The Nankeen Kestrel, also known as the Australian Kestrel, is a common native to the open country's grasslands and farmlands, preferring agricultural areas. They are drawn to animal pests like mice, insects, small animals, reptiles, and birds. Due to the shape and ability of their tail feathers, which allows them to hoover over their prey, they do not rely on speed to catch their meal like most falcons in their family group. These birds are among the smallest raptors in the Falcon family, having well-known face characteristics and body shapes. The females of the species are distinguished by their darker patterns and red-brown (rufous) tones, as well as their larger size, whilst the males are more greyish. The yellow markings around the eyes and top of the beak, as well as the noticeable black dipped wings, distinguish each species. 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 Nankeen Kestrel is a small raptor in the Falcon family. It has a stockier appearance, with the upper parts of its body, such as the head and the tops of its wings, being a light red-brown (rufous) colour and the tips of its wings appearing dipped in black. The top of the beak and the eye rings are both yellow, and this bird's falcon appearance shows its inherent dark streak markings visible near the eyes and on the chest. The underparts are pale, with a tail feather that spreads out to help it hover and is ornamented with fine black decorations.20. / Unnamed / Catalogue page 5 / taxidermy mount, taxidermy, animalia, burke museum, beechworth, australian museum, skin, reynell eveleigh johns, bird, nankeen kestrel

The Nankeen Kestrel, a small type of falcon, can be found all over Australia, usually in grassland or farmland areas. This falcon is carnivorous and hunts all manner of small prey including mice, lizards, insects, and other birds. When hunting, Nankeen Kestrels can be seen hovering in the air searching for prey. Nankeen Kestrels are generally monogamous, staying with the same breeding partner for multiple seasons. The Nankeen Kestrel is known for its reddish-brown feathers, spotted with a distinctive black pattern on its back, and have black-tipped wings and tail band, a stark contrast to its white chest. Females tend to be larger, and males will have a grey head and neck area. 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 female Nankeen Kestrel is relatively small and slender. It is mostly reddish-brown, streaked with darker coloured areas. The tips of the wings and tail feathers are tipped in black. The chest is white with streaks of reddish-brown. The areas around its eyes, beak, and feet are a bright yellow. This specimen stands upon a wooden platform and has an identification tag tied around its leg.Swing-tag: 19. / Unnamed / Catalogue page, 5 /taxidermy mount, taxidermy, animalia, burke museum, beechworth, australian museum, skin, nankeen kestrel, falcon

Red Headed Woodpeckers can be found in Southern Canada and a large portion of the United States of America, generally migrating to the south if they originated in the northern regions. Their habitat is open forests or savannahs. They are classed as omnivores, finding food from pecking at wood or in flight. The Red Headed Woodpecker is threatened in Canada and some areas of the United States due to deforestation, lack of deadwood for nesting, competition with other birds, and a lack of food. They are an important part of the ecosystem, controlling insect populations and pollinating flora. Red Headed Woodpeckers typically have a beautiful, vibrant red neck and head, a stark white chest, black back, and black wings with white secondary remiges. They have a large chisel-like beak, suitable for foraging for their food. Their heads are rounded and they have short tails. 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 Red Headed Woodpecker is a small to medium-sized bird found in North America. This specimen is tricoloured: it has a red head and neck, a white chest, a black back, and black wings with white secondary remiges. It has a large chisel-like beak. This specimen has pest or humidity damage on the neck and head area. This specimen is standing on a wooden mount with a swing tag attached to it's leg.Swing-tag: 151a. Unnamed / Catalogue page, 60 /taxidermy mount, taxidermy, animalia, burke museum, beechworth, australian museum, skin, reynell eveleigh johns, bird, red headed woodpecker

