbon, coal, copper, chemistry, clay, chrome, electricity, fire clay, gas, gold, gold bullion, glass, gold test for, iron metallurgy, light, lead, metallurgy, mica, mineralogy, pyrites, sulphur in pyrites, sugar, slags, wolfram, preparation of pure gold, scorification, gold bullion assay, petrography, melting poinys of bodies, metric system, geology, mount morgan, queensland, rock salt, assay of tailings, classification of rocks, muffle furnace, ballarat school of mines wind furnace, assay of antinomy, recovery of silver from solutionsheat pyrometer, spectroscope, organic acids, metallurgy of iron, assat of copper, cornstock lode nevada, mount morgan queensland, scarification, elmwood, metallurgy of lead, specific gravity, copper assay, seperation of gold from other metals, test for gold, wet assay, mercury