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

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

‘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

Although it is not known where these specimens were collected, 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. 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. The term carnelian primarily refers to the reddish shading of the stone; whether the stone is termed an agate or chalcedony type is often influenced by the degree of colour banding the specimen shows. 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.Three small geological specimens that appear visually consistent with images of rough or unpolished Carnelian Agate or Chalcedony. geological specimen, geology, geology collection, burke museum, beechworth, indigo shire, north-east victoria, gemstones, agate, carnelian

Quartz is an extremely common mineral to find across the world. Quartz can have two forms; Microcrystalline quartz or Crystalline quartz. Microcrystalline quartz is a fine grain quartz where crystalline quartz is often a large crystal. This specimen is a crystalline quartz. Made of silicon oxide, this specimen is called smokey quartz crystals because of its brownish colour. However, the colour of quartz can vary. In addition, quartz are formed in deep-seated igneous rocks and crystallized through hot aqueous solutions. This type of crystal can be found all over Australia, including Beechworth in Victoria. Other places quartz can be found is the Ashburton River area in Western Australia, Marlborough in Queensland, the Lune River area in Tasmania and Kingsgate in New South Wales. This specimen is significant because it is common to find this kind of mineral. While the location of where this specimen was originally from is unknown, it highlights the many places in Australia where quartz is found. It demonstrates that quartz makes up a large portion of Australia's geology. In addition, quartz itself can vary in its colour and shape. This specimen represents one of these variations. That being smoky quartz crystals. 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 large hand-sized quartz mineral with shades of brown and gray throughout.Smoky quartz / crystals /locality/ unknown / (needs a wash) /BBgeological specimen, geology, geology collection, burke museum, beechworth, microcrystalline, quartz, quartz mining, quartz reefs beechworth, smokey quartz crystals, crystals, crystalline, silicon oxide, brown, colour, igneous rocks, magma, ashburton river, western australia, marlborough, queensland, lune river, tasmania, kingsgate, new south wales, nsw

Common Opal is a mineraloid that is non crystallising and is classed as an amorphous silicate, the chemical composition for Opal is SiO2 nH2O. Opals can develop in weathered sedimentary rock typical in arid regions where limited water enters small gaps in the rock, and the silicate is hydrated. Common opals, unlike precious opals, do not exhibit ‘play of colour’ in which the colour appears to change depending on the angle of view. While precious opals are highly valuable and cut as gemstones for jewellery, common opals can be cut into inexpensive gemstones and are also mined for various uses including as ingredients in ceramics, insulation, fillers, and abrasives. The source of this common opal specimen is unknown, but common opals are found around the world, notable deposits are found in Queensland, South Australia, New South Wales, Peru, Kenya, Nevada, Oregon, and Mexico. This common opal specimen is of historic and scientific significance due to its donation in 1868 as part of the Geological Survey of Victoria and as a typical example of uncut common opal. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A palm-sized amorphous (non-crystallising) hydrated silicate mineraloid specimen in shades of brown, orange, and white.Existing label: Common Opal / Locality unknowngeological specimen, geology, geology collection, burke museum, beechworth, common opal, opal, mineraloid, amorphous silicates, hydrated silicate

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

Malachite is a water soluble, crystalline, triphenyl methylene chloride salt. It has a close relationship to copper because it is common for Malachite and copper to come from the same ore. Malachite often has shades of green, making it also known as Malachite Green. As a result of it's colour, it is known for being a dye and has been used in the dye industry, the textile industry and in medical fields. Cobar in New South Wales is well known for it's mining. This is because of the number of important deposits present in the area and include three important mining belts where most of the materials are found. These are the 'Cobar belt', the 'Canbelego belt' and the 'Girilambone belt'. The 'Cobar belt' runs underneath the main town. Copper was first discovered in Cobar in 1869 and since then, many deposits of other materials have been found, including Malachite.This specimen is significant because it comes from Cobar, NSW and represents the many deposits of materials found there. Cobar has a long history of mining and is a source of Australia's copper minerals. Malachite is often found in copper deposits meaning that it is representative of Cobar's copper production. Malachite is known for it's vivid green colour and as a result, has many uses, such as meaning used as a dye. This makes it a valuable material and highly significant. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A solid hand-sized mineral with shades of brown , white and light green throughout.geological specimen, geology, geology collection, burke museum, beechworth, malachite, copper, water soluble, cobar, cobar mines, cobar mining, cobar nsw, nsw, new south wales, mining belts, ore, copper ore, malachite green, dye, green, dye industry, textile industry, desposits, canbelego, girilambone, alfred selwyn

