This specimen is from Barefoot Hills, Victoria. Sandstones are economically important as major reservoirs for both petroleum and water, as building materials, and as valuable sources of metallic ores. Most significantly, they are the single most useful sedimentary rock type for deciphering Earth history. 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 sedimentary rock composed mostly of quartz sand. Sandstone is the second most common sedimentary rock after shale. Sandstones consist of sand-sized grains principally quartz, feldspar and rock fragments. The two major classes of sandstone are arenite and wacke. the colour of sandstone varies from grey, yellow, red and white reflecting the variation in mineral content and cement and is gritty to touch (like sandpaper).Geological survey / R.... S 61 / Loc Bareboot Hills / Sheet / 24SE / 94 /burke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, mineralogy, sandstone, yellow sandstone, victoria, barefoot hills

Manual of the New Zealand Coleoptera Author: CaptainThomas Broun Publisher: Colonial Museum and Geological Survey dept Date: 1880Label on spine with typed text RH 595.76 BRO Inside front cover has a sticker that reads Warrnambool Mechanics Institute and Free Library warrnambool, shipwrecked-coast, flagstaff-hill, flagstaff-hill-maritime-museum, maritime-museum, shipwreck-coast, flagstaff-hill-maritime-village, shipwrecked-artefact, book, manual of the new zealand coleoptera

Map, Geological Survey of Victoria, Bendigo Gold Field - Golden Square, Campaspe 10 000/2.2. Victoria 10,000.Dept. 0f Manufacturinf & Industry Development.map, bendigo, golden square gold field

Map, Geological Survey of Victoria, Bendigo Gold Field - Eaglehawk.Campaspe10 000/2.3; Victoria 1:10,000. Index of Shafts.Dept. of Manufacturing & Industry Developmentmap, bendigo, eaglehawk gold field

Map, Geological Survey of Victoria, Bendigo Gold Field - Spring Gully, Campaspe 10 000 2/1; Victoria 10,000.Cept. Of Industry, Technology & Resources.map, bendigo, spring gully gold field

Memoirs Of The Geological Survey Of Victoria No.12. List Of Nuggets Found In Victoria. Issued by Department of Mines, 69 pages in yellow soft cover.Department of Minesvictoria, history, mining

This particular specimen was found in the Moorabool Slate quarries in Victoria. The Moorabool Slate quarries was established in the 1860’s by a company of Welshmen with a crew of six who purchased land by the riverside to mine for slate. Under the promise of adding to existing recourses the crew mined the slate which was used for paving and roofing. Slate is a fine-grained, low-grade metamorphic rock that is formed by the transformation of mudstone, shale or sometimes volcanic ash under low pressure and temperatures. It dark colour is due to carbonaceous material or to finely divided iron sulphide. It is believed that Evan Rowlands and Theophilus Williams of Ballarat were the first to discover the slate veins. Slate is a one of the most common natural stones in general use. Being used as paving, flooring, roofing and more. However, its history of being mined in Australia is not common as it is considered that the best places to mine slate is Spain and parts of the United Kingdom. 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 somewhat rectangular foliated metamorphic rock composed of quartz, sericite and minerals from the chlorite group that make up the compounds of slate. The rock is dark grey almost black.Geological survey / R S / Loc Moorabool /Slate quarries / 1/4 sheet | 78 | Roofing Slate /burke museum, beechworth, geological, slate, metamorphic, slate (metamorphic), geological specimen, slate specimen, indigo shire

Department of Mines, Memoirs of the Geological Survey Of Victoria No 12 List of Nuggets found in Victoria. 67 pages in spiral binder with clear plastic cover.victoria, history, gold mining, geology, and gold pros, victoria- gold mining-gold nuggetts

