Councilor A.D.Moverley was elected to Council in 1958 serving till1961.Original Historic photo of all Councilors for the year 1959.Taken to commemorate opening of Wendouree Municiple Centre 20th November 1959.Councilor A.D. Moverley, sepia photo (rectangular),on white mount,situated second from right of middle row of composite photo of all councilors,taken to commemorate the opening of the Wendouree Municiple Centre 20th November 1959.Presented by Councilor Charles Edward "Ted" Brown,Shire President, to Commemorate the opening of the Wendouree Municiple Centre 20th November 1959.wendouree municiple centre opening 20th november 1959, ballarat shire council, moverley a d councilor 1958 61

Letter mounted into plaque. dated Sept 2005 from the Minister for Planning. The letter is addressed to the mayor and Councillors of South Gippsland Shire Council. Brown polished wood plaque. Clear perspex sheet over letter affixed four brass screws with knobs.

Kraft-Walker Cheese Company commenced in Allansford in 1935 leasing the factory premises from Warrnambool Cheese and Butter Factory Company. Dairy companies entered competitions organised by the Dairy Industry Association and associated organisations and local agricultural societies to encourage improvement in products. Some of these awards are considered prestigious and highly regarded within the industry. The certificates were passed to Cheese World Museum by the factory management.A blue background full colour certificate and a cream cartouche with a darker banner across it and the insignia of the Royal Agricultural Society of Victoria; in the lower right hand corner of this section is the Australian coat of arms; around this are grasses, grapes and wheat. On the left hand side and across the bottom are images in various shapes. The circular image on the top shows a Royal coat of arms; below are two gold medals featuring a female and a laurel wreath; underneath is an image of two black sheep and a blue ringed circle has two sheep with blue ribbons around their necks standing in front of a wooden fence. Along the bottom are three images -first a black riding horse together with a brown shire horse in harness; second a horse drawn harvester; third a brown prize bull.THE ROYAL/AGRICULTURAL/SOCIETY/ OF VICTORIA Gold Medal/Royal Melbourne Dairy Show/1997/WARRNAMBOOL MILK PRODUCTS P/L/Class 127/Exhibit 165/EXCELLENCE IN AGRICULTURE allansford, dairy awards, product awards, warrnambool milk products, warrnambool cheese and butter factory company, royal melbourne dairy show, agricultural shows

White covered book with multiple images.ballarat shire, shire of ballarat, c.e. brown, learmonth sire hall, gold memorial, miners rest reticulated water, australian timken, ballarat airport, joe white maltings, franklin caravans, kirk's reservoir, white swan reservoir, electricity, lucas, unilever australia, ballarat gas company, coronet caravans, lindsay gunn, martin stoneware, w. r. walton, m.b. john, ballarat agricultural and pastoral society, planning scheme, webcona estate, brown's heavy haulage, ballarat mental hospital, alfredton pre-school centre, wendouree recreaton reserve, wendouree pre-school, wendouree youth club, corporation saleyards, arch of victory, lake burrumbeet, perry park, ballarat high school, wendouree west state school, ewing house, ballarat grammar school, ballarat teachers' college, learmonth presbyterian church, st mathew's wendouree, st mary's redemptorist monastery, norm doodt, pre-mixed concrete, wendouree bowls club, ballarat shire councillors, rex hollioake, david baird, thomas ford, william troup, wilfred hirst, charles brown, charles giot, william walton, david powell, john pemberton, hugh patterson, alexander mcdonald, edward edwards, james mitchell

