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The Beechworth Burke Museum
Geological specimen - Ropy Lava
‘Ropy lava’ is known for its sculptural and layered qualities. It occurs in specific lava flows that are slow moving and slow cooling, allowing for unique formations to be created out of the motion. Ropy Lava is a flow that has a hardened crust with molten material underneath, the tension between these states is what creates its characteristic form. The brown/red hue of the stone is an indication of age, as it is oxidised iron deposits. This rock deposit is thought to be sourced from the area by Talbot, in western Victoria. This area has a rich mineral history and experienced the gold rush in the 1850's. The traditional owners of this area are the Dja Dja Wurrung people.This geological specimen shows the conditions in which the Australian landscape was created as well as provides an indication as to how these events occurred. It is representative of a common natural process that contextualises the formation of Australia with the formation of other landmasses. 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 specimen in brown/red hues42 / victoria, talbot, lava, ropy, ropy lava, mineral, geological specimen, geological, geological heritage, natural stone, natural history -
The Beechworth Burke Museum
Geological specimen - Basalt (igneous-volcanic) containing Olivine, unknown
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 -
The Beechworth Burke Museum
Geological specimen - Coorongite
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 -
The Beechworth Burke Museum
Geological specimen - Brown Coal
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 -
The Beechworth Burke Museum
Geological specimen - Smoky quartz crystals, unknown
Quartz is an extremely common mineral to find across the world. Quartz can have two forms; Microcrystalline quartz or Crystalline quartz. Microcrystalline quartz is a fine grain quartz where crystalline quartz is often a large crystal. This specimen is a crystalline quartz. Made of silicon oxide, this specimen is called smokey quartz crystals because of its brownish colour. However, the colour of quartz can vary. In addition, quartz are formed in deep-seated igneous rocks and crystallized through hot aqueous solutions. This type of crystal can be found all over Australia, including Beechworth in Victoria. Other places quartz can be found is the Ashburton River area in Western Australia, Marlborough in Queensland, the Lune River area in Tasmania and Kingsgate in New South Wales. This specimen is significant because it is common to find this kind of mineral. While the location of where this specimen was originally from is unknown, it highlights the many places in Australia where quartz is found. It demonstrates that quartz makes up a large portion of Australia's geology. In addition, quartz itself can vary in its colour and shape. This specimen represents one of these variations. That being smoky quartz crystals. 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 large hand-sized quartz mineral with shades of brown and gray throughout.Smoky quartz / crystals /locality/ unknown / (needs a wash) /BBgeological specimen, geology, geology collection, burke museum, beechworth, microcrystalline, quartz, quartz mining, quartz reefs beechworth, smokey quartz crystals, crystals, crystalline, silicon oxide, brown, colour, igneous rocks, magma, ashburton river, western australia, marlborough, queensland, lune river, tasmania, kingsgate, new south wales, nsw -
The Beechworth Burke Museum
Geological specimen - Common Opal, unknown
Common Opal is a mineraloid that is non crystallising and is classed as an amorphous silicate, the chemical composition for Opal is SiO2 nH2O. Opals can develop in weathered sedimentary rock typical in arid regions where limited water enters small gaps in the rock, and the silicate is hydrated. Common opals, unlike precious opals, do not exhibit ‘play of colour’ in which the colour appears to change depending on the angle of view. While precious opals are highly valuable and cut as gemstones for jewellery, common opals can be cut into inexpensive gemstones and are also mined for various uses including as ingredients in ceramics, insulation, fillers, and abrasives. The source of this common opal specimen is unknown, but common opals are found around the world, notable deposits are found in Queensland, South Australia, New South Wales, Peru, Kenya, Nevada, Oregon, and Mexico. This common opal specimen is of historic and scientific significance due to its donation in 1868 as part of the Geological Survey of Victoria and as a typical example of uncut common opal. 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 amorphous (non-crystallising) hydrated silicate mineraloid specimen in shades of brown, orange, and white.Existing label: Common Opal / Locality unknowngeological specimen, geology, geology collection, burke museum, beechworth, common opal, opal, mineraloid, amorphous silicates, hydrated silicate -
The Beechworth Burke Museum
Geological specimen - Actionlite and Pyrite
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 -
The Beechworth Burke Museum
Geological specimen - Malachite, unknown
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 -
The Beechworth Burke Museum
Geological specimen - Oil shale
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 -
The Beechworth Burke Museum
Geological specimen - Amazonite, unknown
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 -
The Beechworth Burke Museum
Geological specimen - Malachite in Conglomerate, Unknown
Malachite is a green copper carbonate hydroxide mineral and was one of the first ores used to make copper metal. Malachite has been utilised as a gemstone and sculptural material in the past as its distinctive green color does not fade when exposed to light or after long periods of time. Malachite is formed at shallow depths in the ground, in the oxidizing zone above copper deposits. The material has also been used as a pigment for painting throughout history. Malachite is considered a rare gemstone in that the original deposits for the stones have been depleted leaving behind very few sources. In addition, the use of Malachite as gemstones and sculptural materials remains just as popular today as they were throughout history. It is quite common to cut the stone into beads for jewellery. The fact that Malachite has such a rich colour and one that does not fade with time or when exposed to light makes it particularly rare. Although there is no indication available of the locality from which the specimen was sourced, it is likely that the specimen was collected either in South Australia in the vicinity of the Burra Burra mines or in Victoria as part of programs of geological surveying undertaken in the Nineteenth and Twentieth centuries. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A solid hand-sized copper carbonate hydroxide mineral with quartz pebbles in red conglomorate matrix presenting shades of cream, brown and green.Existing label: Malachite / (green) in / conglomerate / (white quartz / pebbles / in red matrix /geological specimen, geology, geology collection, burke museum, beechworth, geological, indigo shire, malachite, malachite specimen, australian mines, mines, geological survey, conglomorate, matrix -
