Taken on Christmas of 1941, shown is a track to Lake Kerferd with forest on both sides. The construction on Lake Kerferd began in 1862 however it wasn't completed until 1874 due to engineering and funding issues. The lake was named after George Briscoe Kerferd (1831–1889) who was responsible for Beechworth's water scheme. George Briscoe Kerferd was born on 21 January 1831 in Liverpool, England and arrived in Melbourne April 1853. He spent his first years in Australia in Bendigo before settling down in Beechworth as a wine and spirits merchant. He married Ann Martindale on 17th December 1853 at St James Cathedral, Melbourne and between them they had three sons and five daughters. Kerferd began his political and legal career in Beechworth when he was first elected to the Municipal Council in May 1857. Later he would be elected to the Legislative Assembly for the Ovens District in November 1864, and continued to represent the area until February 1886.This photograph is historically significant as it provides insight into surrounding areas of the water reserves of Victoria. It is also linked to political identity of George Briscoe Kerferd and the Beechworth Municipal Council.Black and white rectangular photograph printed on matte photographic paper.Obverse: Reverse: 8163/ Back track to Lake Kerford/ Beechworth/ Xmas 1941lake kerferd, beechworth, water scheme, water reserve, forest track, forest pathway, reservoir, legislative assembly, hon. george briscoe kerferd, catchments, beechworth water reserve, beechworth catchments, municipal council, st. james cathedral, lakes, reserve, water supply, political projects

Taken between 1920-1930s, shown is the banks of Lake Kerferd with wooden man-made fencing. The construction on Lake Kerferd began in 1862 however it wasn't completed until 1874 due to engineering and funding issues. The lake was named after George Briscoe Kerferd (1831–1889) who was responsible for Beechworth's water scheme. George Briscoe Kerferd was born on 21 January 1831 in Liverpool, England and arrived in Melbourne April 1853. He spent his first years in Australia in Bendigo before settling down in Beechworth as a wine and spirits merchant. He married Ann Martindale on 17th December 1853 at St James Cathedral, Melbourne and between them they had three sons and five daughters. Kerferd began his political and legal career in Beechworth when he was first elected to the Municipal Council in May 1857. Later he would be elected to the Legislative Assembly for the Ovens District in November 1864, and continued to represent the area until February 1886.The postcard holds Historic significance due to its connection to Beechworth and its Lake Kerford. It demonstrates the interactions between nature and colonialists, especially how the lake has somewhat been 'protected' with the man made fencing. It also presents information on the environmental development or degradation for the area, with possible changes to the environment that may have been caused by human physical forces, natural decay or Global Warming.Black and white rectangular postcard printed on paper.Obverse: Lake Kerferd, Beechworth / Reverse: 8164 / Post Card / Correspondence / Address Only / Kodak Austral [Kodak Australia Stamp] /lake kerferd, beechworth, water scheme, water reserve, reservoir, legislative assembly, hon. george briscoe kerferd, catchments, beechworth water reserve, beechworth catchments, municipal council, st. james cathedral, lakes, reserve, water supply, political projects, man-made fence, environmental changes

This postcard depicts Lake Kerferd during the winter season. With the photograph possibly been taken in the 1930s.The postcard holds Historic significance due to its connection to Beechworth and its Lake Kerford. It demonstrates the interactions between nature and colonialists, especially how the lake is surrounded by man made fencing and roads. It also shows that there was frequent human interaction with the area, due to the small snow slopes where vehicles would travel across. Black and white rectangular postcard, printed on card.Reverse: 56. / A03092 / 97.2205 POSTCARD / AUSTRALIA / KODAK CORRESPONDENCE / ADDRESS ONLY / KODAK / AUSTRALIA 84 - 134 - 1beechworth, lake, postcard, burke museum, black and white photograph, lake kerford

The construction on Lake Kerferd began in 1862 however it wasn't completed until 1874 due to engineering and funding issues. The lake was named after George Briscoe Kerferd (1831–1889) who was responsible for Beechworth's water scheme. George Briscoe Kerferd was born on 21 January 1831 in Liverpool, England and arrived in Melbourne April 1853. He spent his first years in Australia in Bendigo before settling down in Beechworth as a wine and spirits merchant. He married Ann Martindale on 17th December 1853 at St James Cathedral, Melbourne and between them they had three sons and five daughters. Kerferd began his political and legal career in Beechworth when he was first elected to the Municipal Council in May 1857. Later he would be elected to the Legislative Assembly for the Ovens District in November 1864, and continued to represent the area until February 1886. The postcard holds Historic significance due to its connection to Beechworth and its Lake Kerford. It demonstrates the interactions between nature and colonialists, especially how the lake has somewhat been 'protected' with the man made fencing. It also presents information on the environmental development or degradation for the area, with possible changes to the environment that may have been caused by human physical forces, natural decay or Global Warming.Sepia rectangular postcard printed on paper.Obverse: The Rose Series P. 10542 / Copyright / Evening lights, Lake Kerferd, Beechworth, VIC Reverse: Farley / Published by the Rose Stereograph Co., / Armadale Victoria. / 84-132-1 / Post card / The "Rose" Series De Luxe / A Real Photograph Produced in Australia / BMM299 lake kerferd, beechworth, water scheme, water reserve, reservoir, legislative assembly, hon. george briscoe kerferd, catchments, beechworth water reserve, beechworth catchments, municipal council, st. james cathedral, lakes, reserve, water supply, political projects, rose series, postcard, rose series stereograph

