Showing 98 items matching "mineral specimen"
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The Beechworth Burke MuseumGeological specimen - Rhodonite with Galena and Sphalerite
... ...mineral specimen...Rhodonite is an uncommon mineral once used as an ore of manganese in India, however today the scarcity and fragility of the crystals mean it is primarily used as lapidary materials or mineral specimens. ...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. ...This specimen is from Broken Hill, NSW. Galena is a natural mineral form of lead sulphide and is often found associated with sphalerite, calcite, and fluorite. Galena is an important lead ore mineral, and, in some regions, it is also an important mineral associated with silver ore. Sphalerite is a sulphide mineral that is the main ore of zinc. Rhodonite is an uncommon mineral once used as an ore of manganese in India, however today the scarcity and fragility of the crystals mean it is primarily used as lapidary materials or mineral specimens. In 1883, Charles Rasp who was a boundary rider at the time, discovered what he thought were deposits of tin but were in fact samples of silver and lead. He and six others went on to set up the first mining company in Broken Hill (BHP). The ore body became the largest and richest of its kind in the world mining ore worth more than 42,000 pounds in its first year. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study. Galena contains lead and silver, Sphalerite contains zinc. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A hand-sized piece of Sphalerite and Galena with Rhodonite crystalsburke museum, beechworth, geological, geological specimen, galena, rhodonite, sphalerite, silver ore, manganese, lead sulphide, lead ore, zinc ore, lapidary, mineral specimen, broken hill, nsw -
The Beechworth Burke MuseumGeological specimen - Mangan Hedenbergite
... specimen was recovered from Broken Hill, NSW. It was given the name Mangan Hedenbergite in 1819 by Jöns Jakob Berzelius in honor of Mr. Anders Ludvig of Hedenberg who was the first to define hedenbergite as a mineral. ...A hand-sized mineral specimen in shades of silver and black...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. ...This specimen was recovered from Broken Hill, NSW. It was given the name Mangan Hedenbergite in 1819 by Jöns Jakob Berzelius in honor of Mr. Anders Ludvig of Hedenberg who was the first to define hedenbergite as a mineral. Hedenbergite, belongs in the pyroxene group having a monoclinic crystal system. The mineral is extremely rarely found as a pure substance. Mangan Hedenbergite is a manganese bearing variety of Hedenbergite. Manganese is the world’s fourth most used mineral after iron, aluminium, and copper primarily because it has no satisfactory substitute in its major applications. Globally, the steel industry is the primary user of manganese metal, utilizing it as an alloy to enhance the strength and workability of steel and in the manufacture of tin cans. Manganese is a key component of certain widely used aluminium alloys and, in oxide form, dry cell batteries used in electric vehicles. These batteries are in high demand. Another potential use for manganese may as an additive to help coat and protect a car’s engine. Manganese is also used for non-metallurgical purposes such as plant fertilizers, animal feed, and colorants for bricks. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A hand-sized mineral specimen in shades of silver and blackmanganese, open cut mine, manganese ore processing, bell bay, tasmania, northern territory, steel industry, zinc-carbon batteries, alkaline batteries, tin cans -
The Beechworth Burke MuseumGeological specimen - Olivine with Chromian diopside (dark green), Unknown
... The luster of the specimen is vitreous, the luminescence non-fluorescent and when fractured the mineral is very brittle producing small, conchoidal fragments. ...A solid mineral specimen in shades of green, grey and brown...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. ...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 -
The Beechworth Burke MuseumGeological specimen - Malachite, Unknown
... Specimen...Geological...Mineral...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. ...A hand-sized solid copper-carbonate hydroxide mineral specimen in shades of blue, green and copper tones throughout....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. ...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 -
The Beechworth Burke MuseumGeological specimen - Native Sulphur, unknown
... 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...A solid, small, crystalline mineral specimen that is largely bright yellow, with some darker spotting. ...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. ...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 -
The Beechworth Burke MuseumGeological specimen - Opal Bearing Stone, Unknown
... ***A palm-sized solid mineral specimen in shades of beige and light orange*** silica based? ...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. ...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 -
The Beechworth Burke MuseumGeological specimen - Calcite crystals
... mineral that scratches easily and is often found colourless or with a cream/white shade but may show up in colours such as red, yellow, green, and violet. In sedimentary rocks calcite is often found in the form of invertebrate shells, making it an important biomineral. Calcite is used in many industries such as farming, building, and medicine. This particular specimen...A small sized calcium, carbon and oxygen made mineral specimen in shades cream and grey...Calcite Mineral Limestone Marble Sedimentary Invertebrate Shells Biomineral Farming Medicine Broken Hill Broken Hill Mine New South Wales Charles Rasp Syndicate of Seven Volcanic Activity Black Sulphide Precipitates Calcite Crystals Beechworth Museum Indigo Shire Beechworth A small sized calcium, carbon and oxygen made mineral specimen in shades cream and grey Geological specimen Calcite crystals ...Calcite is a common mineral and is found worldwide due to it being a primary component of many other rocks such as limestone and marble. It is a softer mineral that scratches easily and is often found colourless or with a cream/white shade but may show up in colours such as red, yellow, green, and violet. In sedimentary rocks calcite is often found in the form of invertebrate shells, making it an important biomineral. Calcite is used in many industries such as farming, building, and medicine. This particular specimen was found at Broken Hill mine in Broken Hill, New South Wales, Australia. Broken Hill mine is one of the largest mines working silver and lead in Australia and at its peak employed 6500 staff across 7.5km long of land. The site was founded in 1883 by Charles Rasp, where Rasp and 6 other men from various backgrounds came together to form the first BHP mine. It has become one of the most popular mining sites due to its abundance and longevity. The ore body was created 1685 million years ago due to volcanic activity causing heated seawater to flow up through the seafloor where it mixed with the cold water creating black sulphide precipitates. These then settled back onto the seafloor forming sediment layers rich in minerals. Over time the land eroded until it was discoverable by humans.Historically this specimen is significant due to the origin of its location. Broken Hill mine has a long history in both its location and its findings and has resulted in a variety of minerals being discovered at its site. It is beneficial in the understanding of the Australian landscape over millions of years. Due to its properties, calcite today is used in a multitude of different industries such as agriculture, construction, medicine, and farming.A small sized calcium, carbon and oxygen made mineral specimen in shades cream and greycalcite, mineral, limestone, marble, sedimentary, invertebrate shells, biomineral, farming, medicine, broken hill, broken hill mine, new south wales, charles rasp, syndicate of seven, volcanic activity, black sulphide precipitates, calcite crystals, beechworth museum, indigo shire, beechworth -
The Beechworth Burke MuseumGeological specimen - Laterite
... a palm-sized solid iron-aluminium oxide mineral specimen in shades of brown, orange and grey...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. ...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 -
The Beechworth Burke MuseumGeological specimen - Tourmaline (schorl), Unknown
