This booklet gives a brief description of the local settlement in Canterbury giving the landholders names and name of the house (before street numbering was introduced) and street it was located in.This booklet gives a brief description of the local settlement in Canterbury giving the landholders names and name of the house (before street numbering was introduced) and street it was located in.canterbury, (ms) jane f portingale, postmistress, (mr) arundel wrighte, wood brothers, koonung creek, (mr) thomas power, (mr) oliver russell, (mr) frederick griffin, (mr) thomas payne, shrublands, w creek, (mr) john gardiner, (mr) james shanley, (mr)robert hoddle, (mr) michael logan, (mr) patrick moloney, (mr) hugh glass, r. larkins, t. hassett, e. sturt, d.s. campbell, (mr) joseph camm, riversdale road, w. logan, rochester road, 1843, trees, mont albert road, a. sikes, (mr) william smith, 1853, (mr) ernest carter, dentist, elgar's surrey, hindson family, (mr) george granville mercy, (mr) alfred golding, (mr)alexander patterson, (mr) thomas boanas, (mr) thomas hyde, builders, (mr) richard terrill, architects, (mr) thomas miles, drapers

This is an extract/copy of an original photo that showed both Alfred and Charlie D'Alton together. (see Record # 126 for section with Charles D'Alton and Record # 117 for the entire photo).Photo of Alfred D'Alton looking for gold on Stoney Creek.people, d'alton, mining, stoney creek

Frances Gertrude Gladstone was born on the 18th of September 1919 to Arthur George Ladson and Gertrude Hunrick Irving. France's grandfather, Alfred Ladson, came Beechworth from Norfolk, England, during the gold rush. Alfred had a grocery business, and was well known for writing letters for the miners to send to their families. Alfred also travelled to Beechworth with his sister, who was a trained nurse and helped establish a hospital for the goldfields. Frances remembers her father saying the Chinese miners were not allowed to bring their families to the goldfields, hence there were no Chinese children in schools around Beechworth. Frances was an avid botanist, and wrote a book called 'The Little Huntsman', which she wrote while watching her husband gold mining. This oral history recording was part of a project conducted by Jennifer Williams in the year 2000 to capture the everyday life and struggles in Beechworth during the twentieth century. This project involved recording seventy oral histories on cassette tapes of local Beechworth residents which were then published in a book titled: Listen to what they say: voices of twentieth century Beechworth. These cassette tapes were digitised in July 2021 with funds made available by the Friends of the Burke.Frances Gladstone's story is significant, as she remembered important information about Chinese miners in the gold rush, explained the role of women in the 20th century in Beechworth, and the history of the hospitals in the region. This is a digital copy of a recording that was originally captured on a cassette tape. The cassette tape is black with a horizontal white strip and is currently stored in a clear flat plastic rectangular container. It holds up 40 minutes of recordings on each side.listen to what they say, beechworth, oral history, burke museum, botanist, chinese miners, goldmining, gladstone

