Kaolin is also known as china clay. This specimen came from Dunolly, Victoria and was donated to the Museum in 1868 as part of the Geological Survey of Victoria. This survey helped map and study the geology of Victoria. In Victoria, Kaolin is particularly used as a filler and coating material in paper manufacture. It can also be used in paints, ceramics, rubbers and plastics. There are many kaolin deposits in Victoria but many of these have been mined out and there is not much Kaolin left. Rocks that have a high amount of Kaolinite and it can be formed through the decomposition of other materials. There are two types of Kaolin; hard and soft kaolin. Soft kaolin's are coarse but have a soapy texture. It can also break easily. The hard kaolins have an earthly texture and are finer grained. This means that they are harder to break, unlike the soft kaolin. Hard kaolin's are formed by flocculation in salt water, a process that in basic terms, bonds particles together. Kaolin is a common material in Victoria and that is why it is significant. While this specimen was mined in Dunolly, Victoria Kaolin can also be found Pittong, Pakenham, Bulla, Hallam and Ballarat as well as many other places throughout Victoria. This specimen represents the presence of Kaolin deposits in this region of Australia. It is also significant because Kaolin has many uses and is largely beneficial to many manufacturing processes in 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.Two pieces of Kaolinite mineral with shades of white and graygeological specimen, geology, geology collection, burke museum, beechworth, kaolin, china clay, dunolly, geological survey of victoria, kaolinite, victoria, mining, mining deposits, geology of victoria, australia, filler, coating material, paper manufacture, paint, ceramics, rubbers, plastics, decomposition, materials, soft kaolin, hard kaolin, flocculation, particles, salt water

Actinolite is usually found in metamorphic rocks, such as contact aureoles surrounding cooled intrusive igneous rocks. It also occurs as a product of the metamorphism of magnesium-rich limestones. Pyrite is usually found with other sulfides or oxides in quartz veins, sedimentary rock, and metamorphic rock, as well coal beds, and as a replacement mineral in fossils. Actinolite is an amphibole silicate mineral. It is named after the Greek word "aktinos" meaning “ray” in allusion to the mineral's fibrous nature. Fibrous actinolite is a type of asbestos and was once mined along Jones Creek at Gundagai, New South Wales. Pyrite or "Fool's Gold" is the most common sulfide mineral. It is named after the Greek "pyr" meaning "fire" because it can be used to create sparks needed for a fire if struck against metal or a hard surface. Due to its gold colour, pyrite can be mistaken for gold and often forms alongside it, causing small amounts of gold to be present in rocks containing pyrite. Most importantly, pyrite is an ore of gold. Pyrite is sometimes used as a gemstone but is not great for jewellery as it easily tarnishes. In some fossils of ammonites – shelled cephalopods that died ~66 million years ago – pyrite also replaces the shell. 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-medium-sized solid specimen with the minerals actinolite (dark green fibrous) and pyrite (brassy) with shades of brown, black/grey, and white. Actinolite is an amphibole mineral in the tremolite-actinolite series of calcium, magnesium, and iron silicates. Pyrite is an iron disulfide mineral.geological specimen, geology, geology collection, burke museum, beechworth, indigo shire, geological, mineralogy, pyrite, actinolite, victoria, sewyln, alfred selwyn

Malachite is a water soluble, crystalline, triphenyl methylene chloride salt. It has a close relationship to copper because it is common for Malachite and copper to come from the same ore. Malachite often has shades of green, making it also known as Malachite Green. As a result of it's colour, it is known for being a dye and has been used in the dye industry, the textile industry and in medical fields. Cobar in New South Wales is well known for it's mining. This is because of the number of important deposits present in the area and include three important mining belts where most of the materials are found. These are the 'Cobar belt', the 'Canbelego belt' and the 'Girilambone belt'. The 'Cobar belt' runs underneath the main town. Copper was first discovered in Cobar in 1869 and since then, many deposits of other materials have been found, including Malachite.This specimen is significant because it comes from Cobar, NSW and represents the many deposits of materials found there. Cobar has a long history of mining and is a source of Australia's copper minerals. Malachite is often found in copper deposits meaning that it is representative of Cobar's copper production. Malachite is known for it's vivid green colour and as a result, has many uses, such as meaning used as a dye. This makes it a valuable material and highly significant. 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 mineral with shades of brown , white and light green throughout.geological specimen, geology, geology collection, burke museum, beechworth, malachite, copper, water soluble, cobar, cobar mines, cobar mining, cobar nsw, nsw, new south wales, mining belts, ore, copper ore, malachite green, dye, green, dye industry, textile industry, desposits, canbelego, girilambone, alfred selwyn

