This photograph is recorded as depicting the presentation by Mr Alan Dunlop to Cr Val Mason, Shire President, of a 2.86-gram solid gold nugget found in the area more than 100 years ago, at the Burke Museum. The gold is reported as attached to a small amount of milk quartz mounted onto a tie pin. The photo and an article about the donation appeared in the Border Morning Mail on Friday 14th May, 1979. Alan Dunlop, pictured, was Sir Edward 'Weary' Dunlop's older brother. The tie pin artefact being donated in this photo is entered into the Victorian Collections database as follows: 'This nugget was found on the Beechworth Goldfield in the late 1800s by Mr Fred McIntosh (Alan & Edward Dunlop's Uncle by marriage, husband of Elizabeth (Bessie) Dunlop), who had made it into a tie pin and presented it to the Dunlop family'. Furthermore, Val Mason was the first female president of the former Beechworth Shire for two terms and a councillor for nine years. This photograph is of historic significance as it depicts known individuals who have connections to key Australian figures. Alan Dunlop is the brother of famous war doctor Edward 'Weary' Dunlop, and both men are Beechworth locals. The object Alan holds is a tie pin made from gold found by the Dunlops' uncle. It's also significant as it documents visually the origin of the tie pin artefact in the Burke Museum collection, via donation by Alan Dunlop. In addition, it depicts Val Mason, the first female president of the former Beechworth Shire for two terms and a councillor for nine years. It is of social significance as it depicts two well-known and respected Beechworth locals handling a key artefact of significance to the Beechworth Goldfields, and therefore Beechworth local history. It also shows the Burke Museum in 1979, providing research potential for those interested in the history of the development of the museum's collection.Black and white, rectangular photograph printed on paper.Obverse: (lllegible) Reverse: A02653weary dunlop, gold, beechworth, val mason, tie pin, jewellery, goldfield, beechworth goldfield, fred mcintosh, bessie dunlop, elizabeth dunlop, dunlop, border morning mail, victorian collections, donation, burke museum

This photograph depicts members of the Beechworth Band at a 'Liedertafel' concert in the main hall at the Burke Museum in 1999. The concert was associated with an exhibition titled, 'From the Liedertafel to the Skating Rink: Entertainment in Beechworth 1852 - early 1900s', which celebrated the rich and diverse entertainments that were a part of Beechworth life in the nineteenth and early twentieth centuries. Marching bands, choirs, circus acts, theatrical performances, races, and seasonal activities, such as Mr. Spiller's roller skating rink, founded in the late 1860s, were among the attractions on offer. 'Liedertafel' is a tradition that accompanied German settlers to Australia. It refers to a friendly society of men united by an enthusiasm for singing. The Beechworth Brass Band was formed by Mr. H. Vandenberg in 1887. The Beechworth Liedertafel was established 14 March 1894 at the London Tavern, Camp Street, Beechworth, by Mr. A.A. Billson, and a visiting conductor, Mr. H. Fielder. German clubs, complete with marching bands, athletics associations and Liedertafel choirs, were centres of social activity attracting wide audiences not limited to members of their own ethnicity. Alfred Arthur Billson was the youngest son of Mr. George Billson, who served as Beechworth’s mayor between 1869-1871. In 1872, George purchased the Oven’s Brewery in Last Street, which became Billson’s Brewery, one of the oldest continuing beverage manufacturers in Australia. An active member of Beechworth’s cultural, business and political life around the turn of the century, A.A. Billson served on Beechworth Shire Council from 1884 to 1893, and from 1895 to 1910, with three terms as president (1888–89, 1899–1901, 1908–09). He founded the Beechworth Progress Association in 1891 and produced an ‘Illustrated Guide to Beechworth and Vicinity’ to develop tourism potential. This photograph of the Beechworth Band playing at the Burke Museum is historically significant for the information it conveys about an exhibition at the Burke Museum between September and November 1999. The use of the contemporary Beechworth Band in a 'Liedertafel' performance provides insight into curatorial approaches at the turn of the twenty-first century and improves our understanding of how exhibitions use objects in the Burke Museum's Collection to tell stories about the past in the present. The image is historically and socially significant for attesting to the enduring appeal of local musical associations, which were a popular means of entertainment that fostered social connections among settlers from diverse ethnic backgrounds. Rectangular colour photograph printed on matte photographic paper. Reverse: 7029 / Label: 7029 / Source / Burke Museum / Beechworth / Band / 1999/2000 /liedertafel, beechworth band, burke museum, from the liedertafel to the skating rink, entertainment in beechworth 1852 - early 1900s, gold rush, immigration, beechworth's german heritage, london tavern beechworth, beechworth's first brick tavern, spiller's skating rink, vandenberg's beechworth brass band, protestantism, teetotallism, skating carnivals, beechworth german association, yma's, beechworth skating rink, progress societies, billson's brewery, german-australians, beechworth progess association, lodges, freemasonry, colonial australia

