One of a series of photographs taken after refurbishment of Museum, during "On Fire" exhibition.Colour photograph of the interior of the Home Economics room of the Common School Museum, featuring a display of photographsOn back of photo: "7 Historical Society. Fire photos. 20/6/03"on fire display, common school museum

One of a series of photographs taken after refurbishment of Museum, during "On Fire" exhibition.Colour photograph of the interior of the Home Economics room of the Common School Museum, featuring a display of photographsOn back of photo: "6 Historical Society. Fire photos. 20/6/03"on fire display, common school museum

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

Agate occurs when amygdales (gas pockets) form in the upper levels of basaltic lava flows. If these pockets or bubbles are iniltrated by water bearing silica in solution, the fluid dries and hardens in layers, forming round or egg shaped nodules or geodes within the rocky matrix. Agate is formed of a silica mineral chalcedony similar to quartz. Although relatively common and semi-precious, agate has been prized since at least 1450 BC - an intricately carved agate seal was found in the 2015 excavation of a grave belonging to a Mycenaeum priest or warrior near Pylos in Greece. Agate is also used in jewellery and other decorative or ritual purposes due to its often striking appearance. These specimens originated in North Queensland, which contains noted agate-fossicking regions such as in the area surrounding Forsayth. They were collected in approximately 1852 as an adjunct to the Geological Survey of Victoria. It was donated to the Museum in 1868. Victoria and other regions of Australia were surveyed for sites of potential mineral wealth throughout the 19th Century. The identification of sites containing valuable commodities such as gold, iron ore and gemstones in a locality had the potential to shape the development and history of communities and industries in the area. The discovery of gold in Victoria, for instance, had a significant influence on the development of the area now known as 'the goldfields', including Beechworth; the city of Melbourne and Victoria as a whole. The specimens are significant as examples of surveying activity undertaken to assess and direct the development of the mineral resource industries in Victoria and Australia, as well as the movement to expand human knowledge of earth sciences such as mineralogy and geology in the nineteenth century. Two solid egg-sized pieces of peach/orange toned agate (a common semi-precious chalcedony, similar to quartz) with a striped pattern, embedded in a light and dark brown matrix. geological specimen, geology, geology collection, burke museum, beechworth, agate, north queensland agate, 1852 geological survey of victoria, l. hufer - donor, mineralogy, agate specimen, indigo shire

This bottle was used in the Tawonga District General Hospital which was built in the 1950's specifically for the increase in population due to the Kiewa Hydro Scheme.Clear glass bottle with straight sides tapering in to a short thin neck with a screw top.Base: Top - Common Seal; Middle 'J835'; Bottom 'M'medical, hospital, chemist

This jar was used in the Tawonga District General Hospital which was built in the 11950's specifically for the increase in population due to the Kiewa Hydro Scheme.Small wide white 'milk glass' jar with screw top. Used for ointment e.g.. zinc, magnesium sulphate. Embossed on base. Base is 'pushed inwards/upwards' forming a lip around the circumference.Base: Common Seal - A with G above and M below / 15 medical, hospital, ointment

The inscription in the brick was made by Lanzinger a German internee who escaped several times from Camp 1, recaptured and placed in Camp 4 gaol. The brick was recovered by the Stanhope Museum, where it is now on display. The curator of the Museum contacted Tatura Museum for information about Lanzinger, and was advised that Lanzinger's daughter ( Ann Flegel) had visited Tatura Museum and Camp 1, from Canada. A photo of the brick was forwarded from Stanhope to Flegels, who in turn forwarded it to Josef Friedrich whom she had made contact with through the Tatura Museum. Friedrich then forwarded a copy of the photo to Tatura Museum.Colour photo of common red brick with inscriptions carved by and named Lanzinger, a date in 1941,and two swastikas.lanzinger escape, camp 1, camp 4 gaol, photography, photograph, slides, film

Small black leather case containing black leather covered hymn book and common prayer book.books, religion

One of a series of photographs taken after refurbishment of Museum.Colour photograph of the interior of the Home Economics room of the Common School Museum, facing the north-east corner.On back of photo: "19 Historical Society. New floor & painted room. 21/9/03"common school museum

Colour photograph of pupils seated at desks, being instructed by teacher, in the school room of the Common School Museum.rutherglen primary school, school pupils, reenactment, rutherglen common school

Colour photograph of pupils seated at desks, being instructed by teacher, in the school room of the Common School Museum.rutherglen primary school, school pupils, reenactment, rutherglen common school

Colour photograph of the front of the Rutherglen Common School Museum with a man walking down the driveway toward Murray StreetOn back of photo: "Taken by Barry Hill on 2-3-1997. Henry Pleming walking out."henry pleming, rutherglen common school, common school museum

Colour photograph of children in Rutherglen Primary School uniforms, seated at desks in the school room of the Common School Museum.rutherglen primary school, school pupils, reenactment, rutherglen common school

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

The Common buzzard, a medium-sized raptor, is found across Europe and Asia, and in Africa in the winter months. It is the UK’s commonest bird of prey, found in nearly every county. Due to their large size and their brown color, they are often confused with other species, especially the Red kite and the Golden eagle. They may look the same from a distance, but the Common buzzard has a very distinctive call, like a cat’s mew, and a distinctive flying shape. When soaring and gliding, the tail is fanned and its wings are often held in a shallow 'V'. The colour of individuals varies from dark brown to much lighter, though they all have a finely barred tail and dark wingtips. This species occurs across Europe and Russia, and parts of Northern Africa and Asia in the cooler winter months. It lives in a range of habitats, especially woodland, moorland, pasture, scrub, arable land, marsh bog, villages, and sometimes towns and cities. This particular specimen has been mounted in a correct stylised fashion. 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 Common Buzzard is brown in colour with lighter markings on the chest. It has a white patch of feathers on the back of its head and it has darker wingtips and yellow feet. This specimen stands upon a wooden platform and has an identification tag tied around its leg.Swing tag: 30 / Buzzard / Catalogue page 52. / Metal tag: 4043 /taxidermy mount, taxidermy, animalia, burke museum, beechworth, australian museum, skin, reynell eveleigh johns, bird, common buzzard, bird of prey

