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 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

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

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

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

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

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

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 image appears to show nurses at what is now the Mayday Hills Mental Asylum arriving for work in approximately 1900. These individuals are part of a long history of nursing in Beechworth. Three medical or social welfare facilities opened in the mid-1800s as part of a push by the township to become a regional centre for Government services. These were the Ovens District Hospital (opened in 1857), the Ovens Benevolent Asylum (opened in 1863), and the Beechworth Mental Hospital (opened in 1867 and renamed Mayday Hills Hospital at Centenary celebrations in 1967). It was recognised that the unsettled living conditions, poverty and relative isolation of the Goldfields environment could produce 'mental disturbances' which required local treatment facilities as services in Melbourne were too far away. Carole Woods' publication 'A Titan's Field' describes activities undertaken by patients at Beechworth Mental Hospital as including monthly balls and occasional concerts as well as work to make the facility self-supporting such as farm work and making clothes. She mentions a report in 1870 that the approximately 300 patients were clean and neat with 'no-one in restraint or seclusion' but that by 1905 the organisation had 623 patients which placed strain on building infrastructure such as heating and water supplies, leading to high turnover of nurses and other issues. A program of building works to extend and improve facilities followed over subsequent decades. 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 social and medical amenities in the early Twentieth Century, around the time of Australia's Federation into one nation. 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 rectangular 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.Obverse: i /burke museum, beechworth, lantern slide, slide, glass slide, plate, burke museum collection, photograph, monochrome, magic lantern, indigo shire, north-east victoria, nineteenth century, 1900s, twentieth century, emulsion slides, nursing, nurses, mental hospitals, lunatic asylums, asylums, social services, social welfare, insane asylums, mental health, infrastructure

This image shows a view of a properties bordering a river in the vicinity of Beechworth in approximately 1900. Although the exact location of the photograph is yet to be determined, the water source pictured may feed into the bigger system that flows through Beechworth Gorge. A man wearing a hat, possibly the photographer, is silhouetted in the foreground of the picture. 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, photographer, beechworth gorge, river, stream, water source, 1900s

This image appears to show nurses at what is now the Mayday Hills Mental Asylum in approximately 1900. These individuals are part of a long history of nursing in Beechworth. Three medical or social welfare facilities opened in the mid-1800s as part of a push by the township to become a regional centre for Government services. These were the Ovens District Hospital (opened in 1857), the Ovens Benevolent Asylum (opened in 1863), and the Beechworth Mental Hospital (opened in 1867 and renamed Mayday Hills Hospital at Centenary celebrations in 1967). It was recognised that the unsettled living conditions, poverty and relative isolation of the Goldfields environment could produce 'mental disturbances' which required local treatment facilities as services in Melbourne were too far away. Carole Woods' publication 'A Titan's Field' describes activities undertaken by patients at Beechworth Mental Hospital as including monthly balls and occasional concerts as well as work to make the facility self-supporting such as farm work and making clothes. She mentions a report in 1870 that the approximately 300 patients were clean and neat with 'no-one in restraint or seclusion' but that by 1905 the organisation had 623 patients which placed strain on building infrastructure such as heating and water supplies, leading to high turnover of nurses and other issues. A program of building works to extend and improve facilities followed over subsequent decades. 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 social and medical amenities in the early Twentieth Century, around the time of Australia's Federation into one nation. 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 circular 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, magic lantern, indigo shire, north-east victoria, nineteenth century, 1900s, twentieth century, emulsion slides, nursing, nurses, mental hospitals, lunatic asylums, asylums, social services, social welfare, insane asylums, mental health, infrastructure