Pink covered book showing the Council Offices of the Shire of Ballaratballarat, shire of ballarat, ballarat shire council, brown, george powell, learmonth shire hall, cobb & co, learmonth, ballarat townscape, australian timken, wendouree west housing estate, wendouree west, ballarat airport, joe white maltings, alfredton, a.v. wehl industries, begonia house, walton, valenite-modco, sec substation, ballarat agricultural and pastoral society, gong gong, wendouree sewerage teatment works, alfredton recreation and sports centre, wendouree west library, wendouree recreation reserve, wendouree youth club, norton villiers, planning scheme, lucas textiles, immunizaton, kelaston, linda brown pre-school, wendouree pre-school, parklands clinic, alfredton infant welfare centre, darriwell park, vitclay pipes, t.m. burke estate, webbcona estate, franklin caravans, lake burrumbeet, forrest street primary school, ballarat high school, wendouree west state school, coronet industries, wendouree primary school, learmonth presbyterian church, st matthew's wendouree, st mary's redemptorist fathers monastery, robert ritchie, robert ritchie foodstores, stan farquhar, berklee products, ballarat golf course, s. j. weir, dowling forest racecourse, norm doodt, hines plaster, ballarat aerial view, victorian inland meat authority, s.k. mcivor, j. & g. dart, wendouree west aerial view, egg and egg pulp marketing board, councillors, kinnersly, giot, powell, sansom, cornell, edmonston, crick, ford, mitchell, cobb & co, j. g. dart, rex hollioake, mcdonald, baird, cobb & co, j. & g. dart

The 1930 Back to Bacchus Marsh celebrations were held on 23 to 28 October 1930. The committee were Cr L.M. Gugdale (president), A.W. Bond (General secretary), W. Grant Morton, J.G. Wells, Dr E. McDonald, Charles Dickie, G.H. Anderson, F.M. Crisp, W.R. Vigor. Bacchus Marsh State School No. 28 was established in 1851 as a National School in a rented building on the right-hand side of Bacchus Marsh-Melbourne Road, just beyond Woolpack Inn. Several willow trees mark the site. H.G. Ball was the first Head Teacher of the school, and the enrolmen towas 34. In 1854 Governor Charles Hotham visited the school. In 1855 two new schools, East and West, were recommended. School No. 28 closed in 1862 and the sitre was sold. The present school site was purchased in 1865 for 67 pounds. The cost of the building was 782 pounds. (Visions and Realisations, Vol 3., 1973) A clock purchased by public subscription was placed in the front of the building to the memory of scholars who served during World War One. (Back to Bacchus Marsh, 1930)Brown covered book of 44 pages. Contents include Bacchus Marsh and its soldiers, Red Cross, Lerderderg Gorge, Werribee Gorge, Lerderderg Park, Coimadai, Darely Firebrick Co., Myrniong, Underbank, Balliang, Rowsley, Parwan, schoosl, churches, Shire Council, Federal Milk Pty Ltd, Bacchus Marsh Milk, Old Maddingley Bridge Images include: * Bacchus Marsh looking east, 1930 * Bacchus Marsh Looking West, 1872 * Bacchus Marsh Looking West, 1930 * Aerial View of Bacchus Marsh Township looking east * Aerial View of Bacchus Marsh Township looking south * Bacchus Marsh Agricultural Society & Pastoral Society, 1893 (named), * Original Bacchus Marsh State School No 28 * Holy Trinity Bacchus Marsh * Bacchus Marsh Baptist Church * St Bernard's Catholic Church * Bacchus Marsh Methodist Church * St Andrew's Presbyterian Church Bacchus Marsh * View of Maddingley Park, showing Original Courthouse, 1890 * Werribee Gorge * Underbank Stud Farm * Ballarat State School Number 28. Signed 'C. Hodgson'bacchus marsh, maddingley, maddingley park, underbank, lerderderg park, coimadai, darely firebrick co., myrniong, balliang, rowsley, parwan, schoosl, churches, shire council, federal milk pty ltd, bacchus marsh milk, old maddingley bridge, police, police paddock, maddingley gates, crisp, mccormack, cain, harkness, howe, bence, mcdonald, mcfarlane, cosgrave, flagg, burnip, scott, lodge, cameron, vallance, bacchus marsh state school, bacchus marsh state school no 28., geology, r.w. thompson, lederderg gorge, weribee gorge, comadai, darley firebrick company