This photo was taken in the 1960s from a northeast position looking down towards Lake Sambell, the caravan park, and the surrounding area. This photo was taken during a period of rejuvenation for the lake area including the opening of the caravan park in 1959 and the swimming pool area in 1961 (this pool is just visible in the centre of the photo). The popularity of caravanning in Australia exploded during this post-war period of the late 1950s and 1960’s. This popularity was driven by multiple factors, including: the stopping of fuel rations, the accessibility of car ownership through the manufacturing of affordable cars, technological developments in caravan design, and the increase in prosperity and leisure time for many Australians. Lake Sambell is an artificial lake that was developed on the previous site of the Rocky Mountain Mining Company workings and was officially opened by Minister for Lands, Mr Baily, on October 5, 1928. The disused and unattractive remains of the mine were converted into a recreational area intended for swimming, boating, and fishing. The lake is named after Mr L.H. Sambell, shire engineer and secretary of the Forward Beechworth Committee, who advocated for the enhancement of Beechworth into a tourist destination and was central to the planning and establishment of the lake. Funding for the project was raised by both competition funds and donations. Since the construction in 1928 several engineering issues have arisen. In 1939 the water levels were low, and the lake was considered both an eyesore and ‘mudhole’, Beechworth Shire Council sort funding to raise the height of the lake six feet to improve the quality of water. Throughout the 1940s the Beechworth Swimming Club tried to raise awareness and funds to address the structural engineering issues and improve swimming facilities at the lake. R.E. Carter, similar to L.H. Sambell, was a shire engineer who advocated the importance of positioning Beechworth as a tourist destination. Carter held the position from 1954-63 and organised many improvements to the Lake Sambell area including the caravan park in 1959, the lake swimming pool in 1961, water skiing and boating facilities, and increased the lake surface are in 1964. These improvements were financed mainly by grants from the Tourist Development Authority. This photograph is of historical significance as it documents Lake Sambell and the surrounding area in the 1960s after a phase of enhancements to improve the appearance and usability for both the people of Beechworth and tourists. It is also of social significance in providing an insight into the increase in leisure time and access to travel during a period of post-war prosperity.Black and white rectangle photograph printed on matte photographic paper and unmounted.Reverse: 1 / [logo KODAK/ VELOX/ PAPER] / C798 / 3535lake sambell, lake sambell caravan park, lake sambell swimming pool, caravan park, caravanning 1960s, rocky mountain mining company, l.h. sambell, r.e. carter, beechworth swimming club, forward beechworth committee, minister of lands, tourist development authority, lake swimming, swimming, boating, fishing, water skiing, beechworth 1960s, lake sambell fishing, lake sambell boating

The photograph depicts a view across the water at Lake Sambell. The image is thought to date from the 1960s so may show the lake during a period of drought, such as that experienced across South-Eastern Australia in 1967. The present day park and reserve occupies the site of the former Rocky Mountain Mining Company, an open-cut sluice mine that began operations in the mid-Nineteenth Century and operated until the early 1900s, through the peak of Victoria’s Gold Rush. It was converted into a park and leisure area in the 1920s. Lake Sambell was formally opened to the public on Friday 5th October 1928 and was opened by the Victorian Government’s Minister of Lands, Mr Bailey, as part of initiatives to boost the economies and development of country towns. The lake was named after Mr L.H. Sambell, a shire engineer and secretary of the Forward Beechworth Committee who was involved in promoting the transformation of the mining site and promoting plantation forestry and tourism as alternative industries. £300 to begin the process was provided by Mr J. McConvill, a former resident of Beechworth, who is remembered in a street name adjacent to the lake. Residents of Beechworth have worked to raise funds to improve the Lake Sambell reserve several times, such as efforts in the 1930s and 1940s to raise the banks several feet to deepen the water for swimming purposes. Fundraising campaigns include the ‘Ugly Man’ competition conducted on behalf of the Wallace Park-Lake Sambell Development Scheme. The latter competition was run by the Fire Brigade Bend’s team as part of a larger competition called the ‘Mile of Pennies’; it was won by Mr Len Knight of Beechworth’s Commercial Hotel. The ‘Mile of Pennies’ was conducted at a Carnival held on New Year’s Eve, 1947. It was proposed by the Beechworth and District Progress Association. As well as improving swimming facilities, funds were raised to install a caravan park facility near the lake. Funds were also donated by commercial entities, such as £250 received from Zwar Bros. Pty Ltd.The photograph is significant as it shows Lake Sambell at lower water levels, such as may have been experienced during period of drought.Sepia rectangular photograph printed on matte photographic paperObverse: nil Reverse: 3470beechworth, beechworth lake, lake sambell, lake, beechworth and district progress association, forward beechworth committee, ugly man, mile of pennies, wallace park lake sambell development scheme, wallace park-lake sambell development scheme, zwar bros, zwar, l.h. sambell, j. mcconvill, minister of lands, commercial hotel, len knight, rocky mountain mining company, rocky mountain mining co, gold rush, redevelopment, transformation, community fundraising, drought, 1967, 1960s

