An antique thick heavy brown covered children's book entitled - The Leisure Hour 1887. The front cover has the title printed in large gold lettering surrounded by black outlined flowers and leaves. It is a bound edition of a collection of British general interest periodicals of the Victorian era. It has a variety of genres of fiction and factual stories, historical and topical. There are black and white illustrations throughout with some large frontispiece ones too. The stained back cover has a bunch of wildflowers printed in black outline. 860p.non-fictionA book of British general interest periodicals of the Victorian era which ran weekly from 1852 - 1905. Each issue mixed multiple genres of fiction, and factual stories, historical and topical. The articles were a mix, including biographies, poetry, essays and fiction. Each issue usually started with a piece of serialised fiction.magazines, fiction books, historical fiction, children's books, non fiction book

The map was created by Tulloch and Brown. David Tulloch was one of the earliest engravers and lithographers in the state of Victoria. He arrived in Melbourne from Greenock, Scotland, on 3 January 1849. Following the discovery of gold Tulloch went to the Victorian goldfields in 1851, commissioned to make sketches of the diggers and the diggings for Ham’s Illustrated Australian Magazine. In November 1852 Tulloch set up in business as engraver, draughtsman, copperplate printer and lithographer. Tulloch took a map engraver, James Davie Brown, into partnership in March 1853; the several maps and specimens of commercial engraving they showed at the 1854 Melbourne Exhibition were awarded a bronze medal. That year Tulloch and Brown also received a silver medal at the Victorian Industrial Exhibition. The partnership was dissolved towards the end of 1856.This is a very early map of the Colony of Victoria including Belvoir (now know as Wodonga).A foldable map mounted on linen and with a board cover. It records the Colony of Victoria according to Surveyor's Records revised in 1857. Areas of the map are shaded to highlight different counties.At bottom right hand section of map: Tulloch & Brown's map of the Colony of Victoria : comprising part of New South Wales, the boundaries, counties, also seaport & inland townships, the gold fields with the latest discoveries, roads, tracks, &c. &c. / compiled from drawings in the Survey Office and correctly revised till 1857. Respectfully dedicated by Permission, to the Honorable Captain Andrew Clarke R.E. Surveyor General of Victoria by His Obediant Servants Tulloch & Brown, Engravers & Publishers, Melbourne". At bottom right below border : Published as the Act directs by the Proprietors, Melbourne, 1st Feb. 1856. tulloch and brown maps, rare maps victoria, victorian cartography

Spiral boundnon-fictionA history of Baranduda in Northeast Victoria. Baranduda is a rural area and, since the 1970s, a rural and residential locality formed under the authority of the Albury Wodonga Development Corporation. It is near the junction of Yackandandah Road and the Kiewa Valley Highway, 10 km south-east of Wodonga. This publication traces the history of the area from its earliest know indigenous inhabitants, through the days of the earlier establishment of pastoral runs to more recent developments.baranduda, pioneers victoria, huon family, wodonga pioneers

This black and white photograph shows the front view of the Ovens Benevolent Home with one person sitting on a bench seat against the nearest part of the building and another person walking on the grass. This photo is estimated to have been taken in the early 1900’s when the Ovens Benevolent home would have still been fairly contemporary. According to Woods (p. 121) in the 1860’s the government spent considerable sums to establish several public buildings such as the Benevolent Asylum, the Hospital and Insane Asylum to support those in need of care in the area directly after the Indigo gold rush which had left Beechworth, a fairly remote regional and newly formed township (Gold was first discovered in Beechworth in 1852) with a number of infirm and destitute people in its wake and which due to the support and establishment of these facilities ‘made Beechworth a significant social welfare centre in Victoria’ (Woods, p. 121). Originally named the Benevolent Asylum, the building was renamed as The Ovens Benevolent Asylum in 1935 and again to The Ovens and Murray Home in 1954. The building construction began in 1862 and was unique in its features of Flemish Gothic Revival style which utilised red brick and granite, ‘the main facade is dominated by four curved, Flemish gable ends, […] incorporates paired windows of pointed Gothic form and dark brick diaperwork patterning. The adjacent J. A. Wallace Wing of 1899 was designed by Donald Fiddes as a separate building. Also constructed of red brick, Fiddes adopted a conservative approach, designing a simple domestic scale building with central projecting gable porch and flanking bull nosed verandahs.’ (https://vhd.heritagecouncil.vic.gov.au/places/118). Initially established to provide housing and care for aged, orphaned or widowed members of the population, over time the Ovens Benevolent Home focused more on the age care responsibility which functioned as such up until 2005.The Ovens Benevolent Home is significance due to its association with the early development of Beechworth. It shows the civic, social welfare development that took place in the town after the peak of the gold rush which helps to establish the character of the community being built at the time and their cultural values at play. This photograph also clearly shows the early functioning landscape of that building and its purpose as well as the significant elements of its aesthetic significance and unique and striking architectural forms of the building.Black and white rectangular photograph [copy from slide]Reverse: / 7588 /housing and care, aged care, donald fiddes, ovens benevolent home, flemish gable, brick diaperwork, photograph, black and white photograph, public building, benevolent asylum, indigo gold rush, beechworth, the ovens and murray home