This photograph depicts female singers accompanied by members of the Beechworth Band at a 'Liedertafel' concert in the main hall at the Burke Museum in 1999. The concert related to an exhibition titled, 'From the Liedertafel to the Skating Rink: Entertainment in Beechworth 1852 - early 1900s', which celebrated the rich and diverse entertainments that were part of Beechworth life in the nineteenth and early twentieth centuries. 'Liedertafel' is a German tradition that accompanied European settlers to Australia. It refers to a friendly society of men united by an enthusiasm for singing. The Beechworth Liedertafel was established 14 March 1894 at the London Tavern, Camp Street, Beechworth, by president, Mr. A.A. Billson, and a visiting conductor, Mr. H. Fielder. The Beechworth Brass Band was formed by Mr. H. Vandenberg in 1887. Marching bands, choirs, circus acts, theatrical performances, races, and seasonal activities, such as Mr. Spiller's roller skating rink, which was founded in the late 1860s, were among the entertainments on offer in Beechworth.This photograph of the Beechworth Band playing at the Burke Museum is historically significant for the information it conveys about an exhibition at the Burke Museum between September and November 1999. The use of the contemporary Beechworth Band in a 'Liedertafel' performance provides insight into curatorial approaches at the turn of the twenty-first century and improves our understanding of how exhibitions use objects in the Burke Museum's Collection to tell stories about the past in the present. The image is historically and socially significant for attesting to the enduring appeal of local musical associations, which were a popular means of entertainment that fostered social connections among settlers from diverse ethnic backgrounds. Liedertafel choirs were originally male-only, therefore, the presence of female singers at the 1999 exhibition reflects progressive social and community values with regard to gender and inclusion.Rectangular colour photograph printed on matte photographic paper.Reverse: 7030 / Label: Burke Museum / Liedertafel Exh / Emily Messen, Luetta / Schier, Hannah / Routledge, Sarah / McKinley 2000 (?) / 2000 (?) / liedertafel, beechworth band, burke museum, exhibition 1999, from the liedertafel to the skating rink, entertainment in beechworth 1852 - early 1900s, past exhibitions, performances at the burke museum, european settlers, german community, german choral societies, brass bands, male choir, colonial passtimes, colonial entertainments, cultural traditions, gold rush, immigration, beechworth's german heritage, london tavern beechworth, camp st beechworth, beechworth historic district, beechworth's first brick tavern, spiller's skating rink, vandenberg's beechworth brass band, benevolent societies, intellectual societies, protestantism, billson brewery beechworth, teetotallism, fancy dress carnivals, skating carnivals, fundraising societies, german musicians, crimean war, beechworth german association, freemasonry, yma's, beechworth athenaeum, beechworth skating rink

