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

Quartz is an extremely common mineral to find across the world. Quartz can have two forms; Microcrystalline quartz or Crystalline quartz. Microcrystalline quartz is a fine grain quartz where crystalline quartz is often a large crystal. This specimen is a crystalline quartz. Made of silicon oxide, this specimen is called smokey quartz crystals because of its brownish colour. However, the colour of quartz can vary. In addition, quartz are formed in deep-seated igneous rocks and crystallized through hot aqueous solutions. This type of crystal can be found all over Australia, including Beechworth in Victoria. Other places quartz can be found is the Ashburton River area in Western Australia, Marlborough in Queensland, the Lune River area in Tasmania and Kingsgate in New South Wales. This specimen is significant because it is common to find this kind of mineral. While the location of where this specimen was originally from is unknown, it highlights the many places in Australia where quartz is found. It demonstrates that quartz makes up a large portion of Australia's geology. In addition, quartz itself can vary in its colour and shape. This specimen represents one of these variations. That being smoky quartz crystals. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A large hand-sized quartz mineral with shades of brown and gray throughout.Smoky quartz / crystals /locality/ unknown / (needs a wash) /BBgeological specimen, geology, geology collection, burke museum, beechworth, microcrystalline, quartz, quartz mining, quartz reefs beechworth, smokey quartz crystals, crystals, crystalline, silicon oxide, brown, colour, igneous rocks, magma, ashburton river, western australia, marlborough, queensland, lune river, tasmania, kingsgate, new south wales, nsw

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

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

Anthracite typically occurs in geologically deformed areas due to extreme heating – with temperatures ranging from 170 to 250 °C – caused by igneous intrusions or high geothermal gradients. It is most commonly found in northeastern Pennsylvania in the United States; however, smaller amounts are also found in Australia, China, eastern Ukraine, South Africa, western Canada, and other countries. This specimen was recovered from Tasmania and is 85-95% carbon.Anthracite is the mineral name for hard coal and is the least plentiful of all coal types. It is clean to the touch and, when polished, is used for decorative purposes. Before natural gas and electricity, anthracite was used for domestic heating as it produces little dust, burns slowly, and gives off a minor amount of smoke. However, it is also limited in abundance and expensive. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A hand-sized highly metamorphosed coal mineral with a black/steel-grey shiny metallic lustre.geological specimen, geology, geology collection, burke museum, beechworth, indigo shire, geological, mineralogy, victoria, alfred selwyn, anthracite

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

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 shows six older Chinese men standing in a row with two younger non-Chinese men outside a small wooden business or official building in the Beechworth region, circa 1900. The two non-Chinese men are wearing clothes of the period that indicate relative prosperity (such as three piece suits, top hats, and a pocket handkerchief), whereas most of the Chinese men are wearing Western-style working clothes of the era. One Chinese man at the far right of the image is wearing similar garments to the non-Chinese men, including a bowler hat and longer, more tailored suit jacket. Chinese miners were a significant cultural group in Beechworth's gold rush period. Carole Woods' history of Beechworth, 'A Titan's Field', details that there were approximately 60 Chinese people in the area in 1855, more than 1000 in 1856 and 4700 (a quarter of the population) in 1857, despite the introduction in 1855 of official policies such as additional taxes formulated by the Victorian Government to limit access by Chinese immigrants. Most Chinese miners in the region came from southern China and had formerly worked as merchants, mechanics, farmers and shop-keepers. Chinese people were subjected to a 'protectorate' system, ostensibly to minimise the potential for conflict with other groups; this system required Chinese people to live in designated 'hygienic' camps with paid Chinese headmen who supervised the village and enforced the protectorate's rules. Chinese people were required to purchase an annual protection ticket to fund this system. The protectorate system was abolished in 1861, before this image was taken in approximately 1900, but it may still provide insight into social stratification or relationships between and within cultural groups in Beechworth resulting from such practices. 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 cultural and social relationships in the early Twentieth Century, in particular the experiences of Chinese miners. 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, chinese, chinese miners, protectorate system, protection licence, immigration, racism, classism, social groups, cultural groups, taxes, hygiene camps

