Taken some time after 1864, these photographs depict the Star Hotel both directly (8674.1) and from the Hotel north west down Ford Street (8674.2). The images depict the building with its modern exterior, having settled for this brick form after several other building designs. The Star Hotel was the first hotel opened in Beechworth, and would go through a series of dramatic changes under its first three owners. The original timber structure was built by W.H. Neuber, though at the time it was only known as ‘The Beechworth Hotel’. The site was later purchased in 1855 by mining entrepreneur, and prolific business owner, John Alston “Six Stars” Wallace. He would go on to extend the established hotel, rebuilding much of it with weatherboard and a shingled roof, adding a two storey structure with a verandah and a theatre capable of supporting 400-500 people, which was often used for international performances. Renamed as the Star Hotel, it was the second in a chain franchise, eventually leading to the “Six Stars” moniker Wallace went by, with hotels at Rutherglen, Chiltern, Yackandandah, Bright, Snake Valley, and of course, Beechworth. Under his ownership, it developed into a popular location for merchants, wayfarers, and locals alike, with the help of his brother Peter as manager. Situated on a road once synonymous with Melbourne to Sydney roadtrips, and the allure of the gold mines, the popularity of the Star drew all manner of clientele from across the country. As such a central hub, the ‘Star Assembly Rooms’ were used as a meeting place for debates, discussions, festivities, and problem solving among the various working sects of the area. These meetings included shareholder discussions for prospecting companies, railway planning, council meetings, and discussions surrounding the interactions between European and Chinese miners, both good and bad. By late 1856, John had the Beechworth at auction through J.H. Grey & Co. It was most likely due to the high profile murder of the manager, Robert Murdoch, during an altercation in relation to a dine and dash event by a Swedish miner, Charles Jansen, who had been ‘excited by drink’ on November 17th. He had refused to pay for his meal and waiter James Mitchell failed to persuade him otherwise. Mitchell, or possibly Murdoch himself, forced him out as tempers and threats escalated. As the photos tell, there are a number of doors which may be entered through, and Jansen used an alternate entrance to access the building. Murdoch was investigating the noise when he encountered the furious man. He was subsequently stabbed with no warning by a small clasp knife, as he tried to stop the intrusion. His exclamations, "I’m stabbed, I’m stabbed!” alerting other occupants, and Jansen was restrained and arrested. Murdoch died the next day from his injuries, with the inquest carried out on the theatre stage. Some 3000 members of the town attended the funeral, and the Star hung black cloth in memory of Robert and his death. Afterwards, an auction caw the property pass to Messrs Robertson and Quirk, though would return shortly thereafter to Six Stars’ portfolio. Six Stars would later sell off his properties from 1862, with the Beechworth Star purchased by 1864 by John Sitch Clark. This allowed Clark to redevelop a significant portion of the Hotel, stripping a central section and constructing the brick structure that survives today, reopening the Star in July that year. It was after this time that our photographs were taken. Clark would later sell the property to Frank Mitchell, shortly before his own death. The next owner, Frederick Allen, lived on the property before the deed was sold to him in the 1880s. He would later sell the property to William Carroll in 1890, with proprietorship eventually moving to Mr. W.H. Porter, and transferring to a Mr. Marendaz by 1913 and Mr. Holly in 1915. Licensing disputes would arise 1917 between Margaret Carroll and a Mrs. McDonald, before it became delicenced some years prior to 1935. It was around this year that the property was bought by Mr. W.J. Pemberton at the meagre price of £500, down from the £13,000 Six Stars originally auctioned it for. It served as a Youth Hostel for a period of time around 1972, and currently the building serves as a private accommodation on the second floor, with shops taking up the ground floor level.These photographs of the Beechworth Star Hotel as they depict a form of Beechworth's first hotel, and also the site of a high profile murder. Two black and white rectangular photographs printed on matte photographic paper.8674.1 (reverse) Beechworth/ 734/ Tanswell’s Hotel [crossed out]/? Old Star/ Hotel,/[small pencil scratching]/ Saunders/ BMM 8674.1 8674.2 (reverse) Beechworth/ 60%[circled]/ Old Star Hotel/Building etc.,/ 12 ½ cm/ 3"[circled, arrows extending horizontally to edges]/[arrows extending top to bottom mid-right of reverse]/ Saunders/ 734[circled]/ BMM 867.2,/ [thin scribbled bordering around top, right, and bottom edges]star hotel, beechworth hotel, john alston wallace, ja wallace, john sitch clark, frederick allen, robert murdoch, meeting place, tragedy, theatre, mining town

Depicted in the photograph are ten miners standing at a cliff face using a high pressure hose, in Beechworth, Victoria. The miners are located in the Three Mile Creek division, in the Beechworth Mining District established January 4th 1858 under An Act for Amending the Laws Relating to the Goldfields by the Governor-in-Council. The Ovens Gold Rush began at Beechworth in February 1852 and was followed by Yackandandah and the 'Indigo Goldfield'. The strategies applied to mining in Beechworth were distinct in comparison to other goldfields in Victoria such as Bendigo and Ballarat. The miners in Beechworth utlised 'hydraulic sluicing' to remove washdirt, the long water races and deep tailraces constructed through solid rock with an estimated 900 miles of water races cut through the Beechworth fields by 1880, demonstrating great engineering feats. The photograph taken is significant as it is a visual representation of the mining strategy, 'hydraulic sluicing' that was particularly unique to the Beechworth mines, particularly in Victoria and an engineering feat.Black and white rectangular photograph printed on matte photographic paper, unmounted print.beechworth mining district, mining, three mile creek division, three mile creek