Bacchus Marsh celebrated 100 years of white settlement in 1936. The centenary celebrations committee comprised of L.M. Dugdale (President), A.W. Bond (Hon. Secretary), Charles Dickie, W. Grant Morton, W.R. Vigor, C.J. McFarlane, G.H. Anderson, T.J. Shea, F.C. McC Crisp, Dr E. McDonald, Robert Elliott (treasurer), R.H. Lambert (Decorations manager)Brown covered book of 28 pages. The book includes an historical essay, official centenary programme, Electric Light Plant, Patriotic Bacchus Marsh, milk industry, Pioneer Women's Memorial Avenue, Bacchus Marsh Gas Works . The book includes numerous advertisement, some illustrated. Images include: * Bacchus Marsh Flats from Anthony's Cutting; * Manor house; * Scene in Maddingley Park * Werribee Valley; * Werribee Gorge * Maddingley Park lake; * ANA Hall and Post Office * Shire Hall and Soldiers' Memorial Hall, * State School No 28 * At Werribee Gorge ** The Gas Supply Co, Bacchus Marsh * Bacchus Marsh Shire Council, 1935-6 (named) Images depicted in the book were supplied by H.J.M. Vallancebacchus marsh, merrimu guest house, anthony's cutting, captain bacchus, manor house, maddingley, maddingley park, werribee gorge, bacchus marsh shire, bacchus marsh shire council

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 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

Agate occurs when amygdales (gas pockets) form in the upper levels of basaltic lava flows. If these pockets or bubbles are iniltrated by water bearing silica in solution, the fluid dries and hardens in layers, forming round or egg shaped nodules or geodes within the rocky matrix. Agate is formed of a silica mineral chalcedony similar to quartz. Although relatively common and semi-precious, agate has been prized since at least 1450 BC - an intricately carved agate seal was found in the 2015 excavation of a grave belonging to a Mycenaeum priest or warrior near Pylos in Greece. Agate is also used in jewellery and other decorative or ritual purposes due to its often striking appearance. These specimens originated in North Queensland, which contains noted agate-fossicking regions such as in the area surrounding Forsayth. They were collected in approximately 1852 as an adjunct to the Geological Survey of Victoria. It was donated to the Museum in 1868. Victoria and other regions of Australia were surveyed for sites of potential mineral wealth throughout the 19th Century. The identification of sites containing valuable commodities such as gold, iron ore and gemstones in a locality had the potential to shape the development and history of communities and industries in the area. The discovery of gold in Victoria, for instance, had a significant influence on the development of the area now known as 'the goldfields', including Beechworth; the city of Melbourne and Victoria as a whole. The specimens are significant as examples of surveying activity undertaken to assess and direct the development of the mineral resource industries in Victoria and Australia, as well as the movement to expand human knowledge of earth sciences such as mineralogy and geology in the nineteenth century. Two solid egg-sized pieces of peach/orange toned agate (a common semi-precious chalcedony, similar to quartz) with a striped pattern, embedded in a light and dark brown matrix. geological specimen, geology, geology collection, burke museum, beechworth, agate, north queensland agate, 1852 geological survey of victoria, l. hufer - donor, mineralogy, agate specimen, indigo shire

Sphalerite or sphaelerite is named from the Greek word for 'treacherous' or 'deceiver' as specimens can vary widely in appearance, making them hard to visually identify. It is a zinc sulfide with the chemical composition (Zn,Fe)S, the most important ore of zinc. Specimens of sphalerite can contain iron as a substitute for up to 25% of the usual zinc present, as well as trace elements of gallium, cadmium, geranium and indium. Small amounts of arsenic and manganese may also be detected. Sphalerite is found in igneous, sedimentary and metamorphic rocks. It forms when carbonate rock encounters acidic, zinc-bearing fluid. It often forms in veins or in fissures of the existing rock, with colours and crystal shapes dependent on the composition of the the combining elements. It forms isometric crystal shapes including cubes, tetrahedrons, octahedrons, dodecahedrons. This specimen was collected in approximately 1852, in Broken Hill, NSW, as an adjunct to the Geological Survey of Victoria. It was donated to the Museum in 1868. Victoria and other regions of Australia were surveyed for sites of potential mineral wealth throughout the 19th Century. The identification of sites containing valuable commodities such as gold, iron ore and gemstones in a locality had the potential to shape the development and history of communities and industries in the area. The discovery of gold in Victoria, for instance, had a significant influence on the development of the area now known as 'the goldfields', including Beechworth; the city of Melbourne and Victoria as a whole.The specimen is significant as an examples of surveying activity undertaken to assess and direct the development of the mineral resource industries in Victoria and Australia, as well as the movement to expand human knowledge of earth sciences such as mineralogy and geology in the nineteenth century.A pipe-shaped specimen of sulfide-mineral zinc ore displaying patches of black, brown, beige and gold colouring. The main item has associated broken pieces. geological specimen, geology, geology collection, burke museum, beechworth, mineralogy, indigo shire, geological survey, sphalerite, sphaelerite, zinc ore, broken hill, nsw, victoria, galena, fluorite, chalcopyrite, lead, cadmium, gallium, germanium, indium, iron