Cover is navy blue with the title and author on the spine in gold lettering.non-fictionThe Parson's Handbook contains practical directions both for parsons and others as to the management of the parish church and it's services according to the Anglican use, as set forth in the book of common prayer.parsons, parish church, management, services, anglican, common prayer

When Ballarat Junior Technical School building was opened in 1921, there was little cleared space for the students to use for sporting activities. The area known as Battery Paddock was used for dodge-ball and football. Gradually the slope area was cleared and planted. In November 1922 a tennis court was opened in the Battery Paddock. It was designed and built by two former students of the Ballarat School of Mines. The old Mount Doran school house was moved to the area as a students' common room. A new tennis court was built in the same vicinity in 1934. This area was on the corner of Grant and Albert Streets. Area is where the Corbould Building and the Automotive Skills Centre of School of Mines Ballarat Grant Street Campus now stand. Black and white photograph of the tennis court built in 1934 at Ballarat Junior Technical School. Gaol wall to the left and the old Mount Doran school house that was moved to the school grounds in 1922 and used as a Students' common room. Four students playing tennis with others watching.Stamp on back indicating photographer - "Richards & Co - Ballarat"ballarat junior technical school, student, 1921, battery paddock, ballarat school of mines, ballarat school of mines tennis court, mount doran, students' common room, 1934, grant street, albert street, corbould building, automotive skills centre, student activities

Detailed description of plants, one plant per page. Alphabetical listing according to botanical name, with common names provided.Maps, colour photographs, pronunciation guide, glossarygrassland, plants, south-eastern australia, botany, ecology

One of a series of photographs taken after refurbishment of Museum.Colour photograph of part of the 'weights & measures' collection displayed in the old fireplace of the Home Economics Room of the Common School MuseumOn back of photo: "21 Historical Society. New floor & painted room. 21/9/03"common school museum

In 1958 Robin Boyd was elected a Fellow of the The Royal Australian Institute of Architects.Certificate from The Royal Australian Institute of Architects, with common seal, stating that Robin Boyd has been elected Fellow on 27th June 1958. It is signed by the President, Wilfred Thomas Haslam, and Hon. Secretary, Allan E Stafford. Certificate is registered No 2008. There are pin marks at each of the corners.The Royal Australian Institute of Architects. This is to certify that Robin Gerard Penleigh Boyd of Melbourne, Victoria has been elected Fellow of the Royal Australian Institute of Architects, founded in the year of our Lord One Thousand Nine Hundred and Twenty Nine (1929) as The Australian Institute of Architects, and incorporated in the year of our Lord One Thousand Nine Hundred and Thirty as Royal Australian Institute of Architects for the Advancement, Protection, and Elevation of Architecture. In Witness whereof the Common Seal has been hereunto affixed as required under the Articles of Association this Twenty-seventh day of June, 1958. Signed by the President and Hon Secretary.royal australian institute of architects, fellow, raia fellow, robin boyd

Born 3rd June 1922 in Surrey Hills, Norman documents his life as it revolved around Surrey Hills and Box Hill. He went to Surrey Hills State School and later, after the war he became a postman at Box Hill Post Office. Some notes have been documents by specific years. The Addendum documents the common lifestyles of the day.Born 3rd June 1922 in Surrey Hills, Norman documents his life as it revolved around Surrey Hills and Box Hill. He went to Surrey Hills State School and later, after the war he became a postman at Box Hill Post Office. Some notes have been documents by specific years. The Addendum documents the common lifestyles of the day.shepherd street, presbyterian church, (mr) - woolford, surrey hills, schools, (mr) - fury, webb's dairy, surrey hills state school, (mr) - pola, (mr) - bevan, verona street, postmasters, (mrs) - webb, box hill south, box hill post office, churches, world war, 1939-1945, (mr) norman bruce kerr

Programme, sample invitation, newspaper clippings and photograph relating to the official opening of the school's administration building, staff offices and common room.Newspaper clipping extract: "The Minister for Education, Ms Hogg, has officially opened the Norwood High School - 30 years after it started teaching students. The Minister was about to open the School;s new administration block, completed at a cost of $830,000, when she discovered the school had never been officially opened."

The booklet was prepared by Safety Publishing Services in collaboration with the Department of Health Victoria, and issued with the approval of the Minister of Health. E.P. Cameron M.L.C. was the Minister of Health.26 page booklet. 10 pages with insturcions on prevention and action of common accidents in the home. The last 16 pages are advertisements for business.prevention of home accidents, health, children, first aid

According to the 1912 Department of Mines Bulletin of the Geological Survey of Victoria, basalt covers a considerable portion of the Macedon area including Mount Macedon. Basalt is the most common form of rock underlying the earth's surface and is found in three kinds of rock forming environments: ocean divergent boundaries, oceanic hotspots, and mantle plumes and hotspots beneath continents.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 mass, geological specimen in shades of grey and white. Hyalite is a colourless variety of opal. It occurs as globular and botryoidal masses and irregular crusts in volcanic and pegmatite environments where the silica deposits from the gas phase. Basalt is dark in colour, fine-grained igneous rock composed of plagioclase and pyroxene minerals. It is commonly formed as an extrusive rock, such as lava flow. It is one of the most common forms of rock underlying the earth's surface.burke museum, geological specimen, department of mines, geological survey of victoria, basalt, mount macedon, beechworth