Malachite is a water soluble, crystalline, triphenyl methylene chloride salt. It has a close relationship to copper because it is common for Malachite and copper to come from the same ore. Malachite often has shades of green, making it also known as Malachite Green. As a result of it's colour, it is known for being a dye and has been used in the dye industry, the textile industry and in medical fields. Cobar in New South Wales is well known for it's mining. This is because of the number of important deposits present in the area and include three important mining belts where most of the materials are found. These are the 'Cobar belt', the 'Canbelego belt' and the 'Girilambone belt'. The 'Cobar belt' runs underneath the main town. Copper was first discovered in Cobar in 1869 and since then, many deposits of other materials have been found, including Malachite.This specimen is significant because it comes from Cobar, NSW and represents the many deposits of materials found there. Cobar has a long history of mining and is a source of Australia's copper minerals. Malachite is often found in copper deposits meaning that it is representative of Cobar's copper production. Malachite is known for it's vivid green colour and as a result, has many uses, such as meaning used as a dye. This makes it a valuable material and highly significant. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A solid hand-sized mineral with shades of brown , white and light green throughout.geological specimen, geology, geology collection, burke museum, beechworth, malachite, copper, water soluble, cobar, cobar mines, cobar mining, cobar nsw, nsw, new south wales, mining belts, ore, copper ore, malachite green, dye, green, dye industry, textile industry, desposits, canbelego, girilambone, alfred selwyn

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

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

Malachite is a green copper carbonate hydroxide mineral and was one of the first ores used to make copper metal. Malachite has been utilised as a gemstone and sculptural material in the past as its distinctive green color does not fade when exposed to light or after long periods of time. Malachite is formed at shallow depths in the ground, in the oxidizing zone above copper deposits. The material has also been used as a pigment for painting throughout history. Malachite is considered a rare gemstone in that the original deposits for the stones have been depleted leaving behind very few sources. In addition, the use of Malachite as gemstones and sculptural materials remains just as popular today as they were throughout history. It is quite common to cut the stone into beads for jewellery. The fact that Malachite has such a rich colour and one that does not fade with time or when exposed to light makes it particularly rare. Although there is no indication available of the locality from which the specimen was sourced, it is likely that the specimen was collected either in South Australia in the vicinity of the Burra Burra mines or in Victoria as part of programs of geological surveying undertaken in the Nineteenth and Twentieth centuries. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A solid hand-sized copper carbonate hydroxide mineral with quartz pebbles in red conglomorate matrix presenting shades of cream, brown and green.Existing label: Malachite / (green) in / conglomerate / (white quartz / pebbles / in red matrix /geological specimen, geology, geology collection, burke museum, beechworth, geological, indigo shire, malachite, malachite specimen, australian mines, mines, geological survey, conglomorate, matrix

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

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

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

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

A granular metamorphic rock, marble is derived from limestone or dolomite and composed of calcite or dolomite interlocking grains. Heat and pressure from overlying sediments form it from limestone buried deep in Earth's crust. Graphite, pyrite, quartz, mica, and iron oxides can affect rock texture and colour. This specimen was found in Carrara, Italy. Carrara marble is the most common marble found in Italy, and it gets its name from the region where it is located. The marble was also called Luna marble and was used as a decorative element in buildings and sculptures. It has been quarried since Roman times in the Lunigiana, the northernmost tip of Tuscany, just outside the city of Carrara in the province of Massa and Carrara.Marble is one of the most popular and expensive rocks used in sculpture, architecture, interior decorations, statues, table tops, and novelties. It is available in various colors and textures depending on the chemical composition. The strength of the rock and its ability to hold finer details have made it a favorite among designers. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A solid hand sized Marble (metamorphic rock) predominantly white with specks light grey and ochre geological specimen, geology, geology collection, burke museum, beechworth, marble, carrara marble, italian marble, marble specimen, tuscany

