Handwritten letter on Amalgamated Mining Managers' Association of Australasia letterhead inviting students of the Ballarat School of Mines to attend the lecture on 'A Chapter in West Australian Geology' delivered by F.G. Johnson, F.G.S. at the Ballarat Mining Exchange. The artwork on this letterhead may have been executed by Henry James Hall.amalgamated mining managers' association of australasia, letterhead, j. sharpe, ballarat mining exchange, f.d. johnson, west australian geology, henry hall

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 book was used by Charles Bacon who studied at the University of Nevada in the late 1930s/early 1940s. Bacon worked at Bunker Hill Mines and Kellogg Idaho, before arriving in Australian in 1951. He worked for CN Myers, a company involved with paper converting. CN Myers was a family business (on Charles Bacon's maternal line). The Mackay School of Mines, Nevada was established in 1908. At the time of writing this mook T.J. Hoover was Professor of Mining and Metallurgy and Dean of the School of Engineering at Stanford University. Theodore Jesse Hoover, brother of the 31st President of the United States, was born in West Branch, Iowa, on January 28, 1871. He attended Stanford and received the Bachelor of Arts degree in Geology and Mining in 1901. Following graduation his professional career started with the position of assayer for the Keystone Consolidated Mining Company. After one year, he became assistant manager for the Standard Consolidated Mine, and a year later he was promoted to manager of the operation. In 1907 Hoover went to London as general manager of Minerals Separation, Ltd. This company was developing the froth flotation process for recovering minerals from ores. Hoover took an active part in the development of the flotation concentration process and authored one of the first books on the concentration of ores by flotation. After four years with Minerals Separation, Ltd., Hoover entered private practice as a consulting mining and metallurgical engineer with offices in London and in San Francisco. He was very successful and held positions of consulting engineer, managing director, director, and president of many mining companies in America, Europe, Asia, Africa, and Australia. He returned to Stanford in 1919 as Professor of Mining and Metallurgy and Executive Head of the Department of Mining and Metallurgy. His experience and ability in organization made him a natural leader. He was influential in the formation of the School of Engineering at Stanford. The School was formed in 1925 and he was made dean, a position he held until his retirement in 1936. As dean of engineering, he promoted a broad fundamental training program for undergraduate engineering students. Under his guidance, emphasis was placed upon graduate work and he was responsible for developing strong graduate engineering curricula at Stanford. While dean he continued teaching and his course, "The Economics of Mining," developed into a book which was published in 1933. He became interested in the functions of engineers and, with Professor Fish, wrote a book entitled "The Engineering Profession" which was published in 1940 and revised in 1950. In addition to his academic activities he was generous in his hospitality. Faculty and students alike enjoyed the annual field day and barbecue at his Rancho del Oso, near Santa Cruz. He was widely read and had a lively interest in all the things he encountered. He speculated on the antiquity of man and man's early production processes. To verify an idea regarding flint tools, he studied their shapes and became proficient in making arrow heads. He was also interested in wild life, and was one of the founding members of the Cooper Ornithological Society. (http://engineering.stanford.edu/about/bio-hoover) Blue hard covered book of 547 pages including an index. Contents include mine valuation (sampling, ore deposits, ore reserves, financial provisions, sale of mineral product, metal prices, reports) and Mining Organization (Co-operative effort, Mining Companies, Promoting Mining Enterprises, fluctuations of share prices, valuation of mining shares, fakes and fallacies, the mining Engineer and the law) and Mine Management (Organization of staff, mine manager, efficiency, industrial relations, training and discipline, safety). Inside front cover 'Charles Bacon Mackay School of Mines"charles bacon, mining engineering, metallurgy, university of nevada, mackay school of mines, stanford, bacon, mining, economics, divining, theodore hoover

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

William Baragwanath was educated at the Ballarat School of Mines, obtaining a Geology Certificate in 1911. After further study he went on the become Secretary for Mines, and Chief Mining Surveyor. Baragwanath was a Councillor of the Ballarat School of Mine from 1916 to 1950.Pink covered foolscap book of 257 pages and 32 maps and plans by William Baragwanath. Contents include topography, physiography, historical, geology, basalt, faults, dykes, minerals leads, alluvial mines, nuggets, structure of Ballarat West goldfields, structure of Ballarat East gold-field, quartz formation, indicators, defunct mines, existing mines, table of deepest shafts. Images include: section of the Ballarat Gold-Field, Dead HOrse Flat, lakes formed by Basalt Flows, Gong Gong Creek, Frenchman's Lead, Ballarat West Mines, LEases and positions of shafts (1857), puddling, White Horse Lead, Woah Hawp Canton, Ballarat Township mines, Sebastopol, syncline, Victoria United Line, First Chance Mine, Llanberris No 1 Mine, Saddle Reef, New Normanby Mine, Woah Hawp Canton Mine, South Star Mine, Sebastopol Plateau, south Woah Hawp Mine, Woah No. 2 Minegeology, geological survey no 14, ballarat, baragwanath, william baragwanath

The Ballarat School of Mines was the first school of technical education in Australasia.Large format brown scrapbooks with newsclips relating to the Ballarat School of Mines.ballarat school of mines, newsclips, art examinations, ballarat west art school, st john ambulance association, andrew anderson, university affiliations, university of melbourne, professor kernot, geological cause and effect of faults, cassilis chlorination works, electric rock drills, museum, ballarat school of mines museum, latham watson, william barnard, krause, blucher amalgamator, f.m. krause, photography, ludovico hart, pyrites works, ballarat school of mines puries works, pyrities roaster, ballarat east school of art, art gallery association technical art school, hannay electro-cyanide process, x-ray, roetgen x-rays, xray, bairnesdale school of mines, technical education in germany, ballarat amateur photographic club, moonta, moonta excursion, moonta visit, broken hill visit, broken hill excursion, wallaroo excursion, ballarat west election, ballarat mechanics' institute, dr kenworthy, james oddie, william b. withers, william collard smith, duncan gillies, john phillips, james long, ballarat industrial institute

Blue soft covered report with 40 plates and plans. Inciudes Geology of Ballarat. Little Bendigo Goldfield, Ballarat West Goldfield, Ballarat East Goldfield, history, nuggets, indicators, faults, microscopic structure of Ballarat Rocks and ores, general type of the Ballarat East Mines and the genesis of their ores. Mines include New Zealand Trust, Llanberris No. 1, Llanberris No 2, Victoria United, Britannia United, New Britannia, Last Chance, Exchange, Normanby North, New Normanby, North Woah Hawp. Photpgraphic plates include: Victoria United Mine, Llanberres No. 1, Normanby North, North Woah Hawp Mine, View looking south from the Britannia Mullock Heap, View from Sovereign Hill, The place in Learmonth Street Golden Point where gold was first discovered at Ballarat. j.w. gregory, ballarat east, ballarat east goldfield, e.j. dunn, geolological survey of victoria, new zealand trust, llanberris no. 1, llanberris no 2, victoria united, britannia united, new britannia, last chance, exchange, normanby north, new normanby, north woah hawp, mining, indicators, gold mining, poppet head

Copy of a geological map of Glenalbyn. Some areas have been colours green. Creeks have been coloured blue, roads and reefs have been coloured orange.glenalbyn, county of gladstone, tarnagulla, inglewood, kingower, kurting, old inglewood deep lead, salisbury west