The Common pheasant is a gregorious, colorful bird renowned for the striking plumage of the male. It is native to Asia and parts of Europe but has been widely introduced elsewhere as a game bird, including Australia. In their natural habitat, Common pheasants live in grassland near the water with small copses of trees, but can also be found in can be found in woodland, farmland, scrub, and wetlands. Common pheasants are diurnal and spend most of their time on the ground. This specimen is part of a collection of almost 200 animal specimens that were originally acquired as skins from various institutions across Australia, including the Australian Museum in Sydney and the National Museum of Victoria (known as Museums Victoria since 1983), as well as individuals such as amateur anthropologist Reynell Eveleigh Johns between 1860-1880. These skins were then mounted by members of the Burke Museum Committee and put-on display in the formal space of the Museum’s original exhibition hall where they continue to be on display. This display of taxidermy mounts initially served to instruct visitors to the Burke Museum of the natural world around them, today it serves as an insight into the collecting habits of the 19th century.This specimen is part of a significant and rare taxidermy mount collection in the Burke Museum. This collection is scientifically and culturally important for reminding us of how science continues to shape our understanding of the modern world. They demonstrate a capacity to hold evidence of how Australia’s fauna history existed in the past and are potentially important for future environmental research. This collection continues to be on display in the Museum and has become a key part to interpreting the collecting habits of the 19th century.This male Common Pheasant is colourful and has striking plumage. It has a small white crest, greenish/blue neck and a pinkish/brown chest. The rest of its feathers are brown, black, white with hints of light grey, where a variety of speckled patterns are apparent on its belly, legs and back feathers. This specimen stands upon a wooden perch attached to platform, facing forward and leaning slightly to the right.taxidermy mount, taxidermy, animalia, burke museum, beechworth, australian museum, skin, reynell eveleigh johns, bird, common pheasant, phasianidae

Historical photograph taken of the frontage of the Burke Museum in Beechworth. As Australia’s oldest regional museum, the building used for the Burke Museum was originally built as the Beechworth Athenaeum, and was later dedicated as a museum in memorial to the explorer Robert O’Hara Burke, who died on the Burke and Wills expeditions in 1861. The Burke and Wills exhibitions were a significant colonial event that was memorialised in paintings, buildings, monuments, and statues. The photograph has historical significance, connecting with various themes such as exploring, establishing pathways, and significant colonial events or persons. The photograph depicts the frontage of the Burke Museum, which was dedicated as a memorial to the explorer Robert O’Hara Burke, who died on the Burke and Wills expeditions in 1861. Robert O’Hara Burke was a significant person who was connected to both Beechworth and to an important colonial event, the Burke and Wills expeditions. Born in Ireland, Burke migrated to Australia in 1853 and nearly a year later, was appointed to senior inspector at Beechworth. Described as quick-tempered yet generous, Burke later joined an expedition to explore the interior of the Victorian colony, which was later termed the Burke and Wills expeditions. While the expeditions generated a significant amount of interest, the objectives of the Burke and Wills expeditions were hazy, as was its planned route, leading to disaster on the trip as group infighting, poor provisions, and a lack of clear instructions ultimately resulted in Burke’s death. Regardless, the Burke and Wills expeditions promoted discovery and endures today in popular memory.Black and white rectangular photograph printed on paper.Obverse: 1856/ BEECHWORTH/ PUBLIC/ LIBRARY/ BURKE/ MUSEUM/ BURK MUSEUM/ (parking signs illegible) Reverse: BMM 84-2-1/ A02989 1997 2696/ BMM 84-2-3burke museum, beechworth, beechworth athenaeum, athenaeum, memorial, robert o'hara burke, robert burke, burke and wills exhibitions

