This specimen originated from Mount Lyell on the west coast of Tasmania, where a large group of open cut and underground copper-silver-gold mines began operating in 1883. Between 1893-1994, the Mt Lyell Mining and Railway Company were responsible for operations. The Mt Lyell copper-gold mines produce some excellent crystallised specimens of chalcopyrite and other minerals. The deposits are generally considered to be of Cambrian volcanic origin, but there are indications of Devonian granitic influence on the ores, plus local remobilisation during Devonian deformation. Over 120 million tonnes of ore was produced from several workings, including the main Prince Lyell mine and the North Lyell mine, which was also of great importance. The Mount Lyell mines have a long history of human and environmental disasters, including the 1912 North Lyell fire that killed 42 miners, and two separate incidents in 2013 in which three people lost their lives. The environmental impacts from this complex of mines are extensive, with waste tailings and heavy metal contamination flowing directly into the King and Queen River catchments. In 1954, the eminent Australian historian, Geoffrey Blainey, published 'The Peaks of Lyell' which delves into the history of the 1912 North Mount Lyell Disaster.Chalcopyrite does not contain the most copper in its structure relative to other minerals, but it is the most important copper ore since it can be found in many localities and occurs in a variety of ore types. The brassy-yellow colours in Chalcopyrite mean it is often confused with pyrites and gold, leading to use of the term, "fool's gold." Chalcopyrite has been the primary ore of copper since smelting began five thousand years ago. 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.This hand sized solid mineral specimen has shades of brass-yellow with spots of iridescent green-black tarnish. Chalcopyrite is a copper iron sulphide mineral and a major ore of copper common in sulphide veins and disseminated in igneous rocks. Chalcopyrite has a hardness of 3.5-4 on the Mohs Scale. It is a member of the tetragonal crystal system and has metallic lustre and opaque transparency.burke museum, beechworth, indigo shire, beechworth museum, geology, geological specimen, chalcopyrite, copper pyrites, copper mining, tasmanian geology, mount lyell, mount lyell mines, fools gold, mohs scale, crystals, minerals, historical geological collection, victorian geological survey, a.r.c selwyn, gold rush, van diemans land

This specimen is from Barefoot Hills, Victoria. Sandstones are economically important as major reservoirs for both petroleum and water, as building materials, and as valuable sources of metallic ores. Most significantly, they are the single most useful sedimentary rock type for deciphering Earth history. 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 sedimentary rock composed mostly of quartz sand. Sandstone is the second most common sedimentary rock after shale. Sandstones consist of sand-sized grains principally quartz, feldspar and rock fragments. The two major classes of sandstone are arenite and wacke. the colour of sandstone varies from grey, yellow, red and white reflecting the variation in mineral content and cement and is gritty to touch (like sandpaper).Geological survey / R.... S 61 / Loc Bareboot Hills / Sheet / 24SE / 94 /burke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, mineralogy, sandstone, yellow sandstone, victoria, barefoot hills

This specimen was recovered from Philip Island in Victoria. Chalcedony is composed of Quartz and Silicon Dioxide represented as SIO2. It has and is still used as a gemstone for thousands of years. This is an excellent specimen Chalcedony that shows its aesthetic properties. 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. Uniquely shaped piece of Chalcedony with opening in the centerburke museum, beechworth, geological, geological specimen

Gold usually is found as a native metal, but it also forms minerals with tellurium, sulphur, or selenium. The gold-bearing minerals that contain tellurium are called tellurides. Kalgoorlie, Western Australia contains greater than 1500 tonnes of gold.Seventy to seventy-five percent of the deposit occurs as native gold, but a further twenty percent appears as tellurides. What remains is in the form of 'invisible' gold. Extracting gold from telluride minerals, such as calaverite, which contains around forty-two percent gold, has produced approximately three hundred tonnes of gold. Prior to 1896, rocks containing tellurides were not recognised as rich gold ores, and were discarded.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 silvery to pyrite-yellow striated mineral containing tellurium and goldburke museum, beechworth, beechworth museum, geological, geological specimen, mineralogy, telluride, tellurite, gold-bearing, kalgoorlie, tellurium

This specimen is from Broken Hill, NSW. Galena is a natural mineral form of lead sulphide and is often found associated with sphalerite, calcite, and fluorite. Galena is an important lead ore mineral, and, in some regions, it is also an important mineral associated with silver ore. Sphalerite is a sulphide mineral that is the main ore of zinc. Rhodonite is an uncommon mineral once used as an ore of manganese in India, however today the scarcity and fragility of the crystals mean it is primarily used as lapidary materials or mineral specimens. In 1883, Charles Rasp who was a boundary rider at the time, discovered what he thought were deposits of tin but were in fact samples of silver and lead. He and six others went on to set up the first mining company in Broken Hill (BHP). The ore body became the largest and richest of its kind in the world mining ore worth more than 42,000 pounds in its first year. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study. Galena contains lead and silver, Sphalerite contains 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 hand-sized piece of Sphalerite and Galena with Rhodonite crystalsburke museum, beechworth, geological, geological specimen, galena, rhodonite, sphalerite, silver ore, manganese, lead sulphide, lead ore, zinc ore, lapidary, mineral specimen, broken hill, nsw