Amazonite is classed as a Tectosilicate and is part of the Feldspar group of minerals. Amazonite forms in a triclinic crystal structure and its chemical formula is K(AlSi3O8). In appearance, Amazonite can range from shades of green to green blue to blue, and often with white streaks or veining. The greenish colour is believed to come from the small amount of lead contained in its composition. Amazonite is named after the Amazon River due to its colour and similarities to another rock found along the riverbanks, although Amazonite is not actually found at or near the Amazon. Although less commonly used in jewellery today, Amazonite has been mined and used by humans for thousands of years and Amazonite jewellery from at least 2000BCE have been discovered in North Africa. Amazonite is found in many locations around the world including Brazil, Peru, Ethiopia, Canada, Russia, Mozambique, Myanmar, Pakistan, China, Madagascar, and the United States of America. This specimen most probably comes from the U.S.A., Amazonite is found in several US states particularly in Colorado, Virginia, Pennsylvania. This specimen is of both scientific and historic significance as a striking blue green example of Amazonite mined prior to 1868 in the United States of America, most likely from Colorado, Virginia, or Pennsylvania. These three states are all locations of significant Amazonite deposits. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A palm-sized Feldspar mineral specimen from the Tectosilicate class in shades of blue-green with white veining.Existing label: green/blue Feldspar / "amazonite" / possibly USA geological specimen, geology, geology collection, burke museum, beechworth, tectosilicate, amazonite, feldspar, triclinic crystal structure, amazonite usa, amazonite colorado, amazonite virginia, amazonite pennsylvania

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. Quartz is found all over Australia, including Beechworth in Victoria. It is formed in deep-seated igneous rocks and crystallized through hot aqueous solutions. It can have two forms; Microcrystalline quartz or Crystalline quartz. Microcrystalline quartz is a fine grain quartz where crystalline quartz is often a large crystal. The colour of quartz can vary. These specimens were collected in Victoria in the vicinity of the Burke Museum. 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.Geological specimens of Agate and Quartz respectively; the fist-sized piece of Agate has peach/coral colouring with grey concentric patterning and the smaller piece of quartz is a uniform yellow/orange shade. Existing label: Local pebbles / (agate and / quartz / (yellowish) / egg-shaped). / BB geological specimen, geology, geology collection, burke museum, beechworth, agate, quartz, north-east victoria, indigo shire, geological surveys

Galena occurs in a range of deposit contexts, often in metalliferous veins, such as Broken Hill, Australia; Coeur d’Alene, Idaho, United States.; Clausthal Zellerfeld, Germany; and Cornwall, England. Large deposits also replace limestone, dolomite, or occasionally organic matter, or have a contact-metamorphic origin. Galena is additionally found in cavities, brecciated (fractured) zones in limestone and chert, and in coal beds. This specimen was recovered from Broken Hill NSW and is 60% lead with 8-12 oz/silver to the ton.Galena or 'lead glance' is a grey lead sulfide and the chief ore mineral of lead. It forms isometric crystals in which the ionic lattice is similar to sodium chloride. Galena is brittle and easily weathers to secondary lead minerals, with the upper part of mineral deposits often containing cerussite, anglesite, and pyromorphite. It usually contains silver, which is mined along with its lead content. Other commercially important minerals that form in close association with galena are antimony, copper, and zinc. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A small-sized solid specimen containing one mineral with a sparkly silver metallic lustre exterior and pastel-grey interior.geological specimen, geology, geology collection, burke museum, beechworth, galena, lead sulphide, alfred selwyn, broken hill

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

It is not known where this opal originated. Common Opal is formed from silica-rich water entering the earths crust and hardening into a gel of water and silica-spheres, layered through the specimen. Common opal differs from precious opal in colouration and appearance, with precious opal including more colours, and having a translucent or glossy appearance, where common opal shows less colour and is typically opaque. It scores high on the Mohs hardness scale, and is common throughout the world, especially in Australia, where it is far more prevalent than the highly-prized precious opal. Australia is also the highest producer of opals in the modern world. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A solid, silica-based mineral specimen of Common Opal in shades of grey, green, and yellow, with a thick grey vein running through the centre. geological specimen, geology, geology collection, burke museum, beechworth, opal, common opal, gemstone, mining

A granular metamorphic rock, marble is derived from limestone or dolomite and composed of calcite or dolomite interlocking grains. Heat and pressure from overlying sediments form it from limestone buried deep in Earth's crust. Graphite, pyrite, quartz, mica, and iron oxides can affect rock texture and colour. This specimen was found in Carrara, Italy. Carrara marble is the most common marble found in Italy, and it gets its name from the region where it is located. The marble was also called Luna marble and was used as a decorative element in buildings and sculptures. It has been quarried since Roman times in the Lunigiana, the northernmost tip of Tuscany, just outside the city of Carrara in the province of Massa and Carrara.Marble is one of the most popular and expensive rocks used in sculpture, architecture, interior decorations, statues, table tops, and novelties. It is available in various colors and textures depending on the chemical composition. The strength of the rock and its ability to hold finer details have made it a favorite among designers. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A solid hand sized Marble (metamorphic rock) predominantly white with specks light grey and ochre geological specimen, geology, geology collection, burke museum, beechworth, marble, carrara marble, italian marble, marble specimen, tuscany

