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The Beechworth Burke Museum
Geological specimen - Malachite in Conglomerate, Unknown
Malachite is a green copper carbonate hydroxide mineral and was one of the first ores used to make copper metal. Malachite has been utilised as a gemstone and sculptural material in the past as its distinctive green color does not fade when exposed to light or after long periods of time. Malachite is formed at shallow depths in the ground, in the oxidizing zone above copper deposits. The material has also been used as a pigment for painting throughout history. Malachite is considered a rare gemstone in that the original deposits for the stones have been depleted leaving behind very few sources. In addition, the use of Malachite as gemstones and sculptural materials remains just as popular today as they were throughout history. It is quite common to cut the stone into beads for jewellery. The fact that Malachite has such a rich colour and one that does not fade with time or when exposed to light makes it particularly rare. Although there is no indication available of the locality from which the specimen was sourced, it is likely that the specimen was collected either in South Australia in the vicinity of the Burra Burra mines or in Victoria as part of programs of geological surveying undertaken in the Nineteenth and Twentieth centuries. 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 copper carbonate hydroxide mineral with quartz pebbles in red conglomorate matrix presenting shades of cream, brown and green.Existing label: Malachite / (green) in / conglomerate / (white quartz / pebbles / in red matrix /geological specimen, geology, geology collection, burke museum, beechworth, geological, indigo shire, malachite, malachite specimen, australian mines, mines, geological survey, conglomorate, matrix -
The Beechworth Burke Museum
Geological specimen - Agate and Quartz pebbles
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. Quartz is found all over Australia, including Beechworth in Victoria. It is formed in deep-seated igneous rocks and crystallized through hot aqueous solutions. It can have two forms; Microcrystalline quartz or Crystalline quartz. Microcrystalline quartz is a fine grain quartz where crystalline quartz is often a large crystal. The colour of quartz can vary. These specimens were collected in Victoria in the vicinity of the Burke Museum. 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.Geological specimens of Agate and Quartz respectively; the fist-sized piece of Agate has peach/coral colouring with grey concentric patterning and the smaller piece of quartz is a uniform yellow/orange shade. Existing label: Local pebbles / (agate and / quartz / (yellowish) / egg-shaped). / BB geological specimen, geology, geology collection, burke museum, beechworth, agate, quartz, north-east victoria, indigo shire, geological surveys -
The Beechworth Burke Museum
Geological specimen - North Queensland Agates, Unknown
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 -
The Beechworth Burke Museum
Geological specimen - Galena (lead sulphide), Unknown
Galena occurs in a range of deposit contexts, often in metalliferous veins, such as Broken Hill, Australia; Coeur d’Alene, Idaho, United States.; Clausthal Zellerfeld, Germany; and Cornwall, England. Large deposits also replace limestone, dolomite, or occasionally organic matter, or have a contact-metamorphic origin. Galena is additionally found in cavities, brecciated (fractured) zones in limestone and chert, and in coal beds. This specimen was recovered from Broken Hill NSW and is 60% lead with 8-12 oz/silver to the ton.Galena or 'lead glance' is a grey lead sulfide and the chief ore mineral of lead. It forms isometric crystals in which the ionic lattice is similar to sodium chloride. Galena is brittle and easily weathers to secondary lead minerals, with the upper part of mineral deposits often containing cerussite, anglesite, and pyromorphite. It usually contains silver, which is mined along with its lead content. Other commercially important minerals that form in close association with galena are antimony, copper, and zinc. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A small-sized solid specimen containing one mineral with a sparkly silver metallic lustre exterior and pastel-grey interior.geological specimen, geology, geology collection, burke museum, beechworth, galena, lead sulphide, alfred selwyn, broken hill -
The Beechworth Burke Museum
Geological specimen - Anthracite crystal, Unknown
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 -
The Beechworth Burke Museum
Geological specimen - Common Opal, Unknown
It is not known where this opal originated. Common Opal is formed from silica-rich water entering the earths crust and hardening into a gel of water and silica-spheres, layered through the specimen. Common opal differs from precious opal in colouration and appearance, with precious opal including more colours, and having a translucent or glossy appearance, where common opal shows less colour and is typically opaque. It scores high on the Mohs hardness scale, and is common throughout the world, especially in Australia, where it is far more prevalent than the highly-prized precious opal. Australia is also the highest producer of opals in the modern world. 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, silica-based mineral specimen of Common Opal in shades of grey, green, and yellow, with a thick grey vein running through the centre. geological specimen, geology, geology collection, burke museum, beechworth, opal, common opal, gemstone, mining -
The Beechworth Burke Museum
Geological specimen - Selwynite, Unknown
Selwynite is a fine-grained, compact green rock made primarily of chromian muscovite (fuchsite) and diaspore. Corundum and fuchsite can occur together in the form of massive aggregates or nodules. Often, copper carbonates are found as earthy films or tiny crystals in joint planes. The mineral name honours the late A. R. C. Selwyn, founding Director of the Geological Survey of Victoria. The particular specimen, a mottled green stone suitable for carving was recovered and found in Heathcote, Victoria, Australia. The rarity and qualities of this mineral attracted commercial mining, which was not successful, but traces of the mine shafts still exist today, and it is still highly valued by mineral collectors.Selwynit is considered to be one of the rare forms of rock because it is composed of phosphate minerals containing zirconium. This is an extremely rare combination found in nature. 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 fine grained rock composed of mainly of chromian muscovite (fuchsite) diaspore and corundum.geological specimen, geology, geology collection, burke museum, beechworth, mineralogy, heathcote, mineral collectors, selwynite, green rock, rock specimen -