This specimen was found in Cape Patterson, Vic. Cape Paterson is a cape and seaside village located near the town of Wonthaggi, 132 kilometres southeast of Melbourne, in the Bass Coast Shire of Gippsland, Victoria, Australia. These dark, fossiliferous Mudstones were deposited in slow-moving water associated with sedimentary basins & continental shelves. They are rich in carbon which makes them almost black. This is typical of an anoxic, reducing environment such as deep water or stagnant conditions where carbon-rich material would remain unoxidised during subsequent deposition & diagenesis. it has an imprint of a leaf in the rock itself, displaying the fossil of the plant. This specimen is unique due to the leaf impression within the stone itself. Imprint fossils are formed from an organism moving in some way, leaving behind a trace or track. These tracks are preserved when the clay/silt dries slowly and is covered by other sediment. Plants can also leave imprint fossils when they are covered by sediment. The leaf tissue degrades, leaving an imprint of where the leaf once was. 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.These dark, fossiliferous Mudstones were deposited in slow moving water associated with sedimentary basins & continental shelves. They are rich in carbon which makes them almost black. This is typical of an anoxic, reducing environment such as deep water or stagnant conditions where carbon rich material would remain unoxidised during subsequent deposition & diagenesis. FOSSILIFEROUS MUDSTONE / Locality: Cape Patterson, Victoria | Descriptive catalogue / Pg 27 No 95 / "Grey Clay, / Cape Paterson with leaf impressions' / 15/4/21 C. William /mudstone, cape patterson, leaf imprint, fossilised leaf, fossiliferous mudstone

This specimen was found in Harcourt, Victoria. Harcourt is a small historic gold rush town located in a valley at the foot of Mount Alexander (741 m) in the Central Highlands of Victoria. In recent times the goldrush origins of the town have been replaced by a district known for apples, cider and wine. The Traditional owners of Harcourt are The Dja Dja Wurrung people. Granodiorite is a coarse-grained intrusive igneous rock similar to granite, but containing more plagioclase feldspar than orthoclase feldspar. Granodiorite has greater than 20% quartz by volume, and between 65% and 90% of the feldspar is plagioclase. This piece is of significance due to its provenance in Harcourt, Vic. Granodiorite is commonly produced in volcanic arcs, and in mountain buildings where it emplaces as large batholiths in mountain roots. Granodiorite is the plutonic equivalent of dacite. 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.Granodiorite is a coarse-grained intrusive igneous rock similar to granite, but containing more plagioclase feldspar than orthoclase feldspar. According to the QAPF diagram, granodiorite has a greater than 20% quartz by volume, and between 65% and 90% of the feldspar is plagioclase.GRANDIORITE. / Locality: / Harcourt, Victoria / Other label: Geological survey / R S / Loc Harcourt quarries [?] Alexander / 1/4 Sheet. | 4 | Granite /granodiorite, granite, burke museum, harcourt, coarse-grained, igneous, plagioclase feldspar, orthoclase feldspar, quartz, mount alexander, the dja dja wurrung people, the traditional owners, central highlands of victoria, gold rush

This particular specimen was found in the Moorabool Slate quarries in Victoria. The Moorabool Slate quarries was established in the 1860’s by a company of Welshmen with a crew of six who purchased land by the riverside to mine for slate. Under the promise of adding to existing recourses the crew mined the slate which was used for paving and roofing. Slate is a fine-grained, low-grade metamorphic rock that is formed by the transformation of mudstone, shale or sometimes volcanic ash under low pressure and temperatures. It dark colour is due to carbonaceous material or to finely divided iron sulphide. It is believed that Evan Rowlands and Theophilus Williams of Ballarat were the first to discover the slate veins. Slate is a one of the most common natural stones in general use. Being used as paving, flooring, roofing and more. However, its history of being mined in Australia is not common as it is considered that the best places to mine slate is Spain and parts of the United Kingdom. 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 somewhat rectangular foliated metamorphic rock composed of quartz, sericite and minerals from the chlorite group that make up the compounds of slate. The rock is dark grey almost black.Geological survey / R S / Loc Moorabool /Slate quarries / 1/4 sheet | 78 | Roofing Slate /burke museum, beechworth, geological, slate, metamorphic, slate (metamorphic), geological specimen, slate specimen, indigo shire

This specimen was recovered from Sedgwick, VIC. Spotted slate is a fine-grained porphyroblastic metamorphic rock with a number of compounds including muscovite, quartz, graphite with cordierite poikiloblasts and more. The cordierite poikiloblasts are rounded crystals that size up to 2.5 mm. the growth of these crystals is in response to metamorphism of low to medium intensity. The town Sedgwick was named after British geologist Adam Sedgwick 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 rectangular hand-sized spotted slate specimen in a shade of light grey with darker flecks throughout Spotted Slate / Locality: Sedgwick Victoria | This is an early specimen / from the Quarter sheet / map. See sample 62 / page 18. Described as 'Spotted Slate' but these / days we would call it spotted hornfels / C. William 15/4/21 slate, spotted slate, victoria, beechworth, burke museum, geological specimen, mineralogy, sedgwick, sedgwick victoria, spotted slate specimen