Quartz is one of the most common minerals in the world. It is formed by a 3d structure of silicon and oxygen. While it is a simple mineral, it can come in a variety of shapes and colours. When quartz is pure it is colourless, transparent and can appear glass-like. Better known and more rare variations of quartz include amethyst and smoky quartz. This specimen is a vein of quartz in Breccia Conglomerate. Breccia is coarse-grained clastic rock which is made up of broken rock fragments and held together by mineral cement. The locality of this specimen is unknown. While quartz is a very common mineral and does not have rarity, it is an important material in industrial settings. One of it's physical and chemical properties is that it is piezoelectric, which means it can be used to generate an electric charge. This has made it useful in the manufacturing of timekeeping devices. This specimen was donated to the Burke Museum between 1868-1880 among a larger collection of geological specimens. It was collected as part of the Geological Survey of Victoria which begun in 1852 as a response to the Gold Rush. Collections were distributed to organisations across Australia to encourage the further study of the scientific makeup of the Earth. A solid egg-shaped rock with a mineral vein forming a ring around the rock in shades of brown and beige.burke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, 1852 geological survey of victoria, mineralogy, quartz, breccia, breccia conglomerate, conglomerate

Tourmaline is a group of minerals belonging to the complex borosilicate mineral class. These minerals are known for their striking and varied colours, making them prized gemstones. Tourmaline crystals can come in various shades, including pink, green, blue, brown, black, and colourless. They are often transparent or translucent. Tourmaline's chemical composition is complex, but it typically includes elements such as aluminium, iron, magnesium, sodium, lithium, and potassium. The specific arrangement of these elements in the crystal lattice gives rise to the different colours and properties of tourmaline specimens. Tourmaline specimens from Beechworth, Victoria, Australia, are a notable part of the region's mineral heritage. These tourmalines are of interest to mineral collectors and enthusiasts. While the tourmaline found in Beechworth is not as well-known as some other tourmaline varieties, it has unique characteristics and a historical context associated with the gold mining areas in Beechworth.The significance of tourmaline in Beechworth, Victoria, Australia, lies in its unique geological and historical context, contributing to both scientific and cultural aspects. The tourmaline mined in Beechworth is a rare and unique variety of tourmaline that is primarily found in the historic gold mining areas surrounding Beechworth. Its occurrence is closely linked to the geological processes that shaped the region during the Gold Rush era. The discovery of tourmaline in Beechworth adds to the rich mineral heritage of the area, which was historically known for gold mining. The specimens serve as a tangible connection to the region's mining history and contribute to preserving its geological legacy. The presence of tourmaline in Beechworth showcases the mineralogical diversity of the area. Tourmaline is known for its wide range of colours and unique properties, making it a valuable subject of study for mineralogists and geologists. Tourmaline specimens from Beechworth have educational significance, providing opportunities for research and study. They offer insights into the geological processes and mineral formation in the region, contributing to a better understanding of Earth's geological history.A hand-sized solid mineral specimen in shades of brown, green, light grey and dark greyTOURMALINE (schorl) / (Silicate of boron and aluminum) burke museum, beechworth, indigo shire, geological, geological specimen, mineralogy, tourmaline