This particular specimen is found in Wolgan Valley, New South Wales. It could be linked to the abandoned oil shale mining sites in Wolgan Valley such as Newnes. Newnes was an industrial complex operational in the early 20th century is now partly surrounded by Wollemi National Park. It produced motor spirit, kerosene, and gas oil. Newnes's Torbanite oil shale rock contained around 350 litres of oil shale per tonne. The Torbanite was mined by the Commonwealth Oil Corporation Ltd. Oil shale is a sedimentary rock and also a form of fossil fuel. It is often formed millions of years ago and usually contain fossilised remains of plants and/or animals. Oil shale is rich in kerogen that releases hydrocarbon when heated. These hydrocarbon can be used as an alternative petroleum or natural gas. The oil-shale rock was converted into oil by "destructive distillation"; the rock being heated until it broke down to form an oily vapour and an ash residue. Oil bearing shale is one of Australia's national assets. There are many oil companies established in Australia. It reflects Australia's rich natural resources as well as connection to the Australia's engineering and oil industry. The booming oil shale extraction businesses can be traced as far back as 1920s. 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.Piece of dark gray oil bearing shale with shades of light brown and fossilised leavesExisting label: OIL BEARING SHALE with / FOSSILISED LEAVES / Locality: Wongan Valley, NSW / Donor: Miss M. Cambell geological specimen, geology, geology collection, burke museum, beechworth, oil shale, shale, fossil fuels, alfred selwyn, wolgen valley, 1868 geological survey of victoria, rocks, sedimentary rocks, newnes, torbanite, commonwealth oil corporation ltd

Amazonite is classed as a Tectosilicate and is part of the Feldspar group of minerals. Amazonite forms in a triclinic crystal structure and its chemical formula is K(AlSi3O8). In appearance, Amazonite can range from shades of green to green blue to blue, and often with white streaks or veining. The greenish colour is believed to come from the small amount of lead contained in its composition. Amazonite is named after the Amazon River due to its colour and similarities to another rock found along the riverbanks, although Amazonite is not actually found at or near the Amazon. Although less commonly used in jewellery today, Amazonite has been mined and used by humans for thousands of years and Amazonite jewellery from at least 2000BCE have been discovered in North Africa. Amazonite is found in many locations around the world including Brazil, Peru, Ethiopia, Canada, Russia, Mozambique, Myanmar, Pakistan, China, Madagascar, and the United States of America. This specimen most probably comes from the U.S.A., Amazonite is found in several US states particularly in Colorado, Virginia, Pennsylvania. This specimen is of both scientific and historic significance as a striking blue green example of Amazonite mined prior to 1868 in the United States of America, most likely from Colorado, Virginia, or Pennsylvania. These three states are all locations of significant Amazonite deposits. 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 Feldspar mineral specimen from the Tectosilicate class in shades of blue-green with white veining.Existing label: green/blue Feldspar / "amazonite" / possibly USA geological specimen, geology, geology collection, burke museum, beechworth, tectosilicate, amazonite, feldspar, triclinic crystal structure, amazonite usa, amazonite colorado, amazonite virginia, amazonite pennsylvania