Fluorite comes in a variety of natural colours and crystal formations and glows under ultraviolet light (the word 'fluorescence' comes from the same etymological source). In its pure form, calcium fluoride, it is a colourless combination of the elements calcium and fluorine, but gains its colour from trace elements that infiltrate or replace calcium within its crystal structure during its formation. Although fluorite crystals polish well and can achieve a high level of lustre, the mineral is very soft (4 on MOHS hardness scale) so it is unsuitable for use in rings and must be handled and stored carefully if used in other forms of jewellery. Most crystals of the mineral are too coarse for decorative purposes but have been mined under the name fluorspar for a variety of commercial and industrial purposes. These include the production of hydrofluoric acid, smelting metal alloys, producing glazes and ceramic finishes and use in medical and dental products. An existing label for this specimen indicates that its origin or collection-point was 'probably USA.' Fluorspar, the form of fluorite used commercially and industrially, was mined in significant quantities in the counties of Hardin and Pope in South-Eastern Illinois throughout the Nineteenth and Twentieth Centuries. Fluorite was made Illinois' state mineral in recognition of its contribution to the state's identity and economy. The specimens are significant as examples of surveying activity undertaken to assess and direct the development of the mineral resource industries, as well as the movement to expand human knowledge of earth sciences such as mineralogy and geology in the nineteenth century.The specimen is a piece of purple shaded fluorite (also known as fluorspar), the mineral form of calcium fluoride. The unpolished specimen presents a dark purple interior with a substantial dark grey crust representing the matrix from which the specimen was obtained. Existing label: Flourite / (purple) / probably / USA / BB /burke museum, beechworth, geological, geological specimen, fluorite, flourite, calcium fluoride, hydrofluoric acid, jewellery, indigo shire, north-east victoria, mining, illinois, usa, united states, fluorine, gemstones, purple stones

Laterite refers to both a rock and a soil type that is rich in clay, as well as Iron and Aluminium. It is created during a process that is called laterization, where high heat and seasonal heavy rainfall cause there to be wet and dry periods, which over time hardens the soil into rock. Because of this, most laterite is formed between tropics of Cancer and Capricorn. The iron oxide in laterite is what gives it it’s orange-red colouring. The largest religious complex in the world, Angkor Wat in Cambodia, is partially constructed of laterite, particularly its foundations, as laterite is porous and allows rainwater to drain. This specimen of laterite was collected from the Democratic Republic of Congo while it was colonised by Belgium in the 19th century. Laterite forms in many parts of the world, particularly between the tropics. It is used both for ore and as a building material, and comparing specimens from different parts of the world allows us to document the different compositions that this mineral can have when formed at different locations. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.a palm-sized solid iron-aluminium oxide mineral specimen in shades of brown, orange and greyburke museum, beechworth, geological, geological specimen, laterite, laterite specimen, geology

Montmorillonite is a type of clay composed of aluminium silicate that forms very small particles that are not well-bonded to one another. This is why it is so soft. When in the presence of water, all types of clay swell. Montmorillonite swells even more than most types of clay, which is why it is often chosen over other types of clay in its practical uses. Montmorillonite has many different practical uses, including in the mining industry, as a soil additive, as a sealant, as a desiccant to draw water out of the air, to clean ponds, to make kitty litter and in cosmetics. Montmorillonite is a common mineral and, despite being named after Montmorillon, France, can be found all over the world, including many deposits in Australia. It is not known where this particular specimen originates from. Montmorillonite is an economically and socially significant material with a wide variety of uses. Having samples of common and important minerals allows collections, like the Burke Museum, to have a more complete view of the land on which they are located, and therefore a more complete view of heritage. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A solid tennis-ball sized chunk of aluminium silicate clay. It is primarily white, accented with orange and brown.burke museum, beechworth, geological, geological specimen, clay, montmorillonite

This specimen is Cassiterite in Quartz. Cassiterite is a tin oxide metal that forms in thin crystals which can have a beautiful lustre. Quartz is made of silicon dioxide, also known as silica, and is one of the most common minerals on earth. Cassiterite has been a fundamental source of tin ore for humans throughout history, including today. Tin is an important metal that has a wide variety of human uses in different areas, from dying fabric, to making mirrors, and their most well-known use ‘tin’ cans. Tin cans are primarily made of steel and are coated with tin in order to take advantage of tin’s property of being non-corroding. This is a massive step in the history of food preservation. Tinned food first reached Australia in 1815 with early settlers, and it began to be manufactured here in the 1840s. It was incredibly popular, and was a highly exported product, which would be a contributing factor to the ‘tin mining boom’ of the early 1880s. This specimen was collected at Jingellic, New South Wales, in about 1852. Although the Goldfields of the 1800s are much more well-known, tin mines existed alongside the gold mines which began in the mid 19th century and extended almost one hundred years, to the mid 20th century. Specimens like this would have been used as evidence to justify tin mining operations in the region as an investment. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study. The Geological Survey of Victoria was headed by British geologist, Alfred Richard Cecil Selwyn (1824-1902), who was responsible for issuing over 60 geological maps during his 17 years as director. These maps were all hand-drawn and coloured and became the benchmark for accuracy for geological mapping. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study. A fist-sized solid geological specimen made on one half of tin oxide, which is dark grey, and on the other side of silica, which is brown and cream.burke museum, beechworth, geological, geological specimen