The Powder Magazine was built in 1859 by T Dawson and Company for fifteen hundred pounds and was restored in 1966 by the National Trust. The building was constructed to store black-powder used by miners on the goldfields for blasting for mining and quarrying as legally, miners had to leave bulk gunpowder the Powder Magazine overnight. Due to the passing of an 1857 act regulating the importation, transportation and importation of black powder, several Powder Magazines like the Beechworth Powder Magazine were constructed. The Magazine Powder is uniquely designed to ensure that in the chance of an explosion, the explosion is minimalized by travelling vertically rather than horizontally. The Powder Magazine was constructed using granite, slate roofing and a high stone wall and includes several safety features including wooden nails, lightning rod and a solid outer wall. This photograph is historically significant as it documents the development of laws related to mining, the actions taken to ensure the safety of those nearby potentially dangerous equipment and the architectural skills to design a storage facility to minimize damage caused by a potential explosion. A sepia toned rectangular photograph printed on matte paper.Reverse: Beechworth Candid Photos/ Phone 281570/ 5 Finch Street 3747/historic building, beechworth historic building, powder magazine, beechworth

Mayday Hills Mental Hospital was originally constructed in 1864 under the name of the Beechworth Lunatic Asylum. It was built for locals in need of help who were kept in the local gaol. In its first decade, the residents of the hospital were used as menial labourers but over time, as mental healthcare progressed, were cared for in more nuanced ways. This site became a training hospital for nurses in the 1960's. Eventually, mental health patients were moved to other care facilities and Mayday Hills was operating as a geriatric care facility. It was closed in 1995, after which the buildings and their grounds were purchased to La Trobe University to be used as a campus. The university sold the site in 2011 to private ownership. The image depicts an interior room which is presumed to be a dining or common room. This space has been decorated for Christmas.Mayday Hills Mental Hospital is a historically significant site for many factors. It is representative of healthcare practice in nineteenth century Victoria. It contains rare examples of construction and architecture. It is also significant for aesthetic and technical reasons. Black and white rectangular photograph printed on photographic paperObverse: PRINTED BY/ L.MAHER/ BEECHWORTH/ 1997.2702mayday, mayday hills hospital, mayday hills, mayday hills mental asylum, beechworth lunatic asylum, lunatic asylum, beechworth, gaol, beechworth hospital for the insane, beechworth mental hospital, mental hospital, hospital, nurse, nurses quarters, la trobe university, training facility, christmas, christmas party

Mayday Hills Mental Hospital was originally constructed in 1864 under the name of the Beechworth Lunatic Asylum. It was built for locals in need of help who were kept in the local gaol. In its first decade, the residents of the hospital were used as menial labourers but over time, as mental healthcare progressed, were cared for in more nuanced ways. This site became a training hospital for nurses in the 1960's. Eventually, mental health patients were moved to other care facilities and Mayday Hills was operating as a geriatric care facility. It was closed in 1995, after which the buildings and their grounds were purchased to La Trobe University to be used as a campus. The university sold the site in 2011 to private ownership. This image depicts people enjoying the grounds and gardens.Mayday Hills Mental Hospital is a historically significant site for many factors. It is representative of healthcare practice in nineteenth century Victoria. It contains rare examples of construction and architecture. It is also significant for aesthetic and technical reasons.Black and white photograph printed on matte photographic paperReverse: at the Beechworth Lunatic Asylum/ (wade)/ do not copy - copy for Burke Museum/ for collection only only/ BMM 8326mayday, mayday hills hospital, mayday hills, mayday hills mental asylum, beechworth asylum, beechworth lunatic asylum, beechworth mental hospital, beechworth institution, healthcare, mental health, nurses quarters, nurses, gaol, garden, garden party

Mayday Hills Mental Hospital was originally constructed in 1864 under the name of the Beechworth Lunatic Asylum. It was built for locals in need of help who were kept in the local gaol. In its first decade, the residents of the hospital were used as menial labourers but over time, as mental healthcare progressed, were cared for in more nuanced ways. This site became a training hospital for nurses in the 1960's. Eventually, mental health patients were moved to other care facilities and Mayday Hills was operating as a geriatric care facility. It was closed in 1995, after which the buildings and their grounds were purchased to La Trobe University to be used as a campus. The university sold the site in 2011 to private ownership. This image depicts the front facade of the building and a portion of the gardens, including a fountain. Mayday Hills Mental Hospital is a historically significant site for many factors. It is representative of healthcare practice in nineteenth century Victoria. It contains rare examples of construction and architecture. It is also significant for aesthetic and technical reasons.Black and white photograph printed on matte photographic paperReverse: Mental Hospital/ Beechworth Lunatic Asylum/ Xmas 1930/ 8190 VELOX (Watermark)mayday, mayday hills hospital, mayday hills, mayday hills mental asylum, beechworth, beechworth asylum, beechworth lunatic asylum, beechworth hospital for the insane, garden, gardens & parks, architecture, historic victorian architecture, healthcare, health, fountain, la trobe university

Mayday Hills Mental Hospital was originally constructed in 1864 under the name of the Beechworth Lunatic Asylum. It was built for locals in need of help who were kept in the local gaol. In its first decade, the residents of the hospital were used as menial labourers but over time, as mental healthcare progressed, were cared for in more nuanced ways. This site became a training hospital for nurses in the 1960's. Eventually, mental health patients were moved to other care facilities and Mayday Hills was operating as a geriatric care facility. It was closed in 1995, after which the buildings and their grounds were purchased to La Trobe University to be used as a campus. The university sold the site in 2011 to private ownership. This postcard depicts an interior room which is presumed to be a living or reception room. It is filled with period furnishings. Mayday Hills Mental Hospital is a historically significant site for many factors. It is representative of healthcare practice in nineteenth century Victoria. It contains rare examples of construction and architecture. It is also significant for aesthetic and technical reasons.Black and white postcard printed on matte cardReverse: 11.5.35/ Miss Peach/ Best wishes/ from/ P. Beckman mayday, mayday hills hospital, mayday hills, mayday hills mental asylum, mayday hills mental hospital, beechworth, beechworth asylum, beechworth hospital for the insane, beechworth lunatic asylum, lunatic asylum, healthcare, health, living in country towns, living room, furniture, interior

