This item is part of the Federation University Art Collection. The Art Collection features over 1000 works and was listed as a 'Ballarat Treasure' in 2007.Lidded ceramic pot with blue crystalline glaze.art, artwork, coralee asker, asker, crystalline, ceramics

Native Sulphur in its solid form is a yellow crystalline mineral that forms near volcanic vents and fumaroles where it is the solid form of hot gases. It is also frequently found in the subsurface as a by-product of sulphide ore mineralization. In all its forms, sulphur is one of the most commonly occurring minerals on the planet, especially in natural gases, and is key to the make-up of a range of other minerals. It is essential to continuing life on earth, and was used in ancient societies as part of medical care, religious rites, and entertainment, and was key to the invention of gunpowder by the Chinese. Native Sulphur in its solid form is a yellow crystalline mineral that forms near volcanic vents and fumaroles where it is the solid form of hot gases. It is also frequently found in the subsurface as a by-product of sulphide ore mineralization. In all its forms, sulphur is one of the most commonly occurring minerals on the planet, especially in natural gases, and is key to the make-up of a range of other minerals. It is essential to continuing life on earth and was used in ancient societies as part of medical care, religious rites, and entertainment, and was key to the invention of gunpowder by the Chinese. The exact site of extraction for this specimen is unknown, but it was probably collected in New Zealand in the 1850s. Sulphur is significant both for its historical and current uses, and for its nature as one of the most abundant minerals on the planet. Sulphur's importance comes both from its abundance and its role in ensuring survival, creating other minerals, and daily human life. This specimen is significant as representative of sulphur's solid properties. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A solid, small, crystalline mineral specimen that is largely bright yellow, with some darker spotting. geological specimen, geology, geology collection, burke museum, beechworth, sulphur, native sulphur, new zealand, native sulphur specimen, sulphur specimen

David WILLIAMs David Williams established Toolangi Pottery in Toolangi, Victoria, in 1977. In 1980, he completed a BA in Fine Art from Phillip Institute of Technology (now part of RMIT University). He produces mainly crystalline glazed bowls, platters, vases, lampbases and other domestic ware. His works are marked with an impressed stamp reading 'David Williams' or 'David WIlliams Handcrafted in Australia ' and he also used a cursive 'DP Williams'.Photograph of a hand thrown ceramic vase with crystalline glaze. It is signed on the base with a cursive 'DP Williams'. ceramics, pottery, david williams, crystaline glaze, crystalline glaze, toolangi pottery, studio pottery, australian studio pottery

Box of 22 specimens of crystalline form, 3 missing

Number of parts: 27. Box of 26 specimens (glass) of crystalline

Bottle clear glass with ground glass stopper. Contains Ephedrine Alk, a yellow crystalline substanceflagstaff hill, warrnambool, shipwrecked-coast, flagstaff-hill, flagstaff-hill-maritime-museum, maritime-museum, shipwreck-coast, flagstaff-hill-maritime-village

This item is part of the Federation University Art Collection. The Art Collection features over 1000 works and was listed as a 'Ballarat Treasure' in 2007.Two stoneware clay with crystalline glaze forms with relief pattern on surface made from fabric impression.art, artwork, corolee asker, ceramics

8305.1 - Small opaque white flattened ovoid crystalline pebble showing rhomboidal cleavage planes typical of calcite.

Number of parts: 35. Box of 34 specimens (glass) of crystalline form 1 missing, used in crystal growth demonstration.

