Showing 39 items matching "mineral districts"
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Ballarat Heritage Services
Photograph, Nucolorvue, A Section of Lake Daylesford, 1957
Daylesford is a tourist town in Central Victorian, known for its mineral water springs.A Section of Lake DaylesfordDaylesford, Victoria, Australia This famous holiday resort is famous for its up-to-date facilities, as well as for its natural attractions. The mineral Springs are renowned for their high medicinal elements. The visitor finds ample to amuse, in excellent fishing, boating, Boating, Swimming, golfing, hiking and riding. The district provides a wide range of typical Australian bush scenery, and the altitude of 2,000 feet above sea level as a tonic effect on all. Daylesford has modern hotels, guest houses, shops and places of amusement, also many other places of interest within short travelling distance. Bendigo, 50 miles, Ballara 30 miles, and Melbourne 75 miles, bring Daylesford within easy reach of many parts of Victoria. daylesford, swimming, lake daylesford -
Ballarat Heritage Services
Photograph, Nucolorvue, Caravans in Victoria Park Camping Ground, Daylesford, 1957
Daylesford is a tourist town in Central Victorian, known for its mineral water springs.Caravans in Victoria Park Camping Ground, DaylesfordDaylesford, Victoria, Australia This famous holiday resort is famous for its up-to-date facilities, as well as for its natural attractions. The mineral Springs are renowned for their high medicinal elements. The visitor finds ample to amuse, in excellent fishing, boating, Boating, Swimming, golfing, hiking and riding. The district provides a wide range of typical Australian bush scenery, and the altitude of 2,000 feet above sea level as a tonic effect on all. Daylesford has modern hotels, guest houses, shops and places of amusement, also many other places of interest within short travelling distance. Bendigo, 50 miles, Ballara 30 miles, and Melbourne 75 miles, bring Daylesford within easy reach of many parts of Victoria. daylesford, victoria park caravan park, camping, victoria park, caravan park -
Otway Districts Historical Society
Book, Barongarook School Centenary Committee, Barongarook: a rural portrait. Norman Houghton, 1979
Barongarook: a rural portrait. Norman Houghton. John Reid (illus.) Robert Ashley (cart.) 1st ed. Barongarook School Centenary Committee; Barongarook (Vic.); 1979. 52 p.; illus, maps. Soft cover. ISBN 0 9596142 0 6barongarook; norman houghton; john reid; robert ashley; housing; schools; commercial premises; railway; roads; timber; minerals; social history; -
Otway Districts Historical Society
Book, Closed 50 Years Ago. Norman Houghton, 2012
June 2012 represented 50 years since the Colac to Beech Forest to Weeaproinah narrow guage railway was closed. The last goods train ran on 27 June 1962, and the last passenger excursion train on 30 June 1962. The railway was the lifeblood of the West Otways for several decades, enabling farmers and saw millers to bring into economic production the natural wealth of the region. Timber, butter, wool, livestock, potatoes, fodder and minerals flowed out for the benefit of Victorian consumers.Closed 50 years ago. The Colac to Beech Forest narrow guage railway. Commemorative booklet - 30 June 2012. Norman Houghton. Norman Houghton; Geelong (Vic); 2012. iv, 52 p.; illus., maps. Soft cover.colac; beech forest; weeaproinah; railway; -
The Beechworth Burke Museum
Geological specimen - Slice Dendrites on Sandstone, Unknown
Dendrites are deposits of black minerals, typically manganese oxides that precipitated from water seeping through fractures in fine-grain rocks like a sandstone or limestone. Dendrites are much less regular than plant fossils and lacks vein structures. The manganese cryztallizes through the process called 'supercooling'. Some samples of dendrites occur in volcanic rocks in the Lilydale district, east of Melbourne. Sandstones are made of tiny sand grains that may have been deposited in the sea and later formed together. Most sandstones are made of quartz which are chemically-resistant minerals. This particular specimen was donated by Alfred Selwyn in 1868 as part of the Geological Survey of Victoria. It is connected to the original 1875 catalogue on Geological Specimen with number 189 'Quartz Crystals_Quartz Crystals (two are polished)'Dendrites on sandstones This specimen is an important contribution to the geological history of Victoria, as well as its links to the 1868 Geological Survey of Victoria. This specimen is part of larger collection of significant geological specimens in the Burke Museum that was collected from around the world between 1868-1880. A large percentage of these specimens were collection as part of the Geological Survey of Victoria 1852-1974. The Geological Survey of Victoria was an organisation founded in response to the Victorian gold rush to explore the geological and mineral resources and to record a detailed map of the state. It was headed by British geologist, Alfred Richard Cecil Selwyn (1824-1902), who was responsible for issuing over 60 geological maps during his 17 years as director. These maps were all hand-drawn and coloured and became the benchmark for accuracy for geological mapping. 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 slice of light brown sandstone with dendrites formed from crystallized manganese oxide.Existing label: Not sure what / 'Slica dondrites' / means. / Sample is sandstone and original label / identifies it as from / the Grampians near Stawell. / C. Willman / 15/4/21 Other label: [illegible] / stone [ illegible] / from Grampians Stawell / 1894 /geological specimen, geology, geology collection, burke museum, beechworth, dendrites, sandstones, quartz, lilydale district, geological survey of victoria, grampians, victoria rocks, minerals, rocks, manganese oxides, alfred selwyn -