This specimen is a native copper specimen that is metallic. Copper is typically found in the earth's crust and is often found alongside other metals such as gold, zinc, lead and silver which all belong to the same group which is the Copper/Gold group. Copper is most commonly formed from large masses of molten lava rock which has solidified in the earth's crust and over time though different sizes and speeds of crystal growth has turned into large amounts of copper, stored in porphyry copper deposits. Copper has a distinctive colour, yet can sometime appear blue and greenish which is often caused by oxidisation or a mixture of copper and other metals. This specific specimen was recovered from Moonta, South Australia. The Moonta Mining Company was established in 1861, after a Shepard in the area noticed traces of copper. This lead to a rush in the copper mining industry which was relatively young in Australia at the time, making Moonta Mining Company one of the richest in Australia. By the 1860's, South Australia had been nicknamed the "Copper Kingdom" due to its vast amount of Large copper mines and resources. As of 2016, Australia was the second largest producer of Copper internationally, following behind Chile in first place. This copper specimen is significant historically and scientifically as it is such an important metal commonly used throughout the world in various ways. Copper is an invaluable recourse used in daily life, used in most electrical appliances as it is a great conductor of heat and electricity, as well as being soft and malleable, making it easy to bend and mould into delicate sheets and wires. Copper does not corrode and is therefore used in the production of water pipes among countless other significant necessities that are often overlooked in our society. Historically, Copper holds great significance as it was the first metal used by humans. It was discovered roughly 9000 years ago and was utilised by the Neolithic Man who learnt that heating the metal made it more malleable, thus tools and utensils were made which were far superior to the previous stone tools used by humans. This history and its connection to the current and ongoing relationship between humans and copper must be preserved and highlighted as it is integral to the history of all humankind. A small, palm-sized solid native copper mineral specimen with shades of browns, black and rustic tones throughout the specimen.NATIVE (metalic) COPPER / Locality: Moonta, South Australiabeechworth, burke museum, geological specimen, native specimen, geological, mineral, mineralogy, indigo shire, beechworth museum, copper, copper ore

This demijohn was made for Sharpe Bros., brewers of non- alcoholic drinks such as Dandelion Ale, ginger beer and cordial. Sharpe Bros began in New Zealand and expanded to Australia in the early 20th century. The company was taken over by Cadbury Schweppes in 1972. The likely manufacturer of this demijohn was Hoffman's Pottery of Brunswick.This item was recovered from the abandoned barn of the Pope family in 1971, when the property was sold to the Shire of Diamond Valley. This barn was located on the northern side of Pope Place and sketched by Ron Reynolds for the book "Greensborough and Greenhills".Glazed stoneware jar with dark brown glaze to top, narrow threaded neck with wire handle. Stopper missing.Transfer text on front: "This jar is the absolute property of and must be returned to Sharpe Bros. Australia and New Zealand"sharpe bros., hoffman pottery, stoneware jars

Numbered grid map of the City of Heidelberg showing municipal boundaries in 1984 . Scale 1 inch to 160 feet. Side 2: MMBW Plans Yarra 2000, note Ward boundaries not updated on this plan.An example of hard copy plans from the 1960s. Mainly from the Shire of Diamond Valley era (1964-1994).Map printed on brown paper and laminated. Double sided.city of heidelberg, mmbw

Shire of Diamond Valley timber sign. This sign would have been at the entry to one of the many public parks and reserves created during the time of the Shire of Diamond Valley (1964-1994). Following the redistribution of local government areas in 1994, the previous Shire of Diamond Valley was split between City of Banyule and Shire of Nillumbik. Signage would have been replaced to reflect the new 'owners' of the property. The exact location of this sign is unknown.Brown painted Timber sign with yellow writing etched into timbershire of diamond valley, sign, parks - greensborough

This specimen was recovered from Silverton Mine in Broken Hill, New South Wales. Otherwise known as the 'Day Dream Mine', the Silverton Mine was first established in 1883, when silver and lead deposits where discovered. Within a few short years, the population of Broken Hill reached 3000 people. As of today the Silverton Mine is still open, and has produced over 200 million tonnes of ore, which has generated over $100 billion. The Silverton Mine was also famous for a number of specimens such as silver, iron and zinc.Copper is considered to be a rare ore in that finding it in its pure form is rare. Nowadays when mining for Copper it is often found in mixed in with other minerals or it is recycled from use. Moreover, Copper is found in a range of everyday uses such as coins, cookware, pipes, heating conductors and anything that generate electricity. The fact that Copper is heat a heat conductor, electricity conductor and it does not corrode easily, makes this ore a versatile and useful. 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 cube-shaped sulfide and oxide with shades of green, grey and brown throughout. Copper is typically found as nuggets in the ground. It can be found in a range of forms such as its native state; mixed with other ores, such as zinc and iron; as porphyry copper deposits; and as major deposits. Porphyry deposits are when the mineral is scattered evenly throughout the rock. Major deposits are when the mineral is scattered amongst other minerals.burke museum, beechworth, indigo shire, beechworth musum, geological, geological specimen, mineraology, copper, copper ore, copper ore speciment, broken hill, new south wales