Bituminous coal is the most common type of coal, abundantly found in ancient coal deposits which can be dated back millions of years. Often referred to as soft or black coal, this specimen exhibits a high carbon content, ranging from 76-86%. It also holds a relatively high energy density (27 MJ/kg) meaning that it releases significant amounts of energy when burned. Bituminous coal is most commonly used for electricity generation, as well as in the production of steel. This particular piece of coal was collected as part of the Geological Survey of Victoria in the nineteenth century. It originates from Cape Paterson, a seaside village located in South Gippsland, Victoria (located on Bunurong Country). The discovery of bituminous coal in this locality was first made in 1826 by explorer William Hovell. More discoveries were gradually made over the following decades and in 1859 the Victorian Coal Company commenced the first active coal mining operations in the state by sinking a number of shafts and bores near the area of Cape Paterson. Evidence of this coal-focused past can be found today at the State Coal Mine Museum in the nearby town of Wonthaggi. This specimen is significant as it was collected from the locality of Cape Paterson in Victoria, an area that has since become historically instrumental in the mining of coal and other substances in the state of Victoria. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study. A solid hand-sized piece of bituminous coal with a shiny black-grey surface and jagged edges.Existing Label: BITUMINOUS COAL / Locality: Cape / Patterson, VIC. burke museum, beechworth, geological, geological specimen, state coal mine museum, wonthaggi coal mine, victorian coal company, bituminous coal, coal victoria, coal energy generation, william hovell, cape paterson, coal specimen

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

Laterite refers to both a rock and a soil type that is rich in clay, as well as Iron and Aluminium. It is created during a process that is called laterization, where high heat and seasonal heavy rainfall cause there to be wet and dry periods, which over time hardens the soil into rock. Because of this, most laterite is formed between tropics of Cancer and Capricorn. The iron oxide in laterite is what gives it it’s orange-red colouring. The largest religious complex in the world, Angkor Wat in Cambodia, is partially constructed of laterite, particularly its foundations, as laterite is porous and allows rainwater to drain. This specimen of laterite was collected from the Democratic Republic of Congo while it was colonised by Belgium in the 19th century. Laterite forms in many parts of the world, particularly between the tropics. It is used both for ore and as a building material, and comparing specimens from different parts of the world allows us to document the different compositions that this mineral can have when formed at different locations. 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 iron-aluminium oxide mineral specimen in shades of brown, orange and greyburke museum, beechworth, geological, geological specimen, laterite, laterite specimen, geology

Montmorillonite is a type of clay composed of aluminium silicate that forms very small particles that are not well-bonded to one another. This is why it is so soft. When in the presence of water, all types of clay swell. Montmorillonite swells even more than most types of clay, which is why it is often chosen over other types of clay in its practical uses. Montmorillonite has many different practical uses, including in the mining industry, as a soil additive, as a sealant, as a desiccant to draw water out of the air, to clean ponds, to make kitty litter and in cosmetics. Montmorillonite is a common mineral and, despite being named after Montmorillon, France, can be found all over the world, including many deposits in Australia. It is not known where this particular specimen originates from. Montmorillonite is an economically and socially significant material with a wide variety of uses. Having samples of common and important minerals allows collections, like the Burke Museum, to have a more complete view of the land on which they are located, and therefore a more complete view of heritage. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A solid tennis-ball sized chunk of aluminium silicate clay. It is primarily white, accented with orange and brown.burke museum, beechworth, geological, geological specimen, clay, montmorillonite

This specimen is Cassiterite in Quartz. Cassiterite is a tin oxide metal that forms in thin crystals which can have a beautiful lustre. Quartz is made of silicon dioxide, also known as silica, and is one of the most common minerals on earth. Cassiterite has been a fundamental source of tin ore for humans throughout history, including today. Tin is an important metal that has a wide variety of human uses in different areas, from dying fabric, to making mirrors, and their most well-known use ‘tin’ cans. Tin cans are primarily made of steel and are coated with tin in order to take advantage of tin’s property of being non-corroding. This is a massive step in the history of food preservation. Tinned food first reached Australia in 1815 with early settlers, and it began to be manufactured here in the 1840s. It was incredibly popular, and was a highly exported product, which would be a contributing factor to the ‘tin mining boom’ of the early 1880s. This specimen was collected at Jingellic, New South Wales, in about 1852. Although the Goldfields of the 1800s are much more well-known, tin mines existed alongside the gold mines which began in the mid 19th century and extended almost one hundred years, to the mid 20th century. Specimens like this would have been used as evidence to justify tin mining operations in the region as an investment. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study. The Geological Survey of Victoria was headed by British geologist, Alfred Richard Cecil Selwyn (1824-1902), who was responsible for issuing over 60 geological maps during his 17 years as director. These maps were all hand-drawn and coloured and became the benchmark for accuracy for geological mapping. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study. A fist-sized solid geological specimen made on one half of tin oxide, which is dark grey, and on the other side of silica, which is brown and cream.burke museum, beechworth, geological, geological specimen

