Professor Ferdinand M. Krause lectured in Geology at the Ballarat School of Mines. His subscription to the Geological Society of London was paid by the School.Geology, geological, FM Krause, Ferdinand Krause, Ballarat School of Mines, FE Brown, Thomas WiltshirePrinted and handwritten receipt on blue paper from the Geological Society of London and made out to F.M. Krause of the Ballarat School of Mines. The receipt was signed by treasurer Thomas Wiltshire and clerk F.E. Brown.

The Ballarat School of Mines was established in 1870. The first enrolments took place in 1871 making this group of documents historically important.Paper documents relating to the advice being sought by the Sandhurst Mechanics' Institute from Ballarat School of Mines in relation to starting a School of Mines at Bendigo. .8) Correspondence to the Ballarat School of Mines from Joseph Phillips of the Sandhurst Mechanics' Institute and Free Library. The letter seeks advice on setting up a School of Mines in Bendigo. The correspondence was dated 01 January 1871, was signed by Joseph Phillips, and was answered on 04 January 1871. .14) Ballarat School of Mines Council Agenda, 20 January 1871. Signed by James Baker, secretary. .18) Letter from R.M. Serjeant to the Ballarat School of Mines dated 09 January 1871. .22) Letter from prospective student A. Ansaldi regarding starting at the Ballarat School of Mines. .24) Letter from prospective student James Hore regarding starting at the Ballarat School of Mines. .26) Memorandum during the Mechanics' Institute Sandhurst requesting information concerning teachers. Dated 25 April 1871. .27) Sandhurst Mechanics' Institute & Free Library requesting information from the Ballarat School of Mines in relation to numbers of pupils, number of paid staff, number of honorary staff, salary of head master and whether the school was a success. It is dated 19 April 1871 and is signed by Joseph Phillips. .35) My dear sir If it will suit youor convenience I take the liberty of appointing Friday the 2nd of June for my lecture on Geology at the School of Mines. You expressed a wish to assist me in any diagrams that it might be possible to obtain. In am very anxious to have a large map of the solar system. One that might be clearly seen from any part of the Hall. It will be of great importance to my lecture. [ ? ] diagrams I will find it necessary to prepare myself. I am most faithfully H. B. de la Poer Wall R.W. Newman Esqr Vice President PS as the whole of my lecture depends on the hearing the early part it might be well to put in the Advt at 8.00 punctually. In announcing my name it might be well to put ex-Fellow of the Royal Geological Society. Asking your pardon for these suggestions. Sebastopol June 14th 1871 Gentlemen, I am desirous of joining the classes of Surveying, drawing, &c in your valuable Institution.i am 16 years of age, and been through the 1st first book of Euclid, Decimals &c. Trusting to meet with your approbation. I am gentlemen, Yours obedietly A. Ansaldi To the Administrative Council School of Mines Ballarat Darling Streetl Ballarat July 1871 To the secretary of the School of Mines Ballarat. Sir, I called on Monday but you were not present but I saw Mr Phillips and he informed me that I might commence at once, and that my nomination &c might be going on in the mean time. If there be any objection to my joining the classroom Monday night, will you be good enough to let me know. Yours &c John Hore. Sandhurst April 25 1871 To The secretary School of Mines, Ballarat, Please let me know what subjects your paid instructor teachersl JP By Jas Philipsballarat school of mines, bendigo school of mines, sandhurst school of mines, sandhurst mechanics' institute, bendigo, sandhurst, joseph phillips, phillips, hore, john hore, james phillips, ansaldi, ballarat school of mines establishment, robert borugh smyth, robert m. sergeant, james baker, de la poer wall, warrington rogers, h.b. de la poer wall, r.w. newman, lecture, royal geological society, a. ansaldi, mechanics' institute sandhurst, r.m. sergeant

