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

This photograph was taken in the 1960s at Lake Sambell Caravan Park and visible in the photograph are individual caravan sites with electricity outlets, a large single-story building with a caravan park banner, dirt roads, a freestanding message board, and a parked car. Lake Sambell Caravan Park opened in 1959 owing to the work of R.E. Carter, Beechworth Shire engineer from 1954-63. Carter advocated for improvements to the lake and surrounding area in order to encourage tourism in Beechworth. The opening of the caravan park was part of many improvements to Lake Sambell made in this period by Carter including: the swimming pool in 1961, water skiing and boating facilities, and increased lake surface in 1964. These improvements were financed mainly by grants from the Tourist Development Authority. The popularity of caravanning in Australia exploded during this post-war period of the late 1950s and 1960s. 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. Facilities such as electrical outlets to power caravans are present in this photograph of Lake Sambell Caravan Park. 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. This photograph is of historical and social significance in providing insight into caravanning during the 1960s in Australia. Caravanning was extremely popular during the 1960s in Australia due to multiple social and economic 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.Black and white rectangle photograph printed on photographic paper and unmounted.Reverse: 3536/ [logo back printing: KODAK/ VELOX/ PAPER] / C798 lake sambell caravan park, lake sambell, caravanning 1960s, caravan park, rocky mountain mining company, kodak velox paper, r.e. carter, l.h. sambell, caravan electricity outlets, tourist development authority, post-war prosperity, forward beechworth committee, lake sambell boating, lake sambell swimming pool, lake sambell fishing, artificial lake, travel 1960s, recreation 1960s

This photograph was taken in the 1960s of the Lake Sambell Swimming Pool with the lake itself in the background. The swimming pool area has multiple features including park benches, a water slide, and a fenced area with a diving pontoon for lap swimming and racing. Lake Sambell Swimming Pool was completed in 1961, driven largely by R.E. Carter, Beechworth shire engineer from 1954-63. Carter advocated for improvements to the lake and surrounding area in order to encourage tourism in Beechworth. The opening of the swimming pool was part of many improvements to Lake Sambell made during this period by Carter including establishing the caravan park in 1959, water skiing and boating facilities, and increasing the lake surface in 1964. These improvements were financed mainly by grants from the Tourist Development Authority. For many decades, members of the local Beechworth community had advocated for the development of swimming pool at the lake that would include a safe wadding area and Olympic standard lanes for laps and races. Throughout the 1940s the Beechworth Swimming Club tried to raise awareness and funds to address the structural engineering issues, raise the water levels, and improve swimming facilities at the lake. Beechworth Swimming Club hosted a swimming carnival at the lake in 1948, but it was decided due to several issues at the event, that no further carnivals would be hosted until necessary improvements were made to the area. Swimming pools, both artificial and built into natural environments, were an extremely popular public space throughout the 20th century in Australia. Increasing in accessibility and popularity through such developments as less restrictive swimming outfits during 1920s, public building works during the 1920s and 30s, and an increase in leisure time during a period of post-war prosperity. This photograph is of historical significance as it documents the newly established Lake Sambell Swimming Pool in the 1960s after many decades of discussion and proposals around creating a safe swimming area at the lake. Further, this photograph provides important social insights into the facilities and uses of this pool in the 1960s, and underlines the significant role public swimming pools have played in Australian social and recreational experiences. Black and white rectangle photograph printed on photographic paper and unmounted.Reverse: 3537 / C798lake sambell swimming pool, lake sambell water slide, water slide 1960s, lake sambell pontoon, lake sambell 1960s, lake swimming pool, lake swimming, beechworth swimming club, swimming pools in the 20th century, r.e. carter, tourist development authority, beechworth 1960s, lake water slide, lake sambell, wadding pool, swimming, swimming pool 1960s, leisure, recreation 1960s