This particular geological specimen was found in Mount Franklin or Lalgambook in Djadjawurrung, located between Daylesford and Newstead, approximately ninety minutes drive from Melbourne. The mountain is an example of a breached scoria cone (a steep conical hill of loose pyroclastic fragments) which was created by a volcanic eruption about 470,000 years ago, a date which may indicate the age of this geological specimen. The volcanic eruptions of Mount Franklin were most likely witnessed by members of the Dja Dja Wurrung Aboriginal tribe, who referred to this country as the 'smoking grounds'. Mount Franklin and the surrounding area appears to have been a place of considerable religious significance to Aboriginal people, there is evidence which indicates that frequent large ceremonial gatherings took place in the area. Basalt is the most common rock on Earth’s surface, more than 90% of all volcanic rock on Earth is basalt. Basalt is an aphanitic extrusive igneous rock formed from the rapid cooling of low-viscosity lava exposed at or very near the surface of a rocky planet or moon. Specimens are black in colour and weather to dark green or brown. Basalt is rich in iron and magnesium and is mainly composed of olivine, pyroxene, and plagioclase. Olivine is the name of a group of rock-forming silicate minerals with compositions ranging between Mg2SiO4 and Fe2SiO4. Unlike other minerals, Olivine has a very high crystallisation temperature which makes it the first of the minerals to crystallise from magma. As magma cools, the crystals begin to form and settle on the bottom of the lava and form basalts that are abnormally enriched in olivine in the lower part of lava flows. According to H. M. King (on geology.com) "Olivine is thought to be an important mineral in Earth's mantle. Its presence as a mantle mineral has been inferred by a change in the behaviour of seismic waves as they cross the boundary between Earth's crust and mantle". Lava from Mount Franklin and other volcanoes in the area filled valleys and buried the gold bearing streams that became the renowned ‘deep leads’ of the gold mining era. In 1852, as part of the Victorian gold rush, gold was discovered in the immediate area, this gold was created by lava flows during the Newer Volcanic period, which were mined intensively during the nineteenth century. Around 1865 the presence of a deep lead in Mount Franklin was established. Deep lead mining was initially unsuccessful, and it was not until the late 1870s that the Franklinford Gold Mining Company mined at Mount Franklin on a significant scale. A few years later the Mount Franklin Estate Gold Mining Company also struck gold, followed by the Shakespeare and Great Western companies in the mid-1880s. By the late 1880s, however, deep lead mining had ceased in the area. Soon after gold was discovered in 1851, Victoria’s Governor La Trobe wrote to the Colonial Office in London, urging ‘the propriety of selecting and appointing as Mineral Surveyor for this Colony a gentleman possessed of the requisite qualifications and acquaintance with geological science and phenomena’. Alfred Selwyn was appointed geological surveyor in Australia in 1852 which began the Geological Survey of Victoria. In 1853-69 the Geological Survey issued under Selwyn's direction sixty-one geological maps and numerous reports; they were of such high standard that a writer in the Quarterly Journal of the Geological Society of London bracketed the survey with that of the United States of America as the best in the world. During his years spent in Australia, Selwyn collected numerous significant geological specimens, examples of which are held in collections such as the Burke Museum.This geological specimen is an example of basalt and olivine which shows the volcanic lava activity and geographical specific nature of Mt Franklin as a significant volcanic site. According to Agriculture Victoria 'The crater is one of the deepest in the Central Highlands area. It is a major megacryst site with some of the largest known Victorian examples of megacrysts of augite and an orthoclase. The small parasitic mound of Lady Franklin on the western flanks adds to the geological interest of the site'. This specimen also highlights the locality as a significant place for both indigenous activity and Victorian gold rush era mining practices. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.An angular, solid hand-sized piece of grey volcanic Basalt with green/brown Olivine phenocrysts along one flat edge.Olivine in basalt / - label is probably / correct. / C. Willman / 15/4/21burke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, mineralogy, basalt, igneous rock, igneous-volcanic, volcanic geology, volcanic, olivine, olivine specimen, basaltoid