This photograph depicts two members of the Beechworth Band at a 'Liedertafel' concert in the main hall at the Burke Museum in 1999. The concert related to an exhibition titled, 'From the Liedertafel to the Skating Rink: Entertainment in Beechworth 1852 - early 1900s', which celebrated the rich and diverse entertainments that were a part of Beechworth life in the nineteenth and early twentieth centuries. 'Liedertafel' is a German tradition that accompanied European settlers to Australia. It refers to a friendly society of men united by an enthusiasm for singing. The Beechworth Liedertafel was established 14 March 1894 at the London Tavern, Camp Street, Beechworth, by president, Mr. A.A. Billson, and a visiting conductor, Mr. H. Fielder. The Beechworth Brass Band was formed by Mr. H. Vandenberg in 1887. Marching bands, choirs, processions, circus acts, theatrical performances, races, fancy dress and roller skating carnivals, were among the vibrant and diverse entertainments offered in Beechworth during the gold rush period. Race meetings were revived with a gala atmosphere at Baarmutha on New Year's Day and Easter Monday in the early 1880s. 'Spiller's Skating Rink', which premiered at St. Georges Hall in August 1869, was accompanied by the 'Beechworth Fire and Drum band'. In 1888, Beechworth had two skating rinks in operation, the Columbia Elite at Oddfellow's Hall, and the Beechworth Skating Rink, corner Camp and Last Streets, Beechworth. Vandenberg's Beechworth Brass Band was reported to have provided musical entertainment for patrons at both venues.This photograph of the Beechworth Band playing at the Burke Museum is historically significant for the information it conveys about an exhibition at the Burke Museum between September and November 1999. The use of the contemporary Beechworth Band in a 'Liedertafel' performance provides insight into curatorial approaches at the turn of the twenty-first century and improves our understanding of how exhibitions use objects in the Burke Museum's Collection to tell stories about the past in the present. The story of Liedertafel's and Beechworth Brass Band is historically and socially significant for understanding the role played by German immigrants in building Victorian communities. In settler communities, cultural associations centred on artistic, recreational and sporting activities not only provided a popular means of entertainment, but fostered social cohesion among settlers from diverse ethnic backgrounds.Rectangular colour photograph printed on matte photographic paper. Obverse (On keyboard): Technics / Reverse: 7028 / Label: Liedertafel / exh. / Beechworth / Band / 1999/2000 /liedertafel, beechworth band, burke museum, from the liedertafel to the skating rink, entertainment in beechworth 1852 - early 1900s, gold rush, immigration, beechworth's german heritage, london tavern beechworth, beechworth's first brick tavern, spiller's skating rink, vandenberg's beechworth brass band, protestantism, teetotallism, skating carnivals, beechworth german association, yma's, beechworth skating rink, progress societies, billson's brewery, german-australians, roller skating history

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

This is a photograph of two people (James Toole and Beryl Witkowski) amid celebrations for St Patrick's Day at the Burke Museum in an unknown year. St Patrick's Day is traditionally an Irish religious holiday, but has been adopted in countries such as Australia to celebrate an idea of Irish culture. These celebrations often include wearing green clothes, especially a shamrock hat, and drinking beer, all pictured here. This celebration appears to be taking place within the Burke Museum itself, with museum's iconic stained glass oval window in the background. The Museum, situated in Beechworth, holds a collection of over 30,000 individual objects - including this photograph. James Toole (left) was the 'face of the Beechworth Post Office' until his retirement in 2015, following a 45-year career in mail service. He is a Friend of the Burke Museum, volunteering on projects such as crafting the Burke Museum's float in the 2018 Beechworth Bakery and Beechworth Honey Grand Parade at the Golden Horseshoes Festival. He is known for his flamboyant character. Beryl Witkowski (right) was a historian and curator for the Burke Museum, retiring from her position in 2016. She was involved as a Friend of the Burke Museum from at least 2004.This photograph is significant to the Burke Museum and Beechworth as it depicts two prominent, contemporary members of the museum's paid and volunteer staff in the museum itself. It highlights both how the staff interacted with the museum through celebrations and how the museum itself was used in capacities other than object display. The photograph can also be used to interpret Australia's relationship to the St Patrick's Day holiday, especially given the presence of Irish immigrants to the Beechworth area in the nineteenth century.A colour, square photograph printed on rectangular photographic paper.First Card: WITKOWSKI, Beryl / TOOLE, James / BMM 3067 / Databased Second Card: Burke Museum / 3067 /burke museum, beechworth, museum staff, celebrations, st patrick's day, beer, australia, st patrick's day celebration