The Common Buzzard is part of the buteo genus (Latin for buzzard or hawk) which indicates it is part of the raptor group whose features include a medium to large build, a strong body and larger wings. The family includes birds of prey such as hawks and buzzards. Like their name suggests, Common Buzzards are very ‘common’ in the UK but can also be found in other parts of Europe, Africa and Asia. The birds’ habitat consists of woodland, shrubland, forest, wetlands and countryside, and they can live in cold, tropical and temperate climate zones. Similar to other raptor species, Common Buzzards make their nests in tree branches or tree forks. With finely tuned hearing, they are able to detect small marsupials, and their diet consists of small amphibians, birds and mammals. Normally solitary, these raptors can occasionally be seen with others. Common Buzzards are classified as of ‘Least Concern’ on the IUCN Red List. While there is some noticeable fading of this particular taxidermy specimen’s plumage, it is relatively well presented. The completely black eyes and string through the nose of the specimen seem to be taxidermy/curatorial choices, as this is not something that is normally found on living versions today, and the eyes of Common Buzzards are normally golden eyes with black pupils. It is interesting to note, when considering the selected artificial eyes, that the original swing tag labeled this specimen as Saleo tinnunculus Lina, a form of kestrel (known to have complete black eyes), which perhaps explains this taxidermist choice. As a Common Buzzard, this particular specimen could have had its frame and breast area bulked out a little more, as birds within the buteo genus are generally recognised to be of medium to large build. Overall however, this is a fairly reasonable and accurate representation of the species. 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.With similar colourings and features to a range of raptor species, the Common Buzzard can often be mistaken for other varieties of buteo and raptor. The bird’s plumage generally varies by location, but normally includes a variety of shades of brown, commonly with darker brown on its back and lighter coloured feathers on its breast, underbelly areas and face. These birds normally have fine bands on their tail and darker tipped wings. Common Buzzards have smaller heads with a band of yellow around the base of their small curved beaks and golden yellow eyes. This particular specimen’s feathers have faded and he stands upon a wooden perch with an identifying tag hanging from its right leg.Swing Tag: Swing tag obverse seems to read: ‘…io [? First few symbols aren’t clear]/ Saleo /tinnunculus/ Lina [there is also another illegible symbol on the tag in the centre on the second line] Swing tag reverse: illegible sections of text and the beginning of a number ‘403…[?]. Metal tag: 1032[?]taxidermy mount, taxidermy, animalia, burke museum, beechworth, australian museum, skin, reynell eveleigh johns, bird, common buzzard, buteo, hawks, raptors, birds of prey, buzzards

This Merlin specimen is large for the falco columbarius species. It is brown and white in colouring which suggests that this particular specimen is female. This is because male Merlin's are usually blue, black, silver or grey. This species is predominantly found in the Northern Hemisphere. They are small, fast and highly skilled in hunting. The Merlin is generally a solitary bird outside of the mating season when it will socialise with other Merlins. The Merlin will consume smaller birds, mammals and bugs. 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 female Merlin has a medium brown back with light brown and white speckled chest. The edges of her wings are dark brown and underneath her tail is white but also patterned in spots of light brown. It's bright yellow eyes are framed by tan coloured feathers and elaborate spotted patterns throughout it's body. Her small hooked beck ranges from orange to dark brown and feet are a faded yellow.Swing tag: 28 / Merlin / Catalogue, page 6 / Other swing tag: 56 / Falco / Cesalon Metal tag: 4033 /taxidermy mount, taxidermy, animalia, burke museum, beechworth, australian museum, skin, bird, northern hemisphere, falcon, falco columberius, merlin, pigeon hawk

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

The Yellow-billed Spoonbill is a waterbird which can be commonly seen wading through shallow waters. This particular variety of Spoonbill is found across Australia, mostly in the northern and well-watered inland areas. It resides in freshwater wetlands, dams, lagoons and swamps. The species feeds on mainly aquatic insects and larvae. The bill has vibration detectors called papillae inside the spoon which enables the bird to feel the vibrations of its prey in murky water. These birds nest in the colonies of other birds like the Ibises and Royal Spoonbills. They live in high forks of trees over water or in reed beds. 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 Yellow-billed Spoonbill specimen is a large taxidermy of mainly white colouring. The bill is a large and unique spoon shape and is yellow. The long gangly legs and the skin on the face are also yellow. The eyes are made from a black and yellow glass and the bird is stylized standing on a square wooden platform. A paper identification tag is tied to the bird's upper left leg.6c. / [illegible] / Spoonbill / taxidermy mount, taxidermy, animalia, burke museum, beechworth, australian museum, skin, reynell eveleigh johns, bird, australian birds, spoonbill, yellow-billed spoonbill, yellow billed spoonbill, waterbird

