The Bendigo School of Mines was opened in 1873 following the first report of the Technological Commission in 1869 which recommended the establishment of schools of design and science to meet the scientific and technical needs of the mining industry on the local gold fields. Initially mining, chemistry, geology, metallurgy and art were taught while a separate school of design was established in c. 1870 but incorporated into the School of Mines around 1883 when it was renamed as the School of Mines and Industry. In 1904 The Mechanics Institute was liquidated and its assets and buildings acquired by the School of Mines. Around 1907 a Junior Technical School commenced to operate at the School of Mines and Industry but ceased operating in 1961 with that function being transferred to the White Hills and Kangaroo Flat Technical Schools.Obverse; Ornate relief design made up of a coat of arms with mining icons in each quarter flanked by flags on either side. Per varios usus artem experientia fecit written in scroll underneath. Translation: Practice has brought skill through different exercises. (Manilius) Reverse; Outer wheel Bendigo School of Mines and Industries. Inner; 1873 /Jubilee /1923Obverse; Per varios usus artem experientia fecit Reverse; Outer wheel Bendigo School of Mines and Industries. Inner; 1873 /Jubilee /1923city of greater bendigo education, bendigo school of mines

4 pages from the 'Mining and Geological Journal', July 1938. Front page is an index to figures in the graptolite collection. 'Numbers in brackets are taken from the Fossils Register of the Mines Department Museum, Melbourne, and refer to the specimens in the Museum.' Lancefieldian, Bendigonian, Chewtonian, Castlemainian, Yapeenian, Middle Ordovician, Upper Ordovician, Gisbornian, Estonian and Bolindian categories are described. The numbers on the BHS fossil collection relate to the numbers/names on the page. Two following pages illustrate the fossil types within the major categories. Small sign with pages ' 'Fossils, Bendigo & /surrounding Districts' was with the fossil display in a glass display cabinet, ex Museum of Mines Museum, Bendigo.

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

New Zealand Greenstone, also called Pounamu is found on New Zealand’s South Island in riverbeds and boulders, and colours vary depending on the source, but always include green tones. It is a form of the mineral nephrite, also known as jade, and is a tough stone with a crystalline structure, made up of calcium magnesium and iron silicate. Its hardness means it is ideal for carving, and has been used for this purpose throughout history, especially by the Maori people of New Zealand. Greenstone features heavily in Maori mythology, and the traditional name for the South Island, Te-Wai-Pounamu, literally translates to waters of greenstone. Wearing of Greenstone pendants with different carvings is practiced by Maori to represent connection to land and ancestors, or to endow the wearer with certain attributes. The sticker on the base of the specimen identifies it as a product of Hokitika Jade Company. The company, which was active in the 1970s, sold jade and greenstone specimens and ornaments. Hokitika, which started life as an 1860s gold rush town, is the origin of most nephrite found in New Zealand, and the centre of the Greenstone carving industry. The object has scientific and research potential as part of the Burke Museum's Geology Collection, and as and example of New Zealand Greenstone. It also has spiritual significance for it's role in Maori beliefs and communities, where it is both traditionally worn and features in mythology. As a valuable stone regularly used in carving and jewellery, it has aesthetic significance. Sticker on base: "N.Z. Greenstone/ a product of/ Hokitika Jade Coy."geological specimen, geology, geology collection, burke museum, beechworth, new zealand, greenstone, hokitika, nephrite, jade

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

A collection of eight large fold out coloured maps published in a bound book formnon-fictionThe Melbourne Study Report is a series of volumes describing the physical nature of the land and its environment, examines the likely forms of land use, and assesses the hazards associated with these uses. This is Volume 2 (coloured maps). The first page featues a black and white map described as "Shire of Diamond Valley" with public land marked in yellow. Followed by eight large fold out maps. Melbourne Study Area Public land and descriptive blocks, Population description, Geology, Physiography, topography and rainfall, vegetation and water supply. The Land Conservation Act 1970 established the Land Conservation Council whose functions is to "carry out investigations and make recommendations to the Minister with respect to the use of public land in order to provide for the balanced use of land in Victoria. This report sets out to describe and assess the natural resources of the public lands in the Melbourne area and provides a factual basis on which members of the community may base submissions to the [Land Conservation] Council of Victoria. maps, shire of diamond valley, population, geology, topography, rainfall, vegetation, water supply, land use, public lands