Mayday Hills Mental Hospital was originally constructed in 1864 under the name of the Beechworth Lunatic Asylum. It was built for locals in need of help who were kept in the local gaol. In its first decade, the residents of the hospital were used as menial labourers but over time, as mental healthcare progressed, were cared for in more nuanced ways. This site became a training hospital for nurses in the 1960's. Eventually, mental health patients were moved to other care facilities and Mayday Hills was operating as a geriatric care facility. It was closed in 1995, after which the buildings and their grounds were purchased to La Trobe University to be used as a campus. The university sold the site in 2011 to private ownership. This postcard depicts the Mayday Hills Mental Hospital (Titled as 'Asylum for insane') from a distance and includes the surrounding grounds and farmlands.Mayday Hills Mental Hospital is a historically significant site for many factors. It is representative of healthcare practice in nineteenth century Victoria. It contains rare examples of construction and architecture. It is also significant for aesthetic and technical reasons.Sepia tone postcard printed on matte cardObverse: Beautiful Beechworth (Vic.) 1880 ft. above Sea Level - General View of Asylum for Insane/ Copyright F. Foxcroft Reverse: 1997.2459/ Post Card/ THIS SPACE MAY BE USED FOR CORRESPONDENCE/ THIS SPACE FOR NAME AND ADDRESSmayday, mayday hills hospital, mayday hills, mayday hills mental asylum, mayday hills mental hospital, beechworth, beechworth asylum, beechworth hospital for the insane, beechworth lunatic asylum, beechworth mental hospital, healthcare, health, rural australia, farm, architecture, historic victorian architecture, classical architecture

Two rectangular black and white photographs of the Beechworth Mental Hospital (Mayday Hills) administrative building showing the left and right hand sides of the exterior building with three cars parked in driveway turning circle in the foreground taken in the 1950's by E. Yellard. Mayday Hills Hospital, originally known as the Beechworth Lunatic Asylum was constructed between 1864-67 designed by The Public Works Department. The hospital is made up of a number of buildings, landscaping, ha-ha, workshops, laundry, administrative facilities and farmland, it was constructed in 'Italianate' style by a team of up to two hundred and fifty workers (Woods p. 122). The asylum was established in response to the need for the regional shire to locally care for those particularly affected by their time working the Ovens goldfield during the Indigo Shire gold rush era where poor living conditions and isolation were significantly affecting the welfare of a great many people through poverty and lack of resources. The gaol and orphan labour systems were not able to effectively support to give housing, rehabilitation and ongoing care for the mentally ill, and transporting to Melbourne by waggon was a time consuming and counter-productive solution when the metro facilities were already overcrowded. According to Woods (A Titan's Field p. 122), between 1901 and 1911 a large percentage (thirty five percent in 1901 and twenty four in 1911) of the Beechworth population were either patients or inmates of Beechworth institutions, Mayday Hills accounted for some six hundred and seventy four patients in 1901, Beechworth's Mayday Hills was chosen as the site of Victoria's newest asylum, at the time, due to the landscape and altitude. The hilltop atmosphere and the native fauna, it was argued, would assist in the cure of the patients kept at the hospital (Wood 1985, 122). The positioning of the hospital had a beneficial effect on the rural town and the large volume of people living at the hospital and contributing to this population growth is counted as reason for the survival of Beechworth as a regional township. According to the Victorian Heritage database, during the period 1921-1950 Mayday Hills underwent some modernisation by Public Works Department architect Percy Everett which included a nurses' hostel and new ward which were further developed and continued to function as a mental hospital up until 1995 when it was sold to LaTrobe university. The building and grounds are listed on the Victorian Heritage Register under criterion A, B, D, E and F.These photographs give a good indication of the ongoing use of Mayday Hills from its original establishment in the 1860's through to almost one hundred years later when these photographs were taken. The clarity of the images combined with the style and make of the cars in the foreground give a good indication of the time period and show the continued use and need for the facility over the years. Through images of building facades such as these, we might gain fuller understanding of the structural and aesthetic characteristics to be used in any future development or restorative work.2 x black and white rectangular photographs [copies] printed on Ilford photographic paper8688.1 reverse: Beechworth / Mental / Hospital / 80% 19cm / 12 cm / 80% / 728 / New / Print / BMM / 8688.1 / E. / Yellard / [Stamped : ILFORD] 8688.2 reverse: Beechworth / Mental / Hospital / E. / Yellard / BMM / 8688.1 / [Stamped : ILFORD]administrative building, black and white photographs, beechworth, mental hospital, beechworth mental hospital, mayday hills, cars, 1950, e. yellard, the public works department, public works department, hospital, mayday hills hospital, beechworth lunatic asylum, lunatic asylum, asylum, ovens goldfield, indigo shire, indigo shire gold rush

