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The Beechworth Burke Museum
Geological specimen - Fluorite (purple)
Fluorite comes in a variety of natural colours and crystal formations and glows under ultraviolet light (the word 'fluorescence' comes from the same etymological source). In its pure form, calcium fluoride, it is a colourless combination of the elements calcium and fluorine, but gains its colour from trace elements that infiltrate or replace calcium within its crystal structure during its formation. Although fluorite crystals polish well and can achieve a high level of lustre, the mineral is very soft (4 on MOHS hardness scale) so it is unsuitable for use in rings and must be handled and stored carefully if used in other forms of jewellery. Most crystals of the mineral are too coarse for decorative purposes but have been mined under the name fluorspar for a variety of commercial and industrial purposes. These include the production of hydrofluoric acid, smelting metal alloys, producing glazes and ceramic finishes and use in medical and dental products. An existing label for this specimen indicates that its origin or collection-point was 'probably USA.' Fluorspar, the form of fluorite used commercially and industrially, was mined in significant quantities in the counties of Hardin and Pope in South-Eastern Illinois throughout the Nineteenth and Twentieth Centuries. Fluorite was made Illinois' state mineral in recognition of its contribution to the state's identity and economy. The specimens are significant as examples of surveying activity undertaken to assess and direct the development of the mineral resource industries, as well as the movement to expand human knowledge of earth sciences such as mineralogy and geology in the nineteenth century.The specimen is a piece of purple shaded fluorite (also known as fluorspar), the mineral form of calcium fluoride. The unpolished specimen presents a dark purple interior with a substantial dark grey crust representing the matrix from which the specimen was obtained. Existing label: Flourite / (purple) / probably / USA / BB /burke museum, beechworth, geological, geological specimen, fluorite, flourite, calcium fluoride, hydrofluoric acid, jewellery, indigo shire, north-east victoria, mining, illinois, usa, united states, fluorine, gemstones, purple stones -
The Beechworth Burke Museum
Geological specimen - Malachite, 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. This particular specimen was recovered from the Burra Burra Copper Mine in Burra, South Australia. Otherwise known as the 'Monster Mine', the Burra Burra Copper Mine was first established in 1848 upon the discovery of copper deposits in 1845. Within a few short years, people from around the world migrated to Burra to lay their claim in the copper economy. By April 1848 the mine was employing over 567 people and supporting a population of 1,500 in the local township. Up until 1860, the mine was the largest metals mine in Australia, producing approximately 50,000 tonnes of copper between 1845 to its closure in 1877. The Burra Burra Mine was also famous for a number of other specimens, including; crystalline azurite, cuprite, and botryoidal and malachite.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. 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 shades of yellow, blue, and light green throughout.geological, geological specimen, burke museum, indigo shire, malachite, malachite specimen, burra burra mine, burra, south australia, australian mines, mines, monster mine -
Coal Creek Community Park & Museum
Mineral Water
tall Green Bottle with lots of air bubbles Faded brown labelDeep Spring Mineral Water Daylesford Vic -
The Beechworth Burke Museum
Geological specimen - Greenstone / Gabbro, Unknown
This specimen was recovered from Ceres West of Geelong, Victoria. Greenstone is the name for any metamorphosed basic igneous rock (in the case of this specimen, Gabbro) that gains its greenish colour to the presence of the minerals chlorite, actinolite, or epidote, hence the term 'green' and 'stone'. Greenstone is often formed through metamorphsis along a convergent plate boundary. In the rock cycle (the series of processes that creates the various types of rocks) there are identified three different types of rocks, which are the sedimentary, the igneous and the metamorphic. Metamorphic rocks started out as sedimentary, igneous or earlier metamorphic rocks but changed from their original condition under the effect of high heat, high pressure or hot, mineral-rich fluid. However, if pressure or heat is too high, then the rock will melt, resulting in the formation of an igneous rock. The name used to describe these types of rocks reflects this specific inherent trait of change, since the word “metamorphic” derives from the Greek word “metamorphosis”, meaning “change of form or structure”. Metamorphic rocks form in the Earth`s crust but can be also found on the surface, due to elevation of the Earth`s surface. They are divided into two categories: the foliated metamorphic and the non-foliated metamorphic rocks. Gabbro is a highly useful mineral that is often polished to create cemetery markers and kitchen benches. It is notable for its qualities of durability, being able to withstand extreme elements and wear. Whilst not rare, Gabbro is of great utility and has been highly desirable for its qualities. 