The Beechworth Burke Museum
Geological specimen - Marble, Unknown
A granular metamorphic rock, marble is derived from limestone or dolomite and composed of calcite or dolomite interlocking grains. Heat and pressure from overlying sediments form it from limestone buried deep in Earth's crust. Graphite, pyrite, quartz, mica, and iron oxides can affect rock texture and colour. This specimen was found in Carrara, Italy. Carrara marble is the most common marble found in Italy, and it gets its name from the region where it is located. The marble was also called Luna marble and was used as a decorative element in buildings and sculptures. It has been quarried since Roman times in the Lunigiana, the northernmost tip of Tuscany, just outside the city of Carrara in the province of Massa and Carrara.Marble is one of the most popular and expensive rocks used in sculpture, architecture, interior decorations, statues, table tops, and novelties. It is available in various colors and textures depending on the chemical composition. The strength of the rock and its ability to hold finer details have made it a favorite among designers. 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 Marble (metamorphic rock) predominantly white with specks light grey and ochre geological specimen, geology, geology collection, burke museum, beechworth, marble, carrara marble, italian marble, marble specimen, tuscany -
The Beechworth Burke Museum
Geological specimen - Bituminous Coal, Unknown
Bituminous coal is the most common type of coal, abundantly found in ancient coal deposits which can be dated back millions of years. Often referred to as soft or black coal, this specimen exhibits a high carbon content, ranging from 76-86%. It also holds a relatively high energy density (27 MJ/kg) meaning that it releases significant amounts of energy when burned. Bituminous coal is most commonly used for electricity generation, as well as in the production of steel. This particular piece of coal was collected as part of the Geological Survey of Victoria in the nineteenth century. It originates from Cape Paterson, a seaside village located in South Gippsland, Victoria (located on Bunurong Country). The discovery of bituminous coal in this locality was first made in 1826 by explorer William Hovell. More discoveries were gradually made over the following decades and in 1859 the Victorian Coal Company commenced the first active coal mining operations in the state by sinking a number of shafts and bores near the area of Cape Paterson. Evidence of this coal-focused past can be found today at the State Coal Mine Museum in the nearby town of Wonthaggi. This specimen is significant as it was collected from the locality of Cape Paterson in Victoria, an area that has since become historically instrumental in the mining of coal and other substances in the state of Victoria. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study. A solid hand-sized piece of bituminous coal with a shiny black-grey surface and jagged edges.Existing Label: BITUMINOUS COAL / Locality: Cape / Patterson, VIC. burke museum, beechworth, geological, geological specimen, state coal mine museum, wonthaggi coal mine, victorian coal company, bituminous coal, coal victoria, coal energy generation, william hovell, cape paterson, coal specimen -
The Beechworth Burke Museum
Geological specimen - Malachite, Unknown
Malachite is a copper carbonate hydroxide mineral. It has a chemical composition of Cu2(CO3)(OH)2. It often forms within limestone where a subsurface chemical environment favourable for the formation of carbonate minerals can occur. It is a substance that can be found in many different parts of the world including: Australia, USA, Russia and the Democratic Republic of Congo. Malachite has historically been used to produce copper, with mining of the mineral dating back over a period of four thousand years. Due to its beautiful green colourations, it is also commonly used for aesthetic purposes such as in the production of sculptures and jewellery. This particular specimen was collected from the town of Burra, South Australia as part of a geological survey undertaken during the nineteenth century. The locality (located on Ngadjuri Country) has a long history of mining, particularly in copper mining, as the area is rich in copper deposits. The first significant discovery of this was made in Burra (Burra Burra Mine) in 1845 and, at the time, the mine was the largest and richest of its kind in the world, producing nearly five percent of the total world copper output. This specimen is significant as it is considered to be a rare gemstone, as many of the original deposits for the stones are significantly depleted, leaving behind very few sources. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A solid palm-sized copper carbonate hydroxide mineral with patterns of green colourations Existing Label: MALACHITE / Locality: Burra / S. Aust. Other Label: Confirmed / as Malachite / C. Willman / 15/4/1 / + Bill Birch burke museum, beechworth, geological, geological specimen, malachite, gemstone, green gemstone, burra, burra burra mine, burra south australia, carbonate mineral, copper, copper mining, copper mining burra, carbonate hydroxide mineral, copper carbonate, malachite mining, malachite burra, monster mine -
The Beechworth Burke Museum
Geological specimen - Laterite