There are 17 opal fields in Australia. This opal bearing stone was found in Lightning Ridge, NSW over what is known as the Great Australian Basin. This basin was formed and covers an area of 1.7 million square kilometers in eastern Australia in the Cretaceous period. This basin used to contain an inland sea, which provided an environment where silcrete eventually formed when water levels changed. This eventually seeped into other structures, and eventually hardened and formed opal. Lightning Ridge has a population of around 2000 people, with about 80 000 visitors every year. It is a historic mining town, and is known for its deposits of a rare black opal. Mining started in the area in the late 1800s, early 1900s when the black opal was discovered. This opal-bearing stone is of social and historical significance. It is from Lightning Ridge, which is well-known for being a large producer of opal stones, most famously black opal. The history of the period dates back to 140 million years, with the discovery of black opal in the early 1900s causing interest in the area. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.***A palm-sized solid mineral specimen in shades of beige and light orange*** silica based? burke museum, beechworth, geological, geological specimen, opal, opal fields, australia, lightning ridge, new south wales, great australian basin, cretaceous, silcrete, black opal, mining

It is made up of andalusite. Andalusite is a rock-forming mineral, sometimes found in granite or schist. It is often used to make glass, ceramic products, chemicals, and heat-resistant bricks as it can withstand high temperatures without changing. The chiastolite contains particles of graphite, which arranges in geometric patterns. When crystal growth occurs in the rock, the granite particles concentrate at crystal interfaces and can result in cross shapes. These ‘cross stones’ have been valued and used for their spiritual or religious meaning and used as charms, gems, or amulets. Chiastolite was first discovered in 1754, seen in a description in a published book by a palaeontologist, Franciscan priest, and Spanish author, Jose Torrubia. Deposits have been found in Australia, France, the USA, Chile, Canada, Spain, Brazil, Sri Lanka, and Russia. Deposits have been found in Western Australia and South Australia. This particular specimen was found in Bimbowrie, South Australia. Other chiastolite specimens have been found in Bimbowrie, along with jasper, quartz, and aventurine in the form of rolled pebbles or schist. This chiastolite specimen is socially and historically significant. It is a very rare sort of andalusite mineral. It is from one of only two locations where it is regularly found in Australia. The carbon cross has made it an important religious symbol in the past. Its ability to withstand high temperatures has made it a common ingredient in heat-resistant bricks and ceramics today. 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 metamorphic mineral consisting of andalusite, with a cross shaped graphite pattern in colours of grey, brown and yellowburke museum, beechworth, geological, geological specimen, andalusite, chiastolite, geometric, cross stone, spiritual, religious, australia, south australia, bimbowrie, quartz, jasper, aventurine, schist

This specimen was donated in 1868 by Alfred Selwyn. Olivine is typically found in basic and ultra-basic igneous rocks around the world, in a variety of colours including yellowish green, olive green, greenish black and reddish brown with a transparent to translucent diaphaneity. The luster of the specimen is vitreous, the luminescence non-fluorescent and when fractured the mineral is very brittle producing small, conchoidal fragments. Chromian diopside is normally found in small sizes as the larger the size of the mineral the darker the colour is, almost black rather than green. Chromium is the element that gives chromian diopside and emeralds their rich green colour. Diopside is found across the world in multiple colours however gem-quality chromian diopside is mined in Siberia, Russia and prominent within the jewellery industry as a more affordable substitute to emeralds. Chromium-bearing diopside has been located across Australia. Chromium-bearing Diopside is located across the world found in North America, parts of South America, and across Australia, Africa, Europe and Asia. Chromium-bearing Diopside is mined in Siberia, Russia and is sold as a commercial substitute for emeralds. The stone is often turned into jewellery. This item is one of many geological and mineral specimens that constitute a broader collection obtained from various regions across Australia (as well as some international locales) and generously contributed to the Burke Museum between 1868 and 1880. A significant portion of these specimens originated from Victoria and were acquired as a result of the Geological Survey of Victoria, initiated in 1852 during the Gold Rush era. The primary objective of this survey was to investigate and chart the geological characteristics of Victoria. The procurement of geological specimens played a vital role in advancing our comprehension of the Earth's scientific composition and was instrumental in supporting research and educational institutions throughout Australia, including the Burke Museum, in their efforts to foster further exploration and study. A solid mineral specimen in shades of green, grey and brownburke museum, beechworth, geological, geological specimen