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

Email from "Heike Dansard"

William Lawrence Bragg was born in Adelaide in 1890. Lawrence was only fifteen years old when he started study at the University of Adelaide. In 1908 he graduated with a first-class honours degree in mathematics. He worked as a professor of physics at the University of Manchester in 1919-1938 and at Cambridge in 1938-54. He shared the Nobel Prize in 1915 with his father, Sir William Henry Bragg at the age of twenty-five "for their services in the analysis of crystal structure by means of X-rays". He died in Waldringfield, England, 1 July 1971. Red hardcovered book with black and white illustrations. At the top of title "The Crystalline State Vol. IV". 409pp [inkstamped name on front free endpaper]. The book discusses the Crystal structures of minerals, by Sir L. Bragg and G. F. Claringbull, with a chapter by W.H. Taylor.metallic crystal structures, sir lawrence bragg, g f claringbull, physics

Picrotoxin is a bitter crystalline compound derived from the seed of an East Indian woody vine (Anamirta cocculus). It is a central nervous system and respiratory stimulant formerly used in barbiturate and other anaesthetic poisonings. Hexagon shaped amber glass bottle with red rubber stopper. There is an ivory coloured manufacturer's label with black printed text adhered to the front of the bottle, along with some handwritten notations. The bottle has powdery contents.Handwritten on manufacturer's label: PURE FIRST USED 8/10/64 •Moulded into base of bottle: T195respitaroty stimulalnt, t and h smith, barbiturate poisoning, edinburgh, blandfield chemical works

Feldspathic arenites are sandstones that contain less than 90% quartz, and more feldspar than unstable lithic fragments, and minor accessory minerals.Feldspathic sandstones are commonly immature or sub-mature.These sandstones occur in association with cratonic or stable shelf settings. Feldspathic sandstones are derived from granitic-type, primary crystalline, rocks. If the sandstone is dominantly plagioclase, then it is igneous in origin Sandstone features prominently in public buildings throughout Victoria. Most of the sandstone used as dimension stone in the State came from three sources: the Heatherlie quarry in the Grampians (Silurian), the Bacchus Marsh area (Permian), and the Barrabool Hills near Geelong (Cretaceous).Sandstone features prominently in public buildings throughout Victoria, making this specimen special as it shows the materials used by Victorian building companies. Sandstone can also be crushed, crushed stone is used in the construction of roadways and road structures such as bridges, and in buildings, both commercial and residential. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study. A feldspar-rich sandstone, a sandstone intermediate in composition between an arkosic sandstone and a quartz sandstone, containing 10% to 25% feldspar and less than 20% matrix material of clay, sericite, and chlorite. Feldspathic arenite containing less than 90 percent of the composition of quartz. Feldspar is the main composition. Feldspathic arenite may contain fragments of unstable rock, and a little amount of other minerals such as mica and heavy minerals. Some feldspathic arenite have pink or red color because of the presence of potassium feldspar or iron oxide. There are also colored light gray to white. These sandstones are usually medium to coarse grained and can contain a high percentage of granules with angular until subangular roundness. The content of the matrix can appear as the rest up to more than 15 percent, and sorting of grains can present as moderate to poorly sorted. Feldspathic sandstones are generally immature in textural maturity. Feldspathic arenite can not be judged from the structure of the sediment. Bedding can emerge from the laminate parallel to the crossbed. Fossils may appear in the layer deposited on the sea. Feldspathic arenites usually appear on the craton or the continental shelf, which can be associated with conglomerate, quartz lithic arenite, carbonate rock, or evaporites. This sandstone may also appear on the succession of sedimentary basins deposited on an unstable or deep sea, and moving arc setting. According to Pettijohn (1963) Arkose make up about 15 percent of all sandstones. Some Arkose formed in situ when the granite and related rocks disintegrate and generate granular sediments. Most of the material feldspathic sandstones derived from primary crystalline granitic rocks, such as granite or metasomatic rocks containing abundant potassium feldspar. Mineral contained in sandstones is mostly a form of plagioclase feldspar derived from quartz diorite or volcanic rock. Feldspar contained on this sandstone comes from arid to cool climates when the chemical weathering process is reduced.sandstone, natural stone, feldspathic sandstone, burke museum, geology, geological, geological specimen