Laterite refers to both a rock and a soil type that is rich in clay, as well as Iron and Aluminium. It is created during a process that is called laterization, where high heat and seasonal heavy rainfall cause there to be wet and dry periods, which over time hardens the soil into rock. Because of this, most laterite is formed between tropics of Cancer and Capricorn. The iron oxide in laterite is what gives it it’s orange-red colouring. The largest religious complex in the world, Angkor Wat in Cambodia, is partially constructed of laterite, particularly its foundations, as laterite is porous and allows rainwater to drain. This specimen of laterite was collected from the Democratic Republic of Congo while it was colonised by Belgium in the 19th century. Laterite forms in many parts of the world, particularly between the tropics. It is used both for ore and as a building material, and comparing specimens from different parts of the world allows us to document the different compositions that this mineral can have when formed at different locations. 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 iron-aluminium oxide mineral specimen in shades of brown, orange and greyburke museum, beechworth, geological, geological specimen, laterite, laterite specimen, geology -
The Beechworth Burke Museum
Geological specimen - Montmorillonite
Montmorillonite is a type of clay composed of aluminium silicate that forms very small particles that are not well-bonded to one another. This is why it is so soft. When in the presence of water, all types of clay swell. Montmorillonite swells even more than most types of clay, which is why it is often chosen over other types of clay in its practical uses. Montmorillonite has many different practical uses, including in the mining industry, as a soil additive, as a sealant, as a desiccant to draw water out of the air, to clean ponds, to make kitty litter and in cosmetics. Montmorillonite is a common mineral and, despite being named after Montmorillon, France, can be found all over the world, including many deposits in Australia. It is not known where this particular specimen originates from. Montmorillonite is an economically and socially significant material with a wide variety of uses. Having samples of common and important minerals allows collections, like the Burke Museum, to have a more complete view of the land on which they are located, and therefore a more complete view of heritage. 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 tennis-ball sized chunk of aluminium silicate clay. It is primarily white, accented with orange and brown.burke museum, beechworth, geological, geological specimen, clay, montmorillonite -
The Beechworth Burke Museum
Geological specimen - Cassiterite
This specimen is Cassiterite in Quartz. Cassiterite is a tin oxide metal that forms in thin crystals which can have a beautiful lustre. Quartz is made of silicon dioxide, also known as silica, and is one of the most common minerals on earth. Cassiterite has been a fundamental source of tin ore for humans throughout history, including today. Tin is an important metal that has a wide variety of human uses in different areas, from dying fabric, to making mirrors, and their most well-known use ‘tin’ cans. Tin cans are primarily made of steel and are coated with tin in order to take advantage of tin’s property of being non-corroding. This is a massive step in the history of food preservation. Tinned food first reached Australia in 1815 with early settlers, and it began to be manufactured here in the 1840s. It was incredibly popular, and was a highly exported product, which would be a contributing factor to the ‘tin mining boom’ of the early 1880s. This specimen was collected at Jingellic, New South Wales, in about 1852. Although the Goldfields of the 1800s are much more well-known, tin mines existed alongside the gold mines which began in the mid 19th century and extended almost one hundred years, to the mid 20th century. Specimens like this would have been used as evidence to justify tin mining operations in the region as an investment. 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. The Geological Survey of Victoria was headed by British geologist, Alfred Richard Cecil Selwyn (1824-1902), who was responsible for issuing over 60 geological maps during his 17 years as director. These maps were all hand-drawn and coloured and became the benchmark for accuracy for geological mapping. 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 fist-sized solid geological specimen made on one half of tin oxide, which is dark grey, and on the other side of silica, which is brown and cream.burke museum, beechworth, geological, geological specimen -
The Beechworth Burke Museum
Geological specimen - Opal Bearing Stone, Unknown
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 -
The Beechworth Burke Museum
Geological specimen - Chiastolite
It is made up of andalusite. Andalusite is a rock-forming mineral, sometimes found in granite or schist. It is often used to make glass, ceramic products, chemicals, and heat-resistant bricks as it can withstand high temperatures without changing. The chiastolite contains particles of graphite, which arranges in geometric patterns. When crystal growth occurs in the rock, the granite particles concentrate at crystal interfaces and can result in cross shapes. These ‘cross stones’ have been valued and used for their spiritual or religious meaning and used as charms, gems, or amulets. Chiastolite was first discovered in 1754, seen in a description in a published book by a palaeontologist, Franciscan priest, and Spanish author, Jose Torrubia. Deposits have been found in Australia, France, the USA, Chile, Canada, Spain, Brazil, Sri Lanka, and Russia. Deposits have been found in Western Australia and South Australia. This particular specimen was found in Bimbowrie, South Australia. Other chiastolite specimens have been found in Bimbowrie, along with jasper, quartz, and aventurine in the form of rolled pebbles or schist. This chiastolite specimen is socially and historically significant. It is a very rare sort of andalusite mineral. It is from one of only two locations where it is regularly found in Australia. The carbon cross has made it an important religious symbol in the past. Its ability to withstand high temperatures has made it a common ingredient in heat-resistant bricks and ceramics today. 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 metamorphic mineral consisting of andalusite, with a cross shaped graphite pattern in colours of grey, brown and yellowburke museum, beechworth, geological, geological specimen, andalusite, chiastolite, geometric, cross stone, spiritual, religious, australia, south australia, bimbowrie, quartz, jasper, aventurine, schist -
The Beechworth Burke Museum
Geological specimen - Olivine with Chromian diopside (dark green), Unknown