The Little Pied Cormorant is commonly seen in Australia's wetlands. These birds reside amongst large flocks in locations where fish is plentiful. On the occasion that this bird is seen on inland streams and dams they will be solitary. This particular species willingly mixes with similar sized birds including the Little Black Cormorant. They feed on aquatic animals ranging from insects and yabbies and are labelled as benthic feeders because they find their prey on the seafloor. This specimen is part of a collection of almost 200 animal specimens that were originally acquired as skins from various institutions across Australia, including the Australian Museum in Sydney and the National Museum of Victoria (known as Museums Victoria since 1983), as well as individuals such as amateur anthropologist Reynell Eveleigh Johns between 1860-1880. These skins were then mounted by members of the Burke Museum Committee and put-on display in the formal space of the Museum’s original exhibition hall where they continue to be on display. This display of taxidermy mounts initially served to instruct visitors to the Burke Museum of the natural world around them, today it serves as an insight into the collecting habits of the 19th century.This specimen is part of a significant and rare taxidermy mount collection in the Burke Museum. This collection is scientifically and culturally important for reminding us of how science continues to shape our understanding of the modern world. They demonstrate a capacity to hold evidence of how Australia’s fauna history existed in the past and are potentially important for future environmental research. This collection continues to be on display in the Museum and has become a key part to interpreting the collecting habits of the 19th century.The Little Pied Cormorant specimen is a small bird with white and black colouring. The back of the head, neck, wings and tail are black while the undersides are a creamy white. The feet are webbed and are also dark in colouring. The bird has pale glass eyes and a medium sized bill and a long tail. This specimen is styled to look over it's left wing with its long neck bent to look in that direction. It stands on a wooden mount with a paper identification tag attached to the bird's right foot. The mount has the number 152 written on the wood.Swing tag: 21a. / Pied Cormorant / Catalogue page 41 / Mount: 152 /taxidermy mount, taxidermy, animalia, burke museum, beechworth, australian museum, skin, reynell eveleigh johns, bird, cormorant, little piet cormorant, waterbird

Taken in the early 1900s, the postcard depicts two girls dressed in old style, white knee length dress which was common for this period for young women. This compared to the ankle length styles which were acceptable for adult women. We can also see an example of early bridge construction and engineering, notably made from timber rather than from stone or steel, noted in the postcard as Snow's Bridge. Sepia rectangular postcard printed on card Obverse: Snow's Bridge/Beechworth Reverse: Dear Julie/ I received your pretty PB/ We haven't gone away yet. Mr Stokes/ asked me were you going to be/ married. He wished you luck/ (I wonder/ if he meant it.) We sent the Magpie to Annie to-day. I haven't got any/ word about going to a [unknown]/ yet. We had a great Friendly Societies/ day yesterday but it rained a bit/ Sally is going to get a [illegible] silk/ dress. When are you to be married?/ Mr Pounceby is back at Allen's shop./ [unknown]. We are going to Belle's for a [unknown] if we can. With Love from Lilly. bridge, beechworth, snow's bridge, children, childhood, postcard

Early photo of the Bridge over Spring Creek taken along Camp Street facing East. This photograph was taken after 1890, when powerlines were beginning to be put up in regional Victoria.Black and white rectangular photograph printed on matte photographic paperbeechworth, spring creek, camp street

Galena Chalcopyrite is the earth's primary ore of lead and is mined from a large number of deposits in many countries. It is also an important source of silver. Galena Chalcopyrite is one of the most abundant and widely distributed sulfide minerals across the world. The mineral is found in igneous and metamorphic rocks in medium- to low-temperature hydrothermal veins. This specific specimen was recovered from the mines in Broken Hill, New South Wales. The mines in Broken Hill were first established after Charles Rasp discovered a large amount of silver-lead-zinc ore-body in the area in 1883. BHP (Broken Hill Proprietary) mining company was then established in 1885 and quickly became the lead in Australia's mining industry after they began excavating and exporting the country's largest amount of lead, silver, and zinc. This feat generated over $100 billion in wealth for the company.Galena Chalcopyrite is signifiant as it represents the catalyst for the rise of Australia's most influential mining companies - BHP. The mineral was one of the first to be mined in the country and after being made into lead, was used for a variety of things such as paint, batteries, ammunition, and plumbing materials before it was known to be harmful to humans. 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 grey, solid hand-sized lead sulfide mineral with a silver metallic luster.burke museum, beechworth, geological, geological specimen, galena, galena chalcopyrite, chalcopyrite, broken hill, bhp, bhp mining, broken hill mine, mine, australia mine, lead, lead mine