BHS CollectionPart of a map of the Bendigo Gold Field - Golden Square. Geological Survey of Victoria. Shown are reefs, faults and anticlines. Many of the mines are shown on the map. Gullies, hills and streets are also shown.bendigo, history, long gully history group, the long gully history group - bendigo gold field - golden square geological survey of victoria, north bendigo state school reserve, hospital reserve, benevolent asylum reserve, empire hill, richmond hill, raes hill, south end hill, victoria hill, new chum hill, iron bark hill, redan hill, view hill, hustlers hill, camp hill

Office of Mines published progressive reports on the Geological Survey of parts of Victoria.This book includes a chapter on 'Dargo and Bogong' Pages 96 - 117 and includes a fold out map of this area. These pages show heavy use.Hard deep red cover with gold printed title located at the centre top. Bound with spine blank. 217 pages. Date 1878 First chapter and some pages have pencil marks including page 97.geological survey 1878, dargo, bogong

This specimen was found in Harcourt, Victoria. Harcourt is a small historic gold rush town located in a valley at the foot of Mount Alexander (741 m) in the Central Highlands of Victoria. In recent times the goldrush origins of the town have been replaced by a district known for apples, cider and wine. The Traditional owners of Harcourt are The Dja Dja Wurrung people. Granodiorite is a coarse-grained intrusive igneous rock similar to granite, but containing more plagioclase feldspar than orthoclase feldspar. Granodiorite has greater than 20% quartz by volume, and between 65% and 90% of the feldspar is plagioclase. This piece is of significance due to its provenance in Harcourt, Vic. Granodiorite is commonly produced in volcanic arcs, and in mountain buildings where it emplaces as large batholiths in mountain roots. Granodiorite is the plutonic equivalent of dacite. 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.Granodiorite is a coarse-grained intrusive igneous rock similar to granite, but containing more plagioclase feldspar than orthoclase feldspar. According to the QAPF diagram, granodiorite has a greater than 20% quartz by volume, and between 65% and 90% of the feldspar is plagioclase.GRANDIORITE. / Locality: / Harcourt, Victoria / Other label: Geological survey / R S / Loc Harcourt quarries [?] Alexander / 1/4 Sheet. | 4 | Granite /granodiorite, granite, burke museum, harcourt, coarse-grained, igneous, plagioclase feldspar, orthoclase feldspar, quartz, mount alexander, the dja dja wurrung people, the traditional owners, central highlands of victoria, gold rush

Rectangular plan of a geological survey edged in masking tape. It is predominantly grey, pink and green, but has some yellow. scale is 40 chains to one inch. (see Cat. No. 1098 for report on the Parish of Scarsdale)scarsdale, grenville, krause, browns and scarsdale, mopianimum, watershed, yarrowee, woady yalloak, timber reserve, department of mines, plans, cgt, crown lands, ferdinand krause

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 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

Map, Hustler's Line of Reefs, Hustler's Reef & Hustler's Reef No.1 Mines, Plan view . Plate No. XV (15).Sheet 1 Bulletin No. 33. Included is the emblem of the Geological Survey of Victoria. Signed by H.A.Whitelaw Underground Survey Office, Bendigo, Septembe ,1913.Underground Survey Office, Bendigo.map, bendigo, hustler's reef & hustler's reef 1

Book, Department of Mines, Bulletins of the Geological Survey of Victoria, No.33, Hustler's Line Of Reef, Bendigo, with plans,sections, and photographs, by H.S.Whitelaw. 13833, Price 2s.6d.`Back cover shows J.A. and J.A Strugnell , 12 Mulbar St Swan Hill 3585 .Albert J. Mullett, Government Printer, Melbourne.book, bendigo, hustler's line of reef