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

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

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

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

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

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

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

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

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

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

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

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

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

This was owned and used by J.G. Ralston of Orbost. John Gavin Ralston was born 26 July 1914 at Eden, N.S.W. and came to Orbost in the early 1920's, with his parents and siblings. They lived at the corner of Tennyson and Salisbury Streets. Jack was educated at Orbost Higher Elementary School before being apprenticed to William Ross at the Snowy River Mail as a lino-type operator. He married Jean Cameron. After WW11 when he served overseas in the islands) He resumed his trade at the Snowy River Mail until 1949 when began J.G.& J.M. Ralston, Seed & Produce Merchants. Jack Ralston was very involved in the Orbost sporting community, the Presbyterian Church and the Orbost Municipal Band. He also served in the Orbost sub-branch of the R.S.L. He died on April 15 1967. (ref. Margaret Smith O.D.H.S. Newsletter) Collecting match box holders / grips was a popular hobby. They were made to fit over a box of matches for protection. Some were especially produced for significant occasions. This item is an example of a very common personal item rarely used today.A painted metal matchbox cover with a thin wooden matchbox inside. It is cream coloured with a picture of a cricketer being bowled out. In the top right hand corner is "OWZAT". The matches are Bryant & May's Crown Safety Matches. it is a rectangular cardboard box with a sliding cardboard drawer. The box has a paper label with text reading, "BRYANT & MAY'S CROWN SAFETY MATCHES" and an image of a crown. The top and bottom side has a purple striking paper, to light match. Bottom and sides of sliding drawer are a green color.J.G.Ralstonmatchbox-holder smoking-accessories ralston-j.g.

Ushabti are tiny anthropoid (human-shaped) figures placed in the tombs of wealthy Egyptians. They were intended to do the work of the deceased in the afterlife. This purpose is implied through their name, which may have derived from the Egyptian word “to answer”. The Burke Museum in Beechworth is home to a particular ancient Egyptian Ushabti figure. This artefact was donated to the Museum in 1875. No details about how it left Egypt, arrived in Australia, and where it was located before this donation are known. The Nineteenth Century, when this artefact was donated, was a period when many museums acquired items of ancient Egyptian heritage. Many of these items were procured in less than desirable circumstances, having often been looted from ancient tombs and sold to tourists without documentation as to their original location and/or accompanying grave goods. These artefacts were also divested through partage (the trading of artefacts for funds); however, the latter is unlikely to have been the case for this artefact. Since the Ushabti was donated by an unknown donor, it is likely to have been in a private collection rather than an institution. Ushabti can be dated using iconographic analysis which is non-invasive and provides a comprehensive study of the artefact. The later period of the 18th Dynasty marked the beginning of an increase in both the inclusion of Ushabti as essential funerary items and the creation of Ushabti with tools. From this period, they are no longer depicted without tools. Depictions of tools including gardening hoes are frequently depicted grasped in the Ushabti’s hands whilst items like the seed-bag are depicted hanging on the back rather than in an alternative position. This Ushabti figure grasps a gardening hoe and a mattock and a small seed bag surrounded by a yoke bearing water jars are depicted on the upper back of the Ushabti. These features are essential in helping narrow this dating to the late 18th and before the early 20th Dynasty. The position of this seed bag also provides dating information. In the early 18th Dynasty this bag was consistently drawn on the front of the figurine; however, by the reign of Seti I, this feature moved to the back. Thus, since the seed bag is located on the back of this Ushabti, it cannot date to the early 18th Dynasty. By the 19th Dynasty, Ushabti’s were increasingly made from either faience or terracotta. The availability of these materials in Egypt resulted in the increase of Ushabti production with tombs containing many more figurines than previously seen. The Ushabti held by the Burke collections is made from terracotta. Terracotta was rarely used for Ushabti before and during the early 18th Dynasty with only the odd appearance until the late 18th Dynasty and becoming common through that period until the late Third Intermediate Period. Whilst the face has been damaged, there is no evidence for the Ushabti having been provided with an Osirian false beard. This omission rules out a dating of later than the 25th Dynasty when beards became prominent. The inscriptions also date the Ushabti to the New Kingdom. This is because of the use of sḥḏ (“to illuminate”) with Wsjr (“Osiris”) which only occurs in these periods. Therefore, considering all these elements, the Ushabti can be confidently be dated to between the late 18th to early 19th dynasty.Artefacts like this Ushabti are no longer exclusively representative of their origins in burial assemblages and significance in the mythology of the Egyptian afterlife but are also significant for the accumulated histories they have gained through travel. The movement of this artefact from Egypt to Australia allows insight into the collecting habits of the 19th century, and in particular, the reception of ancient Egyptian artefacts in small rural museums. The procurement of Egyptian artefacts was a social trend around the late 1800s to early 1900s. Egyptian artefacts were considered curiosities and recognised for their ability to attract public attention to museums. They were also utilised in Australian museums, like the Burke Museum, to connect the collection to one of the oldest civilisations known to man and since Australia was considered a “young” country by European settlers, this was vital and derived from an interest in Darwin’s “Origin of the Species” 1859. Furthermore, there was a culture of collecting in the 1800s amongst the affluent in English society which led to the appearance of many Egyptian artefacts in private collections. The acquisition of this Ushabti figure is not certain, but it was likely donated from a private collection rather than an institution. This particular artefact is significant as an example of a high-quality Ushabti representative of those produced during the late 18th or early 19th century. It provides insight into the individualism of an Ushabti and the mythology of ancient Egypt. It also provides an example of the types of items required in the tomb assemblages of this period and reinforces the importance of ensuring the successful afterlife of the deceased through art. This Ushabti belonged to a woman named Taweret-Khaiti, Chantress of Amun, in the late 18th Dynasty or early 19th Dynasty (c.1292 BC) of the Egyptian New Kingdom. It likely comes from an undetermined tomb in the locality of Thebes. This figure is made from Nile silt clay (a polyester terracotta; clay sourced from the banks of the Nile River) which was a popular material for Ushabti construction in the early 19th Dynasty. It is in a fair state of preservation (with the exception of a break through the centre) and originally made to a high quality. The face has been damaged but the eyes and eyebrows are clearly marked with black ink and the sclera painted white. The Ushabti is painted a light brown/yellow colour and features a vertical line of inscription down the lower front. The Ushabti wears a large wig and and a schematic collar. The arms are painted light brown and depicted crossed with bracelets around the wrists. It grasps a hoe and mattock. A yellow seed-basket is depicted on the Ushabti’s back. These features represent the likelihood that this particular Ushabti was intended to complete farm work for the deceased in the next life. There would have been additional Ushabti of similar design within the tomb who worked under the supervision of a foreman Ushabti. The foreman Ushabti would be depicted dressed in the clothing of the living. The inscriptions are painted freehand in black ink and written in a vertical column from the base of the collar to the foot pedestal on the front of the Ushabti. The owner of the Ushabti could elect to have the figures inscribed with their name, the Ushabti spell and any other details they deemed necessary. In the case of this example, the Ushabti is inscribed with the owner’s details and is an abbreviated version of the standard Ushabti formula. This formula ensured that the Ushabti would complete the desired task in the afterlife when called upon by the deceased. Ushabti which were not inscribed would represent their intended purpose through design; however, this Ushabti, like most made in the late 18th Dynasty, conveys its purpose both through both design and inscription. The inscription is as follows: sHD wsir nbt pr Smayt imn tA-wr(t)-xai(ti) mAa xrw which translates to: "The illuminated one, the Osiris (the deceased), the mistress of the household, Chantress of Amun, Taweret-Khaiti, true of voice (justified)"ancient egypt