Coorongite is a dark, rubber-like, highly resilient structureless algal deposit. In the Coorong district of South Australia it occurs in moderate quantities associated with the coastal swamps and sand dunes which extend for a considerable distance east of the mouth of the Murray. This particular specimen was recovered from the south of the Coorong River, South Australia. A type of sediment rich in organic matter, Coorongite is the unlithified end-member of the sapropelic coal series. The members of the sapropelic coal series can be ranked in order as sapropel (the unlithified form), sapropelic-lignite, and sapropelic-coal (the lithified forms) based on increasing carbon content and decreasing volatile content. Sapropel (Coorongite) is an unlithified dark, pulpy, fine organic mud containing concentrations of algae and miospores that are more or less identifiable. Coorongite is typically found as an algae like substance, that can be found in irregular size pieces. Coorongite was believed to be dried up oil due to its rubber-like texture. The Coorongite is also soft to the point where it can be cut into with a knife or it can be broken and torn by hand. Otherwise known as 'Kurangk', the Coorong River is home to the Ngarrindjeri people, which acts as both a place for gathering food and a spiritual place. In 1852 the first sight of Coorongite was found along the Coorong River. The finders mistook the Coorongite for dried up oil, which lead to the belief that there were oil reserves under the Coorong River. Between the 1860s and the 1930s the Coorong River became a place where mining oil and Coorongite became precedent. Nowadays, the local council and the South Australian Government are working together with the Ngarrindjeri people to sustain and preserve the Coorong River and the culture that is with it. Soon after gold was discovered in 1851, Victoria’s Governor La Trobe wrote to the Colonial Office in London, urging ‘the propriety of selecting and appointing as Mineral Surveyor for this Colony a gentleman possessed of the requisite qualifications and acquaintance with geological science and phenomena’. Alfred Selwyn was appointed geological surveyor in Australia in 1852 which began the Geological Survey of Victoria. Selwyn went on to collect geological samples and catalogue thousands of specimens around Australia. In 1853-69 the Geological Survey issued under Selwyn's direction sixty-one geological maps and numerous reports; they were of such high standard that a writer in the Quarterly Journal of the Geological Society of London bracketed the survey with that of the United States of America as the best in the world. During his years spent in Australia, Selwyn collected numerous significant geological specimens, examples of which are held in collections such as the Burke Museum.Coorongite is considered to be a mineral with a unique texture, where it can be both hard and soft. Coorongite can also be considered to be a rare mineral, as it is only located along the Coorong River and due to the mining of it, has left very few sources. It was believed at one point that Coorongite could be used to replace oil. 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.Three solid varyingly hand-sized pieces of wooden appearing organic matter derived from the river in the Coorong District in South Australia. A rubber-like, highly resilient structureless algal deposit.Specimen 245 page 69 / in Descriptive Register / "Elcestic Bitumen, / Coorangite" South of / Coorung River, South Australia . / C. WIllman / 15/4/21burke museum, beechwoth, indigo shire, beechworth museum, geological, geological specimen, mineraology, coorong, coorong river, kurangk, ngarrindjeri, south australia, coorongite, coorongite specimen

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

Alfred 'Alf' Spencer grew up on a dairy farm run by his mother, west south west of Beechworth 'down Robertson Road', and was very well connected to the wider Beechworth area. In this oral history, he recalls his time driving the milk cart around Beechworth as well as the time he spent buying lollies and seeing the pictures. He talks extensively about working as a butcher at his brother's store, including how the butchers interacted with the rest of the town and the staff, as well as his time constructing roads and the pipe network of Beechworth. He discusses the dynamics of other workplaces around Beechworth, describing issues with how the local tannery treated its workers as well as how post-war migrants integrated across the town. He briefly discusses racial tensions between Chinese migrants and other miners on the goldfields. He also discusses the experience of health care in a rural area during his childhood. This oral history recording was part of a project conducted by Jennifer Williams in the year 2000 to capture the everyday life and struggles in Beechworth during the twentieth century. This project involved recording seventy oral histories on cassette tapes of local Beechworth residents which were then published in a book titled: Listen to what they say: voices of twentieth century Beechworth. These cassette tapes were digitised in July 2021 with funds made available by the Friends of the Burke.Alfred Spencer's oral history of his life around Beechworth during the 20th century is historically and socially significant to the cultural history of the region and Victoria. There is a lot of detail about workplaces, their staff, and how the resources of the town interacted. He explores themes that are important to Victorian history, such as migration. This oral history account is socially and historically significant as it is a part of a broader collection of interviews conducted by Jennifer Williams which were published in the book 'Listen to what they say: voices of twentieth-century Beechworth.' While the township of Beechworth is known for its history as a gold rush town, these accounts provide a unique insight into the day-to-day life of the town's residents during the 20th century, many of which will have now been lost if they had not been preserved.This is a digital copy of a recording that was originally captured on a cassette tape. The cassette tape is black with a horizontal white strip and is currently stored in a clear flat plastic rectangular container. It holds up to 40 minutes of recordings on each side.Mr Alfred Spencer /listen to what they say, beechworth, oral history, burke museum, spencer, alfred spencer, migration, post-war migration, goldfields, health care, farm, farming, dairy farm, black springs, butchers, meat processing, butcher, road, road network, labour relations