This banner was one of five banners gifted to the Beechworth Chinese community in recognition of their support of the Hospital and Benevolent Asylum in 1875, from the Carnival Committee. These banners had been purchased in China by a social envoy from Beechworth then presented to the Chinese community during the Beechworth Fine Arts Exhibition in May of that same year, by Donald Fiddes, President of the Ovens District Hospital. The Burke Museum's Chinese Collection presents the history of Chinese settlement in Beechworth from 1856 and its involvement in local community affairs in the second half of the 19th century. In settling in the area they formed their own community with distinctive Chinese cultural traditions, forming their own 'camps' with laid out streets, housing a Temple, Chinese Theatre and restaurants, hotels, stores, gambling houses and dwellings. Members of the Chinese community took an active interest in town affairs and were generous donors to the appeal to build the Ovens District Hospital in 1856/7. The vibrant colours and dynamic graphics of the silk embroidered Chinese banners were a highlight of Beechworth Charitable processions that took place in the main street. Two of the Chinese banners were conserved for the Burke Museum in 2006 by Carol Campbell of Phoenix Conservation Services with funding from Victoria’s Heritage Grants. In 2015, with the enormous support of the Copland Foundation and fundraising activities by the Friends of the Bur Museum Committee, conservation of the third banner was undertaken by Artlab Australia in Adelaide. The banners display traditional Chinese textile techniques and are visually beautiful and very rare and are considered of local and national significance, with the potential to be deemed internationally significant.Multi panelled banner with embroidery and applied design motifs on front. Back panel is painted design of two men. The front panels have been constructed using strips of various weaves and colours of silk that have been embroidered or had a design applied prior to the overall construction of the piece. The embroidery is predominantly gold work with both plyed and floss silk threads. Silk macrame fringe and tassels to central panel and padded lotus and bowl motif hanging tassel from side panels. Velvet lettering applied to front "CHINA" CHINA /beechworth, burke museum, chinese, benevolent asylum, ovens district hospital, beechworth carnival processions, carnival, processions, beechworth chinese community, beechworth fine arts exhibition, donald fiddes

This banner was one of five banners gifted to the Beechworth Chinese community in recognition of their support of the Hospital and Benevolent Asylum in 1875, from the Carnival Committee. These banners had been purchased in China by a social envoy from Beechworth then presented to the Chinese community during the Beechworth Fine Arts Exhibition in May of that same year, by Donald Fiddes, President of the Ovens District Hospital. The Burke Museum's Chinese Collection presents the history of Chinese settlement in Beechworth from 1856 and its involvement in local community affairs in the second half of the 19th century. In settling in the area they formed their own community with distinctive Chinese cultural traditions, forming their own 'camps' with laid out streets, housing a Temple, Chinese Theatre and restaurants, hotels, stores, gambling houses and dwellings. Members of the Chinese community took an active interest in town affairs and were generous donors to the appeal to build the Ovens District Hospital in 1856/7. The vibrant colours and dynamic graphics of the silk embroidered Chinese banners were a highlight of Beechworth Charitable processions that took place in the main street. Two of the Chinese banners were conserved for the Burke Museum in 2006 by Carol Campbell of Phoenix Conservation Services with funding from Victoria’s Heritage Grants. In 2015, with the enormous support of the Copland Foundation and fundraising activities by the Friends of the Bur Museum Committee, conservation of the third banner was undertaken by Artlab Australia in Adelaide.The banners display traditional Chinese textile techniques and are visually beautiful and very rare and are considered of local and national significance, with the potential to be deemed internationally significant.Multi panelled banner with embroidery and applied design motifs on front. The front panels have been constructed using strips of various weaves and colours of silk that have been embroidered or had a design applied prior to the overall construction of the piece. The embroidery is predominantly gold work with both plyed and floss silk threads.beechworth, burke museum, chinese, benevolent asylum, ovens district hospital, beechworth carnival processions, carnival, processions, beechworth chinese community, beechworth fine arts exhibition, donald fiddes

This banner was one of five banners gifted to the Beechworth Chinese community in recognition of their support of the Hospital and Benevolent Asylum in 1875, from the Carnival Committee. These banners had been purchased in China by a social envoy from Beechworth then presented to the Chinese community during the Beechworth Fine Arts Exhibition in May of that same year, by Donald Fiddes, President of the Ovens District Hospital. The Burke Museum's Chinese Collection presents the history of Chinese settlement in Beechworth from 1856 and its involvement in local community affairs in the second half of the 19th century. In settling in the area they formed their own community with distinctive Chinese cultural traditions, forming their own 'camps' with laid out streets, housing a Temple, Chinese Theatre and restaurants, hotels, stores, gambling houses and dwellings. Members of the Chinese community took an active interest in town affairs and were generous donors to the appeal to build the Ovens District Hospital in 1856/7. The vibrant colours and dynamic graphics of the silk embroidered Chinese banners were a highlight of Beechworth Charitable processions that took place in the main street. Two of the Chinese banners were conserved for the Burke Museum in 2006 by Carol Campbell of Phoenix Conservation Services with funding from Victoria’s Heritage Grants. In 2015, with the enormous support of the Copland Foundation and fundraising activities by the Friends of the Bur Museum Committee, conservation of the third banner was undertaken by Artlab Australia in Adelaide. The banners display traditional Chinese textile techniques and are visually beautiful and very rare and are considered of local and national significance, with the potential to be deemed internationally significant.Multi panelled banner with embroidery and applied design motifs on front. The front panels have been constructed using strips of various weaves and colours of silk that have been embroidered or had a design applied prior to the overall construction of the piece. The embroidery is predominantly gold work with both plyed and floss silk threads.beechworth, burke museum, chinese, benevolent asylum, ovens district hospital, beechworth carnival processions, carnival, processions, beechworth chinese community, beechworth fine arts exhibition, donald fiddes

