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

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

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

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

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

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

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

Fluorite comes in a variety of natural colours and crystal formations and glows under ultraviolet light (the word 'fluorescence' comes from the same etymological source). In its pure form, calcium fluoride, it is a colourless combination of the elements calcium and fluorine, but gains its colour from trace elements that infiltrate or replace calcium within its crystal structure during its formation. Although fluorite crystals polish well and can achieve a high level of lustre, the mineral is very soft (4 on MOHS hardness scale) so it is unsuitable for use in rings and must be handled and stored carefully if used in other forms of jewellery. Most crystals of the mineral are too coarse for decorative purposes but have been mined under the name fluorspar for a variety of commercial and industrial purposes. These include the production of hydrofluoric acid, smelting metal alloys, producing glazes and ceramic finishes and use in medical and dental products. An existing label for this specimen indicates that its origin or collection-point was 'probably USA.' Fluorspar, the form of fluorite used commercially and industrially, was mined in significant quantities in the counties of Hardin and Pope in South-Eastern Illinois throughout the Nineteenth and Twentieth Centuries. Fluorite was made Illinois' state mineral in recognition of its contribution to the state's identity and economy. The specimens are significant as examples of surveying activity undertaken to assess and direct the development of the mineral resource industries, as well as the movement to expand human knowledge of earth sciences such as mineralogy and geology in the nineteenth century.The specimen is a piece of purple shaded fluorite (also known as fluorspar), the mineral form of calcium fluoride. The unpolished specimen presents a dark purple interior with a substantial dark grey crust representing the matrix from which the specimen was obtained. Existing label: Flourite / (purple) / probably / USA / BB /burke museum, beechworth, geological, geological specimen, fluorite, flourite, calcium fluoride, hydrofluoric acid, jewellery, indigo shire, north-east victoria, mining, illinois, usa, united states, fluorine, gemstones, purple stones

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

Malachite is a copper carbonate hydroxide mineral. It has a chemical composition of Cu2(CO3)(OH)2. It often forms within limestone where a subsurface chemical environment favourable for the formation of carbonate minerals can occur. It is a substance that can be found in many different parts of the world including: Australia, USA, Russia and the Democratic Republic of Congo. Malachite has historically been used to produce copper, with mining of the mineral dating back over a period of four thousand years. Due to its beautiful green colourations, it is also commonly used for aesthetic purposes such as in the production of sculptures and jewellery. This particular specimen was collected from the town of Burra, South Australia as part of a geological survey undertaken during the nineteenth century. The locality (located on Ngadjuri Country) has a long history of mining, particularly in copper mining, as the area is rich in copper deposits. The first significant discovery of this was made in Burra (Burra Burra Mine) in 1845 and, at the time, the mine was the largest and richest of its kind in the world, producing nearly five percent of the total world copper output. This specimen is significant as it is considered to be a rare gemstone, as many of the original deposits for the stones are significantly depleted, leaving behind very few sources. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A solid palm-sized copper carbonate hydroxide mineral with patterns of green colourations Existing Label: MALACHITE / Locality: Burra / S. Aust. Other Label: Confirmed / as Malachite / C. Willman / 15/4/1 / + Bill Birch burke museum, beechworth, geological, geological specimen, malachite, gemstone, green gemstone, burra, burra burra mine, burra south australia, carbonate mineral, copper, copper mining, copper mining burra, carbonate hydroxide mineral, copper carbonate, malachite mining, malachite burra, monster mine

Montmorillonite is a type of clay composed of aluminium silicate that forms very small particles that are not well-bonded to one another. This is why it is so soft. When in the presence of water, all types of clay swell. Montmorillonite swells even more than most types of clay, which is why it is often chosen over other types of clay in its practical uses. Montmorillonite has many different practical uses, including in the mining industry, as a soil additive, as a sealant, as a desiccant to draw water out of the air, to clean ponds, to make kitty litter and in cosmetics. Montmorillonite is a common mineral and, despite being named after Montmorillon, France, can be found all over the world, including many deposits in Australia. It is not known where this particular specimen originates from. Montmorillonite is an economically and socially significant material with a wide variety of uses. Having samples of common and important minerals allows collections, like the Burke Museum, to have a more complete view of the land on which they are located, and therefore a more complete view of heritage. 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 tennis-ball sized chunk of aluminium silicate clay. It is primarily white, accented with orange and brown.burke museum, beechworth, geological, geological specimen, clay, montmorillonite