This specimen was recovered from Mica Schist, Canada. Chalcopyrite is a copper iron sulfide mineral with a chemical composition of CuFeS2. Its name derives from the Greek words for copper (chalco-) and brass (pyrite). It can be found in shades of yellow, green and grey, and, when exposed to acid, it can change to purple, blue, violet and yellow tones. Weathering can cause loss of its metallic luster and its brass-yellow colour. Chalcopyrite forms under various conditions, with the most significant deposits being hydrothermal in their origin. It is known globally as the most important ore of copper for thousands of years, and is thus considered a very important mineral formation. Given its golden appearance, it is often confused for the mineral gold, earning it the popular reputation as 'fool's gold' or 'yellow copper'. However, it can be straightforwardly distinguished from gold; the latter is soft, with higher specific gravity and a yellow streak, whereas chalcopyrite is brittle, easily scratched by a nail, and has a greenish grey streak. Copper was the first metal that was used by people. It was discovered by the Neolithic man about 9,000 years ago and it gradually replaced stone as it was easier to be shaped. In Australia, search for copper began after the European settlement, leading to the discovery of substantial deposits, like the one at the Olympic Dam in South Australia, which is regarded as one of the largest copper deposits in the world. Chalcopyrite has been used for copper since smelting processes began approximately five thousand years ago. Although by no means rare, this the specimen of this mineral can be used to reflect a wider history of industrial uses of copper for a significant portion of human history. 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 iron sulfide mineral of brass yellow, often with an iridescent tarnish, with greenish-black streak and submetallic luster. Chalcopyrite can be formed in several ways, including crystalizing from accessory minerals in igneous rocks, or from magma or within volcano sulfide deposits. Most commonly, chalcopyrite are found in hydrothermal conditions, where it forms in hydrothermal veins. As a member of the tetragonal crystal system, it often takes the shape of tetra-headed crystals, often with striations along the sides of the crystals. #18 Copper pyrites/(chalcopyrite) in/Laurentian Slate/(page 315 of inventory)/page missing from/descriptive catalogue/ Other label: 81 /fool's gold, chalcopyrite, mineral, rock, geology, geological, hydrothermal, neolithic, european settlement, olympic dam, south australia, stone, deposits, specific gravity, greenish grey streak, brittle, mineral gold, metallic luster, cufes2, greek words

John Halfey (1825-89) was born in Southport, Lancashire and migrated to Victoria in 1852. After finding gold at Sandhurst, and representing the latter in the Victorian Parliament, he moved to Melbourne to engage in various commercial pursuits, including directorships of insurance, mining and banking companies. A resident of Kew from the late 1850s, he was known for the hospitality provided at his house Ordsall (later Southesk) in Cotham Road. On 14 December 1860, Halfey chaired a public meeting calling for separation from the Boroondara Roads Board, which led, four days later, to the proclamation of Kew as a separate municipality. He was elected to the Council in 1861, replacing Cr. Oswin, and subsequently served as the second Chairman of the Municipality in 1862-1863. John Halfey became a trustee of Holy Trinity Church in Bulleen Road (now High Street) in 1862. He was to resign from Council after four years in 1865. Twenty-four years later in January 1889, he died aged 63 from a seizure, at his rooms at the Herald Office. He was interred in the Boroondara General Cemetery where his monument is the tallest in the Cemetery. Donated by Eileen Grigg, 2017Small, full-length portrait of John Halfey in an original gilded frame. The artist depicts him formally dressed in a frock coat beside an open window. He is shown holding a document or perhaps a pair of gloves. The painting is badly damaged with a hole in the area of his face that has been patched and repainted.john halfey, ordsall, chairman of kew, boroondara roads board, municipality of kew