This specimen was recovered from Ceres West of Geelong, Victoria. Greenstone is the name for any metamorphosed basic igneous rock (in the case of this specimen, Gabbro) that gains its greenish colour to the presence of the minerals chlorite, actinolite, or epidote, hence the term 'green' and 'stone'. Greenstone is often formed through metamorphsis along a convergent plate boundary. In the rock cycle (the series of processes that creates the various types of rocks) there are identified three different types of rocks, which are the sedimentary, the igneous and the metamorphic. Metamorphic rocks started out as sedimentary, igneous or earlier metamorphic rocks but changed from their original condition under the effect of high heat, high pressure or hot, mineral-rich fluid. However, if pressure or heat is too high, then the rock will melt, resulting in the formation of an igneous rock. The name used to describe these types of rocks reflects this specific inherent trait of change, since the word “metamorphic” derives from the Greek word “metamorphosis”, meaning “change of form or structure”. Metamorphic rocks form in the Earth`s crust but can be also found on the surface, due to elevation of the Earth`s surface. They are divided into two categories: the foliated metamorphic and the non-foliated metamorphic rocks. Gabbro is a highly useful mineral that is often polished to create cemetery markers and kitchen benches. It is notable for its qualities of durability, being able to withstand extreme elements and wear. Whilst not rare, Gabbro is of great utility and has been highly desirable for its qualities. 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.Greenstone is a solid hand-sized metamorphic mineral of a green colour. Greenstone is the name for any metamorphosed basic igneous rock (in the case of this specimen, Gabbro) that gains its greenish colour to the presence of the minerals chlorite, actinolite, or epidote, hence the term 'green' and 'stone'. Gabbro is a medium to coarse grained rocks that consist primarily of plagioclase feldspar and pyroxene. Greenstone is often formed through metamorphsis along a convergent plate boundary. Gabbro forms due to cooling and crystallization of magma underneath Earth's surface. Greenstone/Gabbro/from Ceres west/of Geelong. Has old Geological Survey label/and probably collected by/Richard Daintree in 1861/C.Willam 15/4/21/ Other label: 62 /greenstone, metamorphosed, igneous rock, gabbro, chlorite, actinolite, epidote, metamorphsis, rock cycle, various types of rocks, sedimentary, high heat, high pressure, mineral-rich fluid, metamorphosis, foliated metamorphic, non-foliated metamorphic, convergent plate boundary, greenish colour, minerals

This specimen was recovered from Moonambel, Donkey Hill, Victoria. Established in the early 1860's, Moonambel is a small town in the Pyrenees region of the Australian state of Victoria. In the 1850s the location of Moonambel was part of the ‘Mountain Creek’ pastoral run, but in 1860 reports began to appear of a gold-rush at McKinnon’s ‘Mountain Creek’ station. By 1861, a township had developed on the diggings site, and on 21 October 1861 the “municipal district of Moonambel, on Mountain Creek” was proclaimed. The name 'Moonambel' is believed to be an aboriginal word meaning 'hollow in the hills'. Slate is a stone with a fine grain that is noted for its persistent strength and ability to naturally split into slabs. It forms under low temperatures and is most often created from clay. Pyrite is a crystallising compound that occurs naturally in grey and blue-black slate that is colloquially referred to as slate-rust as it resembles regular rust. 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.Pyrite is iron sulphide (also known as “fool's gold”) which is commonly found in slates.Existing label: 53 /moonambel, slate, pyrite, burke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, mineralogy, victoria

This specimen was recovered from Adelong, NSW. The initial discovery of gold at Adelong by a Mr Williams took place in 1857. Much of the area is underlain by granitic rocks, while at Adelong itself a prominent norite intrusive body occurs. To the west of Adelong is a belt of intermediate to mafic igneous rocks and sediments which extends from Batlow in the south to at least as far north as the Snowy Mountains Highway. Around 26 tonnes of gold was found at the Adelong goldfield from its discovery in the 1850s until the last miners left in the 1940s. Pyrite has the formula of FeS2 and forms as an isometric (cube) form. It is a common occurring material and is often mistaken for gold, now colloquially known as ‘fool’s gold’. Pyrite that has strongly crystallised is considered stable, but the mineral has the potential to oxidise and decay. 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.Pyrite is iron sulphide (also known as “fool's gold”) which is commonly found in slates.Existing Label: 104 /burke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, mineralogy, pyrite, adelong

‘Ropy lava’ is known for its sculptural and layered qualities. It occurs in specific lava flows that are slow moving and slow cooling, allowing for unique formations to be created out of the motion. Ropy Lava is a flow that has a hardened crust with molten material underneath, the tension between these states is what creates its characteristic form. The brown/red hue of the stone is an indication of age, as it is oxidised iron deposits. This rock deposit is thought to be sourced from the area by Talbot, in western Victoria. This area has a rich mineral history and experienced the gold rush in the 1850's. The traditional owners of this area are the Dja Dja Wurrung people.This geological specimen shows the conditions in which the Australian landscape was created as well as provides an indication as to how these events occurred. It is representative of a common natural process that contextualises the formation of Australia with the formation of other landmasses. 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 specimen in brown/red hues42 / victoria, talbot, lava, ropy, ropy lava, mineral, geological specimen, geological, geological heritage, natural stone, natural history