This specimen is Cassiterite in Quartz. Cassiterite is a tin oxide metal that forms in thin crystals which can have a beautiful lustre. Quartz is made of silicon dioxide, also known as silica, and is one of the most common minerals on earth. Cassiterite has been a fundamental source of tin ore for humans throughout history, including today. Tin is an important metal that has a wide variety of human uses in different areas, from dying fabric, to making mirrors, and their most well-known use ‘tin’ cans. Tin cans are primarily made of steel and are coated with tin in order to take advantage of tin’s property of being non-corroding. This is a massive step in the history of food preservation. Tinned food first reached Australia in 1815 with early settlers, and it began to be manufactured here in the 1840s. It was incredibly popular, and was a highly exported product, which would be a contributing factor to the ‘tin mining boom’ of the early 1880s. This specimen was collected at Jingellic, New South Wales, in about 1852. Although the Goldfields of the 1800s are much more well-known, tin mines existed alongside the gold mines which began in the mid 19th century and extended almost one hundred years, to the mid 20th century. Specimens like this would have been used as evidence to justify tin mining operations in the region as an investment. 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. The Geological Survey of Victoria was headed by British geologist, Alfred Richard Cecil Selwyn (1824-1902), who was responsible for issuing over 60 geological maps during his 17 years as director. These maps were all hand-drawn and coloured and became the benchmark for accuracy for geological mapping. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study. A fist-sized solid geological specimen made on one half of tin oxide, which is dark grey, and on the other side of silica, which is brown and cream.burke museum, beechworth, geological, geological specimen

There are 17 opal fields in Australia. This opal bearing stone was found in Lightning Ridge, NSW over what is known as the Great Australian Basin. This basin was formed and covers an area of 1.7 million square kilometers in eastern Australia in the Cretaceous period. This basin used to contain an inland sea, which provided an environment where silcrete eventually formed when water levels changed. This eventually seeped into other structures, and eventually hardened and formed opal. Lightning Ridge has a population of around 2000 people, with about 80 000 visitors every year. It is a historic mining town, and is known for its deposits of a rare black opal. Mining started in the area in the late 1800s, early 1900s when the black opal was discovered. This opal-bearing stone is of social and historical significance. It is from Lightning Ridge, which is well-known for being a large producer of opal stones, most famously black opal. The history of the period dates back to 140 million years, with the discovery of black opal in the early 1900s causing interest in the area. 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 solid mineral specimen in shades of beige and light orange*** silica based? burke museum, beechworth, geological, geological specimen, opal, opal fields, australia, lightning ridge, new south wales, great australian basin, cretaceous, silcrete, black opal, mining