Gabo Island sits off the coast of East Gippsland in Victoria, with cliffs of granite in a relatively unique red/pink colour. Early attempts to build a lighthouse on the island were abandoned due to poor foundations, but when a ship ran aground on the nearby Tullaberga Island in 1853 and led to the death of 37 people, efforts were reignited. Construction of a new lighthouse was completed by 1858, using Gabo Island granite. The lighthouse is Australia's second tallest in Australia and continues to play an important role in guiding boats around the coast as they journey between Melbourne and Sydney. The distinct pink colour from the granite means the lighthouse continues to be a defining feature of the island. Gabo Island granite was also used to construct the Treasury Building at 117 Macquarie Street in Sydney, now the Intercontinental Hotel.Granite in the pink colour of this specimen is relatively rare. The connection to the lighthouse on Gabo Island also gives the specimen historic significance and social significance regarding the maritime history 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 palm-sized mineral, coloured by flecks of pink, red, and grey. Granite is formed by the slow crystallisation of magma below the earth's surface. It is typically composed of a mix of quartz, feldspar, and other minerals, though syenitic granite like this sample has a smaller amount of quartz than typical granite. This different mineral composition leads to the more distinct pink and red colouring.First sticker: [torn]logical survey / R........ S........ / Loc Gabo Island / 1/4 Sheet / Second Sticker: 15 Third Sticker: Syenitic Graniteburke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, mineralogy, gabo island, gabo island lighthouse, lighthouse, granite, coast, coastal, granite specimen, victoria, coastal cliffs

In Australia, precious opal is found in Cretaceous age sandstones and mudstones. These sedimentary rocks were deeply weathered and this weathering released silica into the groundwater.Australia is the only part of the world where opalised animal and plant fossils have been found. Opal artefacts several thousands of years old have been discovered in East Africa. As early as 250 BC the Romans prized opals, thought to have come from mines in Eastern Europe, the ancient world's main source of opals. There are many aboriginal dreamtime stories that feature opal. Australian opals discovered during the late 1800's found little favour with European markets but their commercial value increased in the 1900's and in 1932 Australia took over as the major producer of opals in the world and remains the largest producer to this day. Opal is found around the world (Brazil, Mexico, Honduras and the western US) however Australia produces 95% of the world's precious opal and it is our official national gemstone. Opal was first mined commercially at Listowel Downs in Queensland in 1875 and later at White Cliffs in NSW. Today, Coober Pedy (SA) is the main producer of white opal, though in recent years this field has expanded and all types of opals are found. Other centres in SA include Andamooka and Mintabe. Lightning Ridge (NSW) is renowned for black opal and formerly White Cliffs was a large producer of high quality opal. Boulder opals (opals in concretionary ironstone) are mined in Queensland from numerous localities in a zone extending from the Eulo and Cunnamulla district in the south and northwest for a distance of over 700 km to Kynuna in the north. The towns of Quilpie, Yowah and Winton are the main opal mining and wholesale centres. Opals are considered gemstones and have been used in jewellery for thousands of years.Throughout much of history, opals were actually believed to be good luck. The Romans thought that opals were one of the luckiest gemstones and a symbol of hope. In the Middle Ages, opals were believed to be bestowed with all the positive properties of coloured gemstones due to its rainbow-like play of colour. Finally, there is a superstition that you should not wear an opal unless it is your birthstone otherwise misfortune will befall you. This, of course, is far-fetched, but the notion could have been promoted in the late 19th and early 20th Centuries by diamond traders who were trying to increase sales of diamonds and deter people from buying opals. Possibly related to this is the thought that you should set opal jewellery with diamonds as their powers of good fortune will override any negativity held by the opal. The great majority of opal does not show play of colour and is called common opal or potch however this is not the case with a precious opal. Opal is a precious gemstone, like rubies, emeralds or diamonds. Opal is rare, and it is expensive to prospect and mine for.Silica is one of the most common minerals on the planet, but precious opal is very rare – far more rare than diamonds. Precious opal is rare because the natural processes that create it rarely occur.Most (at least 95%) of the opal found by miners is common opal without gem colour. In Australia we call it potch. It can be white, grey, black or amber coloured. Even when a miner finds gem-coloured opal, most of it can’t be cut into gemstones because it’s too thin, or sandy. 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.It is not known where this opal originated, except that it is probably from Victoria, as it has been recorded from many localities in the State. Common Opal is formed from silica-rich water circulating through rocks near the Earth’s surface. It consists of minute spheres of silica arranged in different ways. In common opal, the spheres are of different sizes and randomly arranged, unlike in precious opal where the spheres are of similar size and uniformly arranged in three dimensions. These differences account for common opal generally being translucent to opaque and without the play of colours, or opalescence, displayed by precious opal. Common opal is found in many localities and different geological environments throughout Australia and the world. Precious opal requires special conditions to form and is much less common. Australia produces most to the world’s precious opal. burke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, precious opal, opal, brazil, mexico, honduras, queensland, coober pedy, gemstones, jewellery, play-of-colour, light blue