This particular geological specimen was found in Mount Franklin or Lalgambook in Djadjawurrung, located between Daylesford and Newstead, approximately ninety minutes drive from Melbourne. The mountain is an example of a breached scoria cone (a steep conical hill of loose pyroclastic fragments) which was created by a volcanic eruption about 470,000 years ago, a date which may indicate the age of this geological specimen. The volcanic eruptions of Mount Franklin were most likely witnessed by members of the Dja Dja Wurrung Aboriginal tribe, who referred to this country as the 'smoking grounds'. Mount Franklin and the surrounding area appears to have been a place of considerable religious significance to Aboriginal people, there is evidence which indicates that frequent large ceremonial gatherings took place in the area. Basalt is the most common rock on Earth’s surface, more than 90% of all volcanic rock on Earth is basalt. Basalt is an aphanitic extrusive igneous rock formed from the rapid cooling of low-viscosity lava exposed at or very near the surface of a rocky planet or moon. Specimens are black in colour and weather to dark green or brown. Basalt is rich in iron and magnesium and is mainly composed of olivine, pyroxene, and plagioclase. Olivine is the name of a group of rock-forming silicate minerals with compositions ranging between Mg2SiO4 and Fe2SiO4. Unlike other minerals, Olivine has a very high crystallisation temperature which makes it the first of the minerals to crystallise from magma. As magma cools, the crystals begin to form and settle on the bottom of the lava and form basalts that are abnormally enriched in olivine in the lower part of lava flows. According to H. M. King (on geology.com) "Olivine is thought to be an important mineral in Earth's mantle. Its presence as a mantle mineral has been inferred by a change in the behaviour of seismic waves as they cross the boundary between Earth's crust and mantle". Lava from Mount Franklin and other volcanoes in the area filled valleys and buried the gold bearing streams that became the renowned ‘deep leads’ of the gold mining era. In 1852, as part of the Victorian gold rush, gold was discovered in the immediate area, this gold was created by lava flows during the Newer Volcanic period, which were mined intensively during the nineteenth century. Around 1865 the presence of a deep lead in Mount Franklin was established. Deep lead mining was initially unsuccessful, and it was not until the late 1870s that the Franklinford Gold Mining Company mined at Mount Franklin on a significant scale. A few years later the Mount Franklin Estate Gold Mining Company also struck gold, followed by the Shakespeare and Great Western companies in the mid-1880s. By the late 1880s, however, deep lead mining had ceased in the area. Soon after gold was discovered in 1851, Victoria’s Governor La Trobe wrote to the Colonial Office in London, urging ‘the propriety of selecting and appointing as Mineral Surveyor for this Colony a gentleman possessed of the requisite qualifications and acquaintance with geological science and phenomena’. Alfred Selwyn was appointed geological surveyor in Australia in 1852 which began the Geological Survey of Victoria. In 1853-69 the Geological Survey issued under Selwyn's direction sixty-one geological maps and numerous reports; they were of such high standard that a writer in the Quarterly Journal of the Geological Society of London bracketed the survey with that of the United States of America as the best in the world. During his years spent in Australia, Selwyn collected numerous significant geological specimens, examples of which are held in collections such as the Burke Museum.This geological specimen is an example of basalt and olivine which shows the volcanic lava activity and geographical specific nature of Mt Franklin as a significant volcanic site. According to Agriculture Victoria 'The crater is one of the deepest in the Central Highlands area. It is a major megacryst site with some of the largest known Victorian examples of megacrysts of augite and an orthoclase. The small parasitic mound of Lady Franklin on the western flanks adds to the geological interest of the site'. This specimen also highlights the locality as a significant place for both indigenous activity and Victorian gold rush era mining practices. 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.An angular, solid hand-sized piece of grey volcanic Basalt with green/brown Olivine phenocrysts along one flat edge.Olivine in basalt / - label is probably / correct. / C. Willman / 15/4/21burke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, mineralogy, basalt, igneous rock, igneous-volcanic, volcanic geology, volcanic, olivine, olivine specimen, basaltoid

Coorongite is a dark, rubber-like, highly resilient structureless algal deposit. In the Coorong district of South Australia it occurs in moderate quantities associated with the coastal swamps and sand dunes which extend for a considerable distance east of the mouth of the Murray. This particular specimen was recovered from the south of the Coorong River, South Australia. A type of sediment rich in organic matter, Coorongite is the unlithified end-member of the sapropelic coal series. The members of the sapropelic coal series can be ranked in order as sapropel (the unlithified form), sapropelic-lignite, and sapropelic-coal (the lithified forms) based on increasing carbon content and decreasing volatile content. Sapropel (Coorongite) is an unlithified dark, pulpy, fine organic mud containing concentrations of algae and miospores that are more or less identifiable. Coorongite is typically found as an algae like substance, that can be found in irregular size pieces. Coorongite was believed to be dried up oil due to its rubber-like texture. The Coorongite is also soft to the point where it can be cut into with a knife or it can be broken and torn by hand. Otherwise known as 'Kurangk', the Coorong River is home to the Ngarrindjeri people, which acts as both a place for gathering food and a spiritual place. In 1852 the first sight of Coorongite was found along the Coorong River. The finders mistook the Coorongite for dried up oil, which lead to the belief that there were oil reserves under the Coorong River. Between the 1860s and the 1930s the Coorong River became a place where mining oil and Coorongite became precedent. Nowadays, the local council and the South Australian Government are working together with the Ngarrindjeri people to sustain and preserve the Coorong River and the culture that is with it. Soon after gold was discovered in 1851, Victoria’s Governor La Trobe wrote to the Colonial Office in London, urging ‘the propriety of selecting and appointing as Mineral Surveyor for this Colony a gentleman possessed of the requisite qualifications and acquaintance with geological science and phenomena’. Alfred Selwyn was appointed geological surveyor in Australia in 1852 which began the Geological Survey of Victoria. Selwyn went on to collect geological samples and catalogue thousands of specimens around Australia. In 1853-69 the Geological Survey issued under Selwyn's direction sixty-one geological maps and numerous reports; they were of such high standard that a writer in the Quarterly Journal of the Geological Society of London bracketed the survey with that of the United States of America as the best in the world. During his years spent in Australia, Selwyn collected numerous significant geological specimens, examples of which are held in collections such as the Burke Museum.Coorongite is considered to be a mineral with a unique texture, where it can be both hard and soft. Coorongite can also be considered to be a rare mineral, as it is only located along the Coorong River and due to the mining of it, has left very few sources. It was believed at one point that Coorongite could be used to replace oil. 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.Three solid varyingly hand-sized pieces of wooden appearing organic matter derived from the river in the Coorong District in South Australia. A rubber-like, highly resilient structureless algal deposit.Specimen 245 page 69 / in Descriptive Register / "Elcestic Bitumen, / Coorangite" South of / Coorung River, South Australia . / C. WIllman / 15/4/21burke museum, beechwoth, indigo shire, beechworth museum, geological, geological specimen, mineraology, coorong, coorong river, kurangk, ngarrindjeri, south australia, coorongite, coorongite specimen