This banner was one of five banners gifted to the Beechworth Chinese community in recognition of their support of the Hospital and Benevolent Asylum in 1875, from the Carnival Committee. These banners had been purchased in China by a social envoy from Beechworth then presented to the Chinese community during the Beechworth Fine Arts Exhibition in May of that same year, by Donald Fiddes, President of the Ovens District Hospital. The Burke Museum's Chinese Collection presents the history of Chinese settlement in Beechworth from 1856 and its involvement in local community affairs in the second half of the 19th century. In settling in the area they formed their own community with distinctive Chinese cultural traditions, forming their own 'camps' with laid out streets, housing a Temple, Chinese Theatre and restaurants, hotels, stores, gambling houses and dwellings. Members of the Chinese community took an active interest in town affairs and were generous donors to the appeal to build the Ovens District Hospital in 1856/7. The vibrant colours and dynamic graphics of the silk embroidered Chinese banners were a highlight of Beechworth Charitable processions that took place in the main street. Two of the Chinese banners were conserved for the Burke Museum in 2006 by Carol Campbell of Phoenix Conservation Services with funding from Victoria’s Heritage Grants. In 2015, with the enormous support of the Copland Foundation and fundraising activities by the Friends of the Bur Museum Committee, conservation of the third banner was undertaken by Artlab Australia in Adelaide.The banners display traditional Chinese textile techniques and are visually beautiful and very rare and are considered of local and national significance, with the potential to be deemed internationally significant.The banner has a narrow fuchsia embroidered top border, a wider embroidered panel depicting 2 dogs with embroidered Chinese text and a larger lower panel with the embroidered text “PRESENTED TO THE CHINESE OF BEECHWORTH BY THE COMMITEES OF THE PUBLIC INSTITUTIONS (missing) THAT TOWN IN COMMEMOR (missing) OF THE CARNIVAL 1873” The 2 lower panels have narrow decorative borders decorated with mirrors and extensive embroidery. There is an additional embroidered tab running along the right hand edge. The bottom edge has a wide knotted fringe. The back is lined with fabric decorated with a painted scene. Refer Attachment 1 quote ARTLAB AustPRESENTED TO THE CHINESE / OF BEECHWORTH BY THE / COMMITEES OF THE PUBLIC / INSTITUTIONS THAT / TOWN IN COMMEMOR / OF THE CARNIVAL 1873beechworth, burke museum, chinese, benevolent asylum, ovens district hospital, beechworth carnival processions, carnival, processions, beechworth chinese community, beechworth fine arts exhibition, donald fiddes

This banner was one of five banners gifted to the Beechworth Chinese community in recognition of their support of the Hospital and Benevolent Asylum in 1875, from the Carnival Committee. These banners had been purchased in China by a social envoy from Beechworth then presented to the Chinese community during the Beechworth Fine Arts Exhibition in May of that same year, by Donald Fiddes, President of the Ovens District Hospital. The Burke Museum's Chinese Collection presents the history of Chinese settlement in Beechworth from 1856 and its involvement in local community affairs in the second half of the 19th century. In settling in the area they formed their own community with distinctive Chinese cultural traditions, forming their own 'camps' with laid out streets, housing a Temple, Chinese Theatre and restaurants, hotels, stores, gambling houses and dwellings. Members of the Chinese community took an active interest in town affairs and were generous donors to the appeal to build the Ovens District Hospital in 1856/7. The vibrant colours and dynamic graphics of the silk embroidered Chinese banners were a highlight of Beechworth Charitable processions that took place in the main street. Two of the Chinese banners were conserved for the Burke Museum in 2006 by Carol Campbell of Phoenix Conservation Services with funding from Victoria’s Heritage Grants. In 2015, with the enormous support of the Copland Foundation and fundraising activities by the Friends of the Bur Museum Committee, conservation of the third banner was undertaken by Artlab Australia in Adelaide. The banners display traditional Chinese textile techniques and are visually beautiful and very rare and are considered of local and national significance, with the potential to be deemed internationally significant.Multi panelled banner with embroidery and applied design motifs on front. The front panels have been constructed using strips of various weaves and colours of silk that have been embroidered or had a design applied prior to the overall construction of the piece. The embroidery is predominantly gold work with both plyed and floss silk threads. beechworth, burke museum, chinese, benevolent asylum, ovens district hospital, beechworth carnival processions, carnival, processions, beechworth chinese community, beechworth fine arts exhibition, donald fiddes

This photograph was taken during the late 1800s at the Chinese camp at Beechworth, Victoria. It was in camps such as these that many would-be gold miners made their home after arriving in Australia from across Asia. After arriving in South Australia where there was no poll-tax required of migrants as was the norm in Victoria and New South Wales, those looking to settle on the gold fields walked en mass overland for hundreds of kilometres before arriving in destinations such as Beechworth. Due to widespread prejudice against Chinese gold diggers they were forced to live separate from the town and developed enclaves much like the one depicted in the photograph. As the years progressed the Chinese camp began to construct more permanent structures and included temples of worship, shops and separate burial grounds. This photograph demonstrates the early multi-cultural aspects of Australia and Victoria during the late 1800s. It also showcases pressures and prejudices specific to the Chinese migrant community and the measures taken to separate them from the rest of the predominantly white community. It also reflects the gold-rush period and one of the first draws to Australia due to its mineral wealth. Black and white rectangular photograph developed on paperObverse: None Reverse: From the/Chinese Camp/84-80-1/1997-3221chinese camp, beechworth, houses, immigrants, gold mining, gold rush, late 1800s, chinese, asia

Although it is not known where these specimens were collected, Victoria and other regions of Australia were surveyed for sites of potential mineral wealth throughout the 19th Century. The identification of sites containing valuable commodities such as gold, iron ore and gemstones in a locality had the potential to shape the development and history of communities and industries in the area. The discovery of gold in Victoria, for instance, had a significant influence on the development of the area now known as 'the goldfields', including Beechworth; the city of Melbourne and Victoria as a whole. Agate occurs when amygdales (gas pockets) form in the upper levels of basaltic lava flows. If these pockets or bubbles are iniltrated by water bearing silica in solution, the fluid dries and hardens in layers, forming round or egg shaped nodules or geodes within the rocky matrix. Agate is formed of a silica mineral chalcedony similar to quartz. The term carnelian primarily refers to the reddish shading of the stone; whether the stone is termed an agate or chalcedony type is often influenced by the degree of colour banding the specimen shows. The specimens are significant as examples of surveying activity undertaken to assess and direct the development of the mineral resource industries in Victoria and Australia, as well as the movement to expand human knowledge of earth sciences such as mineralogy and geology in the nineteenth century.Three small geological specimens that appear visually consistent with images of rough or unpolished Carnelian Agate or Chalcedony. geological specimen, geology, geology collection, burke museum, beechworth, indigo shire, north-east victoria, gemstones, agate, carnelian