This photograph was taken in the 1960s at Lake Sambell Caravan Park, visible in the photograph are individual caravan sites with electricity outlets, a large single-story building, a parked car, and two caravans partially obstructed by trees. Lake Sambell Caravan Park opened in 1959 owing to the work of R.E. Carter, Beechworth Shire engineer from 1954-63. Carter advocated for improvements to the lake and surrounding area in order to encourage tourism in Beechworth. The opening of the caravan park was part of many improvements to Lake Sambell made in this period by Carter including: the swimming pool in 1961, water skiing and boating facilities, and increased lake surface in 1964. These improvements were financed mainly by grants from the Tourist Development Authority. The popularity of caravanning in Australia exploded during this post-war period of the late 1950s and 1960s. 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. Facilities such as electrical outlets to power caravans are present in this photograph of Lake Sambell Caravan Park. 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. This photograph is of historic and social significance in documenting the enhancement of the Lake Sambell area overseen by R.E. Carter and providing insight into caravanning during the 1960s in Australia. Caravanning was extremely popular in Australia during the late 1950s and 60s due to multiple social and economic 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. Black and white rectangle photograph printed on photographic paper and unmounted.Reverse: 3538/ [logo back printing KODAK/ VELOX/ PAPER] / C798lake sambell caravan park, lake sambell, lake sambell 1960s, lake sambell fishing, lake sambell boating, lake sambell swimming pool, r.e. carter, l.h. sambell, tourist development authority, caravanning 1960s, caravan electricity outlets, caravan park, forward beechworth committee, rocky mountain mining company, lake caravan park, caravan mid 20th century, beechworth tourism, travel in the 1960s, holiday 1960s

The photograph depicts two young men standing atop a prominent outcrop at Lake Sambell, with buildings visible on the further shore. 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. An article in the Ovens and Murray Advertiser on Saturday, 5th May, 1917, gives some insight into issues in the Rocky Mountain Mining Company’s final years. The writer details the 1917 annual meeting of the Rocky Mountain Mining Company, stating that locals present appeared ‘well pleased this important local industry is in such a prosperous condition and that future prospects are so encouraging’. The author describes plans to give workers a bonus as evidence of profit-sharing that would ‘bridge the gulf between capital and labour’. The article concludes, however, with the statement that ‘there is a little arithmetical puzzle in the report in connection with the dredging operations I have been unable to solve.' The photograph is significant as it contributes to knowledge about how Beechworth reinvented itself after the Gold rush period, and more broadly how country towns repurpose and redevelop infrastructure and facilities to meet the present needs of their population. Sepia rectangular photograph printed on matte photographic paper. Obverse: nil. Reverse: 3471 / Velox (paper mark)beechworth, beechworth lake, lake sambell, l.h. sambell, mcconvill, rocky mountain mining company, rocky mountain mining co, minister of lands, forward beechworth committee, wallace park-lake sambell development scheme, wallace park lake sambell development scheme, lake, sambell, j. mcconvill, recreation, reserve, park, transformation, repurposed, redeveloped

The photograph depicts a view across the water at Lake Sambell. The image dates from approximately 1960. 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 the level of development of Beechworth in the early to mid-Twentieth Century. Sepia rectangular photograph printed on matte photographic paperObverse: nil. Reverse: 3470 / Velox (paper mark)beechworth, 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

Taken in 1920, depicted are four people in a rowing boat on Lake Sambell, Beechworth. From left to right, it is believed that the names of the people are Eric Beard, Mrs Doris Beard, and S/L to Bert Beard. The last two figures are unknown. Lake Sambell is a beautiful Victorian recreation lake and urban park with a unique history. It was created in the mid-1800s by the Rocky Mountain Mining company during the gold rush era and used as a mining site until the early 1900s, which brought Europeans into the area. It was turned into a reserve for residents in 1920 and is considered an icon of Beechworth as it represents the development of the community, human endeavour, and the spirit of the landscape.This photograph represents the community's social use of the lake in 1920.Black and white rectangular photograph print on paper.Reverse: LAKE SAMBELL/ c 1920/ from LTOR/ 1 ERIC? - BERT'S SON/ 2 MRS DORIS BEARD/ 3 S/L TO BERT BEARD/ 4 #beechworth, lake sambell, lake sambell boating, beechworth lake, social, 1920, victoria