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 -
The Beechworth Burke Museum
Photograph - Lantern Slide, c1900
This image shows a pathway in the gardens adjacent to Beechworth's Town Hall at the beginning of the Twentieth Century, around the time of Australia's Federation. The pathway leading to a circular rotunda or covered seating area with a steep conical roof is lined with shrubs set in grass verges that appear to be covered with snow. It is unknown whether the snowfall or a factor to do with the gardens occasioned the taking of the image, which at the time may have been an exotic practice. Climate records going back to 1908 indicate that snow in winter is not unusual due to Beechworth's elevation and orientation, and the Town Hall itself was built in 1859. Lantern slides, sometimes called 'magic lantern' slides, are glass plates on which an image has been secured for the purpose of projection. Glass slides were etched or hand-painted for this purpose from the Eighteenth Century but the process became more popular and accessible to the public with the development of photographic-emulsion slides used with a 'Magic Lantern' device in the mid-Nineteenth Century. Photographic lantern slides comprise a double-negative emulsion layer (forming a positive image) between thin glass plates that are bound together. A number of processes existed to form and bind the emulsion layer to the base plate, including the albumen, wet plate collodion, gelatine dry plate and woodburytype techniques. Lantern slides and magic lantern technologies are seen as foundational precursors to the development of modern photography and film-making techniques. This glass slide is significant because it provides insight into Beechworth's social amenities and climate in the early Twentieth Century, around the time of Australia's Federation into one nation. It is also an example of an early photographic and film-making technology in use in regional Victoria in the time period. Thin translucent sheet of glass with a circular image printed on the front and framed in a black backing. It is held together by metals strips to secure the edges of the slide.burke museum, beechworth, lantern slide, slide, glass slide, plate, burke museum collection, photograph, monochrome, town hall, town hall gardens, snow, rotunda, magic lantern, indigo shire, north-east victoria, nineteenth century, 1900s, twentieth century, emulsion slides -
The Beechworth Burke Museum
Photograph - Lantern Slide, c1900
This image shows the gorge adjacent to Beechworth in approximately 1900. Although the exact location of the photograph is yet to be determined, the present-day Beechworth Gorge Walk includes views of the Cascades at the point at which Spring Creek flows into the valley on the level below. Gold-sluicing techniques in use in the town during periods of active gold extraction may have altered the landscape since the photograph was taken, however. In the 1850s a mill was built at the top of the Spring Creek falls by Russian-born Louis Chevalier, brother of artist Nicholas Chevalier. The mill supplied the town with lumber that supported the town's initial construction boom. Lantern slides, sometimes called 'magic lantern' slides, are glass plates on which an image has been secured for the purpose of projection. Glass slides were etched or hand-painted for this purpose from the Eighteenth Century but the process became more popular and accessible to the public with the development of photographic-emulsion slides used with a 'Magic Lantern' device in the mid-Nineteenth Century. Photographic lantern slides comprise a double-negative emulsion layer (forming a positive image) between thin glass plates that are bound together. A number of processes existed to form and bind the emulsion layer to the base plate, including the albumen, wet plate collodion, gelatine dry plate and woodburytype techniques. Lantern slides and magic lantern technologies are seen as foundational precursors to the development of modern photography and film-making techniques.This glass slide is significant because it provides insight into Beechworth's built environment and natural landscape in the early Twentieth Century, around the time of Australia's Federation. It is also an example of an early photographic and film-making technology in use in regional Victoria in the time period.Thin translucent sheet of glass with a square image printed on the front and framed in a black backing. It is held together by metals strips to secure the edges of the slide.burke museum, beechworth, lantern slide, slide, glass slide, plate, burke museum collection, photograph, monochrome, indigo shire, north-east victoria, spring creek falls, beechworth gorge, louis chevalier, nicholas chevalier, lumber industry, timber industry, 1850s, construction, building, mill, mills, waterfall -
The Beechworth Burke Museum
Photograph - Lantern Slide, c1900
This image shows a semi-aerial view of a property along a river adjacent to Beechworth in approximately 1900. The photographer has capitalised words in the label, indicating that 'The Precipice' may have suggested a particular rather than a general vantage point to local people at the time. Although the exact location of the photograph is yet to be determined, Beechworth Gorge is popular today with hikers and nearby Mt Stanley is noted for its views. Lantern slides, sometimes called 'magic lantern' slides, are glass plates on which an image has been secured for the purpose of projection. Glass slides were etched or hand-painted for this purpose from the Eighteenth Century but the process became more popular and accessible to the public with the development of photographic-emulsion slides used with a 'Magic Lantern' device in the mid-Nineteenth Century. Photographic lantern slides comprise a double-negative emulsion layer (forming a positive image) between thin glass plates that are bound together. A number of processes existed to form and bind the emulsion layer to the base plate, including the albumen, wet plate collodion, gelatine dry plate and woodburytype techniques. Lantern slides and magic lantern technologies are seen as foundational precursors to the development of modern photography and film-making techniques.This glass slide is significant because it provides insight into Beechworth's built environment and natural landscape in the early Twentieth Century, around the time of Australia's Federation. It is also an example of an early photographic and film-making technology in use in regional Victoria in the time period.Thin translucent sheet of glass with a square image printed on the front and framed in a black backing. It is held together by metals strips to secure the edges of the slide.Obverse: Image from The Precipice. /burke museum, beechworth, lantern slide, slide, glass slide, plate, burke museum collection, photograph, monochrome, views, landscapes, farmsteads, rivers, beechworth gorge, mt stanley, emulsion, the precipice -