The Beechworth Burke Museum
Geological specimen - Galena (lead sulphide), Unknown
Galena occurs in a range of deposit contexts, often in metalliferous veins, such as Broken Hill, Australia; Coeur d’Alene, Idaho, United States.; Clausthal Zellerfeld, Germany; and Cornwall, England. Large deposits also replace limestone, dolomite, or occasionally organic matter, or have a contact-metamorphic origin. Galena is additionally found in cavities, brecciated (fractured) zones in limestone and chert, and in coal beds. This specimen was recovered from Broken Hill NSW and is 60% lead with 8-12 oz/silver to the ton.Galena or 'lead glance' is a grey lead sulfide and the chief ore mineral of lead. It forms isometric crystals in which the ionic lattice is similar to sodium chloride. Galena is brittle and easily weathers to secondary lead minerals, with the upper part of mineral deposits often containing cerussite, anglesite, and pyromorphite. It usually contains silver, which is mined along with its lead content. Other commercially important minerals that form in close association with galena are antimony, copper, and zinc. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A small-sized solid specimen containing one mineral with a sparkly silver metallic lustre exterior and pastel-grey interior.geological specimen, geology, geology collection, burke museum, beechworth, galena, lead sulphide, alfred selwyn, broken hill -
The Beechworth Burke Museum
Geological specimen - Anthracite crystal, Unknown
Anthracite typically occurs in geologically deformed areas due to extreme heating – with temperatures ranging from 170 to 250 °C – caused by igneous intrusions or high geothermal gradients. It is most commonly found in northeastern Pennsylvania in the United States; however, smaller amounts are also found in Australia, China, eastern Ukraine, South Africa, western Canada, and other countries. This specimen was recovered from Tasmania and is 85-95% carbon.Anthracite is the mineral name for hard coal and is the least plentiful of all coal types. It is clean to the touch and, when polished, is used for decorative purposes. Before natural gas and electricity, anthracite was used for domestic heating as it produces little dust, burns slowly, and gives off a minor amount of smoke. However, it is also limited in abundance and expensive. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A hand-sized highly metamorphosed coal mineral with a black/steel-grey shiny metallic lustre.geological specimen, geology, geology collection, burke museum, beechworth, indigo shire, geological, mineralogy, victoria, alfred selwyn, anthracite -
The Beechworth Burke Museum
Geological specimen - Common Opal, Unknown
It is not known where this opal originated. Common Opal is formed from silica-rich water entering the earths crust and hardening into a gel of water and silica-spheres, layered through the specimen. Common opal differs from precious opal in colouration and appearance, with precious opal including more colours, and having a translucent or glossy appearance, where common opal shows less colour and is typically opaque. It scores high on the Mohs hardness scale, and is common throughout the world, especially in Australia, where it is far more prevalent than the highly-prized precious opal. Australia is also the highest producer of opals in the modern world. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A solid, silica-based mineral specimen of Common Opal in shades of grey, green, and yellow, with a thick grey vein running through the centre. geological specimen, geology, geology collection, burke museum, beechworth, opal, common opal, gemstone, mining -
The Beechworth Burke Museum
Geological specimen - Selwynite, Unknown
Selwynite is a fine-grained, compact green rock made primarily of chromian muscovite (fuchsite) and diaspore. Corundum and fuchsite can occur together in the form of massive aggregates or nodules. Often, copper carbonates are found as earthy films or tiny crystals in joint planes. The mineral name honours the late A. R. C. Selwyn, founding Director of the Geological Survey of Victoria. The particular specimen, a mottled green stone suitable for carving was recovered and found in Heathcote, Victoria, Australia. The rarity and qualities of this mineral attracted commercial mining, which was not successful, but traces of the mine shafts still exist today, and it is still highly valued by mineral collectors.Selwynit is considered to be one of the rare forms of rock because it is composed of phosphate minerals containing zirconium. This is an extremely rare combination found in nature. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A fine grained rock composed of mainly of chromian muscovite (fuchsite) diaspore and corundum.geological specimen, geology, geology collection, burke museum, beechworth, mineralogy, heathcote, mineral collectors, selwynite, green rock, rock specimen -
The Beechworth Burke Museum
Geological specimen - Marble, Unknown
A granular metamorphic rock, marble is derived from limestone or dolomite and composed of calcite or dolomite interlocking grains. Heat and pressure from overlying sediments form it from limestone buried deep in Earth's crust. Graphite, pyrite, quartz, mica, and iron oxides can affect rock texture and colour. This specimen was found in Carrara, Italy. Carrara marble is the most common marble found in Italy, and it gets its name from the region where it is located. The marble was also called Luna marble and was used as a decorative element in buildings and sculptures. It has been quarried since Roman times in the Lunigiana, the northernmost tip of Tuscany, just outside the city of Carrara in the province of Massa and Carrara.Marble is one of the most popular and expensive rocks used in sculpture, architecture, interior decorations, statues, table tops, and novelties. It is available in various colors and textures depending on the chemical composition. The strength of the rock and its ability to hold finer details have made it a favorite among designers. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A solid hand sized Marble (metamorphic rock) predominantly white with specks light grey and ochre geological specimen, geology, geology collection, burke museum, beechworth, marble, carrara marble, italian marble, marble specimen, tuscany -