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

Penicillin is a group of antibiotics derived from Penicillium fungi, including penicillin G, procaine penicillin, benzathine penicillin, and penicillin V. Penicillin antibiotics are historically significant because they are the first drugs that were effective against many previously serious diseases, such as syphilis, and infections caused by staphylococci and streptococci. Penicillins are still widely used today, though many types of bacteria have now become resistant. All penicillins are β-lactam antibiotics and are used in the treatment of bacterial infections caused by susceptible, usually Gram-positive, organisms. The development of penicillin for use as a medicine is attributed to the Australian Nobel laureate Howard Walter Florey, together with the German Nobel laureate Ernst Chain and the English biochemist Norman Heatley A clear glass bottle with a metal fixed top in which the central rubber disc has been pierced by a needle .Front: CRYSTALLINE PENICILLIN / ( SODIUM SALT) G / GLAXO / FOR INJECTION / Use only under medical supervision / 1000000 / UNITS PER VIAL. Left side : Refrigeration unnecessary....MANFD. DEC. 1955 / EXPIRY DEC. 1958 / POTENCY 1667 / IU/MG / BATCH 269. Right side :Contains over 90% / penicillin G / Contains no preservatives / GLAXO LABORATORIES / (AUST.) PTY. LTD. / Melbourne Sydneypharmacy, medicines, penicillin, early settlers, market gardeners, moorabbin, bentleigh, cheltenham, manufactured glass, bottles, glaxo laboratories melbourne

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

Reference: American Journal of Pharmacy, volume 1, page 162. "So rapid is the progress of this change, that it is seldom we meet with the article in our shops which is not more or less injured by it. The first sign of the loss of alkali, is the efflorescence on the surface, which gradually extends till the whole crystalline mass is altered. It is from this cause that we have so much difficulty in pleasing those who are particular about the quality of their "smelling salts." A preparation, called " the Preston smelling salts," has within a few years been introduced from England, and has deservedly been much sought after. The manufacturers have wisely put it up in very wide mouthed bottles, which enable one to inhale a much larger quantity of ammonia at once, and thus increase the apparent strength of the salt. But it has other qualities to recommend it, than the manner in which it is put up for sale. It retains its odour for a longer time and wastes more slowly than the common smelling salts. It was generally believed, when the article was first brought here, that its superiority was owing to the sublimation being made at once into the bottle, so as to avoid any loss of ammonia by unnecessary exposure to the air. An examination, however, will satisfy any one that the salt is crystallized and not sublimed. The superior compactness and hardness of a crystalline over a sublimed salt, are great advantages in so volatile a substance as the carbonate of ammonia; and to this, I have no doubt the good qualities of the Preston salts are to be attributed. The salt may be crystallized with great facility in the winter season".Round squat clear glass bottle, wide neck with rough cut top, embossed text on side.'PRESTON SALTS' on side.smelling salts, preston salts

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

This specimen is a copper-carbonate malachite mineral. It is often found as crystalline aggregates or crusts, which have a banded agate-like appearance while also commonly found as botryoidal clusters of radiating crystals. Malachite is often bright green in colour, with dark green and blackish blooms or stripes/bands throughout the mineral. This particular specimen was recovered from the Burra Burra Copper Mine located Burra, South Australia. By the 1860's, South Australia was known as the "Copper Kingdom" due to its large amount of copper mines and huge success in the copper mining industry. Burra Burra was no exception to this phenomena, as this mining company was greatly famous and successful, being nicknamed the "Monster Mine". It was first established in 1848 and was the largest metal mine in Australia up until 1860. This specimen is significant as it highlights the historic use and value of malachite and the rarity of the mineral. Malachite is a rare gemstone which has been used in various ways historically. It has been cut and sculpted into beads for jewellery use as its rich colour and distinct yet unique patterns have made it a well sought after gemstone. Its' continued use over time only heightens the value and significance of this mineral.A hand-sized solid copper-carbonate hydroxide mineral specimen in shades of blue, green and copper tones throughout.MALACHITE / (Copper carbonite) / Locality: Burra, South Aust. | Malachite / Burra Burra / South Australia / (good specimen) / needs a wash / BBburke museum, burke museum collection, beechworth museum, beechworth, geological specimen, geological, mineral, mineraology, copper carbonate, malachite, burra burra mine, copper mining