This lantern slide shows the Ovens District Hospital (also called the Ovens Goldfields Hospital) in Beechworth in approximately 1900. The Hospital was built as part of a community push to develop the infrastructure needed for a permanent town in the 1850s. At the time there was no hospital located between Melbourne and the NSW town of Goulburn and it was recognised that the nature of mining and agricultural work predisposed people to serious injury. The community voted in 1853 to raise funds for a hospital and a voluntary committee elected from people who contributed £2 or more annually determined the organisation's management policies, which aimed to provide care for poor people at rates levied according to the person's means. Ongoing operations of the hospital were primarily supported by Government grants, however. The foundation stone was laid at a site in Church Street at a ceremony held 1st September 1856 which was attended by 2000 people using a locally crafted trowel with a tin ore handle and pure gold blade. The hospital, which was designed by J.H. Dobbyn, cost £2347. The hospital had two wards, a dispensary, apartments for a resident surgeon and the matron, an operating theatre and a board room. Further medical facilities including services to meet the cultural and health needs of the local Chinese community were later added, in addition to a Palladian-style cut-granite face built in 1862-63. It functioned as the region's primary hospital until surpassed by the Wangaratta Hospital in 1910. In the 1940s much of the building materials were salvaged and repurposed, with the exception of the facade which was restored in 1963 by the Beechworth Lions Club and still stands today. The facade featured on the covers of local history volume 'Beechworth: a Titan's Field' by Carole Woods and heritage-focused travel guide the 'Readers Digest Book of Historic Australian Towns'. Lantern slides, sometimes called 'magic lantern' slides, are glass plates on which an image has been secured for the purpose of projection. Glass slides were etched or hand-painted for this purpose from the Eighteenth Century but the process became more popular and accessible to the public with the development of photographic-emulsion slides used with a 'Magic Lantern' device in the mid-Nineteenth Century. Photographic lantern slides comprise a double-negative emulsion layer (forming a positive image) between thin glass plates that are bound together. A number of processes existed to form and bind the emulsion layer to the base plate, including the albumen, wet plate collodion, gelatine dry plate and woodburytype techniques. Lantern slides and magic lantern technologies are seen as foundational precursors to the development of modern photography and film-making techniques.This glass slide is significant because it provides insight into Beechworth's built environment and infrastructure in the early Twentieth Century, around the time of Australia's Federation. It is also an example of an early photographic and film-making technology in use in regional Victoria in the time period.Thin translucent sheet of glass with a round-edged square image printed on the front and framed in a black backing. It is held together by metal strips to secure the edges of the slide.Obverse: Y /burke museum, beechworth, lantern slide, slide, glass slide, plate, burke museum collection, photograph, monochrome, ovens district hospital, indigo shire, north-east victoria, hospital, palladian architecture, granite, community fundraising, community infrastructure, j.h. dobbyn, beechworth lions club, ovens goldfields hospital, chinese community

This image shows the gorge adjacent to Beechworth in approximately 1900. Although the exact location of the photograph is yet to be determined, the present-day Beechworth Gorge Walk includes views of the Cascades at the point at which Spring Creek flows into the valley on the level below. Gold-sluicing techniques in use in the town during periods of active gold extraction may have altered the landscape since the photograph was taken, however. In the 1850s a mill was built at the top of the Spring Creek falls by Russian-born Louis Chevalier, brother of artist Nicholas Chevalier. The mill supplied the town with lumber that supported the town's initial construction boom. Lantern slides, sometimes called 'magic lantern' slides, are glass plates on which an image has been secured for the purpose of projection. Glass slides were etched or hand-painted for this purpose from the Eighteenth Century but the process became more popular and accessible to the public with the development of photographic-emulsion slides used with a 'Magic Lantern' device in the mid-Nineteenth Century. Photographic lantern slides comprise a double-negative emulsion layer (forming a positive image) between thin glass plates that are bound together. A number of processes existed to form and bind the emulsion layer to the base plate, including the albumen, wet plate collodion, gelatine dry plate and woodburytype techniques. Lantern slides and magic lantern technologies are seen as foundational precursors to the development of modern photography and film-making techniques.This glass slide is significant because it provides insight into Beechworth's built environment and natural landscape in the early Twentieth Century, around the time of Australia's Federation. It is also an example of an early photographic and film-making technology in use in regional Victoria in the time period.Thin translucent sheet of glass with a square image printed on the front and framed in a black backing. It is held together by metals strips to secure the edges of the slide.burke museum, beechworth, lantern slide, slide, glass slide, plate, burke museum collection, photograph, monochrome, beechworth gorge, indigo shire, landscapes, mill, sluicing, gold mining, north-east victoria, spring creek, louis chevalier, cascades