The Beechworth Burke Museum
Geological specimen - Bituminous Coal, Unknown
Bituminous coal is the most common type of coal, abundantly found in ancient coal deposits which can be dated back millions of years. Often referred to as soft or black coal, this specimen exhibits a high carbon content, ranging from 76-86%. It also holds a relatively high energy density (27 MJ/kg) meaning that it releases significant amounts of energy when burned. Bituminous coal is most commonly used for electricity generation, as well as in the production of steel. This particular piece of coal was collected as part of the Geological Survey of Victoria in the nineteenth century. It originates from Cape Paterson, a seaside village located in South Gippsland, Victoria (located on Bunurong Country). The discovery of bituminous coal in this locality was first made in 1826 by explorer William Hovell. More discoveries were gradually made over the following decades and in 1859 the Victorian Coal Company commenced the first active coal mining operations in the state by sinking a number of shafts and bores near the area of Cape Paterson. Evidence of this coal-focused past can be found today at the State Coal Mine Museum in the nearby town of Wonthaggi. This specimen is significant as it was collected from the locality of Cape Paterson in Victoria, an area that has since become historically instrumental in the mining of coal and other substances in the state of Victoria. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study. A solid hand-sized piece of bituminous coal with a shiny black-grey surface and jagged edges.Existing Label: BITUMINOUS COAL / Locality: Cape / Patterson, VIC. burke museum, beechworth, geological, geological specimen, state coal mine museum, wonthaggi coal mine, victorian coal company, bituminous coal, coal victoria, coal energy generation, william hovell, cape paterson, coal specimen -
The Beechworth Burke Museum
Geological specimen - Malachite, Unknown
Malachite is a copper carbonate hydroxide mineral. It has a chemical composition of Cu2(CO3)(OH)2. It often forms within limestone where a subsurface chemical environment favourable for the formation of carbonate minerals can occur. It is a substance that can be found in many different parts of the world including: Australia, USA, Russia and the Democratic Republic of Congo. Malachite has historically been used to produce copper, with mining of the mineral dating back over a period of four thousand years. Due to its beautiful green colourations, it is also commonly used for aesthetic purposes such as in the production of sculptures and jewellery. This particular specimen was collected from the town of Burra, South Australia as part of a geological survey undertaken during the nineteenth century. The locality (located on Ngadjuri Country) has a long history of mining, particularly in copper mining, as the area is rich in copper deposits. The first significant discovery of this was made in Burra (Burra Burra Mine) in 1845 and, at the time, the mine was the largest and richest of its kind in the world, producing nearly five percent of the total world copper output. This specimen is significant as it is considered to be a rare gemstone, as many of the original deposits for the stones are significantly depleted, leaving behind very few sources. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A solid palm-sized copper carbonate hydroxide mineral with patterns of green colourations Existing Label: MALACHITE / Locality: Burra / S. Aust. Other Label: Confirmed / as Malachite / C. Willman / 15/4/1 / + Bill Birch burke museum, beechworth, geological, geological specimen, malachite, gemstone, green gemstone, burra, burra burra mine, burra south australia, carbonate mineral, copper, copper mining, copper mining burra, carbonate hydroxide mineral, copper carbonate, malachite mining, malachite burra, monster mine -
The Beechworth Burke Museum
Geological specimen - Laterite
Laterite refers to both a rock and a soil type that is rich in clay, as well as Iron and Aluminium. It is created during a process that is called laterization, where high heat and seasonal heavy rainfall cause there to be wet and dry periods, which over time hardens the soil into rock. Because of this, most laterite is formed between tropics of Cancer and Capricorn. The iron oxide in laterite is what gives it it’s orange-red colouring. The largest religious complex in the world, Angkor Wat in Cambodia, is partially constructed of laterite, particularly its foundations, as laterite is porous and allows rainwater to drain. This specimen of laterite was collected from the Democratic Republic of Congo while it was colonised by Belgium in the 19th century. Laterite forms in many parts of the world, particularly between the tropics. It is used both for ore and as a building material, and comparing specimens from different parts of the world allows us to document the different compositions that this mineral can have when formed at different locations. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.a palm-sized solid iron-aluminium oxide mineral specimen in shades of brown, orange and greyburke museum, beechworth, geological, geological specimen, laterite, laterite specimen, geology -
The Beechworth Burke Museum
Geological specimen - Montmorillonite
Montmorillonite is a type of clay composed of aluminium silicate that forms very small particles that are not well-bonded to one another. This is why it is so soft. When in the presence of water, all types of clay swell. Montmorillonite swells even more than most types of clay, which is why it is often chosen over other types of clay in its practical uses. Montmorillonite has many different practical uses, including in the mining industry, as a soil additive, as a sealant, as a desiccant to draw water out of the air, to clean ponds, to make kitty litter and in cosmetics. Montmorillonite is a common mineral and, despite being named after Montmorillon, France, can be found all over the world, including many deposits in Australia. It is not known where this particular specimen originates from. Montmorillonite is an economically and socially significant material with a wide variety of uses. Having samples of common and important minerals allows collections, like the Burke Museum, to have a more complete view of the land on which they are located, and therefore a more complete view of heritage. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A solid tennis-ball sized chunk of aluminium silicate clay. It is primarily white, accented with orange and brown.burke museum, beechworth, geological, geological specimen, clay, montmorillonite -
