This set of mustard and honeycomb coloured cushions (items F088-F092 and F099-F103) are located on Penleigh and Suzy's beds in the east facing back rooms of the Children's Pavilion.Solid mustard cotton fabric with concealed zip and pipingwalsh st furnishings, robin boyd

This set of mustard and honeycomb coloured cushions (items F088-F092 and F099-F103) are located on Penleigh and Suzy's beds in the back east facing rooms of the Children's Pavilion.Solid mustard cotton fabric with concealed zip and pipingwalsh st furnishings, robin boyd

This set of mustard and honeycomb coloured cushions (items F088-F092 and F099-F103) are located on Penleigh and Suzy's beds in the back east facing rooms of the Children's Pavilion.Solid mustard cotton fabric with concealed zip and pipingwalsh st furnishings, robin boyd

No specific information is available for this object. However, fountain pens originated in France in 1827, with the first patent attributed to a Parisian student named Romanian Petrache Poenaru. The fountain pen typically has a fine stainless-steel tip that is filled with ink via an ink well. Widespread production of fountain pens occurred from 1857, with new designs having improved filling techniques. Fountain pens became popular with professionals, such as barristers, professors, doctors, and accountants for over 100 years. The only downside to using fountain pens was their tendency to sometimes leak onto documents, so in the 1950s, they were made with disposable cartridges. The cartridges made the pens more popular, especially with university students. For this reason, in the early 1960s, fountain pens were renamed cartridge pens and were deemed the best writing instrument in most schools.This object is an example of the use of fountain pens in domestic households and professional workplaces since 1827.A solid and complete green and gold patterned fountain pen.There is green shimmer-like decorative patterning on the body with gold-coloured veining.pen, fountain pen, ink, france, chiltern athenaeum museum, victoria

Ùsed for engineering purposes possibly mining.Brown painted solid metal mortar and a separate pestle.mining, crushing & milling, medicine, pharmacy

Wreath laying ceremony for Legacy widows at the Cenotaph at the Shrine of Remembrance. This is an annual event for Legacy widows at the start of Legacy Week, which is the first week in September. Photo shows a widow with a wreath and a member of the Defence Force near the Cenotaph. Her badge reads 'President' - Joyce Cleaves was president of the ILLC (Intermediate Legacy Ladies Club). She laid a floral wreath at the Cenotaph in 2000 (see 00525) - this may be the same year.A record of a ceremony at the Shrine.Colour photo of Joyce Cleaves of the ILLC and a solider at the Shrine.Printing on the back "widows, widows' sunday, pilgrimage, wreath laying ceremony, illc

Imported and retailed by Holden and Frost for military and civilian use on saddlery during the 19th and 20th centuries Sold by Holden and Frost for military and agriculture use c1900Solid brass swedge buckle used as equine accessoryequine, military, agriculture, civilian c1900, swedge buckle

Heidelberg Golf Club members' tie with logo.One of a collection of various HGC members' ties.Solid navy necktie with letters "HGC" embroidered in gold.Manufacturer's tag on back of tie: "Tee Dee Made in Australia", "100% polyester"heidelberg golf club, memorabilia, vic mcgavin, neckties, club ties

Round white willow polo ball imported by Holden and FrostImported by Holden and FrostWhite round solid ball as used in equestrian sportMade in England Chas Meurisse and Co Chicago Willowhorse, polo, ball

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

Satchels such as these were commonly used by young boys to carry their lunch and school items between school and home. They were used commonly in the days when much of the requirements such as slates and paper were used as class sets. They proved to be serviceable and required only the most basic of maintenace as in stitching, to be kept in good order. Being adjustable they would also serve a student for a number of years.No information is available on Henry Alexander Cain of Surrey Hills.A common item with which many people would identify.Brown leather rectanular satchel with gusset on either side . It is fastened on the front with two metal buckles and has four adjustable leather back straps attached to the bag with metal studs. These are adjustable through holes in the leather straps. Likewise the front straps can be fastened in a number of different holes. The leather has an overall snake skin pattern.Solid leather is stamped in the leather on the front. henry Alexander Cain ******Rd Surrey Hillswarrnambool, school history, boy's school bag

