Number of parts: 18. Samples of the Rare Earth Group - Erbium, Dypsrosium, Lanthanum Oxides

John COLLIER (1937- 2012) John Collier was born at Ballarat in 1937. He received a Diploma of Mining and a Diploma of Civil Engineering at the Ballarat School of Mines (SMB), later graduating from the University of Melbourne with a Bachelor of Engineering (Mining). Early in his career he received a Diploma of Accountancy from the Australian Society of Accountants. Collier believes his experience at SMB had a profound influence on his life, especially what he learnt in Geology, Engineering, Chemistry, etc., all of which he found beneficial to his later working life and he is proud of that association. Through his experience in the world-wide mining industry John Collier has made a major impact on the mining industry. He has been exploration leader for a large number of worldwide discoveries and farm-ins both major and minor. He has experience in every facet of the mining industry, and his record in identifying diamond opportunities include Australian (Argyle), Canada (Diabik), Zimbabwe, and the Brazil Pipe (Collier Falls). His success in diamond exploration may be unparalleled. John Collier also has significant success with lead-zinc, iron ore, coal, copper, gold-silver, petroleum, heavy minerals, nickel, uranium, industrial minerals, rare earths, and tin. In 2006 John Collier was made a Legend in Mining by the Australian Mining Industry. Over his last 10 years, he had become a passionate painter, holding several successful solo exhibitions. His naive style featured beautiful and unexpected colour combinations. Many of his most lauded paintings depicted mining scenes, harking back to his Ballarat days. This item is part of the Federation University Art Collection. The Art Collection features over 2000 works and was listed as a 'Ballarat Treasure' in 2007.Two artworks by John Collier inspired by his alma mater, the Ballarat School of Mines. art, artwork, john collier, ballarat school of mines, alumni

John COLLIER (1937- 2012) John Collier was born at Ballarat in 1937. He received a Diploma of Mining and a Diploma of Civil Engineering at the Ballarat School of Mines (SMB), later graduating from the University of Melbourne with a Bachelor of Engineering (Mining). Early in his career he received a Diploma of Accountancy from the Australian Society of Accountants. Collier believes his experience at SMB had a profound influence on his life, especially what he learnt in Geology, Engineering, Chemistry, etc., all of which he found beneficial to his later working life and he is proud of that association. Through his experience in the world-wide mining industry John Collier has made a major impact on the mining industry. He has been exploration leader for a large number of worldwide discoveries and farm-ins both major and minor. He has experience in every facet of the mining industry, and his record in identifying diamond opportunities include Australian (Argyle), Canada (Diabik), Zimbabwe, and the Brazil Pipe (Collier Falls). His success in diamond exploration may be unparalleled. John Collier also has significant success with lead-zinc, iron ore, coal, copper, gold-silver, petroleum, heavy minerals, nickel, uranium, industrial minerals, rare earths, and tin. In 2006 John Collier was made a Legend in Mining by the Australian Mining Industry. Over his last 10 years, he had become a passionate painter, holding several successful solo exhibitions. His naive style featured beautiful and unexpected colour combinations. Many of his most lauded paintings depicted mining scenes, harking back to his Ballarat days. This work and subject matter was painted for the artist's alma mater, the Ballarat School of Mines (now Federation University Australia). This item is part of the Federation University Art Collection. The Art Collection features over 2000 works and was listed as a 'Ballarat Treasure' in 2007.Colourful acrylic on canvas painting depicting the Port Phillip Gold Mining Company, Clunes.art, artwork, john collier, port phillip cold mine, clunes, clunes, available, alumni, mining

An annular eclipse occurs when the moon passes between Earth and the Sun and the moon's apparent diameter is smaller than the Sun's blocking most of the sun's light and causing the sun to look like an annulus or ring. An annular eclipse appears as a partial eclipse over a large region of the earth. In 1916, annularity was only visible in Australia. This photo card records a rare annular eclipse of the sun as viewed in Warrnambool at 12:45pm on 30 July 1916This Foyle photo card shows the progress of the eclipse of the sun with four images and white writing on a black background. There is hand writing in black ink and other black printing on the rear of the card. Front: Middle of the bottom edge "Eclipse of the Sun Warrnambool 12.45. 30.7.16" Bottom right hand corner: "Foyle Photo" Four numbers beside each image. Rear: Foyles Photo Card Studios_Liebig St, Warrnambool; "Warrnambool" handwritten.solar eclipse, warrnambool, foyle photo card, liebig street, annular solar eclipse

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

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

Rhodonite is a reddish-pink manganese silicate material and often contains iron, magnesium and calcium. It is usually found in metamorphic rocks (rocks which have been altered by heat, pressure or chemical process). It can range in size from tiny to massive. Because of their composition they are not suitable for use in jewellery because they are hard enough. It is quite rare to find, though has been found in Australia, North America, South America and Europe.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 specimen is a palm shaped piece of loellingite within rhodonite. It is mostly reddish-pink coloured, with flecks of light and dark grey. Loellingite is a grey iron arsenide which often forms into crystal shapes. It is mostly found in mesothermal veins (caused by immense heat) with sulfides or in limestone. It is toxic when heated or struck. rhodonite, loellingite, burke museum, beechworth, geological survey of victoria