Map, Longitudinal section through the Saddle Reefs along portion of Hustler's Line of Reefs, Bendigo. Plate No. XXX1V(34). Underground Survey Office,Bendigo, September 1913. Geological Society of Victoria.//Signed H.A.Whitelaw. Drawing shows the vertical shaft descending to over 3454 ftUnderground Survey Office, Bendigomap, bendigo, hustler's line of reefs

Henry Louis, M.A. was an Associate of the Royal School of miens, Fellow of the Geological Society; Fellow of the Institute of Chemistry of Great Britain; Member of the Institution of Mining Engineers; Member of the American Institute of Mining Engineers and Professor of Mining in the Durham College of Science. Green hardcovered book of 599 pages including index and illustrations. Contents include: Mode of occurance of gold; physical and chemical properties of gold; physical and chemical properties of mercury; Primitive Methods or ore-breaking; The stamp; Hoisting gear; Water Supply; Ore-Feeders; Crushing Machinery; amalgamation; concentration; Spitzkasten; Amalgam; Milling; Cam Curve; sampling and assaying; horse-power developed by fall of water; value of gold according to its fineness; conversionInside front cover in pencil "Rhys Brook"

The author, Bennett H. Brough was an associate of theRoyal School of Mines, a member of the COuncil of the Institution of Mining Engineers, a fellow of the geological society and of the Institute of Chemistry, a member of the Mining Institute of Cornwall, and a former instructor of mine-surveying at the Royal School of MinesRed had covered book 372 pages - part of Griffin's Mining Series. Contents include general explanatinos of surveying, an historical sketch, mineral deposits, mining terms, measures of length, measurement distances, the chain, rods, steel bands, measuring wheel, Miner's Dial, Magnetic needle, Fixed needle, German Dial, theodolite, traversing underground. Surface-surveys. plotting the survey, calculation of area, leveling, Telescope, Setting out, Mine-Surveying Problems, Mine Plans, Photographic Surveying, examination Surveying. Illustrations include: Whitelaw's Dial (Fig 22), Theodolite of the American Type with Hoffman tripod head, (fig 37a)mining, surveying, miner's dial, chain, survey, theodolite, scientific instruments