Produced c. 1910 by The Rose Stereograph co. This colourised photographic postcard shows the exterior of the administrative buildings at Mayday Hills mental hospital with three young boys in the foreground. This postcard forms part of the extensive Rose Series. (P. 4689) of postcards being produced by the Rose Stereograph co. which depicted landmarks from across Australia. Despite the early date attributed to this image, according to Walsh dates from this series place the postcards being produced typically between 1920-54. Mayday Hills Hospital, then known as the Beechworth Lunatic Asylum was constructed between 1864-67 designed by The Public Works Department. The hospital is made up of a number of buildings, landscaping, ha-ha, workshops, laundry, administrative facilities and farmland, it was constructed in 'Italianate' style by a team of up to two hundred and fifty workers (Woods p. 122). The asylum was established in response to the need for the regional shire to locally care for those particularly affected by their time working the Ovens goldfield during the Indigo Shire gold rush era where poor living conditions and isolation were significantly affecting the welfare of a great many people through poverty and lack of resources. The gaol and orphan labour systems were not able to effectively support to give housing, rehabilitation and ongoing care for the mentally ill, and transporting to Melbourne by waggon was a time consuming and counter-productive solution when the metro facilities were already overcrowded. According to Woods (A Titan's Field p. 122), between 1901 and 1911 a large percentage (thirty five percent in 1901 and twenty four in 1911) of the Beechworth population were either patients or inmates of Beechworth institutions, Mayday Hills accounted for some six hundred and seventy four patients in 1901, Beechworth's Mayday Hills was chosen as the site of Victoria's newest asylum, at the time, due to the landscape and altitude. The hilltop atmosphere and the native fauna, it was argued, would assist in the cure of the patients kept at the hospital (Wood 1985, 122). The positioning of the hospital had a beneficial effect on the rural town and the large volume of people living at the hospital and contributing to this population growth is counted as reason for the survival of Beechworth as a regional township. Mayday Hills continued to function as a mental hospital up until 1995 when it was sold to LaTrobe university. The building and grounds are listed on the Victorian Heritage Register under criterion A, B, D, E and F. Through the colourisation of the photograph and through the unusual choice of the subject matter being used as a postcard, we can get a good indication of aesthetic interests of the time.Rectangular coloured photograph printed as postcardObverse: Beautiful / Beechworth / (Vic.) / 1800 ft. / above / Sea / Level / - / Asylum / for / insane / (Front / View) / Copyright. / F. / Foxcroft / Photo Reverse: 1997.2454 / Postcard / THIS / SPACE / MAY / BE / USED / FOR / CORRESPONDENCE: / THIS / SPACE / FOR / NAME / AND / ADDRESS / STAMPpostcard, rose series, mayday hills hospital, mayday hills, beechworth lunatic asylum, photographic postcard, george rose, the rose stereograph co., social welfare, welfare services, ovens goldfield, lunatic asylum, the public works department, australian landmark, regional shire, indigo shire council, gold rush, beechworth institution, victorian heritage register

Believed to have been taken sometime between 1858 and 1908, featuring a man with moustache, dressed in hat and long riding coat, seated on a bob-tailed horse, is stopped in the middle of a wide dirt road in Beechworth. He is outside a row of businesses, including R.McKenzie & Sons Grain Store and Mackenzie Family Store (Wholesale & Retail Est. 1855), along a sloping hill. Behind the main rider are a parked horse and laden two-wheeled cart backed up directly outside the grain store's verandah, and another man is driving a horse and four-wheeled wagon forward towards them. At the bottom of the hill is a bridge (Newtown Bridge) with forked road on the far side, leading to a number of houses on both sides of another hill. This image is looking down Bridge Street, Newtown, Beechworth and across to Ford Street (left) and High Street (right). Road-making was a focus of town development during the 1850s, and the wide streets were created on the instructions of the surveyor-general to be between sixty-six and ninety-nine feet wide to give the town a pleasing aspect.This photograph is important in showing the development and expansion of the various businesses and buildings in Bridge Street of Newtown, Beechworth. Black and white rectangular photograph printed on paperReverse: 6980/ PH 118/ 1998.00059/beechworth, new town, newtown, newtown beechworth, local business, mackenzie family store, mackenzie's family store, mackenzie, grain store, bridge, ford steet, high street, colonial australia, australian gold rushes, mining technology, beechworth historic district, indigo gold trail, migration, indigo shire, mckenzie and sons grainstore, mckenzie family store, mckenzie, newtown bridge

This photograph taken c1999/2000, depicts the Burke Museum’s granite façade and vestibule entrance. The museum's large red door is closed and there is a white sign is attached to the door. The museum site dates to the 1857 founding of the Beechworth Public Library and Athenaeum by a newly formed Young Men's Association (YMA). In 1863 the museum was dedicated as a memorial to former Beechworth police superintendent (1854-1858) and explorer Robert O’Hara Burke, following Burke’s death from malnutrition on the Burke and Wills expedition in 1861. Funded by the Victorian Government and the Royal Society of Victoria, the officially titled 'Victorian Exploring Expedition' was tasked with being the first European party to traverse Australia from south to north. The Burke Museum holds objects from the famous expedition and explores the multi-layered history of Beechworth and surrounds from the gold rush era to the present.This photograph is historically significant for its depiction of the Burke Museum c1999/2000. The Burke Museum is Australia’s oldest regional museum and part of Beechworth's Historic and Cultural Precinct, one of Australia’s best preserved historic-town sites and a popular tourist destination. Once the government centre for a vast gold fields region, this collection of nationally significant buildings tells the story of how Australia grew and prospered. The frequent use of honey-coloured local granite as a building material, which can be seen in the museum's fabric, gives Beechworth’s historic buildings a distinct and cohesive local character. This photograph captures this distinctive character and may be compared and studied alongside other images of historic buildings in the Burke Museum Photographic Collection.Rectangular colour photograph printed on photographic paper.Reverse: 7031 / Label: Burke Museum / 1999/2000 /burke museum, indigo shire, beechworth athanaeum, beechworth library, beechworth historic building, historic precinct, burke museum exhibition, from the liedertafel to the skating rink, honey-coloured local granite, robert o'hara burke, victorian gold fields, historic towns in victoria, colonial australia, liedertafel, colonial entertainments, beechworth brass band, historic victorian architecture, australia's oldest regional museum, burke and wills expedition, first europeans to cross australia, yound mens associations, beechworth tourism, things to see in beechworth, beechworth historic trail, young men's associations