Dolomite is a mineral, calcium magnesium carbonate, with the chemical formula CaMg(CO3)2. It is a principle component of various rock types sometimes also referred to as dolomite, including dolostone, dolomitic marble and dolomitic limestone (according to the composition of each type). Dolomite rock is found in sedimentary basins throughout the world, comprising approximately 2% of the Earth's crust. It is formed when lime mud or limestone encounters groundwater containing magnesium. Dolomite can contain elements such as lead, zinc and copper. Dolomite and limestone are used in various construction, landscaping and agricultural processes. This specimen was donated to the Burke Museum in 1868 by Alfred Selwyn as part of 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. Dolomite and limestone are mined at several locations in Victoria, including sites in the North-East of the state in Bindi and Limestone Creek. There are notable dolomite deposits in most Australian states. The dolomitised form of the mineral tends to come from older limestone deposits, formed during the palaeozoic era in marine settings, so this specimen may have come from a deposit located along a coastline in Victoria or another state. The specimen is significant as an example 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. 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.Hand-sized piece of pale pink dolomite (calcium magnesium carbonate) with dark grey rim and hollowed centre. geological specimen, geology, geology collection, burke museum, beechworth, dolomite, mineralogy, geological survey, alfred selwyn, limestone, calcium magnesium carbonate

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

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

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

Idylls of the King,first published between 1859 and 1885, is a cycle of twelve narrative poems by the English poet Alfred, Lord Tennyson (1809–1892) who was the Poet Laureate from 1850. It retells the legend of King Arthur, his knights, his love for Guinevere and her tragic betrayal of him. The book was given by Emmie Gibbs as a Christmas gift to Hilda Wehner. Hilda Wehner was the daughter of Herman Wehner (1862-1937) one of Orbost's early blacksmiths.A small red cloth covered book with a black motif on the cover. There is gold print on the spine.Inside- To Hilda M. Wehner from her friend Emma Gibbs wishing her the complimenst of the season Xmas 1916tennyson literature idyls-of-the-king book

This photograph shows Nelson Burn reading a telegram from the queen to his grandmother, Mrs Paul Hocking, on her 100th birthday. Her husband, James Hocking, was the first watchmaker in Orbost. He had been a lay preacher at Wangaratta and Yan Yean before coming to Orbost. He was an 1891 Rechabite and an Orbost Shire Councillor. Eliza Ann Hocking (nee Eddy) was born on 16.7.1856 at Blackwater Hall in England, She had arrived in Australia on the sailing boat "Poocia" on 8-7-1880. The voyage following the Cape route took about 7 weeks. For a time, with her husband, she lived at Chewton, on the gold fields, before coming to Orbost. She was a foundation member of the Methodist Ladies’ Guild in 1912. She lived in Salisbury Street, Orbost. She died on 9.4.1957. Colin Nelson Burn, born 7.7.1921, was her grandson, son of Robert Alfred Burn and Edith Jane Hocking. He began Sta-Brite' Painting and Decorating Services in Salisbury Street, Orbost. He served in the forces during World War II. He was a Life member of the Snowy Rovers Football Club. He joined the Orbost Fire Brigade on 1-5-1946. He died 1.2.2015. His son, Peter continues the painting business in Orbost. (info. from John Phillips)This is a pictorial record of an Orbost resident reaching 100 years. A 100 year birthday is a significant milestone. The Hocking / Burn family have been associated with the Orbost district since 1889.A large black / white photograph of an elderly lady standing beside a younger man who is holding a letter and reading to her.hocking-mrs burn-nelson telegram-queen-100th-birthday

