Six grey soft covered Coventry Engineering Society Journals. .1) Vol. 6 No. 3, March 1925. Includes * The Influences of Rates of Colling upon Cast Iron by H. Beeny * Pulverised Coal by J. Pickin (Junior) .2) Vol. 7. No. 1, January 1926. Includes * Coventry Engineering Society Annual Report * Road Springs by C.E. Cary .3) Vol. 7. No. 2, February 1926. Includes * Some methods of Testing Engines by G.H. Walker Vol. 7. No. 3, March 1926. Includes * Notes on the Disposal of a Town's Refuse by H.L. Bunting * How roadcasting is Done by J.A. Cooper Vol. 7. No. 4, April, 1926. Includes * The Applicaton of Thermionic Repeaters to Long Distance Telephony by H.C. Hannam-Clark Vol. 7. No. 5, May 1926. Includes * Automobile Design by W. Ferrier Brown * Floodlighting and its Possibilities by H.C. Wheat Vol. 7. No. 6, June 1926. Includes * Machines for Testing Materials by H.N. Cox * Characteristics and uses of Ground Gears by H.F.L. Orcutt * Instruments for Recording Minute Oscillations * Characteristics of Iron Ores by A.J. Aierscoventry, engineering, coventry engineering society, peterborough cathedral, cast iron, h. beeny, pulverised coal, j. pickin (junior), road springs, c.e. cary, testing engines, g.h. walker, disposal of a town's refuse, h.l. bunting, roadcasting, j.a. cooper, thermionic repeaters, long distance telephony, h.c. hannam-clark, automobile design, w. ferrier brown, floodlighting, h.c. wheat, machines for testing materials, h.n. cox, ground gears, h.f.l. orcutt, instruments for recording minute oscillations, iron ores, a.j. aiers

Brown hard covered book. Chapter 16 is on gold deposits and discusses the discovery of gold in California and Australia.Brown hard covered book geology, water, rivers, the atlantic, great deep, africa, australian interior, eyre's expedition, murray river, darling river, earthqaukes, leichardt, moreton bay, volcanos, darwin's theory, evolution, egyptian race, human remains in caverns and gravel, rocks, metamorphism, iron ores, coal, coal fields, gold deposits, california, water-glass, artificial stone, porous stones, cements

This plan was printed in the Ballarat School of Mines Annual Report were Ferdinand Krause was a professor.Printed plan showing iron ore deposits at Lal Lal.lal lal ore, moorabool river, ferdinand krause

The School of Mines Annual Report, 9 February, 1881, Additional Examination Statute 1880, Balance Sheet, Certificates Granted by Council, Donations and Fees - carriage of, Extracts from Visitors' Book, Fees, Form of Bequest, Honorary Correspondents, Life Governors, Mining and Mineral Contributions Invited - Paper of Particulars, Museum - open to visitors, Office Bearers, Obituary, Report of the Lecturer in Mathematics, Report of the Lecturer in Mining-Land- and Engineering-Surveying, Report of the Lecturer in Mechanical Engineering, Report of the Lecturer in Telegraphy, Report of the Curator of the Museum (with Plans), Report of the Superintendent of Laboratories, Subjects and Lecturers, Subjects and Examiners, Statement of Receipts and Expenditure for the year 1880, Subscriptions and Donations from 1 January to 31 December 1880, The Lal-Lal Iron Ore Deposits - (with Section and Plan)Pale green booklet of 70 pages, Annual Report 1880. Image of Guage Test Tower, Image of The School of Mines, Plan of Ground and Buildings - Albert Street, The School of Mines Ballaarat - The Museum - Plan of Groundfloor, Image of the Lal-Lal Iron Ore Deposits, Moorabool Riverthe school of mines, annual report, additional examination statute 1880, balance sheet, certificates granted by council, donations and fees - carriage of, extracts from visitors' book, fees, form of bequest, honorary correspondents, life governors, mining and mineral contributions invited-paper of particulars, museum open to visitors, office bearers, obituary, report of the lecturer in mathematics, report of the lecturer in mining-land and engineering-surveying, report of the lecturer in mechanical engineering, report of the lecturer in telegraphy, report of the curator of the museum (with plans), report of the superintendent of laboratories, subjects and lecturers, subjects and examiners, statement of receipts and expenditure for the year 1880, subscriptions and donations from 1 january to 31 december 1880, the lal-lal iron ore deposits-(with section and plan), obituary - sir redmond barry - arthur leahy - jacob upfold - john day, mr james oddie, dr. r. f. hudson, john victor, chas. wm. thomas, w. h. shaw, walter d. campbell, ferdinand m. krause, joseph flude, geo. perry, w. hy. barnard, examination statute, his excellency sir wm. f. drummond jervois, charles h. pearson, t. brodribb, professor pepper, james mitchell, robert adam, wm. lant carperter, h. b. de la poer wall, w. h. brokenshire, arthur parker, henry parkinson, c. davies, simon richards, c. v. gorton, c. r. blackett, david jones, wilberforce dyke, ferdinand krause, ballarat school of mines museum, ballarat school of mines museum plan, lal lal ore deposits, moorabool river, william land carpenter, william jervois, william henry tbarnard