The Beechworth Burke Museum
Photograph - Lantern Slide, c1900
This image appears to show nurses at what is now the Mayday Hills Mental Asylum arriving for work in approximately 1900. These individuals are part of a long history of nursing in Beechworth. Three medical or social welfare facilities opened in the mid-1800s as part of a push by the township to become a regional centre for Government services. These were the Ovens District Hospital (opened in 1857), the Ovens Benevolent Asylum (opened in 1863), and the Beechworth Mental Hospital (opened in 1867 and renamed Mayday Hills Hospital at Centenary celebrations in 1967). It was recognised that the unsettled living conditions, poverty and relative isolation of the Goldfields environment could produce 'mental disturbances' which required local treatment facilities as services in Melbourne were too far away. Carole Woods' publication 'A Titan's Field' describes activities undertaken by patients at Beechworth Mental Hospital as including monthly balls and occasional concerts as well as work to make the facility self-supporting such as farm work and making clothes. She mentions a report in 1870 that the approximately 300 patients were clean and neat with 'no-one in restraint or seclusion' but that by 1905 the organisation had 623 patients which placed strain on building infrastructure such as heating and water supplies, leading to high turnover of nurses and other issues. A program of building works to extend and improve facilities followed over subsequent decades. Lantern slides, sometimes called 'magic lantern' slides, are glass plates on which an image has been secured for the purpose of projection. Glass slides were etched or hand-painted for this purpose from the Eighteenth Century but the process became more popular and accessible to the public with the development of photographic-emulsion slides used with a 'Magic Lantern' device in the mid-Nineteenth Century. Photographic lantern slides comprise a double-negative emulsion layer (forming a positive image) between thin glass plates that are bound together. A number of processes existed to form and bind the emulsion layer to the base plate, including the albumen, wet plate collodion, gelatine dry plate and Woodburytype techniques. Lantern slides and magic lantern technologies are seen as foundational precursors to the development of modern photography and film-making techniques This glass slide is significant because it provides insight into Beechworth's social and medical amenities in the early Twentieth Century, around the time of Australia's Federation into one nation. It is also an example of an early photographic and film-making technology in use in regional Victoria in the time period.Thin translucent sheet of glass with a rectangular image printed on the front and framed in a black backing. It is held together by metals strips to secure the edges of the slide.Obverse: i /burke museum, beechworth, lantern slide, slide, glass slide, plate, burke museum collection, photograph, monochrome, magic lantern, indigo shire, north-east victoria, nineteenth century, 1900s, twentieth century, emulsion slides, nursing, nurses, mental hospitals, lunatic asylums, asylums, social services, social welfare, insane asylums, mental health, infrastructure -
The Beechworth Burke Museum
Photograph - Lantern Slide, c1900
This image shows a view of a properties bordering a river in the vicinity of Beechworth in approximately 1900. Although the exact location of the photograph is yet to be determined, the water source pictured may feed into the bigger system that flows through Beechworth Gorge. A man wearing a hat, possibly the photographer, is silhouetted in the foreground of the picture. Lantern slides, sometimes called 'magic lantern' slides, are glass plates on which an image has been secured for the purpose of projection. Glass slides were etched or hand-painted for this purpose from the Eighteenth Century but the process became more popular and accessible to the public with the development of photographic-emulsion slides used with a 'Magic Lantern' device in the mid-Nineteenth Century. Photographic lantern slides comprise a double-negative emulsion layer (forming a positive image) between thin glass plates that are bound together. A number of processes existed to form and bind the emulsion layer to the base plate, including the albumen, wet plate collodion, gelatine dry plate and woodburytype techniques. Lantern slides and magic lantern technologies are seen as foundational precursors to the development of modern photography and film-making techniques.This glass slide is significant because it provides insight into Beechworth's built environment and natural landscape in the early Twentieth Century, around the time of Australia's Federation. It is also an example of an early photographic and film-making technology in use in regional Victoria in the time period.Thin translucent sheet of glass with a square image printed on the front and framed in a black backing. It is held together by metals strips to secure the edges of the slide.burke museum, beechworth, lantern slide, slide, glass slide, plate, burke museum collection, photograph, monochrome, photographer, beechworth gorge, river, stream, water source, 1900s -
The Beechworth Burke Museum
Photograph - Lantern Slide, c1900