This book contains the report from the select committee on Castlemaine and Sandhurst water supply; with the proceedings of the committee, minutes of evidence and appendices. It also contains the report Of the Engineer-In-Chief of Railways, and reply of the Chief Engineer of Water Supply on the works constructed by the Victorian Water Supply Department, presented to both houses of parliament by His Excellency’s command. Ferdinand M. Krause, was a lecturer at the Ballarat School of Mines in Geology Mineralogy Mining Engineering and Surveying. He was a Fellow of the Geological Society and a Fellow of the Linnian Society. He was assistant engineer for the Ballaarat and Ballarat East Water Supply Committee and helped plan local reservoirs.A brown cloth hard cover, foolscap book with leather spine. Title is written in black on the title page. "Water Supply Reports" is engraved in gold on spine. It includes a table showing the monthly and yearly rainfall and shade temperature at Ballarat, 2nd February, 1885. It also includes two reports and two replies, a map No.7082.2 of Victorian Water Supply, Castlemaine and Sandhurst district general plan including lines of Aqueduct, Reservoirs. No. 7082.3 of Victorian Mining districts, Mining Divisions and The Gold Fields in 1866 - includes districts to be supplied under the Waterworks Act, 1965. It also includes: *Report of the Engineer-in-chief of Railways and Reply of the Chief Engineer of Water Supply on the works constructed by the Victorian Water Supply Department, 1869. * Coliban Water Scheme, 1864 * Ballarat and Ballarat East Water Supply (1869) including the Ballarat Water Supply List containing names of occupiers and nature of improvements on lands comprised within the proposed reserve of Gong Gong Reservoir, Ballaarat. At Warrenheip the names included: Honora McCallin, William Honan, C. McMahon, Patrick McMahon, J.P. Beach, J.H. Smith, Michael Nestor, Martin Quinn, Martin McIntyre, Robert Higgins, Coleman Kane, Robert Bond. At Ballarat: William Clarke, Richard White, John Hosking, Wesleyan Chapel, J. Hewitt, Robert McRobinson. At Bungaree: John Pullin, John Llewellyn. William Daw, Smith and Wynne, William Brough, A. Alexander. * Ballarat and Ballaarat East Water Supply report upon the advisability, or otherwise, of constructing a reservoir at the junction of the Yarrowee Creek and Gile's Creek, upon a site known as Gile's Reservoir (printed by Frank Pinkerton). This report has numerous notes written on it (most probably by Krause) and includes the capacity of Harry Beale's Reservoir, Pimcott's Reservoir and the Proposed Gong Gong Reservoir. * Statement as to the position of the Ballaarat and Ballaarat East Borough Councils in Connection with Water Supply, September 1869. * Ballarat and Ballaarat East Water Supply - General Statement upon the Ballaarat and Ballaarat east Scheme of Water Supply. Includes information on Moorabool reservoir, Harry Beale's Reservoir, Lal Lal Creek, Two Mile Creek, Beale's Dam, Yarrowee Creek, Gong Gong Reservoir, Kirk's Dam, Devil's Creek, Moorabool Creek. Additional handwritten notes (probably by Krause) * Engineer's Report on the resolution of the COmmittee of Water Supply, of the 7th July 1868. The report refers to the Country around Mount Warrenheip. Names mentioned are L. Abraham, Great North-West Gold Mining Company, Border Sawmills, Ferdinand Krause, Ohlfsen Bagge, W.H. Shaw, A signature by "Ferdinand M. Krause" at the top corner of the title page. A few pages have handwriting on the margins, it is believed to be his handwriting. water supply victoria, castlemaine directories, sandhurst directories, ballarat directories, james blackburn, edward wardle, daylesford water race, c j taylor, george avery fletcher, bagge, ohlfsen bagge, george foote, john h reilly, ambrose johnson, george francis, timber preservation, james forbes, alfred surplice, malcolm carmichael, robert adams, frederick hugh thomas, h o christerpherson, william downe, thomas lawrence brown, francis hadgson nixon, strangways, guildford, maldon, muckleford, lauriston, malmesbury, franklinford, walmer, strathloddon, downe, ferdinand krause, m7082, trentham, castlemaine, drummond, metcalfe, sutton grange, lockwood, ravenswood, mandurang, yandoit, c.h. ohlfsen bagge, moorabool reservoir, gong gong reservoir, harry beale's reservoir, pincott reservoir, frank pinkerton, water

This booklet contains an article on the plant fossil deposits in Eastern Victoria. It has been written by Dr John Douglas in 1963. He published extensively on a range of geological and natural history themes. His major works included co-editing the Geological Society of Victoria’s Geology of Victoria and his PH.D. thesis for the University of Melbourne contained in two Geological Survey Memoirs on the Mesozoic floras of Victoria. He was also responsible for the Geology and Sport and Recreation chapters in the State Government’s Atlas of Victoria and wrote the booklet, What Fossil Plant is That? He was a Supervising Geologist with the Department of Minerals and Energy in Victoria for many years and lectured extensively at Botany and Geology conferences in Australia and overseas. This book is of some interest as it was written by a former resident of Warrnambool, Dr John Douglas (1997 to his death in 2007). He was an active member of the Warrnambool Field Naturalists’ Group and edited for this group the book, The Nature of Warrnambool. This is a small booklet of 16 pages reprinted from the Proceedings of the Royal Society of Victoria, Vol. 77, Part 1. It has a grey cover with the logo of the Royal Society of Victoria on the front cover. It has printed material on plant fossil deposits in eastern Victoria and several sketches and black and white plates of plant fossil photographs and cross-sections. The pages were stapled but the staples have been removed. There is some rust where the staples were removed. Front cover: ‘Royal Society of Victoria, New Bennettitalean Leaves from the Mesozoic of Eastern Australia by J. G. Douglas, reprinted from Proc. Roy. Soc. Victoria, Vol 77, Part 1, Issued separately, 13 December, 1963.’ micro- paleontology in eastern victoria, dr john douglas, warrnambool