This specimen was recovered from Creswick in Victoria. Basalt is dark in colour, often black and has a fine grain. It is composed of plagioclase and pyroxene minerals and an igneous rock. 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 cylindrical fine-grained piece of igneous rockburke museum, geological survey of victoria, geological specimen, geology

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 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 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

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

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

Sister Elizabeth McGovern, Sister Mary Lacey, Sister Mary Griffiths, and Sister Gerardus Thistlewaite were all nuns of the Brigidine Order in Beechworth in the second half of the twentieth century. They had backgrounds in teaching and office work. As nuns, their contributions to the community included teaching, running camps, being there for community members wishing to talk to them or pray, and visiting prisons and hospitals. During their time in the order, the role of the nuns in Beechworth shifted due to the closing down of the Priory School, and changes in where housing for nuns was provided. The oral history also includes stories of boarding at the convent in the 1950s, and reflections on how the experience of being a nun has changed due to increasing immersion in the modern world, and the move from convent to house. 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.Sister Elizabeth McGovern, Sister Mary Lacey, Sister Mary Griffiths, and Sister Gerardus Thistlewaite's interview with Jennifer Williams is revealing of the history of the Brigidine order in Beechworth, and the role religion and nuns played in the wellbeing, education, and life of the community in the latter half of the twentieth century. It is significant both for what it illustrates about the lives and motivation of the Sisters, and for what it tells us about how the role of religious education and figures shifted in Beecjhworth from 1950 onward. It is especially illuminating about the experience of women in education. This oral history account is socially and historically significant as it is a part of a broader collection of interviews conducted by Jennifer Williams which were published in the book 'Listen to what they say: voices of twentieth-century Beechworth.' While the township of Beechworth is known for its history as a gold rush town, these accounts provide a unique insight into the day-to-day life of the town's residents during the 20th century, many of which will have now been lost if they had not been preserved.This is a series of digital recordings that were originally recorded on multiple cassette tapes. The cassette tapes are black with a horizontal white strip and are currently stored in a clear flat plastic rectangular container. They up to 40 minutes of recordings on each side.Sister Elizabeth McGovern, Sister Mary Lacey, Sister Mary Griffiths, Sister Gerardus Thistlewaitelisten to what they say, listen to what they say: voices of twentieth century beechworth, nuns, brigidine sisters, brigidine convent, school, religion, prison, boarding school, modernization, food, women's history, teaching, teachers, education, hospitals, beechworth hospital, charity, old priory, father stockdale, easter, beechworth 1950s

Ric Edwards was born in Melbourne, but moved to Beechworth in 1962. He had strong associations with Beechworth Prison, which is now called Beechworth Correctional Centre after 144 years. Ric had a strong role in creating the education program for the prisoners. 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.Although Beechworth is famous for its history in gold, the project by Jennifer Williams is significant as it captures the everyday life and struggles of residents living in Beechworth during the twentieth century. Ric Edwards story is significant as his story brings to light the prison system in Beechworth and it gives insight into not only Ric's role in the prison, but it also gives insight into the psychology of the prisoners.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, edwards, ric edwards, beechworth prison, beechworth correctional centre