This image shows a semi-aerial view of commercial and official properties lining Ford Street, Beechworth, in approximately 1900. The tower of Christ Church of St Peter and St Paul can be seen in the middle section of the photograph, on the left-hand side of the street. The Church was constructed in 1858 with the tower added to the structure in 1864. Lantern slides, sometimes called 'magic lantern' slides, are glass plates on which an image has been secured for the purpose of projection. Glass slides were etched or hand-painted for this purpose from the Eighteenth Century but the process became more popular and accessible to the public with the development of photographic-emulsion slides used with a 'Magic Lantern' device in the mid-Nineteenth Century. Photographic lantern slides comprise a double-negative emulsion layer (forming a positive image) between thin glass plates that are bound together. A number of processes existed to form and bind the emulsion layer to the base plate, including the albumen, wet plate collodion, gelatine dry plate and woodburytype techniques. Lantern slides and magic lantern technologies are seen as foundational precursors to the development of modern photography and film-making techniques.This glass slide is significant because it provides insight into Beechworth's built environment and commercial and official infrastructure in the early Twentieth Century, around the time of Australia's Federation into one nation. It is also an example of an early photographic and film-making technology in use in regional Victoria in the time period.Thin translucent sheet of glass with a square image printed on the front and framed in a black backing. It is held together by metals strips to secure the edges of the slide.burke museum, beechworth, lantern slide, slide, glass slide, plate, burke museum collection, photograph, monochrome, ford street, christ church of st peter and st paul, church tower, landmarks, 1900, shopping facilities, public buildings, 1900s, built environment, streetscape -
The Beechworth Burke Museum
Photograph - Lantern Slide, c1900
This image appears to show nurses at what is now the Mayday Hills Mental Asylum in approximately 1900. These individuals are part of a long history of nursing in Beechworth. Three medical or social welfare facilities opened in the mid-1800s as part of a push by the township to become a regional centre for Government services. These were the Ovens District Hospital (opened in 1857), the Ovens Benevolent Asylum (opened in 1863), and the Beechworth Mental Hospital (opened in 1867 and renamed Mayday Hills Hospital at Centenary celebrations in 1967). It was recognised that the unsettled living conditions, poverty and relative isolation of the Goldfields environment could produce 'mental disturbances' which required local treatment facilities as services in Melbourne were too far away. Carole Woods' publication 'A Titan's Field' describes activities undertaken by patients at Beechworth Mental Hospital as including monthly balls and occasional concerts as well as work to make the facility self-supporting such as farm work and making clothes. She mentions a report in 1870 that the approximately 300 patients were clean and neat with 'no-one in restraint or seclusion' but that by 1905 the organisation had 623 patients which placed strain on building infrastructure such as heating and water supplies, leading to high turnover of nurses and other issues. A program of building works to extend and improve facilities followed over subsequent decades. Lantern slides, sometimes called 'magic lantern' slides, are glass plates on which an image has been secured for the purpose of projection. Glass slides were etched or hand-painted for this purpose from the Eighteenth Century but the process became more popular and accessible to the public with the development of photographic-emulsion slides used with a 'Magic Lantern' device in the mid-Nineteenth Century. Photographic lantern slides comprise a double-negative emulsion layer (forming a positive image) between thin glass plates that are bound together. A number of processes existed to form and bind the emulsion layer to the base plate, including the albumen, wet plate collodion, gelatine dry plate and Woodburytype techniques. Lantern slides and magic lantern technologies are seen as foundational precursors to the development of modern photography and film-making techniques.This glass slide is significant because it provides insight into Beechworth's social and medical amenities in the early Twentieth Century, around the time of Australia's Federation into one nation. It is also an example of an early photographic and film-making technology in use in regional Victoria in the time period.Thin translucent sheet of glass with a circular image printed on the front and framed in a black backing. It is held together by metals strips to secure the edges of the slide.burke museum, beechworth, lantern slide, slide, glass slide, plate, burke museum collection, photograph, monochrome, magic lantern, indigo shire, north-east victoria, nineteenth century, 1900s, twentieth century, emulsion slides, nursing, nurses, mental hospitals, lunatic asylums, asylums, social services, social welfare, insane asylums, mental health, infrastructure -
The Beechworth Burke Museum
Photograph - Lantern Slide, c1900
This lantern slide shows the Ovens District Hospital (also called the Ovens Goldfields Hospital) in Beechworth in approximately 1900. The Hospital was built as part of a community push to develop the infrastructure needed for a permanent town in the 1850s. At the time there was no hospital located between Melbourne and the NSW town of Goulburn and it was recognised that the nature of mining and agricultural work predisposed people to serious injury. The community voted in 1853 to raise funds for a hospital and a voluntary committee elected from people who contributed £2 or more annually determined the organisation's management policies, which aimed to provide care for poor people at rates levied according to the person's means. Ongoing operations of the hospital were primarily supported by Government grants, however. The foundation stone was laid at a site in Church Street at a ceremony held 1st September 1856 which was attended by 2000 people using a locally crafted trowel with a tin ore handle and pure gold blade. The hospital, which was designed by J.H. Dobbyn, cost £2347. The hospital had two wards, a dispensary, apartments for a resident surgeon and the matron, an operating theatre and a board room. Further medical facilities including services to meet the cultural and health needs of the local Chinese community were later added, in addition to a Palladian-style cut-granite face built in 1862-63. It functioned as the region's primary hospital until surpassed by the Wangaratta Hospital in 1910. In the 1940s much of the building materials were