Potassium permanganate is an inorganic chemical compound with the chemical formula KMnO4. Formerly known as permanganate of potash or Condy's crystals, it is a strong oxidizing agent. It dissolves in water to give intensely pink or purple solutions, the evaporation of which leaves prismatic purplish-black glistening crystals. c1859 London chemist Henry Bollmann Condy had an interest in disinfectants; he found that fusing pyrolusite with sodium hydroxide (NaOH) and dissolving it in water produced a solution with disinfectant properties. He patented this solution, and marketed it as 'Condy's Fluid'. Although effective, the solution was not very stable. This was overcome by using potassium hydroxide (KOH) rather than NaOH. This was more stable, and had the advantage of easy conversion to the equally effective potassium permanganate crystals. This crystalline material was known as 'Condy's crystals' or 'Condy's powder'. Potassium permanganate was comparatively easy to manufacture.A brown glass bottle with a red plastic topped cork stopper for 'Tromax' , 'Purple Crystals' ie Permanganate of Potash , that was used as an antiseptic and disimfectant.TROMAX BRAND / PURPLE CRYSTALS/ or Permanganate of Potash / (Poisonous )/ For Household and Medicinal Uses / 2oz. / TROMAX / A PRODUCT OF/ SIGMA Co.Ltd. / MANF. CHEMISTS / MELBOURNE. Directions for Use are on back of bottlepharmacy, medicines, tromax, purple crystals, permaganate of potash, disinfectants, sigma co.ltd. melbourne, athritis, glassware, bottles, moorabbin, bentleigh, cheltenham

Tourmaline specimens are members of a crystalline silicate mineral group based on boron but influenced by elements including aluminium, iron, magnesium, sodium, lithium, or potassium. Specimens present a wide variety of colours and forms according to the specific mix of these elements. Tourmalines are semi-precious gemstones with many applications, including commercial jewellery production. The word 'tourmaline' derives from the Sinhalese term for the carnelian or red-shaded specimens, "tōramalli". This specimen has been classified by geologists as 'Black Schoalou/Tourmaline in quartz'. Schoalou may equate to a common black-hued type of Tourmaline associated since around 1400 with mines in Saxony, Germany near a village called Schorl (today's Zchorlau). If this specimen is part of the 'Schorl' species of tourmaline it is a member of the most common group of Tourmalines, a divalent sodium ion influenced group accounting for 95% of specimens. On assessment, it was noted that the crossed lines (XIs) of this tourmaline have been fractured and rehealed by the quartz matrix in which the tourmaline rests. This item is significant as an example of its type of gemstone and the geological processes leading to its formation. A solid medium-sized piece of Black Schoalou/Tourmaline in a cream and peach coloured quartz matrix. Existing label: Black Schoalou / Tourmaline in / quartz. / Tourmalines XIs have / been fractured and / rehealed with / quartz / C. Willman / 15/4/21 /geological specimen, geology, geology collection, burke museum, beechworth, indigo shire, north-east victoria, tourmaline, quartz, boron, crystals, minerals, gemstones, semi-precious, black schoalou, zchorlau, schorl