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.Greenstone is a solid hand-sized metamorphic mineral of a green colour. Greenstone is the name for any metamorphosed basic igneous rock (in the case of this specimen, Gabbro) that gains its greenish colour to the presence of the minerals chlorite, actinolite, or epidote, hence the term 'green' and 'stone'. Gabbro is a medium to coarse grained rocks that consist primarily of plagioclase feldspar and pyroxene. Greenstone is often formed through metamorphsis along a convergent plate boundary. Gabbro forms due to cooling and crystallization of magma underneath Earth's surface. Greenstone/Gabbro/from Ceres west/of Geelong. Has old Geological Survey label/and probably collected by/Richard Daintree in 1861/C.Willam 15/4/21/ Other label: 62 /greenstone, metamorphosed, igneous rock, gabbro, chlorite, actinolite, epidote, metamorphsis, rock cycle, various types of rocks, sedimentary, high heat, high pressure, mineral-rich fluid, metamorphosis, foliated metamorphic, non-foliated metamorphic, convergent plate boundary, greenish colour, minerals -
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 -
Ballarat Heritage Services
Photograph - Colour, Hepburn Mineral Springs Reserve, 2019, 22/04/2019
Colour photograph of the Hepburn Mineral Springs Reserve.hepburn springs, mineral springs reserve -
Ballarat Heritage Services
Photograph - Colour, Hepburn Mineral Springs Reserve, 2019, 22/04/2019
Colour photograph of the Hepburn Mineral Springs Reserve.hepburn springs, mineral springs reserve -
Ballarat Heritage Services
Photograph - Black and White, Mineral Spring at Daylesford, 1934
Black and white photograph of a mineral spring at Daylesford. john joseph gervasoni, mineral springs, daylesford -
Ballarat Heritage Services
Photograph - Colour, Entrance to Vaughan Springs, 2017, 16/07/2017
Colour photograph of the entrance to Vaughan Mineral Springs. vaughan, vaughan springs, vaughan chinese cemetery, chinese -
Ballarat Heritage Services
Digital photograph, Lisa Gervasoni, Hepburn Mineral Springs Reserve changes without permit, 2017
Colour photograph to changes at the Hepburn Mineral Springs.hepburn mineral springs reserve, locarno, pleasure gardens, social heritage, state significant, landscaping -
Ballarat Heritage Services
Photograph, Clare Gervasoni, Plaque at Locarno Springs, Hepburn Mineral Springs, 24/09/2019
Plaque at Locarno Springs, Hepburn Mineral SpringsHEPBURN SPRINGS Where reverent gum trees gray-leaved aroming stems Enshrine the greem 'tween walls of slanting slate, Run waters, sihones from some buried grate, In drops more precious than deep mined gems. The elements are liquid in that stream and bursting bubbles charge the atmosphere The breath of nature moves the grasses here, and all is tranquil as a midday dream. The alchemist did set a mighty task, to list an learn the components of life, To change and find some radiant power new from atoms boiled in baking tube ad flask, and now we fear colossal human strife with things the caldrons of the Earth Eschew W.H.S. 1962hepburn springs, whs, mineral springs reserve, locarno spring -
The Beechworth Burke Museum
Geological specimen - Chalcopyrite
This specimen originated from Mount Lyell on the west coast of Tasmania, where a large group of open cut and underground copper-silver-gold mines began operating in 1883. Between 1893-1994, the Mt Lyell Mining and Railway Company were responsible for operations. The Mt Lyell copper-gold mines produce some excellent crystallised specimens of chalcopyrite and other minerals. The deposits are generally considered to be of Cambrian volcanic origin, but there are indications of Devonian granitic influence on the ores, plus local remobilisation during Devonian deformation. Over 120 million tonnes of ore was produced from several workings, including the main Prince Lyell mine and the North Lyell mine, which was also of great importance. The Mount Lyell mines have a long history of human and environmental disasters, including the 1912 North Lyell fire that killed 42 miners, and two separate incidents in 2013 in which three people lost their lives. The environmental impacts from this complex of mines are extensive, with waste tailings and heavy metal contamination flowing directly into the King and Queen River catchments. In 1954, the eminent Australian historian, Geoffrey Blainey, published 'The Peaks of Lyell' which delves into the history of the 1912 North Mount Lyell Disaster.Chalcopyrite does not contain the most copper in its structure relative to other minerals, but it is the most important copper ore since it can be found in many localities and occurs in a variety of ore types. The brassy-yellow colours in Chalcopyrite mean it is often confused with pyrites and gold, leading to use of the term, "fool's gold." Chalcopyrite has been the primary ore of copper since smelting began five thousand years ago. 