Quartz is an extremely common mineral to find across the world. Quartz can have two forms; Microcrystalline quartz or Crystalline quartz. Microcrystalline quartz is a fine grain quartz where crystalline quartz is often a large crystal. This specimen is a crystalline quartz. Made of silicon oxide, this specimen is called smokey quartz crystals because of its brownish colour. However, the colour of quartz can vary. In addition, quartz are formed in deep-seated igneous rocks and crystallized through hot aqueous solutions. This type of crystal can be found all over Australia, including Beechworth in Victoria. Other places quartz can be found is the Ashburton River area in Western Australia, Marlborough in Queensland, the Lune River area in Tasmania and Kingsgate in New South Wales. This specimen is significant because it is common to find this kind of mineral. While the location of where this specimen was originally from is unknown, it highlights the many places in Australia where quartz is found. It demonstrates that quartz makes up a large portion of Australia's geology. In addition, quartz itself can vary in its colour and shape. This specimen represents one of these variations. That being smoky quartz crystals. 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 large hand-sized quartz mineral with shades of brown and gray throughout.Smoky quartz / crystals /locality/ unknown / (needs a wash) /BBgeological specimen, geology, geology collection, burke museum, beechworth, microcrystalline, quartz, quartz mining, quartz reefs beechworth, smokey quartz crystals, crystals, crystalline, silicon oxide, brown, colour, igneous rocks, magma, ashburton river, western australia, marlborough, queensland, lune river, tasmania, kingsgate, new south wales, nsw

Common Opal is a mineraloid that is non crystallising and is classed as an amorphous silicate, the chemical composition for Opal is SiO2 nH2O. Opals can develop in weathered sedimentary rock typical in arid regions where limited water enters small gaps in the rock, and the silicate is hydrated. Common opals, unlike precious opals, do not exhibit ‘play of colour’ in which the colour appears to change depending on the angle of view. While precious opals are highly valuable and cut as gemstones for jewellery, common opals can be cut into inexpensive gemstones and are also mined for various uses including as ingredients in ceramics, insulation, fillers, and abrasives. The source of this common opal specimen is unknown, but common opals are found around the world, notable deposits are found in Queensland, South Australia, New South Wales, Peru, Kenya, Nevada, Oregon, and Mexico. This common opal specimen is of historic and scientific significance due to its donation in 1868 as part of the Geological Survey of Victoria and as a typical example of uncut common opal. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A palm-sized amorphous (non-crystallising) hydrated silicate mineraloid specimen in shades of brown, orange, and white.Existing label: Common Opal / Locality unknowngeological specimen, geology, geology collection, burke museum, beechworth, common opal, opal, mineraloid, amorphous silicates, hydrated silicate

Dolomite is a mineral, calcium magnesium carbonate, with the chemical formula CaMg(CO3)2. It is a principle component of various rock types sometimes also referred to as dolomite, including dolostone, dolomitic marble and dolomitic limestone (according to the composition of each type). Dolomite rock is found in sedimentary basins throughout the world, comprising approximately 2% of the Earth's crust. It is formed when lime mud or limestone encounters groundwater containing magnesium. Dolomite can contain elements such as lead, zinc and copper. Dolomite and limestone are used in various construction, landscaping and agricultural processes. This specimen was donated to the Burke Museum in 1868 by Alfred Selwyn as part of the Geological Survey of Victoria. It was donated to the Museum in 1868. Victoria and other regions of Australia were surveyed for sites of potential mineral wealth throughout the 19th Century. The identification of sites containing valuable commodities such as gold, iron ore and gemstones in a locality had the potential to shape the development and history of communities and industries in the area. The discovery of gold in Victoria, for instance, had a significant influence on the development of the area now known as 'the goldfields', including Beechworth; the city of Melbourne and Victoria as a whole. Dolomite and limestone are mined at several locations in Victoria, including sites in the North-East of the state in Bindi and Limestone Creek. There are notable dolomite deposits in most Australian states. The dolomitised form of the mineral tends to come from older limestone deposits, formed during the palaeozoic era in marine settings, so this specimen may have come from a deposit located along a coastline in Victoria or another state. The specimen is significant as an example of surveying activity undertaken to assess and direct the development of the mineral resource industries in Victoria and Australia, as well as the movement to expand human knowledge of earth sciences such as mineralogy and geology in the nineteenth century. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.Hand-sized piece of pale pink dolomite (calcium magnesium carbonate) with dark grey rim and hollowed centre. geological specimen, geology, geology collection, burke museum, beechworth, dolomite, mineralogy, geological survey, alfred selwyn, limestone, calcium magnesium carbonate