This publication consists of many Decades which contain "figuers and descriptions of the fossil organic remains to be used for the determination of the geological ages of the different geological formations of the country." (p. 3). Frederick McCoy was born in Dublin, Ireland in 1817. He was a Professor of Natural Sciences, University of Melbourne 1854-1899. McCoy lectured in geology, zoology, chemistry, mineralogy, geography and botany. In 1858 He became the Director of the National Museum of Victoria and the President of the Royal Society of Victoria in 1864. In 1888, McCoy was awarded FRS for work in Palaeontology in Ireland, England and Australia. He died in his office while correcting examination papers in 1899.A Paperback cover book. Decade v. Title is written in black on front cover and on title page. At head of title: Geological Survey of Victoria. Illustrations, plates in b/w; 41 p. It includes figures and descriptions of Victorian Organic Remains and contents of Decades on back cover.Stamped Ballarat East Public Library"australia palaeobotany, victoria palaeontology, geological survey of victoria, frederick mccoy, organic remains, ballarat east library, ballarat east public library

This publication consists of many Decades which contain "figuers and descriptions of the fossil organic remains to be used for the determination of the geological ages of the different geological formations of the country." (p. 3). Frederick McCoy was born in Dublin, Ireland in 1817. He was a Professor of Natural Sciences, University of Melbourne 1854-1899. McCoy lectured in geology, zoology, chemistry, mineralogy, geography and botany. In 1858 He became the Director of the National Museum of Victoria and the President of the Royal Society of Victoria in 1864. In 1888, McCoy was awarded FRS for work in Palaeontology in Ireland, England and Australia. He died in his office while correcting examination papers in 1899.A Paperback cover book. Decade VI. Title is written in black on front cover and on title page. At head of title: Geological Survey of Victoria. Illustrations, plates in b/w; 42 p. It includes figures and descriptions of Victorian Organic Remains and contents of Decades at back of the book.australia palaeobotany, victoria palaeontology, geological survey of victoria, frederick mccoy, organic remains, john ferres

Bulletin 62 from the Geological Survey of Victoria, titled ' Derep Lead Gold Deposits of Victoria' by F. Canavan, M Sc. K. Bowen and H. Tan, Technical Editors, R.A. Bull, Editor. Bendigo and Sebastian District and the Huntly Telegraph Lead, are discussed in the paper.bendigo, mining, geological survey bulletin 62, bendigo, sebastian, geological survey.

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). William Emmons was Professor and head of Geology and Mineralogy at the University of Minnesota; Director of Minnesota geological Survey; and previously Geologist, Section of Metalliferous Deposits, United States Geological Survey.Maroon soft covered book of 529 pages. Chapters include Magmatic Segregations, Pegmatities, Hypothermal Deposits, Sedimentary Depostis, Openings in Rocks, Metasomatic Processes, Mineral Associations and more.Inside front cover "Charles Bacon 1940 Lincoln Hall Ass. University of Nevada Reno, Nevada"charles bacon, mining engineering, metallurgy, university of nevada, mackay school of mines, geology, california

This publication consists of many Decades which contain "figuers and descriptions of the fossil organic remains to be used for the determination of the geological ages of the different geological formations of the country." (p. 3). Frederick McCoy was born in Dublin, Ireland in 1817. He was a Professor of Natural Sciences, University of Melbourne 1854-1899. McCoy lectured in geology, zoology, chemistry, mineralogy, geography and botany. In 1858 He became the Director of the National Museum of Victoria and the President of the Royal Society of Victoria in 1864. In 1888, McCoy was awarded FRS for work in Palaeontology in Ireland, England and Australia. He died in his office while correcting examination papers in 1899A Paperback cover book. Decade IV. Title is written in black on front cover and on title page. At head of title: Geological Survey of Victoria. Illustrations, plates in b/w; 32 p. It includes figures and descriptions of Victorian Organic Remains and contents of Decades on the back cover of the book.australia palaeobotany, victoria palaeontology, geological survey of victoria, frederick mccoy, organic remains

Sixteen page booklet Geological Survey Report, Mines Department Victoria. 'Geology of the Bendigo Area' by H.E. Wilkinson. Photo of Lansell's 222 Mine on the New Chum Line, Bendigo. Tallest poppet head on the field, approximately 38 m high, with a shaft depth of 635 m.bendigo, mining, geological survey report