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.This hand sized solid mineral specimen has shades of brass-yellow with spots of iridescent green-black tarnish. Chalcopyrite is a copper iron sulphide mineral and a major ore of copper common in sulphide veins and disseminated in igneous rocks. Chalcopyrite has a hardness of 3.5-4 on the Mohs Scale. It is a member of the tetragonal crystal system and has metallic lustre and opaque transparency.burke museum, beechworth, indigo shire, beechworth museum, geology, geological specimen, chalcopyrite, copper pyrites, copper mining, tasmanian geology, mount lyell, mount lyell mines, fools gold, mohs scale, crystals, minerals, historical geological collection, victorian geological survey, a.r.c selwyn, gold rush, van diemans land -
The Beechworth Burke Museum
Geological specimen - Kaolin, unknown
Kaolin is also known as china clay. This specimen came from Dunolly, Victoria and was donated to the Museum in 1868 as part of the Geological Survey of Victoria. This survey helped map and study the geology of Victoria. In Victoria, Kaolin is particularly used as a filler and coating material in paper manufacture. It can also be used in paints, ceramics, rubbers and plastics. There are many kaolin deposits in Victoria but many of these have been mined out and there is not much Kaolin left. Rocks that have a high amount of Kaolinite and it can be formed through the decomposition of other materials. There are two types of Kaolin; hard and soft kaolin. Soft kaolin's are coarse but have a soapy texture. It can also break easily. The hard kaolins have an earthly texture and are finer grained. This means that they are harder to break, unlike the soft kaolin. Hard kaolin's are formed by flocculation in salt water, a process that in basic terms, bonds particles together. Kaolin is a common material in Victoria and that is why it is significant. While this specimen was mined in Dunolly, Victoria Kaolin can also be found Pittong, Pakenham, Bulla, Hallam and Ballarat as well as many other places throughout Victoria. This specimen represents the presence of Kaolin deposits in this region of Australia. It is also significant because Kaolin has many uses and is largely beneficial to many manufacturing processes in Victoria. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.Two pieces of Kaolinite mineral with shades of white and graygeological specimen, geology, geology collection, burke museum, beechworth, kaolin, china clay, dunolly, geological survey of victoria, kaolinite, victoria, mining, mining deposits, geology of victoria, australia, filler, coating material, paper manufacture, paint, ceramics, rubbers, plastics, decomposition, materials, soft kaolin, hard kaolin, flocculation, particles, salt water -
University of Melbourne, Burnley Campus Archives
Document, Managing Victoria's Mineral Resources for you, c. 1978
Information Booklet. Department of Minerals and Energy, 40 pp.mineral resources, management, victoria -
Ballarat Heritage Services
Photograph - Colour, Clare Gervasoni, Entrance to Vaughan Springs, 2017, 16/07/2017
Timber entrance feature to Vaughan Mineral Springs Reserve.vaughan, vaughan springs, vaughan chinese cemetery, chinese, mineral water -
Federation University Historical Collection
Book, F. Higham, FOurth Empire Mining and Metallurgical Congress Proceedings, 1950
Red book of 551 pages. Contents include: * Invitation to hold the next congress in Australia * Mineral Industry in Australia (P.B. Nye) * Some notes on the Mineral Resources of the Union of South Africa (A.R. Mitchell) * Mineral Exploration in Australia (C.J. Sullivan) * Environmental COnditions in British Coal Minesnon-fictionmining, australia, canada, south africa, mining and metallurgical congress -
The Beechworth Burke Museum
Geological specimen - Sphalerite, Unknown
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 -
Federation University Historical Collection
Book, Mines and Minerals: A Guide for the Australian Miner, 1885
This book was presented to Professor Ferdinand Krause of the Ballarat School of Mines by the co-author Felix Ratte who had taught Geology at the Ballarat School of Mines. Felix Ratte became mineralogist to the Australian Museum, Sydney.Hardcovered book with brown cloth cover. 341 pages with illustrations. Chapters in the book include Geology; Rocks and their Movements; Stratified Deposits; Mineral Veins and Lodes; Dynamics of Lodes; Filling of Lodes; Irregular Deposits; Alluvial Deposits; Physical Properties of Minerals; Compsition and Determination of Minerals; Noble Mineral; Silver and Lead; Quicksilver or Mercury; Haloids and salts; Quartz and Opal; Precious stones; assays and the use of Blowpipes; Special Assays for Gold and SilverFrontise page handwritten in ink: 'Prof. Krause from F. Ratte'mining, ballarat school of mines, geology, felix ratte, minerals, ferdinand krause -
Ballarat Heritage Services