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

Aerial view of Lake Sambell, Beechworth with town views. Lake Sambell is a beautiful Victorian recreation lake and urban park with a unique history. It was created in the mid-1800s by the Rocky Mountain Mining company during the gold rush era and used as a mining site until the early 1900s, which brought Europeans into the area. It was turned into a reserve for residents in 1920 and is considered an icon of Beechworth as it represents the development of the community, human endeavour, and the spirit of the landscape.This photograph represents Lake Sambell with town views.Black and white reproduced rectangular photograph print on paper.Reverse: Stampbeechworth lake, lake sambell, aerial photo, construction, australian landscape, #beechworth, victoria

The photographs in this set depict views across the water at Lake Sambell. The images date from approximately 1960. 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-19th 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 photographs are significant as they show the level of development in Beechworth in the middle of the Twentieth Century. Four sepia and black and white rectangular photographs printed on matte photographic paper. 3469.1: Obverse: nil Reverse: 3469-1 3469.2: Obverse: nil Reverse: 3469-2 3469.3: Obverse: nil Reverse: 3469-3 3469.4: Obverse: nil Reverse: 3469-4beechworth, 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

Taken in the 1960s, depicted are approximately twenty-nine male and female spectators at a school swimming carnival on Lake Sambell near the caravan park. Lake Sambell is a beautiful Victorian recreation lake and urban park with a unique history. It was created in the mid-1800s by the Rocky Mountain Mining company during the gold rush era and used as a mining site until the early 1900s, which brought Europeans into the area. It was turned into a reserve for residents in 1920 and is considered an icon of Beechworth as it represents the development of the community, human endeavour, and the spirit of the landscape. This photograph represents the post-gold rush era use of Lake Sambell as a recreational reserve. Swimming carnivals were held at the lake and considered a social event for the Beechworth community.Black and white reproduced rectangular photograph print on paper.Reverse: Community/ Swimming pool 1960s/ near the caravan park/ Lakes?lake swimming pool, lake swimming, beechworth carnival processions, carnival, #beechworth, beechworth 1960s, victoria

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

The photograph is of the Powder Magazine and gorge in Beechworth. The Magazine was built for six hundred and ninety-seven pounds in 1859 by "T Dawson and company." However, the walls were constructed later in 1860 by "Atchison and Lumsden," a different building firm. The Beechworth Magazine was one of many made by the government for the storage of gunpowder. However, the building eventually stopped being used as the mining decreased in the area, finally becoming unsused with the invention of nitro-glycerine compounds. The magazine was created to hold large quantities of gunpowder and much of its design was to hinder the prospective of damage. These safety features included double arched foundations and an arched inner roof, which would move a possible explosion upwards. Also, a process of lighting conductors, ventilation and heavy granite walls were incorporated in the designThe photograph shows historic significance due to its association with the mining era in Beechworth in the late 1800s. The photo shows the Powder Magazine after construction, most likely when it was storing gunpowder during a signifiant time period for the region.Black and white photograph printed on paper.beechworth, powder magazine, gunpowder, mining, beechworth powder magazine, explosives, atchison and lumsden, t dawson and company, gorge, granite, granite building, 1860

Beechworth Town Hall was designed by architects J.J. Coe and Thomas Dalziel and is dated to 1859. The building was made of granite and constructed to local builders Donald and William Fiddes. The original front to the building was replaced by a two story facade in 1889 designed by George Jobbins and built by Thomas Sandham according to a plaque on the front. The Town Hall is remarkable for its vaulted ceilings and columns. Originally the building was used as the Shire Offices but also doubled as a fire station and a courthouse, with still surviving cells underneath. Among the inmates was notorious bushranger Harry Power who was originally transported to Van Dieman’s Land for stealing a pair of shoes. He gained his freedom six years later but spent time in and out of gaol for the rest of his life for a variety of offences including a number of armed robberies. The Town Hall is now home to the Visitor Information Centre which helps visitors with amongst other things, accommodation, tours, event enquiries, and is the commencement point for Precinct walking tours. The Beechworth Town Hall is one of five distinctive granite buildings on Ford Street that comprise the Justice Precinct. It is of considerable historical significance as activity on the site dates from Australia’s gold rush period and was the administrative centre for north-eastern Victoria. The building has seen continual use from 1858 as an important public building and displays many aspects of the history of law enforcement in Victoria. The building is also of substantial architectural significance for its construction from local honey coloured granite, which also showcases early stone masonry techniques and craftsmanship. The Precinct is listed on the Victorian Heritage register and is protected by Heritage Victoria under the Victorian Heritage Act 2017. The buildings are also registered by the National Estate, the National Trust and protected by Indigo Shire Council’s Planning Scheme. Black and White rectangular postcard printed on cardReverse: 1906-1910?beechworth, beechworth town hall, town hall, jj coe, thomas dalziel, granite, beechworth historic building, courthouse, cells, geoge jobbins, thomas sandham, 1859, 1889, walking tours, beechworth historic precinct, historic precinct, harry power, bushranger, australian bushrangers, van dieman's land, transportation, armed robberies