Three handwritten pages relating to gold discovery at Ballarat.ballarat, gold discovery, smythesdale, bunninyong, warrenheip, geology, archibald yuille, pyrenees, clunes, herbert swindles

Colour photograph of a metal fire brigade at Cape Bridgewater.cape bridgewater, geology, ocean, coastal, landscape, cfa, fire, station, fire brigade, cape bridgewater fire brigade

Native Sulphur in its solid form is a yellow crystalline mineral that forms near volcanic vents and fumaroles where it is the solid form of hot gases. It is also frequently found in the subsurface as a by-product of sulphide ore mineralization. In all its forms, sulphur is one of the most commonly occurring minerals on the planet, especially in natural gases, and is key to the make-up of a range of other minerals. It is essential to continuing life on earth, and was used in ancient societies as part of medical care, religious rites, and entertainment, and was key to the invention of gunpowder by the Chinese. Native Sulphur in its solid form is a yellow crystalline mineral that forms near volcanic vents and fumaroles where it is the solid form of hot gases. It is also frequently found in the subsurface as a by-product of sulphide ore mineralization. In all its forms, sulphur is one of the most commonly occurring minerals on the planet, especially in natural gases, and is key to the make-up of a range of other minerals. It is essential to continuing life on earth and was used in ancient societies as part of medical care, religious rites, and entertainment, and was key to the invention of gunpowder by the Chinese. The exact site of extraction for this specimen is unknown, but it was probably collected in New Zealand in the 1850s. Sulphur is significant both for its historical and current uses, and for its nature as one of the most abundant minerals on the planet. Sulphur's importance comes both from its abundance and its role in ensuring survival, creating other minerals, and daily human life. This specimen is significant as representative of sulphur's solid properties. 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, small, crystalline mineral specimen that is largely bright yellow, with some darker spotting. geological specimen, geology, geology collection, burke museum, beechworth, sulphur, native sulphur, new zealand, native sulphur specimen, sulphur specimen

Fiver black and white photographs showing the former Union Building, now the Federation University Albert Coates Complex, under construction. .1) View of the first stage residences site south west, shows Stage 1 Engineering and Metallurgy/Geology. .2) View of the first stage residences site to the South west. Roadway dam creates upper pond. .3) View of the first stage residences site to the eastward. Shows lower pond and roadway dam. .4) View of the first stage residences site to the South. Start of Union Building Construction. .5) .View to the south east across lower pond, shows the Tree of Knowledge and first stage buildings.albert coates complex, union building, mount helen campus

Between 1869 and 1892, the Ringwood antimony mines produced more than 3,500 tons of antimony ore, which represented bout 15 per cent of Victoria's antimony production for that period. Much greater amounts were later taken from the mines at Costerfield and the Ringwood mines lapsed into obscurity. Most of the information in this booklet has been obtained from published and unpublished Geological Survey and Mines Department reports and Lease Records. (See full list of references included).