This photograph depicts the entrance to the Burke Museum in Beechworth, most likely in 1980. The building was originally established as the Beechworth Athenaeum in 1857 to provide a lecture hall and reading room at the peak of the gold rush. In 1859, it became the Beechworth Public Library, which is why the writing embossed above the main entry says 'Library' rather than 'Museum'. The building was turned into a museum and renamed the Robert O'Hara Burke Memorial Museum in 1863 in honour of Robert O'Hara Burke, former Police Superindendent of Beechworth who died in 1861 on the Burke and Wills expedition. The Burke Museum has been in almost continual operation since that time. In the 1970s, the building underwent renovations to create several verandas, though the main façade visible in this photograph remained as it was when originally built. The Burke Museum currently contains over 30,000 individual objects, including the Gold Rush era items and the Ned Kelly collection advertised on the a-frame in the photograph. The photograph itself is also part of the Burke Museum collection.The Burke Museum itself is very significant to Victorian history. It is on both the Victorian Heritage Register and is part of the National Trust due to its relevance to the history of the Gold Rush period, its architectural features, and its significant collection. Photographs of it throughout its history are an important part of telling the museum's story. This photograph in particular highlights what the museum staff believed would be appealing to a 1980s public, evident by the A-frame advertising board.A black and white rectangular photograph printed on photographic paper.Top right text: 5147. Bottom left text: Beryl Seatt (or possibly Scatt) & friend 1980beechworth, burke museum, beechworth museum, beechworth historic precinct, architecture, museum, library, 1980s, 1980s australia, museum staff

Taken on 14 May 1979, this photo depicts Mr Alan J. Dunlop and his wife presenting a 2.86-gram solid gold nugget found in the Beechworth area more than 100 years ago, to the Shire President, Councillor Mrs Valerie Mason. The gold is reported as attached to a small amount of milk quartz mounted onto a tie pin, and was donated to the Burke Museum by the Dunlop family. Alan Dunlop, pictured, was Sir Edward 'Weary' Dunlop's older brother. The tie pin artefact being donated in this photograph is entered into the Victorian Collections, and records that the nugget was found in the Beechworth Goldfields by Mr Fred McIntosh, in the last 1800s. Fred McIntosh, the husband of Elizabeth (Bessie) Dunlop (the sister of Alan & Edward's father, John) had the nugget made into tie pin and presented it to the Dunlop Family. Furthermore, Valerie 'Val' Mason was the first female president of the former Beechworth Shire for two terms and a councillor for nine years. This photograph is of historic significance as it depicts known individuals who have connections to key Australian figures. Alan Dunlop is the brother of famous war doctor Edward 'Weary' Dunlop, and both men are Beechworth locals. The object Alan holds is a tie pin made from gold found by the Dunlops' uncle, and the provenance of the item – from goldfield to family collection to museum collection – provides a recent context with which to interpret the significance of gold-mining on present and future generations, as well as strong research potential on minerals known to be sourced in the area. In conjunction with other photographs in the collection, this photograph visually documents the donation and acquisition of the tie pin artefact into the Burke Museum Collection. In addition, it depicts Valerie ‘Val’ Mason, in her role as the president of the former Beechworth Shire. Val was the first female in this role, which she held for two terms, and was a councillor in the Shire for nine years. This photograph is of social significance as it depicts two well-known and respected Beechworth locals handling a key artefact of significance to the Beechworth Goldfields. It also shows the Burke Museum in 1979, providing research potential for those interested in the history of the development of the museum's collection. Colour rectangular photograph printed on matte photographic paper.Reverse: Polacolor (Registered Trademark symbol) Type 108 / LR / Mrs Valerie Mason / Mr Dunlop (Weary's brother) / Mrs Vivian Payne (erased) / 14-5-1979 A.J. Dunlop & wife with Cr. Mason /L85052P gold, nugget, tie pin, pin, beechworth, burke museum, goldrush, goldfield, dunlop, edward dunlop, weary dunlop, alan dunlop, valerie mason, fred mcintosh, gold mining, donation, museum, collection, president, councillor, shire, female