Originally called Graham's South Moon Mine was situated on the Garden Gully Reef, Eaglehawk. Initially owned by George William Graham (1827-1896) who was born in England. George moved out of mining in 1855 when he opened a hotel and store at Milkmaids flat and later he opened a business in Emu Creek. He retired from business in 1870 but then invested in various mining enterprises. HE married twice in 1852 and 1878.Horwood Collection - South Moon. Some of the remains at the site of the South Moon Mine. Markings; The remains of the state battery South Moon. OCT65Kodakmine, gold, south moon, horwood collection - south moon. some of the remains at the site of the south moon mine

Today’s Panton Hill Hotel was built around 1920. Published: Nillumbik Now and Then /​ Marguerite Marshall 2008; photographs Alan King with Marguerite Marshall.; p61 Panton Hill was originally known as Kingstown, and consisted of only one hotel when the Orams Reef was discovered in 1859. Kingstown was a quartz mining centre and many old mine shafts remain in the area.1 Orams Reef was one of the first reefs with a rich find of gold in the area. The Hotel Francais, which had been operating in 1861, was well situated on the way to Queenstown (later St Andrews). So was Herr Hirt’s Hotel and store at Smiths Gully. The Kingstown hotel, known as the Frenchman’s and in 1864 as the Hotel de France, was run by a Monsieur Emile Hude and his wife Jeanne, and known for its good food. They hosted social events, business conventions and debates, attracting patrons from as far as Melbourne. The hotel’s name was changed to Panton Hill Hotel in 1905.2 In 1883 Charles Caudwell built another hotel nearby, possibly in Long Gully Road,3 which it is thought, was burnt down early last century. Today’s Panton Hill Hotel, built around 1920, is the only one of the cluster of buildings in the main road, not to date from around the turn of last century. It was severely damaged by fire in 2003, then underwent extensive alterations. It is the township’s only hotel and is an example of a modest hotel building exterior, constructed early last century. In its early days the hotel also housed the first post office, newsagency and store. Orams Reef yielded a total of £100,000, and fossikers also found alluvial gold in the creeks and gullies, but there is no record of the total value of their finds.4 Gold greatly increased the Panton Hill population, which peaked between 1865 and 1885. On holidays large sports meetings were held with wood chopping contests and foot races and the day would end with a ball. Miners came from various countries to seek their fortune, including many from China. The Chinese became unpopular however, and gradually left the district, although some stayed and grew and sold vegetables.5 Panton Hill was named after Joseph Panton, who in 1862 was appointed Police Magistrate for the Woods Point, Heidelberg and Yarra districts. Panton was an outstanding man, who in 1852, was Commissioner of Crown Lands and Assistant Commissioner of Goldfields at Bendigo. In 1874 he was promoted to Chief Magistrate for the Melbourne Police. Panton was also an artist, becoming president of the Victorian Arts Society in 1888, and in 1913, president of the Royal Geographical Society. Despite Panton Hill’s prosperity, it still lacked many services as poor roads made access to Melbourne difficult. A horse-drawn mail coach travelled to Melbourne until 1890, when the railway came to Heidelberg. The nearest doctor was at Yarra Glen or Heidelberg, and the Indian hawker Singh’s annual visit was very welcome. A miner’s shack opposite the school was used as a post office. Today’s general store and post office in the main road dates from early last century, and has changed considerably. While most people searched for gold, the more enterprising ones established farms to feed the diggers. Farmers grew wheat, barley and oats, and sent animal skins to the Eltham tannery, to make furs in Melbourne.6 As gold became scarce from around 1880, miners took up farming on 19 to 20 acre (8ha) allotments. The first settlers in Cherry Tree Road included Purcell, Smith, Owens, Hughes and Shillinglaw. By 1900 all the land had been taken up around Panton Hill and Hurstbridge. The orchards in Panton Hill and the wider district, particularly of apple and pear, were very successful, and made Panton Hill a cohesive and successful community. About 1914 the Moores built the first cool-store and refrigeration plant at their orchard in Cherry Tree Road. Many settlers planted vineyards and made high quality wine, but in 1922 the blight destroyed them.This collection of almost 130 photos about places and people within the Shire of Nillumbik, an urban and rural municipality in Melbourne's north, contributes to an understanding of the history of the Shire. Published in 2008 immediately prior to the Black Saturday bushfires of February 7, 2009, it documents sites that were impacted, and in some cases destroyed by the fires. It includes photographs taken especially for the publication, creating a unique time capsule representing the Shire in the early 21st century. It remains the most recent comprehenesive publication devoted to the Shire's history connecting local residents to the past. nillumbik now and then (marshall-king) collection, panton hill hotel