Miners from Snake Valley lobbied the Victorian Government in 1855 to make land available for sale for farming purposes as an alternative occupation and income for people who wished to stay in the region but move away from gold mining. A secondary motivation was to increase the supply of fresh produce and decrease prices of items that otherwise needed to be transported from Melbourne or other regions. Forty-three country lots were initially offered in the Three Mile area, ranging in size from two to ninety acres and costing from £1 to £3 per acre. An additional eighty-five country lots were auctioned later in the year, in addition to many smaller suburban lots. More lots were offered than sold, initially, but this represented conditions of sale requiring the total purchase cost up front which many people interested in purchasing could not afford, especially as land purchased for farming would accrue substantial additional costs for clearing and labour before becoming productive. Further lobbying activities and the election of parliamentary members sympathetic to the cause took place through the 1850s. Ovens Parliamentary Member, Daniel Cameron, was re-elected in 1856 on a platform of surveying the land for public selection with deferred payment options. Land reform remained an issue in the area through the 1850s and early 1860s, impacting broader decisions in the new State of Victoria relating to voting rights, use of Crown land and the farming of land that wasn't always suitable for the purpose. This photograph depicts Beechworth in approximately 1900, after several waves of land sales resulted in increasingly levels of development. Lantern slides, sometimes called 'magic lantern' slides, are glass plates on which an image has been secured for the purpose of projection. Glass slides were etched or hand-painted for this purpose from the Eighteenth Century but the process became more popular and accessible to the public with the development of photographic-emulsion slides used with a 'Magic Lantern' device in the mid-Nineteenth Century. Photographic lantern slides comprise a double-negative emulsion layer (forming a positive image) between thin glass plates that are bound together. A number of processes existed to form and bind the emulsion layer to the base plate, including the albumen, wet plate collodion, gelatine dry plate and woodburytype techniques. Lantern slides and magic lantern technologies are seen as foundational precursors to the development of modern photography and film-making techniques.This glass slide is significant because it provides insight into Beechworth's built environment and infrastructure in the early Twentieth Century, around the time of Australia's Federation. It is also an example of an early photographic and film-making technology in use in regional Victoria in the time period.Thin translucent sheet of glass with a square-edged image printed on the front and framed in a black backing. It is held together by metal strips to secure the edges of the slide.burke museum, beechworth, lantern slide, slide, glass slide, plate, burke museum collection, photograph, monochrome, indigo shire, north-east victoria, farming, squatters, miners, agriculture, land-clearing, land reform, daniel cameron, land sales, three mile, snake valley, tarrawingee

This cardbord box was used to package explosives which were used for mining. Black powder and dynamite were heavily used on the goldfields to blast away large sections of earth which. Explosives were stored at Beechworth Powder MagazineMining played an important role in the history of Beechworth, for the township was established in the mid-1850s after gold was discovered in the area. The success of goldmining lead to the growth and development of early Beechworth.A brown rectangular cardbord box with opening flaps at top and features printed text on sides and top.GLASGOW / THE PERFECT COMBINATION / NOBEL-GLASGOW EXPLOSIVES / NOBEL-GLASGOW DETONATORSburke museum, beechworth, mining, explosives

A tin trunk used by the Rocky Mountain Extended Sluicing Company (Limited).Mining played an important role in the history of Beechworth, for the township was established in the mid-1850s after gold was discovered in the area. The success of goldmining lead to the growth and development of early Beechworth. The Rocky Mountain Company was a very successful gold mining company and had a big impact on the people and landscape of early Beechworth.A tin trunk painted in black with gold script painted on the front.The Rocky Mountain Extended / Gold Slucing Company. (Limited / BMM 8068

These protective over-boots were compulsorily worn in the Powder Magazine so as not to induce static electricity.The Beechworth Powder Magazine was constructed in 1859, and was used as a storage room for large amounts of black-powder used in mining and quarrying. By law, miners were required to leave bulk black-powder in this building overnight.Pair of brown over-boots. Large, lighter leather foot with polished harder leather back and sole, stitched at sides, four lace holes. Stitched leather insole and pull tab at back.burke museum, beechworth, mining, powder magazine, footware

Nozzle was fitted in the end of the director and was used for hydraulic gold miningMining played an important role in the history of Beechworth, for the township was established in the mid-1850s after gold was discovered in the area. The success of goldmining lead to the growth and development of early Beechworth.A sluicing nozzle attachment which is 3 inch diameter inside top. Base area has thread machined inside for attachment to sluice. Casting venturi shaped internally.3 /burke museum, beechworth, gold mining, sluicing

Alluvial deposits along with water were scooped into this pan and aggressively agitated to allow dense material, such as gold, sink to the bottom for easy extraction.Mining played an important role in the history of Beechworth, for the township was established in the mid-1850s after gold was discovered in the area. The success of goldmining lead to the growth and development of early Beechworth.A circular gold panning tin featuring sloped sides, a folded over rim, and handles.burke museum, beechworth, gold mining, alluvial mining