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

Coorongite is a dark, rubber-like, highly resilient structureless algal deposit. In the Coorong district of South Australia it occurs in moderate quantities associated with the coastal swamps and sand dunes which extend for a considerable distance east of the mouth of the Murray. This particular specimen was recovered from the south of the Coorong River, South Australia. A type of sediment rich in organic matter, Coorongite is the unlithified end-member of the sapropelic coal series. The members of the sapropelic coal series can be ranked in order as sapropel (the unlithified form), sapropelic-lignite, and sapropelic-coal (the lithified forms) based on increasing carbon content and decreasing volatile content. Sapropel (Coorongite) is an unlithified dark, pulpy, fine organic mud containing concentrations of algae and miospores that are more or less identifiable. Coorongite is typically found as an algae like substance, that can be found in irregular size pieces. Coorongite was believed to be dried up oil due to its rubber-like texture. The Coorongite is also soft to the point where it can be cut into with a knife or it can be broken and torn by hand. Otherwise known as 'Kurangk', the Coorong River is home to the Ngarrindjeri people, which acts as both a place for gathering food and a spiritual place. In 1852 the first sight of Coorongite was found along the Coorong River. The finders mistook the Coorongite for dried up oil, which lead to the belief that there were oil reserves under the Coorong River. Between the 1860s and the 1930s the Coorong River became a place where mining oil and Coorongite became precedent. Nowadays, the local council and the South Australian Government are working together with the Ngarrindjeri people to sustain and preserve the Coorong River and the culture that is with it. Soon after gold was discovered in 1851, Victoria’s Governor La Trobe wrote to the Colonial Office in London, urging ‘the propriety of selecting and appointing as Mineral Surveyor for this Colony a gentleman possessed of the requisite qualifications and acquaintance with geological science and phenomena’. Alfred Selwyn was appointed geological surveyor in Australia in 1852 which began the Geological Survey of Victoria. Selwyn went on to collect geological samples and catalogue thousands of specimens around Australia. In 1853-69 the Geological Survey issued under Selwyn's direction sixty-one geological maps and numerous reports; they were of such high standard that a writer in the Quarterly Journal of the Geological Society of London bracketed the survey with that of the United States of America as the best in the world. During his years spent in Australia, Selwyn collected numerous significant geological specimens, examples of which are held in collections such as the Burke Museum.Coorongite is considered to be a mineral with a unique texture, where it can be both hard and soft. Coorongite can also be considered to be a rare mineral, as it is only located along the Coorong River and due to the mining of it, has left very few sources. It was believed at one point that Coorongite could be used to replace oil. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.Three solid varyingly hand-sized pieces of wooden appearing organic matter derived from the river in the Coorong District in South Australia. A rubber-like, highly resilient structureless algal deposit.Specimen 245 page 69 / in Descriptive Register / "Elcestic Bitumen, / Coorangite" South of / Coorung River, South Australia . / C. WIllman / 15/4/21burke museum, beechwoth, indigo shire, beechworth museum, geological, geological specimen, mineraology, coorong, coorong river, kurangk, ngarrindjeri, south australia, coorongite, coorongite specimen