This undated photograph depicts two people standing in the vestibule entrance at the Burke Museum, Beechworth. The museum site dates to the 1857 founding of the Beechworth Public Library and Athenaeum by a newly formed Young Men's Association (YMA). In 1863 the museum was dedicated as a memorial to former Beechworth police superintendent (1854-1858) and explorer Robert O’Hara Burke, following Burke’s death from malnutrition on the Burke and Wills expedition in 1861. Funded by the Victorian Government and the Royal Society of Victoria, the officially titled 'Victorian Exploring Expedition' was tasked with being the first European party to traverse Australia from south to north. The Burke Museum holds objects from the famous expedition and explores the multi-layered history of Beechworth and surrounds from the gold rush era to the present.This photograph is historically significant for its depiction of the Burke Museum and Loch Street streetscape. The Burke Museum is Australia’s oldest regional museum and part of Beechworth's Historic and Cultural Precinct, one of Australia’s best preserved historic-town sites and a popular tourist destination. Once the government centre for a vast gold fields region, this collection of nationally significant buildings tells the story of how Australia grew and prospered. The frequent use of honey-coloured local granite as a building material, which can be seen in the museum's fabric, gives Beechworth’s historic buildings a distinct and cohesive local character. This photograph may be compared and studied alongside other images of historic buildings in the Burke Museum Photographic Collection.Rectangular colour photograph printed on photographic paper.Reverse: 3440burke museum, beechworth athenaeum, beechworth library, beechworth historic precinct, robert o'hara burke, australia's oldest regional museum, indigo shire, beechworth athanaeum, beechworth historic building, historic precinct, honey-coloured local granite, victorian gold fields, historic towns in victoria, victoria's high country, colonial australia, beechworth tourism, things to see in beechworth, beechworth historic trail, historic victorian architecture, burke and wills expedition, first europeans to cross australia, young men's associations

Taken in the 1990's, this photograph depicts a row of shop fronts in the 'Street of Shops' exhibition in the Burke Museum in Beechworth. This exhibition was created and opened in 1979 and was intended to reflect and imitate a historic peirod in the town's past. The time period decpicted is that of the Gold Rush which swept through many Victorian towns from the 1850's onwards. For the town of Beechworth, the gold rush began in 1852, when gold was discovered in Spring Creek, drawing in many new residents seeking to make a fortune and transforming a once remote town into a bustling centre brimming with hope and opportunity. By 1857, the town contained over 200,000 residents and with this, the need for more amenities and intsitutions arose. Multiple churches, banks, schools, shops, hospitals and other essential buildings appearing over the years. The wealth acquired through the gold rush is largely responsible for the vast development of the town and many of its significant buildings which still remain to this day. This photograph also highlights the significance of this type of exhibition, providing a new mode of experiencing and learning about the past. The street depicts the many supporting trades and industries that arose from the mass migration during the gold rush. The creation of the Street of Shops in 1979 was envisioned by Roy Harvey who was the curator at the time, with the intention of recreating an authentic feel to the environment while collecting from the community to accurately portray the multiculturalism that is ingrainded in many towns and communities of Victoria. This photograph contains historical significance as it relates to and portrays an especially important period of time within Beechworth and Victoria's history. The gold rush phenomena ushered in a wave of hope and prosperity for citizens and immigrants alike. It provided many with the opportunity to strike it rich, while the town prospered and grew in many ways. This widespread development that accompanied the gold rush occured throughout Victoria and holds great historical importance when recording the social, economic and communal developments that occured throughout the time period which gave way to the beloved towns and communities we know today. Beechworth itself is acknowledged as Victoria's best-preserved gold mining town and deserves recognition of its significance. it also showcases the great significance of social develpment and globalization that occured throughout the state during this period. Coloured rectangular photograph printed on matte photographic paper and unmounted. Obverse: Dancing every night 8pm-6am [mirror] / Gold Diggers Arms Hotel façade / Star / Beechworth Gold / J. Davidson / Saloon Reverse: 3306 beechworth, burke museum, street of shops, gold rush, indigo shire gold rush, 1850s beechworth, burke museum exhibitions, saloon, gold buyer, hotel, historical streetscape, gold rush immigration

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

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

This specimen was recovered from Silverton Mine in Broken Hill, New South Wales. Otherwise known as the 'Day Dream Mine', the Silverton Mine was first established in 1883, when silver and lead deposits where discovered. Within a few short years, the population of Broken Hill reached 3000 people. As of today the Silverton Mine is still open, and has produced over 200 million tonnes of ore, which has generated over $100 billion. The Silverton Mine was also famous for a number of specimens such as silver, iron and zinc.Copper is considered to be a rare ore in that finding it in its pure form is rare. Nowadays when mining for Copper it is often found in mixed in with other minerals or it is recycled from use. Moreover, Copper is found in a range of everyday uses such as coins, cookware, pipes, heating conductors and anything that generate electricity. The fact that Copper is heat a heat conductor, electricity conductor and it does not corrode easily, makes this ore a versatile and useful. 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 cube-shaped sulfide and oxide with shades of green, grey and brown throughout. Copper is typically found as nuggets in the ground. It can be found in a range of forms such as its native state; mixed with other ores, such as zinc and iron; as porphyry copper deposits; and as major deposits. Porphyry deposits are when the mineral is scattered evenly throughout the rock. Major deposits are when the mineral is scattered amongst other minerals.burke museum, beechworth, indigo shire, beechworth musum, geological, geological specimen, mineraology, copper, copper ore, copper ore speciment, broken hill, new south wales