This picture shows an angle of Beechworth Primary School (State School number 1560) which is also pictured in the building's entry in the Victorian Heritage Register (VHR record 1718). The school began as a national school in 1858 as an alternative to Wesleyan and Anglican schools already operating in the area. Its name was changed to Common School number 36 in 1862 and the Beechworth Academy prior to being taken over by the Education department in 1873. The new premises were built in 1875 utilising the skills of architect Henry Bastow though the original design may be attributable to the firm Wharton and Vickers. The design was used with modifications for other schools in Victoria, including the Competition School in Errol Street, North Melbourne. The school moved to the building pictured from its original premises in Loch Street, designed by Thomas Dalziel, which later became the office of the Ovens Advertiser. The school was opened on 2 July 1875 by former Beechworth resident G.B. Kerferd, who was then the Premier of Victoria. The image shows approximately ninety older students at the school in approximately 1900. There are approximately equal numbers of boys and girls pictured, with most of the individuals pictured appearing to be between the ages of twelve and fifteen. Although the school had more than 1000 students enrolled at its height, enrolments had declined to 304 in 1890. Also visible is a fringe of sequoia pines which were planted by the school children as a project lasting through to the late 1930s. 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.The image is significant because it sheds light on the educational infrastructure present in Beechworth in the early part of the Twentieth Century, including the prevalence of education for students after current-day primary-school age and the education of girls. It also provides insight into the building and design practices used by Government departments at the time. 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.Obverse: L / burke museum, beechworth, lantern slide, slide, glass slide, plate, burke museum collection, photograph, monochrome, schools, education, high school, primary school, common school, state school, state school 1560, common school 36, beechworth academy, g.b. kerferd, thomas dalziel, henry bastow, victorian heritage register, beechworth primary school, girls education, boys education, public schools, education department, pines, trees, sequoias, competition school

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 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

This fence post is from the original Snowy River Station stock yards which were where "Merindah" stands today. It was probably owned by the Marshall family at the time of transfer to "Merindah" in 1985. It was lifted out by Geoff Stevenson with a bucket on a tractor in 1986. The post was originally twice the length. The Snowy River Station was established in 1842 by Peter Imlay. In 1845 the land was sold to Norman MCLeod who named the area Orbost. After financial difficulties in the 1870's the run was taken over by W.J.Clarke and known as Orbost Station.Peter Imlay established the first white settlement in 1842 settling on the eastern side of the Snowy River where the township of Orbost now stands. This settlement was the Snowy River Station. A corner post from a post and rail fence. It is possibly made of red box.. On one side are three rectangular sections cut out with a similar one on the other sides. The post is hollow and has metal staples in the sides for attaching wires.orbost-station mcleod fence-post

An aeronautical chart is a map designed to assist in navigation of aircraft. Using these charts and other tools, pilots are able to determine their position, safe altitude, best route to a destination, navigation aids along the way, alternative landing areas in case of an in-flight emergency, and other useful information such as radio frequencies and airspace boundaries. World aeronautical charts have a scale of 1:1,000,000 and cover relatively large areas. Orbost Aero Club began in 1969 with Basil Dowie as Chair, David Nixon as Secretary/Treasurer. The group went into recess from 1977-1991 closing in 1997. The mid 1960s were boom years in flying training in Australia and the number of Aero Clubs grew rapidly. The Club played a significant role in the establishment of the small airport at Marlo and in the ongoing operation and development of the airport over the years particularly for patient transfer by aerial ambulance. The Orbost Aero Club Club played a significant role in the establishment of the small airport at Marlo and in the ongoing operation and development of the airport over the years.A laminated map of eastern Victoria. A World Aeronautical Chart. It shows elevations, longitude etc and is designed for pre-flight planning as well as pilotage. Top left hand corner - D.F.N.Nixon VH-FWD 12 Kristine Ct Cheletenham 27/7/87orbost-aero-club aeronautical-map

The Weekly Times was first published on September 11, 1869. After absorbing two other rural publications and expanding its publications, in 1902 The Herald and Standard Newspaper Company Ltd became the Herald and weekly Times, now Australia's oldest rural newspaper (more information on Weekly Times website). The article on Orbost was part of a series written by Steve Cooper with photographer, Mark Griffin. It explored communities which were struggling to survive. At that time the timber industry in the area was in decline and there was much discontent about flows to the Snowy River,This newspaper is a useful research tool.A newspaper, titled The Weekly Times, dated October 23, 1996. It contains articles about Orbost - Towns Against The Tide. The paper has an orange cover with the title in blue print and coloured photographs throughout. orbost-history-1996 weekly-times-newspaper

This book was produced by Gordon and Nina Andrews of Netherbyre in Orbost.This is a locally created book. It helps to tell the story of who the Snowy River pioneers and therefore how we came to settle here. It is a useful research tool and is significant to the history of the Orbost area.A 47pp soft covered book titled, Snowy River Pioneers, by Gordon and Nina Andrews, On the front cover is a coloured painting of a hut in bushland. It contains Charles West and other selected stories. The text is by Gordon Andrews. The artwork is by Nina Andrews and Vere Moon.Copyright 1990 Gordon & Nina Andrews Netherbyre, Orbost 3888snowy-river-pioneer stockmen