Brown Coal is typically found as rocks. During formation the Brown Coal starts as peats, which is an acidic brown deposit resembling soil, and over time when subjected to pressure and heat these peats form the Coal. Brown Coal is the lowest rank of coal as it has a low carbon (energy) content, and a high moisture content. This high moisture content makes Brown Coal unsuitable for overseas exports. This particular specimen was recovered from the Yallourn Mine in Latrobe Valley, Victoria as part of the geological survey of Victoria being carried out by Alfred Selwyn. Otherwise known as the 'Yallourn Power Station', the Yallourn Mine is Australia's second largest mine. Yallourn Mine was first built in 1920, and since then it has been providing over 1 billion tonnes of Brown Coal to Australia every year. The Yallourn Mine is responsible for 22% of Victoria's electricity and 8% of Australia's electricity. As of 2021 the mine employs around 500 people. Due to ongoing maintenance issues and Australia's move to cleaner energy, the Yallourn Mine intends to shut down permanently as of 2028. Soon after gold was discovered in 1851, Victoria’s Governor La Trobe wrote to the Colonial Office in London, urging ‘the propriety of selecting and appointing as Mineral Surveyor for this Colony a gentleman possessed of the requisite qualifications and acquaintance with geological science and phenomena’. Alfred Selwyn was appointed geological surveyor in Australia in 1852 which began the Geological Survey of Victoria. In 1853-69 the Geological Survey issued under Selwyn's direction sixty-one geological maps and numerous reports; they were of such high standard that a writer in the Quarterly Journal of the Geological Society of London bracketed the survey with that of the United States of America as the best in the world. During his years spent in Australia, Selwyn collected numerous significant geological specimens, examples of which are held in collections such as the Burke Museum.Brown coal is considered to be an essential rock to Australia's energy consumption. Although plentiful in sources, Brown Coal is not able to be exported overseas due to its high moisture content. As Australia moves towards cleaner energy, Brown Coal is going become less used. 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 sedimentary rock that is a dark shade of brown.13 / BROWN COAL / Showing Woody structure / Locality: Yallourn, Vic. | Label probably / correct but / can't find reference / no. 13 to match in / registers. / C Willman / 15/4/21burke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, mineralogy, yallourn, yallourn mine, victoria, coal, brown coal, brown coal specimen, alfred selwyn, geological survey of victoria, geological survey, yallourn power station

This image shows Bethanga Bridge, which was constructed between 1927 and 1930 in Albury, NSW. The bridge was a necessity due to the building of the Hume Dam (Wier), 1919-1936. Bethanga Bridge is a long, nine-span, riveted-steel, variable depth, Pratt Truss road bridge of nine principal spans of 82 metres and a total length of 752 metres over the flooded valley of the Murray River, now part of Hume Reservoir. Because of its unique location, over the waters of a dam with the border running down the centre of the body of water, the Bethanga bridge is the only built structure shared by both New South Wales and Victoria. It was built 1.6 kilometres upstream of the dam and in 1961 was raised 300mm, with a concrete deck replacing the original wooden deck. The State Rivers and Water Supply Commission of Victoria and the New South Wales Department of Public Works were responsible for the construction works for the Hume Weir under the River Murray Waters Agreement. It is apparent that a similar joint arrangement was made for the construction of the Bethanga Bridge as part of the Hume Weir works.This photograph of the Bethanga Bridge is of historical significance as it showcases the architectural skills of Percy Allen and Vincent Packer. Additionally, it reveals the environmental landscape of the 1920s-1930s, is linked to the Hume Dam and both New South Wales and Victorian heritage. Unmounted black and white rectangular photograph. Reverse: 1997.3196 84-20-3bethanga, bethanga bridge, hume dam, pratt truss, murray river, hume weir, transportation

This rectangle black and white photograph shows a bush scene with part of a suspension rope and wooden plank bridge visible in the middle of the image. It is likely this suspension bridge was used by the Tannery workers to move between the town and the Ovens Tannery located South-West of Beechworth due to its secluded bush location, the bridge likely spanned the gorge across Spring creek. The tannery itself was located alongside Gimlet Creek, about three kilometres from town, down what is now known as Malakoff and Old Tannery Road but which at the time was remote and accessed through bushland. The Ovens tannery was stablished in 1858 by Matthew Dodd and Hallahan and later Matthew and his brother Thomas Dodd in 1866 who developed it over the years. According to Doyle, 'we have little information about its early operations except the tannery itself comprised four small buildings' by 1870 ‘a small village with gardens of vines and fruit trees surrounded the tannery’ (Woods, 121), and by 1887 the Tannery employed fifteen men. The Ovens tannery was among several new businesses establishing themselves such as a foundry that brought industrial manufacturing alongside the developing township and which strengthened the economic stability of Beechworth after the receding mining surge. According to Woods (p. 121) in the 1860’s the government spent considerable sums to establish several public buildings such as the Benevolent Asylum, the Hospital and Insane Asylum to support those in need of care in the area directly after the Indigo gold rush which had left Beechworth, a fairly remote regional and newly formed township (Gold was first discovered in Beechworth in 1852) with a number of infirm and destitute people in its wake and which due to the support and establishment of these facilities ‘made Beechworth a significant social welfare centre in Victoria’ (Woods, p. 121). The tannery provided employment and connected the regional centre with other parts of Victoria and the wider colonial outposts and would have been a welcome opportunity for those seeking work after gold was no longer a source of income.A good example of the ingenuity of regional settlers to achieve what would have been a difficult and remote construction of a bridge as a means of access. This bridge is evidence of planning and forethought and shows dedication to establishing a life in a remote landscape.Black and white rectangular photograph printed on paperreverse: / 2983 / / BMM2983 /black and white photograph, bush, suspension bridge, rope bridge, tannery, spring creek, ovens tannery, bushland, gimlet creek, matthew dodd, beechworth