There are 17 opal fields in Australia. This opal bearing stone was found in Lightning Ridge, NSW over what is known as the Great Australian Basin. This basin was formed and covers an area of 1.7 million square kilometers in eastern Australia in the Cretaceous period. This basin used to contain an inland sea, which provided an environment where silcrete eventually formed when water levels changed. This eventually seeped into other structures, and eventually hardened and formed opal. Lightning Ridge has a population of around 2000 people, with about 80 000 visitors every year. It is a historic mining town, and is known for its deposits of a rare black opal. Mining started in the area in the late 1800s, early 1900s when the black opal was discovered. This opal-bearing stone is of social and historical significance. It is from Lightning Ridge, which is well-known for being a large producer of opal stones, most famously black opal. The history of the period dates back to 140 million years, with the discovery of black opal in the early 1900s causing interest in the area. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.***A palm-sized solid mineral specimen in shades of beige and light orange*** silica based? burke museum, beechworth, geological, geological specimen, opal, opal fields, australia, lightning ridge, new south wales, great australian basin, cretaceous, silcrete, black opal, mining

It is made up of andalusite. Andalusite is a rock-forming mineral, sometimes found in granite or schist. It is often used to make glass, ceramic products, chemicals, and heat-resistant bricks as it can withstand high temperatures without changing. The chiastolite contains particles of graphite, which arranges in geometric patterns. When crystal growth occurs in the rock, the granite particles concentrate at crystal interfaces and can result in cross shapes. These ‘cross stones’ have been valued and used for their spiritual or religious meaning and used as charms, gems, or amulets. Chiastolite was first discovered in 1754, seen in a description in a published book by a palaeontologist, Franciscan priest, and Spanish author, Jose Torrubia. Deposits have been found in Australia, France, the USA, Chile, Canada, Spain, Brazil, Sri Lanka, and Russia. Deposits have been found in Western Australia and South Australia. This particular specimen was found in Bimbowrie, South Australia. Other chiastolite specimens have been found in Bimbowrie, along with jasper, quartz, and aventurine in the form of rolled pebbles or schist. This chiastolite specimen is socially and historically significant. It is a very rare sort of andalusite mineral. It is from one of only two locations where it is regularly found in Australia. The carbon cross has made it an important religious symbol in the past. Its ability to withstand high temperatures has made it a common ingredient in heat-resistant bricks and ceramics today. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A metamorphic mineral consisting of andalusite, with a cross shaped graphite pattern in colours of grey, brown and yellowburke museum, beechworth, geological, geological specimen, andalusite, chiastolite, geometric, cross stone, spiritual, religious, australia, south australia, bimbowrie, quartz, jasper, aventurine, schist

This specimen was donated in 1868 by Alfred Selwyn. Olivine is typically found in basic and ultra-basic igneous rocks around the world, in a variety of colours including yellowish green, olive green, greenish black and reddish brown with a transparent to translucent diaphaneity. The luster of the specimen is vitreous, the luminescence non-fluorescent and when fractured the mineral is very brittle producing small, conchoidal fragments. Chromian diopside is normally found in small sizes as the larger the size of the mineral the darker the colour is, almost black rather than green. Chromium is the element that gives chromian diopside and emeralds their rich green colour. Diopside is found across the world in multiple colours however gem-quality chromian diopside is mined in Siberia, Russia and prominent within the jewellery industry as a more affordable substitute to emeralds. Chromium-bearing diopside has been located across Australia. Chromium-bearing Diopside is located across the world found in North America, parts of South America, and across Australia, Africa, Europe and Asia. Chromium-bearing Diopside is mined in Siberia, Russia and is sold as a commercial substitute for emeralds. The stone is often turned into jewellery. This item is one of many geological and mineral specimens that constitute a broader collection obtained from various regions across Australia (as well as some international locales) and generously contributed to the Burke Museum between 1868 and 1880. A significant portion of these specimens originated from Victoria and were acquired as a result of the Geological Survey of Victoria, initiated in 1852 during the Gold Rush era. The primary objective of this survey was to investigate and chart the geological characteristics of Victoria. The procurement of geological specimens played a vital role in advancing our comprehension of the Earth's scientific composition and was instrumental in supporting research and educational institutions throughout Australia, including the Burke Museum, in their efforts to foster further exploration and study. A solid mineral specimen in shades of green, grey and brownburke museum, beechworth, geological, geological specimen