The Beechworth Burke Museum
Geological specimen - Cassiterite
This specimen is Cassiterite in Quartz. Cassiterite is a tin oxide metal that forms in thin crystals which can have a beautiful lustre. Quartz is made of silicon dioxide, also known as silica, and is one of the most common minerals on earth. Cassiterite has been a fundamental source of tin ore for humans throughout history, including today. Tin is an important metal that has a wide variety of human uses in different areas, from dying fabric, to making mirrors, and their most well-known use ‘tin’ cans. Tin cans are primarily made of steel and are coated with tin in order to take advantage of tin’s property of being non-corroding. This is a massive step in the history of food preservation. Tinned food first reached Australia in 1815 with early settlers, and it began to be manufactured here in the 1840s. It was incredibly popular, and was a highly exported product, which would be a contributing factor to the ‘tin mining boom’ of the early 1880s. This specimen was collected at Jingellic, New South Wales, in about 1852. Although the Goldfields of the 1800s are much more well-known, tin mines existed alongside the gold mines which began in the mid 19th century and extended almost one hundred years, to the mid 20th century. Specimens like this would have been used as evidence to justify tin mining operations in the region as an investment. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study. The Geological Survey of Victoria was headed by British geologist, Alfred Richard Cecil Selwyn (1824-1902), who was responsible for issuing over 60 geological maps during his 17 years as director. These maps were all hand-drawn and coloured and became the benchmark for accuracy for geological mapping. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study. A fist-sized solid geological specimen made on one half of tin oxide, which is dark grey, and on the other side of silica, which is brown and cream.burke museum, beechworth, geological, geological specimen -
The Beechworth Burke Museum
Geological specimen - Opal Bearing Stone, Unknown
There are 17 opal fields in Australia. This opal bearing stone was found in Lightning Ridge, NSW over what is known as the Great Australian Basin. This basin was formed and covers an area of 1.7 million square kilometers in eastern Australia in the Cretaceous period. This basin used to contain an inland sea, which provided an environment where silcrete eventually formed when water levels changed. This eventually seeped into other structures, and eventually hardened and formed opal. Lightning Ridge has a population of around 2000 people, with about 80 000 visitors every year. It is a historic mining town, and is known for its deposits of a rare black opal. Mining started in the area in the late 1800s, early 1900s when the black opal was discovered. This opal-bearing stone is of social and historical significance. It is from Lightning Ridge, which is well-known for being a large producer of opal stones, most famously black opal. The history of the period dates back to 140 million years, with the discovery of black opal in the early 1900s causing interest in the area. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.***A palm-sized solid mineral specimen in shades of beige and light orange*** silica based? burke museum, beechworth, geological, geological specimen, opal, opal fields, australia, lightning ridge, new south wales, great australian basin, cretaceous, silcrete, black opal, mining -
The Beechworth Burke Museum
Geological specimen - Chiastolite
It is made up of andalusite. Andalusite is a rock-forming mineral, sometimes found in granite or schist. It is often used to make glass, ceramic products, chemicals, and heat-resistant bricks as it can withstand high temperatures without changing. The chiastolite contains particles of graphite, which arranges in geometric patterns. When crystal growth occurs in the rock, the granite particles concentrate at crystal interfaces and can result in cross shapes. These ‘cross stones’ have been valued and used for their spiritual or religious meaning and used as charms, gems, or amulets. Chiastolite was first discovered in 1754, seen in a description in a published book by a palaeontologist, Franciscan priest, and Spanish author, Jose Torrubia. Deposits have been found in Australia, France, the USA, Chile, Canada, Spain, Brazil, Sri Lanka, and Russia. Deposits have been found in Western Australia and South Australia. This particular specimen was found in Bimbowrie, South Australia. Other chiastolite specimens have been found in Bimbowrie, along with jasper, quartz, and aventurine in the form of rolled pebbles or schist. This chiastolite specimen is socially and historically significant. It is a very rare sort of andalusite mineral. It is from one of only two locations where it is regularly found in Australia. The carbon cross has made it an important religious symbol in the past. Its ability to withstand high temperatures has made it a common ingredient in heat-resistant bricks and ceramics today. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A metamorphic mineral consisting of andalusite, with a cross shaped graphite pattern in colours of grey, brown and yellowburke museum, beechworth, geological, geological specimen, andalusite, chiastolite, geometric, cross stone, spiritual, religious, australia, south australia, bimbowrie, quartz, jasper, aventurine, schist -
Port of Echuca
Black and white photograph
Macintosh's sawmill was on the banks of the Murray River in Echuca east where the Banyule State forest is now located. A tramway ran out to it from the main rail line near the iron bridge. Macintoshes Sawmill was one of the largest in the area. (Ref. Clare Jackson. )Macintoshes sawmill was set up by James Macintosh in 1868 in Echuca East. His sawmill prospered and in 1878 was "equal to five normal sawmills" (Ref; Coulson, Helen, "Echuca Moama On the Murray." P.158) He also owned 2 paddle steamers and 8 barges. The Macintosh Family contributed substantially to the development of Echuca East, but by 1901 the Family was in severe debt and were forced to sell the sawmill to the Nicholas Family.A black and white photograph of a large group of men outside a sawmill, reputed to be Macintoshes Sawmill in Echuca East.On the back of the photograph written in pencil are the words "Believed to be workmen at McIntosh's mill (Charlie Dowell says)macintosh's sawmill, sawmill industry, echuca east, banyule state forest, macintosh james, dowell, charlie, logging industry, jackson, clare -
Eltham District Historical Society Inc
Binder, Eltham District History, Eltham Road Board, 1856-1871; Research by Keith Chappel, 1971-1974