This specimen is a copper-carbonate malachite mineral. It is often found as crystalline aggregates or crusts, which have a banded agate-like appearance while also commonly found as botryoidal clusters of radiating crystals. Malachite is often bright green in colour, with dark green and blackish blooms or stripes/bands throughout the mineral. This particular specimen was recovered from the Burra Burra Copper Mine located Burra, South Australia. By the 1860's, South Australia was known as the "Copper Kingdom" due to its large amount of copper mines and huge success in the copper mining industry. Burra Burra was no exception to this phenomena, as this mining company was greatly famous and successful, being nicknamed the "Monster Mine". It was first established in 1848 and was the largest metal mine in Australia up until 1860. This specimen is significant as it highlights the historic use and value of malachite and the rarity of the mineral. Malachite is a rare gemstone which has been used in various ways historically. It has been cut and sculpted into beads for jewellery use as its rich colour and distinct yet unique patterns have made it a well sought after gemstone. Its' continued use over time only heightens the value and significance of this mineral.A hand-sized solid copper-carbonate hydroxide mineral specimen in shades of blue, green and copper tones throughout.MALACHITE / (Copper carbonite) / Locality: Burra, South Aust. | Malachite / Burra Burra / South Australia / (good specimen) / needs a wash / BBburke museum, burke museum collection, beechworth museum, beechworth, geological specimen, geological, mineral, mineraology, copper carbonate, malachite, burra burra mine, copper mining

Panning dishes were used for washing fine gold from river sediments or from the residue trapped in cradles and puddling tubs. They were often used on the edge of streams/rivers to sift gold from alluvial soil or crushed quartz. This simple pan would have been filled with sand and gravel which might have contained gold. The pan was submerged in the water and shaken to sort the gold from the gravel and other material, with the lighter material gradually being washed over the lip until only the heavy deposits, such as gold, remained at the bottom. (ref. Museum Victoria) This pan was used by George Henry Douglas Russell Snr. As a young man prior to his enlistment in WW1 he panned for gold using this dish. During the war he became a vet sergeant in charge of horse lines.Gold panning is the oldest and simplest method of extracting gold. Gold pans had widespread use in alluvial gold fields where water is available. This item is an example of the type of pan commonly used on Victorian gold fields.A circular dull metal panning dish which has a wide rolled top lip which tapers down to a smaller diameter for the base which is flat. The pan has been made from ironmetal which has a coating of another metal with a matte grey finish. It has a small hanging hole and a reinforcing ring all around the top.russell-doug gold-panning mining

This clock was made by Charles Frederick Falck who was a watchmaker and jeweller in Beechworth from 1863-1908. Falck was born in Körlin, Prussia on May 22nd in 1833 and died at the age of 75 in 1908. Ovens and Murray Advertiser, Beechworth: edition June 13, 1908 OBITUARY: Falck was brought up to the business of watch-making, in which he developed exceptional mechanical ingenuity. Attracted by the favourable prospects held out by the Australian discoveries of gold he, like many other young adventurous spirits, left his native land to seek his fortune in the great southern Eldorado, arriving in Adelaide in 1854, and shortly after came to Melbourne where he worked as a journeyman, and subsequently started in business on his own account. Feeling inclined to test his fortune on the goldfields, he went to Blackwood but, meeting with little success, he returned to Melbourne where he was married. In 1862, he moved to Beechworth, where he commenced business as watchmaker and gold-buyer. He then embarked in vine-growing on the Sydney road, but eventually resumed his business avocations. His skill in practical horology was evinced in a clock of his own design and manufacture, surmounted by a golden eagle, which was exhibited at the first Melbourne Exhibition in 1856, and which afterwards formed a pre-eminent attraction in the window of his business premises in Ford Street. For many years, he filled the position of timekeeper to the Beechworth Racing Club, with complete satisfaction also at various sports meetings. He leaves a family of six sons and one daughter (Mrs. Jas. Broadfoot) all arrived at maturity. The funeral, which was well attended by a number of residents, took place at the Beechworth Cemetery on Sunday, the burial service being performed by the Ven. Archdeacon Potter. The cortege was capably supervised by Mr. D. Wilson, undertaker. The clock was returned to Beechworth in 2020 through the generous support of the Copland Foundation. Given that Mr. C. F. Falck traded as a watchmaker and jeweller in Beechworth for 45 years and traded with the 1855 clock mounted in his front window, there is a direct link between the clocks and the social, cultural and economic life of nineteenth century Beechworth at time when the town was developing and expanding in response to gold mining. This clock represent the significant skill and expertise of Charles Falck as an horologist. Medium-sized pendulum clock featuring a carved gilt wood eagle with wings outstretch (épandre - expanded with wing-tips directed upwards) and perched above a pendulum rod that holds a silver dial clock face within a reeded sunburst surround. The clock has an eight-day fuse movement with dead beat escapement wound from the clock face. C. F. F. FALCK / EXHIBITION 1856 / MELBOURNEburke museum, copland foundation, beechworth, leonard joel, auction, purchase, clock, pendulum, eagle, eagle clock, charles frederick falck, c. f. falck, falck, horology, pendulum clock, melbourne