Taken during the construction of the Bethanga Bridge (1927-1930), this sepia photograph shows a view of the incomplete bridge taken from inside the structure and looking down the span of the bridge from where the photographer stands. The photograph depicts an incomplete deck, with loose-looking wooden planks/panels lain along the centre in groups of three. Once complete, the original decking of the bridge was made of timber before being replaced by cement in 1961 (Victorian Heritage Database).Bethanga Bridge is of historical significance to the Indigo Shire for its associations with the construction of Hume Dam, its associations with the River Murray Waters Agreement and the River Murray Commission, and illustration of the needs and influence of the farming communities along the river in this area - particularly in relation to the building of the Weir. It also represents the collaboration between New South Wales and Victoria on a large infrastructure project, being the only built structure shared by both New South Wales and Victoria due to its location. also reflecting on the Shire's geographical closeness to this neighboring state. This photograph is part of a series that documents the construction of this well-known heritage site of significance to the Indigo Shire. It reflects upon a period of growth and change in the area.Sepia, rectangular photograph printed on matt photographic paper, unmountedReverse: 1997.3190 / Another snap of the bridge. taken on the bridge showing huge steel sides / 84-19-4 / V [in circle] 354 / KODAK PRINTbethanga bridge, hume dam, bridges album, construction, road construction, hume weir

This image shows the Punt (a kind of small boat) that took residents of Bethanga across the Murray River before the Bethanga Bridge was built. Bethanga Bridge was built between 1927 and 1930, and was made a necessity by the building of the Hume Dam. The Hume Dam, formerly known as the Hume Weir, was in construction between 1919 and 1936, which swelled the Murray River into the floodplain to the East of the dam permanently, creating Lake Hume, and isolating the residents of Bethanga and nearby towns, for whom the trip all the way around the new lake to another river crossing was a massive undertaking. The person who wrote on the back of this card instead chose to cross the river on a boat until the Bethanga Bridge became available. Interestingly, partially submerged trees can be seen in the lake in the background of this photograph, illustrating that the dam had already begun to fill the floodplain even before the bridge was built. This photograph shows the methods the residents of Bethanga used while the Bethanga Bridge was being built. This record is associated with the Heritage Listed sites of the Hume Dam and the Bethanga Bridge, and shows the environment during the process of construction and the creation of Lake HumeSepia rectangular photograph printed on matte photographic paperReverse: 1997.3189 / 84 -19 -1 / This is the snap of the Punt. / Our only means of getting out / of Bethanga for the present / Until the bridge is completed / it is 2 miles above the junction / of the Mitta + Murray. It is / 1/2 a mile wide + runs across / the Murray into NSW / Kodak Print / bethanga, bethanga bridge, hume, hume dam, artificial lake, lake hume, hume weir, flood, floodplain, boat, punt, weir, pier, dock, transport, transportation

Taken on 25 October 1930, various houses with the Hume Dam under construction are depicted in the background. The construction of the Hume Dam took place from 1919 to 1936. At the time of construction, it was the second largest dam in the world. It was also one of the earliest civil projects developed after the Federation. Some of the Dam workers consisted of World War I veterans. Dam workers often settled their families in Mitta Junction Village and Wodonga. Archaeological surveys were completed by Austral Archaeology, which was done when the Department of Land & Water Conservation was doing work to improve Hume Dam. The archaeological report that came out of the survey recommended three sites of interest where archaeological excavation should be done: Camp Ganger’s Quarters, Stableman’s Quarters, and the Industrial Dump. The excavation uncovered artefacts. Mitta Mitta: Mitta Mitta is situated between Mount Welcome and Mount Misery. It is named after the river that explorers Hume and Hovell discovered in 1824. The town would eventually become a huge gold mining town. Mitta Mitta is called Midamodunga by the local Indigenous peoples Wodonga: Wodonga is situated on the Murray River and is part of North East Victoria. Hume and Hovell: Hamilton Hume (1979-1873) and William Hilton Hovell (1786-1875). W. H. Hovell was born in Norfolk England and Hume was born in Parramatta, New South Wales Hovell and Hume undertook an exploration journey in 1824 and thought they discovered a river, which turned out to be the Murray River. They returned home in 1825, but returned to the area in 1826 and discovered coal in the area. This photo is historically significant as it shows the Hume Dam under construction in 1930. The Dam was named after Hamilton Hume, who is an important historical figure for this area as he helped discover the area where resources were found.Sepia rectangular photograph printed unmountedReverse: 84-19-5 / 1997.3185/ Values & spillway. / When completed the wall / will be as high as the / scaffolding. [featuring trademark: kodak print]construction, houses, veterans, mitta junction village, hume dam, world war i, federation, wodonga, archaeological survey, excavation, austral archaeology, department of land & water conservation, camp ganger's quarter's, stableman's quarters, industrial dump, artefacts, mitta mitta, mount welcome, mount misery, murray river, hamilton hume, william hilton hovell, hume and hovell expedition