Mrs Margaret Galbraith was born in Beechworth in 1913 on the 5th February. Her parents immigrated to Australia in 1910 from England. Her father was killed after being thrown from a cart in 1912, and her mother eventually purchased the general store in which she worked from the Ladson family. Margaret has some insights into the local area during the Depression from the perspective of a store owner, as well as the presence of 'tramps' in the town, and Chinese immigrants in the community. She speaks a lot about her mother who was a very strong woman. She retired at 80. Margaret married a Ladson in Melbourne and had children. She lived at 47 Finch Street, Beechworth. This oral history recording was part of a project by Jennifer Williams in 2000 to capture the everyday life and struggles in Beechworth during the 20th century. This project involved recording 70 oral history stories on cassette tapes of local Beechworth residents, which were then published in a book called Listen to What they Say: Voices of 20th Century Beechworth. The cassettes were digitised in 2021 with funds made available by the Friends of Bourke.Mrs Margaret Galbraith's account of her life in Beechworth and the local area during the 20th century is historically and socially significant to the cultural heritage of the region. She details important historical events and hardships in the region's history that had a lasting local, regional and national impact, including Australia during war time, the Great Depression, immmigration, economic struggles, and women's societal roles in a rural area. This oral history account is socially and historically significant as it is a part of a broader collection of interviews conducted by Jennifer Williams which were published in the book 'Listen to what they say: voices of twentieth-century Beechworth.' While the township of Beechworth is known for its history as a gold rush town, these accounts provide a unique insight into the day-to-day life of the town's residents during the 20th century, many of which will have now been lost if they had not been preserved.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 stored in a clear, flat, plastic, rectangular container. It holds up to 40 minutes of recordings each sideMrs Margaret Galbraithlisten to what they say, ladson, oral history, bourke museum, beechworth, galbraith, margaret galbraith, general store

Frances Gertrude Gladstone was born on the 18th of September 1919 to Arthur George Ladson and Gertrude Hunrick Irving. France's grandfather, Alfred Ladson, came Beechworth from Norfolk, England, during the gold rush. Alfred had a grocery business, and was well known for writing letters for the miners to send to their families. Alfred also travelled to Beechworth with his sister, who was a trained nurse and helped establish a hospital for the goldfields. Frances remembers her father saying the Chinese miners were not allowed to bring their families to the goldfields, hence there were no Chinese children in schools around Beechworth. Frances was an avid botanist, and wrote a book called 'The Little Huntsman', which she wrote while watching her husband gold mining. 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.Frances Gladstone's story is significant, as she remembered important information about Chinese miners in the gold rush, explained the role of women in the 20th century in Beechworth, and the history of the hospitals in the region. 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, botanist, chinese miners, goldmining, gladstone

Mr Albert (Bert) Nankervis was born at Thougla, in the Upper Murray, in 1903. He had a large family and was one of eight children, four boys and four girls. He and his family moved to a farm in Wooragee named ‘Wattle Grove’ in 1918 after his father returned from serving as a soldier in World War One. The family established ‘Wattle Grove’ as a dairy farm as Beechworth has a high demand for milk and little supply. They had 25 milk cows that were hand milked every morning in order to provide milk for approximately 100 customers in the town, with any extra going to the butter factory at Springhurst. Albert married Floré Lilias Hardy in 1930 and they had two sons, Phillip and Barry. In this oral history, Albert discusses his life as a farmer in Wooragee, including his role in getting electricity to Beechworth, as well as his participation in the Young Farmer’s Association Immigration Scheme, which provided work experience to migrants in order for them to learn how to farm. 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. Mr Albert (Bert) Nankervis’s account of his life in Wooragee and the local area, including Beechworth, during the early 20th century is historically and socially significant to the cultural heritage of the region. He details his life as a farmer and milkman in the early 20th century, particularly the interwar period (1918-1939), but also discusses life after the Second World War, including employing young migrant men to train them as farmers through the Young Farmer’s Association. This oral history account is socially and historically significant as it is a part of a broader collection of interviews conducted by Jennifer Williams which were published in the book 'Listen to what they say: voices of twentieth-century Beechworth.' While the township of Beechworth is known for its history as a gold rush town, these accounts provide a unique insight into the day-to-day life of the town's residents during the 20th century, many of which will have now been lost if they had not been preserved. 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 45 minutes of recordings on each side.Mr Albert (Bert) Nankervis / albert nankervis, bert nankervis, nankervis, wattle grove, wooragee, dairy farm beechworth, dairy farm, dairy factories beechworth, dairying, milkman, oral history, springhurst, butter factory, electricity, rural life, farming and agriculture, farm, farm work, cow, cattle, jersey cattle, interwar period, first world war, second world war, wwi, wwii, greatest generation, centenarian, nonagenarian, 1920s, 1930s beechworth, thougla, upper murray, murray, lucyvale, benalla