The firm Dring and Fage were active from 1790 to 1940 in London and were manufacturers of hydrometers and mathematical instruments they became established in London in 1790 by John Dring, who was a brass worker and hydrometer maker, and William Fage. Dring and Fage manufactured also saccharometers and other instruments used to measure the strength of alcohol. These instruments were primarily used to calculate excises. They traded at various addresses in London and they were at 56 Stamford St. between 1903 and 1938. By 1850 the company was owned by Edward Hall and Edward Jenkin and in 1940 the company became Dring & Fage Ltd, trading till the 1960s. Historically, gauging has meant measuring a volume, these gauging instruments were used by Customs and Excise and manufacturers for determining the volume and contents of liquid containers. For Customs the determination and collection of duty on imported goods which has had a very long history. Chaucer was a Customs Officer as was his father and grandfather, excise was first officially introduced in 1643, with the aim of maintaining military forces raised by the English Parliament at that time. Excise was initially a duty on home produced alcoholic beverages and soap but being easily applied, spread rapidly to a wide range of goods including imports of varying kinds. The government departments of Customs and Excise merged only in 1909 and it is from around this time that our instrument was made and used. The item demonstrates a long social history of the practice of Government's collecting duty on alcoholic beverages and thereby makes this item historically significant as it was used locally at Port Fairy by the ports Customs agents. Gauging rod or bung rod; ullaging gauge. Long brown wooden gauging rod with brass tips and sliding brass marker. Measurements are marked along the length of the rod. Used for measuring volume of liquor in casks in order for Customs to calculate excise (tax) on the contents. Made by Dring & Fage, London.Engraved “Dring & Fage 56 Stamford St London flagstaff hill, warrnambool, shipwrecked coast, flagstaff hill maritime museum, maritime museum, shipwreck coast, flagstaff hill maritime village, great ocean road, gauging rod, ullaging rods, measuring instruments, customs tax, dring & fage, alcohol measurement