Eltham District History, Eltham Road Board, 1856-1871Two binders containing 486 A4 pages (photocopied) of mostly handwritten notes from research undertaken of Public Office Records of Victoria various holdings. Some photocopies from source reference books. Includes 20 page subject index (handwritten) at front and 5 pages of notes and sources at rear and a photocopy of short biography of Keith Chappel.a. foley, a. harkness, a. mackie, a. mcintyre, a. von ziegler, a.a. vivian, a.d. kinninmont, a.d. quadri, a.h. grimshaw, a.w. page, aboriginal reserve, aborigines, abraham quarman, abraham rooks, abraham taylor, adam goudie, aenaes harrison, agnes black, agnes charlton, agnes dalrymple, ah chong, ah cock, ah hein, ah lie, ah sing, albert lunson, albert ness, albert parker, albert ramseyor, alert hunt, alex cameron, alex eason, alex mcandrew, alexander crichton, alexander donaldson, alexander falconer, alexander innes, alexander james, alexander mcdonald, alexander miller, alexander thompson, alexander walker, alexander white, alfred armstrong, alfred burgess, alfred davey, alfred deschamp, alfred eddy, alfred hinley, alfred hooper, alfred hubbard, alfred lowman, alfred smith, alfred whelpton, alice power, allen heeps, allwood, amelia neuman, amos taylor, anderson, andersons creek, andrew brown, andrew byrne, andrew harkness, andrew herbert, andrew ross, andrew smith, angus mcdonald, ann emmott, ann mcphee, ann odea, ann plunkett, ann snell, ann tatty, annie ashmore, annie herbert, annie stuart, anthony beale, anthony currie, ants nest, archibald mcphee, arthur connor, arthur lyttle, arthur rooke, arthur young, arthurs creek, arthurs creek school, august ostling, b.o. wallis, barkers creek, barr, belton, benjamin bain, benjamin jenken, benjamin lawford, benjamin rice, benjamin shaw, benjamin smith, benjamin wallis, benjamin walton, berry, bismark hotel, black calf gully, black thursday, boomers gully, bridget bunker, bridget hailes, bridget kearse, bruno hirt, burns, bushranger, c. twiss, c.h. bade, caleb sherar, caledonia, caledonia diggings, campbell hunter, carl euman, caroline davey, catherine kennedy, cathren brock, cecilia farman, chamberlain, chapman, charles caldwell, charles campbell, charles dale, charles draper, charles fowler, charles green, charles hawkins, charles hempel, charles hirt, charles hirtson, charles jefer, charles jesse, charles kerchevell, charles lidgerwood, charles morris, charles peake, charles prince, charles rielly, charles roberts, charles rowand, charles simms, charles souter, charles swan, charles verso, charles wells, charles whelpton, charles williams, charles wingrove, charles woodley, charleys gully, charlotte beltison, charlotte goodwin, ching ah hock, christine brennan, christine mckenzie, christmas hills hotel, christmas hills school, christopher battaila, christopher twiss, chune grove, church of england, church of england school, clarissa milton, cleir hills, colin amos, constable quirke, constable talty, cornelius haley, cornelius stewart, cottles bridge, councillors hotel, cricket, cucksons brewery, d. nicholson, d.w. morrissey, dalry, daniel charleston, daniel harding, daniel jepps, daniel mccarthy, daniel mckenzie, daniel mcloughlin, daniel oloughlin, david boyd, david christian, david clark, david creighton, david rogers, david rolfe, david sharp, david shawcross, david smith, david stevenson, diamond accommodation store, diamond reef mine, dickson, dixon bertram, donald cameron, donald mcmillan, donaldson, dougald mcphee, dr barclay, dugald mcphee, dugald taylor, duncan fraser, duncan smith, dungey, e. hildebrand, e. stichlins, e.f. falkiner, e.j. hughes, e.m. garsed, e.w. morrissey, edith staff, edmund clarke, edmund cuckson, edmund hall, edmund picket, edward bage, edward beltison, edward bunker, edward ford, edward hindley, edward jackson, edward jones, edward kelly, edward qualtrough, edward staff, edward tresain, edward weller, edward whelpton, edward whilpson, edwin biley, edwin cartwright, edwin cohen, edwin deschamp, edwin mcleish, edwin rodda, edwin smith, effie rodda, eliza bellamy, eliza dawson, eliza howell, eliza nield, eliza smith, elizabeth cockshutt, elizabeth eiles, elizabeth fitch, elizabeth gillespie, elizabeth harris, elizabeth herbert, elizabeth hollow, elizabeth le juge, elizabeth plunkett, elizabeth whelpton, ellen hurst, ellen kearse, ellen quarman, ellen sweeney, ellen white, ellis, eltham cemetery, eltham hotel, eltham lower park, eltham market, eltham police station, eltham pound, eltham quarry, eltham racecourse, eltham roads board, eltham school, emile hude, emily anderson, emily blamire, emily coutie, emma smith, emma taylor, ephraim wyett, ernest baillie, ernest henrick, ernest steer, esther porter, ethel baillie, evan jones, evelyn hotel, evelyn observer, ewen cameron, ewen jones, f. chrimes, f. grundel, f.e. falkiner, f.r. howard, fanny benson, fanny white, felix hude, felix noisette, ferdinand ramseyer, flora vale, florence hurst, fogarty, forbes mackenzie, fords creek, frances kearse, francis baker, francis hales, francis raselli, francis steer, frank eiles, frank rogerson, frank tanner, fraser, fred hurst, frederick falkiner, frederick hurst, frederick muller, frederick nink, frederick walker, frederick wharington, friedrich muller, fryers gully, furphy, g. donaldson, g. houghton, g. turnbull, geanetta hude, george assender, george bear, george beare, george benson, george bird, george boston, george brain, george brandt, george burley, george buswell, george coutie, george eiles, george ewings, george ford, george godber, george goodman, george gray, george griffiths, george hall, george herbert, george horn, george kirk, george langhorne, george mann, george mclelland, george mosely, george neumayer, george orchard, george parish, george porter, george purcell, george ralph, george reid, george rocke, george rogers, george rolfe, george stebbing, george stebbings, george stebbins, george switzer, george symons, george thompson, georgina hilton, glenda moriss, glengloy, gold, goulstone, greensborough police station, gulf station, h. jennings, h. mann, h.h. farquason, hannah sunderland, happy valley, harkness, harold scarce, harriet hunt, harriet smith, harry hollow, hazel glen, healesville, heinrich hirt, helena peters, henrietta hill, henry arthur, henry ashmore, henry austin, henry brown, henry dendy, henry dineen, henry fowler, henry gardner, henry green, henry griffin, henry hart, henry hirst, henry hirt, henry hopkinson, henry hude, henry hurst, henry inch, henry jones, henry mills, henry scarce, henry st paul, henry stevens, henry stooke, henry thomson, henry vogt, henry wallace, henry wilson, herbert rodda, herman henrick, hermann lampe, hermann steinmann, hester staff, hitchill, holbert, honoree