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 object is a photographic postcard showing some of the above-ground structures of the Golden Bar mine in Chiltern, including a building with a smokestack and the poppet head which is used to haul equipment, materials, and men above or below ground. The Golden Bar site, mined by the Golden Bar Mining Company which was formed in 1901, managed to yield approximately 12,453 oz of gold before work stopped in 1912 - it was one of the principal mines in the area, as well as the deepest and one of the richest. The text on the postcard was handwritten by H.Gordon (?) to Issy (?), to show the mine where he presumably worked as he promises to take them 'above and below'. The postcard can be approximately dated to between 1901-1912. It is stated that after 1902 Kodak added the line on the postcard backs to divide into correspondence and address sections as seen on the reverse of this object. In addition, there is also a similar Kodak photographic postcard in the Burke Museum collection that is dated to 1908 and has the same specific font type and manufacturer markings (see references for link). Lastly, the Golden Bar mine ceased operations in 1912 so the photograph was likely taken prior to this. This photographic postcard is a rare and fair conditioned representation of one of the most significant gold mines in the Chiltern area, showing the above ground structures at the time it was being actively mined. This postcard also holds social significance as a snapshot of working life in the gold mining rush of Victoria, and a personal record of one of its miners. A sepia rectangular postcard printed on card.Obverse: Dudley Studio / Golden Bar. Chiltern Reverse: BMM 8034 / Post Card. / Correspondence. / Address Only. / Kodak. Austral. 110 / My Dear Issy (?), / A card only, to show (?) the mine / and when you come down I will / take you above and below, / All (...) love, me to. Has the baby / gone home yet Heini (?) wants to know / give my love to Syd when next you write / Your loving (...), H. Gordon (?)photographic postcard, postcard, chiltern, golden bar mine, golden bar mining company, dudley studio, kodak

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

This photograph depicts a reef mine in Beechworth. Reef mining, or quartz reef mining, was common in 19th Century Victoria. This gold mining technique requires mine shafts to be sunk into underground quartz reefs, with horizontal tunnels dug from the original shaft at differing levels to find the gold-bearing rock. The quartz would then be hoisted to the surface, which would then be pounded to access the gold in its metallic state. Gold was discovered in Beechworth in February 1852, at Spring Creek. Within 11 months of that discovery, over 8000 hopeful prospectors quickly descended on this region, transforming it into a thriving, wealthy township. Reef mining and hydraulic sluicing were gold mining techniques used in this region in the 19th and early 20th centuries. This photograph interestingly contains dogs alongside the miners. While dogs have been recorded as deterrents to thieves in the Victorian goldfields, these dogs appear as companions to these men.The search for gold is ingrained into the history of Victoria and therefore, images like this one can reveal important information for society and technology for the date when the photograph was taken. It also shows a location where reef mining was undertaken which provides insight into the impact on the environment at a time when it was done. Although quartz is one of the most common minerals found in the earth's crust, it does not always contain gold. Those reefs that do are rare and highly sought after by prospectors. The Beechworth Burke Museum has additional images relating to gold mining which can be analysed and studied alongside images like this one.Sepia coloured rectangular photograph printed on gloss photographic paper. Obverse: Reverse: United Shire of Beechworth/ Shire Secretary/ Reef Mining, Beechworth./ 6167.abeechworth, burke museum, gold, gold mining, gold rush, victorian gold rush, reef mining, quartz, companion dog, horse and cart