salvaged and repurposed, with the exception of the facade which was restored in 1963 by the Beechworth Lions Club and still stands today. The facade featured on the covers of local history volume 'Beechworth: a Titan's Field' by Carole Woods and heritage-focused travel guide the 'Readers Digest Book of Historic Australian Towns'. Lantern slides, sometimes called 'magic lantern' slides, are glass plates on which an image has been secured for the purpose of projection. Glass slides were etched or hand-painted for this purpose from the Eighteenth Century but the process became more popular and accessible to the public with the development of photographic-emulsion slides used with a 'Magic Lantern' device in the mid-Nineteenth Century. Photographic lantern slides comprise a double-negative emulsion layer (forming a positive image) between thin glass plates that are bound together. A number of processes existed to form and bind the emulsion layer to the base plate, including the albumen, wet plate collodion, gelatine dry plate and woodburytype techniques. Lantern slides and magic lantern technologies are seen as foundational precursors to the development of modern photography and film-making techniques.This glass slide is significant because it provides insight into Beechworth's built environment and infrastructure in the early Twentieth Century, around the time of Australia's Federation. It is also an example of an early photographic and film-making technology in use in regional Victoria in the time period.Thin translucent sheet of glass with a round-edged square image printed on the front and framed in a black backing. It is held together by metal strips to secure the edges of the slide.Obverse: Y /burke museum, beechworth, lantern slide, slide, glass slide, plate, burke museum collection, photograph, monochrome, ovens district hospital, indigo shire, north-east victoria, hospital, palladian architecture, granite, community fundraising, community infrastructure, j.h. dobbyn, beechworth lions club, ovens goldfields hospital, chinese community -
The Beechworth Burke Museum
Photograph - Lantern Slide, c1900
This image shows the gorge adjacent to Beechworth in approximately 1900. Although the exact location of the photograph is yet to be determined, the present-day Beechworth Gorge Walk includes views of the Cascades at the point at which Spring Creek flows into the valley on the level below. Gold-sluicing techniques in use in the town during periods of active gold extraction may have altered the landscape since the photograph was taken, however. In the 1850s a mill was built at the top of the Spring Creek falls by Russian-born Louis Chevalier, brother of artist Nicholas Chevalier. The mill supplied the town with lumber that supported the town's initial construction boom. Lantern slides, sometimes called 'magic lantern' slides, are glass plates on which an image has been secured for the purpose of projection. Glass slides were etched or hand-painted for this purpose from the Eighteenth Century but the process became more popular and accessible to the public with the development of photographic-emulsion slides used with a 'Magic Lantern' device in the mid-Nineteenth Century. Photographic lantern slides comprise a double-negative emulsion layer (forming a positive image) between thin glass plates that are bound together. A number of processes existed to form and bind the emulsion layer to the base plate, including the albumen, wet plate collodion, gelatine dry plate and woodburytype techniques. Lantern slides and magic lantern technologies are seen as foundational precursors to the development of modern photography and film-making techniques.This glass slide is significant because it provides insight into Beechworth's built environment and natural landscape in the early Twentieth Century, around the time of Australia's Federation. It is also an example of an early photographic and film-making technology in use in regional Victoria in the time period.Thin translucent sheet of glass with a square image printed on the front and framed in a black backing. It is held together by metals strips to secure the edges of the slide.burke museum, beechworth, lantern slide, slide, glass slide, plate, burke museum collection, photograph, monochrome, beechworth gorge, indigo shire, landscapes, mill, sluicing, gold mining, north-east victoria, spring creek, louis chevalier, cascades -
The Beechworth Burke Museum
Photograph - Lantern Slide, c1900
Miners from Snake Valley lobbied the Victorian Government in 1855 to make land available for sale for farming purposes as an alternative occupation and income for people who wished to stay in the region but move away from gold mining. A secondary motivation was to increase the supply of fresh produce and decrease prices of items that otherwise needed to be transported from Melbourne or other regions. Forty-three country lots were initially offered in the Three Mile area, ranging in size from two to ninety acres and costing from £1 to £3 per acre. An additional eighty-five country lots were auctioned later in the year, in addition to many smaller suburban lots. More lots were offered than sold, initially, but this represented conditions of sale requiring the total purchase cost up front which many people interested in purchasing could not afford, especially as land purchased for farming would accrue substantial additional costs for clearing and labour before becoming productive. Further lobbying activities and the election of parliamentary members sympathetic to the cause took place through the 1850s. Ovens Parliamentary Member, Daniel Cameron, was re-elected in 1856 on a platform of surveying the land for public selection with deferred payment options. Land reform remained an issue in the area through the 1850s and early 1860s, impacting broader decisions in the new State of Victoria relating to voting rights, use of Crown land and the farming of land that wasn't always suitable for the purpose. This photograph depicts Beechworth in approximately 1900, after several waves of land sales resulted in increasingly levels of development. Lantern slides, sometimes called 'magic lantern' slides, are glass plates on which an image has been secured for the purpose of projection. Glass slides were etched or hand-painted for this purpose from the Eighteenth Century but the process became more popular and