hude, hotel de france, hugh mccann, humphrey peers, humphrey spicer, hurstbridge, hurstbridge general store, i.h. clarke, ida adelskold, ignatz kinzel, ira pimm, irene donaldson, isaac briggs, isaac hickson, isaac hill, isaac kerr, isaac varby, isaac williams, isabella donaldson, isabelle herbert, j. dungate, j. eccleston, j. harkness, j. hartley, j. hude, j. irvine, j. jones, j. manduell, j. mason, j. mcdonald, j. mcnamara, j. nichenson, j. renahen, j. scott, j. seymour, j.a. goold, j.a. panton, j.c. hughes, j.d. thompson, j.f. hughes, j.f. johnstone, j.g. walter, j.h. taylor, j.p. morris, jack ewart, jacob belsham, jacob goldstein, jacob morast, jam loon, james alexander, james anderson, james andrew, james andrews, james baines, james batchelor, james bond, james bradford, james brennan, james brock, james brown, james brunning, james buchanan, james cockburn, james cowan, james dalrymple, james donaldson, james duckworth, james goodwin, james harding, james harrison, james hartley, james hawkins, james hewish, james holinger, james hughes, james inglis, james jamieson, james johnson, james johnston, james kaye, james kew, james lindsay, james lindsey, james lynan, james macpherson, james mann, james martley, james mayger, james mccutcheon, james mcmahon, james mcpherson, james mess, james miller, james mitton, james morton, james murdoch, james murdock, james nickinson, james orford, james purcell, james 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Mission to Seafarers Victoria
Article, Argus newspaper, The propose Seaman's Hospital at Williamstown, 9 June 1852
"A meeting for the purpose of considering the best means of estabishing an Institution of this kind, at the above place was held at the Ship Inn on Monday evening. Charles Ferguson, Esq, being voted to the Chair, briefly stated the intention of the present meeting, and that all must concur as to the necessity of founding same Institution for the relief of the numerous cases daily occuring in this port, amongst so great a number of ships, large at present but small in comparison to what may be expected in a short time. For the last five months ending May 31st, five hundred and eleven vessels en-tered Hobson's Bay, amounting to a tonnage of ninety-five thousand three hundred and seventy-two tons, which, in tho same proportion for twelve months, would give two hundred thousand tons annually and, calculating four men for each one hundred tons, shows that eight thou-sand sailors arrive at this port in the space of a year, for whom, at present, there is no provision made for either sickness or accidents. A lengthened conversation ensued, in th» course of which several instances were pointed out of he great benefit conferred upon the ship ping interest, by the establishment of an hospital at various ports named, and all agreed that such would be a great boon here. After some further discussion as to the wording of the re solution, the following was proposed by Captain Beaseley, and seconded by Captain Goss, «That this meeting is convinced of the necessity exist ing for a Seaman's Hospital, at Williams Town; and that a committee be appointed to draw up a menorial to His Excellency the Lieutenant Governor, respectfully praying, that a sum of money be placed on the Estimate for the en suing year, fur this purposoe ; and that the memorial be given to William Westgarth, Esq. M.L.C. in order to its presentation, -and that the committee accompany Mr Westgarth at the presenting of the said memorial. This proposi tion was carried unanimously, and the following gentlemen were appointed a committee to draw up the memorial: Captain Berzeley (Clifton), Captain Ross (Kashemy), Captain Baker (City of Manchester), Captain Goss (Candahar), Capt Luke (Diana), Captain Nicholson (Calphurnia), Captain Hammach (Cambodia); and for carrying out the above, a meeting is appointed to take place on board the Clifton, this day, at four p.m. A vote of thanks to the Chairman being proposed by Thomas Hunt, Esq, and seconded by A. A. Broadfoot, Esq. the meeting adjourned."With the increase of commercial and migrant shipping, it was made obvious that seamen needed specific attention. The hospital in Williamstown was the first attempt to provide such service.argus, seaman's hospital, williamstown, the ship inn, welfare, captain charles ferguson (1813-1868) -
Mission to Seafarers Victoria
Booklet - Manual, Sailing directions for Port Phillip, in the colony of Victoria including the ports of Melbourne and Geelong, 1854
Captain Charles Ferguson was born in Scotland in 1813. He was the Master of the "Rajah" from 1838 to 1850 on voyages from England to Australia and vice versa. He became the First Chief Harbour Master for the port of Melbourne in 1852 after being the first Harbour Master and Water Police Officer in Geelong for 12 months. On the 5th of April 1841, the Rajah sailed with James Donovan M.D. as Surgeon Superintendent, and the Rajah sailed from Woolwich with 180 female convicts. The Rajah arrived on the 19th of July in Hobart, with 179 females (one died during the voyage) and 10 children. Miss Kezia Elizabeth Hayter was the matron on board. On page 28 of the "Sailing directions for Port Phillip, in the colony of Victoria including the ports of Melbourne and Geelong", a mention is made of the Mariner's Hospital and Floating Church soon to be established. There were discussions to built the hospital in Williamstown but instead the Government decided to build it in Melbourne. The Harbour Master and a commiittee decided to use the water police hulk, Emily, left unsold in 1856, to create a floating church: the Bethel was open in July 1857 with Reverend Kerr Johnston as Chaplain. Latrobe wrote a letter to Captain Cole in 1869, a few months after learning his death : "To Captain George Ward Cole † [from a draft in another’s hand] Clapham House, Lewes, Sussex, January 28th, 1869. My dear Captain Cole, Last mail will have taken out the sad intelligence of the death of our excellent old friend, Captain Ferguson. This will have been a terrible blow to his children and to his friends in the colony, who may have held reason to expect his early return to his home, with a not unreasonable prospect of ultimate restoration to health and activity. In the course of last October I went up to town with one of my children, mainly with the purpose of finding my way to Pinner, where he and Mrs. Ferguson were staying with an intimate friend. I found him in excellent health and spirits, and enjoying the prospect of a speeding resumption of the service to which he had devoted his best days, and upon the furtherance of which his entire energy was still directed. A week or two later Captain and Mrs. Ferguson went to Dover for change of air, and being still under the impression