Cast iron lace was made in foundries in most cities. There were 42 such foundries in Melbourne alone. It was cheaper to make than wrought iron. "Pig iron", iron ore, was melted in a blast furnace, mixed with alloys and poured into molds made of sand. The alloys needed a minimum of 2% carbon.Black and White Photo by A Doney Bendigo of balustrade in Forest Street next to Wesley ChurchA. Doney Bendigoa doney, forest street

Cast Iron lace was made in foundries in most cities. There were 42 such foundries in Melbourne alone. It was cheaper to make than wrought iron. "Pig iron", iron ore was melted in a blast furnace, mixed with alloys and then poured into molds usually made of sand. The alloys needed a minimum of 2% carbon.A black and white photograph by Alan Doney of the building at 247 View St in Bendigo. The photo shows detail of the wrought iron on the verandah. alan doney, bendigo, wrought iron

Cast Iron lace was made in foundries in most cities. There were 42 such foundries in Melbourne alone. It was cheaper to make than wrought iron. "Pig iron", iron ore, was melted in a blast furnace, mixed with alloys and then poured into moulds usually made of sand. The alloys needed a minimum of 2% carbon.A black and white photograph by Alan Doney of the building at 257 View St in Bendigo. The photo shows detail of the wrought iron on the verandah. alan doney, bendigo, wrought iron

Cast Iron lace was made in foundries in most cities. There were 42 such foundries in Melbourne alone. It was cheaper to make than wrought iron. "Pig iron", iron ore, was melted in a blast furnace, mixed with alloys and then poured into molds usually made of sand. The alloys needed a minimum of 2% carbon.A black and white photograph by Alan Doney of the building at 22 Valentine St in Bendigo. The photo shows detail of the wrought iron on the verandah. alan doney, bendigo, wrought iron

Cast iron lace was made in foundries in most cities. There were 42 such foundries in Melbourne alone. It was cheaper to make than wrought iron. "Pig iron",iron ore, was melted in a blast furnace, mixed with alloys and then poured into moulds usually made of sand. The alloys needed a minimum of 2% carbon. A black and white photograph by Alan Doney of 288 View St in Bendigo. The photo shows detail of the wrought iron on the fence. alan doney, bendigo, wrought iron

Cast Iron lace was made in foundries in most cities. There were 42 such foundries in Melbourne alone. It was cheaper to make than wrought iron. "Pig iron", iron ore, was melted in a blast furnace, mixed with alloys and then poured into moulds usually made of sand. The alloys needed a minimum of 2% carbon.A black and white photograph by Alan Doney of 159 Forest St in Bendigo. The photo shows detail of the wrought iron on the verandah. alan doney, bendigo, wrought iron

Cast iron lace was made in foundries in most cities. There were 42 such foundries in Melbourne alone. It was cheaper to make than wrought iron. "Pig iron", iron ore, was melted in a blast furnace, mixed with alloys and then poured into moulds usually made of sand. The alloys needed a minimum of 2% carbon.Black and White photos by A Doney of House on corner of Mc Kenzie and Short Street Bendigo showing lace ironwork on the balustrade.Photo A Doneyiron lace work, a doney, historical home bendigo

Cast iron lace was made in foundries in most cities. There were 42 such foundries in Melbourne alone. It was cheaper to make than wrought iron. "Pig iron", iron ore, was melted in a blast furnace, mixed with alloys and then poured into moulds usually made of sand. The alloys needed a minimum of 2% carbon.A black and white photograph by Alan Doney of Caretakers Residence Cathedral Short Street Bendigo showing detail of the wrought iron on the verandah. A Doney Bendigoalan doney, bendigo, wrought iron, balustrade

Cast iron lace was made in foundries in most cities. There were 42 such factories in Melbourne alone. It was cheaper to make than wrought iron. "Pig iron", iron ore was melted in a blast furnace, mixed with alloys and then poured into moulds usually made of sand. The alloys needed a minimum of 2% carbon.Black and White photos by A Doney of bench seats one showing fern detail and the other leaves and flowers.Photo A Doneyiron lace work, a doney, bench seats

CAst iron lace was made in foundries in most cities. There were 42 such foundries in Melbourne alone. It was cheaper to make than wrought iron. "Pig iron"' iron ore, was melted in a blast furnace, mixed with alloys and poured into moulds usually made with sand. The alloys needed a minimum of 2% carbon.Black and White photo by A Doney of Balustrade on property on the corner of Forest and Barnard Streets Bendigo.A Doney Bendigoalan doney, bendigo, wrought iron, forest street bendigo, barnard street bendigo