This was the House Cup of a Warrnambool private school, Braemar Grammar. It operated from 1931 to 1950 and was in Manifold Street. The school had an average enrolment of 45 primary school students and closed because of the unavailability of suitable school premises. The donor of the House trophy, Dr Alfred Brauer, was born in South Australia and studied medicine at Melbourne University. He had a practice in Koroit Street Warrnambool for 45 years and had many community interests including horse racing, football, golf, cricket and education. He was associated with Warrnambool High School, Braemar Grammar School and Warrnambool Technical School, donating trophies to all three schools. Today the former Warrnambool Technical School is called Brauer College. This cup is of interest as a memento of a 20th century private school in Warrnambool, Braemar Grammar and of a prominent 20th century doctor in Warrnambool, Dr Alfred Brauer.This is a gold-coloured metal cup with two side handles and a long thin stem on a metal base mounted on a Bakelite stand. The lower portion of the stand is missing. The cup is much stained.This is a gold-coloured metal cup with two side handles and a long thin stem on a metal base mounted on a Bakelite stand. The lower portion of the stand is missing. The cup is much stained.braemar grammar school, warrnambool, dr brauer, warrnambool

Brauer College is situated in Caramut Road, Warrnambool . It's origins date back to 1913 when Warrnambool Technical School was established in Timor Street, Warrnambool. In 1972 this school was re located to Caramut Road and in 1990 was renamed Brauer College after Dr. Alfred Brauer , a noted doctor in Warrnambool closely connected to the development of the Technical School.These items are of interest as mementoes of Brauer College, a leading educational institution in Warrnambool today. .1 Circular metal tie pin with burgundy outer circle edged in golden lines and text, burgundy stylised sea horse with gold coloured outline, stylised green waves with gold coloured lines in centre. Pin and press clip on back roughened gold coloured metal . .2 Oval metal brooch with golden rim, top section is green, middle section is burgundy, lower section is pale yellow. A stylised pale yellow, golden edged sea horse is sited on the right hand side at the base of the middle section and extends into the upper area. There is text in the middle section. A pin clip on the roughened gold coloured back. .3 Identical to .2.1 BRAUER COLLEGE .2 BRAUER COLLEGE WARRNAMBOOL .3 BRAUER COLLEGE WARRNAMBOOL

This glass is a souvenir of the 75th anniversary of the founding of Warrnambool Technical School. This school was established in Timor Street Warrnambool in 1913 and was relocated to Caramut Street Warrnambool in the 1970s. The Timor Street site now has the campus of South West TAFE (Technical and Further Education). Warrnambool Technical School in Caramut Road was re-named Brauer College in 1990 to reflect the change to a broad secondary curriculum embracing both technical and general educational subjects. The name also honours Dr Alfred Brauer, a well-known Warrnambool doctor with a strong involvement in local schools. This glass is of interest as a memento of the 75th anniversary of the founding of Warrnambool Technical School, today known as Brauer College.This is a glass tumbler with a heavy base and a gold rim around the top of the glass. The sides of the glass have a gold image of a school, the school logo (a seahorse) and some gold printing. Warrnambool Technical School 1913-1988warrnambool technical school, history of warrnambool