In the early 1880s the Ballarat School of Mines Council introduced a three year course of training under the professors to qualify students in the following professions: 1. Mining Engineering 2. Metallurgy 3. Geology 4. Electricity [45] Each of these courses had an additional, but optional, fourth year of study. The prescribed subjects of study for an Associateship was set out in the Calendar of the Ballarat School of Mines in each year. Any student who passed the prescribed examinations in any of the above courses was issued with a Certificate of Competency, and conferred with the distinction of Associate. By the 1890s the professorial staff had drawn up a curriculum leading to an Associateship of the Ballarat School of Mines. The first two years work was to be common to all courses, but in the third and subsequent years the student wold be devoted to a specialised branch of study. The Associateship was to be conferred in one of another of the following Courses: Agriculture, Civil Engineering, Electrical Engineering, [Geology], Metallurgy and Mining Engineering. All were three year courses except for Agriculture which was two years. Each course was conducted in accordance with a prescribed curriculum and syllabus. During the 1910s there was an expectation that candidates for the Associate course should have attained the age of sixteen, and have received preparatory training equivalent to University Matriculation at least in the subjects of Elementary Mathematics, English Grammar and Composition, or have passed through Junior Technical School. In 1960 an new procedure for admission to graduate status as Associates was introduced to the Ballarat School of Mines where Associateship would be conferred at a public ceremony. After 01 July 1976 graduates of Ballarat College of Advanced Education and Ballarat College of Advanced Education were admitted in major studies relating to mining for Australian accreditation and overseas purposes. Ballarat School of Mines Associates could ascribe ASMB after their name.Black and white photograph of Associatedsof the Ballarat School of Mines from 1951-1957.Associates of the Ballarat School of Mines :Lists names 1989-1964ballarat school of mines, smb campus, electrical engineering 1958, brian w. schreenan civil engineering 1958, clifford j. restarick metallurgy 1958, john t h. clelland metallurgy 1958, donald c. stevens mining engineering 1958, john g. wolfe civil engineering 1959, james e. mcneil electrical engineering 1959, patrick h. nally civil engineering 1959, graham j. willey metallurgy 1959, stanley p. kisler civil engineering 1959, donald j. overall electrical engineering 1959, brian j. mclennan civil engineering 1959, philip j. davis art 1959, bruce v. mcdougall mining engineering 1959, lancelot j. matthews mechanical engineering 1959, alan w. wilson mechanical engineering 1959, alan w. wilson electrical engineering 1959, george a r. lewis art 1959, noel e. meagher electrical engineering 1960, john l. collier mining engineering 1960, john l. collier civil engineering 1960, frank andrewartha mechanical engineering 1960, norman leckie art 1960, lansell j. groat civil engineering 1960, boon thiam lu mining engineering 1960, oswyn n. hails civil engineering 1960, john a. watts applied chemistry 1960, thomas b. gallagher civil engineering 1960, brian a. bellingham civil engineering 1961, alan c leviston applied chemistry 1961, walter j wynd civil engineering 1961, francis d benjamin civil engineering 1961, leonard e fox mechanical engineering 1961, yan kai chung applied chemistry 1961, george d mcgrath mechanical engineering 1961, john r sawyer mechanical engineering 1961, ronald horgan applied chemistry 1961, douglas j vendy civil engineering 1961, john a barnes electrical engineering 1961, brian w smith metallurgy 1961, william r carlyon metallurgy 1961, chris p livitsanos metallurgy 1961, lawrence g trevan civil engineering 1961, richard g dunlop mechanical engineering 1961, ronald m ingleton mechanical engineering 1961, peter m robinson mechanical engineering 1961, david j jelbart mechanical engineering 1961, john g hollway mechanical engineering 1961, george m hetherington civil engineering 1961, david w brown mechanical engineering 1961, john r gowan civil engineering 1961, geoffrey a christian civil engineering 1961, arthur c burrow mechanical engineering 1961, john n mcarthur applied chemistry 1961, graeme r bromley mechanical engineering 1961, william davison civil engineering 1961, ben a johnson electrical engineering 1961, ben a johnson civil engineering 1961, allan j tinney civil engineering 1961, thomas h j coad applied chemistry 1961, brian h duthie civil engineering 1961, basil c bautovich mechanical engineering 1961, reece pullen electrical engineering 1961, john d carmichael electrical engineering 1961, william j spencer civil engineering 1961, neil a brogden civil engineering 1961, michael villani civil engineering 1961, ralph j hepburn mechanical engineering 1961, peter w linaker mechanical engineering 1961, peter j matthews mechanical engineering 1961, edgar mca bartrop mining engineering 1961, donald j stewart, brian schreenan