This particular specimen was recovered from the Lal Lal Coal and Iron Mine in Victoria, 19km from Ballarat. Brown Coal was discovered here in 1857, just alongside the Geelong to Ballarat Railway line. This discovery of lignite (brown coal) was the first in Victoria, which would bring important benefits to the region and state, both of which had previously been reliant on coal imports. In the 1860s, iron ore was found just 5km from Lal Lal, and the area was converted into an Iron Ore Mine. The Lal Lal Iron Mining Company took over operations in 1874, who then peaked iron production in 1884. This mine continued operations until June 1884, when the blast furnace was extinguished and never recommenced. The blast furnace at Lal Lal is considered one of the most important and highly significant sites ion early industrial history in Australia, as it is the only remaining best furnace from the nineteenth century in the Southern Hemisphere. The furnace ruins are 17 metres high, and are clearly visible today on Iron Mine Road, Lal Lal, near the Bungal Dam. This specimen of Lignite (brown coal) is significant, as it was mined from the area where brown coal was first discovered in Victoria, leading to an important and controversial future of the mining and use of brown coal in this State. The Victorian Heritage Database has listed the Lal Lal Coal Mine with local significance, with their Statement of Significance stating: "The Lal Lal coal mine is historically significant as the site of the first discovery of lignite (brown coal) in Victoria, and one that promised important benefits to regional and state industries that were reliant on coal imports at the time. The significance of the stie is reduced by the poor state of preservation of the coal mining and processing fabric". 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 light-weight, soft and combustable sedimentary rock specimen, that is dark brown in colour. The specimen has jagged edges, as though parts of the rock have crumbled away. Brown coal, or Lignite, is formed naturally from compressed peat, and is typically found in natural basins. The stages to the formation of coal ('coalification') begin with plant material and wood, which will decay if it is not subjected to deep burial or heating, and turn into Peat. Peat, when sufficiently compressed naturally, will turn into Brown Coal (Lignite), and finally into Black Coal (sub-bituminous, bituminous and anthracite). Each successive stage has a higher energy content and lower water content. It is brownish-black in colour. Brown Coal has a high moisture content, between 50 and 75 percent, and a low carbon content. Some Brown Coals may be stratified, with layers of plant matter, which means little coalification has occurred beyond the peat natural processing stage. When Brown Coal is submerged in dilute nitric acid or boiling potassium hydroxide solution, it reacts to produce a reddish solution, of which higher-ranked coals do not. When brown coal is pulverised and burned in boilers, the steam is used to drive turbines, which generates electricity. It is the lowest rank of coal, as when burned, it creates a relatively low heat content, which in turn does not create a great output of steam. burke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, mineralogy, brown coal, brown coal specimen, lignite, lal lal, lal lal coal mine, lal lal iron mine, ballarat, blast furnace

Gabo Island sits off the coast of East Gippsland in Victoria, with cliffs of granite in a relatively unique red/pink colour. Early attempts to build a lighthouse on the island were abandoned due to poor foundations, but when a ship ran aground on the nearby Tullaberga Island in 1853 and led to the death of 37 people, efforts were reignited. Construction of a new lighthouse was completed by 1858, using Gabo Island granite. The lighthouse is Australia's second tallest in Australia and continues to play an important role in guiding boats around the coast as they journey between Melbourne and Sydney. The distinct pink colour from the granite means the lighthouse continues to be a defining feature of the island. Gabo Island granite was also used to construct the Treasury Building at 117 Macquarie Street in Sydney, now the Intercontinental Hotel.Granite in the pink colour of this specimen is relatively rare. The connection to the lighthouse on Gabo Island also gives the specimen historic significance and social significance regarding the maritime history of Victoria. 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 palm-sized mineral, coloured by flecks of pink, red, and grey. Granite is formed by the slow crystallisation of magma below the earth's surface. It is typically composed of a mix of quartz, feldspar, and other minerals, though syenitic granite like this sample has a smaller amount of quartz than typical granite. This different mineral composition leads to the more distinct pink and red colouring.First sticker: [torn]logical survey / R........ S........ / Loc Gabo Island / 1/4 Sheet / Second Sticker: 15 Third Sticker: Syenitic Graniteburke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, mineralogy, gabo island, gabo island lighthouse, lighthouse, granite, coast, coastal, granite specimen, victoria, coastal cliffs