Mrs Sheila Parkinson was born in Wagga in 1916 and came to Beechworth as a young woman around 1938. Sheila trained as a psychiatric nurse at Mayday Hills hospital prior to the second World War. At that time, unmarried women were accommodated and received nursing training on-site. Shiela was obliged to cease professional training and employment when she married in 1941, which disrupted completion of her final nursing examinations. Following post-war changes to the law that allowed married women to work, Sheila returned to Mayday Hills. Sheila's husband, Don, returned to Beechworth after four years abroad as a serviceman in the Australian Air Force. Beechworth's institutions were a major source of local employment throughout the twentieth century. As well as providing limited employment opportunities to young women like Shiela, post-war European migrants from Bonegilla Migrant camp found at Mayday Hills, encouraging European migrant settlement in the district. Mayday Hills was renamed several times since its establishment in 1867. At the peak of operations, it comprised sixty-seven buildings housing over twelve hundred patients patients and five hundred staff. The hospital officially closed in 1998. Today, the decommissioned two-storey Italianate style main building stands on eleven hectares of botanical gardens under National Trust protection. The site remains a popular cultural heritage destination for visitors. 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. The cassette tapes were digitised in July 2021 with funds made available by the Friends of the Burke.Employed as a psychiatric nurse at one of Beechworth's large welfare institutions, Mayday Hills, Mrs Sheila Parkinson recalls the conditions faced by staff and patients at the hospital, which cared for chronically ill people from the Ovens region and patients from the Yarra Bend Asylum, Melbourne, which closed in 1925. When Sheila first began her nurse training, Mayday Hills suffered from a lack of resources and rudimentary facilities and patients frequently suffered from the cold due to poor heating and inadequate clothing and bedding. However, as the twentieth century progressed, Sheila recalls how conditions and treatments improved as a result of increased government funding of services and advances in psychiatry and pharmaceutical medicine. Mrs Sheila Parkinson's oral history recording is historically and socially significant for its witness to life in Beechworth in the pre- and post-WWII period. Sheila's story enriches our understanding of processes of modernisation with regard to psychiatric and welfare services, while the course of Sheila's professional training and employment brings attention to systemic and socio-economic barriers faced by women, as well as the valuable contribution women and migrants make in the delivery of care and ancillary services. This oral history account is socially and historically significant as it is a part of a broader collection of interviews conducted by Jennifer Williams which were published in the book 'Listen to what they say: voices of twentieth-century Beechworth.' While the township of Beechworth is known for its history as a gold rush town, these accounts provide a unique insight into the day-to-day life of the town's residents during the twentieth century, many of which would have been lost if they had not been preserved.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.Mrs Sheila Parkinson /twentieth century beechworth, mayday hills, psychiatric care, benevolent asylums, nursing, wwii, psychiatric treatment, country women, psychiatric hostpital, beechworth's institutions, local employment, government institutions, listen to what they say, oral history, burke museum, sheila parkinson, beechworth lunatic asylum, beechworth mental hospital, beechworth hospital for the insane, the kerferd clinic, bonegilla migrant camp, working women, white australia policy