J & G Meakin was an English pottery manufacturing company founded in 1851 and based in Hanley, Stoke-on-Trent, Staffordshire. In the 19th century, J & G Meakin was known for the vast quantities of cheap ironstone china it produced for the domestic English market and export to Australia, Canada, New Zealand, and the United States and one of these pottery lines was called "EMPRESS" and was in production through the 1930s. From around 1970, designs included Liberty, Sterling, Trend, Classic, and Heirloom. Some of these were influenced by earlier designs. The newer wares can be distinguished by back stamp markings such as 'permanent colours', 'everlasting colour', or 'dishwasher proof'. J & G Meakin had close family and corporate affiliations to the potteries Johnson Brothers, and Alfred Meakin Ltd, which explains why many patterns are similar, if not almost the same. There was a takeover by J. & G. Meakin in 1968 of Midwinter Pottery. The firm was then taken over by the Wedgwood Group in 1970. In 2000 production under the Meakin name ceased and their long-established works, Eagle Pottery, was then used for the production of Johnson Bros pottery. Eagle Pottery closed in 2004 when production was transferred abroad; the works were demolished in 2005.Item is significant as today the "EMPRESS" china pattern from the 1930s by Meakin is today a collectable item and a good example of the Meakin range of china.Plate china white oval with a pattern inscribed along the edge Inscription to base "EMPRESS" warrnambool, flagstaff-hill, flagstaff-hill-maritime-museum, maritime-museum, shipwreck-coast, flagstaff-hill-maritime-village, alfred meakin, staffordshire potteries, iron stone pottery, serving dish

The inscription in the book indicates that it once belonged to Edwin J Dale, who may have received it May 13th 1901, the date on the inscription. The album was made in Germany and has English, German, French and Spanish language on the fly page. It has 2000 pockets for holding stamps and is illustrated. The printer, Spottiswoode and Co., was established in 1738 by William Strahan, with premises in New Street Square, London. The growing firm advertised as Printers, Lithographers, Stationers, Electrotypers, Publishers, and Booksellers and by 1914 there were 1,000 employees.The stamp album is of Victorian vintage and shows that at the end of the 19th century people collected stamps. It represents the hobbies and past times of the people of that era.Illustrated Postage Stamp Album. Publisher: Lalso by CF Lucke, Leipzig, Germany Printer: Spottiswoode & Co Ltd, London Date: 1908 Red hardcover, illustrated with a robed figure image and text in English, German, French and Spanish. Book has information, advertising and pages divided into blank squares for attaching stamps. Some pages have cutouts where squares would have been, perhaps holding stamps. An inscription with the name Edwin J Dale, 13 May 1901 is on the first turned page..Inscription: Edwin J Dale, May 13th 1901" Cover: "Illustrated POSTAGE STAMP ALBUM" Inage on cover: "within a floral border, a robed figure wearing a winged helmet, holding a staff with two snakes in one hand, and a sealed letter in the other." Fly: "Registered" "Schaubeks Postage Stamp Album" "Victoria" "Briefmarken"[German - stamps] "Pour Timbres-poste" [French - for postage Stamps] "Para Selloyde Correo" [Spanish - for postage stamps] "With 1070 reduced illustrations, 2200 blank cases for stamps" (also in German, French and Spanish) "Made in Germany"flagstaff hill, warrnambool, shipwrecked-coast, flagstaff-hill, flagstaff-hill-maritime-museum, maritime-museum, shipwreck-coast, flagstaff-hill-maritime-village, illustrated postage stamp album, postage stamp album, stamp album, book, postage stamp, stamp, edwin j dale, may 13th 1901, stamp collecting, german stamp album, spottiswoode & co ltd, germany, cf lucke leipzig, cf lucke, leipzig