... Tourmaline specimens from Beechworth, Victoria, Australia, are a notable part of the region's mineral heritage. ...A hand-sized solid mineral specimen in shades of brown, green, light grey and dark grey...Tourmaline specimens from Beechworth have educational significance, providing opportunities for research and study. They offer insights into the geological processes and mineral formation in the region, contributing to a better understanding of Earth's geological history. burke museum beechworth indigo shire geological geological specimen mineralogy tourmaline TOURMALINE (schorl) / (Silicate of boron and aluminum) A hand-sized solid mineral specimen in shades of brown, green, light grey and dark grey Geological specimen Tourmaline (schorl) ...Tourmaline is a group of minerals belonging to the complex borosilicate mineral class. These minerals are known for their striking and varied colours, making them prized gemstones. Tourmaline crystals can come in various shades, including pink, green, blue, brown, black, and colourless. They are often transparent or translucent. Tourmaline's chemical composition is complex, but it typically includes elements such as aluminium, iron, magnesium, sodium, lithium, and potassium. The specific arrangement of these elements in the crystal lattice gives rise to the different colours and properties of tourmaline specimens. Tourmaline specimens from Beechworth, Victoria, Australia, are a notable part of the region's mineral heritage. These tourmalines are of interest to mineral collectors and enthusiasts. While the tourmaline found in Beechworth is not as well-known as some other tourmaline varieties, it has unique characteristics and a historical context associated with the gold mining areas in Beechworth.The significance of tourmaline in Beechworth, Victoria, Australia, lies in its unique geological and historical context, contributing to both scientific and cultural aspects. The tourmaline mined in Beechworth is a rare and unique variety of tourmaline that is primarily found in the historic gold mining areas surrounding Beechworth. Its occurrence is closely linked to the geological processes that shaped the region during the Gold Rush era. The discovery of tourmaline in Beechworth adds to the rich mineral heritage of the area, which was historically known for gold mining. The specimens serve as a tangible connection to the region's mining history and contribute to preserving its geological legacy. The presence of tourmaline in Beechworth showcases the mineralogical diversity of the area. Tourmaline is known for its wide range of colours and unique properties, making it a valuable subject of study for mineralogists and geologists. Tourmaline specimens from Beechworth have educational significance, providing opportunities for research and study. They offer insights into the geological processes and mineral formation in the region, contributing to a better understanding of Earth's geological history.A hand-sized solid mineral specimen in shades of brown, green, light grey and dark greyTOURMALINE (schorl) / (Silicate of boron and aluminum) burke museum, beechworth, indigo shire, geological, geological specimen, mineralogy, tourmaline -
The Beechworth Burke MuseumGeological specimen - Amazonite, unknown
... A palm-sized Feldspar mineral specimen from the Tectosilicate class in shades of blue-green with white veining....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. ...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 -
Federation University Historical CollectionBook - Report Register, Ballarat School of Mines Monthly Reports, 1918-1929, 1918-1929
... ...primock mineral specimen donation...Barker Library (top floor) Mount Helen goldfields plaster casts letter letterbook ballarat school of mines monthly reports principals reports world war one student involvement in world war one aboriginal male skeleton ralph g. moore robert a. clinton ralph ingram moore japanese warship officers visit c.h. vale g.d. evans geoffrey ballantyne tundbridge w.j. paterson new guinea mica smith schola mica smith scholarship nolrfolk island pine primock mineral specimen donation e. duncan e.j. mcconnon j.r. gordon j.c. molloy j.c. molloy death c. fenner h.h. smith w.h. collyer a.f. tweedie colin brittain australian mining corp w.h. clutterbuck a.l. ronaldson thomas hurley j.c. hurley alan t. perry wolfrey henry clutterbuck miss abrams' commercial classes norman barker australian flying corps l.h. vernon h.c. smith rowland c. valentine repatriation department returned soldiers t.h. shattock returned soldiers league ina smith john keith caledonian society w.g. coates percival j. ripper s.h. mayo fees in arrears j.b. robinson bannerman stenotype machine influenza ruby lonie Pharmacy Ballarat E.G. ...Ledger monthly reports from the Registrar to the Ballarat School of Mines Council. Information includes student numbers, new enrolments, financial reports, reports of Council member and staff deaths. 1915 World War One Staff Enlistments. 1916 Advertisement for Teaching Positions 1917 Enlistment of Colin C. Brittain to the 'Miners' and Engineers'. 1919 Pg 75 - Low student numbers due to the influenza pandemic (Spanish Flu) Pg 76 - Ruby Lonie suffering from influenza (Spanish Flu). 1922 * Page 146 Plaster casts from Victoria & Albert Museumplaster casts, letter, letterbook, ballarat school of mines, monthly reports, principals reports, world war one, student involvement in world war one, aboriginal male skeleton, ralph g. moore, robert a. clinton, ralph ingram moore, japanese warship officers visit, c.h. vale, g.d. evans, geoffrey ballantyne tundbridge, w.j. paterson, new guinea, mica smith schola, mica smith scholarship, nolrfolk island pine, primock mineral specimen donation, e. duncan, e.j. mcconnon, j.r. gordon, j.c. molloy, j.c. molloy death, c. fenner, h.h. smith, w.h. collyer, a.f. tweedie, colin brittain, australian mining corp, w.h. clutterbuck, a.l. ronaldson, thomas hurley, j.c. hurley, alan t. perry, wolfrey henry clutterbuck, miss abrams' commercial classes, norman barker, australian flying corps, l.h. vernon, h.c. smith, rowland c. valentine, repatriation department, returned soldiers, t.h. shattock, returned soldiers league, ina smith, john keith, caledonian society, w.g. coates, percival j. ripper, s.h. mayo, fees in arrears, j.b. robinson, bannerman, stenotype machine, influenza, ruby lonie, pharmacy, ballarat, e.g. vawdry, annie a. jones, lancelot austin, l. stg. p. austin, spanish flu, rubie lonie, pandemic -
Tarnagulla History ArchivePhotographic copy of Intercolonial Exhibition certificate, won by Tarnagulla Borough Council, c.1866-1867
... Black and white photograph being a copy of an Intercolonial Exhibition certificate, won by Tarnagulla Borough Council for mineral specimens...This photograph is a black and white copy created from a colour original. tarnagulla awards mining mineralogy intercolonial exhibition borough council Black and white photograph being a copy of an Intercolonial Exhibition certificate, won by Tarnagulla Borough Council for mineral specimens Photographic copy of Intercolonial Exhibition certificate, won by Tarnagulla Borough Council ...Murray Comrie Collection. This photograph is a black and white copy created from a colour original.Black and white photograph being a copy of an Intercolonial Exhibition certificate, won by Tarnagulla Borough Council for mineral specimenstarnagulla, awards, mining, mineralogy, intercolonial exhibition, borough council -
The Beechworth Burke MuseumGeological specimen - Native (metallic) copper, Unknown
... Specimen...Geological...Mineral...A small, palm-sized solid native copper mineral specimen with shades of browns, black and rustic tones throughout the specimen....Beechworth Burke Museum Geological Specimen Native Specimen Geological Mineral mineralogy indigo shire Beechworth Museum copper copper ore NATIVE (metalic) COPPER / Locality: Moonta, South Australia A small, palm-sized solid native copper mineral specimen with shades of browns, black and rustic tones throughout the specimen. ...This specimen is a native copper specimen that is metallic. Copper is typically found in the earth's crust and is often found alongside other metals such as gold, zinc, lead and silver which all belong to the same group which is the Copper/Gold group. Copper is most commonly formed from large masses of molten lava rock which has solidified in the earth's crust and over time though different sizes and speeds of crystal growth has turned into large amounts of copper, stored in porphyry copper deposits. Copper has a distinctive colour, yet can sometime appear blue and greenish which is often caused by oxidisation or a mixture of copper and other metals. This specific specimen was recovered from Moonta, South Australia. The Moonta Mining Company was established in 1861, after a Shepard in the area noticed traces of copper. This lead to a rush in the copper mining industry which was relatively young in Australia at the time, making Moonta Mining Company one of the richest in Australia. By the 1860's, South Australia had been nicknamed the "Copper Kingdom" due to its vast amount of Large copper mines and resources. As of 2016, Australia was the second largest producer of Copper internationally, following behind Chile in first place. This copper specimen is significant historically and scientifically as it is such an important metal commonly used throughout the world in various ways. Copper is an invaluable recourse used in daily life, used in most electrical appliances as it is a great conductor of heat and electricity, as well as being soft and malleable, making it easy to bend and mould into delicate sheets and wires. Copper does not corrode and is therefore used in the production of water pipes among countless other significant necessities that are often overlooked in our society. Historically, Copper holds great significance as it was the first metal used by humans. It was discovered roughly 9000 years ago and was utilised by the Neolithic Man who learnt that heating the metal made it more malleable, thus tools and utensils were made which were far superior to the previous stone tools used by humans. This history and its connection to the current and ongoing relationship between humans and copper must be preserved and highlighted as it is integral to the history of all humankind. A small, palm-sized solid native copper mineral specimen with shades of browns, black and rustic tones throughout the specimen.NATIVE (metalic) COPPER / Locality: Moonta, South Australiabeechworth, burke museum, geological specimen, native specimen, geological, mineral, mineralogy, indigo shire, beechworth museum, copper, copper ore -