Kaolin is also known as china clay. This specimen came from Dunolly, Victoria and was donated to the Museum in 1868 as part of the Geological Survey of Victoria. This survey helped map and study the geology of Victoria. In Victoria, Kaolin is particularly used as a filler and coating material in paper manufacture. It can also be used in paints, ceramics, rubbers and plastics. There are many kaolin deposits in Victoria but many of these have been mined out and there is not much Kaolin left. Rocks that have a high amount of Kaolinite and it can be formed through the decomposition of other materials. There are two types of Kaolin; hard and soft kaolin. Soft kaolin's are coarse but have a soapy texture. It can also break easily. The hard kaolins have an earthly texture and are finer grained. This means that they are harder to break, unlike the soft kaolin. Hard kaolin's are formed by flocculation in salt water, a process that in basic terms, bonds particles together. Kaolin is a common material in Victoria and that is why it is significant. While this specimen was mined in Dunolly, Victoria Kaolin can also be found Pittong, Pakenham, Bulla, Hallam and Ballarat as well as many other places throughout Victoria. This specimen represents the presence of Kaolin deposits in this region of Australia. It is also significant because Kaolin has many uses and is largely beneficial to many manufacturing processes in 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.Two pieces of Kaolinite mineral with shades of white and graygeological specimen, geology, geology collection, burke museum, beechworth, kaolin, china clay, dunolly, geological survey of victoria, kaolinite, victoria, mining, mining deposits, geology of victoria, australia, filler, coating material, paper manufacture, paint, ceramics, rubbers, plastics, decomposition, materials, soft kaolin, hard kaolin, flocculation, particles, salt water

Actinolite is usually found in metamorphic rocks, such as contact aureoles surrounding cooled intrusive igneous rocks. It also occurs as a product of the metamorphism of magnesium-rich limestones. Pyrite is usually found with other sulfides or oxides in quartz veins, sedimentary rock, and metamorphic rock, as well coal beds, and as a replacement mineral in fossils. Actinolite is an amphibole silicate mineral. It is named after the Greek word "aktinos" meaning “ray” in allusion to the mineral's fibrous nature. Fibrous actinolite is a type of asbestos and was once mined along Jones Creek at Gundagai, New South Wales. Pyrite or "Fool's Gold" is the most common sulfide mineral. It is named after the Greek "pyr" meaning "fire" because it can be used to create sparks needed for a fire if struck against metal or a hard surface. Due to its gold colour, pyrite can be mistaken for gold and often forms alongside it, causing small amounts of gold to be present in rocks containing pyrite. Most importantly, pyrite is an ore of gold. Pyrite is sometimes used as a gemstone but is not great for jewellery as it easily tarnishes. In some fossils of ammonites – shelled cephalopods that died ~66 million years ago – pyrite also replaces the shell. 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-medium-sized solid specimen with the minerals actinolite (dark green fibrous) and pyrite (brassy) with shades of brown, black/grey, and white. Actinolite is an amphibole mineral in the tremolite-actinolite series of calcium, magnesium, and iron silicates. Pyrite is an iron disulfide mineral.geological specimen, geology, geology collection, burke museum, beechworth, indigo shire, geological, mineralogy, pyrite, actinolite, victoria, sewyln, alfred selwyn

Malachite is a water soluble, crystalline, triphenyl methylene chloride salt. It has a close relationship to copper because it is common for Malachite and copper to come from the same ore. Malachite often has shades of green, making it also known as Malachite Green. As a result of it's colour, it is known for being a dye and has been used in the dye industry, the textile industry and in medical fields. Cobar in New South Wales is well known for it's mining. This is because of the number of important deposits present in the area and include three important mining belts where most of the materials are found. These are the 'Cobar belt', the 'Canbelego belt' and the 'Girilambone belt'. The 'Cobar belt' runs underneath the main town. Copper was first discovered in Cobar in 1869 and since then, many deposits of other materials have been found, including Malachite.This specimen is significant because it comes from Cobar, NSW and represents the many deposits of materials found there. Cobar has a long history of mining and is a source of Australia's copper minerals. Malachite is often found in copper deposits meaning that it is representative of Cobar's copper production. Malachite is known for it's vivid green colour and as a result, has many uses, such as meaning used as a dye. This makes it a valuable material and highly significant. 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 mineral with shades of brown , white and light green throughout.geological specimen, geology, geology collection, burke museum, beechworth, malachite, copper, water soluble, cobar, cobar mines, cobar mining, cobar nsw, nsw, new south wales, mining belts, ore, copper ore, malachite green, dye, green, dye industry, textile industry, desposits, canbelego, girilambone, alfred selwyn

This particular specimen is found in Wolgan Valley, New South Wales. It could be linked to the abandoned oil shale mining sites in Wolgan Valley such as Newnes. Newnes was an industrial complex operational in the early 20th century is now partly surrounded by Wollemi National Park. It produced motor spirit, kerosene, and gas oil. Newnes's Torbanite oil shale rock contained around 350 litres of oil shale per tonne. The Torbanite was mined by the Commonwealth Oil Corporation Ltd. Oil shale is a sedimentary rock and also a form of fossil fuel. It is often formed millions of years ago and usually contain fossilised remains of plants and/or animals. Oil shale is rich in kerogen that releases hydrocarbon when heated. These hydrocarbon can be used as an alternative petroleum or natural gas. The oil-shale rock was converted into oil by "destructive distillation"; the rock being heated until it broke down to form an oily vapour and an ash residue. Oil bearing shale is one of Australia's national assets. There are many oil companies established in Australia. It reflects Australia's rich natural resources as well as connection to the Australia's engineering and oil industry. The booming oil shale extraction businesses can be traced as far back as 1920s. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.Piece of dark gray oil bearing shale with shades of light brown and fossilised leavesExisting label: OIL BEARING SHALE with / FOSSILISED LEAVES / Locality: Wongan Valley, NSW / Donor: Miss M. Cambell geological specimen, geology, geology collection, burke museum, beechworth, oil shale, shale, fossil fuels, alfred selwyn, wolgen valley, 1868 geological survey of victoria, rocks, sedimentary rocks, newnes, torbanite, commonwealth oil corporation ltd