New Zealand Greenstone, also called Pounamu is found on New Zealand’s South Island in riverbeds and boulders, and colours vary depending on the source, but always include green tones. It is a form of the mineral nephrite, also known as jade, and is a tough stone with a crystalline structure, made up of calcium magnesium and iron silicate. Its hardness means it is ideal for carving, and has been used for this purpose throughout history, especially by the Maori people of New Zealand. Greenstone features heavily in Maori mythology, and the traditional name for the South Island, Te-Wai-Pounamu, literally translates to waters of greenstone. Wearing of Greenstone pendants with different carvings is practiced by Maori to represent connection to land and ancestors, or to endow the wearer with certain attributes. The sticker on the base of the specimen identifies it as a product of Hokitika Jade Company. The company, which was active in the 1970s, sold jade and greenstone specimens and ornaments. Hokitika, which started life as an 1860s gold rush town, is the origin of most nephrite found in New Zealand, and the centre of the Greenstone carving industry. The object has scientific and research potential as part of the Burke Museum's Geology Collection, and as and example of New Zealand Greenstone. It also has spiritual significance for it's role in Maori beliefs and communities, where it is both traditionally worn and features in mythology. As a valuable stone regularly used in carving and jewellery, it has aesthetic significance. Sticker on base: "N.Z. Greenstone/ a product of/ Hokitika Jade Coy."geological specimen, geology, geology collection, burke museum, beechworth, new zealand, greenstone, hokitika, nephrite, jade

Malachite is a green copper carbonate hydroxide mineral and was one of the first ores used to make copper metal. Malachite has been utilised as a gemstone and sculptural material in the past as its distinctive green color does not fade when exposed to light or after long periods of time. Malachite is formed at shallow depths in the ground, in the oxidizing zone above copper deposits. The material has also been used as a pigment for painting throughout history. This particular specimen was recovered from the Burra Burra Copper Mine in Burra, South Australia. Otherwise known as the 'Monster Mine', the Burra Burra Copper Mine was first established in 1848 upon the discovery of copper deposits in 1845. Within a few short years, people from around the world migrated to Burra to lay their claim in the copper economy. By April 1848 the mine was employing over 567 people and supporting a population of 1,500 in the local township. Up until 1860, the mine was the largest metals mine in Australia, producing approximately 50,000 tonnes of copper between 1845 to its closure in 1877. The Burra Burra Mine was also famous for a number of other specimens, including; crystalline azurite, cuprite, and botryoidal and malachite.Malachite is considered a rare gemstone in that the original deposits for the stones have been depleted leaving behind very few sources. In addition, the use of Malachite as gemstones and sculptural materials remains just as popular today as they were throughout history. It is quite common to cut the stone into beads for jewellery. The fact that Malachite has such a rich colour and one that does not fade with time or when exposed to light makes it particularly rare. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study. A solid hand-sized copper carbonate hydroxide mineral with shades of yellow, blue, and light green throughout.geological, geological specimen, burke museum, indigo shire, malachite, malachite specimen, burra burra mine, burra, south australia, australian mines, mines, monster mine