Brown quarter leather bound book with examinations results for students of the Ballarat School of Mines. non-fictionExamination results for a range of subjectsballarat school of mines, examination, alumni, j.b. robinson, practical chemistry, land surveying, assaying, mineralogy, metallurgy, geology, mining geology, building contruction, engineering, geometry, botany, mining, mechanics applied to mining, petrology, sound and light, steam and gas engines, engineering drawing, maxwell gaunt, a.s. ritchie, john adam, george hepburn, george cornell, godfrey hary, valentine anderson, john sutherland, william h. callister, lionel lambert, john currie, ferdnand g. krause, thomas lakeland, william troon, charles lund, richard cowles, glyndwr evans, norman buley, wilfred avery, norman lagerche, frederick l. treloar, arthur tandy, reginald callister, henry kofoed, david bonar, herbert j. semmens, a.d.r. galloway, william e. figgis, emma wardle, photography, leslie blick, leslie coulter, ernest heighway, henty whittingham, charles vale, james brokenshire, eric bieske, william baragwanath, harold cornell, j. raymond blight, george kidd, joseph mcgoldrick, samuel j. tongway, thomas k. sim, hevill tinworth, israel flegeltaub, oliver jaegar, charles flude, william burbridge, hubrt murphy, samuel mayo, ellen b. morris, elsie m. naples, jean rankin, hilda wardle, ernest morshead, arthur lilburne, herbert malin, robert serjeant, mollie o'dowd, robert w. allan, albert w. steane, leslie de j. grut, norman tinworth, robert m. serjeant jnr, vincent giuliano, william coates, allan bernaldo, loyal finch, john dulfer, william carroll, noel brelaz, guido brelaz, kathleen fisher

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

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

These photographs were taken by Caroline Winter, lecturer at the University of Ballarat. Horace Pickford was born at Clunes, Victoria. He was killed in action on 27 September 1917. According to his dossier Pickford was in the 58th battalion and was buried in the vicinity of Polygon Wood. Glyndwr Evans was a native of Treorchy in the Welsh Rhondda Valley. He emigrated to Australia with his parents who lived at Randwick in New South Wales. He attended the Ballarat School of Mines, and served on the Student's Magazine Committee in 1905. The following year Glyndwr took up a position as a solutionist at the Golden Horseshoe Mine at Kalgoorlie. In the application for a commission in the AIF Glyndwr stated at he had completed three years at the Ballarat School of Mines, obtaining a Mine Manager's Certificate of Competancy, an Assayers Certificate and additional certificates in Land Surveying, Electrical Technology, Metallurgy and Geology. Gyndwr was a member of the AIF 1st Australian Tunnelling Coy. He was killed in Action at Hill 60 on 25 April 1917 and is buried in Belgium at the Railway Dugout Burial Ground (Plot VII, Row G, Grave 33). (http://guerin.ballarat.edu.au/aasp/is/library/collections/art_history/honour-roll/honourroll_Evans.shtml) A number of colour photographs of World War One war graves of soldiers from the Ballarat district. .1) Horace Pickford's headstone, Tyne Cot Cemetery .2) Glyn Evans tombstone, Railway Dugouts Cemetery south of Ypres. 3. Railway Dugouts Cemetery, Glyn Evans tombstone has a poppy on it. university of ballarat, world war one, war graves, war cemetery, world war i, world war, pickford, evans, horace pickford, harry pickford