Brown Coal is typically found as rocks. During formation the Brown Coal starts as peats, which is an acidic brown deposit resembling soil, and over time when subjected to pressure and heat these peats form the Coal. Brown Coal is the lowest rank of coal as it has a low carbon (energy) content, and a high moisture content. This high moisture content makes Brown Coal unsuitable for overseas exports. This particular specimen was recovered from the Yallourn Mine in Latrobe Valley, Victoria as part of the geological survey of Victoria being carried out by Alfred Selwyn. Otherwise known as the 'Yallourn Power Station', the Yallourn Mine is Australia's second largest mine. Yallourn Mine was first built in 1920, and since then it has been providing over 1 billion tonnes of Brown Coal to Australia every year. The Yallourn Mine is responsible for 22% of Victoria's electricity and 8% of Australia's electricity. As of 2021 the mine employs around 500 people. Due to ongoing maintenance issues and Australia's move to cleaner energy, the Yallourn Mine intends to shut down permanently as of 2028. Soon after gold was discovered in 1851, Victoria’s Governor La Trobe wrote to the Colonial Office in London, urging ‘the propriety of selecting and appointing as Mineral Surveyor for this Colony a gentleman possessed of the requisite qualifications and acquaintance with geological science and phenomena’. Alfred Selwyn was appointed geological surveyor in Australia in 1852 which began the Geological Survey of Victoria. In 1853-69 the Geological Survey issued under Selwyn's direction sixty-one geological maps and numerous reports; they were of such high standard that a writer in the Quarterly Journal of the Geological Society of London bracketed the survey with that of the United States of America as the best in the world. During his years spent in Australia, Selwyn collected numerous significant geological specimens, examples of which are held in collections such as the Burke Museum.Brown coal is considered to be an essential rock to Australia's energy consumption. Although plentiful in sources, Brown Coal is not able to be exported overseas due to its high moisture content. As Australia moves towards cleaner energy, Brown Coal is going become less used. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A solid hand-sized sedimentary rock that is a dark shade of brown.13 / BROWN COAL / Showing Woody structure / Locality: Yallourn, Vic. | Label probably / correct but / can't find reference / no. 13 to match in / registers. / C Willman / 15/4/21burke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, mineralogy, yallourn, yallourn mine, victoria, coal, brown coal, brown coal specimen, alfred selwyn, geological survey of victoria, geological survey, yallourn power station

Small statuette of kneeling soldier Vietnam, with M60, solid brassmodel, vietnam

Most likely collected and donated by Dr Frank ForsterBlunt hook with solid, turned mahogany handle. Unknown manufacturer.obstetric delivery, blunt hook, destructive instrument

Photograph of 6 bearded soliders in jungle greens armed with SLR'sphotograph, slr, jungle greens

Olivine is mostly found on the Earth's surface in igneous rocks that are dark-coloured. It is common at divergent plate boundaries and at warm spots, such as volcanic areas. It crystalises and forms during the cooling of magma. Olivine is used in refractory sand, bricks, and gemstones. Olivine has been found on a number of meteorites, which might have originated from large asteroids or the mantle of a now-destroyed planet. This olivine crystal is thought to originate from Mount Noorat, with speculation that it could have originated from Mount Shadwell. Mount Noorat is a dormant volcano cone located in the Newer Volcanics Province of Victoria. Mount Noorat belongs to the Kirrae Wuurong people, who used the Mount as a place for meetings and gatherings prior to European settlement. Contact was first made between European settlers and the Indigenous people in 1841. The Mount has mostly been used for cattle and sheep grazing. Mount Shadwell is a well-known source of olivine and is the highest of a gathering of volcanic cones. The New Volcanic Province is located in South East Australia and covers 15000 square kilometres. It contains 400 explosive vents and small shield volcanoes. The last eruption is thought to have occurred 5000 years ago at Mount Gambier and Mount Schank. This olivine crystal has been identified as a volcanic bomb, which is a molten rock which was pushed out and ejected into the air when a volcano reupts. A rock needs to be larger than 65 mm in diameter to be classified as a volcanic bomb. This olivine volcanic bomb and its locality is historically and socially significant. The olivine was found in the Newer Volcanic Province, an area which contains over 400 dormant volcanoes. This olivine is one part of a volcanic bomb, which would have ejected when magma erupted out of a volcano. 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 iron-magnesium silicate mineral with shades of green and brownburke museum, beechworth, geological, geological specimen, olivine, igneous rock, volcanic, gemstones, volcanic bomb, meteorites, asteroids, plantes, mount noorat, mount shadwell, indigenous, kirrae wuurong people, newer volcanics province, victoria, european settlement, eruption