Photograph - Colour, Caretaker's Cottage at Hepburn Mineral Water Spring, c2003
Colour photographs of the caretaker's cottage at Hepburn Springs Mineral Reservehepburn springs, hepburn springs mineral reserve, caretaker's cottage -
Ballarat Heritage Services
Photograph - digital photographs, Lisa Gervasoni, Hepburn Springs Bathhouse, c2000
Ccolour photograph of a brick bathouse at Hepburn Mineral Springs Reserve. baths, bathhouse, mineral water, renovation, chimney -
Ballarat Heritage Services
Photograph - Photograph - Colour, Locarno Spring in the Hepburn Springs Reserve, 2019, 22/04/2019
Colour photograph of the Locarno Spring at Hepburn Mineral Springs Reserve.hepburn springs, locarno, mineral water, hepburn springs reserve -
The Beechworth Burke Museum
Geological specimen - Olivine Crystals, Unknown
Olivine is mostly found on the Earth's surface in igneous rocks that are dark-coloured. It is common at divergent plate boundaries and at warm spots, such as volcanic areas. It crystalises and forms during the cooling of magma. Olivine is used in refractory sand, bricks, and gemstones. Olivine has been found on a number of meteorites, which might have originated from large asteroids or the mantle of a now-destroyed planet. This olivine crystal is thought to originate from Mount Noorat, with speculation that it could have originated from Mount Shadwell. Mount Noorat is a dormant volcano cone located in the Newer Volcanics Province of Victoria. Mount Noorat belongs to the Kirrae Wuurong people, who used the Mount as a place for meetings and gatherings prior to European settlement. Contact was first made between European settlers and the Indigenous people in 1841. The Mount has mostly been used for cattle and sheep grazing. Mount Shadwell is a well-known source of olivine and is the highest of a gathering of volcanic cones. The New Volcanic Province is located in South East Australia and covers 15000 square kilometres. It contains 400 explosive vents and small shield volcanoes. The last eruption is thought to have occurred 5000 years ago at Mount Gambier and Mount Schank. This olivine crystal has been identified as a volcanic bomb, which is a molten rock which was pushed out and ejected into the air when a volcano reupts. A rock needs to be larger than 65 mm in diameter to be classified as a volcanic bomb. This olivine volcanic bomb and its locality is historically and socially significant. The olivine was found in the Newer Volcanic Province, an area which contains over 400 dormant volcanoes. This olivine is one part of a volcanic bomb, which would have ejected when magma erupted out of a volcano. 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 iron-magnesium silicate mineral with shades of green and brownburke museum, beechworth, geological, geological specimen, olivine, igneous rock, volcanic, gemstones, volcanic bomb, meteorites, asteroids, plantes, mount noorat, mount shadwell, indigenous, kirrae wuurong people, newer volcanics province, victoria, european settlement, eruption -
Federation University Historical Collection
Booklet, George Skinner (Acting Government Printer), Mineral Statistics of Victoria for the Year 1874, 1875
White Foolscap printed Government document relating Victoria's mineral statistics.mineraal statistics, statistics, angus mackay, gold exports, ballarat, beechworth, sandhurst, maryborough, castlemaine, ararat, gippsland, silver, tin, copper, antinomy, lead, iron, coal, lignite, kaolin, flagging, slates, magnesite, diamonds, sapphires, robert brough smyth, miners, machines, gold yeild, water rights, gunpowder, mining companies, mining divisions, wages, miners' rights, miners rights, business licenses -
Federation University Historical Collection
Booklet, Report of the Board Appointed to Advise the Government as to the Best Mode of Developing the Auriferous and Mineral Resources of the Colony, 1879-80, 1880
White Foolscap printed Government document relating Victoria's mineral resources.mineral resources, mining, mining districts, ballarat mining district, auriferous resources, william collard smith, rivett henry bland, henry rosales, robert m. sergeant, a.w. howitt, deep leads, carisbrook, sebastopol, sebastopol plateau, r.m. harvey, james m. main, john wall, g. hale, t.h. thompson, james leckie, e.h. uren, james cotter, p. matthews, w.k. peden, john sharp, g.c. robinson, dead horse lead, william benson, j. keith, smythesdale, charles thorne, haddon, linton, little bendigo, scarsdale, blackwood, daylesford, owen jones, james mcmillan, h.h. sainsbury, thomas bury -
Federation University Historical Collection
Booklet, Robert Brain, Government Printer, Mineral Statistics of Victoria for the Year 1880-1881, 1881
White Foolscap printed Government document relating Victoria's mineral statistics.statistics, mineral statistics, h.r. williams, gold yeild, gold, silver, tin, copper, antinomy, lead, iron, coal, lignite, kaolin, flagging, slates, quartz mining, gold districts, ballarat, beecworth, bendigo, sandhurst, maryborough, castlemaine, ararat, gippsland, water rights, gunpoweder, mining companies -
Bendigo Historical Society Inc.