The Beechworth Burke MuseumGeological specimen - Common Opal, Unknown
... 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. ...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. ...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 -
The Beechworth Burke MuseumGeological specimen - Ventifact (wind- or ice-shaped) pebble
... A hand-sized solid mineral specimen in shades of dark and light browns with light lines visible in all configurations and a groove on configuration 2....This specimen was among those donated to the Burke Museum in 1868. burke museum beechworth geological geological specimen ventifact antarctic region antarctic Alfred Richard Cecil Selwyn Alfred Selwyn wind direction wind strength abraders wind flow climate change reconstruction of wind flow conditions weather change Mars light lines visible in all configurations and a groove on configuration 2 A hand-sized solid mineral specimen in shades of dark and light browns with light lines visible in all configurations and a groove on configuration 2. ...Ventifacts are sand-blasted rocks that are typically faceted and often display parallel grooves carved by wind-blown sand. They are useful indicators of wind direction and strength in environments such as deserts, mountains, and coastal areas because they are usually not hidden by later sediment, soil or vegetation cover. In Antarctica ventifaction is strongly related to the composition or type of rock. Ventifacts are important because they provide evidence for abraders such as sand, dust or snow and ice crystals, and offer a unique understanding of past wind processes that are effective in the reconstruction of past wind flow conditions and can provides clues to weather and climate changes in the past. Interestingly ventifacts have also been found on the surface of Mars. They were a threat to the NASA rover due to the sharp angles of the facets, created by the Martian wind over the course of millions of years. These Martian ventifacts act like weathervanes for past wind and weather patterns on the red planet in a similar manner to those found on earth.The Geological Survey of Victoria was instigated in response to the Victorian Gold Rush which began around 1851 in the Beechworth, Castlemaine, Daylesford, Bendigo and Ballarat areas. The survey was conducted by Alfred Richard Cecil Selwyn from his arrival in December 1852 until his resignation in 1869and during this time he trained many notable geologists, e.g. Aplin, Wilkinson, Daintree, who went on to other State survey senior positions. This specimen was among those donated to the Burke Museum in 1868.A hand-sized solid mineral specimen in shades of dark and light browns with light lines visible in all configurations and a groove on configuration 2.light lines visible in all configurations and a groove on configuration 2burke museum, beechworth, geological, geological specimen, ventifact, antarctic region, antarctic, alfred richard cecil selwyn, alfred selwyn, wind direction, wind strength, abraders, wind flow, climate change, reconstruction of wind flow conditions, weather change, mars -
The Beechworth Burke MuseumGeological specimen - Ropy Lava
... mineral...Geological Specimen...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. ...‘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 -
The Beechworth Burke MuseumGeological specimen - Porphyritic Rhyodacite
... A solid, dark grey mineral specimen with pale terracotta coloured inclusions. ...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. ...This specimen was recovered from the Nigretta Falls (previously named the Upper Wannon Falls), Victoria. The falls are fed by the Wannon River that has its head waters in the Grampians mountains. Approx. 10km upstream of the Wannon Falls, Nigretta is a multi-channel segmented cascade of smaller drops and bounces guided by patterns of joints in a much older (Devonian) rhyolitic volcanic rock. Both the Wannon and Nigretta Falls are iconic landscape features, entrenched in the history and identity of the region. These falls are particularly rare as they are the product of volcanic activity, which is unique in the context of the Volcanic Plain of Victoria. Waterfalls of this capacity are generally associated with the Uplands areas of Victoria, rather than the edges of the Volcanic Plain. 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, dark grey mineral specimen with pale terracotta coloured inclusions. Rhyodacite is a volcanic rock intermediate in composition between dacite and rhyolite. Rhyodacites form from rapid cooling of lava relatively rich in silica and low in alkali metal oxides.GEOLOGICAL SURVEY / R / S 55 FELSTONE PORPHYburke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, porphyritic rhyodacite, lava, nigretta falls, upper wannon falls, dacite, rhyolite, volcanic geology -
The Beechworth Burke MuseumGeological specimen - Ilvaite
... mineral...ilvaite...ilvaite specimen...Given that Ilvaite is not commonly found in Australia, it marks a unique contribution to an Australian collection of minerals. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. ...Ilvaite has acquired its name from Ilva (Latin for Elba) Island, Greece, where Ilvaite is most commonly found. The geological setting in which Ilvaite occurs is through contact with magnetite, zinc and copper ore deposits, along with contact metamorphic deposits and zeolite zones. llvaite crystallizes in the form of black prismatic crystals and columns . This specimen was retrieved from Broken hill, known as the world's richest and largest zinc-lead ore deposit. Because of Ilvaite's often unaesthetic crystal formations compared to other minerals, Ilvaite is uncommon in most rock collections, particularly specimens that are not well formed, such as this one. Ilvaite is also a member of the Sorosilicate subclass of the silicate minerals, which have an unusual basic unit of Si2O7, making Ilvaite a unique mineral. Given that Ilvaite is not commonly found in Australia, it marks a unique contribution to an Australian collection of minerals. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A solid hand-sized ferrous iron analogue mineral with of black with shades of beige Ilvaite is a brittle, opaque rock formation that has acquired its name from Ilva (Latin for Elba) Island, Greece, where Ilvaite is most commonly found. The geological setting in which Ilvaite occurs is through contact with magnetite, zinc and copper ore deposits, along with contact metamorphic deposits and zeolite zones. llvaite crystallizes in the form of black prismatic crystals and columns rock, mineral, ilvaite, ilvaite specimen -
The Beechworth Burke MuseumGeological specimen - Garnet crystals in galena, Unknown
... ...Geological Specimen...Mineral...mineral form of lead sulfaide. It occurs generally as fine to large crystals due to syntectonic remobilization at low temperatures and moves to a suitable location. The colour is a shining lead and silvery gray with high specific gravity between 7.2 and 7.6 gms/cm3 and contains 86.6 lead sulfaide in its purest form. Its cyrstal system is cubic with perfect cleavages, and contract penetration and lamellar twinning. This particular specimen... is rare for examples of Australian Galena. This mineral specimen is one part to a larger collection, aquistion, and distribution of Garnet in Galena around Australia and parts of the world and donated to the Burke Museum between 1860-1880. ...Majority of Galena in Australia is found in hydrothermal deposits emplaced around 1680 million years ago which have been heavily metamorphosed. Galena is the natural mineral form of lead sulfaide. It occurs generally as fine to large crystals due to syntectonic remobilization at low temperatures and moves to a suitable location. The colour is a shining lead and silvery gray with high specific gravity between 7.2 and 7.6 gms/cm3 and contains 86.6 lead sulfaide in its purest form. Its cyrstal system is cubic with perfect cleavages, and contract penetration and lamellar twinning. This particular specimen is from the Broken Hill mine, it is one of the largest lead mines located in Western New South Wales and still has ore