This particular specimen was recovered from the Lal Lal Coal and Iron Mine in Victoria, 19km from Ballarat. Brown Coal was discovered here in 1857, just alongside the Geelong to Ballarat Railway line. This discovery of lignite (brown coal) was the first in Victoria, which would bring important benefits to the region and state, both of which had previously been reliant on coal imports. In the 1860s, iron ore was found just 5km from Lal Lal, and the area was converted into an Iron Ore Mine. The Lal Lal Iron Mining Company took over operations in 1874, who then peaked iron production in 1884. This mine continued operations until June 1884, when the blast furnace was extinguished and never recommenced. The blast furnace at Lal Lal is considered one of the most important and highly significant sites ion early industrial history in Australia, as it is the only remaining best furnace from the nineteenth century in the Southern Hemisphere. The furnace ruins are 17 metres high, and are clearly visible today on Iron Mine Road, Lal Lal, near the Bungal Dam. This specimen of Lignite (brown coal) is significant, as it was mined from the area where brown coal was first discovered in Victoria, leading to an important and controversial future of the mining and use of brown coal in this State. The Victorian Heritage Database has listed the Lal Lal Coal Mine with local significance, with their Statement of Significance stating: "The Lal Lal coal mine is historically significant as the site of the first discovery of lignite (brown coal) in Victoria, and one that promised important benefits to regional and state industries that were reliant on coal imports at the time. The significance of the stie is reduced by the poor state of preservation of the coal mining and processing fabric". 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 light-weight, soft and combustable sedimentary rock specimen, that is dark brown in colour. The specimen has jagged edges, as though parts of the rock have crumbled away. Brown coal, or Lignite, is formed naturally from compressed peat, and is typically found in natural basins. The stages to the formation of coal ('coalification') begin with plant material and wood, which will decay if it is not subjected to deep burial or heating, and turn into Peat. Peat, when sufficiently compressed naturally, will turn into Brown Coal (Lignite), and finally into Black Coal (sub-bituminous, bituminous and anthracite). Each successive stage has a higher energy content and lower water content. It is brownish-black in colour. Brown Coal has a high moisture content, between 50 and 75 percent, and a low carbon content. Some Brown Coals may be stratified, with layers of plant matter, which means little coalification has occurred beyond the peat natural processing stage. When Brown Coal is submerged in dilute nitric acid or boiling potassium hydroxide solution, it reacts to produce a reddish solution, of which higher-ranked coals do not. When brown coal is pulverised and burned in boilers, the steam is used to drive turbines, which generates electricity. It is the lowest rank of coal, as when burned, it creates a relatively low heat content, which in turn does not create a great output of steam. burke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, mineralogy, brown coal, brown coal specimen, lignite, lal lal, lal lal coal mine, lal lal iron mine, ballarat, blast furnace

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

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

Front cover has a black and white photograph of a bearded man whose story is in the book. The back cover has a photograph of a man with his back to the camera and the blurb about the book.non-fictionThe devastating Victorian bushfires of February 2009 claimed the lives of 173 people. Since then, residents and property-owners throughout the Shire of Murrindindi have rallied together to reclaim their homes, their communities, their relationships and the landscapes they love. Many of them are senior citizens, who have demonstrated through their resilience, wisdom and sense of humour that age often means nothing more than numbers. From CFA volunteers to church-wardens, shearers to scone-makers, older members of the Shire of Murrindindi continue to play their parts in helping communities rise from the ashes. These are their portraits-and some of their stories.black saturday, bushfire, photographs, portraits, victoria