In Australia, precious opal is found in Cretaceous age sandstones and mudstones. These sedimentary rocks were deeply weathered and this weathering released silica into the groundwater.Australia is the only part of the world where opalised animal and plant fossils have been found. Opal artefacts several thousands of years old have been discovered in East Africa. As early as 250 BC the Romans prized opals, thought to have come from mines in Eastern Europe, the ancient world's main source of opals. There are many aboriginal dreamtime stories that feature opal. Australian opals discovered during the late 1800's found little favour with European markets but their commercial value increased in the 1900's and in 1932 Australia took over as the major producer of opals in the world and remains the largest producer to this day. Opal is found around the world (Brazil, Mexico, Honduras and the western US) however Australia produces 95% of the world's precious opal and it is our official national gemstone. Opal was first mined commercially at Listowel Downs in Queensland in 1875 and later at White Cliffs in NSW. Today, Coober Pedy (SA) is the main producer of white opal, though in recent years this field has expanded and all types of opals are found. Other centres in SA include Andamooka and Mintabe. Lightning Ridge (NSW) is renowned for black opal and formerly White Cliffs was a large producer of high quality opal. Boulder opals (opals in concretionary ironstone) are mined in Queensland from numerous localities in a zone extending from the Eulo and Cunnamulla district in the south and northwest for a distance of over 700 km to Kynuna in the north. The towns of Quilpie, Yowah and Winton are the main opal mining and wholesale centres. Opals are considered gemstones and have been used in jewellery for thousands of years.Throughout much of history, opals were actually believed to be good luck. The Romans thought that opals were one of the luckiest gemstones and a symbol of hope. In the Middle Ages, opals were believed to be bestowed with all the positive properties of coloured gemstones due to its rainbow-like play of colour. Finally, there is a superstition that you should not wear an opal unless it is your birthstone otherwise misfortune will befall you. This, of course, is far-fetched, but the notion could have been promoted in the late 19th and early 20th Centuries by diamond traders who were trying to increase sales of diamonds and deter people from buying opals. Possibly related to this is the thought that you should set opal jewellery with diamonds as their powers of good fortune will override any negativity held by the opal. The great majority of opal does not show play of colour and is called common opal or potch however this is not the case with a precious opal. Opal is a precious gemstone, like rubies, emeralds or diamonds. Opal is rare, and it is expensive to prospect and mine for.Silica is one of the most common minerals on the planet, but precious opal is very rare – far more rare than diamonds. Precious opal is rare because the natural processes that create it rarely occur.Most (at least 95%) of the opal found by miners is common opal without gem colour. In Australia we call it potch. It can be white, grey, black or amber coloured. Even when a miner finds gem-coloured opal, most of it can’t be cut into gemstones because it’s too thin, or sandy. 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.It is not known where this opal originated, except that it is probably from Victoria, as it has been recorded from many localities in the State. Common Opal is formed from silica-rich water circulating through rocks near the Earth’s surface. It consists of minute spheres of silica arranged in different ways. In common opal, the spheres are of different sizes and randomly arranged, unlike in precious opal where the spheres are of similar size and uniformly arranged in three dimensions. These differences account for common opal generally being translucent to opaque and without the play of colours, or opalescence, displayed by precious opal. Common opal is found in many localities and different geological environments throughout Australia and the world. Precious opal requires special conditions to form and is much less common. Australia produces most to the world’s precious opal. burke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, precious opal, opal, brazil, mexico, honduras, queensland, coober pedy, gemstones, jewellery, play-of-colour, light blue

Basalt is a common igneous rock that composes most of the Earth's surface and can be found on the Moon and other rocky planets of the Solar System. It is generally composed minerals such as calcic plagioclase, clinopyroxene and iron ore which form grains that are indistinguishable to the naked eye. It can be dark grey or black in colouring and sometimes may contain holes left by gas bubbles. Most of the Earth's basalt was produced in environments such as oceanic divergent boundaries, oceanic hotspots, and mantle plumes and hotspots beneath continents. Basalt is commonly used in construction where it is crushed and used for multiple purposes such as concrete aggregate, road base, or railroad ballast. Thin slabs of basalt can also be cut and used for floor tiles, stone monuments, and building veneer. This particular specimen was excavated from Talbot in Victoria, which was a small gold mining town established in 1852. As basalt is a common rock, it is not specific to Talbot. However, this specimen can be assumed to be of the Cainozoic age due to previous geomorphic surveys of the area. This particular type of Basalt was used mainly for roads due to the durability of the rock.Basalt holds significance due to the continued use of the rock from historic until present times. The rock has been utilised for many types of construction and is still used for the same purposes today. Basalt also has significance to the Earth and other rocky planets of the Solar System as it makes up most of the planet's surface. 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 smaller than hand sized rock specimen which is dark grey in colour with small holes and white deposits across its surface.Geological survey / [illegible] /burke museum, beechworth, geological specimen, geology, basalt, basalt specemin, indigo shire, talbot, cainozoic, igneous rock

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 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

This specimen is from Barefoot Hills, Victoria. Sandstones are economically important as major reservoirs for both petroleum and water, as building materials, and as valuable sources of metallic ores. Most significantly, they are the single most useful sedimentary rock type for deciphering Earth 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 sedimentary rock composed mostly of quartz sand. Sandstone is the second most common sedimentary rock after shale. Sandstones consist of sand-sized grains principally quartz, feldspar and rock fragments. The two major classes of sandstone are arenite and wacke. the colour of sandstone varies from grey, yellow, red and white reflecting the variation in mineral content and cement and is gritty to touch (like sandpaper).Geological survey / R.... S 61 / Loc Bareboot Hills / Sheet / 24SE / 94 /burke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, mineralogy, sandstone, yellow sandstone, victoria, barefoot hills

This particular specimen was found in the Moorabool Slate quarries in Victoria. The Moorabool Slate quarries was established in the 1860’s by a company of Welshmen with a crew of six who purchased land by the riverside to mine for slate. Under the promise of adding to existing recourses the crew mined the slate which was used for paving and roofing. Slate is a fine-grained, low-grade metamorphic rock that is formed by the transformation of mudstone, shale or sometimes volcanic ash under low pressure and temperatures. It dark colour is due to carbonaceous material or to finely divided iron sulphide. It is believed that Evan Rowlands and Theophilus Williams of Ballarat were the first to discover the slate veins. Slate is a one of the most common natural stones in general use. Being used as paving, flooring, roofing and more. However, its history of being mined in Australia is not common as it is considered that the best places to mine slate is Spain and parts of the United Kingdom. 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 somewhat rectangular foliated metamorphic rock composed of quartz, sericite and minerals from the chlorite group that make up the compounds of slate. The rock is dark grey almost black.Geological survey / R S / Loc Moorabool /Slate quarries / 1/4 sheet | 78 | Roofing Slate /burke museum, beechworth, geological, slate, metamorphic, slate (metamorphic), geological specimen, slate specimen, indigo shire