This photograph shows George Temple's store which began operating C1888 opposite the post office in the main street of Orbost. The store stocked other stores at Bendoc supplying the gold fields. The men with their pack horses are on their way to the survey camp. George Temple, born in Yorkshire on 26/2/1832 was one of the earliest Orbost storekeepers. Temple's Store was on the corner of Ruskin and Nicholson Streets opposite the post office. He packed stores to the Bendoc area goldfields. The store building eventually became part of Herbert's store when he died in 1917.This item is associated with the very early history of Orbost. George and Mary Temple were early shopkeepers who operated a store opposite the Post Office for many years. Their daughters were very talented women.A faded black / white photograph of men with pack horses standing outside George Temple's store, The Orbost Equitable, in the main street. It is on a cream coloured buff card.temple-george-orbost gold-fields-bendoc

The first meeting to form an Agricultural society in Orbost was convened by the then Orbost Progress Association and held in the Mechanics Hall on Saturday, 10th October 1891. Its first show was held on 3rd March 1904...on a site alongside the Bonang Road where the present Golf Club stands. It is currently held at the Recreation Reserve at Newmerella. This item is associated with the Orbost Agricultural Society 's Annual Show which has been a major event in Orbost for over a century. Agricultural shows are an important part of cultural life in small country towns and the Orbost Show is an integral part of Orbost 's agricultural history. Horse riding as transport, a recreational and sporting activity has always played a significant role in the social history of Orbost. A small black / white photograph of several small groups of people at an agricultural show. Some are walking, others are on horseback and some are in carts / coaches. They are in an open grassed area with trees in the background.equestrian orbost-agricultural-show recreation

This is the annual photograph of Grades 111 and 1V for pupils of the Orbost State School. The 19th of March 1886 proved an important day in the lives of many early settlers in the Orbost area, because on this day the Orbost State School opened. The fact that the school had first operated tem­porarily in a leased building, and on a half-time basis with SS2745 Jarrahmond, did not dampen the enthusiasm of the local inhabitants as they saw their offspring commence their education under the guidance of Head Teacher Campbell Mackay. However he remained in charge only until 12th of May 1886. The second Head Teacher, John Rowe, served until 1908. On 30th of June 1887, a portable room was provided; it being brought to the area by schooner. The school now had accommodation for 30 pupils; the teacher's welfare was considered because quarters of two rooms were attached. As the population increased so did the needs of the school. This was reflected in the provision of a larger classroom in 1898. This item is associated with the history of education in Orbost.A black / white photograph mounted on brown car. There are five rows of school children standing outside a wooden building. Some are sitting and others standing. A female teacher is seated on a chair in the second front row. A girl in the front row is holding a card - "Grades 111 & 1V Orbost".on front - "W. Stanley Vogt Bairnsdale"orbost-state-school education-primary-schools

Food safes / cabinets are used principally to keep food safe (from flies and other pests), clean and cool. They have been used to store perishable foodstuffs for centuries, and are still made and used today. They are usually placed in a well ventilated area to allow for air flow, thus ensuring the produce is kept cool. This was a normal household item before iceboxes came into regular use.This was a normal household item before iceboxes came into regular use.A wooden cabinet / safe. It has two doors and zinc mesh insets on the sides and front. Inside are two shelves. The back and top are closed. The knob fittings are brass. It has four turned wooden legs and the doors are hinged.furniture-domestic cabinet food-safe

Probably used in the local bean growing industry. The Orbost area was once a large bean growing area as the fertile snowy River flats produced good quality beans. It was exported to other states of Australia. Green beans were sent to Melbourne by train and later to Sydney, either via Bombala where they were railed, or to Eden to continue the journey on fish trucks. One pound per bag was considered a good price in the early 1920's and pickers were paid one shilling and sixpence. (Ref: Newmerella Valley of Plenty)A round wooden framed sieve. The frame holds the wire mesh sieve. It is braced with seven thin wire strips.sieve agriculture tool

The Orbost area was once a large bean growing area as the fertile snowy River flats produced good quality beans. It was exported to other states of Australia. Green beans were sent to Melbourne by train and later to Sydney, either via Bombala where they were railed, or to Eden to continue the journey on fish trucks. One pound per bag was considered a good price in the early 1920's and pickers were paid one shilling and six pence. Ref: Newmerella Valley of PlentyThis stationery is significant because it was specially made for the seed bean industry which was a major industry in the Orbost district for the first half of the 20th century. .1 - 2 letterheads for Orbost Beans and Grains on white paper. .2 - a buff coloured envelope for Orbost Beans and Grains Co-Operative LtdOrbost Beans and Grains Co-operative Ltd (incorporating Gippsland Bean Cleaners)stationery correspondence orbost-beans envelope letterhead