received from the advisers by whom they had been guided during their residence at a hydropathic establishment at Matlock, felt encouraged to plan almost immediate return to the colony by the Jerusalem early in December. However, certain misgivings in the mind of a medical gentleman, then in England, under whose care Captain Ferguson had at one time placed himself in Williamtown, led them to consider it judicious before departure to take the advice of some surgeon of eminence in London. Accordingly they came up to town at the close of November. The first London practitioners they consulted shook their heads, and advised consultation with Sir Wm. Ferguson. The result was that amputation, without loss of time, was pronounced necessary. The rest is soon told. He received the painful intelligence with calmness and full resignation to God's will, and underwent the operation at King's College Hospital with exemplary firmness and Courage on the 28th of November. Perfect success seemingly attended it, and there seemed, humanly speaking, to be every prospect of a prompt cure and early convalescence; everything seemed in his favour. A few days later, however, all was clouded by symptoms of hospital fever (pyoe æm ia). This resisted all control, and finally carried him off on the 27th of December, just one month after the operation. He had lived a Christian life, and his death was the peaceful and resigned death of a Christian. It was a melancholy satisfaction to me to be able to join a few friends in following his remains to their resting place in one of the outlying London cemeteries on the last day of the year. You know Mrs Ferguson well, and will be prepared to hear me say that her whole conduct and demeanour throughout this period of suspense and bitter trial has been worthy of her high character and steadfast principle. Come what will, and happen what may, I have the fullest conviction that neither the widow nor the children will be forsaken, however doubtful and clouded the future may appear, in consequence of the irreparable loss which, they have sustained. And now, dear Captain Cole, it is possible that you may already have heard all this from other sources, but I have dictated it to you under strong impulse, for I feel assured that there is no member of the community in which you live who will more sincerely deplore the loss of Captain Ferguson on private grounds; at the same time that there is no one who, from long acquaintance with his official character and services, will be in a better position to estimate their real value or the loss which the colony has sustained. The circumstances in which Captain Ferguson's family are left not only demands the utmost display of sympathy and interest on the part of friends, but may call for decided and prompt action; therefore I cannot rest satisfied without discharging what I consider my duty, and seeking to strengthen your hands as far as I may in bringing the character of his long services before the existing colonial authorities. Of his private career previous to his entering the service of the Colonial Government in 1851 nothing need be said. Captain Ferguson was appointed as the Harbour Master at Geelong in April, 1851 – a few months before the separation of the colony from New South Wales. He there did excellent service in a variety of ways calculated to advance the interests of the port, and to introduce www.latrobesociety.org.au 27 order, where, from circumstances, but little order had hitherto prevailed. His was the first appointment of this class in that locality. The separation of the colony from New South Wales took place in the month of July following. Shortly after, the late Captain Bunbury resigned the Harbour Mastership of Port Phillip. Captain Ferguson was at once (February, 1852) appointed to succeed him, and from that time performed all duties of Chief Harbour Master of the colony. The previous year (May 1851) the first gold discoveries in New South Wales had taken place, and in the month of August those of our colony followed. At the time of Captain Ferguson’s taking charge of the Port of Melbourne their influence had begun to be fully felt, and in no department more seriously than in that of the Harbour Master. This is no place for statistical details, but they must bear me out in reminding you of a few facts connected with our late friend’s career. At the time of separation that department comprised only 30 individuals of all ranks, and when he took charge the number was much reduced. There were at that time, according to the returns, no fewer than 54 vessels, registering 26,785 tons, in Hobson’s Bay alone. The crews on arrival numbered 1,235 men. Of this number only 463 remained on board, 500 having deserted, and the rest having been discharged by arrangement or pure necessity. For the first six months after Captain Ferguson’s assumption of office as Harbour Master the duties of Police Magistrate and Chief of the Water Police were superadded, and how much labour they involved may be surmised from the fact that from 1st of April to the 31st July, 1852, four months only, no less than 236 marine cases were brought before the bench at Williamstown - sometimes as many as 30 in a day. A year later (March 1853) the returns show that the number of vessels in the harbour in Hobson’s Bay alone were 91, tonnage 43,754; and passing on to the still later returns of May, 1853, two years after Captain Ferguson’s assumption of office, we find from the records that the number of ships in port had increased to 129; tonnage, 63,292; crew on board on arrival, 2872, and at the date of report, 1628; the amount of desertions at that time having, however, proportionally diminished, in consequence of the abatement of the gold fever, caused by the non-success attendant upon the labours of thousands at the goldfields. The above numbers take no account of the large number of vessels and amount of tonnage lying at the wharves at Melbourne or elsewhere. From these figures alone it may be judged what must have been a struggle in which the Chief Harbour Master was engaged from the very outset to secure order, and answer the innumerable calls on every branch of his department, at the same time that there was for many months an almost complete impossibility of securing subordinate agency, such as boatmen, pilots, and police, at any price. But I may bear witness to the untiring diligence, energy, and self-devotion with which Captain Ferguson grappled with the difficulties of his position, and the seemingly insurmountable obstacles which stood in his way. Ashore and afloat he was always ready, showing the same directness of purpose, intelligence, and forgetfulness of self. He shunned no responsibility, and turned his hand from no work, whether within or