Scarifiers were traditionally used for blood letting, and in folk medicine for the practice of cupping. Spring loaded knives cut the skin, then a warmed metal or glass cup is placed over the cuts. As the air inside the cup cools, it creates a vacuum drawing out the "bad" blood. The process is also related to the ancient medical theory of "humors". This theory dates back to the Hippocratic tradition and persisted through to the mid-19th Century. According to this theory, the body had four "humors", "airs" or "elements" which neeed to be kept in balance. Any imbalance could cause illness and this was often explained in terms of excess fluids. One prescribed treatment was to remove the excess blood which would restore the balance.Square, solid brass object with lever to release blades underneath.Etched on side: Mundy / Londonmetal, blades, bloodletting

Azurite is a secondary copper mineral made by the weathering of copper sulphide ore deposits. Azurite is formed from copper, carbon, oxygen and hydrogen. There are over 45 forms of azurite that are more well-known, however over 100 forms have been found. Azurite is also commonly found together with Malachite, and Azurite is often psuedomorphed to Malachite. This specimen was found at the Great Cobar Copper Mine in New South Wales, which was founded in 1870. At the time it was one of the largest mining operations in the world. It was the largest copper mine in Australia and housed the southern hemisphere’s tallest chimney stack. The international price of copper collapsed at the end of World War 1 which led to the closure of the Great Cobar Mine on March 16th 1919. A year later on March 10th 1920 an underground fire in the CSA (Cornish, Scottish, Australian) mine started and burned for 16 years. The closure of the mine and the fire left thousands jobless and many people left the area. These were factors in Cobar facing a long stretch of poverty, until a boom in the 1960s led to the reopening of the mine. The mine still operates today, obtained by Metals Acquisition Limited in June 2023. Azurite is considered an uncommon mineral. Named for its deep blue colour, azurite was historically used for pigment making and as a gemstone, despite its softness. This specimen was donated to the Burke Museum between 1868-1880 as part of a larger collection of geological and mineral specimens. Many of the specimens in this collection were obtained as part of the Geological Survey of Victoria, which started in 1852. The Survey aimed to map the scientific makeup of the earth.A solid copper mineral with shades of darker blues almost covering it.burke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, mineralogy, cobar mines, great cobar copper mine, cobar mining, new south wales, azurite, azurite specimen

Chert is a sedimentary rock composed of microcrystalline or cryptocrystalline quartz. While usually biological in origin, chert may also occur as a chemical precipitate or a diagenetic replacement--the product of petrified trees. Chert, also known as flint, was a common tool for early peoples during the stone age. It forms in limestone and chalk sediments as silicon dioxide microcrystals which grow into nodules of chert. Chert is found in many mines across the Northern Territory, however this specimen is sourced from the Mount Todd gold mine in Katherine. Its use in weaponry, both during the Stone Age and during the 18th century. Chert produces a spark when struck against steel, meaning t hat it can be used to start fires and fire guns. Chert was thus used in flintlock firearms, in which the gunpowder is ignited by a flint hammer striking a steel plate. Chert was commonly used in the Stone Age as a result of conchoidal fracturing causing very sharp edges, allowing early peoples to fashion weapons and cutting tools. It also rates a 7 on the Mohs Scale, making it a very hard and durable stone that maintains its sharpness. As a result, the significance of chert as a signifier of early indigenous Australian life makes this specimen important. It is also known that chert is a valuable mineral that was used as a trading commodity. Chert has also been valuable during the 1700s, proving itself to a be an important historical specimen in matters of war. A solid silicon dioxide mineral in shades of brown, white, and beigeburke museum, northern territory, chert, flint, minerals, geological specimen, katherine, mount todd gold mine, katherine northern territory