This specimen was recovered from Moonambel, Donkey Hill, Victoria. Established in the early 1860's, Moonambel is a small town in the Pyrenees region of the Australian state of Victoria. In the 1850s the location of Moonambel was part of the ‘Mountain Creek’ pastoral run, but in 1860 reports began to appear of a gold-rush at McKinnon’s ‘Mountain Creek’ station. By 1861, a township had developed on the diggings site, and on 21 October 1861 the “municipal district of Moonambel, on Mountain Creek” was proclaimed. The name 'Moonambel' is believed to be an aboriginal word meaning 'hollow in the hills'. Slate is a stone with a fine grain that is noted for its persistent strength and ability to naturally split into slabs. It forms under low temperatures and is most often created from clay. Pyrite is a crystallising compound that occurs naturally in grey and blue-black slate that is colloquially referred to as slate-rust as it resembles regular rust. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.Pyrite is iron sulphide (also known as “fool's gold”) which is commonly found in slates.Existing label: 53 /moonambel, slate, pyrite, burke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, mineralogy, victoria

This specimen was recovered from Adelong, NSW. The initial discovery of gold at Adelong by a Mr Williams took place in 1857. Much of the area is underlain by granitic rocks, while at Adelong itself a prominent norite intrusive body occurs. To the west of Adelong is a belt of intermediate to mafic igneous rocks and sediments which extends from Batlow in the south to at least as far north as the Snowy Mountains Highway. Around 26 tonnes of gold was found at the Adelong goldfield from its discovery in the 1850s until the last miners left in the 1940s. Pyrite has the formula of FeS2 and forms as an isometric (cube) form. It is a common occurring material and is often mistaken for gold, now colloquially known as ‘fool’s gold’. Pyrite that has strongly crystallised is considered stable, but the mineral has the potential to oxidise and decay. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.Pyrite is iron sulphide (also known as “fool's gold”) which is commonly found in slates.Existing Label: 104 /burke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, mineralogy, pyrite, adelong

This particular geological specimen was found in Mount Franklin or Lalgambook in Djadjawurrung, located between Daylesford and Newstead, approximately ninety minutes drive from Melbourne. The mountain is an example of a breached scoria cone (a steep conical hill of loose pyroclastic fragments) which was created by a volcanic eruption about 470,000 years ago, a date which may indicate the age of this geological specimen. The volcanic eruptions of Mount Franklin were most likely witnessed by members of the Dja Dja Wurrung Aboriginal tribe, who referred to this country as the 'smoking grounds'. Mount Franklin and the surrounding area appears to have been a place of considerable religious significance to Aboriginal people, there is evidence which indicates that frequent large ceremonial gatherings took place in the area. Basalt is the most common rock on Earth’s surface, more than 90% of all volcanic rock on Earth is basalt. Basalt is an aphanitic extrusive igneous rock formed from the rapid cooling of low-viscosity lava exposed at or very near the surface of a rocky planet or moon. Specimens are black in colour and weather to dark green or brown. Basalt is rich in iron and magnesium and is mainly composed of olivine, pyroxene, and plagioclase. Olivine is the name of a group of rock-forming silicate minerals with compositions ranging between Mg2SiO4 and Fe2SiO4. Unlike other minerals, Olivine has a very high crystallisation temperature which makes it the first of the minerals to crystallise from magma. As magma cools, the crystals begin to form and settle on the bottom of the lava and form basalts that are abnormally enriched in olivine in the lower part of lava flows. According to H. M. King (on geology.com) "Olivine is thought to be an important mineral in Earth's mantle. Its presence as a mantle mineral has been inferred by a change in the behaviour of seismic waves as they cross the boundary between Earth's crust and mantle". Lava from Mount Franklin and other volcanoes in the area filled valleys and buried the gold bearing streams that became the renowned ‘deep leads’ of the gold mining era. In 1852, as part of the Victorian gold rush, gold was discovered in the immediate area, this gold was created by lava flows during the Newer Volcanic period, which were mined intensively during the nineteenth century. Around 1865 the presence of a deep lead in Mount Franklin was established. Deep lead mining was initially unsuccessful, and it was not until the late 1870s that the Franklinford Gold Mining Company mined at Mount Franklin on a significant scale. A few years later the Mount Franklin Estate Gold Mining Company also struck gold, followed by the Shakespeare and Great Western companies in the mid-1880s. By the late 1880s, however, deep lead mining had ceased in the area. Soon after gold was discovered in 1851, Victoria’s Governor La Trobe wrote to the Colonial Office in London, urging ‘the propriety of selecting and appointing as Mineral Surveyor for this Colony a gentleman possessed of the requisite qualifications and acquaintance with geological science and phenomena’. Alfred Selwyn was appointed geological surveyor in Australia in 1852 which began the Geological Survey of Victoria. In 1853-69 the Geological Survey issued under Selwyn's direction sixty-one geological maps and numerous reports; they were of such high standard that a writer in the Quarterly Journal of the Geological Society of London bracketed the survey with that of the United States of America as the best in the world. During his years spent in Australia, Selwyn collected numerous significant geological specimens, examples of which are held in collections such as the Burke Museum.This geological specimen is an example of basalt and olivine which shows the volcanic lava activity and geographical specific nature of Mt Franklin as a significant volcanic site. According to Agriculture Victoria 'The crater is one of the deepest in the Central Highlands area. It is a major megacryst site with some of the largest known Victorian examples of megacrysts of augite and an orthoclase. The small parasitic mound of Lady Franklin on the western flanks adds to the geological interest of the site'. This specimen also highlights the locality as a significant place for both indigenous activity and Victorian gold rush era mining practices. 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.An angular, solid hand-sized piece of grey volcanic Basalt with green/brown Olivine phenocrysts along one flat edge.Olivine in basalt / - label is probably / correct. / C. Willman / 15/4/21burke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, mineralogy, basalt, igneous rock, igneous-volcanic, volcanic geology, volcanic, olivine, olivine specimen, basaltoid