This photograph is recorded as having been taken in the North East Victoria Regional Tourist Authority, Wangaratta and depicts an exhibition display of items and interpretative labels associated with the Kelly Gang. The display was reportedly laid out as part of a Vic Tour Stamp, with items from the Burke Museum Collection.This photograph is of social significance due to its connection with the Burke Museum as well as the Kelly Gang. The Kelly Gang story is integral to the formation of the Australian identity and highlights the Irish oppression during the 1880s. Ned Kelly is an Australian icon, mythologised in Australian literature, art, folklore and history, and the Kelly Gang permeates Australia's national consciousness. The significance of the Burke Museum is also highlighted here, as the photograph shows the importance of the Kelly story to the Beechworth area and local identity, as well as its significance within the museum collection. The photograph is of strong research potential due to its depiction of the Kelly Gang history in Australia and its presentation of a historical museum exhibition which toured from Beechworth to other Victorian locations. With a depiction of the exhibition and associated label, the photograph provides insight into how the language and historical interpretation of Kelly Gang has developed, and how cultural and social opinions which are often shaped by exhibition displays, have shifted. Black and white rectangular photograph printed on matte photographic paper.Obverse: Gold Cradle / History / Claim 1835 / The north east is rich in history. It was the home of Ned Kelly, the 'Man from Snowy River' and (???) dog Mogan. Century old buildings are common and (???)nders of the gold rush days are everywhere / V. R. / £8000 Reward / Robbery and Murder / (indeterminate) Reverse: The historical display laid out in VICTOUR / 1997 3135 / North East Victoria/ Regional Tourist Authority/ P.O. Box 250/ Wangaratta. 3577 /BMMA03324burke museum, ned kelly, kelly gang, museum collection, exhibition, display, gallery, museum, exhibit

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

Taken between 1928 and 1930, depicted is the Bethanga Bridge under construction. The Bridge was completed in 1930 and was built to assist residents of the Bethanga district to travel to Albury. Other bridges would become submerged by the backed-up water of the Murray and Mitta Rivers so the Bethanga bridge was built two miles above the Mitta Weir. The Bethanga Bridge was built north of the future Hume Dam which would be completed in 1936. At 2430 feet long, Bethanga Bridge was the longest road bridge in Australia at the time of its completion. The Bridge is 20 feet wide and made up of nine 270 feet long spans. Materials used include ten tons of paint for the steel works; 1600 tons of steel; 900 tons of timber for the decking; and reinforced concrete for the piers. The tender for the construction was awarded to C. Ruwolt Pty. Ltd., engineers who were located on Victoria Street, West Richmond. The contract was awarded for £71,890. It was predicted between 250 and 300 men would find employment on the project. The news was well received by trade unions at the time as there had been a drop in available engineering work.This photograph is historically significant as it depicts the progress of the Bethanga Bridge construction, which was important infrastructure for the area. It is also a good example of methods used in the area to assist in travel over the river prior to the construction of the Hume Dam.Black and white rectangular photo printed on matte photographic paper.Reverse: 1997 3186 / 84-19-3 / This is the bridge. / It is not yet open to traffic / yet. will not be completed / until May next / It is a wonderful bridge the / pillars are 100 feet high. / KODAK PRINT Envelope Obverse: Peterson PHOTO / Hume Weir Envelope Reverse: BMM 84-20-1,2+3. bethanga bridge, lake hume, hume dam, hume weir, murray river, bridge, bethanga, albury

Galena Chalcopyrite is the earth's primary ore of lead and is mined from a large number of deposits in many countries. It is also an important source of silver. Galena Chalcopyrite is one of the most abundant and widely distributed sulfide minerals across the world. The mineral is found in igneous and metamorphic rocks in medium- to low-temperature hydrothermal veins. This specific specimen was recovered from the mines in Broken Hill, New South Wales. The mines in Broken Hill were first established after Charles Rasp discovered a large amount of silver-lead-zinc ore-body in the area in 1883. BHP (Broken Hill Proprietary) mining company was then established in 1885 and quickly became the lead in Australia's mining industry after they began excavating and exporting the country's largest amount of lead, silver, and zinc. This feat generated over $100 billion in wealth for the company.Galena Chalcopyrite is signifiant as it represents the catalyst for the rise of Australia's most influential mining companies - BHP. The mineral was one of the first to be mined in the country and after being made into lead, was used for a variety of things such as paint, batteries, ammunition, and plumbing materials before it was known to be harmful to humans. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study. A grey, solid hand-sized lead sulfide mineral with a silver metallic luster.burke museum, beechworth, geological, geological specimen, galena, galena chalcopyrite, chalcopyrite, broken hill, bhp, bhp mining, broken hill mine, mine, australia mine, lead, lead mine