This ice cream freezer, manufactured in South Australia in the 1930's, was advertised to "keep the contents of the cream compartment frozen for many hours". It was promoted for use at picnics to keep salads cool. Its design is very similar to other freezers of The Frigid name which were made in 1939; those freezers were all one colour whereas this one is blue around the top and bottom of the barrel and cream in the centre with blue/green lettering. The process of making ice cream was to pack the outer chamber full with a combination of 3 parts ice cubes of about 1 inch (2.cm) to one part coarse salt, then pour into the chamber about 1 cup of cold water. After this, the ingredients for ice cream or sorbet were poured into the inner chamber, then attach the lid and turn The Frigid freezer upside down for about 40 minutes or until the right consistency is reached. Advice as given to open the freezer every 20 minutes and stir around the contents that were frozen against the sides of the inner chamber. The ingredients for the ice cream could include cream, sugar, vanilla and eggs. The label on the box of The Frigid shows the address of A Simpson and Son to be at Pirie Street, Adelaide. This address was used as early as 1876 and later catalogues, 1931 - 1960 still show this address. Alfred Simpson and his family emigrated from England, arriving in South Australia in 1849. He had already completed his apprenticeship as a tinplate worker but he tried various other occupations, including trying out the gold mines in Victoria, before he established himself as a tinsmith in 1853. His products included many agricultural items. His son, Alfred Muller Simpson, joined the business when he turned 21. In the 1860 Simpson's products included 'explosion proof' safes. In the late 1880's A Simpson and Son manufactured munitions and mines for the war. At the time of Alfred's death in 1891, A Simpson and Son had the largest metal manufacturing plant in Australia. From 1898 the company's reputation grew from the process of enamel plating with porcelain. During the First World War, Simpsons returned to the manufacture of munitions. Alfred M. Simpson's sons (Alfred Allen, known as Allen, and Fredrick Neighbour) joined the company when they finished their schooling. Allen was also associated with the Royal Geological Society over many years and when the CT Madigan surveyed Central Australia in 1929, the Simpson Desert was named in his honour. Cape Simpson in Antarctica is also named after him due to his assistance to Douglas Mawson. A new factory was opened at Dudley Park in the 1940s and the company began the manufacture of whitegoods. In 1963 A. Simpson and Son merged with Pope Industries to form Simpson Pope Holdings. Alfred Simpson became chairman of the board of Simpson Pope Holdings. The Simpson brand, now owned by Electrolux, continues to produce a variety of household appliances. (Reference: State Library of South Australia) A Simpson and Son was an early colonial business that has lasted well into the 20th century and the name Simpson is still associated with whitegoods. Freezer, 2 quart (1.8 litre) capacity, made by A Simpson and Son Ltd, marked "The Frigid". Cylinder shaped, constructed from enamelled sheet metal, has two catches one on the base and one on top. Inner cylinder for holding contents for freezing. Slightly rusted. Freezer is inside original cardboard box with yellow label showing manufacturer details. Circa 1930'sOutside of freezer is printed in blue"The Frigid". Box includes "THE "FRIGID" FREEZER" and branded "S & S" inside a circle.flagstaff hill, warrnambool, shipwrecked-coast, flagstaff-hill, flagstaff-hill-maritime-museum, maritime-museum, shipwreck-coast, flagstaff-hill-maritime-village, a. simpson & son limited, manufacturer, foundry, freezer, 2 quart freezer, portable freezer, kitchen appliance, the frigid, ice cream freezer, ice cream maker 1930's

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

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

In the early 1900s black marble was being mined in the Bruthen district. Some was used for the Shrine of Remembrance in Melbourne and Australia House in London. 900 tonnes were shipped to London to be included in the construction of Australia House.Marble quarrying has been a significant part of the history of Buchan in East Gippsland. Its inclusion in the Shrine of Remembrance War Memorial and Australia House in London is noteworthy.A large black / white photograph of men working in a marble quarry.buchan-marble geology shrine-of-remembrance australia-house-london

Inspected by George Rawlings on 6.12.2013. This fossil was probably found at the Newmerella cutting.Fossils are among the most valuable sources of information about the Earth's history. This fossil is part of the geological history of the Orbost area.A gastropod fossil from the Miocene Era.fossils gastropods shells

Found at Newmerella. Inspected by George Rawlings 6.2.2013Fossils are among the most valuable sources of information about the Earth's history. This fossil is part of the geological history of the Orbost district.A gastropod fossil from the Miocene Era.gastropod fossil miocene