Taken on 25 October 1930, various houses with the Hume Dam under construction are depicted in the background. The construction of the Hume Dam took place from 1919 to 1936. At the time of construction, it was the second largest dam in the world. It was also one of the earliest civil projects developed after the Federation. Some of the Dam workers consisted of World War I veterans. Dam workers often settled their families in Mitta Junction Village and Wodonga. Archaeological surveys were completed by Austral Archaeology, which was done when the Department of Land & Water Conservation was doing work to improve Hume Dam. The archaeological report that came out of the survey recommended three sites of interest where archaeological excavation should be done: Camp Ganger’s Quarters, Stableman’s Quarters, and the Industrial Dump. The excavation uncovered artefacts. Mitta Mitta: Mitta Mitta is situated between Mount Welcome and Mount Misery. It is named after the river that explorers Hume and Hovell discovered in 1824. The town would eventually become a huge gold mining town. Mitta Mitta is called Midamodunga by the local Indigenous peoples Wodonga: Wodonga is situated on the Murray River and is part of North East Victoria. Hume and Hovell: Hamilton Hume (1979-1873) and William Hilton Hovell (1786-1875). W. H. Hovell was born in Norfolk England and Hume was born in Parramatta, New South Wales Hovell and Hume undertook an exploration journey in 1824 and thought they discovered a river, which turned out to be the Murray River. They returned home in 1825, but returned to the area in 1826 and discovered coal in the area.This photo is historically significant as it shows the Hume Dam under construction in 1930. The Dam was named after Hamilton Hume, who is an important historical figure for this area as he helped discover the area where resources were found.Sepia rectangular photograph printed unmountedReverse: 84-19-2/ 1997.3188/ These are the four / release valves they are / not always open (illegible) this / when closed the water flows / over the spillway. [featuring trademark: kodak print] photograph number: 354construction, houses, veterans, mitta junction village, hume dam, world war i, federation, wodonga, archaeological survey, excavation, austral archaeology, department of land & water conservation, camp ganger's quarter's, stableman's quarters, industrial dump, artefacts, mitta mitta, mount welcome, mount misery, murray river, hamilton hume, william hilton hovell, hume and hovell expedition

Taken on 25 October 1930, various houses with the Hume Dam under construction are depicted in the background. The construction of the Hume Dam took place from 1919 to 1936. At the time of construction, it was the second largest dam in the world. It was also one of the earliest civil projects developed after the Federation. Some of the Dam workers consisted of World War I veterans. Dam workers often settled their families in Mitta Junction Village and Wodonga. Archaeological surveys were completed by Austral Archaeology, which was done when the Department of Land & Water Conservation was doing work to improve Hume Dam. The archaeological report that came out of the survey recommended three sites of interest where archaeological excavation should be done: Camp Ganger’s Quarters, Stableman’s Quarters, and the Industrial Dump. The excavation uncovered artefacts. Mitta Mitta: Mitta Mitta is situated between Mount Welcome and Mount Misery. It is named after the river that explorers Hume and Hovell discovered in 1824. The town would eventually become a huge gold mining town. Mitta Mitta is called Midamodunga by the local Indigenous peoples Wodonga: Wodonga is situated on the Murray River and is part of North East Victoria. Hume and Hovell: Hamilton Hume (1979-1873) and William Hilton Hovell (1786-1875). W. H. Hovell was born in Norfolk England and Hume was born in Parramatta, New South Wales Hovell and Hume undertook an exploration journey in 1824 and thought they discovered a river, which turned out to be the Murray River. They returned home in 1825, but returned to the area in 1826 and discovered coal in the area.This photo is historically significant as it shows the Hume Dam under construction in 1930. The Dam was named after Hamilton Hume, who is an important historical figure for this area as he helped discover the area where resources were found.Sepia rectangular photograph printed unmountedReverse: 84-19-6/ 1997.3187/ The spillway [featuring trademark: kodak print] construction, houses, veterans, mitta junction village, hume dam, world war i, federation, wodonga, archaeological survey, excavation, austral archaeology, department of land & water conservation, camp ganger's quarter's, stableman's quarters, industrial dump, artefacts, mitta mitta, mount welcome, mount misery, murray river, hamilton hume, william hilton hovell, hume and hovell expedition

Taken on 25 October 1930, various houses with the Hume Dam under construction are depicted in the background. The construction of the Hume Dam took place from 1919 to 1936. At the time of construction, it was the second largest dam in the world. It was also one of the earliest civil projects developed after the Federation. Some of the Dam workers consisted of World War I veterans. Dam workers often settled their families in Mitta Junction Village and Wodonga. Archaeological surveys were completed by Austral Archaeology, which was done when the Department of Land & Water Conservation was doing work to improve Hume Dam. The archaeological report that came out of the survey recommended three sites of interest where archaeological excavation should be done: Camp Ganger’s Quarters, Stableman’s Quarters, and the Industrial Dump. The excavation uncovered artefacts. Mitta Mitta: Mitta Mitta is situated between Mount Welcome and Mount Misery. It is named after the river that explorers Hume and Hovell discovered in 1824. The town would eventually become a huge gold mining town. Mitta Mitta is called Midamodunga by the local Indigenous peoples Wodonga: Wodonga is situated on the Murray River and is part of North East Victoria. Hume and Hovell: Hamilton Hume (1979-1873) and William Hilton Hovell (1786-1875). W. H. Hovell was born in Norfolk England and Hume was born in Parramatta, New South Wales Hovell and Hume undertook an exploration journey in 1824 and thought they discovered a river, which turned out to be the Murray River. They returned home in 1825, but returned to the area in 1826 and discovered coal in the area.This photo is historically significant as it shows the Hume Dam under construction in 1930. The Dam was named after Hamilton Hume, who is an important historical figure for this area as he helped discover the area where resources were found.Black and white rectangular photograph printer unmountedReverse: 84-20-1/ 1997.3147construction, houses, veterans, mitta junction village, hume dam, world war i, federation, wodonga, archaeological survey, excavation, austral archaeology, department of land & water conservation, camp ganger's quarter's, stableman's quarters, industrial dump, artefacts, mitta mitta, mount welcome, mount misery, murray river, hamilton hume, william hilton hovell, hume and hovell expedition