reserves amounting to 20.9 million tonnes of ore grading of 7.4% lead, 9.4% zinc, and 61.5 million oz of Silver. Throughout its history, it has produced over 200 million tonnes of ore throughout its 127 years of mining history dating back to 1885. Galena mineral ore found in Australia is considered rare, as it is only currently found in the Broken Hill Mine of Western New South Wales. It represents heritage value through the systematic collecting of the geological surveyers in Victoria and Australia during the early to late 19th Century. The fact that it is only found in one mining area of Australia, shows that this specimen is rare for examples of Australian Galena. This mineral specimen is one part to a larger collection, aquistion, and distribution of Garnet in Galena around Australia and parts of the world and donated to the Burke Museum between 1860-1880. While this specimen was not found by the Victorian Geological Survey, it shows the historical need for mapping geological areas around the Gold Rush region to further identify areas of precious metal and gem aquisition. Additionally, collecting these specimens was an important part of mapping the scientific make up of the earth's surface. Many were sent to institutions for further contribution to research and scientific knowledge of the specimens. A solid coin-sized lead and zinc sulphaide and zinc silicate ore mineral in shades of black and red with shiny black points. GARNET CRYSTALS in / GALENA (lead sulphide), / SPALERITE (zinc sulphide), / WILLEMITE (zinc silicate) ore. / Locality: Broken Hill, NSWburke museum, #beechworth, indigo shire, beechworth museum, geological, geological specimen, mineral, galena, galena quartz, broken hill mine, broken hill, nsw -
The Beechworth Burke MuseumGeological specimen - Chalcopyrite
... The Mt Lyell copper-gold mines produce some excellent crystallised specimens of chalcopyrite and other minerals. The deposits are generally considered to be of Cambrian volcanic origin, but there are indications of Devonian granitic influence on the ores, plus local remobilisation during Devonian deformation. ...This hand sized solid mineral specimen has shades of brass-yellow with spots of iridescent green-black tarnish. ... 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. ...This specimen originated from Mount Lyell on the west coast of Tasmania, where a large group of open cut and underground copper-silver-gold mines began operating in 1883. Between 1893-1994, the Mt Lyell Mining and Railway Company were responsible for operations. The Mt Lyell copper-gold mines produce some excellent crystallised specimens of chalcopyrite and other minerals. The deposits are generally considered to be of Cambrian volcanic origin, but there are indications of Devonian granitic influence on the ores, plus local remobilisation during Devonian deformation. Over 120 million tonnes of ore was produced from several workings, including the main Prince Lyell mine and the North Lyell mine, which was also of great importance. The Mount Lyell mines have a long history of human and environmental disasters, including the 1912 North Lyell fire that killed 42 miners, and two separate incidents in 2013 in which three people lost their lives. The environmental impacts from this complex of mines are extensive, with waste tailings and heavy metal contamination flowing directly into the King and Queen River catchments. In 1954, the eminent Australian historian, Geoffrey Blainey, published 'The Peaks of Lyell' which delves into the history of the 1912 North Mount Lyell Disaster.Chalcopyrite does not contain the most copper in its structure relative to other minerals, but it is the most important copper ore since it can be found in many localities and occurs in a variety of ore types. The brassy-yellow colours in Chalcopyrite mean it is often confused with pyrites and gold, leading to use of the term, "fool's gold." Chalcopyrite has been the primary ore of copper since smelting began five thousand years ago. 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.This hand sized solid mineral specimen has shades of brass-yellow with spots of iridescent green-black tarnish. Chalcopyrite is a copper iron sulphide mineral and a major ore of copper common in sulphide veins and disseminated in igneous rocks. Chalcopyrite has a hardness of 3.5-4 on the Mohs Scale. It is a member of the tetragonal crystal system and has metallic lustre and opaque transparency.burke museum, beechworth, indigo shire, beechworth museum, geology, geological specimen, chalcopyrite, copper pyrites, copper mining, tasmanian geology, mount lyell, mount lyell mines, fools gold, mohs scale, crystals, minerals, historical geological collection, victorian geological survey, a.r.c selwyn, gold rush, van diemans land -
The Beechworth Burke MuseumGeological specimen - Gold-Sulphide Ore
... A small gold-sulphide ore mineral specimen in shades of silver and grey with flecks of gold. ...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. ...This particular specimen was recovered from two hundred feet down in the Golden Mile in Kalgoorlie, Western Australia. The Golden Mile, named after the estimated sixty million ounces of gold worth around one hundred billion dollars, was the birthplace of the largest gold rush in Australia almost one hundred and thirty years ago when William Brookman and Samuel Pearce leased the Great Boulder mine. The Golden Mile is also the home of the Super Pit, Australia's most well-known mine.The majority of gold deposits will form as a native metal, however, on occasion, it can form a compound with another element, in this case, sulphur. Therefore, this specimen is a rare example of gold naturally forming into a compound mineral with sulphur. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A small gold-sulphide ore mineral specimen in shades of silver and grey with flecks of gold. Precious metals are often found in Sulphide Ores, as sulphides usually bind to these metals. They are also extremely symmetrical in crystaline form. Gold-Sulphide Ore occurs when gold forms a natural compound with other elements. In this form, gold can be present in one of two ways. It can be fully immersed in the sulphide, or a portion may be partially free. This specimen has minimal gold visible, with only a few flecks being partially visible.burke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, mineralogy, gold-sulphide ore -
The Beechworth Burke MuseumGeological specimen - Green Feldspar (orthoclase)
... The huge, 300-million-tonne orebody was discovered in 1883 and the superb mineral specimens attract collectors from around the world. ...The huge, 300-million-tonne orebody was discovered in 1883 and the superb mineral specimens attract collectors from around the world. ...Feldspar, derived from the German word feldspat, is a group of minerals which is the most common mineral group found on Earth, making up more than half of the planet's crust. The major rock-forming minerals in the Feldspar group include albite, anorthite, orthoclase and microcline. (Mindat, Feldspar Group). Orthoclase is part of the Feldspar Group subgroup, Alkaline Feldspar, which are known to be poor in calcium, and mostly rich in potassium. It is further also considered to be a K Feldspar, a subgroup of Alkaline Feldspar that are Potassium-dominant with variable crystal symmetry and Al-Si ordering state. Orthoclase are most commonly Colorless to white, Greenish white, Grayish yellow, or Pale pink and transparent to translucent with slightly pearly cleavage. The mineral rates at a 6 on the Mohs Hardness Scale. (cannot be scratched with a knife, but scratches glass with difficulty). The stronger green colour of this particular specimen is distinctive to the Broken Hill region (where it was found), and due to a small amount of lead. (BB) Its qualities find it misidentified at times as as microcline variety amazonite. Broken Hill is one of the world’s richest lead-zinc-silver deposits. The huge, 300-million-tonne orebody was discovered in 1883 and the superb mineral specimens attract collectors from around the world. (Australian Museum, Minerals from Australia: Australian mining regions)While feldspar is not by any means rare, this particular specimen has qualities distinctive to the Broken Hill mining district, with these properties leading at times to the mineral's misidentification. This creates potential for further study and identification of these mineral deposits through methods such as microscopic twinning, or using the position of certain d values in XRD patterns to calculate the degree of disorder of a K-feldspar, as discussed on the Mindat website (Mindat.com, Orthoclase:About Orthoclase). 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 aluminosilicate mineral composition which is primarily pale green and blue-grey in colour with traces of beige and white throughout. Note: green plumbian orthoclase (aka green feldspar) is an indicator mineral for the Broken Hill style lead-zinc deposits.N/Abroken hill mine, geological specimen, minerology -
Federation University Historical CollectionBook - Book - Ledger, Ballarat School of Mines Donation Book, 1878-1896, 01/01/1878 - 01/08/1896