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

Ilvaite has acquired its name from Ilva (Latin for Elba) Island, Greece, where Ilvaite is most commonly found. The geological setting in which Ilvaite occurs is through contact with magnetite, zinc and copper ore deposits, along with contact metamorphic deposits and zeolite zones. llvaite crystallizes in the form of black prismatic crystals and columns . This specimen was retrieved from Broken hill, known as the world's richest and largest zinc-lead ore deposit. Because of Ilvaite's often unaesthetic crystal formations compared to other minerals, Ilvaite is uncommon in most rock collections, particularly specimens that are not well formed, such as this one. Ilvaite is also a member of the Sorosilicate subclass of the silicate minerals, which have an unusual basic unit of Si2O7, making Ilvaite a unique mineral. Given that Ilvaite is not commonly found in Australia, it marks a unique contribution to an Australian collection of minerals. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A solid hand-sized ferrous iron analogue mineral with of black with shades of beige Ilvaite is a brittle, opaque rock formation that has acquired its name from Ilva (Latin for Elba) Island, Greece, where Ilvaite is most commonly found. The geological setting in which Ilvaite occurs is through contact with magnetite, zinc and copper ore deposits, along with contact metamorphic deposits and zeolite zones. llvaite crystallizes in the form of black prismatic crystals and columns rock, mineral, ilvaite, ilvaite specimen

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

Rhodonite is a reddish-pink manganese silicate material and often contains iron, magnesium and calcium. It is usually found in metamorphic rocks (rocks which have been altered by heat, pressure or chemical process). It can range in size from tiny to massive. Because of their composition they are not suitable for use in jewellery because they are hard enough. It is quite rare to find, though has been found in Australia, North America, South America and Europe.This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study. This specimen is a palm shaped piece of loellingite within rhodonite. It is mostly reddish-pink coloured, with flecks of light and dark grey. Loellingite is a grey iron arsenide which often forms into crystal shapes. It is mostly found in mesothermal veins (caused by immense heat) with sulfides or in limestone. It is toxic when heated or struck. rhodonite, loellingite, burke museum, beechworth, geological survey of victoria

This 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

According to the 1912 Department of Mines Bulletin of the Geological Survey of Victoria, basalt covers a considerable portion of the Macedon area including Mount Macedon. Basalt is the most common form of rock underlying the earth's surface and is found in three kinds of rock forming environments: ocean divergent boundaries, oceanic hotspots, and mantle plumes and hotspots beneath continents.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 mass, geological specimen in shades of grey and white. Hyalite is a colourless variety of opal. It occurs as globular and botryoidal masses and irregular crusts in volcanic and pegmatite environments where the silica deposits from the gas phase. Basalt is dark in colour, fine-grained igneous rock composed of plagioclase and pyroxene minerals. It is commonly formed as an extrusive rock, such as lava flow. It is one of the most common forms of rock underlying the earth's surface.burke museum, geological specimen, department of mines, geological survey of victoria, basalt, mount macedon, beechworth

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 specimen was recovered from Creswick in Victoria. Basalt is dark in colour, often black and has a fine grain. It is composed of plagioclase and pyroxene minerals and an igneous rock. 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 cylindrical fine-grained piece of igneous rockburke museum, geological survey of victoria, geological specimen, geology

This specimen was recovered from Wonthaggi in Victoria. Coal is a sedimentary rock which is composed of peat after it has been exposed over millions of years. This is an example of Australian black coal which is used as either thermal or coking coal for electricity generation or manufacturing processes. It is predominantly composed of Carbon which is 'C' on the periodic table of elements. This early example of a coal sample, shows the important role that coal played/plays in Australia's energy generation and manufacturing processes. 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.Small piece of black coal with museum original labelGeological survey / R..... S...../ Locality Cape Patterson coal specimen, burke museum, geological survey of victoria, geological specimen, geology

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 specimen was recovered from Philip Island in Victoria. Chalcedony is composed of Quartz and Silicon Dioxide represented as SIO2. It has and is still used as a gemstone for thousands of years. This is an excellent specimen Chalcedony that shows its aesthetic 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. Uniquely shaped piece of Chalcedony with opening in the centerburke museum, beechworth, geological, geological specimen