This reproduced photograph depicts a reef mine in Beechworth. Reef mining, or quartz reef mining, was common in 19th Century Victoria. This gold mining technique requires mine shafts to be sunk into underground quartz reefs, with horizontal tunnels dug from the original shaft at differing levels to find the gold-bearing rock. The quartz would then be hoisted to the surface, which would then be pounded to access the gold in its metallic state. Gold was discovered in Beechworth in February 1852, at Spring Creek. 8000 hopeful prospectors quickly descended on this region within the year, transforming it into a thriving, wealthy township. Reef mining and hydraulic sluicing were gold mining techniques used in this region in the 19th and early 20th centuries. This reproduction photograph interestingly contains dogs alongside the miners. While dogs have been recorded as deterrents to thieves in the Victorian goldfields, these dogs appear as companions to these men.The search for gold is ingrained into the history of Victoria and therefore, images like this one can reveal important information for society and technology for the date when the photograph was taken. It also shows a location where reef mining was undertaken which provides insight into the impact on the environment at a time when it was done. The Beechworth Burke Museum has additional images relating to gold mining which can be analysed and studied alongside images like this one.Black and white rectangular reproduction photograph on gloss photographic paper. Obverse: Reverse: L is miners 26%/ 10 x 8/ 6167.bbeechworth, burke museum, gold, gold mining, gold rush, victorian gold rush, reef mining, quartz, companion dog, horse and cart

Depicted are a group of men standing in front of a wooden structure. The men wear attire appropriate to the 1920s. This photos is of the shows miners at the Homeward Bound Mine in Hillsborough. The Homeward Bound reef was discovered in 1865 and was worked continuously until 1880. This image is significant as it shows how Victorians worked during the gold rush era. A black and white rectangular photograph depicting 21 separate men, either standing or sitting around a wooden structure. Each man wears the typical attire for gold mining in the 1900s. A horse appears behind a man on the right side of the photograph.The background shows a wooden structure of a mine and the Australian gumtree 7855 /mining, group photo, burke museum, beechworth, photograph, hillsborough, mine, homeward bound mine

A black and white photograph depicting seven men and four women surrounded by tunnel boring machinery. A tunnel boring machine (TBM), also known as a "mole", is a machine used to excavate tunnels with a circular cross section through a variety of soil and rock strata. They may also be used for microtunneling. They can be designed to bore through anything from hard rock to sand. Tunnel boring machines are used as an alternative to drilling and blasting (D&B) methods in rock and conventional "hand mining" in soil. TBMs have the advantages of limiting the disturbance to the surrounding ground and producing a smooth tunnel wall. This significantly reduces the cost of lining the tunnel, and makes them suitable to use in heavily urbanised areas. The major disadvantage is the upfront cost. TBMs are expensive to construct, and can be difficult to transport. The longer the tunnel, the less the relative cost of tunnel boring machines versus drill and blast methods. This is because tunneling with TBMs is much more efficient and results in shortened completion times, assuming they operate successfully. Drilling and blasting however remains the preferred method when working through heavily fractured and sheared rock layers.This photograph is significant as it shows the machinery used and attire worn by men and women during the gold rush era. Black and white rectangular photograph printed on photographic paperburke museum, mining, beechworth, boring machinery, excavate, gold, gold fields, gold rush, miners

This image taken between 1920-1930 depicts open-cut hydraulic sluicing at the Three Mile Mine, located about five kilometres south of Beechworth. Alluvial, or surface, mining began on this site in the 1850s, but was soon replaced by hydraulic sluicing methods. By the start of 1880 it is estimated that nine hundred miles of water races had been cut though soil and rock in the Beechworth district. 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. Large water quantities were required for hydraulic sluicing, and the long water races and deep tailraces that were constructed were considered great engineering feats. This method of mining is extremely effective, but causes significant environmental damage and impacts to waterways and agricultural operations. Miners at Beechworth built extensive networks of races and dams to secure reliable supplies of water on a scale far greater than elsewhere in Victoria. By the 1880s Beechworth's water barons continued to hold more than half of all the water right licences on issue and undertook sluicing operations on a massive scale. The manipulation of surface and ground water via race networks was well planned and recorded in detail by local mining surveyors. The maps that were created, combined with modern geo-spatial technologies, provide a vital key in understanding the great lengths to which miners went to capture and control critical water resources. Today, Three Mile mine is called Baarmutha. The Three Mile Mine was unproductive until 1865 when John Pund and three other miners secured a fifteen year license and constructed a water race from Upper Nine Mile Creek to Three Mile Creek. In the early twentieth century Pund & Co. averaged over one thousand ounces of gold per year from the mine. After Pund's death in 1915, GSG Amalgamated Co operated the site, continuing sluicing until 1950. This image of hydraulic sluicing methods shows the extent of water-works engineering in the landscape. This photograph has historic and research potential for understanding changes to the landscape, the evolution of mining methods, and the extensive construction, manipulation and management of water networks in the Beechworth district. Black and white rectangular photograph on matte paperReverse: 7597-1 / Sluice Mining / Copied from original on loan from Webb (Qld) / Donated Nov 2009 / Baarmutha Three Mile Mine c1920-1950 / Managed by the Plain Bros then Parkinsons / Current Location is: Beechworth Animal Shelter / used for Baarmuthaburke museum, beechworth museum, beechworth, gold fields, gold rush, victorian gold rush, hydraulic sluicing, spring creek, netwown falls, mining tunnels, water races, tailraces, gold ming history, colonial australia, australian gold rushes, mining technology, beechworth historic district, indigo gold trail, indigo shire, john pund, water manipulation, water engineering, three mile creek, three mile mine, water race, large-scale mining methods, historical mining construction, alluvial mining, mining environmental impacts, baarmutha, water barons