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

This specimen was recovered from Ceres West of Geelong, Victoria. Greenstone is the name for any metamorphosed basic igneous rock (in the case of this specimen, Gabbro) that gains its greenish colour to the presence of the minerals chlorite, actinolite, or epidote, hence the term 'green' and 'stone'. Greenstone is often formed through metamorphsis along a convergent plate boundary. In the rock cycle (the series of processes that creates the various types of rocks) there are identified three different types of rocks, which are the sedimentary, the igneous and the metamorphic. Metamorphic rocks started out as sedimentary, igneous or earlier metamorphic rocks but changed from their original condition under the effect of high heat, high pressure or hot, mineral-rich fluid. However, if pressure or heat is too high, then the rock will melt, resulting in the formation of an igneous rock. The name used to describe these types of rocks reflects this specific inherent trait of change, since the word “metamorphic” derives from the Greek word “metamorphosis”, meaning “change of form or structure”. Metamorphic rocks form in the Earth`s crust but can be also found on the surface, due to elevation of the Earth`s surface. They are divided into two categories: the foliated metamorphic and the non-foliated metamorphic rocks. Gabbro is a highly useful mineral that is often polished to create cemetery markers and kitchen benches. It is notable for its qualities of durability, being able to withstand extreme elements and wear. Whilst not rare, Gabbro is of great utility and has been highly desirable for its qualities. 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.Greenstone is a solid hand-sized metamorphic mineral of a green colour. Greenstone is the name for any metamorphosed basic igneous rock (in the case of this specimen, Gabbro) that gains its greenish colour to the presence of the minerals chlorite, actinolite, or epidote, hence the term 'green' and 'stone'. Gabbro is a medium to coarse grained rocks that consist primarily of plagioclase feldspar and pyroxene. Greenstone is often formed through metamorphsis along a convergent plate boundary. Gabbro forms due to cooling and crystallization of magma underneath Earth's surface. Greenstone/Gabbro/from Ceres west/of Geelong. Has old Geological Survey label/and probably collected by/Richard Daintree in 1861/C.Willam 15/4/21/ Other label: 62 /greenstone, metamorphosed, igneous rock, gabbro, chlorite, actinolite, epidote, metamorphsis, rock cycle, various types of rocks, sedimentary, high heat, high pressure, mineral-rich fluid, metamorphosis, foliated metamorphic, non-foliated metamorphic, convergent plate boundary, greenish colour, minerals

Selwynite is a fine-grained, compact green rock made primarily of chromian muscovite (fuchsite) and diaspore. Corundum and fuchsite can occur together in the form of massive aggregates or nodules. Often, copper carbonates are found as earthy films or tiny crystals in joint planes. The mineral name honours the late A. R. C. Selwyn, founding Director of the Geological Survey of Victoria. The particular specimen, a mottled green stone suitable for carving was recovered and found in Heathcote, Victoria, Australia. The rarity and qualities of this mineral attracted commercial mining, which was not successful, but traces of the mine shafts still exist today, and it is still highly valued by mineral collectors.Selwynit is considered to be one of the rare forms of rock because it is composed of phosphate minerals containing zirconium. This is an extremely rare combination found in nature. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A fine grained rock composed of mainly of chromian muscovite (fuchsite) diaspore and corundum.geological specimen, geology, geology collection, burke museum, beechworth, mineralogy, heathcote, mineral collectors, selwynite, green rock, rock specimen

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

This photograph depicts a reef mine in Beechworth. Reef mining, or quartz reef mining, was common in 19th Century Victoria. This gold mining technique requires mine shafts to be sunk into underground quartz reefs, with horizontal tunnels dug from the original shaft at differing levels to find the gold-bearing rock. The quartz would then be hoisted to the surface, which would then be pounded to access the gold in its metallic state. Gold was discovered in Beechworth in February 1852, at Spring Creek. Within 11 months of that discovery, over 8000 hopeful prospectors quickly descended on this region, transforming it into a thriving, wealthy township. Reef mining and hydraulic sluicing were gold mining techniques used in this region in the 19th and early 20th centuries. This photograph interestingly contains dogs alongside the miners. While dogs have been recorded as deterrents to thieves in the Victorian goldfields, these dogs appear as companions to these men.The search for gold is ingrained into the history of Victoria and therefore, images like this one can reveal important information for society and technology for the date when the photograph was taken. It also shows a location where reef mining was undertaken which provides insight into the impact on the environment at a time when it was done. Although quartz is one of the most common minerals found in the earth's crust, it does not always contain gold. Those reefs that do are rare and highly sought after by prospectors. The Beechworth Burke Museum has additional images relating to gold mining which can be analysed and studied alongside images like this one.Sepia coloured rectangular photograph printed on gloss photographic paper. Obverse: Reverse: United Shire of Beechworth/ Shire Secretary/ Reef Mining, Beechworth./ 6167.abeechworth, burke museum, gold, gold mining, gold rush, victorian gold rush, reef mining, quartz, companion dog, horse and cart

Produced by the VCE Consultative Committee: Women's Art Register in 1991 at a time when art courses in secondary schools had little material to use in relation to Australian women artists. An invaluable resource for secondary school teachers to broaden the scope of student knowledge about women artist's and thereby offer alternative role models for art students. This slide kit and booklet is a comprehensive, practical resource which provides a rare snapshot of women's art practices in the early 1990s. It is an excellent resource for research and teaching purposesKit containing 74 page booklet and 36 slides, activities, artist's comments and other source materials. Published in 1991 by the Women's Art Register. Artists include Elizabeth Gower, Sally Smart, Wendy Stavrianos, Pam Hallandal, tori de Mestre, Lyn Moore, Deborah Halpern, Tracey Moffat & Jill Orr. Cover image by Jill Orr, 'Walking on Planet Earth'elizabeth gower, sally smart, wendy stavrianos, pam hallandal, tori de mestre, lyn moore, deborah halpern, tracey moffat & jill orr.