The Ballarat School of Mines was established in 1870 through the initiatives of the Ballarat Mining Board making it the oldest site of technical education in Australia. The Board was concerned with the shortage of mine managers for the goldfields. Classes began in surveying, mathematics, and chemistry and a decade later they included metallurgy , assaying and geology. With the decline in goldmining the direction of the college changed and broadened, the art School was established and the Ballarat Junior Technical School developed. In 1976, the tertiary sector seperated from the School of Mines and Industries Ballarat to form the Ballarat College of Advanced Education. In the 1980s SMB was a Community College of Technical Education and Further Education (TAFE) offering a wide range of vocational, enrichment and preparatory programs. It is continuing the tradition of providing for the educaiton needs of people within the Central Highlands. During the 1970s and 80s it acquired and refurbished old buildings and developed new facilities to keep up with the needs of an expanding curriculum and student population. The era of these annual reports is just before the merger with the University of Ballarat.A number of soft card covered annual report for the Ballarat School of Mines. .1) 12 page black covered report featuring an image of the E.J. Tippett Library. Includes information on death of E.J. Tippett, disability policy, Peter Quinn, Patti McNulty, Bob Feary, Shane Everand, Integration, Fiona Watson, retirement of Robert Morgan, Opening of the carpentry and Joinery Facility in Davey Street, formation of the School of Business and Information Technology, Melissa Bone, opening of the E.J. T. Tippett Learning Resource Centre (Library), Refurbishment of the Administration Building, Food Service Building (Prospects), Court House Theatre, Enrolment centre, Museum, Creche, Women's Trade technical Program, Rural Education Program, Ararat Prison Program, Community Studies Section, Ararat Adult Literacy Group. Literacy Assistance for Undergraduates, Fire training, fitness, open Learning, Training & Employment Group, Awards, Filipino Visitors, oil Seed Research, Brunei, Barometer (gift) for Horticulture, Special Equipment (guillotine and brake press; programmable logic Controller; theodolite: laser lever; Universal testing Machine; Atomic Absorption Spectrophotometer)., organisational Structure. Photos include Ken Flecknoe, Peter Quinn, Patti McNulty, Bob Feary, Shane Everard, Fiona Watson,Linda Bland, Robert Morgan, David McCaughey, E.J. Tippett, Frank Sheehan, Julie Baulch, Jo Reeves, Col McCurry, Jenny Garnham .3) Blue covered book with a photograph of the M.B. John Building taken from Albert Street on the cover. Topics include: Ken Flecknoe, Peter Shiells, Ararat Campus, David Haddow, Kevin Martin, Rendle Hannah, Gary Eason, Geoff Pope, Albert Peart, M.B. John building opened, Hairdressing Salon, Community Centre, Creche, closure of Lydiard Street, Museum, Jenny Levison, Inskill, Small Business Training, Ballarat Eat free Library, Barkly Street, Wormalds Valve Group, Aboriginal Programs, Horticulture Center, Awards, Country fire Authority, tractor Donation, Women's Policy. Special purchases included surveying equipment with data recorder, test rig , CDT MIG welder, compact gas chromatograph with FID and single pen recorder, Olivetti stand-alone word processing unit. Images include Ken Flecknoe. Peter Shiells, John Crowe, Trevor Slater, Brian McLennan, Kerrie Cross, Albert Peart, John Cain, M.B. John, Enrollment Centre, Museum, Jo Watson, Wormalds, Brian Webber, Dianna Nikelson, Ian Aitken, Brendan B, Chez Dichiera, Heather Dixon, Julie Broadbent .4) 1993 - Brown and white soft covered annual review featuring students of the Ballarat School of Mines at work. Bill Gribble, Brian McLennan, Peter Shiells Retirement, Robert C. Lovett, Steven Mendelson, Max Palmer, Jenny Gough, Mary Molloy, Barrie Firth, Colin McCurry, Dora Hormann, Organisation Structure, Brewery Acquisition, Humffray Street Primary School, Grant Street Retaining Wall, Neville Bunning Plaque, VCE Plus, Ballarat Small Business centre, Ararat Prison, Ballarat Showgrounds Rotunda, .6) Green covered annual review with an aerial photograph over Albert Street, Ballarat. Content include Kerrie Cross, Peter Shiells. Kenneth Flecknoe Obituary, Ian Pimblett, Keith Boast, David Nicholson, Max Palmer, Brian Webber, Bob Lovett, Linda Bland, Prospects, Training restaurant, 3BBB, Malcolm Vallance, Aboriginal Programs, Ian Cathie, Koorie Support Unit, Caroline Hogg, 'Trained Men Make Their Own Terms' exhibition at the Gold Museum, Ricky Hains, Stephen Hughes, Jeff White, Dennis Bolster .8) Blue covered review for 1989. The contents include: Kerrie Cross, Peter Shiells, Ann McCaffrey, Kevin Alsop, Mary Molloy, Ross Furness, Robert Lovett, Victoria Street Student Hostel, Hugh Beggs, Ballarat Small Business Centre, Inskill, Ararat Campus, Hospitality and Tourism, Koorie Support Unit, Fiona Warsn, Bruce Staley, Terry Moran, Anthony Wonish, Ivan Deveson, Leo Shannon Memorial Award, Bryan Crebbin, Geoff Howard, R.C.W. Burdett, Jeff White, Ian Harris, Tom Wiseman, Bill Gribble, Allison Kay, Steven Mendelson, Keith Boast. .9) Grey covered book with a coloured photo of the Victoria Street Student Residence. Contents include: Kerry Cross, Peter Shiells, Morgan Bevan John Illuminated address. Jean