This photo shows the large mining cavity with a hydraulic sluicing machine in operation at Baarmutha Three Mile Mine, Beechworth . The Beechworth Mining District was one of six mining districts established by the Governor-in-Council on 4 January 1858 under the provisions of An Act for Amending the Laws Relating to the Goldfields (21 Vic no.32). The District was further divided into seven divisions: Spring Creek, Snake Valley, Three Mile Creek, Buckland, Woolshed, Yackandandah and Omeo. The boundaries of each of these divisions and of the whole district are described in the Governor-in-Council's proclamation printed in the Government Gazette, 5 January 1858, pages 3-5. Hydraulic mining is a form of mining that uses high-pressure jets of water to dislodge rock material or move sediment. In the placer mining of gold or tin, the resulting water-sediment slurry is directed through sluice boxes to remove the gold. It is also used in mining kaolin and coal.This photograph shows the impact the gold rush era had on Australia and the earth.A black and white rectangular photograph printed on photographic paperCopied from original on loan film (WEBB QLD) / Donated 2009 NOV/ Baarmutha Three Mile Mine c1920-1950/ Managed by John Weir Peter Jereen Jack Cox / Owned by Plain Bros then Parkinsons Sluicing.mining, gold fields, beechworth, gold rush, burke museum, photograph, mining cavity, hydraulic mining, hydraulic sluicing, baarmutha

The photograph printed on this postcard comes from the collection of the Mitchell Library in Sydney. It is sepia in tone and depicts seven men standing and sitting around a mine shaft in the Beechworth region. The photograph has been dated to approximately 1872. This period in history post-dates the Victorian gold rushes which occurred 1852-1853 in Ballarat, Bendigo and Beechworth. During this period, in the 1870s, the surface alluvial gold had been discovered and removed from location. Therefore, in order to reach the deeper and less accessible alluvial gold, diggers began to dig shafts into the earth. These shafts sunk below the ground level by 20 to 30 feet and required timber structures around the entrance and winches to bring the paydirt to the top. The top of this wooden structure is visible behind the man standing in the upper right of the image. This type of mining was highly dangerous as mines often caved in which injured the minors and often resulted in death. Thus, following this period, in the early 1900s, miners opted instead for hydrolic slucing which cut away the earth without the devastating consequences of a mine cave in. This particular group of miners appear to have been unable to afford a horse (then worth around 50 pounds) which were generally used at mines like this to help pull buckets attached to ropes up and down the mine. Instead, this group brought the buckets up and down by windlass. The windlass was a wooden structure mounted over the mining shaft and fitted with a hand-cranked winch which enabled the bucket attached to the rope to be brought up and down.Gold was first discovered in Beechworth in Spring and Reid's Creek in the summer of 1852-1853. At its popularity, this region had approximately 8000 people on the gold fields searching for gold on the banks of these creeks. These periods did not require the use of heavy machinery or the digging of deep mining shafts like the one depicted in this image. Therefore, this image has important connotations for the technologies associated with mining during the approximated 1870s when gold was harder to access. This is a later period in gold history which does not fit into the "gold rush" period. Instead, it occurred after the surface gold had disappeared and therefore, is essential for researchers who are investigating the mining techniques and structures used to reach the alluvial gold which was located deeper under ground in the 1870s. This period predates the use of big heavy machinery used to mine in the 1900s which include dredges. Images such as this one can also impart essential information as to the wardrobe and fashion of men during this period. It also imparts knowledge about the landscape of Beechworth which is useful for people researching the environment and impact of gold mining in the north-east region of Victoria. In addition, since this image is a postcard reproduction of an early Australian image which may date to approximately 1990 it can impart knowledge as to the interests of people during this time period when there may have been an increase into Australian history.A sepia tone facsimile of an early Australian photograph (circa 1872) printed as a postcard.Obverse: BEECHWORTH / Victoria, Australia / Reverse: GM 2 3275 / CORRESPONDENCE / AUSTRALIAN / YESTERYEAR / CARDS / ADDRESS / Published by George Symons (057) 65 3240 / THE MINEHEAD C. 1872 / The easily gleaned gold of the early fields did / not last very long. In order to reach less / accessible alluvial gold diggers began sinking shafts as much as twenty to thirty feet down / and the mines required timbering and winches / to bring the paydirt to the top. / This syndicate has been unable to afford the / luxury of a horse (about 50 pounds) and so everything / must go up and down by windlass and rawhide / bucket. / Photo: Mitchell Library, Sydney / A sepia tone facsimile of / an early Australian photographmining album, gold mine, beechworth, burke museum, mine shaft, postcard, australian yesteryear cards, george symons, the minehead, gold fields, alluvial gold, early australia, c.1872, 1872, gold diggers, north east victoria

