Mining & Geological Journal Vol.2. No.3. September 1940. Published by the Department of Mines Victoria with articles on mining, photographs, maps & advertisements. Name on front A.Richardson 29 Harrison St Bendigo. Softcover.Department of Mines Victoriamagazine, organization, mining, mining, mines, mining equipment.

Two photocopies of hand-drawn sketch of the Barfold Gorge. On the sketch is the location of a house, trees, fences, different types of rock, some accessible areas to get down to the river, geological features and water falls.place, land, barfold gorge, peter ellis collection, barfold area, mitchell's falls, queen's fall

From the Ballarat School of Mines.Argonite geology, argonite

From the Ballarat School of Mines.geology, rock

Three speimens of petrified wookpetrified wood, geology

Research undertaken in the local areaStudy done by resident of the Kiewa ValleyPapers photocopied from books pertaining to the local areageology, fossils

^ plastic cylindrical containers housing five different samples of sandsand, geology

See Geological Survey Victoria: GSV Reference ID: 43711 South Nell Gwynne 'The Central Nell Gwynne which recently took over the reef prospected by Nell Gwynne ( B.M.L.) will continue to work the mine until the new Company, South Nell Gwynne Gold Mining Company is ready to take over. The main development work is at the 1080 feet level where stoping is being carried out on a spur system which has shown several colours of gold. ...The trial crushing in shaft sinking gave 4 dwt per gold per ton..... ' ( 29th July 1938, 'The Herald, Melbourne) 1941 Geological Survey Vic: SOUTH NELL GWYNNE, BENDIGO. MINING AND GEOLOGICAL JOURNAL: ' Journal, dark green hard cover, buff bindings on spine and corners. On spine of book in gold print: ' Share Register South Nell Gwynne G.M. Co. N.L.' South Nell Gwynne Gold Mining Company share register, 1938 to 1941. Alphabetical index in front, four hundred pages. Entries detail date of purchase, name of shareholder, distinctive number range, call account and paid by. Page 299 has a list of forfeited shares in the Company with a list of shares sold by James Andrew & Co., on 8th December 1938. Shares were 'forfeited for non payment of the 2nd call of threepence per share'. Share register is part of the Margaret Roberts Collection. bendigo, goldmining, goldfield, south nell gwynne gold mining co., nell gwynne, margaret roberts collection, mr j.j. stanistreet, mine manager

This geological map from the State Library of Victoria collection has been annotated by GHS member Ian Bryant to show some local landmarksDigital copy of colour map.Annotations on map show locations.greensborough - maps, 1860s melbourne, suburbs, geography, roads

1909 report from the Department of Mines Geological Survey on the Redesdale Goldfield by E. J. Dunn. F.G.S. Reefs mentioned are the Horseshoe Bend Reef, Linda Reef, Bill Smith's workings, the Ben Guy Reef and the Amelia ReefDepartment of Minesgold mining, miners' safety cage, redesdale goldfield, gold mining, redesdale.

This alluvial gold nugget was discovered in 1869 at Moliagul, by Cornish miners, John Deason and Richard Oates. It's gross weight was 109.51 kg and net weight of gold was 72.02 kg. It was melted down and the ingots sent to the Bank of England.Softcover book with gold coloured cover with a sketch of the Welcome Stranger nugget on the front and a blurb on the back. Contains 50 pages covering the history, myths, geology, details of the discoverers and the discovery of the nuggett. Contains black and white photographs and sketches.Terry F Pottergold

The book includes detailed accounts in 4 sections of 1. History and Exploration 2. General Geology 3. Vegetation and slide set index 4. Climate ...Important knowledge/study for the construction of the Kiewa Hydro Electric Scheme on the Bogong High Plains.Cream cardboard cover book with black spiral binding. Title printed in black on cover. 46 pages printed on both sides includes diagrams. Clear blue plastic sheet as last page.e. j. minty, bogong high plains, kiewa hydro electric scheme