beyond the ordinary scope of his duty, which the hard necessity of the times forced the Government to bring under his notice. Already in 1852, when the overflowing of our gaol and stockade rendered the adoption of other methods of restraint absolutely necessary, and addition to the existing buildings could not be thought of, it was Captain Ferguson who first suggested the employment of hulks; and it was with his personal assistance and supervision, and under his unflagging energy, that the three first of these – the Success, the President, and the Sacramento – were purchased, fitted up, and made available for the purpose in view, and the rules and regulations for the employment and safety of the men afloat and ashore prescribed and carried out. He carried the same energy into every branch of his department, and his influence was soon apparent. His subordinates of every class became actuated by his spirit. As time moved on, the range of his duties, both ordinary and extraordinary, increased. In the formation of the quarantine station at the heads, in the management if not the erection of lighthouses, sailing directions, port and wharf regulations, buoys, signal stations, www.latrobesociety.org.au 28 steam dredging &c., he was the main and most active agent. The whole pilot establishment and regulations, men, and vessels, were under his charge; and when I left the colony in May, 1854, the entire range of ports outside Port Phillip Heads from Point Lonsdale to Portland, as well as that of Geelong had felt the influence of his intelligent supervision and care. The entire department of Chief Harbour Master, which I have numbered at the period of separation about thirty individuals, then numbered 230. The character of Captain Ferguson’s unbroken service during the fourteen years which have elapsed since I left the colony must be well known to the Government and the people he has served so long and so faithfully. I confine myself to recalling to mind those earlier, and what must have been the hardest and most difficult, period – none can know how difficult but those who were in that fierce struggle for the maintenance of order under so many disadvantages; and on this subject I have spoken advisedly and with reason, for I may truly say he worked under my own eye. I had sincere regard for the man, and just pride in the qualities of his heart, head, and hand. Whatever mistakes may have been made by the Government of the colony in those hard and difficult times (and I am quite ready to admit that there were many, especially if the past is to be judged by the light of the present), I never have hesitated in believing that, in appointing Captain Ferguson to the office he has so long filled, it was the right man in the right place. I shall be heartily rejoiced to find that the Government and inhabitants of the colony admit that this has been the case, and to learn that they have not forgotten the strong claims of one who has served them so long and so faithfully, and who, removed by God’s providence, so to say, in the maturity of his powers, has left a widow and young family behind him. I have done, I leave you to make use of this communication, or any portion of it, which you may think judicious and called for. There may be among Ferguson’s friends those who may not be sorry to be reminded of facts. By-the-bye, I may mention as a proof how completely Captain Ferguson’s mind was engrossed by devotion to his public duty, that while in Dover, only ten days before the operation, he took an opportunity to drag himself up into the lantern of the S. Foreland Lighthouse, and made a most careful scrutiny of the whole apparatus and arrangement, with a view of the adoption of any hint for the perfection of those under his charge in the colony. And now, goodbye. I trust this will find you in good health, and in comparative vigour. Believe me ever, dear Captain Cole, Yours very truly, C. J. La Trobe"The attempt for a floating church was made as early as 1853 following similar examples in London like the Seamen's Hospital. Captain Ferguson was instrumental in the foundation of the Bethel Church.Digital copies of the 37 pages ; 22 cm.1854, hobsons bay, geelong, melbourne, williamstown, sandridge, mariner's hospital, floating church, seamen's hospital, captain charles ferguson (1813-1868), kezia elizabeth hayter (1818-1885), rajah quilt, prison hulks, water police, harbour master, harbor master, gaols -
Glenelg Shire Council Cultural Collection
Book - Book - Victorian Government Gazette 2, 1868. 1 July - 31 December, 1869
Used by Local Council.Dark blue marbled cloth covered over hard cardboard. Red leather spine and corners. Gold lettering on black band on spine. Gold crown and lettering on spine.Front: Presented to the Committee of the Portland Free Library by the Hon. George Turner, Commissioner of Customs, 6 June 1892. -
City of Moorabbin Historical Society (Operating the Box Cottage Museum)
Furnishings, 'Colonial' metal name plate c1917, c1917
c1917 it became fashionable to give residences a 'name' . Mr August Reitman attached this metal nameplate to the Cottage.when he began leasing the property. The Reitman family purchased the property in 1935 and resided there until 1953 . The property was sold to Lewis Timber Co . c1970. William Reitman, the son of August, donated the sign to the CMHS c1984 during the reconstruction of the pioneer cottage in Joyce Park ,Ormond.An unknown pioneer built the Cottage c1840 then William Box purchased it 1868 and his family resided there until it was leased to August Reitman in 1917. August placed this nameplate on the Cottage c1917. William Reitman, the son of August donated the sign to CMHS in 1984 when the Cottage was reconstructed in Joyce Park Jasper Road OrmondThe original metal name plate attached to Box Cottage c1917 by August Reitman when he and his wife began renting the property. 'COLONIALbox william, box elizabeth, reitman august, moorabbin, bentleigh, brighton, ormond, dendy's special survey 1841, market gardeners, sculptors, reitman william, lewis timber co ltd, box cottage museum -
Learmonth and District Historical Society Inc.
Photo-Nicholson, Unknown, Alexander Nicholson,President 1864-65 (part),1865-66, "Circa 1866"
Councilor Alexander Nicholson was elected to council in1863 serving until1868. He was appointed President in1864-65 of which he only served part,(Conucilor J.Laidlaw serving the remainder) and 1865-66.Original Historic Photo.Photo of Alexander Nicholson is sepia in colour and is in a dark brown moulded frame, inner edge is a lighter brown and mount is dark brown with lightefr brown surounding the oval photo.Councilor Alexander Nicholson,Shire President, Shire of Ballarat.1864-65 (part),1865-66.ballarat shire council, nicholson alexander 1863 1868