In conversation with Mr Tibbett we found out that he obtained this particular unit at an auction in Sydney and brought it home with the intention of one day getting it going again. 'One day' never seemed to come, so he decided to let us have it for our display, rather than jjust collecting dust in his shed.This unit is again of a different manufacturer and construction, highlighting the versatile nature of charcoal producer gas and its applications. A commercially made cast iron unit with a solid round hopper/boiler on a steelframe base. It has a pressure-cooker lid and a car type radiator. Solid built, but rust affected in partsMake: Tysons Cross Draught Model: Official 30hp Heavy Duty Serial: 1368

Sad irons, also called flat irons or smoothing irons, are shaped pieces of metal that are flat and polished on one side and have a handle attached to the other, created for the purpose of de-wrinkling fabric. “Sad” is an Old English word for “solid,” and the term “sad iron” is often used to distinguish the largest and heaviest of flat irons. They often had a trivet on which to rest the hot iron.Two triangular flat irons. They are made of solid cast iron with hollow iron handles. Flat irons (often referred to as sad irons) were heated on trivets in front of open fires, or on the tops of closed ranges, or on specially-designed iron stoves in larger laundries. They were made in numbered series which related to their size, although there was no standardisation in the series between manufacturers. these two are Salter brands. 1872.1 is a No 7 and 1872.2 is a No 8 and slightly heavier.Salter 7 Salter 6flat-iron sad-iron domestic-appliance laundry

A tool for shaping wood - to flatten/reduce the thickness of and leave a smooth surface on a rough piece of timber.ALEX MATHIESON & SON / WARRANTED (on guide) SOLID STEEL WARRANTED (on blade) Trademark crescent and starplane, tool

Printed cardboard container used to retail nickel plated 'best lills', which were small pins.4 oz nett / Dandy / Solid Headed Nickel Plated / Best Lills / Made in Australiadandy pty ltd, containers, pins

This is possibly part of an old gold stamping machine from the Club Terrace/Combienbar/Bendoc area. It could have been used in the gold mining industry between 1890-1920. (Information from Lachlan Macalister - 11/11/2013.)A heavy solid iron octagonal shaped weight. One side is concave.iron-weight gold-mining-processing

A middle school as such was recognised after the 1974 amalgamation but Middle School leaders were nopt appointed until 1998. Prior to this the school recognised homeroom leaders, SRC representatives and head students. Varnished solid wood board with two relief boards and gold lettering. middle-school, leaders, ballarat-and-clarendon-college,

This board honours a school's contribution to the annual Ballarat Girls School Association (B.G.S.A) athletics competitions. Clarendon Presbyterian Ladies' College won the accolade consistently from 1963 - 1970. paralleled the BPSA (Ballarat Public Schools Association) which morphed to become coed in the mid 70s, when College and Grammar became coed, retaining the BPSA acronym. BPSA became the present BAS. Varnished solid wood board with gold lettering and decorative top edging.clarendon-presbyterian-ladies-college, b-g-s-a, sport, honour-board, athletics,

Ring Auger, Solid Centre - Lead Screw. 62.5cmL 3cm diamflagstaff hill, warrnambool, shipwrecked-coast, flagstaff-hill, flagstaff-hill-maritime-museum, maritime-museum, shipwreck-coast, flagstaff-hill-maritime-village

Appears to be a 2nd AIF plaque which may have belonged to SGT Robert Henry Baxter.An item which refers to the 2nd Australian imperial force and WW2.Solid Brass plaque from mold, World War 2 era Plaque comprised of 2 areas(not parts) . Upper ,rising sun emblem marked "AUSTRALIAN COMMONWEALTH MILITARY FORCES" with the number 2 under the crown. Lower, with lettering "A.I.F" on top of a tin helmet. Back of plaque has no markings, is uneven from molding process and has not been filed to a smooth finish. rising sun badge, 2nd aif

Axe with long wooden handle and solid iron wedge-shaped head.No visible markingsrural industry, agriculture, axe, farm, iron, wood, chop/split