During prestige, long distance train journeys some carriages had air-conditioning, and the majority of passengers had to brave unheated carriages. To offer some comfort during the winter months, the non-air-conditioned carriages were provided with footwarmers. These were metal containers roughly 100 mm thick and 300 mm wide, and about 750 mm long, which were filled with salt crystals (concentrated crystalline hydrated sodium acetate). The footwarmers were covered by sleeves of thick canvas, and two footwarmers were usually placed in each compartment of non-air-conditioned carriages. To activate the chemicals, the footwarmers were heated almost to boiling point. This was done by removing the canvas sleeves and placing the footwarmers in a large bath of very hot water. After they had been heated, they were removed from the bath and the sleeves refitted. They were then ready to be placed in the carriages. The McLaren patent foot warmer was used on railways in New South Wales, Queensland, Victoria and South Australia as well as South Africa and New Zealand. It was during the 1901 royal visit by the Duke and Duchess of Cornwall that these foot warmers were first used in New Zealand in the royal carriage. Before railway carriage heating was introduced, McLaren patent foot warmers were placed on the floor of New South Wales government railway carriages from 1891 to provide a little passenger comfort. The rectangular steel container worked a bit like a hot water bottle but instead of water contained six and a half kilograms of loosely-packed salt crystals, (concentrated crystalline hydrated sodium acetate). This was permanently sealed inside the container with a soldered cap. After the foot warmer was heated in vat of boiling water for about one and a quarter hours the crystals became a hot liquid. (The melting point for sodium acetate is 58 degrees). There was a whole infrastructure of special furnaces set up at stations for the daily heating of foot warmers. By 1914 the Victorian railways had 4,000 foot warmers in service and by 1935 there were 33 furnaces at principal stations to heat them. After about 10 hours the container was picked up by the handle and given a good vertical shake which helped the cooled liquid reform into a solid mass of hot crystals. Staff or sometimes passengers shook them en route when the foot warmers began to get cold. However, as they were heavy this was only possible by fit and agile passengers. At the end of the journey the containers were boiled again for reuse on the next trip. Sodium acetate railway foot warmers were introduced in Victoria in 1889, Adelaide to Melbourne express in 1899. "Shaking up" on this service took place at Murray Bridge and Stawell on the tip to Melbourne and at Ballarat and Serviceton on the trip to Adelaide. The use of foot warmers began to decline in New South Wales from the 1930s with the first trial of carriage air-conditioning in 1936, steam heating from 1948 ad LP gas heating from 1961. By the early 1960s the main services using foot warmers were the overnight mail trains. info from : http://www.powerhousemuseum.com/collection/database/?irn=67564#ixzz4UBNzVf6t Under Creative Commons License: Attribution Non-Commercial There was a whole infrastructure set up at stations for the daily heating of foot warmers in special furnaces. In Victoria alone in 1935 there were 33 heating works.Historic - Victorian Railways - Carriage Heater - Foot warmerA rectangular-shaped stainless steel casing with a welded seam down the back and welded ends. There is a handle at one end for carrying and shaking. Inside the foot warmer are two baffle plates and three trays to contain the sodium acetate. There was a cast-iron ball in each internal compartment. puffing billy, victorian railways, carriage haeter, foot warmer, passenger comfort, station furnace, railway ephemera, early heating methods

This crucible was raised from the wreck of the Loch Ard. It is one of six similar relics, in a range of sizes, now in the Flagstaff Hill collection. All were manufactured by the Morgan brothers who founded the Patent Plumbago Crucible Company in 1856, making crucibles in a small factory in Battersea London. A crucible is a container used for purifying and melting metals so that they can be cast in a mold to a predetermined shape and use. They must withstand extremely high temperatures, abrupt cooling, and shed their contents with minimal adherence. The addition of graphite to the traditional firing clays greatly enhanced the durability of industrial crucibles this technique was pioneered by the Morgan Bros thereby making a significant technological advance in foundry technology and metallurgy. The Morgans first noticed the advantages of graphite crucibles at the Great Exhibition held in London in 1851. Initially, they contracted to be sole selling agents for the American-made products of Joseph Dixon and Co. from New Jersey, but in 1856 they obtained that firm's manufacturing rights and began producing their graphite crucibles from the South London site. The Morgans imported crystalline graphite in 4-5 cwt casks from the British colony of Ceylon (now Sri Lanka) and mixed it with conventional English (Stourbridge) clays to be fired in kilns. Their products were purchased by the Royal Mints in London and India and exported to official mints in France and Germany. They were successful exhibitors of their crucibles and furnaces at the London Exhibition held in 1861 (Class 1, Mining, quarrying, metallurgy and mineral products, Exhibit 265, Patent Plumbago Crucible Co). The range of sizes represented by the six crucibles retrieved from the Loch Ard suggests they may have been part of a sample shipment intended for similar promotion in the Australian colonies or at Melbourne's International Exhibition to be held in 1880. A newspaper account of an 1864 tour of the Morgan brothers' 'Black Potteries' at Battersea indicates: "All the pots were numbered according to their contents, each number standing for one kilogram, or a little over two pounds; a No. 2 crucible contains two kilograms; a No. 3, three kilograms, and so on." These numbers are obscured by marine sediment on three of the crucibles in the Flagstaff Hill collection, but those legible on the remaining three are 5, 6, and 8. None of the six is of the same size. (For more information on the Loch Ard wreck see note sec this document) The shipwreck of the Loch Ard is of significance for Victoria and is registered on the Victorian Heritage Register ( S 417). Flagstaff Hill has a varied collection of artefacts from Loch Ard and its collection is significant for being one of the largest accumulation of artefacts from this notable Victorian shipwreck of which the crucible is a small part. The collections objects give us a snapshot of how we can interpret the story of this tragic event. The collection is also archaeologically significant as it represents aspects of Victoria's shipping history that allows us to interpret Victoria's social and historical themes of the time. Through is associated with the worst and best-known shipwreck in Victoria's history.A medium size crucible, or fluxing pot, for heating and pouring molten metal. The container rises in a slight curve from a smaller flat base to a wider open top with a lip for pouring. It was recovered from the wreck of the LOCH ARD. The crucible has a coating of sediment that obscures its numerical specifications of size and capacity. The markings that remain visible indicate it is a Morgan’s crucible, made with graphite to prevent cracking and provide a smooth non-adhesive inner surface. .On base: “…ORGAN’S …ENT”flagstaff hill, warrnambool, flagstaff-hill-maritime-museum, shipwreck-coast, flagstaff-hill-maritime-village, graphite crucible, plumbago crucible, morgan's crucible company, loch ard, morgan potteries, crucible, fluxing pot