This specimen is a native copper specimen that is metallic. Copper is typically found in the earth's crust and is often found alongside other metals such as gold, zinc, lead and silver which all belong to the same group which is the Copper/Gold group. Copper is most commonly formed from large masses of molten lava rock which has solidified in the earth's crust and over time though different sizes and speeds of crystal growth has turned into large amounts of copper, stored in porphyry copper deposits. Copper has a distinctive colour, yet can sometime appear blue and greenish which is often caused by oxidisation or a mixture of copper and other metals. This specific specimen was recovered from Moonta, South Australia. The Moonta Mining Company was established in 1861, after a Shepard in the area noticed traces of copper. This lead to a rush in the copper mining industry which was relatively young in Australia at the time, making Moonta Mining Company one of the richest in Australia. By the 1860's, South Australia had been nicknamed the "Copper Kingdom" due to its vast amount of Large copper mines and resources. As of 2016, Australia was the second largest producer of Copper internationally, following behind Chile in first place. This copper specimen is significant historically and scientifically as it is such an important metal commonly used throughout the world in various ways. Copper is an invaluable recourse used in daily life, used in most electrical appliances as it is a great conductor of heat and electricity, as well as being soft and malleable, making it easy to bend and mould into delicate sheets and wires. Copper does not corrode and is therefore used in the production of water pipes among countless other significant necessities that are often overlooked in our society. Historically, Copper holds great significance as it was the first metal used by humans. It was discovered roughly 9000 years ago and was utilised by the Neolithic Man who learnt that heating the metal made it more malleable, thus tools and utensils were made which were far superior to the previous stone tools used by humans. This history and its connection to the current and ongoing relationship between humans and copper must be preserved and highlighted as it is integral to the history of all humankind. A small, palm-sized solid native copper mineral specimen with shades of browns, black and rustic tones throughout the specimen.NATIVE (metalic) COPPER / Locality: Moonta, South Australiabeechworth, burke museum, geological specimen, native specimen, geological, mineral, mineralogy, indigo shire, beechworth museum, copper, copper ore

Before the invention of spin driers around the 1950's most households had a mangle. A mangle or wringer is a mechanical laundry aid. This one is powered by a hand crank and used to wring water from wet laundry and seems to be a commercial one. This mangle is from the Orbost Club Hotel. It was used in the Club Hotel and later by Bronwen Di Bari in her art workshop.This item was used by the Orbost Club Hotel, the first hotel in the Orbost district.It was built in 1884 by Mr J.A. Petterson with the licence in the name of Mr Thomas Maguire, Mr Petterson's step-son (more information in Deborak Hall's In Times Gone By).A large commercial wooden and cast iron laundry mangle. It has two wooden trays and two wooden rollers. It was originally painted green. There are four metal casters on the bottom. It has a metal spring to adjust the tension with two tap handles.On side - EWBANK On turning wheel - 511 On wood at top - 24 X 5 1/4 (size of rollers) EMERALD laundry mangle wringer

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 item was used on P.C. Toby Nixon and Grace Nixon's farm, "Rolling Downs" at Bete Bolong. During WW11 the farm grew carrots, red beet, cabbages, beans and maize. Because of labour shortages the government built a Prisoner of War Camp on Russell's Hill. The manager, Dick Northrope, used three Italian prisoners to frill ring small trees and shrubs between crop harvesting. The introduction of ‘frill ringing’ and poisoning with arsenical tree killers in the 1940's and 1950's helped reduce the amount of labour required and trees on more country were treated. This enabled the hill country at Bete Bolong to become more productive. The dead trees and shrubs were later cleared by Erle Broome's D7 caterpillar bulldozer. This was the first big area of 230 acres to be cleared in the Orbost district. Soon after entering World War 11 Australia was asked by Britain to accept and guard large numbers of 'enemy aliens' and prisoners of war. The British government felt that it could not afford to feed large numbers of prisoners and it was believed that once in Australia the internees would have no chance of escape. Eager to show solidarity with Britain's cause, Australia readily agreed and decided to place the prisoners in a number of different camps scattered around the country and guard them with reservists and soldiers too unfit to serve overseas. There was an internment camp at Bete Bolong, Orbost. This item is an example of an item used by the Italian P.O.W.'s residing there. It is also an example of an agricultural tool not commonly used today.A galvanized iron watering can which has been used to hold poison for ring barking trees (possibly arsenic). It has a narrow spout. There is a handle at the back and a folding handle on the top. The top is conical with an opening for a cork. agriculture prisoner-of-war-camp tree-removal land-clearing

The Snowy Water Inquiry was commissioned in 1998 with a brief to recommend environmental water release options to the Commonwealth, Victorian, and NSW Governments so that corporatisation of the Snowy Mountains Scheme could proceed. These release options related to the Snowy River below Jindabyne, the Murray River and other rivers associated with the Scheme. The Inquiry objectives were that the recommendations would not adversely impact on water supplies to existing irrigators or the viability of the Snowy Mountains Scheme. (ref snowyhydro.com.au)This report contains information about water allocation and uses of the Snowy River.A book of 160 pp - Snowy River Inquiry Final report 23rd October 1998. Submitted to the Governments of New South Wales and Victoria / Commissioner: The Hon. Robert Webster. On the front cover are three aerial photographs of the Snowy River and Snowy Hydro Scheme. The book contains maps and photographs. snowy-river snowy-hydro snowy-mountains government-inquiry