Blue soft covered foolscap report with 15 plans and sections.pitfield, gold, mining, geology, pitfield plains, british banner, pitfield plateau, pitfield quartz and cement, woady-yalloak, queen of the plans, glenfine

Blue soft covered foolscap book of 4 pages. The book includes a folded, colour contour plan shewing reefs and Surface Works Little Bendigo Gold Field and an Underground Survey of Mines, Metropolitan, Monte Cristo Linelittle bendigo, nerrena, h.s. whitelaw, william baragwanath, geology, monte christo, monte cristo, neerena, nerrina, plans, mining cgt

Co-author Gerry Robinson was a speaker at a Surrey Hills Historical Society (SHHS) meeting. Lyndel Walker, member of SHHS, purchased the book for the collection. This book examines the changing landscape of Canterbury Road from the early days of settlement until today (2015)This book examines the changing landscape of Canterbury Road from the early days of settlement until today (2015)burke, surrey hills, canterbury, broughton park, vegetation, (mr) denis delaney, geology, (mr) john mcclare, geography, (mrs) mary mcclare, churches

Tertiary education at Ballarat began with the establishment of the School of Mines in 1870, making it Australia's third oldest tertiary institution. Classes began in surveying, mathematics, chemistry and a decade later they included metallurgy, assaying and geology. The technical division provided such programs as wool classing, plumbing and bricklaying. In 1967, it was split into three separate institutions, Ballarat School of Industries, Ballarat Technical School, and Ballarat Institute of Advanced Education. Then in 1976 the Ballarat Institute of Advanced Education became into Ballarat College of Advanced Education. The Ballarat School of Industries and Ballarat Technical School became the School of Mines and Industries, Ballarat (SMB). In 1998, the Ballarat School of Mines and Industries and the Horsham-based Wimmera Institute of TAFE merged with the University of Ballarat. The university merged with Monash University's Gippsland (Churchill) campus in 2013 and the merged schools are now the Federation University AustraliaThis woven band of dark blue has two narrow bands of gold on either side. It has a 4cm turn back at the end, which is held by a folded and stitched piece of the same band placed at ninety degrees around the band. school of mines ballarat, hat band, uniform, costume, textiles

Tertiary education at Ballarat began with the establishment of the School of Mines in 1870, making it Australia's third oldest tertiary institution. Classes began in surveying, mathematics, chemistry and a decade later they included metallurgy, assaying and geology. The technical division provided such programs as wool classing, plumbing and bricklaying. In 1967, it was split into three separate institutions, Ballarat School of Industries, Ballarat Technical School, and Ballarat Institute of Advanced Education. Then in 1976 the Ballarat Institute of Advanced Education became into Ballarat College of Advanced Education. The Ballarat School of Industries and Ballarat Technical School became the School of Mines and Industries, Ballarat (SMB). In 1998, the Ballarat School of Mines and Industries and the Horsham-based Wimmera Institute of TAFE merged with the University of Ballarat. The university merged with Monash University's Gippsland (Churchill) campus in 2013 and the merged schools are now the Federation University AustraliaThese circular cuff links are the Coat of Arms of the School of Mines Ballarat and are made of sterling silver and white, yellow, green and blue enamel attached by three links to a small bar with dumb bells. On face - Ingenio Effodere Opesschool of mines ballarat, school crest, cuff links