A moulding plane is a specialised plane used for making the complex shapes found in wooden mouldings that are used to decorate furniture or other wooden objects. Traditionally, moulding planes were blocks of wear-resistant hardwood, often beech or maple, which were worked to the shape of the intended moulding. The blade or iron was likewise formed to the intended moulding profile and secured in the body of the plane with a wooden wedge. A traditional cabinetmakers shop might have many, perhaps hundreds, of moulding planes for the full range of work to be performed. Large crown mouldings required planes of six or more inches in width, which demanded great strength to push and often had additional peg handles on the sides, allowing the craftsman's apprentice or other workers to pull the plane ahead of the master who guided it. Company History: We know little of John Manners other than his firm was acquired by Alexander Mathieson & Sons in 1822, Mathieson were one of the leading makers of hand tools in Scotland at this time. 1792 was deemed by Mathieson & Sons to be that of its foundation and it was in all likelihood the year in which John Manners had also set up his plane-making workshop on Saracen Lane off the Gallowgate in the heart of Glasgow, not far from the Saracen's Head Inn. Alexander Mathieson (1797–1851) is recorded in 1822 as a plane-maker at 25 Gallowgate, but in the following year at 14 Saracen's Lane, it is presumed having taken over the premises of John Manners. The 1841 national census described Alexander Mathieson as a master plane-maker at 38 Saracen Lane with his son Thomas Adam working as a journeyman plane-maker, from 1822 we hear nothing regards what happened to John Manners.A vintage tool made by a known maker John Manners the item is a significant wood working tool from the late 18th century that today is quite rare. As this maker sold his business to Alexander Mathieson another collectable tool maker in the early 19th century. This item would be sought after by wood working tool collectors and it gives us a snapshot of how cabinet makers went about creating furniture during this time period. Wood Moulding plane Side Bead - Single Box type Stamped Manners (Maker) (also inside stamped GN, & W, M. Nicol also F W. probably owners of item over the years.)flagstaff hill, warrnambool, shipwrecked-coast, flagstaff-hill, flagstaff-hill-maritime-museum, maritime-museum, shipwreck-coast, flagstaff-hill-maritime-village

During 1978 strips of tickets were used on the Nursery and Link lifts at Falls Creek. For each ride a ticket was torn off by the operator at the bottom of the lift. Ski lift tickets have changed often during the years from single lift coins, single tickets, day tickets, electronic tickets. The names and existence of lifts has also changed over time.In 1978 ski lift tickets were sold as a strip of 7 and operators were employed on each lift to collect them. Falls Creek is a major ski resort in Victoria and Australia. This strip has been superseded by other forms of 'tickets' sold at Falls Creek. This ticket also names 2 of the lifts which operated in 1978. Seven ski lift tickets attached as a strip to a butt. They are for the Nursery lift or the Link Lift at Falls Creek for the 1978 season. The writing is black on white and the strip has a thick green stripe down the length of it. In red at the top hand written: "Please Use."ski lift tickets. falls creek. alpine sport. downhill skiing.

These books celebrate the 130th anniversary of the establishment of the Warrnambool Art Gallery. This Gallery is owned and operated by the Warrnambool City Council as a memorial to Sir David Fletcher Jones who was nationally known and a leading citizen in Warrnambool for many years as a businessman (Fletcher Jones and Staff) and as a philanthropist. The Warrnambool Art Gallery was founded in 1886 and is the third oldest institutional collection in Victoria and the fifth oldest in Australia. This book is of considerable interest as it reproduces many works of art from the Warrnambool Art Gallery, a highly significant collecting institute in Warrnambool. These are two copies of the book containing 130 reproductions of works of art (both in colour and in black and white) held at the Warrnambool Art Gallery. It is a soft cover book of 128 pages edited by Vanessa Gerrans. The cover designed by Ian Robertson has a white background and the shapes of the Warrnambool Art Gallery logo have been used as multi-coloured windows containing details of each of the 130 reproduced works. The title of the book is in black print. As well as the reproduced works of art the book contains A Message from the Mayor, notes on the Friends of the Warrnambool Art Gallery and the Warrnambool Art Gallery Foundation and an article on the history of the Art Gallery. warrnambool art gallery, warrnambool city council, david fletcher jones, history of warrnambool