Commissioned by George W. Bell, designed by Anthony Harvey. An old gold mining and wine growing district eighteen miles from Melbourne, now notable for its arts, crafts, good food and historic buildings. On the reverse side (of one copy only) is printed in 8 panels (3 half-folds) advertising for Montsalvat, Eltham; Setel Downs Coffee Kitchen Art Gallery, Kangaroo Ground; Country Art Store, Eltham; Alfred's Homestead, Warrandyte; Neville F Emmerson Estate Agent, Lower Plenty; Eltham Crafts. Monstsalvat, Eltham; Tantoon native plants and culinary herbs, Eltham; Flavour of Eltham, Shillinglaw Coattage Preservation Society; The Eltham Barrel; Potters Cottage, Warrandyte. In addition is provided by cateogory listing: POTTERY AND CRAFTS Country Art Store, Eltham Diamond Creek Handicrafts, Diamond Creek Eltham Crafts, Eltham John Mills, Eltham Potters Cottage, Warrandyte Setel Downs, Kangaroo Ground The Claypot, Warrandyte Warrandyte Quarries and Pottery, Warrandyte GOOD FOOD AND DRINK Alfred's Homestead, Warrandyte Geranium Parlour,. Research Inglenook, Warrandyte La Ronde, Eltham The Barrel, Research The Potters Restaurant, Warrandyte Setel Downs, Kangaroo Ground GALLERIES Hassall's Gallery, Research Lodge Gallery, Warrandyte The Bird Gallery, Eltham Royalat Gallery, Panton Hill PLANTYS, TREES AND SHRUBS Danson's Gardens, Research Dean's Orchids & Dahlias, Templestowe Diamond Vlley Trees & Shrubs, Warrandyte Jum Jum, Diamond Creek Parson's, Research Tantoon, Eltham Warran Glen, Warrandyte44..8 x 57.5 cm (Two copies) On the reverse side (of one copy only) is printed in 8 panels (3 half-folds) advertisingeltham, warrandyte, map, country art store, diamond creek handicrafts, eltham crafts, john mills, potters cottage, setel downs, the claypot, warrandyte quarries and pottery, alfred's homestead, geranium parlour, inglenook, la ronde, the barrel, the potters restaurant, hassall's gallery, lodge gallery, the bird gallery, royalat gallery, danson's gardens, dean's orchids & dahlias, diamond vlley trees & shrubs, jum jum, parson's, tantoon, warran glen, advertising, eltham barrel