Taken on 25 October 1930, various houses with the Hume Dam under construction are depicted in the background. The construction of the Hume Dam took place from 1919 to 1936. At the time of construction, it was the second largest dam in the world. It was also one of the earliest civil projects developed after the Federation. Some of the Dam workers consisted of World War I veterans. Dam workers often settled their families in Mitta Junction Village and Wodonga. Archaeological surveys were completed by Austral Archaeology, which was done when the Department of Land & Water Conservation was doing work to improve Hume Dam. The archaeological report that came out of the survey recommended three sites of interest where archaeological excavation should be done: Camp Ganger’s Quarters, Stableman’s Quarters, and the Industrial Dump. The excavation uncovered artefacts. Mitta Mitta: Mitta Mitta is situated between Mount Welcome and Mount Misery. It is named after the river that explorers Hume and Hovell discovered in 1824. The town would eventually become a huge gold mining town. Mitta Mitta is called Midamodunga by the local Indigenous peoples Wodonga: Wodonga is situated on the Murray River and is part of North East Victoria. Hume and Hovell: Hamilton Hume (1979-1873) and William Hilton Hovell (1786-1875). W. H. Hovell was born in Norfolk England and Hume was born in Parramatta, New South Wales Hovell and Hume undertook an exploration journey in 1824 and thought they discovered a river, which turned out to be the Murray River. They returned home in 1825, but returned to the area in 1826 and discovered coal in the area. This photo is historically significant as it shows the Hume Dam under construction in 1930. The Dam was named after Hamilton Hume, who is an important historical figure for this area as he helped discover the area where resources were found. Black and white rectangular photograph printer unmountedReverse: 1997.3145/ 84-20-2construction, houses, veterans, mitta junction village, hume dam, world war i, federation, wodonga, archaeological survey, excavation, austral archaeology, department of land & water conservation, camp ganger's quarter's, stableman's quarters, industrial dump, artefacts, mitta mitta, mount welcome, mount misery, murray river, hamilton hume, william hilton hovell, hume and hovell expedition

The photograph is a reproduction of a postcard from the Rocky Mountain Mining Company. In 1875, the Rocky Mountain Extended Gold Sluicing Company Ltd was created, utilising the previous Rocky Mountain claim for the area near Lake Sambell. The company employed A.L Martin to survey an area for a tunnel underneath Beechworth and Johnson Stephens to dig it. The tunnel was built at a rate of 40 feet a month and eventually measured 800 metres. The tunnel was a true accomplishment both in the present and during the 19th century. It was considered to be a marvelous engineering feat. Beechworth is renowned for its hydraulic sluice method of mining. This involved soil being exposed to torrents of water from high-pressure hoses. From 1876 until its closure in 1921, the mine produced an astounding 47,926 ozs of gold. Companies like this were the source of income for many Chinese gold-diggers who sought to make their fortune on the goldfields of Beechworth. During the height of the rush, the town had around 7,000 Chinese inhabitants living on the outskirts of town as they were not permitted to live within Beechworth itself.This image of the Rocky Mountain mine is historically significant as the mining complex is now non-existent, with the only remains being the tunnel built in 1880 by the company, which was considered one of the greatest engineering feats of the time. The image also provides a first-hand look into the social and cultural networks at play during the 19th century with racial segregation of the Chinese at the 'Chinese Camp', as well as an insight into Beechworth's origins during the Gold Rush.Black and white rectangular reproduced photograph printed on paperbeechworth, rocky mountain mine, sluicing, gold rush, mining, gold

Alma Isabell Ashcroft was born on the 11th of July 1920 in Newtown, Beechworth. Her father and four of her brothers worked at the Tannery, her mother was recognised as the ‘district nurse’ in the area and the family were well known and at the heart of the local community. Alma joined the Beechworth branch of the R.S.L. and at the time of the interview in 2000, had been with the R.S.L for 40-50 years. This oral history recording was part of a project conducted by Jennifer Williams in the year 2000 to capture the everyday life and struggles in Beechworth during the twentieth century. This project involved recording seventy oral histories on cassette tapes of local Beechworth residents which were then published in a book titled: Listen to what they say: voices of twentieth century Beechworth. These cassette tapes were digitised in July 2021 with funds made available by the Friends of the Burke.Alma Ashcroft’s story is significant because of her personal and familial connections with Beechworth. Her family were at the heart of the community, and Alma’s association with the RSL in Beechworth spanned 4-5 decades. During the interview with Jennifer Williams, Alma also provided a rich history of the town, the locals and her extensive family.This is a digital copy of a recording that was originally captured on a cassette tape. The cassette tape is black with a horizontal white strip and is currently stored in a clear flat plastic rectangular container. It holds up 40 minutes of recordings on each side.listen to what they say, beechworth, oral history, burke museum, jennifer williams, twentieth century, ashcroft, alma ashcroft, r.s.l, community