This photograph shows the second major bridge across the Snowy River at Orbost. The current Snowy River bridge is the fourth to provide a crossing to the township of Orbost. The first, in 1891, lasted just two years before it succumbed to flood waters. The bridge in this photograph was built in the 1920s as a road and rail bridge, and was again partly washed away by flood waters in 1934. After the end of the first World War the Victorian Railways considered an extension of the railhead across the river at Orbost, and in 1922 a new timber and steel girder structure, a joint Country Roads Board — Victorian Railways venture, was built and completed at a cost of £41,000 (the steel girders came from the Flinders Street viaduct reconstruction). Subsequently it was decided not to take the railway across the river, and the bridge was only used by road traffic. It was severely battered by floods during its life. and after the 1971 floods was eventually replaced by the current bridge in 1975. (info from Newletter 54N by John Phillips) This item is an early pictorial record of the previous Snowy River bridge at Orbost.A postcard with a black / white photograph of a bridge - timber and steel girder structure - across the Snowy River at Orbost, Reflections of the bridge are seen in the water.snowy-river-bridge-orbost

This photo shows the Storm Bird at the end of the jetty and the Wangrabelle in the foreground. Both ships were well known traders. the Wangrabelle became beached and wrecked in 1916 and the Storm Bird became obsolete when the railway from Bairnsdale to Orbost arrived in 1916. (ref. Story of Gippsland Shipping - J.C. Bull) At the start of the river trade goods were shipped from Marlo to Melbourne but when the railway reached Bairnsdale this became unprofitable and the ships plied only between Marlo and Cunninghame. Eventually river transport became economically unviable. The Wongrabelle is still buried in the sands of the entrance of the Snowy River (albeit where the entrance used to be). It took from April 11th 1912 to August 12th 1912 for the loss of the Wongrabelle to be complete, the final entry in the Orbost Shipping Co. records reads:- "The Wongrabelle is completely covered in sand." (ref River, Road, Railway Newsletter O.D.H.S.) This is a pictorial record of a time when the water highways were the only feasible transport mode in sending goods from Orbost and Marlo to Melbourne.A black / white photograph of a ship, sails down, anchored at the Marlo jetty.on back - "M. Gilbert, Wangrabelle at Marlo"storm-bird wangrabelle shipping transport- marlo

The pumpkin in this photograph was an award winner and was grown by Fred Mundy Snr. It weighed 194 lbs (approx. 88 kgs). Pumpkins were grown widely on Orbost farms and used to feed pigs. There was usually a competition for the heaviest or biggest pumpkin at the annual Orbost agricultural Show.This photograph is associated with the history of pumpkin growing in the Orbost district.A small black / white photograph of man with three children sitting in a hollowed out pumpkin in water. An Australian flag is on the left side of the pumpkin.on back - "Alec Cameron, Mr Fred Mundy" ; "Record pumpkin - Mr Fred Mundy 194lbs"mundy-fred pumpkins-orbost

This type of cast iron kettle was used by pioneer families, mainly rural in the early 1900's upon open fires. It provided a source of boiling water, in or mainly outside the kitchen of homesteads. Early homes often had an open fire containing a fountain, buckets and kettles that hung from a hook in the fireplace. These containers supplied hot water for cooking, washing and cups of tea. The fountain was placed on hob until needed and then hung over fire.This water fountain would have been used by early settlers in Orbost before the connection of electricity.A large cast iron water fountain. It has a hook on the curved swinging handle and a tap at the front. This large cast iron camp pot or cauldron has a long tap connection located at the bottom end at the front. The tap has a simple control swivel at the end to control the water flow.On lid 1934.1 - 3 to 4 On base 1934.2 - A. Kenrick & Sons 4 Gallskettle cast-iron kenrick domestic kitchen

A fireplace was the most commonly used form of heating a dwelling, cooking, and heating water for laundry and domestic uses.Fireplace accessories were an important part of the decor of houses as well as being useful items.A curved copper pan. The handle is copper tubing with a wooden handle grip. It has 4 feet in the shape of animal paws (lion?). The handle is attached with lion faces. The paws and feet are brass and attached to the pan with screws.copper fireplace domestic kindling-holder