This crucible was raised from the wreck of the LOCH ARD. It is one of six similar relics, in a range of sizes, now in the Flagstaff Hill collection. All bear markings to indicate their manufacture by the Morgan brothers of Battersea, trading as the Patent Plumbago Crucible Co. A crucible is a container used for purifying and melting metals so that they can be cast in a mould to a predetermined shape and use. They must withstand extremely high temperatures, abrupt cooling, and shed their contents with minimal adherence. The addition of graphite to the traditional firing clays greatly enhanced the durability of industrial crucibles in mid-Victorian Britain, a significant technological advance at a time of great activity in foundries and expansion of demand for refined metals. The Morgans first noticed the advantages of graphite crucibles at the Great Exhibition held in London in 1851. Initially they contracted to be sole selling agents for the American-made products of Joseph Dixon and Co. from New Jersey, but in 1856 they obtained that firm’s manufacturing rights and began producing their own graphite crucibles from the South London site. The Morgans imported crystalline graphite in 4-5 cwt casks from the British colony of Ceylon (now Sri Lanka) and mixed it with conventional English (Stourbridge) clays to be fired in kilns. Their products were purchased by the Royal Mints in London and India, and exported to official mints in France and Germany. They were successful exhibitors of their crucibles and furnaces at the London Exhibition held in 1861 (Class 1, Mining, quarrying, metallurgy and mineral products, Exhibit 265, Patent Plumbago Crucible Co). The range of sizes represented by the six crucibles retrieved from the LOCH ARD, suggest they may have been part of a sample shipment intended for similar promotion in the Australian colonies ― at Melbourne’s International Exhibition to be held in 1880. The summary of cargo manifest, by Don Charlwood in ‘Wrecks and Reputations’ does not mention any crucibles, implying that they were not a large consignment of uniform items. A newspaper account of an 1864 tour of the Morgan brothers’ ‘Black Potteries’ at Battersea indicates: “All the pots were numbered according to their contents, each number standing for one kilogram, or a little over two pounds; a No. 2 crucible contains two kilogrammes; a No. 3, three kilogrammes, and so on.” These numbers are obscured by marine sediment on three of the crucibles in the Flagstaff Hill collection, but those legible on the remaining three are 5, 6, and 8. None of the six are of the same size from a visual appraisal.The shipwreck of the LOCH ARD is of State significance ― Victorian Heritage Register S417A large crucible, or fluxing pot, for heating and pouring molten metal. It was recovered from the wreck of the LOCH ARD. The clay fired vessel rises from circular flat base to a larger rim with pouring lip. It is stained a rust colour and bears some sedimentary accretion. Half of its loose fitting lid with central knob has also survived. Markings on the artefact indicate it is a Morgan’s crucible, made with graphite to prevent cracking in the furnace and provide a smooth (non-adhesive) inner surface. On base: “…RGAN’S PATENT CRUCIBLE”. On rim: “MORGAN’S PATENT P…” Below top edge "BAK"flagstaff hill, warrnambool, shipwrecked-coast, flagstaff-hill, flagstaff-hill-maritime-museum, maritime-museum, shipwreck-coast, flagstaff-hill-maritime-village, graphite crucible, plumbago crucible, morgans crucible company, loch ard, fluxing pot, crucible