Amazonite is classed as a Tectosilicate and is part of the Feldspar group of minerals. Amazonite forms in a triclinic crystal structure and its chemical formula is K(AlSi3O8). In appearance, Amazonite can range from shades of green to green blue to blue, and often with white streaks or veining. The greenish colour is believed to come from the small amount of lead contained in its composition. Amazonite is named after the Amazon River due to its colour and similarities to another rock found along the riverbanks, although Amazonite is not actually found at or near the Amazon. Although less commonly used in jewellery today, Amazonite has been mined and used by humans for thousands of years and Amazonite jewellery from at least 2000BCE have been discovered in North Africa. Amazonite is found in many locations around the world including Brazil, Peru, Ethiopia, Canada, Russia, Mozambique, Myanmar, Pakistan, China, Madagascar, and the United States of America. This specimen most probably comes from the U.S.A., Amazonite is found in several US states particularly in Colorado, Virginia, Pennsylvania. This specimen is of both scientific and historic significance as a striking blue green example of Amazonite mined prior to 1868 in the United States of America, most likely from Colorado, Virginia, or Pennsylvania. These three states are all locations of significant Amazonite deposits. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A palm-sized Feldspar mineral specimen from the Tectosilicate class in shades of blue-green with white veining.Existing label: green/blue Feldspar / "amazonite" / possibly USA geological specimen, geology, geology collection, burke museum, beechworth, tectosilicate, amazonite, feldspar, triclinic crystal structure, amazonite usa, amazonite colorado, amazonite virginia, amazonite pennsylvania

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. 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. Although there is no indication available of the locality from which the specimen was sourced, it is likely that the specimen was collected either in South Australia in the vicinity of the Burra Burra mines or in Victoria as part of programs of geological surveying undertaken in the Nineteenth and Twentieth centuries. 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 quartz pebbles in red conglomorate matrix presenting shades of cream, brown and green.Existing label: Malachite / (green) in / conglomerate / (white quartz / pebbles / in red matrix /geological specimen, geology, geology collection, burke museum, beechworth, geological, indigo shire, malachite, malachite specimen, australian mines, mines, geological survey, conglomorate, matrix

Agate occurs when amygdales (gas pockets) form in the upper levels of basaltic lava flows. If these pockets or bubbles are iniltrated by water bearing silica in solution, the fluid dries and hardens in layers, forming round or egg shaped nodules or geodes within the rocky matrix. Agate is formed of a silica mineral chalcedony similar to quartz. Although relatively common and semi-precious, agate has been prized since at least 1450 BC - an intricately carved agate seal was found in the 2015 excavation of a grave belonging to a Mycenaeum priest or warrior near Pylos in Greece. Agate is also used in jewellery and other decorative or ritual purposes due to its often striking appearance. Quartz is found all over Australia, including Beechworth in Victoria. It is formed in deep-seated igneous rocks and crystallized through hot aqueous solutions. It can have two forms; Microcrystalline quartz or Crystalline quartz. Microcrystalline quartz is a fine grain quartz where crystalline quartz is often a large crystal. The colour of quartz can vary. These specimens were collected in Victoria in the vicinity of the Burke Museum. Victoria and other regions of Australia were surveyed for sites of potential mineral wealth throughout the 19th Century. The identification of sites containing valuable commodities such as gold, iron ore and gemstones in a locality had the potential to shape the development and history of communities and industries in the area. The discovery of gold in Victoria, for instance, had a significant influence on the development of the area now known as 'the goldfields', including Beechworth; the city of Melbourne and Victoria as a whole.The specimens are significant as examples of surveying activity undertaken to assess and direct the development of the mineral resource industries in Victoria and Australia, as well as the movement to expand human knowledge of earth sciences such as mineralogy and geology in the nineteenth century.Geological specimens of Agate and Quartz respectively; the fist-sized piece of Agate has peach/coral colouring with grey concentric patterning and the smaller piece of quartz is a uniform yellow/orange shade. Existing label: Local pebbles / (agate and / quartz / (yellowish) / egg-shaped). / BB geological specimen, geology, geology collection, burke museum, beechworth, agate, quartz, north-east victoria, indigo shire, geological surveys

Agate occurs when amygdales (gas pockets) form in the upper levels of basaltic lava flows. If these pockets or bubbles are iniltrated by water bearing silica in solution, the fluid dries and hardens in layers, forming round or egg shaped nodules or geodes within the rocky matrix. Agate is formed of a silica mineral chalcedony similar to quartz. Although relatively common and semi-precious, agate has been prized since at least 1450 BC - an intricately carved agate seal was found in the 2015 excavation of a grave belonging to a Mycenaeum priest or warrior near Pylos in Greece. Agate is also used in jewellery and other decorative or ritual purposes due to its often striking appearance. These specimens originated in North Queensland, which contains noted agate-fossicking regions such as in the area surrounding Forsayth. They were collected in approximately 1852 as an adjunct to the Geological Survey of Victoria. It was donated to the Museum in 1868. Victoria and other regions of Australia were surveyed for sites of potential mineral wealth throughout the 19th Century. The identification of sites containing valuable commodities such as gold, iron ore and gemstones in a locality had the potential to shape the development and history of communities and industries in the area. The discovery of gold in Victoria, for instance, had a significant influence on the development of the area now known as 'the goldfields', including Beechworth; the city of Melbourne and Victoria as a whole. The specimens are significant as examples of surveying activity undertaken to assess and direct the development of the mineral resource industries in Victoria and Australia, as well as the movement to expand human knowledge of earth sciences such as mineralogy and geology in the nineteenth century. Two solid egg-sized pieces of peach/orange toned agate (a common semi-precious chalcedony, similar to quartz) with a striped pattern, embedded in a light and dark brown matrix. geological specimen, geology, geology collection, burke museum, beechworth, agate, north queensland agate, 1852 geological survey of victoria, l. hufer - donor, mineralogy, agate specimen, indigo shire