... Buley - Ballarat - Prospective of Grenville College 1885 1428. 06 October 1885 - Ballarat - Collection of mineral specimens from Silverton (Collected by Mr James Murray). 1442. 20 October 1885 - Ballarat - Specimen of fossil fruits collected by Haddon by Charles Brown. 1682. 28 February 1887 - James Lamb - Ballarat - Copy of the Ballarat Times Newspaper of 3rd December 1854, framed and protected on both sides with glass. 1730. 23 May 1887 - Bella Guerin - Ballarat - Copy of the Victorian Review No 74 December 1885 4786. 27 March 1894 - James Oddie - Ballarat - 3 mineral specimens 4835. 01 August 1896 - P.V> Barnard - Ballarat - {ortion of Mining truck wheel altered to oxide of iron found in the old workings of the Golden Gate Mine at a depth of 200 feet...Buley - Ballarat - Prospective of Grenville College 1885 1428. 06 October 1885 - Ballarat - Collection of mineral specimens from Silverton (Collected by Mr James Murray). 1442. 20 October 1885 - Ballarat - Specimen of fossil fruits collected by Haddon by Charles Brown. 1682. 28 February 1887 - James Lamb - Ballarat - Copy of the Ballarat Times Newspaper of 3rd December 1854, framed and protected on both sides with glass. 1730. 23 May 1887 - Bella Guerin - Ballarat - Copy of the Victorian Review No 74 December 1885 4786. 27 March 1894 - James Oddie - Ballarat - 3 mineral specimens 4835. 01 August 1896 - P.V> Barnard - Ballarat - {ortion of Mining truck wheel altered to oxide of iron found in the old workings of the Golden Gate Mine at a depth of 200 feet ...Leather bound ledger with hand written details on donations to the Ballarat School of Mines Museum or the Ballarat School of Mines Library. The Ledger was made by J. McHutchison, Bookbinder, paper ruler and Account Book Manufacturer. 267. 07 July 1880 - John Lynch Junior - Smythesdale - Cast of "Golden Age" nugget found at Browns by Co-operative Party - 12 men. Weight 75 oz 12 dwts 12 grs 294. 24 June 1880 - W.H. Shaw - Ballarat - 94 numbers of 'The Engineer'. 295. 28 June 1880 - Rivett Henry Bland - Clunes - Specimen of water pipe from the Port Phillip Consols Mine encrusted with Carbonates of lime and magnesia and sulphate of lime with earthy matter. 418. 17 June 1881 - F. Ratte - Sydney - Catalogue of Rocks, minerals, etc of New Caledonia. 462. 28 September 1881 - Dr Bunce - Ballarat - Concretionary Basalt with Car. Lime and Magnesia. 465. 06 September 1881 - J.J. Sleep (Chairman of the Board) per favor of E.W. Spain, Esq, Manr - Ballarat - Diamond drill core from "Carisbrook Freehold Estate" - cut at a depth of 150 feet. Dedrites from Munster Gully ... 517. 20 January 1882 - William Lester - Ballarat - The Agricultural Teacher 549. 24 March 1882 - C.E. Grainger Manager Ballarat Woollen Mills - Ballarat - Samples of dyed and raw wool and dye material. 600. 04 July 1882 - Henry Sutton - Ballarat - 13th Annual Report of the Aeronautical Society of Great Britain. 1222. 31 October 1884 - Trooper Dowling - Miner's Rest - Owl 1223. 04 November 1884 - W. McKeenan - 3, Adair St, Ballarat - Flying Squirrel. 1259. 16 January 1885 - A.A. Buley - Ballarat - Prospective of Grenville College 1885 1428. 06 October 1885 - Ballarat - Collection of mineral specimens from Silverton (Collected by Mr James Murray). 1442. 20 October 1885 - Ballarat - Specimen of fossil fruits collected by Haddon by Charles Brown. 1682. 28 February 1887 - James Lamb - Ballarat - Copy of the Ballarat Times Newspaper of 3rd December 1854, framed and protected on both sides with glass. 1730. 23 May 1887 - Bella Guerin - Ballarat - Copy of the Victorian Review No 74 December 1885 4786. 27 March 1894 - James Oddie - Ballarat - 3 mineral specimens 4835. 01 August 1896 - P.V> Barnard - Ballarat - {ortion of Mining truck wheel altered to oxide of iron found in the old workings of the Golden Gate Mine at a depth of 200 feet. (4235 is last entry)ballarat school of mines, ballarat school of mines museum, donations, henry sutton, bella guerin -
The Beechworth Burke MuseumGeological specimen - Slice Dendrites on Sandstone, Unknown
... Most sandstones are made of quartz which are chemically-resistant minerals. This particular specimen was donated by Alfred Selwyn in 1868 as part of the Geological Survey of Victoria. ...Most sandstones are made of quartz which are chemically-resistant minerals. This particular specimen was donated by Alfred Selwyn in 1868 as part of the Geological Survey of Victoria. ...Dendrites are deposits of black minerals, typically manganese oxides that precipitated from water seeping through fractures in fine-grain rocks like a sandstone or limestone. Dendrites are much less regular than plant fossils and lacks vein structures. The manganese cryztallizes through the process called 'supercooling'. Some samples of dendrites occur in volcanic rocks in the Lilydale district, east of Melbourne. Sandstones are made of tiny sand grains that may have been deposited in the sea and later formed together. Most sandstones are made of quartz which are chemically-resistant minerals. This particular specimen was donated by Alfred Selwyn in 1868 as part of the Geological Survey of Victoria. It is connected to the original 1875 catalogue on Geological Specimen with number 189 'Quartz Crystals_Quartz Crystals (two are polished)'Dendrites on sandstones This specimen is an important contribution to the geological history of Victoria, as well as its links to the 1868 Geological Survey of Victoria. This specimen is part of larger collection of significant geological specimens in the Burke Museum that was collected from around the world between 1868-1880. A large percentage of these specimens were collection as part of the Geological Survey of Victoria 1852-1974. The Geological Survey of Victoria was an organisation founded in response to the Victorian gold rush to explore the geological and mineral resources and to record a detailed map of the state. It 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 hand-sized slice of light brown sandstone with dendrites formed from crystallized manganese oxide.Existing label: Not sure what / 'Slica dondrites' / means. / Sample is sandstone and original label / identifies it as from / the Grampians near Stawell. / C. Willman / 15/4/21 Other label: [illegible] / stone [ illegible] / from Grampians Stawell / 1894 /geological specimen, geology, geology collection, burke museum, beechworth, dendrites, sandstones, quartz, lilydale district, geological survey of victoria, grampians, victoria rocks, minerals, rocks, manganese oxides, alfred selwyn -
Federation University Historical CollectionBook - Ledger, Ballarat School of Mines Donation Book, 1878 - 1895, 1878-1895
... Daniel Brophy, Ballarat - Collection of mineral specimen form Silverton (Collected by Mrs James Murray)
1442. ...Daniel Brophy, Ballarat - Collection of mineral specimen form Silverton (Collected by Mrs James Murray)
1442. ...The Donation Book relates to the Ballarat School of Mines Museum which opened in 1872. Very few of these items are still held by Federation University. The Museum was emptied in the 1960s with items being distrubuted to the Ballarat Historical Society, returned to original lenders (ie Pern Collection), of disposed of. Donations to the Ballarat School of Mines include: 34. M. Hamburger, Ballarat - bunsen burner 41. W.H. Shaw, Phoenix Foundry - 81 nos of 'Engineer' 89. Juvenile Industrial Exhibition Association Committee per Joseph Flude - dies used for striking medals awarded to successful exhibits. 165. Ferdinand Von Mueller 172 Ferdinand Von Mueller o hortus siccus 6 197. James Stoddart 203. Edward Gazzard, North Creswick - Model of safety Cage invented and made by donor 218. E. Morey 222. Alfred Lestor 228. J.J. Sleep, Ballarat, patent Lever escarpment Clock (displayed in laboratories) 237. Bernard Smith (Warden) per favor of James M. Bickett - Bust of Mr John Lynch, Smythesdale. (Note: This item is not in the present Federation University Historical Collection) 241. James Oddie, J.P., Ballarat, Copy of 'the Chemist and Druggist' 267. John Lynch Junior, Smythesdale - Cast of "Golden Age" nugget, found at Browns by Co-operative party, 12 men. Weight 75 oz, 12 dwts, 12 grs.(Note: This item is not in the present Federation University Historical Collection) 270. Isaac Davis, Main Road, Ballarat 294. W. H. Shaw, Ballarat - 94 nos of 'The Engineer' 295. Rivett Henry Bland, Clunes - Specimen of water pipe from the Port Phillip Company's mine encrusted with carbonites of lime and magnesium (Note: This item is not in the present Federation University Historical Collection) 299. D.J. Williams, Queenscliff - 1 case shells from Fiji 305. C. Retallack, Ballarat 314. William Henry Shaw, Ballarat - glass case 323. W. Longley, Ballarat - Botanical Specimen (Note: This item is not in the present Federation University Historical Collection) 327. W. H. Angove, Perth 337. J. Cosmo Newbery, B Sc, Melbourne 343. James Hector, M.D., New Zealand 353. R.S. Mitchell, Ballarat - 8 specimens live plants (medicinal) (for the Ballarat School of Mines Garden) 355. W. Magee, Ballarat - Sugar cane plants and seeds (for the Ballarat School of Mines Garden) 363. James Hector, Wellington, new Zealand 371. William Wesley, 28 Essex St, Strand, London - Scientific book circular 380. Jacob Upfold (deceased) per favor of the trustees - bequest of steam engine indicator and belongings (boothe and case) 381. Joseph Mitchell, 22 Macarthur Street, Ballarat - sod of turf cut from Warboy's High Few, County Huntingdon, England, 1872. 