Located on the north side of Bridge Street at the intersection with Bolton Street, facing Bolton Street (now part of present day Brisbane Street and occupied by the Kitchen Design Centre). Show's an original early settler's cottage in Bridge Street. The cottage was built by Mrs Mary Jane Smart's parents, Edwin Bailey and Jane (nee Matthews). Mary Jane Smart was born in the cottage. She married an Englishman, Alexander Wilson Smart who disappeared to Western Australia in the early 1900s in search of gold. He ultimately married again in W.A., committing bigamy and then committed murder and was hung in 1911. This photo was taken c.1903 not long before both Mrs Bailey and her grand daughter both passed away. Jane Bailey died 2 Dec. 1904 and Mary Jane Smart and Ruby Jane Bertha Smart died July 1903 are all buried in Eltham Cemetery. SMART'S HOME AT ELTHAM. HIS WIFE AND SONS. In a little bush cottage surrounded by tall gum trees, through which appear glimpses of a willow fringed creek, of road ways hedged by masses of snowy flowering hawthorn, of growing crops and vividly green grazing paddocks, lives Mrs. Smart, the lawful wife of the man who is now in the hands of the police of Western Australia on suspicion of having committed a dreadful crime. Here, about half a mile out of the picturesque village of Eltham, she was born, and has lived her whole life — about 50 years. Smart himself lived here till the time when many years ago, the "lure of gold" got into his blood and he cleared out to Western Australia, to follow the digging rushes, gradually becom ing more and more estranged, till at length all communication ceased and be became lost to his wife and children. "I did not want him to go away," said Mrs. Smart, "because I had heard of so many men who had forgotten their homes in the excite ment of gold seeking, and of many others who died unknown and uncared for. But he would go, and when I saw his mind was set on it I placed no obstacles in his way. My parents built and lived in this cottage, where I was born, and they died in it. When I grew up I met my husband, a young Englishman, and married him. His name is Alexander, not Alfred, and his age is 52. We were very happy here, and although we were not well off we were comfortable, for he was a steady, sober, industrious man and had constant employment. He was just a manual worker, but could turn his hand to anything. We had five children, but one died. Four sons grew up in this little cottage. Thus three generations lived in it, somewhat unusual in an Australian bush home, I think. My eldest son is married and has a family; one is in Western Australia— not with his father— another is away working for him self, and one (indicating a young man by her side) has always stuck to his mother. He is my sole support, and he is as good to me now as his father once was. Yes, his father was a good, home-loving man in our younger days. He was fond of his children and was highly respected in these parts.' "It is fifteen years since my husband went away first. He had then been work ing for the Metropolitan Board of Works, and was engaged in the tunnel under the Yarra near Queen's-bridge when it col-lapsed. After he went to the West he sent me money regularly and wrote constantly. He came home three times — twice for a week or two at a time, the third time, eight years ago, when the Eitham railway was nearing completion. I induced him to stay till the railway opened, and he re-mained with me several months. I tried to get him to leave the West and settle down in his home, but he would not; he seemed restless and anxious to be off. One day when we were in Collingwood together he left me, saying he wanted to see what boats were going West. I implored him not to go away, and he said he would see. However, he returned to me soon after wards and said he had taken his ticket and would go by the next boat, and he went. For a year he wrote at irregular intervals, and then his letters ceased and I heard no more of him. For seven years I have not known whether he was alive or dead. Before that time my two sons in Western Australian used to see him some times, though they did not live with him; they used to tell me in their letters that he was well. It was a hard blow to be forgotten by him, but as my sons grew up I became more reconciled, and now I seem to look back at my life with him as some thing that happened a long time ago and is only a memory. Of his life and doings in Western Australia I know nothing. The last time I heard of him he was working in a foundry at Midland Junction. He was at Cue working on the railway when it opened there, and he caught the fever, but all that time he sent me money. When he returned the first time he took our eldest son with him, and the other boy followed later. They did not stay with him, how ever, and as far as I know they did not know how he lived." 'Mrs. Smart is a quiet, toil worn woman who has the respect of everyone who knows her.Roll of 35mm colour negative film, 3 strips Associated print from negative (Copy of original print)Fuji 100bridge street, cottage, smart home, houses, mary jane smart (nee bailey), smart family home, alexander wilson smart, bigamy, bush cottage, early settlers, eltham, jane bailey (nee matthews), murder, ruby jane bertha smart

This book prize was awarded to Theophilus Heugist Serjeant in the fifth form for first prize for arithmetic. Theo enrolled at Ballarat College in 1884 at the age of 12. Theo's brother, Alfred George Serjeant, also enrolled at the same time at the age of 17. In the original register parent/guardian is listed as R.M Serjeant and their residence as Yarrowee Hall.Presbyterian educators placed great value on a classical education matched with diligence in study. Book prizes were highly regarded and academic success admired. In the school’s early years prizes were ordered direct from London and had the school crest embossed in gold on the front or back cover. Many of the prizes given in early years were returned to the school to equip the Weatherly Library when it opened in 1936.Bound in brown calf with black and gilt decorations on front cover and black decoration with college crest embossed on back cover. Six raised bands on spine with gilt lettering on second compartment and the remaining compartments with gilt decoration. Slight detachment of spine with foxing on pages. Gilt edged pages, black and white illustrations throughout. 624 pages.Book plate inside front cover: college crest/ Arithmetic/ Fifth Form,/ First Prize./ Awarded to/ Theo. H. Serjeant/ Christmas, 1887.theophilus-heugist-serjeant, book-prize, ballarat-college, 1884, alfred-george-serjeant, r-m-serjeant, yarrowee-hall.