Olivine is mostly found on the Earth's surface in igneous rocks that are dark-coloured. It is common at divergent plate boundaries and at warm spots, such as volcanic areas. It crystalises and forms during the cooling of magma. Olivine is used in refractory sand, bricks, and gemstones. Olivine has been found on a number of meteorites, which might have originated from large asteroids or the mantle of a now-destroyed planet. This olivine crystal is thought to originate from Mount Noorat, with speculation that it could have originated from Mount Shadwell. Mount Noorat is a dormant volcano cone located in the Newer Volcanics Province of Victoria. Mount Noorat belongs to the Kirrae Wuurong people, who used the Mount as a place for meetings and gatherings prior to European settlement. Contact was first made between European settlers and the Indigenous people in 1841. The Mount has mostly been used for cattle and sheep grazing. Mount Shadwell is a well-known source of olivine and is the highest of a gathering of volcanic cones. The New Volcanic Province is located in South East Australia and covers 15000 square kilometres. It contains 400 explosive vents and small shield volcanoes. The last eruption is thought to have occurred 5000 years ago at Mount Gambier and Mount Schank. This olivine crystal has been identified as a volcanic bomb, which is a molten rock which was pushed out and ejected into the air when a volcano reupts. A rock needs to be larger than 65 mm in diameter to be classified as a volcanic bomb. This olivine volcanic bomb and its locality is historically and socially significant. The olivine was found in the Newer Volcanic Province, an area which contains over 400 dormant volcanoes. This olivine is one part of a volcanic bomb, which would have ejected when magma erupted out of a volcano. 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 iron-magnesium silicate mineral with shades of green and brownburke museum, beechworth, geological, geological specimen, olivine, igneous rock, volcanic, gemstones, volcanic bomb, meteorites, asteroids, plantes, mount noorat, mount shadwell, indigenous, kirrae wuurong people, newer volcanics province, victoria, european settlement, eruption

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

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

Thunderegg Agates are formed within rhyolite volcanic ash layers. They are rough spherical shapes, varying in size from less than an inch to over a metre long. Thundereggs usually contain centres of chalcedony which may have been fractured followed by deposition of agate, jasper or opal, either uniquely or in combination. A unique characteristic that these specimens have is the fact that they often look like ordinary rocks on the outside, but slicing them in half and polishing them may reveal intricate patterns and colours. These particular specimens are examples of thunderegg agates. Agate is a variety of chalcedony, a cryptocrystalline form of quartz. The agate component contributes to the intriguing internal patterns of the specimens. The specific locality of these specimens is unknown but they can be found in flows of rhyolite lava. They are formed in gas pockets in the lava, which act as moulds. These specimens can be found globally, with specific locations in Germany being particularly abundant. 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.Two small solid specimens with pale, sandy-coloured exteriors and fractured internal patterns. burke museum, beechworth, geological, geological specimen, thundereggs, thundereggs agate, agate, rhyolite, rhyolite lava, volcanic ash, chalcedony, cryptocrystalline

A fossil refers to any remains or traces of past life that are preserved in the rock. It could be remains of plants or animals. Fossil leaves are commonly found on different types of rocks. These fossils can go as far back as the Triassic Age just like the series of fossil plants collected at Denmark Hill, Ipswich in Queensland. Fossils leaves are formed when dead plants get buried by sediments like mud, sand, or volcanic ash. Often, it gets detached cleanly from stems along a special layer of weak cells, then twigs, and, less commonly, cones of conifers and fruits and seeds of flowering plants. Over time, the leaves or pieces of leaves get buried by more sediments and eventually gets 'lithified' or hardened into a rock. Erosions and mining can cause the rocks to break and reveal the fossils buried in it. Fossilisation frequently takes place at sites in the lowlands where deposits of clay, silt, sand are found. This is usually due to weathering and erosion of rocks. Fossil leaves can provide information about ancient Australia's way of living. It contributes to Victorian biodiversity records and its botanical collections. It also contributes information on the geographical profile of Victoria as fossilisation usually occur at estuaries and deltas of rivers, river flood plains, ponds and lakes. 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.Piece of light brown rock with fossilised leaves in shades of golden yellow and brown.Existing label: Fossil Leaves / Locality unknown / might be worth checking if this is Glossopteris, a Permian age plant. / C. William 16/4/21 geological specimen, geology, geology collection, burke museum, beechworth, fossil leaves, fossilization, 1868 geological survey of victoria, lithified, rocks, fossilised leaf, rock, fossils, leaves