accessible to the public with the development of photographic-emulsion slides used with a 'Magic Lantern' device in the mid-Nineteenth Century. Photographic lantern slides comprise a double-negative emulsion layer (forming a positive image) between thin glass plates that are bound together. A number of processes existed to form and bind the emulsion layer to the base plate, including the albumen, wet plate collodion, gelatine dry plate and woodburytype techniques. Lantern slides and magic lantern technologies are seen as foundational precursors to the development of modern photography and film-making techniques.This glass slide is significant because it provides insight into Beechworth's built environment and infrastructure in the early Twentieth Century, around the time of Australia's Federation. It is also an example of an early photographic and film-making technology in use in regional Victoria in the time period.Thin translucent sheet of glass with a square-edged image printed on the front and framed in a black backing. It is held together by metal strips to secure the edges of the slide.burke museum, beechworth, lantern slide, slide, glass slide, plate, burke museum collection, photograph, monochrome, indigo shire, north-east victoria, farming, squatters, miners, agriculture, land-clearing, land reform, daniel cameron, land sales, three mile, snake valley, tarrawingee -
The Beechworth Burke Museum
Document - Magazine, CENTENARY ISSUE / 1867 / The New Open Door / 1967, 1967
Centenary issue of the Open Door Magazine that was produced by both staff and patients. The title reflects Mayday Hills "open door" approach to patient care.Mayday Hills Asylum was one of the three largest psychiatric hospitals in Victoria, and played an important role in the treatment of mental health illnesses from its establishment in 1867 to its closure in 1995. As part of prescribed treatment, many patients participated in craft activities were they were able to create an array of objects. 13-page A4 paper magazine with 4 copper staples.CENTENARY ISSUE / 1867 / The New Open Door / 1967 [The Australian National Coat of Arms]beechworth, burke museum, mayday hills, magazine, centenary -
Camperdown & District Historical Society
Photograph - Chest plate "King George Colungulac", c1860s
In the early days of colonial Australia the governors and the land holders saw advantage in singling out certain First Nations people as leaders and distinguishing them in some way. This chest plate was issued to "King George" of the Koenghegulluk Clan of the Djargurd Wurrung whose Country was near Lake Colongulac. This chest plate is inscribed "King Colungulac" and is held in the Museum Victoria collection. ""King George"" is pictured wearing the chest plate in a photograph of First Nations people at Framlingham Mission in 1867.Colour photograph of brass chest plate inscribed "KING GEORGE COLUNGULAC" Front: "KING GEORGE COLUNGULAC"; Back: XP49214 Museum Victoriabreast plate, cdhs, cdhsfirstnations -
Orbost & District Historical Society
magazine, McLaren & Co Pty Ltd, 1939 1945, C1945
This book/magazine is a record of the company's tasks in WW11. It acknowledges the "debt owed to the armed forces involvement and role in defeating the enemy". The Australian operations of this company were originally founded by Hugh V. McKay in the 1890s. In 1906, H.V. McKay moved his manufacturing operations from Ballarat to Braybrook Junction (later Sunshine) on the western outskirts of Melbourne. In 1921 the company became H.V. McKay Pty Ltd. In 1930 it merged with the Australian operations of the Canadian agricultural implement and tractor manufacturer Massey Harris, to become H.V. McKay Massey Harris Pty Ltd. Throughout World War II H.V. McKay Massey Harris exported over 20,000 Sunshine drills, disc harrows and binders to England to facilitate the increase in food production. (ref Museum Victoria, Wickipedia)Inside this magazine is a photograph of a sprocket similar to that made by Orbost Motor Works during WW11. (Registration No 2001)A large stapled cardboard covered magazine with a tan coloured cover. On the front cover in dark brown print at the bottom is a rising sun with "H. V. McKay Massey Harris Pty Ltd Australia" underneath it. At the top in large font is 1939 1945. It contains coloured photographs and text. massey-harris -
Orbost & District Historical Society
magazine, Aussie, March 18, 1918
Alexander Butters enlisted on 12 November 1914 as a gunner. He was awarded a Meritorious Service medal for his "determination and courage .....setting a splendid example to his men..." on the SOMME. 'Aussie' (1918- circa 1929) was a commercial magazine of opinion, review and entertainment. It was edited by Phillip Harris and published in France 1918 - 1919 on a small printing press that Harris brought with him to France. Initially the print run was only 10,000 copies, but soon it reached 60,000 and later 100,000. The magazine celebrated a distinctive 'Aussie' identity through language, humour and imagery. It distributed news, provided light-hearted ways of seeing the war experience and gave soldiers an outlet to express dissent or dissatisfaction. It also provided a voice for Australian authors such as Banjo Paterson, C.J. Dennis and Bernard O'Dowd. (Ref Museum Victoria)This magazine provides an Australian soldiers' view of the political and world climate during World War I, and also represents the bond between Australian soldiers. The magazine celebrated a distinctive ?Aussie? identity, through language, humour and their assertion of what it meant to be an Australian. It allowed news to be distributed, gave the soldiers an outlet to express any dissent or dissatisfaction, thus preventing any greater form of rebellion and promoted Australian authors like Banjo Paterson, C.J. Dennis and Bernard O'Dowd. (Ref. Museum Victoria)A thin black and white paper magazine called "Aussie". This is Volume 3. The magazine contains stories, illustrations, songs and poetry from the First World War. On the front cover the title is printed across the centre, with a drawing of a soldier in uniform standing sideways, and holding a gun. Four drawings within circles are positioned in each corner, joined by a wreath and ribbons bearing the names of the war fields. His head is in the shape of the map of Australia. On front cover - From Alexandy Butters with best wishesmagazine ww1 aussie military