394. W.H. Barnard 401. James Orr 418. F. Ratte, Sydney 440. Alfred Mica Smith, Sandhurst (Bendigo), Inaugural Address, delivered to the Bendigo School of Mines Science Society, June 20. 1881 by P.H. Macgillivray, MA, MRCS, FLS, President. (Note: This item is not in the present Federation University Historical Collection) (Note: This item is not in the present Federation University Historical Collection) 446. C. C. Shoppee, Ballarat 462. Dr Bunce, Ballarat 468. James Black, Mining Manager "Kerrit Bureet' 479. J.S. North, Mining Manager No. 2 Queen Co, Black Hill Ballarat. 505. Smith Tibbitts - A block of ancient leaves from the Nigtingbool Estate near Haddon on the Ballarat district from shaft 80 feet deep. (Note: This item is not in the present Federation University Historical Collection) 512. F.W. Niven, Ballarat - "A Handy Book to Tasmania" 522. James Hector, Wellington, New Zealand 549. C.E. Grainger, Manager Ballarat Woollen Mills - samples of dyed and raw wools 600. (4 July 1882) Henry Sutton, Ballarat - 13th annual report of the Aeronautical Society of Great Britain; 2 papers from the Proceedings of the Royal Society, nos 217 and 218- 1882, "One a new electrical storage battery by Henry Sutton, Ballarat, Victoria. 608. H. Glenny J.P., Ballarat - Specimen of Asbestos from Tasmania 610. M.H. Edelmann, Munich, Germany 674. W.H. Shaw, Phoenix Foundry - Steel boring 95 feet long taken from bed-plate of locomotive engine. 675 - H.R. Hancock J.P. pre favour Mr James Pryor, Moonta Mines 676. Baron Ferdinand Von Mueller KCMG, etc, Melbourne 678. E.F.A. Gaunt, Royal Navy, H.M.S. Nelson, per favour Lyde Gaunt - Specimen of manganese ore from the mines - Russell - New Zealand 728. Dr Pinnock, Ballarat 760. Simon Morrison, Ballarat 784. James Shugg, Hamilton - 1 case fossils from Muddy Creek, near Hamilton. (Note: This item is not in the present Federation University Historical Collection) 786. W. Bolam (inspector of Schools), Melbourne - 2 spears and 1 fishing prong Fijian 806. James Oddie, Ballarat 708. Henry G. Hanks, San Francisco 786. W. Bolam (Inspector of Government Schools Melbourne) - 2 spears and one fishing prong Fijian 824. Henrique Gorceixm Onro Preto, Brazil 840. W. Laplau, Ballarat - Gas furnace with a large assortment of fittings, also large gas holder and oil-heating apparatus 854. Robert Borch, Main Road, Ballarat - Improved safety chain (Note: This item is not in the present Federation University Historical Collection) 928. James Oddie 944. James P. Munroe, Registrar, Massachusetts 952. L.E. Cutter per favour of Mr F.J. Martell - Unexploded bomb shell from the Eureka Stockade 957. H. Glenny, Hobart 962. George Hart, Ballarat - eagle 976. Henry Sutton, Ballarat - 1 volume "Plattner on the Blowpipe" 978. J.W. Flatow, 45 Madeline Street, Carlton, Melbourne 984. Charles C Shoppee Ballarat - Copies of ancient coins 989-95 - Specimens from Moonta, South Australia 985. W.H. Wooster BOlwarra - books microscope related 1179. James Oddie - Live hedgehog 1181 C. Crisp, Bacchus Marsh, Portugal Copper Coin, 1785 1248 James Oddie, Solomon Islands - Bow and arrows & Spears 1285. C. Colyer, Smythesdale 1327. John L. McKenna, Smeaton - Fragment of Stone Axe. 1395. Mrs O. Skoglund, Nerrina 1428. Daniel Brophy, Ballarat - Collection of mineral specimen form Silverton (Collected by Mrs James Murray) 1442. Henry Sutton, Ballarat - Specimens of fossil fruits collected at Haddon by Charles Brown. 1444. Mining Department - Underground Mine Workings from Band of Hope and others. 1517. W.H. Wooster, Ballarat 1592. Bishop of Ballarat - Stone Axe and other native items 1669. H. McHaffier, Napoleons - 1 Spanish silver coin 1681. James Oddie, Dunedin 1688. W. Burbridge, Ballarat - Native Tomahawk from Metung 1708. A. Doepel, Ballarat 1712. Marty Guerin, Ballarat 1735. Bella Guerin. M.A., Ballarat - Copy Wide Awake Vol 1 No 7 May 28th 1887 and The Bulletin, March 19th 1887. 1747. Bella Geurin M.A., Ballarat - Copy Wide Awake Vol 1 No 8 June 4 1887 1751. Bella Geurin M.A., Ballarat - Copy Wide Awake Vol 1 No 9 June 11th 1887 1842. Linnean Society, London England - Charter, By Laws, Proceedings, Transactions, Journals 1853. W.J. Corbould, Silverton, NSW - chloride of silver from Pinnacles, Broken Hill, Silverton 1888. W. J. Corbould, Sample of metallic silver from Silverton, NSW 1928. E. Morey, Ballarat - Steam Engine 1937. Henry Sutton A.S.I.E., Ballarat - Plate Electric Machine, chimes and Sportman (number crossed out) 1951. Henry Sutton A.S.I.E., Ballarat - Plate Electric Machine, chimes and Sportman 1981. Harrie Wood (per W.H.B.[Barnard?), Ballarat 1996. W.H. Shaw, Phoenix Foundry - Papers "The Vict Engineer July 1887, May June July August 1888 and others 2014. Harrie Wood, Sydney - Report Department of Mines, 18872027. W.J. Bechervaise - Copy of Book by Baldwin Spencer 2034. A.G. Randall - Native Hatchet 2045. W.H. Corbould, Silverton, Collection of silver ores 2051. Fowler, Tarnagulla - Native Tomahawk 2123-2131. James Oddie, London 2163. Roff. F. Taplier, Sturt Street - Native Tomahawk 2178. Syd. Johnson, Meredith - Native Tomahawk, Greenstone 2184. Mr Tupp for Hall - Native Spear and Club 2292. Emmanuel Steinfeld, Melbourne 2313. A. Atwood, Rowlands Factory, Dana Street 2361. Dr Pinnock, Ballarat - Collection of Living Sponges 2363. P. Curnow, Ballarat - Piece of wood with stone naturally embedded 2364. R. Dowling, Waubra 2875. Mrs C, Flude, Ballarat - Collection of (5) mineral specimens 3460. Joseph Weir, Ballarat - Sample of rolled Annibar 3466. J. Hart, Ballarat - Native Shield - supposed to have been made by King Billy 4784. Mr. O. Woolnaugh, Pleasant Street - Four Native Tomahawks 6469. L. Balhausen, Ballarat 3472. John English, Smeaton - three samples of auriferous wash dirt 3607. Columbia College, New York - Handbook of Information of the Columbia College in the Ciry of New York 1892-3. 3672. L.A. Samuels, Bendigo 3724. P. Paperhagen 3736. The Late Rivett Henry Bland per John Noble Wilson - Collection of mineral specimens and fossils 3752. G.A. Denny, South Africa 3755. J. Carroll, Ballarat - Specimen of Native bread found in Ballarat East. 4765. J. Donnelly, Springs, Bungaree I. Fowler, Coolgardie, Specimen of Gold Bearing Quartz ballarat school of mines, doantions, museum, ballarat school of mines museum, safety cage, botanical garden, materia medica garden, library, bella guerin, james oddie, phoenix foundry, w.h. shaw, john lynch, henry sutton, aboriginal, stone axe, tomahawk, geological specimens, moonta, fedinand krause, oddie collection of minerals, thomas bath, spears, solomon islands, king billy, bows and arrows, ancient coins, birds eggs, snakes -
Federation University Historical CollectionBooklet, The Ballarat School of Mines and Industries 1870-1920 Jubilee Booklet, 1920 (estimated)
... The Museum, which now contains a most valuable collection of minerals, was one of the first things attended to, and the reports presented to the Council from time to time speak of additions being made from all parts of the world. New equipment was constantly being added to the School, a good deal of assay work was done, and some specimens were sent from the East Indies for examination as far back as 1873. ...The Museum, which now contains a most valuable collection of minerals, was one of the first things attended to, and the reports presented to the Council from time to time speak of additions being made from all parts of the world. New equipment was constantly being added to the School, a good deal of assay work was done, and some specimens were sent from the East Indies for examination as far back as 1873. ...The first school of Mines in Australia was established at Ballarat in 1870. At the time of its jubilee (1930) the following people were members of the School Council: W.H. Middleton (President), W.T. Humphreys (VP), J.S. Vickery (VP), F. Barrow, Col. W.K. Bolton, William Baragwanath, A.E. Cutter, J.N. Dunn, G. Fitches, W.H. Fleay, F. Herman. W.D. Hill, T. Hurley, K. Kean. J. Kelly, L. Lederman, Mayor of Ballarat, Mayour of Ballarat East, D. Maxwell, M. Martin, R. Maddern, D. Ronaldson, F. Saunders, R. Stephenson, A.O. Stubbs, R.E. Tunbridge. The School Staff in 1920 comprised: Herbert H. Smith, Walter Rowbotham, Reginald L. Cutter, M.C. Young, Hilda Wardle, M. Wiliamson, P.S. Richards, L.H. Archibald, J. Woods, Ken Moss, W. Kenneth, Mrs McIlvena. B. Robinson, S. Rowe, E. Hope-Jones, Miss Abrams, L.St.G.P. Austin, Alfred Mica Smith, J.R. Pound, Herbert R. Murphy, N.H. Junner, Maurice Copland, L.H. Archibald, E.J.A. McConnon, Newton King, D.m. Hull, T.R. Gordon, John M. Sutherland, T.K. Jebb, Dick