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

After gold was discovered to be deposited "for miles along Woolshed Valley" in the early 1850s, the Woolshed became a major site of mining activity in the north-east . This region was divided into large claims of 80 yards long, one of which was the one depicted in this photograph, called 'Big Johnson's Claim'. Claims such as this utilised a range of technology, including water wheels, steam engines, sluices and toms, most of which would not arrive until after 1856 when this photograph was taken. The Woolshed initially became prosperous in 1855, and labourers, such as the ones depicted in this photograph, engaged in sinking work for 7 pounds a week, whilst other mining labourers could earn up to nine. The search for gold is ingrained into the history of Victoria and therefore, images like this one which portray an open cut sluicing site can reveal important information for society and technology for the date when the photograph was taken. This image is of important historical significance for its ability to convey information about the operations of mining claims, particularly of the Woolshed Valley area that this photograph documents. This image is important for current research into the history of Woolshed, which was a major site of mining significance and operations. Therefore, this image has the capacity to be beneficial for research into society and the motivations of those living and working in this region during this period and therefore, has social significance. The Beechworth Burke Museum has additional images relating to gold sluicing and the Woolshed area which can be analysed and studied alongside images like this one. A black and white rectangular photograph printed on matte photographic paper.Reverse: 7791 / page 34. / 52% / Big Johnstone / Claim on Woolshed Goldfields / 1856 / Note canvas [illegible] building / Burke Museum /woolshed, mining, claims, mining claims, big johnson, gold

This image is a reproduction of an 1899 original depicting the 'Williams Good Luck Mine' on the Mopoke Reef (also called 'Morepork Gully') in the Dingle Ranges, approximately three miles from Beechworth. The foreground of the image is littered with piles of smashed rock and detritus, known as ‘mullock’, beside a reinforced mine shaft, a vertical access passageway allowing miners to enter the mine and haul ore out using lifting technology such as a poppet heads, whims or windlasses. A group of miners and a dog appear close to an open-sided miner’s hut. Following the discovery of gold at Beechworth in 1852, rushes quickly followed at surrounding creeks and gullies in the district. In the late nineteenth and early twentieth centuries, small syndicates of miners continued to work old or abandoned quartz reefs, often persisting without the assistance of heavy machinery to remove the large amounts of rock, in order to obtain yields at ever greater depths. The group of miners in this photograph are Mr. Roger Williams and Sons, who revived operations at the ‘Old Good Luck’ mine on the Mopoke Reef in the Dingle Range near Beechworth around 1892, working the site for more than two decades. An emigrant from Cornwall with experience in the tin mining industry, 19 year old Roger Williams senior sailed to New Zealand in 1840, then to Australia where he spent time in the Bendigo Gold Fields before settling in Beechworth in the early 1860s. Mr Williams senior worked on various mining activities in the district, including the Rocky Mountain Tunnel project. Conversant with the character of gold-bearing reefs in the area, the syndicate dug an eight hundred foot tunnel, digging down as far down as two hundred feet with little capital save their labour, to connect and provide better working access to the mass of reefs and veins in the vicinity. Progress was hampered by poor air quality charged with fumes from dynamite and large quantities of rock had to be crushed to obtain payable yields. The Victorian Goldfields are filled with ruins and remnants of the area's rich mining history, ranging from small alluvial diggings to the remains of huge mining companies. Site names often changed several times throughout the nineteenth and twentieth centuries. Some sites were abandoned and forgotten, others were worked continuously over many decades. The names of mines were often repeated at different locations throughout the Victorian Goldfields. For example, there is a Mopoke Gully heritage mine near Fryers Creek, Victoria. 'Mopoke' is a common onomatopoeic name for Morepork and Australian Boobook owls. This image has historical, social and research significance for patterns of emigration during of the Victorian Gold Rush, and the historical, social and environmental impacts of mining at Beechworth at the turn of the nineteenth and twentieth centuries. As gold became scarce and government support and large company investment waned, poor hard-working miners laboured intensively to make a living through periods of high unemployment. This image can be compared and studied alongside other historical mining photographs and objects in the Burke Museum Collection. It has potential to improve our understanding of miners working conditions and the shifting character of mining in the Beechworth district. Black and white rectangular reproduction photograph printed on matte photographic paper.Obverse: Williams Good Luck Mine Beechworth / Roger! / Reverse: 6858 / burke museum, beechworth museum, beechworth, gold fields, gold rush, victorian gold rush, gold ming history, colonial australia, australian gold rushes, mining technology, beechworth historic district, indigo gold trail, migration, indigo shire, good luck gold mine, victorian goldfields, mining syndicates, gold fever, quartz-mining, small-scale mining, old good luck mine, mopoke gully, quartz reefs beechworth