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

Galena is the natural compound of lead and classed as a sulphide, it crystallises in a cubic pattern and its chemical formula is PbS. Galena is a primary source of both lead and silver. This specimen of Galena comes from Broken Hill. Broken Hill has one of the world’s largest and most significant deposit of ore for the production of lead. Mining of Galena at Broken Hill began with the staking of land by Charles Rasp in 1883. By the following year, in 1884, Rasp and six others had formed Broken Hill Mining Company. Broken Hill Mining Company eventually evolved into BHP group limited and is currently the largest mining company in the world and the largest company in Australia. There is archaeological evidence from artefacts discovered in Turkey that humans have been extracting lead from galena by the process of smelting since at least 6500 BCE. This specimen also has quartz on the top surface which is frequently discovered alongside Galena. This mineral specimen is of historic significance as a sample of Galena extracted from Broken Hill during the 19th century. Mining for Galena in Broken Hill begin in 1883 by Charles Rasp and evolved into the world’s largest mining company – BHP Group Limited. Broken Hill is one of the world’s most significant deposits of ore for the production of lead. 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 flat, hand-sized, grey sulphide specimen that is the natural compound of lead with a quartz formation on the top surface. Existing Label: GALENA / (with quartz) / Locality: Broken Hill / N.S.W 120 x 70 x 29geological specimen, geology, geology collection, burke museum, beechworth, galena, galena quartz, quartz, charles rasp, broken hill mining company, bhp group limited, bhp, lead, ore, lead sulphide, sulphide, silver, broken hill

Sphalerite or sphaelerite is named from the Greek word for 'treacherous' or 'deceiver' as specimens can vary widely in appearance, making them hard to visually identify. It is a zinc sulfide with the chemical composition (Zn,Fe)S, the most important ore of zinc. Specimens of sphalerite can contain iron as a substitute for up to 25% of the usual zinc present, as well as trace elements of gallium, cadmium, geranium and indium. Small amounts of arsenic and manganese may also be detected. Sphalerite is found in igneous, sedimentary and metamorphic rocks. It forms when carbonate rock encounters acidic, zinc-bearing fluid. It often forms in veins or in fissures of the existing rock, with colours and crystal shapes dependent on the composition of the the combining elements. It forms isometric crystal shapes including cubes, tetrahedrons, octahedrons, dodecahedrons. This specimen was collected in approximately 1852, in Broken Hill, NSW, as an adjunct to the Geological Survey of Victoria. It was donated to the Museum in 1868. Victoria and other regions of Australia were surveyed for sites of potential mineral wealth throughout the 19th Century. The identification of sites containing valuable commodities such as gold, iron ore and gemstones in a locality had the potential to shape the development and history of communities and industries in the area. The discovery of gold in Victoria, for instance, had a significant influence on the development of the area now known as 'the goldfields', including Beechworth; the city of Melbourne and Victoria as a whole.The specimen is significant as an examples of surveying activity undertaken to assess and direct the development of the mineral resource industries in Victoria and Australia, as well as the movement to expand human knowledge of earth sciences such as mineralogy and geology in the nineteenth century.A pipe-shaped specimen of sulfide-mineral zinc ore displaying patches of black, brown, beige and gold colouring. The main item has associated broken pieces. geological specimen, geology, geology collection, burke museum, beechworth, mineralogy, indigo shire, geological survey, sphalerite, sphaelerite, zinc ore, broken hill, nsw, victoria, galena, fluorite, chalcopyrite, lead, cadmium, gallium, germanium, indium, iron

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

Gold was first discovered in 1852 on what was then named Korong or Mt Korong goldfields. It was soon found that the area was not suitable for alluvial mining because of a lack of water but quartz mining was more successful. The township of Wedderburn was surveyed 1856/57. The first public crushing works was established in 1859.Hardcover book with printed dust jacket and plastic cover. 92 pages with black and white illustrations, fold out map and index. Covers the history of the Wedderburn Goldfields and the discovery of gold generally in Australia from the 1850s until c1880s. Written by Joshua R Gray and edited by Frank Cusack.Joshua R Gray and Frank Cusack.gold, goldfields, goldfield