Tertiary education at Ballarat began with the establishment of the School of Mines in 1870, making it Australia's third oldest tertiary institution. Classes began in surveying, mathematics, chemistry and a decade later they included metallurgy, assaying and geology. The technical division provided such programs as wool classing, plumbing and bricklaying. In 1967, it was split into three separate institutions, Ballarat School of Industries, Ballarat Technical School, and Ballarat Institute of Advanced Education. Then in 1976 the Ballarat Institute of Advanced Education became into Ballarat College of Advanced Education. The Ballarat School of Industries and Ballarat Technical School became the School of Mines and Industries, Ballarat (SMB). In 1998, the Ballarat School of Mines and Industries and the Horsham-based Wimmera Institute of TAFE merged with the University of Ballarat. The university merged with Monash University's Gippsland (Churchill) campus in 2013 and the merged schools are now the Federation University AustraliaThese Coat of Arms of the School of Mines Ballarat are circular lapel badges and are made of sterling silver and enamel. The circular disc is attached to a long pin. 1). The enamel is yellow, green and blue 2). The enamel is white, yellow, green and blueOn face - Ingenio Effodere Opesschool of mines ballarat, school crest, lapel pins

Tertiary education at Ballarat began with the establishment of the School of Mines in 1870, making it Australia's third oldest tertiary institution. Classes began in surveying, mathematics, chemistry and a decade later they included metallurgy, assaying and geology. The technical division provided such programs as wool classing, plumbing and bricklaying. In 1967, it was split into three separate institutions, Ballarat School of Industries, Ballarat Technical School, and Ballarat Institute of Advanced Education. Then in 1976 the Ballarat Institute of Advanced Education became Ballarat College of Advanced Education. The Ballarat School of Industries and Ballarat Technical School became the School of Mines and Industries, Ballarat (SMB). In 1998, the Ballarat School of Mines and Industries and the Horsham-based Wimmera Institute of TAFE merged with the University of Ballarat. The university merged with Monash University's Gippsland (Churchill) campus in 2013 and the merged schools are now the Federation University Australia. Gold coloured School of Mines Ballarat brass badges with blue and green enameling. Box of 72 (8 are loose in the box but 64 are in individual packets).On face - Ballarat School of Mines, Ingenio Effodere Opes Stamped into back - Stokes Melbballarat school of mines, badge, stokes and sons, numismatics

The modern mine is accessed via the Swan Decline, which commences at the Kangaroo Flat site on the southern outskirts of Bendigo and progresses in a north easterly direction between the Deborah and Sheepshead anticlines, reaching a depth of almost 1000 m below the City of Bendigo. Development of this decline commenced in 1998. Swan Decline closed and history preserved In a major rehabilitation milestone at Kangaroo Flat, the Swan Decline Bendigo’s primary gateway to underground mining, was permanently closed in December 2022. Important parts of Bendigo’s gold rush history were also preserved from the onsite office buildings with 19 boxes of records, and 1350 old photos being scanned and provided to the local historical societies and the Goldfields Library Corporation. A volunteer from the Bendigo Historical Society, Kay MacGregor, also scanned approximately 40 bookshelves of newspaper clippings to assist with recording and preserving geological drilling locations.Black and white photocopies of photographs of Swan Decline, showing some stages of underground construction. Eleven images on 3 pages, dated 16/4/2000 (10 a.m.) show decline walls, rock bolts and markout of tunnel shape. One image shows a utility in the tunnel. Final three images on one page, have notations on the photos: 'opposite SP18 LHS decline', 'just up from previous 3 box positions' and 'just up from tank, same side' On bottom RH side 'spots for scale attention, IT required, all lower decline.' All three images dated 12/6/2000.goldmining, kangaroo flat gold mine, western mining corporation, unity mining, swan decline

Hand written letter from Department of Mines to Mr. Keith Rash. Department of Mines Victoria logo.Handwritten on letterhead "Mr Keith Rash 519 Humffray St Ballarat Dear Keith, We are currently preparing an obituary for Mr Baragwanath for our mining & Geological journal. We have found out that he attended Victoria College and the Ballarat School of Mines. Do you know whether Victoria College was the forerunner of the present Ballarat College or not? Any other personal recollections you may have of Mr Baragwanath would also e useful. Yours faithfully John L Kinglet."department of mines, keith edwin rash, rash, keith rash, kinglet, baragwanath, william baragwanath