Ilvaite has acquired its name from Ilva (Latin for Elba) Island, Greece, where Ilvaite is most commonly found. The geological setting in which Ilvaite occurs is through contact with magnetite, zinc and copper ore deposits, along with contact metamorphic deposits and zeolite zones. llvaite crystallizes in the form of black prismatic crystals and columns . This specimen was retrieved from Broken hill, known as the world's richest and largest zinc-lead ore deposit. Because of Ilvaite's often unaesthetic crystal formations compared to other minerals, Ilvaite is uncommon in most rock collections, particularly specimens that are not well formed, such as this one. Ilvaite is also a member of the Sorosilicate subclass of the silicate minerals, which have an unusual basic unit of Si2O7, making Ilvaite a unique mineral. Given that Ilvaite is not commonly found in Australia, it marks a unique contribution to an Australian collection of minerals. 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 ferrous iron analogue mineral with of black with shades of beige Ilvaite is a brittle, opaque rock formation that has acquired its name from Ilva (Latin for Elba) Island, Greece, where Ilvaite is most commonly found. The geological setting in which Ilvaite occurs is through contact with magnetite, zinc and copper ore deposits, along with contact metamorphic deposits and zeolite zones. llvaite crystallizes in the form of black prismatic crystals and columns rock, mineral, ilvaite, ilvaite specimen

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 was recovered from Wonthaggi in Victoria. Coal is a sedimentary rock which is composed of peat after it has been exposed over millions of years. This is an example of Australian black coal which is used as either thermal or coking coal for electricity generation or manufacturing processes. It is predominantly composed of Carbon which is 'C' on the periodic table of elements. This early example of a coal sample, shows the important role that coal played/plays in Australia's energy generation and manufacturing processes. 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.Small piece of black coal with museum original labelGeological survey / R..... S...../ Locality Cape Patterson coal specimen, burke museum, geological survey of victoria, geological specimen, geology

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 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

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

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

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

This cardbord box was used to package explosives which were used for mining. Black powder and dynamite were heavily used on the goldfields to blast away large sections of earth which. Explosives were stored at Beechworth Powder MagazineMining played an important role in the history of Beechworth, for the township was established in the mid-1850s after gold was discovered in the area. The success of goldmining lead to the growth and development of early Beechworth.A brown rectangular cardbord box with opening flaps at top and features printed text on sides and top.GLASGOW / THE PERFECT COMBINATION / NOBEL-GLASGOW EXPLOSIVES / NOBEL-GLASGOW DETONATORSburke museum, beechworth, mining, explosives

These protective over-boots were compulsorily worn in the Powder Magazine so as not to induce static electricity.The Beechworth Powder Magazine was constructed in 1859, and was used as a storage room for large amounts of black-powder used in mining and quarrying. By law, miners were required to leave bulk black-powder in this building overnight.Pair of brown over-boots. Large, lighter leather foot with polished harder leather back and sole, stitched at sides, four lace holes. Stitched leather insole and pull tab at back.burke museum, beechworth, mining, powder magazine, footware