Cast Iron lace was made in foundries in most cities. There were 42 such foundries in Melbourne alone. It was cheaper to make than wrought iron. "Pig iron", iron ore was melted in a blast furnace, mixed with alloys and then poured into moulds usually made of sand. The alloys needed a minimum of 2% carbon. Two black and white photographs by Alan Doney of the Spastic Centre in Don Street, Bendigo. Both photos shows detail of the wrought iron on the verandah. alan doney, bendigo, wrought iron, spastic children's society

Cast Iron lace was made in foundries in most cities. There were 42 such foundries in Melbourne alone. It was cheaper to make than wrought iron. "Pig iron", iron ore was melted in a blast furnace, mixed with alloys and then poured into molds usually made of sand. The alloys needed a minimum of 2% carbon. Three black and white photographs by Alan Doney of the residence 'Illira' at 57 Forest St, Bendigo. The first photo shows the front of the residence. The other two photos show detail of the wrought iron on the verandah. alan doney, bendigo, wrought iron, illira bendigo

CAst iron lace was made in foundries in most cities. There were 42 such factories in Melbourne alone. It was cheaper to make than wrought iron. "Pig iron", iron ore, was melted in a blast furnace, mixed with alloys a nd then poured into moulds usually made of sand. The alloys needed a minimum of 2% carbon.A black and white photograph by Alan Doney of Early Nurses House Lucan Street (Bendigo Base Hospital). Now incorporated in portion of present Nurses home A Doney Bendigo - Copyalan doney, bendigo, wrought iron

Cast iron lace was made in foundries in most cities. There were 42 such foundries in Melbourne alone. It was cheaper to make than wrought iron. "Pig iron", iron ore, was melted in a blast furnace, mixed with alloys and poured into moulds usually med from sand. The alloys needed a minimum of 2% carbon.Black and White photo by A Doney of sandblasting iron lace work on unknown property in Bendigo. Two internal photos of door and arch ways. Larger photo of balustrade with verandah pillars in backgroundA Doney Bendigoalan doney, bendigo, wrought iron

The Ballarat School of Mines is a predecessor institution of Federation University Australia.Ballarat School of Mines Annual Report. The report includes: Ballarat Gaol Reserve and Endowment, Black Hill (F.M. Krause), Lal Lal Geology (F.M. Krause), Lal Lal Iron Ore Deposits (F.M. Krause) , Sedimentary Rocks of the Ballarat District (F.M. Krause), Skipton Lignite Deposit (F. M. Krause) The report includes the following Images: Ballarat School of Mines and Botanical Garden ballarat school of mines, ballarat court house, ballarat circuit court, skipton, coal, skipton coal, ballarat school of mines botanical gardens, ballarat gaol, w.h. shaw, ferdinand krause, black hill, lal lal, lal lal ore deposits, lal lal geology, sedimentary rocks of ballarat district, skipton lignite deposit, john ditchburn, john o'malley, john thompson mckenna, george samual gawler, henry henry keast, george james, donald mcgregor, george kidd, hachin gordon illingworth, john king, josiah curnow, john james patterson, john bailey bullen, john trevan, thomas james, patrick mcloughlin, patrick murray, john hore, henry ferdinand conrad

This particular specimen was recovered from the Lal Lal Coal and Iron Mine in Victoria, 19km from Ballarat. Brown Coal was discovered here in 1857, just alongside the Geelong to Ballarat Railway line. This discovery of lignite (brown coal) was the first in Victoria, which would bring important benefits to the region and state, both of which had previously been reliant on coal imports. In the 1860s, iron ore was found just 5km from Lal Lal, and the area was converted into an Iron Ore Mine. The Lal Lal Iron Mining Company took over operations in 1874, who then peaked iron production in 1884. This mine continued operations until June 1884, when the blast furnace was extinguished and never recommenced. The blast furnace at Lal Lal is considered one of the most important and highly significant sites ion early industrial history in Australia, as it is the only remaining best furnace from the nineteenth century in the Southern Hemisphere. The furnace ruins are 17 metres high, and are clearly visible today on Iron Mine Road, Lal Lal, near the Bungal Dam. This specimen of Lignite (brown coal) is significant, as it was mined from the area where brown coal was first discovered in Victoria, leading to an important and controversial future of the mining and use of brown coal in this State. The Victorian Heritage Database has listed the Lal Lal Coal Mine with local significance, with their Statement of Significance stating: "The Lal Lal coal mine is historically significant as the site of the first discovery of lignite (brown coal) in Victoria, and one that promised important benefits to regional and state industries that were reliant on coal imports at the time. The significance of the stie is reduced by the poor state of preservation of the coal mining and processing fabric". This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A hand-sized light-weight, soft and combustable sedimentary rock specimen, that is dark brown in colour. The specimen has jagged edges, as though parts of the rock have crumbled away. Brown coal, or Lignite, is formed naturally from compressed peat, and is typically found in natural basins. The stages to the formation of coal ('coalification') begin with plant material and wood, which will decay if it is not subjected to deep burial or heating, and turn into Peat. Peat, when sufficiently compressed naturally, will turn into Brown Coal (Lignite), and finally into Black Coal (sub-bituminous, bituminous and anthracite). Each successive stage has a higher energy content and lower water content. It is brownish-black in colour. Brown Coal has a high moisture content, between 50 and 75 percent, and a low carbon content. Some Brown Coals may be stratified, with layers of plant matter, which means little coalification has occurred beyond the peat natural processing stage. When Brown Coal is submerged in dilute nitric acid or boiling potassium hydroxide solution, it reacts to produce a reddish solution, of which higher-ranked coals do not. When brown coal is pulverised and burned in boilers, the steam is used to drive turbines, which generates electricity. It is the lowest rank of coal, as when burned, it creates a relatively low heat content, which in turn does not create a great output of steam. burke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, mineralogy, brown coal, brown coal specimen, lignite, lal lal, lal lal coal mine, lal lal iron mine, ballarat, blast furnace