This blazer would have been worn by a member of the Warrnambool District Football Umpires Association at formal and social occasions. This Association was founded in 1946 and continues today, providing umpires for football matches in the Warrnambool District including the Hampden Football League.This uniform came from a Collectables Shop in Fairy Street, Warrnambool but the original owner is unknown. The blazer is a memento of a Warrnambool sporting group of interest and would be useful for display.This is a black cloth blazer with beige and black bands on the sleeves and pockets. It has one silver coloured button and one missing at the front. Inside the blazer is black lining at the top. The sleeves have a white and black pin striped lining. The pocket has the Association badge embroidered with beige and tan. There is a maker's label inside the front collar and a loop for hanging the blazer on a hook.PURE WOOL Ince Bros. Melbourne Tailors and Blazer Specialists. W.D.F.U.A. WARRNAMBOOL DISTRICT FOOTBALL UMPIRES ASSOCIATION FOUNDED 1946uniforms, warrnambool and district football, warrnambool district football umpires association

This album contains cigarette cards dating from the early 20th Century. The cards include Australian and English cricketers, Australian footballers, animals, racehorses, ships, Pacific Islanders, jockeys, actors and other famous people. The cards come from a variety of Australian and English cigarette companies. The album comes from the Edwards family who lived on the MORVEN property situated about 11 kilometres west of Branxholme in the Western District of Victoria. This property was sub divided in 1911 into 25 farms. There was once a Morven School and today there is a road of that name in the area.. This album is of considerable significance as it has historical value as an early collection of cigarette cards. Collecting of cigarette cards was a major social activity amongst young people, particularly in the first half of the 20th Century. It was a profitable advertising ploy for cigarette companies. Card and small object collecting by children today is still popular and used as an advertising mechanism. This album has a worn cover in faded green and fawn colours with a blue spine almost wholly detached. The back cover is stained. The cover has text. There are eighteen double sided pages with cut spaces for holding seven cigarette cards on each. Most of the pages contain black and white, sepia or coloured cigarette cards. There is an inscription on the first page.To Bennie from Auntie Lou. Xmas 1908cigarette cards, morven, edwards family morven, album

This glass dish would have been used for holding sweets or savouries or small cakes or biscuits.This item, highly collectable Carnival -Ware, is kept for display purposes.This is a Dugan marigold Carnival- ware glass bowl. It is made of iridescent pressed glass.It has an pressed image of a horse's head in the centre surrounded by a patterned rim and fluted edges.vintage household item., glass dish, carnival ware

This cup was produced by Ken Sadler as a souvenir of the 150th anniversary of the settlement of Warrnambool. Ken Sadler was a potter in Liebig Street, Warrnambool for many years (end of 20th century and beginning of 21st century). Warrnambool was founded as a planned town in 1847 to provide port facilities for the produce of squatters who had settled in the area. The town centre was surveyed by William Pickering at the request of Superintendent La Trobe of Melbourne and the first land sales were held in Melbourne in July 1847. The celebrations to mark the 150th anniversary of Warrnambool included concerts, race meetings, church services and the erection of an anniversary tablet on Cannon Hill. Ken Sadler, a well-known Warrnambool potter, made 500 of these cups which are now collectible souvenirs of the city’s 150th anniversary celebrations. This one retained by the Warrnambool and District Historical Society is numbered 189. The 150th anniversary of the founding of Warrnambool was an important event in the city’s history.This is a ceramic cup with a round base and larger rounded body with a round overhanging rim at the top opening. The cup is mottled green with an impressed image of a ship and lettering in white, gold and brown. There is some lettering on the bottom of the cup.‘Warrnambool 150th Anniversary 1847-1997’ ‘Sadler 97 189/500 Warrnambool’ warrnambool’s 150th anniversary, history of warrnambool, ken sadler, warrnambool potter