Named in 1845 by Wilhelm Karl von Haidinger cerussite takes its name from the Latin cerussa, meaning 'white lead'. When viewed under certain lighting conditions cerussite gives of fire and rainbow-like colours (due to its high dispersion) and it is quite sought after by geological collectors for this very reason. Cerussite is usually found in the oxidised zone of lead ore deposits. It is a very common weathering product of galena and other lead ore minerals. It is a secondary mineral, meaning it forms as a result of the alteration of pre-existing minerals in the Earth’s crust. The presence of lead in cerussite makes it potentially toxic. Historically, it has been an important source of lead, which has numerous industrial applications, including in batteries, construction materials, and radiation shielding. Cerussite has a crystal structure that belongs to the orthorhombic crystal system. Its crystal structure is characterized by a three-dimensional arrangement of atoms in a repeating pattern. The crystal lattice of cerussite consists of interconnected lead (Pb) and carbonate (CO3) ions. This crystal structure is visible in the specimen. This specimen was found in Dundas (formerly Mount Dundas), a historical mining locality, mineral field and railway located on the western foothills of the West Coast Range in Western Tasmania. During the 1890s Dundas swelled in numbers however it is now lost in a temperate rainforest and its population is now 2. The present Dundas Extended mine, about 1.5 km east of Dundas is presently worked for specimen material.Faceted cerussite gems are considered rare and valuable, given the softness of the mineral. This item is not a faceted gem however its historical and scientific research potential give it significance; mined in an Australian township, this cerussite could shed light on the now lost history of Dundas and the mining that occurred there. Additionally, the uses of this mineral in historical industrial processes give it scientific significance. Such knowledge can add to understandings of the geographical and geological nature of Western Tasmania and allow for further study of Australian geological specimens. A small lead carbonite mineral with shades of cream, white and brown throughout, flaky shards of white at base. CERUSSITE / (lead carbonite) / Locality: Dundas, W. Tasmaniadundas, tasmania, cerussite, lead, orthorhombic, geology, minerals, mining

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). Robert Peele was Professor Emeritus of mining Engineering at the School of Mines, Columbia University.Maroon hardcovered books. .1) Volume 1 - Chapters include Mineralogy, Geology and Mineral Deposits, Earth Excavation, Explosives, Rock Excavation, Tunneling, Shaft Sinking in Rock, Shaft sinking in Unstable and Waterbearing Ground, Boring, Underground Transport, Mine Ventilation. .2) Volume 2 - Chapers include Compressed Air Practice, Electric Power for mine Service, Surveying,Underground Surveying, Mine Geologic Maps and models, Cost of mining, Mining Laws, Ore sampling, Assaying, Aerial Tramways and Cableways, Gold Amalgamation and Cyanidation, etc.Inside front cover "Charles Bacon"charles bacon, mining engineering, mining, engineering, university of nevada, mackay school of mines, explosives, timbering

Four page document, an extract from the Geological Report on the Bendigo Goldfield. On front page, a line drawing of a puddling machine. Contents include: alluvial mining, reef mining, the boom years, deep sinking, decline of mining, modern exploration, physiography, the hills, the valleys and the soils. A table demonstrates the development of graptolite structures, including the Lancefieldian, Bendigonian, Chewtonian and Castlemainian graptolite species. Two diagrams demonstrate saddle and bedded reefs and fault reefs. Written on top of the document: C.E. William and H.E. Wilkinson, 1992. Geological Survey Report No. 93.bendigo, mining, geological bulletin 93

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

Mining and Geological Journal, Vol.4, No.3. March 1951. Published by Department of Mines Victoria with articles on Mines & mining including Bendigo mines with Photographs, Illustrations, Maps & Advertisements. Name on front A.Richardson 29 Harrison St Bendigo.Dept of Mines Victoria.gold mines, mining, mining - mines - mining equipment, central deborah mine.