This clock was made by Charles Frederick Falck who was a watchmaker and jeweller in Beechworth from 1863-1908. Falck was born in Körlin, Prussia on May 22nd in 1833 and died at the age of 75 in 1908. Ovens and Murray Advertiser, Beechworth: edition June 13, 1908 OBITUARY: Falck was brought up to the business of watch-making, in which he developed exceptional mechanical ingenuity. Attracted by the favourable prospects held out by the Australian discoveries of gold he, like many other young adventurous spirits, left his native land to seek his fortune in the great southern Eldorado, arriving in Adelaide in 1854, and shortly after came to Melbourne where he worked as a journeyman, and subsequently started in business on his own account. Feeling inclined to test his fortune on the goldfields, he went to Blackwood but, meeting with little success, he returned to Melbourne where he was married. In 1862, he moved to Beechworth, where he commenced business as watchmaker and gold-buyer. He then embarked in vine-growing on the Sydney road, but eventually resumed his business avocations. His skill in practical horology was evinced in a clock of his own design and manufacture, surmounted by a golden eagle, which was exhibited at the first Melbourne Exhibition in 1856, and which afterwards formed a pre-eminent attraction in the window of his business premises in Ford Street. For many years, he filled the position of timekeeper to the Beechworth Racing Club, with complete satisfaction also at various sports meetings. He leaves a family of six sons and one daughter (Mrs. Jas. Broadfoot) all arrived at maturity. The funeral, which was well attended by a number of residents, took place at the Beechworth Cemetery on Sunday, the burial service being performed by the Ven. Archdeacon Potter. The cortege was capably supervised by Mr. D. Wilson, undertaker. The clock was returned to Beechworth in 2020 through the generous support of the Copland Foundation and the Friends of the Burke. Given that Mr. C. F. Falck traded as a watchmaker and jeweller in Beechworth for 45 years and traded with the 1855 clock mounted in his front window, there is a direct link between the clocks and the social, cultural and economic life of nineteenth century Beechworth at time when the town was developing and expanding in response to gold mining. This clock represent the significant skill and expertise of Charles Falck as an horologist. Large swinging clock featuring a carved gilt wood eagle with its wings outstretched (abaisé - expanded with wing-tips lowered) and perched above a pendulum rod that holds a silvered dial clock face within a reeded sunburst surround. (Similar to #2019.056.01) The clock has an eight-day fuse movement with dead beat escapement wound from the clock face. C. F. FALCK / WATCHMAKERburke museum, copland foundation, beechworth, leonard joel, auction, purchase, clock, pendulum, eagle, eagle clock, charles frederick falck, c. f. falck, falck, horology, pendulum clock, melbourne