Book - QUALTROUGH COLLECTION: THE GOLDFIELDS AND MINERAL DISTRICTS OF VICTORIA, 06/06/2023
The Goldfields and Mineral Districts of Victoria Written by R Brough Smyth F.G.S. Printed and Published by John Ferres, Government Printer. Melbourne in 1869. Sub tiltle Notes on the Modes of Occurrence of gold and other minerals.R Brough Smyth F.G.S.history -
Federation University Historical Collection
Book, Simple Tests for Minerals or Every Man His Own Analyst, 1898
Green hard covered book of 163 pages. Contents include matter, crytallography, minerals, flame coloration, blow pipe flame, blow pipe analysis, wet tests, precious stones, arrangement of mineral collectionsminerals, analyst, brook, campbell, crystallography, blow-pipe, precious stones -
Ballarat Heritage Services
Photograph, Nucolorvue, Daylesford Pioneer Tower in Wombat Garrdens, 1957
Daylesford is a tourist town in Central Victorian, known for its mineral water springs.Image of the Daylesford Pioneer Memorial Tower in Wombat Gardens, Daylesford.Daylesford, Victoria, Australia This famous holiday resort is famous for its up-to-date facilities, as well as for its natural attractions. The mineral Springs are renowned for their high medicinal elements. The visitor finds ample to amuse, in excellent fishing, boating, Boating, Swimming, golfing, hiking and riding. The district provides a wide range of typical Australian bush scenery, and the altitude of 2,000 feet above sea level as a tonic effect on all. Daylesford has modern hotels, guest houses, shops and places of amusement, also many other places of interest within short travelling distance. Bendigo, 50 miles, Ballara 30 miles, and Melbourne 75 miles, bring Daylesford within easy reach of many parts of Victoria. daylesford, pioneer tower, wombat gardens -
Ballarat Heritage Services
Photograph, Nucolorvue, A Corner of Jubilee Lake, Daylesford, 1957
Daylesford is a tourist town in Central Victorian, known for its mineral water springs.Image of Jubilee Lake, Daylesford.Daylesford, Victoria, Australia This famous holiday resort is famous for its up-to-date facilities, as well as for its natural attractions. The mineral Springs are renowned for their high medicinal elements. The visitor finds ample to amuse, in excellent fishing, boating, Boating, Swimming, golfing, hiking and riding. The district provides a wide range of typical Australian bush scenery, and the altitude of 2,000 feet above sea level as a tonic effect on all. Daylesford has modern hotels, guest houses, shops and places of amusement, also many other places of interest within short travelling distance. Bendigo, 50 miles, Ballara 30 miles, and Melbourne 75 miles, bring Daylesford within easy reach of many parts of Victoria. daylesford, jubilee lake, pier -
Ballarat Heritage Services
Photograph, Nucolorvue, Panorama Looking Towards Wombat Hill at Daylesford, 1957
Daylesford is a tourist town in Central Victorian, known for its mineral water springs.Panorama Looking Towards Wombat Hill at DaylesfordDaylesford, Victoria, Australia This famous holiday resort is famous for its up-to-date facilities, as well as for its natural attractions. The mineral Springs are renowned for their high medicinal elements. The visitor finds ample to amuse, in excellent fishing, boating, Boating, Swimming, golfing, hiking and riding. The district provides a wide range of typical Australian bush scenery, and the altitude of 2,000 feet above sea level as a tonic effect on all. Daylesford has modern hotels, guest houses, shops and places of amusement, also many other places of interest within short travelling distance. Bendigo, 50 miles, Ballara 30 miles, and Melbourne 75 miles, bring Daylesford within easy reach of many parts of Victoria. daylesford, wombat hill, flora