Richards, C. Tonkin, A.W. Steane, J. Paterson, H.W. Malin, R.V. Maddison, S.M. Mayo, F.A. King, W.H. Steane, T.R. Gordon, T.A. Williams, H. Waldron, G. Black, E.J. McConnon, R.V. Duncan. R. Cutter, E.G. Vawdrey, Hilda WardleWhite stapled booklet - landscape format - 20pp + soft covers with blue writing. Includes an historical sketch of the Ballarat School of Mines. Contains images of the school from around 1920. The history outlined in the booklet follows: 'Ballarat has helped to influence the life and destinies of Australia in many ways, the recital of which would perhaps prove tedious to the citizens of less favoured localities! However, it can be said, without much fear of contradiction, that only less known thought Australia than its fame as a gold field is the reputation won for it by its school of Mines, ... Ballarat was still quite a new place when the School was founded, but a very propserous and popular place all the same, with a go-ahead lot of citizens brim full of the spirit of enterprise which seemsto animate mining populations generally. Money was plentiful, and they launched out into ventures, which later, were to develop and take the place of the gold mines, while what is more to the point, they understood the value of education. the old digging days were passing away. So far as Ballarat itself was concerned the day of the cradle and tin dish had already passed into an antiquity "as dead and distant as the age of the Tubal Caon," said dir redmond Barry on declaring the School open. Mining had become a serious business, and the mining engineer, the metallurgist, and the geologist had become a power in the land. In these circumstances the suggestions to found a School of Mines met with ready acceptance. The late Mr James M. Bickett had the honor of bringing forward the proposition at a meeting of the Ballarat Mining Board in October, 1869. it was agreed to, and the Government, having been approached for assistance, granted a lease of the old Supreme Court buildings at a nominal reantal. A modest sum, including 100 pounds from the Borough Council of Ballarat West, was subscribed by a number of sympathisers, and on the 26th October, 1870, the inaugural address was delivered by Sir Redmond Barry, the first President of the School. Classes were commenced on the 23rd January, 1871. The students at first were mostly adults. They were chiefly men emloyed at the mines, who had the wisdom and energy to devote their spare time to study, and, though their attendance was somewhat irregular, they made very good progress. Old prints which have been preserved show them at work at furnaces, big bearded men of the old-fashioned type of miner. It is interesting to note that among those who gave evidence and encouragement was Sir Roderick Murchison, who many years before had advised Cornish miners to emigrate to Australia to search for gold, and who in 1848 was in possession of gold ore sent from this country. Sir Roderick sent a parcel of books for the library, and gave useful advice as to the curriculum which should be adopted. The Museum, which now contains a most valuable collection of minerals, was one of the first things attended to, and the reports presented to the Council from time to time speak of additions being made from all parts of the world. New equipment was constantly being added to the School, a good deal of assay work was done, and some specimens were sent from the East Indies for examination as far back as 1873. By this time there was a difficulty in providing accomodation for the students who wished to enrol, and the number of instructors had grown from two to four. In 1882 the first building was being erected on what was then part of the gaol reserve. A little more than ten years afterwards a buildnig formerly serving as a Methodist Church was absorbed, while later on, the demand for accomodation increasing, the attack upon the gaol was renewed. The School continued to grow in reputation and size, and became the science centre of the district, and in 1889 a learge new building was opened by Sir Alexander Peacock. Students came from over seas as well as from all the States of Australia, and after going through their courses they took with them the name and fame of the old School to all parts of the globe. School of Mines boys have played a great part in developing the mining fields of Western Australia, South Australia, and africa, while old students who have made a name in their profession are constantly dropping in to see how the old place is getting along. It was not to be expected, however, that the Ballarat School would be left without rivals, its very success inspiring competition. Mining Schools were started in other parts of Australia, and, at the same time, Victoria ceased to hold first place as a mining state. On the other hand there was a great advance in manufacturing, and the demand for technicaly trained men became a great and as insistent as ever it had been for trained mining men. The Council was quick to adapt the school to the new conditions, and the result is seen in the institution, which is one of Ballarat's proudest possession. Instruction is given in all branches of technical work, and the classes are filled with students who are building up for Ballarat a reputation as an industrial centre, which promises to equal that which it formerly held as a mining town. Owing to its bracing climate, its abundant opportunities for recreations, and its accessibilty, Ballarat as a city is an ideal place for educational purposed, and is yearly becoming more and more appreciated throughout the State. The chairman of one of Ballarat's biggests industries claims that the workman can do twice the day's work here that he can do in Melbourne. he was a little enthusiastic over it, perhaps, but it is a well-known fact that the healthy and invigourating Ballarat climate is conducive to both physical and mental activity, and the records of the School provide ample proof of it. One of the most interesting and successful branches of the School of Mines and Industries - if the name be enlarged with the enlargement of its scope - is the Technical Art School. "The City of Statues" has from its earliest days been a stronghold of art. Art schools have flourised here, and in 1905 the Education Department came to the conclusion that the best thing to do with them was to place them under the management of the School of Mines Council. A magnificent new Technical Art School was built at a cost of some 12,000 pounds on the site of the old Supreme Court building, and was formally opened on the 23rd July, 1915. The results have not only been justified but surpassed all anticipations. The most comprehensive list of subjects is taught, and this list is constantly added to. Students have flocked to the art School, which may be said to occupy a unique position in Australia, and its record of success is really astonishing. Its students supply art teachers for the newer schools that are being built, and many occupy leading positinos in important business houses. So well is its reputation known that orders are constantly being received, not only from Victoria, but from other States, for honor boards and challenge shields to be designed and made. The most recent addition to the School of Mines and Industries is the Junior Technical School, for which a new building is now being erected on a portion of the gaol site, transferred to the School of Mines Counci by the Government. At the present moment temporary quarters are being occupied. Some students after passing through the Junior School go straight to employment, continuing perhaps to attend the evening trade classes, while others move on to the senior School. In a review of the work of the School of Mines mention must be made of a series of industrial research carried out under supervision of the Principal. One in particular, regarding the suitability of the local ores for the manufacture of pigments attracted much attention, while the experiemtns on the manufacture of white potery from Victorian clayes were considered of sufficient importance by the Federal Advisory Council of Science and Industry to warrant the appointment of a special investigator. The results of these have been most encouraging, and may have far-reaching consequences. The vocational training of returned soldiers also should not be overlooked. The work was taken in hand from the first, before the Repatriation Department gave assistance, and now with the help of the department of the School has become one of the largest vocational training centres in Victoria outside of Melbourne. The soldiers, trained in a variety of occupations, have made remarkable progress, and already considerable numbers have found employment in local workshops and factories. To sum up, the School is divided into the following departments, each well staffed and equipped: - The School of Mines, science, and Engineering; the Techncial Art School, the Boys' Junior Technical School, the Girl's Preparatory Technical Classes, Trade Classes, and the Commercial School. The school of Mines, science and Engineering, comprises the following branches: - Mining, Metallurgy, Geology, Electrical Engineering, Civil Engineering, Mechanical Engineering, Applied