Presumed found in the Buchan area. Inspected by George Rawlings 6.2.2013Fossils are among the most valuable sources of information about the Earth's history. This fossil is part of the geological history of East GippslandTtwo pieces of jasper fossil. Genus-nautiloidea, family-cephalopoda, order - mollusca. Fossil of a cuttlefish like animal- head and tentacles protruding from one end of the long tubular shell. This is in red jasper. The small fossil piece has been polished.jasper fossil nautilloidea mollusc

Found at Hofen's Bluff at Bete Bolong in 1936 by Barry McLeod. Inspected by George Rawlings 6.2.2013.This fossil is an example of the geological history of the Orbost area.A rock with a piece of shark tooth embedded in it. It was found at Hofen's Bluff at Bete Bolong. It belongs to the Oligocene Miocene Age (20 million years ago). The tooth is from the upper jaw probably near the front from a white pointer shark about 6o metres long. Carcharodon Megalodon.fossil shark-tooth hofen's-bluff white-pointer .

This fossil was found by Peter Cook just west of East Cape at Cape Conran (east of Orbost),. Original correspondence re its identification came from Andy Murray - Conservation & Natural Resources, Orbost. It was on display at the Orbost Visitor Information Centre - the Slab Hut.A fossil tooth from a marine species. It may be from a an extinct ziphiid or beaked whale (Warneke Marine Mammal Services 20.10.1993). It may be a fossil from a large species of subadult seal (Ewan Fordyce Senior Lecturer in Geology, University of Otago 11.10.1993).fossil-tooth whale seal marine cape-conran

Shells were collected by Edgar lavell and son, alan.The fossils paint a vivid picture of life below a sea that once covered parts of East Gippsland. They reflect the geological history of the area.Square shaped wooden display case with glass front. Holds a collection of fossil shells on cork. Shells are from the Middle Miocene Age.shells natural-history middle-miocene fossils

These birds’ eggs were collected by Charles Brittlebank before 1910 but at this stage it is not known from which area they came. English-born Charles Brittlebank was a naturalist interested in ornithology, geology and mycology. He was the Government Plant Pathologist for Victoria from 1913 to 1924. He was the first to discover evidence of glaciation in the Werribee Gorge and published many papers on this subject and other aspects of natural history. It is not known when Charles Brittlebank was in the Warrnambool area or the origin of the birds’ eggs but it a very interesting (and perhaps rare) historical collection. .1 Birds’ Eggs - There are 27 eggs, either whole or partial specimens, contained in a box with home–made cardboard partitions. Ten are intact and the rest are broken. Eight are white and the remainder are speckled. The eggs are resting on a turquoise-coloured piece of material .2 Nest – This is woven from hair and fine twigs and is filled with white wool-like fragments .3 Letter – These are two sheets of writing paper with handwritten information in blue ink. .4 Envelope - This is a small envelope which contained the sheets of paper (.3 above) and the front has handwritten material in blue ink..3 ‘To whom it may concern – I hereby declare that these eggs were collected before 1910, and were part of a collection of the late Charles Brittlebank which is now in the Melbourne Museum. Fred. A. Shirrefs.’ .4 ‘To whom it may concern’ charles brittlebank, history of warrnambool

Studies of geology, plant and bird life and water cycle in the early 1960's.Value for study and comparing to current plant and bird life and the water cycle. Geology gives reason for the construction of the Kiewa Hydro Electric Scheme - the use of materials and the locations.Black foolscap 'bend back' folder which holds papers on: Geology, Flora, Orchids, Birds and three booklets: 1. Royal Soc. of Vic. by E.C.Beavis Sept. 1961 - Geology 2. Royal Soc. of Vic. by E.C.Beavis July 1960 Mylonites 3. The Water Cycle in Action / Bogong High Plains by Phyllis Reichl kiewa valley; geology; plant life; bird life; water cycle; kiewa hydro electric scheme