Prize awarded to Raymond Percival Thomas Oxlade, Dux of Remove Upper 1932. Raymond entered Ballarat College 1932. Raymond was born 24 June 1917 at Ballarat, the son of Percy Alfred and Ruby Evelyn (Davies) Oxlade. He enlisted in the Australian Armed Forces in 1940. He transferred to the RAAF in 1942 and was discharged 1946. Raymond's grand-daughter Jessica Oxlade entered the school in 2007, achieving Dux of the school in 2010.Maroon calf binding with decorative gold embossing on cover and spine; gilt title and publisher statements on spine and school crest on front cover; book plate on front cover verso; marbled endpapers; pages gilt-edged and sight foxing; black and white frontispiece;Book plate: school crest / Ballarat College / Remove (Upper) Form / Dux Prize / Awarded to / R P T Oxlade / A Richardson / December 1932 / Principalraymond-percival-thomas-oxlade, 1932, ballarat-college, book, prize, a- richardson, jessica-oxlade, dux

Prize awarded to Raymond Percival Thomas Oxlade, Dux of Fifth A (Upper) 1934. Raymond entered Ballarat College 1932. Raymond was born 24 June 1917 at Ballarat, the son of Percy Alfred and Ruby Evelyn (Davies) Oxlade. He enlisted in the Australian Armed Forces in 1940. He transferred to the RAAF in 1942 and was discharged 1946. Raymond's grand-daughter Jessica Oxlade entered the school in 2007, achieving Dux of the school in 2010. Maroon calf binding with decorative gold embossing on cover and spine; gilt title and publisher statements on spine and school crest on front cover; book plate on front cover verso; marbled endpapers; pages gilt-edged and slight foxing; black and white frontispiece;Book plate: school crest / Ballarat College / Fifth A (Upper) Form / Dux Prize / Awarded to / R P J Oxlade / R E Thwaites / December 1934 / Principalraymond-percival-thomas-oxlade, ballarat-college, 1934, dux, r-e-thwaites, jessica-oxlade

Prize awarded to Raymond Percival Thomas Oxlade, Dux of Fifth A (Upper) 1934. Raymond entered Ballarat College 1932. Raymond was born 24 June 1917 at Ballarat, the son of Percy Alfred and Ruby Evelyn (Davies) Oxlade. He enlisted in the Australian Armed Forces in 1940. He transferred to the RAAF in 1942 and was discharged 1946. Raymond's grand-daughter Jessica Oxlade entered the school in 2007, achieving Dux of the school in 2010. Red calf binding with decorative gold embossing on cover and spine; gilt title and publisher statements on spine and school crest on front cover; book plate on front cover verso; marbled endpapers; pages gilt-edged and sight foxing; black and white frontispiece;Book plate: school crest / Ballarat College / Remove (Upper) Form / Dux Prize / Awarded to / R P J Oxlade / R E Thwaites / December 1932 / Principalraymond-percival-thomas-oxlade, ballarat-college, dux, 1934, jessica-oxlade

Rosina (Rose) Morey was a student at Ballarat Ladies College, girls' school of Ballarat College (1875 - 1892). Rosina Morey was born in 1871 and spent most of her life in Ballarat. Her father was Edward Morey, a mining and civic leader in Ballarat. The book was donated by Poss Morrow (Walker) having belonged to her great aunt Rose Morey. In 2008 Poss wrote: Rose loved sewing and my memories of her are that she was always dressed in black. She was the third daughter of Edward and Mary Ann Morey. Great aunt Rose spent many happy times with our family when we lived in East Malvern. My father Edward McDonald Walker was her nephew. She loved coming to the city by train to go shopping and join in the family celebrations. She never married but lived to a great age. She died in a nursing home in East Malvern 24 July 1960 and was buried in the Morey family grave in the Ballarat Old Cemetery. The prize, presented to Rose in 1889, remained in my father's library for many years and was given to me recently.Red calf-binding with fine gold border to cover; gold lettered title and school crest to front cover; and gold lettered title to spine. Book plate on inside of front cover. Book plate on inside of front cover: School crest / Fancy Needlework / Senior Form / "Gross" prize / Awarded to / Rose Morey / Christmas 1889rose-morey, ballarat-ladies-college, book-prize, needlework