A history of the Baw Baw and Walhalla country of the Narracan Shire, VictoriaHardback. Brown dust cover. Photograph on front cover looks out from the entry of a mine onto the front of a building which has a hill to the side of it. The back cover has a photograph of the side of a hill with some trees on it.G&V THOMAS Stamp of the Marysville & District Historical Society Inc / P.O. Box 22 / Marysville 3779gold, gold field, gold miner, gold mining, gold town, walhalla, baw baw, gippsland, victoria, australia, history

This robe was the last City of Moorabbin Mayoral Robe, and was worn by Mayor Ron Brownlees, (prior to the City of Moorabbin's amalgamation with City of Glen Eira and City of Kingston in 1994). It was donated to the City of Moorabbin Historical Society in February 2007 by the City of Kingston. 12/11/2018 Cr Steve Staikos MAYOR City of Kingston requests that CMHS loan the Mayoral Robes and Jabot with Cuffs for display at KCC Officess Nepean Highway Cheltenham on going 7 Years. The Moorabbin Mayoral Robe with Jabot is displayed along with those of former City of Chelsea Robes and former City of Mordialloc Robes at Kingston City Council Office . The KCC possesses the Mayoral Chains of each former Council and they are displayed on the Mayoral Robes for the Annual Opening meeting of KCC in February .The City of Moorabbin developed from the Moorabbin Roads Board of 1862, becoming The Shire of Moorabbin in 1871 and the City of Moorabbin in 1934. In the 1994 Amalgamation of Councils the City of Moorabbin was divided between the new City of Kingston in the South and the new City of Glen Eira to the North . This is the last Mayoral Robe for the City of Moorabbin 1934- 1994City of Moorabbin Mayoral Robe. Full length garment of royal blue material, 55% Polyester & 45% Wool, with gold braid on hem and sleeves. Full length Collar and the cuffs are brown mink and sleeves are lined with blue satin. Two brass clips on shoulders are for the attachment of the Mayoral Chain. Hook and eye fasteners join the front of the robe. This is the last City of Moorabbin Mayoral Robe and was worn by Mayor Ron Brownlees, (prior to amalgamation in 1994), and donated to the City of Moorabbin Historical Society in February 2007 by the City of Kingston. 2018 the Robe with jabot was moved to Kingston City Council Office Cheltenham for display with former City of Chelsea Robe and former City of Mordialloc Robe. Label " Raymond W. Bredin & Son / 17 Glenola Road / CHELSEA VIC. AUSTRALIA / Robe Makers "clothing, tailors, formal wear, moorabbin, kingston, mayor, city of moorabbin, robes civic, moorabbin roads board, shire of moorabbin, brownlees ron, city of glen eira, city of kingston

Map of the City of Heidelberg from the Yarra River in the South to North of Watsonia Military Camp. Shire of Diamond Valley is shown to the north.Map showing municipal and ward boundaries, black text on light brown paper."Scale: 20 CHS = to 1 IN"city of heidelberg

Boys from the Methodist Children's Home Cheltenham collecting Briquettes from the shed. Briquettes, made from Brown coal, were an economical source of heating for the Home The Methodist Children's Home in Cheltenham was founded c1880 to provide housing for neglected children from the inner city. The Founders aimed to provide regular nourishment, a stable environment and integrate the children into the local community thereby improving their education and lives. ( see 00561) 1950's saw a new direction for the support of children and families in poor and difficult situations . The new Burwood Homes Facility opened in 1951 and children were transferred from Cheltenham in 1952. The land was sold to the St John of God, Catholic Order in1953 who maintained an orphanage until Myer Pty Ltd bought the site in 1967 and constructed the Southland Shopping Centrec1892-1953 The Methodist Children's Home Cheltenham was founded to provide safe accommodation and education for neglected children from the inner city slums. Black & White photograph of some boys in the Briquette Shed at Methodist Children's Home Cheltenham 1935Back Handwritten informationmethodist children's home cheltenham 1892-1953, briquettes, heating, yallourn brown coal mine, city of moorabbin, county of bourke, moorabbin roads board, parish of moorabbin, shire of moorabbin, henry dendy's special survey 1841, were j.b.; bent thomas, o'shannassy john, king richard, charman stephen, highett william, ormond francis, maynard dennis, cheltenham state school no.84, methodist chapel cheltenham, methodist school cheltenham, beaumaris west state school, meeres frederick, meeres walter, education, early settlers