Green, indexed, cloth bound note book containing fourteen pages of hand-written scientific experiments. Subjects include Iron, Standardization of KMn O4 solution, Ferrous Ammonium Sulphate, Sodium Oxalate?, Assay of Titaniferous? Iron ore, To make up Standard solution of Na2 S2 O? 5? For Copper, Standard Sol of (?H4)2 Mo O4) for Lead Assay, Sry Assay of Lead, Antimony, Resolution of ? Compounds, Clarks Modified Method Ores & Alloys, Method of reducing antimony solutions, Bromate Method, Standard Sol Pot Bromate, Standard, Assay, Oxides, Method suitable for alloys of Pb ? ?, Arsenic, Standard Iodine, Starch, Assay, Tungsten, Assay for Pyritic Scheelite, Illuminating Gas, Calcium, Permanganate method, Assay, ? O2, Iron, Ca O, Norman Solutions.sciences, instruments-general, scalebuoy, bill ashman collection, scientific formulas, assay

Although it is not known where these specimens were collected, 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. Agate occurs when amygdales (gas pockets) form in the upper levels of basaltic lava flows. If these pockets or bubbles are iniltrated by water bearing silica in solution, the fluid dries and hardens in layers, forming round or egg shaped nodules or geodes within the rocky matrix. Agate is formed of a silica mineral chalcedony similar to quartz. The term carnelian primarily refers to the reddish shading of the stone; whether the stone is termed an agate or chalcedony type is often influenced by the degree of colour banding the specimen shows. The specimens are significant as examples of surveying activity undertaken to assess and direct the development of the mineral resource industries in Victoria and Australia, as well as the movement to expand human knowledge of earth sciences such as mineralogy and geology in the nineteenth century.Three small geological specimens that appear visually consistent with images of rough or unpolished Carnelian Agate or Chalcedony. geological specimen, geology, geology collection, burke museum, beechworth, indigo shire, north-east victoria, gemstones, agate, carnelian

Basalt is a common igneous rock that composes most of the Earth's surface and can be found on the Moon and other rocky planets of the Solar System. It is generally composed minerals such as calcic plagioclase, clinopyroxene and iron ore which form grains that are indistinguishable to the naked eye. It can be dark grey or black in colouring and sometimes may contain holes left by gas bubbles. Most of the Earth's basalt was produced in environments such as oceanic divergent boundaries, oceanic hotspots, and mantle plumes and hotspots beneath continents. Basalt is commonly used in construction where it is crushed and used for multiple purposes such as concrete aggregate, road base, or railroad ballast. Thin slabs of basalt can also be cut and used for floor tiles, stone monuments, and building veneer. This particular specimen was excavated from Talbot in Victoria, which was a small gold mining town established in 1852. As basalt is a common rock, it is not specific to Talbot. However, this specimen can be assumed to be of the Cainozoic age due to previous geomorphic surveys of the area. This particular type of Basalt was used mainly for roads due to the durability of the rock.Basalt holds significance due to the continued use of the rock from historic until present times. The rock has been utilised for many types of construction and is still used for the same purposes today. Basalt also has significance to the Earth and other rocky planets of the Solar System as it makes up most of the planet's surface. 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 smaller than hand sized rock specimen which is dark grey in colour with small holes and white deposits across its surface.Geological survey / [illegible] /burke museum, beechworth, geological specimen, geology, basalt, basalt specemin, indigo shire, talbot, cainozoic, igneous rock

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

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