The photo from 1907-8 is a sepia print, depicting a small valley with building at base. There are flumes visible above areas of water, trees on hills and a few small cottages on the hillside. Cock's Pioneer Gold & Tin Sluicing Co NZ No 2 Site. The photo was taken of Matthews Gully looking west. Sluicing was undertaken in the area from 1900 to 1942 with some short breaks between these periods. The image depicts a location mined by Cocks Pioneer Gold and Tin Sluicing Company (as recorded on the annotation on the card mount) The Cocks Pioneer Gold and Tin Mines N.L was one of El Dorado's two largest open cut sluicing mines of the 20th Century. The other was named the Cocks El Dorado Gold Dredging Company. The Cocks Pioneer Mines operated from 1901 until 1941 and found a total of 117,378 ounces of Gold and 1,673 tones of tin concentrates over these years. The Cocks company was formed in 1898 and operated until 1941. Open cut sluicing involved the use of high-powered hoses which used the centrifugal sand pump system (known as hydraulic sluicing) which broke down the soil which was then processed for gold and other precious metals. From 1914 , four years after this image was captured, the company reformed to Cocks Pioneer Gold and Tin Mines NL (previously it was known as Cocks Pioneer Sluicing Co) and undertook large scale sluicing operations until 1929 and then 1934-1941. El Dorado is located on Reedy Creek and is surrounded by forested country to the north and east. It is 20 km east of Wangaratta in Victoria's regional north-east. John Cock was the son of a Cornish minor who arrived in El Dorado in 1858. Cock founded his gold and tin mining company which ran successfully for many years in the El Dorado region. It was an open cut sluicing company because of the abandonment of underground mining after this was deemed too dangerous. In 1935 Cock's El Dorado Company commissioned the floating dredge which is still visible in El Dorado today. The dredge was built by the Thompson engineering works, Castlemaine, and weighed over 2,000 tones and today has a place on the Victorian Registers of historic buildings. Interestingly, the name El Dorado does not derive from the gold in the region, but from the Barambogie pastoral run completed by William Baker in 1840-1841. Gold was discovered in El Dorado 1854 but the gold was too deep for individual prospectors to find, it required the use of heavy machinery.The search for gold is ingrained into the history of Victoria and therefore, images like this one which portray an open cut sluicing site can reveal important information for society and technology for the date when the photograph was taken. This image is of important historical significance for its ability to convey information about sluicing and the methods used to find gold in 1910. It also shows a location where sluicing was undertook which provides insight into the impact of sluicing on the environment at a time when it was done. This image is important for current research into the history of El Dorado, a small regional location near Wangaratta in Victoria's North East. Therefore, this image has the capacity to be beneficial for research into society and the motivations of those living and working in this region during this period and therefore, has social significance. The Beechworth Burke Museum has additional images relating to gold sluicing and El Dorado which can be analysed and studied alongside images like this one.Sepia coloured rectangle photograph printed on gloss photographic paper Reverse: 1997. 2613/ A02613/ No2 site/ Matthews Gully/ Cocks Pioneer G&T. ?? Co NZ/ No2 Site looking West/ 1907-8/ (7)sluicing, hydraulic sluicing, 1907, 1908, mining, cock's pioneer gold & tin sluicing co nz, nz, site no 2, matthews gully, west, valley, building, cottages, hillside, trees, water, gold and tin mine

The map is an early one of the township of Ballan showing street names and land owners.The map is significant in that it lists the owners of the house blocks within the township.A map showing the township and surrounding area of Ballan in 1856. Town streets are named as are the owners of the subdivided blocks of land. The map is a lithocopy and there is a scale in chains."D D Fraser" is written across the top of the map and "1856" is written in the near top right corner. There are other additions to the map but they are very difficult to decipher accurately or completely.ballan, ballan township map, ballan1856

A map of the Korweinguboora area showing roads, forests, railway lines and properties with the owners names.The inclusion of the names of landowners is of significance and value to historians.A map of the Korweinguboora area showing land subdivisions and names of owners and other physical features. There is a scale in chains. No date is certain but it could be 1902. The map has been repaired with sellotape.There are various pencil annotations but the are difficult to read.talbot, moorarbool west, wombat, bullarto, korweinguboora, moorarbool east, dean, wombat state forest, barkstead