Orbost Aero Club began in 1969 with Basil Dowie as Chair, David Nixon as Secretary/Treasurer. The group went into recess from 1977-1991 closing in 1997. The mid 1960s were boom years in flying training in Australia and the number of Aero Clubs grew rapidly. The Club played a significant role in the establishment of the small airport at Marlo and in the ongoing operation and development of the airport over the years particularly for patient transfer by aerial ambulance. The Orbost Aero Club Club played a significant role in the establishment of the small airport at Marlo and in the ongoing operation and development of the airport over the years.A buff coloured rectangular shaped cardboard box which contained badges for the Orbost Aero Club. The sides are stapled and the lid has a finger opening, written in blue pen on the lid is Orbost Aero Club Big Wings and Large$10.00 Small $2.00.Top in black print - STOKES (Australasia) Ltd METALWARE DIVISION MANUFACTURERS OF BADGES BUTTONS AND MEDALLIONS SINCE 1856 322-332 ALBERT STREET BRUNSWICK VICTORIA AUSTRALIA TEL 382101 orbost-aero-club

This special issue was produced in conjunction with the coronation of Queen Elizabeth 11.On the 2nd June 1953, the coronation of Queen Elizabeth II took place and the commonwealth countries, including Australia joined in the celebration.A large magazine. The cover has a red background with a large picture of the royal coat of arms and regalia. The title is in blue print at the top. At the foot is CORONATION WEEK DOUBLE in blue print. In smaller black print is Cost 4/-.royalty coronation queen-elizabeth-11 magazine-illustrated-london-news ingram-bruce

In the early 1950's Lionel Nowlan had a Hairdresser & Billiard Room in Nicholson Street (where the Caltex Service Station stands today). A circulating library is a small library with books lent for a small fee to subscribers and was often inside an existing business. Circulating libraries were common before a more substantial local library was established. Circulating libraries offered an alternative to the large number of readers who could not afford the price of new books in the nineteenth century but also wanted new material. Circulating libraries rented out bestsellers in large numbers, allowing publishers and authors to increase their readership and increase their earnings. They were also profitable for those businesses that established them. Nowlan's, Marshall's and McCoys were circulating libraries which operated in Orbost in the first half of the 20th century.Circulating libraries offered an alternative to the large number of readers who could not afford the price of new books in the nineteenth century but also wanted new material. It was common for them to stock the latest novels.A red cloth covered hard back book with a repaired black spine. It is titled "The Cost of a Promise" and is a novel in Three Parts by Mrs Baille Reynolds.Stamped on some pages - McCoy's Circulating Library On inside front cover - No 249 Contains a sticker for Nowlan's Library Orbost Stamped - Marshall's Circulating Library McCoy's Circulating Librarythe-cost-of-a-promise reynolds-baillie libraries-orbost circulating-libraries

These two albums were used at the Slab Hut - Orbost Visitor Information Centre. The Orbost Visitor Information Centre is situated in Forest Park on Nicholson Street. The centre is housed in the historic Slab Hut. The hut was an original family dwelling built in 1872, on a site approximately three kilometres upstream from the junction of the Buchan and Snowy Rivers. No nails were used in the construction; it was all wired together. After a period in storage the slab hut was opened in its present location in Orbost as the Information Centre in 1987.These albums are contemporary records of the construction and relocation of an iconic Orbost building, the Slab Hut.Two large photo albums. 2280.1 has no front cover. The back cover and spine are red. The pages are black and most photos are labelled. They are photographs of the Orbost area. 2280.2 has brown covers. It contains photographs of the construction of the gardens and buildings around the Slab Hut (Orbost Visitor Information Centre). On the cover in gold print is "PHOTOS".slab-hut-orbost album-photographs-orbost

The Gippsland Institute of Advanced Education was established in September 1968. On its establishment, the institute assumed responsibility for the diploma courses previously offered by the Yallourn Technical College which had commenced diploma teaching in 1929. Initially, all the Institute's teaching was conducted in the diploma building of the Yallourn Technical College. In 1972 the Institute transferred part of its operations to the first of its permanent buildings on a large campus in rural surrounds near the township of Churchill south of Morwell. The Gippsland Institute of Advanced Education was opened on 20 November 1976. This book is a useful reference book for research into the history and establishment of Gippsland.A 232 pp plastic-covered soft covered book, The front cover is beige with the title, " Gippsland An Annotated Bibliography to 1980 C.W. Tolley" in black print at the top. In the middle is a black/white print detail from a lithograph of Bairnsdale Advertiser office in 1888. At the foot in black print is "Centre For Gippsland Studies". The book contains a list of books relating to the local social history , agriculture, indigenous, planning and resources . book-bibliography-gippsland gippsland-institute-of-advanced-education