Galena occurs in a range of deposit contexts, often in metalliferous veins, such as Broken Hill, Australia; Coeur d’Alene, Idaho, United States.; Clausthal Zellerfeld, Germany; and Cornwall, England. Large deposits also replace limestone, dolomite, or occasionally organic matter, or have a contact-metamorphic origin. Galena is additionally found in cavities, brecciated (fractured) zones in limestone and chert, and in coal beds. This specimen was recovered from Broken Hill NSW and is 60% lead with 8-12 oz/silver to the ton.Galena or 'lead glance' is a grey lead sulfide and the chief ore mineral of lead. It forms isometric crystals in which the ionic lattice is similar to sodium chloride. Galena is brittle and easily weathers to secondary lead minerals, with the upper part of mineral deposits often containing cerussite, anglesite, and pyromorphite. It usually contains silver, which is mined along with its lead content. Other commercially important minerals that form in close association with galena are antimony, copper, and zinc. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A small-sized solid specimen containing one mineral with a sparkly silver metallic lustre exterior and pastel-grey interior.geological specimen, geology, geology collection, burke museum, beechworth, galena, lead sulphide, alfred selwyn, broken hill

Anthracite typically occurs in geologically deformed areas due to extreme heating – with temperatures ranging from 170 to 250 °C – caused by igneous intrusions or high geothermal gradients. It is most commonly found in northeastern Pennsylvania in the United States; however, smaller amounts are also found in Australia, China, eastern Ukraine, South Africa, western Canada, and other countries. This specimen was recovered from Tasmania and is 85-95% carbon.Anthracite is the mineral name for hard coal and is the least plentiful of all coal types. It is clean to the touch and, when polished, is used for decorative purposes. Before natural gas and electricity, anthracite was used for domestic heating as it produces little dust, burns slowly, and gives off a minor amount of smoke. However, it is also limited in abundance and expensive. 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 highly metamorphosed coal mineral with a black/steel-grey shiny metallic lustre.geological specimen, geology, geology collection, burke museum, beechworth, indigo shire, geological, mineralogy, victoria, alfred selwyn, anthracite

It is not known where this opal originated. Common Opal is formed from silica-rich water entering the earths crust and hardening into a gel of water and silica-spheres, layered through the specimen. Common opal differs from precious opal in colouration and appearance, with precious opal including more colours, and having a translucent or glossy appearance, where common opal shows less colour and is typically opaque. It scores high on the Mohs hardness scale, and is common throughout the world, especially in Australia, where it is far more prevalent than the highly-prized precious opal. Australia is also the highest producer of opals in the modern world. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A solid, silica-based mineral specimen of Common Opal in shades of grey, green, and yellow, with a thick grey vein running through the centre. geological specimen, geology, geology collection, burke museum, beechworth, opal, common opal, gemstone, mining

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

A granular metamorphic rock, marble is derived from limestone or dolomite and composed of calcite or dolomite interlocking grains. Heat and pressure from overlying sediments form it from limestone buried deep in Earth's crust. Graphite, pyrite, quartz, mica, and iron oxides can affect rock texture and colour. This specimen was found in Carrara, Italy. Carrara marble is the most common marble found in Italy, and it gets its name from the region where it is located. The marble was also called Luna marble and was used as a decorative element in buildings and sculptures. It has been quarried since Roman times in the Lunigiana, the northernmost tip of Tuscany, just outside the city of Carrara in the province of Massa and Carrara.Marble is one of the most popular and expensive rocks used in sculpture, architecture, interior decorations, statues, table tops, and novelties. It is available in various colors and textures depending on the chemical composition. The strength of the rock and its ability to hold finer details have made it a favorite among designers. 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 Marble (metamorphic rock) predominantly white with specks light grey and ochre geological specimen, geology, geology collection, burke museum, beechworth, marble, carrara marble, italian marble, marble specimen, tuscany

Bituminous coal is the most common type of coal, abundantly found in ancient coal deposits which can be dated back millions of years. Often referred to as soft or black coal, this specimen exhibits a high carbon content, ranging from 76-86%. It also holds a relatively high energy density (27 MJ/kg) meaning that it releases significant amounts of energy when burned. Bituminous coal is most commonly used for electricity generation, as well as in the production of steel. This particular piece of coal was collected as part of the Geological Survey of Victoria in the nineteenth century. It originates from Cape Paterson, a seaside village located in South Gippsland, Victoria (located on Bunurong Country). The discovery of bituminous coal in this locality was first made in 1826 by explorer William Hovell. More discoveries were gradually made over the following decades and in 1859 the Victorian Coal Company commenced the first active coal mining operations in the state by sinking a number of shafts and bores near the area of Cape Paterson. Evidence of this coal-focused past can be found today at the State Coal Mine Museum in the nearby town of Wonthaggi. This specimen is significant as it was collected from the locality of Cape Paterson in Victoria, an area that has since become historically instrumental in the mining of coal and other substances in the state 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 hand-sized piece of bituminous coal with a shiny black-grey surface and jagged edges.Existing Label: BITUMINOUS COAL / Locality: Cape / Patterson, VIC. burke museum, beechworth, geological, geological specimen, state coal mine museum, wonthaggi coal mine, victorian coal company, bituminous coal, coal victoria, coal energy generation, william hovell, cape paterson, coal specimen