Ballarat Heritage Services
Photograph, Nucolorvue, Vincent Street Daylesford Looking Towards Hepburn Springs, 1957
Daylesford is a tourist town in Central Victorian, known for its mineral water springs.Vincent Street Daylesford Looking Towards Hepburn SpringsDaylesford, Victoria, Australia This famous holiday resort is famous for its up-to-date facilities, as well as for its natural attractions. The mineral Springs are renowned for their high medicinal elements. The visitor finds ample to amuse, in excellent fishing, boating, Boating, Swimming, golfing, hiking and riding. The district provides a wide range of typical Australian bush scenery, and the altitude of 2,000 feet above sea level as a tonic effect on all. Daylesford has modern hotels, guest houses, shops and places of amusement, also many other places of interest within short travelling distance. Bendigo, 50 miles, Ballara 30 miles, and Melbourne 75 miles, bring Daylesford within easy reach of many parts of Victoria. daylesford, vincent street, streetscape -
The Beechworth Burke Museum
Geological specimen - Green Feldspar (orthoclase)
Feldspar, derived from the German word feldspat, is a group of minerals which is the most common mineral group found on Earth, making up more than half of the planet's crust. The major rock-forming minerals in the Feldspar group include albite, anorthite, orthoclase and microcline. (Mindat, Feldspar Group). Orthoclase is part of the Feldspar Group subgroup, Alkaline Feldspar, which are known to be poor in calcium, and mostly rich in potassium. It is further also considered to be a K Feldspar, a subgroup of Alkaline Feldspar that are Potassium-dominant with variable crystal symmetry and Al-Si ordering state. Orthoclase are most commonly Colorless to white, Greenish white, Grayish yellow, or Pale pink and transparent to translucent with slightly pearly cleavage. The mineral rates at a 6 on the Mohs Hardness Scale. (cannot be scratched with a knife, but scratches glass with difficulty). The stronger green colour of this particular specimen is distinctive to the Broken Hill region (where it was found), and due to a small amount of lead. (BB) Its qualities find it misidentified at times as as microcline variety amazonite. Broken Hill is one of the world’s richest lead-zinc-silver deposits. The huge, 300-million-tonne orebody was discovered in 1883 and the superb mineral specimens attract collectors from around the world. (Australian Museum, Minerals from Australia: Australian mining regions)While feldspar is not by any means rare, this particular specimen has qualities distinctive to the Broken Hill mining district, with these properties leading at times to the mineral's misidentification. This creates potential for further study and identification of these mineral deposits through methods such as microscopic twinning, or using the position of certain d values in XRD patterns to calculate the degree of disorder of a K-feldspar, as discussed on the Mindat website (Mindat.com, Orthoclase:About Orthoclase). 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 small aluminosilicate mineral composition which is primarily pale green and blue-grey in colour with traces of beige and white throughout. Note: green plumbian orthoclase (aka green feldspar) is an indicator mineral for the Broken Hill style lead-zinc deposits.N/Abroken hill mine, geological specimen, minerology -
Bendigo Historical Society Inc.
Document - MINING REPORTS - ANNUAL REPORT, INCLUDING GOLD & MINERAL STATISTICS 1936
Handwritten notes from the Annual Report, including Gold & Mineral Statistics, 1936. Mentioned are the London price of gold and the equivalent local price, No of batteries, Abandoned Mining Shafts, Cost of making the shafts safe, Inspection of boilers and the no condemned, No of First and Second Class e 'driver Certificates issued for 1935 and 1936, Alluvial and quartz gold yields for the Bendigo District, men employed in mining, Accidents and development at the Central Nell Gwynne.document, gold, mining reports, annual report including gold & mineral statistics 1936, state batteries, central nell gwynne -
Bendigo Historical Society Inc.
Document - MINING REPORTS - ANNUAL REPORT INC GOLD & MINERAL STATISTICS ETC 1938
handwritten notes from the Annual Report. Mines mentioned ae: Central Nell Gwynne, Deborah, New Chum Syncline and the South Virginia. Carshalton B. M. L. closed down. Also mentioned are District Gold Statistics for alluvial and quartz mining, No. of men employed in mining in Bendigo. Also mentioned are tons crushed, gold yield, fees rec'd, concessions allowed and free trial crushings at the State Battery for Bendigo and Eaglehawk. The London price of gold per ounce is mentioned and also the number of 1st class and 2nd class e' driver Certificate issued for the years 1937 and 1938.Albert Richardsondocument, gold, mining reports, annual repport inc gold & mineral statistics etc 1938, central nell gwynne, deborah, new chum yncline, south virginia, carshalton b m l, state battery