Robert Pullar Cameron was a Shire Councillor for many years. He married Penuel Hossack and had a family of James, Flora, Penuel and Alex. Peter Kerr bought the butchery from William Cumming in 1921.This is an example of a hand-written account from an early Orbost business and is a useful research tool.A white paper account with black print, red lines and handwritten pencil information. It has a yellow duty stamp and a large pink receipt sticker.cameron-robert-pullar kerr-p.c.-butcher account

In 1924 Harry Baughurst, a returned WW1 soldier, in partnership with Mr Hefford, purchased a grocery and ironmonger business in Orbost. It was situated on the corner of Nicholson and Tarra Streets, Orbost. When Mr Hefford left the district two years later , Harry Baughurst purchased and managed the business. In 1927 Baughurst formed a partnership with Robert Gall And Herbert & Co.to form the United Bread Supply Company so that they could purchase flours etc in bulk and therefore sell bread products more cheaply.This item is an exam ple of the book-keeping of an Orbost business in the early 20th century. It is a useful research tool.A large white paper account with blue lines and handwritten black text from H. Baughurst to R.P. Cameron. There is a pink receipt with a yellow duty stamp from Baughurst & Hefford. baughurst-harry account book-keeping cameron-r.p.

Robert Pullar Cameron was a Shire Councillor for many years. He married Penuel Hossack and had a family of James, Flora, Penuel and Alex.This item is an example of the book-keeping of a n Orbost business in the early 20th century. It is a useful research tool.A large white paper account with black print and red lines from W.J. Mierisch, grocer and general merchant, to R. Cameron. There is a green duty stamp.mierisch-w.j. cameron-robert-pullar orbost-supply-stores

Robert Pullar Cameron was a Shire Councillor for many years. He married Penuel Hossack and had a family of James, Flora, Penuel and Alex.This item is an example of the book-keeping of an early 20th century business and is a useful research tool.A large white paper account with black print and red lines from Feely & Co., saddlers and harness makers for R. Cameron.feely-&-co. cameron-robert-pullar

"The History of Australasia" by David Blair was one of three important publications of the author. Written in 1879, the book relates the history of both Australia and New Zealand from their discovery through to the establishment of self-government in both colonies. Blair was born in Ireland and after studying for the ministry in Ireland came to Australia in 1850. Instead of a missionary career he took up journalism, became a member of the Legislative Assembly in Victoria and published his books on Australasia.A large thick hard leather covered book -History of Australasia by David Blair and published in 1879. The covers are black with a gold pattern border. The front cover shows an embossed Australian crest in gilt with kangaroo and emu and ' Advance Australia'. It is an illustrated edition with beautifully coloured maps for each Australian colony and New Zealand.book blair-david history-australasia

A handmade pink rayon crocheted pincushion. It is circular with two circular pieces - one large, one small - to resemble a hat. The top section is to be padded. It is threaded with pink ribbon. Two hatpins have been stuck unto it. One has a white pearl knob and the other a black pearl knob.

Wedel is the oldest chocolate brand in Poland. It has been operating for over 160 years. Beginning with Karol Ernest Wedel, his son, Emil and followed by Jan Wedel the Wedel family waswell known for its social welfare policies. During WW11 Jan Wedel refused to collaborate with the the German government leading to persecution of his employees and his family. Although the company has been taken over several times by larger international groups, the Wedel name remains part of the product.A large tin container which held confectionery. The front of the tin has a black background , decorated with yellow,blue and red stars. In the centre is the Wedel logo, a signature on a yellow oval background.on front - E. Wedel Rolimpex Made in Poland, Warsaw Sole exportercontainer e-wedel confectionery