The old Bank of New South Wales building is located on the corner of Camp and Ford streets in Beechworth, Victoria. It was constructed between 1856 and 1857 from local honey coloured granite. It was designed by architects Robertson & Hale and is a two-storey rendered brick building and the original coat of arms is still visible. The coat of arms is distinctive and consists of a kangaroo, emu, lion, and rising sun. The rear of the building was surrounded by high granite walls for security as it was the original home for the local gold office. Beechworth Honey currently offers tourist accommodation in the Hive Apartment located in the former Bank of New South Wales Managers residence.The Bank of New South Wales building in Beechworth is significant for its location in one of Australia's most prominent goldfield towns. Of particular interest is the use of distinctive local Beechworth honey coloured granite in its construction. The building’s architecture is a simple, conservative classical style known as Renaissance Revival. It is one of the few known surviving works of the architects Robertson and Hale. The decorative composition above the main entrance and the counter in the banking chamber are of special interest.Black and white rectangular photograph printed on cardAHold bank of new south wales, bank of new south wales building, beechworth bank of new south wales, bank of nsw, beechworth 1850s, robertson and hale, architects robertson and hale, rendered brick, coat of arms, granite walls, local honey coloured granite, gold office, 1856, 1857, beechworth, beechworth honey, hive apartment, manager's residence, renaissance revival

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

Date not confirmed, a farm in the Beechworth Warner property with a farmer overlooking calves, poultry and timber. This photograph depicts the farming and agriculture industry in Beechworth. The property, known as Daintree Stud or the Warner property, was formed a part of the town on Beechworth, Victoria. Beechworth became famous in the 19th century from a short- lived gold-rush. The town grew to the extent of building a hospital and mental hospital, court house, hotels, convent, and prison. During this time, the industrial growth of Beechworth was significant, seeing a rise in practices including tanning, cobbling, blacksmithing, and the selling of livestock. This photograph perhaps reveals a small degree of insight into the livestock business.Black and white rectangular photograph on matte photographic paper, unmountedReverse: 5896/ BMM 8093-1farm, agriculture, farming and agriculture, beechworth, beechworth farm, industry

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

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

Tourmaline specimens are members of a crystalline silicate mineral group based on boron but influenced by elements including aluminium, iron, magnesium, sodium, lithium, or potassium. Specimens present a wide variety of colours and forms according to the specific mix of these elements. Tourmalines are semi-precious gemstones with many applications, including commercial jewellery production. The word 'tourmaline' derives from the Sinhalese term for the carnelian or red-shaded specimens, "tōramalli". This specimen has been classified by geologists as 'Black Schoalou/Tourmaline in quartz'. Schoalou may equate to a common black-hued type of Tourmaline associated since around 1400 with mines in Saxony, Germany near a village called Schorl (today's Zchorlau). If this specimen is part of the 'Schorl' species of tourmaline it is a member of the most common group of Tourmalines, a divalent sodium ion influenced group accounting for 95% of specimens. On assessment, it was noted that the crossed lines (XIs) of this tourmaline have been fractured and rehealed by the quartz matrix in which the tourmaline rests. This item is significant as an example of its type of gemstone and the geological processes leading to its formation. A solid medium-sized piece of Black Schoalou/Tourmaline in a cream and peach coloured quartz matrix. Existing label: Black Schoalou / Tourmaline in / quartz. / Tourmalines XIs have / been fractured and / rehealed with / quartz / C. Willman / 15/4/21 /geological specimen, geology, geology collection, burke museum, beechworth, indigo shire, north-east victoria, tourmaline, quartz, boron, crystals, minerals, gemstones, semi-precious, black schoalou, zchorlau, schorl

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