Chemistry, and Pharmacy. Battery treatments, Cyanide Testing, Smelting, Assays, and Clay Testing from a regular part of the School's work. Students gaining qualifications obtain concession in their courses at the university, should they proceed there to continue their studies. The technical Art school curriculum includes training in all branches of pictorial and applied art, an Architectural Diploma Course, a Draughtman's Course, technical Art teachers' Course, Photography,Ticket Writing, Art Metal Work, Woodcarving, Needlework, and Leather work. The Trade Classes give instruction in Telephone Mechanics, telegraphy, Carpentry, Cabinet Making, Plumbing, Blacksmithing, Fitting, Electric Wiring, and Printing. Numerous Scholarships are offered every year, and altogether students will find few places to equal the Ballarat School of Mines and Industries as a training place for their life's work. One of the first in the continent to be established, its Jubilee finds it still in the front rank, keeping pace with the times, and offering to the youths of this country the means of taking advantage of Australia's teeming opportunities. william, battery, smith, herbert, drawing from the antique, ballarat school of mines botanical gardens, ballarat school of mines, redmond barry, alfred mica smith, james bickett, museum, dick richards, ballarat junior technical school, s m b, ballarat school of mines and industries, ballarat technical art school, model mine, james m bickett, j m bickett, roderick murchison, vocational training rooms, wesley church, methodist church, alexander peacock, lathes, repatriation, repatriatin department, war service, school council, baragwanath, gold mining, mining laboratory, plaster cast, r.w. richards, anniversary, jubilee -
Federation University Historical CollectionBook, A Descriptive Catalogue of the Minerals in the Museum of the School of Mines, Ballaarat, 1882, 1882
... minerals accords with that adopted at the Royal School of Mines, London. The numbers prefixed to the species in the catalogue agree with those on the descriptive labels which accompany each specimen, and also with those attached to the specimens themselves. ...minerals accords with that adopted at the Royal School of Mines, London. The numbers prefixed to the species in the catalogue agree with those on the descriptive labels which accompany each specimen, and also with those attached to the specimens themselves. ...The Museum of the Ballarat School of Mines was established in 1872. The curator in 1882 was Ferdinand M. Krause. Prefatory Notice by James Oddie). The want of a guide through the technical collections of The School Mines has long been felt by visitors and students - a guide , not so much to those who merely 'look' at the various exhibits in the Museum, but an instructor to those who desire to take away with them some practical information on the natural occurrence and economical value of the objects exhibited. This want is being filled by the labour of Mr. Krause, whose first installment - 'A Descriptive Catalogue of the Minerals' - is herewith represented to the visiting public." Introduction to the catalogue: " The collection is still in its early growth, and far from being a complete representation of the Mineral Kingdom; many varieties, species, and even whole groups are absent. This state of incompleteness will, no doubt, be adjusted in the sequence, and progressive lists issued from time to time. 'Ad interin' the present catalogue will, be found useful to students and visitors of the School. As far as practicable, the classifications of the minerals accords with that adopted at the Royal School of Mines, London. The numbers prefixed to the species in the catalogue agree with those on the descriptive labels which accompany each specimen, and also with those attached to the specimens themselves. On the descriptive labels the chemical composition of the minerals is expressed in formulae usually employed in standard mineralogical works. Students who have note paid attention to mineralogical chemistry will note that each dot over a symbol is equivalent to one atom of oxygen, .... A bar through a symbol denotes a double atom of the base, .... " In 1882 the collection was housed in 33 cases. The catalogue outlines the specimen types housed in each case. The classification of minerals accords with that adopted at the Royal School of Mines, London. Leather covered book of 94 pages with gold lettering on the front, including "F.M. Krause". The book includes a plan of the museum layout, plan of the grounds and buildings of the Ballarat School of Mines and a prefatory notice by James Oddie.ballarat school of mines, ballarat school of mines museum, museum, krause, ferdinand krause, fm krause, oddie, james oddie, geology, mineralogy, charles boyd, f.m. krause, minerals, curator -
The Beechworth Burke MuseumGeological specimen - Malachite, Unknown
... 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. ...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 -
The Beechworth Burke MuseumGeological specimen - Malachite, Unknown
... 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...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. ...Malachite is a green copper carbonate hydroxide mineral and was one of the first ores used to make copper metal. Malachite has been utilised as a gemstone and sculptural material in the past as its distinctive green color does not fade when exposed to light or after long periods of time. Malachite is formed at shallow depths in the ground, in the oxidizing zone above copper deposits. The material has also been used as a pigment for painting throughout history. This particular specimen was recovered from the Burra Burra Copper Mine in Burra, South Australia. Otherwise known as the 'Monster Mine', the Burra Burra Copper Mine was first established in 1848 upon the discovery of copper deposits in 1845. Within a few short years, people from around the world migrated to Burra to lay their claim in the copper economy. By April 1848 the mine was employing over 567 people and supporting a population of 1,500 in the local township. Up until 1860, the mine was the largest metals mine in Australia, producing approximately 50,000 tonnes of copper between 1845 to its closure in 1877. The Burra Burra Mine was also famous for a number of other specimens, including; crystalline azurite, cuprite, and botryoidal and malachite.Malachite is considered a rare gemstone in that the original deposits for the stones have been depleted leaving behind very few sources. In addition, the use of Malachite as gemstones and sculptural materials remains just as popular today as they were throughout history. It is quite common to cut the stone into beads for jewellery. The fact that Malachite has such a rich colour and one that does not fade with time or when exposed to light makes it particularly rare. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study. A solid hand-sized copper carbonate hydroxide mineral with shades of yellow, blue, and light green throughout.geological, geological specimen, burke museum, indigo shire, malachite, malachite specimen, burra burra mine, burra, south australia, australian mines, mines, monster mine -
The Beechworth Burke MuseumGeological specimen - Galena Chalcopyrite, Unknown
... The mineral is found in igneous and metamorphic rocks in medium- to low-temperature hydrothermal veins. This specific specimen was recovered from the mines in Broken Hill, New South Wales. ... 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. ...Galena Chalcopyrite is the earth's primary ore of lead and is mined from a large number of deposits in many countries. It is also an important source of silver. Galena Chalcopyrite is one of the most abundant and widely distributed sulfide minerals across the world. The mineral is found in igneous and metamorphic rocks in medium- to low-temperature hydrothermal veins. This specific specimen was recovered from the mines in Broken Hill, New South Wales. The mines in Broken Hill were first established after Charles Rasp discovered a large amount of silver-lead-zinc ore-body in the area in 1883. BHP (Broken Hill Proprietary) mining company was then established in 1885 and quickly became the lead in Australia's mining industry after they began excavating and exporting the country's largest amount of lead, silver, and zinc. This feat generated over $100 billion in wealth for the company.Galena Chalcopyrite is signifiant as it represents the catalyst for the rise of Australia's most influential mining companies - BHP. The mineral was one of the first to be mined in the country and after being made into lead, was used for a variety of things such as paint, batteries, ammunition, and plumbing materials before it was known to be harmful to humans. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study. A grey, solid hand-sized lead sulfide mineral with a silver metallic luster.burke museum, beechworth, geological, geological specimen, galena, galena chalcopyrite, chalcopyrite, broken hill, bhp, bhp mining, broken hill mine, mine, australia mine, lead, lead mine