Phillips, Koorie Support Unit, Andrew Sullivan, Victoria Street Student Residence, Horticulture, Inskill, Tertiary Awareness Project, Adult Education, Ivan Deveson, Brian Howe, Barry Jones, Joan Kirner, Andrew Trigg, Warren Perry, Murrell Rock Collections, Gwyn Hanssen-Piggott, Disability Awareness Day, Sebastopol Borough Logo, Phoebe Rimmer, Russell Jackson, R.J. Young Scholarship, Peter Muir, Founders Day Cake, Morgan John. .11) Black card covered booklet with five images of exteriors of the Ballarat School of Mines. the contents include: Jack Barker, Peter Shiells, Peter Ellyard, Ian Stoney, Terry Moran, Wayne Strong, David Ince, Simone Titheridge, Ian Aitken,Kevin Alsop, Bill Bridges, Clive Carmichael, Bob Feary, Rendle hannah, Roly Parfenovics, Graham Snibson, Kevin Stockdale, Len Wilson, Child Care Centre opening, Student accommodation, Victoria Street, Brewery site. naming buildings, E.J. barker. A.W. Steane K.J. Flecknow, Carpentry and joinery, Inskill, Hospitality, Pottery, ceramics, Founders' Day, Warren Perry, Agreement between Ballarat School of Mines and Ballarat university College, merger, Peter Baldwin, Awards, obituary Lindsay Hillman. Images include: Wayne Strong, David Ince, Simone Titheridge, kerrie Cross, Joan Kirner, Frank Sheehan, Bill Gribble Ros Wilkie, Judi O'Loughlin, Tony Leonard, Gemma Hearnes, Brendan Hill, Joanne Bell, Karl Moon, Stella Savy, Shirley Falkinder, Peter Baldwin, Jack Barker, Michael Ronaldson, David Kemp, Peter Shiells, Margot Healey, Sharon McLennan, Kerrie Firns, Petrena Brookers, Deb Goudappel, Claire Bond, Administration Building Lindsay Hillman. .13 ) Brown covered report with photographic images. Content includes: Pam Merrett. , Peter Shiells, Robert Lovett, Steven Mendelson, Max Palmer, Jenny Gough, Barrie Firth .14) Brown covered report with photographic images. Content includes: .15) Green covered report with photographic images. The blond woman standing on the right looking at a computer screen is Pam Merrett. Content includes: Bill Gribble, Ron Wild, Doug Sarah, Martin Hill, John Kemp, David Manterfield, Leslie Comy, Linette Penhall, Glen Martland. Virginia Fenelon. Michael Bracher, Brewery Building. Child care centre, Prospects Cafe Opening, Horticulture Training Centre, Retaining Wall, The Gordon, University of Ballarat and Ballarat School of Mines affiliation, Geoffrey Blainey, Ararat Community College Memo of understanding, Brian McLennan. Founders Day (Hadden Storey), Gwyn Hanssen-Pigott, Ken Latta, Neville Bunning Outstanding Achievement Award, Valerie Wilson, Jack Barker, John Sharpham, Jack Barker Resignation.ballarat school of mines, university of ballarat, integration, shane everard, robery morgan, linda bland, ballarat junior technical school, former court house, ken flecknoe, bruce muir, lindsay hillman, neil crouch, jack barker, keith boast, rex hollioake, m.b. john, bob lovett, brian mclennan, peter shiells, bruce tanner, jeff white, bryan crebbin, kerrie cross, ric dunlop, tom wiseman, barbara hughes, chris matheson, morgan b. john, albert street, steven mendelson, john crowe, ann mccaffrey, kevin alsop, mary molloy, ross furness, robert lovett, victoria street student hostel, student residences, hugh beggs, ballarat small business centre, inskill, ararat campus, hospitality and tourism, koorie support unit, fiona watson, bruce staley, terry moran, anthony wonish, ivan deveson, leo shannon memorial award, geoff howard, r.c.w. burdett, ian harris, bill gribble, allison kay, liz eddy, pam merrett, doug sarah, martin hill, john kemp, david manterfield, leslie comy, linette penhall, glen martland, virginia fenelon, michael bracher, brewery building, child care centre, prospects cafe, horticulture training centre, retaining wall, the gordon, university of ballarat and ballarat school of mines affiliation, geoffrey blainey, ararat community college memo of understanding, founders day, hadden storey, gwyn hanssen-pigott, ken latta, neville bunning outstanding achievement award, valerie wilson, john sharpham, kerry cross, morgan bevan john illuminated address, jean phillips, andrew sullivan, victoria street student residence, horticulture, inskill, tertiary awareness project, adult education, brian howe, barry jones, joan kirner, andrew trigg, warren perry, murrell rock collections, gwyn hanssen-piggott, disability awareness day, sebastopol borough logo, phoebe rimmer, russell jackson, r.j. young scholarship, peter muir, kenneth flecknoe obituary, ian pimblett, david nicholson, brian webber, prospects, training restaurant, 3bbb, malcolm vallance, aboriginal programs, ian cathie, caroline hogg, 'trained men make their own terms' exhibition at the gold museum, ricky hains, stephen hughes, dennis bolster, aboriginal education, e.j. tippett obituary, patti mcnulty, bob feary, equal opportunity officer, robert c. morgan, school of business and information technology, e.j. tippett library, e.j. tippett library opening, carpentry and joinery, women's trade and technical program, rural education program, ararat prison program, barometer, oil seed research, . bill gribble, peter shiells retirement, robert c. lovett, max palmer, jenny gough, barrie firth, colin mccurry, dora hormann, organisation structure, brewery acquisition, humffray street primary school, grant street retaining wall, neville bunning plaque, vce plus, ararat prison, ballarat showgrounds rotunda