This photograph depicts Cock's Pioneer G & T Sluicing site No. 4 in El Dorado. Looking eastwards, the photo captures a wooden and tin building with various mining equipment strewn in the foreground. Underneath the verandah, figures can be seen. These are believed to be a Mr. Hollister (left), Mrs. Breustedt (4th from left), children Min and Chris Breustedt, and Kate Timmons holding a girl's hand. 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. The Cocks Pioneer was an extremely successful mining company during the 20th century. In the Annual Report of the Secretary for Mines for the year 1915, the Cocks Pioneer was the largest producer of gold and tin collecting 5,535 ozs. of gold and £7,500 of tin. Twenty years later in 1935, Cocks Pioneer was still one of the most profitable mines in Victoria, ranking as the second-highest dividend paying mine. The company produced a total of 3,650 kg of gold. 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 northeast. John Cock was the son of a Cornish miner 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 in 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.A black and white copy of a sepia coloured rectangular photograph printed on matte photographic paper mounted on boardObverse: COCKS PIONEER G + T SL CO, N.L. / 1910 - 11 / NO 4 SITE LOOKING EAST / 4 Reverse: 1997.2508 / AUG 29 1909cocks pioneer gold and tin sluicing company, el dorado, mining, sluicing, hydraulic mining, hollister, breustedt, timmons, gold, tin, gold rush, victoria