The A1 Gold Mine is located north of Woods Point, near Jamieson, in the Upper Goulburn region of Victoria. Gold was discovered at the A1 site in 1861 and mining operations began in 1864. The A1 Mine Settlement refers to a small township known variously as Castle Reef, Castle Point, and Raspberry Creek, which developed in the 1860s around mining industry centred on a crushing machine that worked the three gold reefs in the area. Historically, the name "A1"referred to the high quality of gold found in the quartz reefs at depths of at least two thousand feet. Along with the Morning Star mine at Woods Point, the A1 gold mine produced almost sixty percent of Victoria's gold output in the 1950s to 1970s and continued operating until 1992 when it went into administration. Operations at the site were revived in 2016 and the A1 Mine is now considered one of Victoria's premier gold mines. The A1 mine is part of the extensive and prospective Lachlan Fold Belt, a north-west trending belt of tightly folded Early Devonian sedimentary rocks extending from New South Wales to Victoria. Mineralisation is hosted within or immediately adjacent to diorite dykes. Contemporary development of the 'Queens Lode' at the A1 mine signals a move from high-grade, narrow vein airleg mining into larger scale, mechanical mining designed to increase ore production volume. This original, undated photograph of the A1 Mine appears to depict an area or phase of disuse or abandonment. The aged and humble appearance of the cottage suggests association with the historical A1 Mine Settlement, therefore the image may have been taken prior to the 1950s-1970s revival period in which the A1 mine is known to have produced high gold yields. The photograph contributes to our understanding of the A1 Gold Mine's impact on the landscape and the social, environmental impacts of mining on communities and may be compared with others in the Burke Museum's extensive collection of mining photographs to deepen our understanding of mining in the Jamieson area.Black and white rectangular photograph printed on photographic paperReverse: 5577 / A1 Mine / Near Jamieson / Vic. /burke museum, beechworth museum, beechworth, gold fields, gold rush, victorian gold rush, mining tunnels, gold ming history, colonial australia, australian gold rushes, mining technology, beechworth historic district, indigo gold trail, indigo shire, upper goulburn shire, jamieson, woods point-walhalla goldfield, a1 gold mine, victorian high country, modern mining methods, orogenic gold province, gold mineralisation, devonian, dykes

This image shows the approach to Beechworth from the south-west via the Newtown Bridge. Numerous early buildings line the road as it bifurcates to become Ford and High Streets on the ridge above Spring Creek and Newtown Falls. The sloping, rocky terrain and water course along the gorge show evidence of the intense mining activity that occurred at the site. The Ovens Gold Rush at Beechworth started when gold was found at Spring Creek in February 1852, prompting an influx of miners from around the world. The population grew over 20,000 by 1857. While the earliest mining at Beechworth was similar to that in other Victorian goldfields like Ballarat and Bendigo, Beechworth is notable for its use of hydraulic sluicing as a major method of removing wash-dirt. Hydraulic sluicing employs high pressure jets of water to blast away large areas of earth and wash it down to be run through a sluice box. Gold gets caught in the sluice and the remaining slurry is washed away. This method of mining is extremely effective but causes significant environmental impacts and damage to waterways. Large water quantities were required for large-scale sluicing, and the long water races and deep tailraces that were constructed in the Beechworth area in the nineteenth century are nonetheless considered feats of engineering. The site in the photograph is associated with the Rocky Mountain Mining Company who constructed an eight hundred meter tunnel under the township between 1876-1880 to reduce water levels at Spring Creek, which had been subject to diversions since the earliest days of alluvial mining. Over four million ounces of gold (115 tones) were found at Beechworth between 1852 and 1868, and the wealth from the gold rushes built Beechworth and the nationally significant buildings that remain standing today.This image shows the early development of the Beechworth township above Spring Creek, where gold was discovered in 1852. Evidence of hydraulic sluicing, a uniquely predominant method at Beechworth, and water-works engineering are present in the landscape. By the 1870s, alluvial gold deposits were depleted and increasingly complex engineering was required so deeper shafts could reach bedrock. This image is significant for understanding changes to the landscape and the evolution of mining methods and engineering practices related to the extensive construction, manipulation and management of water networks. The shift from smaller scale alluvial mining to larger company dominance in the mining industry has implications for understanding wider social, economic, political and industrial changes in the region of Beechworth and within the context of the Victorian Gold Rush more broadly. A black and white rectangular reproduction photograph printed on photographic paper. burke museum, beechworth museum, beechworth, gold fields, gold rush, victorian gold rush, hydraulic sluicing, rocky mountain mining company, spring creek, netwown falls, mining tunnels, water races, tailraces, colonial australia, australian gold rushes, mining technology, beechworth historic district, indigo gold trail, migration, indigo shire, gold mining, gold mining history