This was probably for a light buggy. Heavy farm, and lumber wagons had wider tires. It would have been made by a blacksmith. The blacksmith fitted steel rims onto wooden wagon wheels. The red hot metal rim expands when hot, so it can be fitted to the wagon wheel. Then it contracts to create a tight fit as it cools after being dropped into a tank of water.Horse-drawn wagons are an important part of Orbost’s agricultural history. Light buggies were popular with farmers for trips into town before the common use of motorised vehicles.A large iron rim for a wagon wheel.wheel-rim wagon transport agriculture

These lamps belonged to Ernie Eaton and were used for spotlighting rabbits. Carbide lamps, or acetylene gas lamps, are simple lamps that produce and burn acetylene (C2H2) which is created by the reaction of calcium carbide (CaC2) with water. Acetylene gas lamps were used to illuminate buildings, as lighthouse beacons, and as headlights on motor-cars and bicycles. Portable acetylene gas lamps, worn on the hat or carried by hand, were widely used in mining in the early twentieth century. They are still employed by cavers, hunters, and cataphiles Torches, candles, oil lamps and kerosene lamps were designed to be carried around but they could be dangerous because they have flame as a source of light. These lanterns are significant examples of lighting devices widely used used before the use of battery powered devices. A pair of Germania lamps. They have brass cases with steel bodied generators and convex lens. .1 is a metal carbide coach lamp. .2 is a similar lamp but has the chimney missing. .3 is a metal handle used to attach a lamp to the front of the vehicle.Germania Base has circle with three leaves.lantern lamp germania coach-lamp

A coolamon is an Indigenous Australian carrying vessel. It is a multi-purpose shallow vessel, or dish with curved sides, ranging in length from 30–70 cm, and similar in shape to a canoe. Coolamons or pitchis were traditionally used by Aboriginal women to carry water, fruits, nuts, as well as to cradle babies. The necessary tools and equipment for hunting, fishing and warfare were one of the very few items that Aboriginals carried with them from place to place. Most were used for a multiplicity of purposes. Because many were made from raw natural materials, such as wood, generally only partial remains are found today. This container is an example of an implement used by the early Indigenous people of Eastern Australia.A large shallow elongated hand-made wooden receptacle used by Australian aborigines as a container for food and drink or for carrying babies.pitchi coolamon aboriginal container

A coolamon or pichi is an Indigenous Australian carrying vessel. It is a multi-purpose shallow vessel, or dish with curved sides, ranging in length from 30–70 cm, and similar in shape to a canoe. Coolamons or pichis were traditionally used by Aboriginal women to carry water, fruits, nuts, as well as to cradle babies. A shallow hand-made wooden dish used for carrying food, water and sometimes small babies. It is decorated on outside with burnt incisions.pitchi coolamon aboriginal container

Used as a bed warmer, or foot warmer. A stoneware hot water bottle, generally a round shape with an opening at the top and a round knob on one end which presumably functions as a holder. The stopper is missing. The main part of the body is cream, with the knob end brown.hot-water-bottle ceramic

Taken during World War I on the Western Front, this photograph depicts four soldiers dressed in full uniform and kit walking through muddy trenches on wooden duckboards.On the Western Front, the war was fought by soldiers in trenches. Trenches were long, narrow ditches dug into the ground where soldiers lived. They were very muddy, uncomfortable and the toilets overflowed. These conditions caused some soldiers to develop medical problems such as trench foot. There were many lines of German trenches on one side and many lines of Allied trenches on the other. In the middle was no man's land, which soldiers crossed to attack the other side. 'Duckboards' (or 'trench gratings') were first used at Ploegsteert Wood, Ypres in December 1914. They were used throughout the First World War being usually placed at the bottom of the trenches to cover the sump-pits, the drainage holes which were made at intervals along one side of the trench. This made it easier to pump out the pits when necessary. The raised edges of the boards in theory helped protect men's feet from accumulated water; walking along them (especially at night and in the wet) was something of an art as it was easy to lose one's footing and slip or trip on the fequently misaligned sections.Sepia rectangular reproduced photograph on matte photographic paperReverse: 6528/ (A copyright and reproduction notice from the Australian War Museum, printed in blue ink)/burke museum, military album, trench warfare, duckboards, soldiers, ww1, wwi, world war 1, world war i, western front

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