This photograph was captured sometime between an estimated 1940s-1950s. It depicts the Beechworth Benevolent Asylum (later the Ovens and Murray Hospital for the Aged) which was built in 1862. It is located on an elevated site in Beechworth, Victoria because it was believed the height was beneficial to the health of the patients at the Benevolent. Later wings were added to the original building between 1867 and 1890. The building was constructed in an unusual Flemish Gothic Revival style which contrasts with the classical style of the Mayday Hills Hospital in close proximity to the Benevolent. The Hospital was designed in Italianate Revival architecture. The appearance of buildings like the Mayday Hills Hospital and the Ovens Benevolent Asylum are representative of the importance of Beechworth as a town shortly after the goldrush. During the 1850s and 1860s, administration buildings were erected alongside churches, shops and structures of justice. This marks a movement away from the "chaotic" structure of life on the goldfields and towards a more civilised and cultural lifestyle. This social phenomenon is also witnessed in Melbourne with the creation of buildings like the State Library and the University of Melbourne. The Beechworth Benevolent Asylum was renamed the Ovens Benevolent Home in 1935. The Asylum had been set up to provide accommodation and care for permanently injured gold miners, and for women and children who were penniless, homeless, or whose parents were guests of the state. In 1954 it was renamed as The Ovens and Murray Home (as pictured in this photograph). The purpose of this building was to provide a refuge for the poor and destitute, homeless older men, deserted women and children along with providing care for the mentally ill. These buildings were built at the government's expense and are of great historical and architectural significance.This photograph depicts the Ovens and Murray Home (previously the Ovens Benevolent Home) during the 1940s or 1950s. Since this building is of great historic and architectural significance, photographs like this are especially valuable in reconstructing the use history and any changes/additions to the building over a period of time. This building is important for what it can reveal about society in Beechworth and also architectural styles. This building is made in the Flemish Gothic Revival style which is quite unusual for the 1860s. It is important as an early example of a building constructed for a specific purpose, in the case of this particular building: caring for the aged/destitute. This building is important for research into the civic development of Beechworth as an early Gold Rush town located in Victoria's North-East. During this period, Beechworth was developing as the main center of administration in this region which made it a very influential and quickly developed town. Photographs like this one which depict a building during one period in history can reveal important information for the use and alterations of a building and for preferences in architectural style. It can also be studied for what it reveals about society in Beechworth and compared and contrasted to similar institutions across Australia and with additional photographs in the Burke Museum collection.Black and white rectangular photograph printed on gloss photographic paperObverse: OVENS & MURRAY HOME / Reverse: KODAK PAPER / 727 / J. Collins BMM 8689.1 /mayday hills, beechworth benevolent asylum, ovens benevolent home, asylum, refuge, poor and destitute, goldrush, flemish gothic revival, architecture

This photograph was captured sometime between an estimated 1940s-1950s. It depicts the Beechworth Benevolent Asylum (later the Ovens and Murray Hospital for the Aged) which was built in 1862. It is located on an elevated site in Beechworth, Victoria because it was believed the height was beneficial to the health of the patients at the Benevolent. Later wings were added to the original building between 1867 and 1890. The building was constructed in an unusual Flemish Gothic Revival style which contrasts with the classical style of the Mayday Hills Hospital in close proximity to the Benevolent. The Hospital was designed in Italianate Revival architecture. The appearance of buildings like the Mayday Hills Hospital and the Ovens Benevolent Asylum are representative of the importance of Beechworth as a town shortly after the goldrush. During the 1850s and 1860s, administration buildings were erected alongside churches, shops and structures of justice. This marks a movement away from the "chaotic" structure of life on the goldfields and towards a more civilised and cultural lifestyle. This social phenomenon is also witnessed in Melbourne with the creation of buildings like the State Library and the University of Melbourne. The Beechworth Benevolent Asylum was renamed the Ovens Benevolent Home in 1935. The Asylum had been set up to provide accommodation and care for permanently injured gold miners, and for women and children who were penniless, homeless, or whose parents were guests of the state. In 1954 it was renamed as The Ovens and Murray Home (as pictured in this photograph). The purpose of this building was to provide a refuge for the poor and destitute, homeless older men, deserted women and children along with providing care for the mentally ill. These buildings were built at the government's expense and are of great historical and architectural significance.This photograph depicts the Ovens and Murray Home (previously the Ovens Benevolent Home) during the 1940s or 1950s. Since this building is of great historic and architectural significance, photographs like this are especially valuable in reconstructing the use history and any changes/additions to the building over a period of time. This building is important for what it can reveal about society in Beechworth and also architectural styles. This building is made in the Flemish Gothic Revival style which is quite unusual for the 1860s. It is important as an early example of a building constructed for a specific purpose, in the case of this particular building: caring for the aged/destitute. This building is important for research into the civic development of Beechworth as an early Gold Rush town located in Victoria's North-East. During this period, Beechworth was developing as the main center of administration in this region which made it a very influential and quickly developed town. Photographs like this one which depict a building during one period in history can reveal important information for the use and alterations of a building and for preferences in architectural style. It can also be studied for what it reveals about society in Beechworth and compared and contrasted to similar institutions across Australia and with additional photographs in the Burke Museum collection.Black and white rectangular photograph printed on gloss photographic paperBack of photograph. Handwriting: "For John Beckingsale"mayday hills, beechworth benevolent asylum, ovens benevolent home, destitute, gold town, beechworth, victoria, north-east vic