This crucible was raised from the wreck of the LOCH ARD. It is one of six similar relics, in a range of sizes, now in the Flagstaff Hill collection. All bear markings to indicate their manufacture by the Morgan brothers of Battersea, trading as the Patent Plumbago Crucible Co. A crucible is a container used for purifying and melting metals so that they can be cast in a mould to a predetermined shape and use. They must withstand extremely high temperatures, abrupt cooling, and shed their contents with minimal adherence. The addition of graphite to the traditional firing clays greatly enhanced the durability of industrial crucibles in mid-Victorian Britain, a significant technological advance at a time of great activity and expansion in foundries and demand for refined metals. The Morgans first noticed the advantages of graphite crucibles at the Great Exhibition held in London in 1851. Initially they contracted to be sole selling agents for the American-made products of Joseph Dixon and Co. from New Jersey, but in 1856 they obtained that firm’s manufacturing rights and began producing their own graphite crucibles from the South London site. The Morgans imported crystalline graphite in 4-5 cwt casks from the British colony of Ceylon (now Sri Lanka) and mixed it with conventional English (Stourbridge) clays to be fired in kilns. Their products were purchased by the Royal Mints in London and India, and exported to official mints in France and Germany. They were successful exhibitors of their crucibles and furnaces at the London Exhibition held in 1861 (Class 1, Mining, quarrying, metallurgy and mineral products, Exhibit 265, Patent Plumbago Crucible Co). The range of sizes represented by the six crucibles retrieved from the LOCH ARD, suggest they may have been part of a sample shipment intended for similar promotion in the Australian colonies ― at Melbourne’s International Exhibition to be held in 1880. A summary of the LOCH ARD cargo manifest, by Don Charlwood in ‘Wrecks and Reputations’ does not mention any crucibles, implying that they were not part of a larger consignment of uniform items. A newspaper account of an 1864 tour of the Morgan brothers’ ‘Black Potteries’ at Battersea indicates: “All the pots were numbered according to their contents, each number standing for one kilogram, or a little over two pounds; a No. 2 crucible contains two kilogrammes; a No. 3, three kilogrammes, and so on.” These numbers are obscured by marine sediment on three of the crucibles in the Flagstaff Hill collection, but those legible on the remaining three are 5, 6, and 8. None of the six are of the same size from a visual appraisal. The shipwreck of the LOCH ARD is of State significance ― Victorian Heritage Register S417A No. 6 size Morgan’s graphite crucible (i.e. 6kgs capacity). The crucible rises in a slight curve from a smaller flat base up to a wider top with a (chipped) pouring lip. It was recovered from the wreck of the LOCH ARD. The artefact is largely accretion free despite its long period of submersion at the wreck site. It has a number of visible maker’s markings which identify the manufacturer and the smelting capacity of the pot. The graphite crucible is in fair and stable condition. The number “6” which is framed in a square. The letters “THE PATENT PLUMBAGO CRUCIBLE COMPANY” and “BATTERSEA WORKS COMPANY”. Below rim "... GNS"flagstaff hill, warrnambool, shipwrecked-coast, flagstaff-hill, flagstaff-hill-maritime-museum, maritime-museum, shipwreck-coast, flagstaff-hill-maritime-village, graphite crucible, plumbago crucible, morgan's crucible company, loch ard, crucible, fluxing pot