This book contains the report from the select committee on Castlemaine and Sandhurst water supply; with the proceedings of the committee, minutes of evidence and appendices. It also contains the report Of the Engineer-In-Chief of Railways, and reply of the Chief Engineer of Water Supply on the works constructed by the Victorian Water Supply Department, presented to both houses of parliament by His Excellency’s command. Ferdinand M. Krause, was a lecturer at the Ballarat School of Mines in Geology Mineralogy Mining Engineering and Surveying. He was a Fellow of the Geological Society and a Fellow of the Linnian Society. He was assistant engineer for the Ballaarat and Ballarat East Water Supply Committee and helped plan local reservoirs.A brown cloth hard cover, foolscap book with leather spine. Title is written in black on the title page. "Water Supply Reports" is engraved in gold on spine. It includes a table showing the monthly and yearly rainfall and shade temperature at Ballarat, 2nd February, 1885. It also includes two reports and two replies, a map No.7082.2 of Victorian Water Supply, Castlemaine and Sandhurst district general plan including lines of Aqueduct, Reservoirs. No. 7082.3 of Victorian Mining districts, Mining Divisions and The Gold Fields in 1866 - includes districts to be supplied under the Waterworks Act, 1965. It also includes: *Report of the Engineer-in-chief of Railways and Reply of the Chief Engineer of Water Supply on the works constructed by the Victorian Water Supply Department, 1869. * Coliban Water Scheme, 1864 * Ballarat and Ballarat East Water Supply (1869) including the Ballarat Water Supply List containing names of occupiers and nature of improvements on lands comprised within the proposed reserve of Gong Gong Reservoir, Ballaarat. At Warrenheip the names included: Honora McCallin, William Honan, C. McMahon, Patrick McMahon, J.P. Beach, J.H. Smith, Michael Nestor, Martin Quinn, Martin McIntyre, Robert Higgins, Coleman Kane, Robert Bond. At Ballarat: William Clarke, Richard White, John Hosking, Wesleyan Chapel, J. Hewitt, Robert McRobinson. At Bungaree: John Pullin, John Llewellyn. William Daw, Smith and Wynne, William Brough, A. Alexander. * Ballarat and Ballaarat East Water Supply report upon the advisability, or otherwise, of constructing a reservoir at the junction of the Yarrowee Creek and Gile's Creek, upon a site known as Gile's Reservoir (printed by Frank Pinkerton). This report has numerous notes written on it (most probably by Krause) and includes the capacity of Harry Beale's Reservoir, Pimcott's Reservoir and the Proposed Gong Gong Reservoir. * Statement as to the position of the Ballaarat and Ballaarat East Borough Councils in Connection with Water Supply, September 1869. * Ballarat and Ballaarat East Water Supply - General Statement upon the Ballaarat and Ballaarat east Scheme of Water Supply. Includes information on Moorabool reservoir, Harry Beale's Reservoir, Lal Lal Creek, Two Mile Creek, Beale's Dam, Yarrowee Creek, Gong Gong Reservoir, Kirk's Dam, Devil's Creek, Moorabool Creek. Additional handwritten notes (probably by Krause) * Engineer's Report on the resolution of the COmmittee of Water Supply, of the 7th July 1868. The report refers to the Country around Mount Warrenheip. Names mentioned are L. Abraham, Great North-West Gold Mining Company, Border Sawmills, Ferdinand Krause, Ohlfsen Bagge, W.H. Shaw, A signature by "Ferdinand M. Krause" at the top corner of the title page. A few pages have handwriting on the margins, it is believed to be his handwriting. water supply victoria, castlemaine directories, sandhurst directories, ballarat directories, james blackburn, edward wardle, daylesford water race, c j taylor, george avery fletcher, bagge, ohlfsen bagge, george foote, john h reilly, ambrose johnson, george francis, timber preservation, james forbes, alfred surplice, malcolm carmichael, robert adams, frederick hugh thomas, h o christerpherson, william downe, thomas lawrence brown, francis hadgson nixon, strangways, guildford, maldon, muckleford, lauriston, malmesbury, franklinford, walmer, strathloddon, downe, ferdinand krause, m7082, trentham, castlemaine, drummond, metcalfe, sutton grange, lockwood, ravenswood, mandurang, yandoit, c.h. ohlfsen bagge, moorabool reservoir, gong gong reservoir, harry beale's reservoir, pincott reservoir, frank pinkerton, water

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

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