Feldspathic arenites are sandstones that contain less than 90% quartz, and more feldspar than unstable lithic fragments, and minor accessory minerals.Feldspathic sandstones are commonly immature or sub-mature.These sandstones occur in association with cratonic or stable shelf settings. Feldspathic sandstones are derived from granitic-type, primary crystalline, rocks. If the sandstone is dominantly plagioclase, then it is igneous in origin Sandstone features prominently in public buildings throughout Victoria. Most of the sandstone used as dimension stone in the State came from three sources: the Heatherlie quarry in the Grampians (Silurian), the Bacchus Marsh area (Permian), and the Barrabool Hills near Geelong (Cretaceous).Sandstone features prominently in public buildings throughout Victoria, making this specimen special as it shows the materials used by Victorian building companies. Sandstone can also be crushed, crushed stone is used in the construction of roadways and road structures such as bridges, and in buildings, both commercial and residential. 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 feldspar-rich sandstone, a sandstone intermediate in composition between an arkosic sandstone and a quartz sandstone, containing 10% to 25% feldspar and less than 20% matrix material of clay, sericite, and chlorite. Feldspathic arenite containing less than 90 percent of the composition of quartz. Feldspar is the main composition. Feldspathic arenite may contain fragments of unstable rock, and a little amount of other minerals such as mica and heavy minerals. Some feldspathic arenite have pink or red color because of the presence of potassium feldspar or iron oxide. There are also colored light gray to white. These sandstones are usually medium to coarse grained and can contain a high percentage of granules with angular until subangular roundness. The content of the matrix can appear as the rest up to more than 15 percent, and sorting of grains can present as moderate to poorly sorted. Feldspathic sandstones are generally immature in textural maturity. Feldspathic arenite can not be judged from the structure of the sediment. Bedding can emerge from the laminate parallel to the crossbed. Fossils may appear in the layer deposited on the sea. Feldspathic arenites usually appear on the craton or the continental shelf, which can be associated with conglomerate, quartz lithic arenite, carbonate rock, or evaporites. This sandstone may also appear on the succession of sedimentary basins deposited on an unstable or deep sea, and moving arc setting. According to Pettijohn (1963) Arkose make up about 15 percent of all sandstones. Some Arkose formed in situ when the granite and related rocks disintegrate and generate granular sediments. Most of the material feldspathic sandstones derived from primary crystalline granitic rocks, such as granite or metasomatic rocks containing abundant potassium feldspar. Mineral contained in sandstones is mostly a form of plagioclase feldspar derived from quartz diorite or volcanic rock. Feldspar contained on this sandstone comes from arid to cool climates when the chemical weathering process is reduced.sandstone, natural stone, feldspathic sandstone, burke museum, geology, geological, geological specimen

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

Quartz is an extremely common mineral to find across the world. Quartz can have two forms; Microcrystalline quartz or Crystalline quartz. Microcrystalline quartz is a fine grain quartz where crystalline quartz is often a large crystal. This specimen is a crystalline quartz. Made of silicon oxide, this specimen is called smokey quartz crystals because of its brownish colour. However, the colour of quartz can vary. In addition, quartz are formed in deep-seated igneous rocks and crystallized through hot aqueous solutions. This type of crystal can be found all over Australia, including Beechworth in Victoria. Other places quartz can be found is the Ashburton River area in Western Australia, Marlborough in Queensland, the Lune River area in Tasmania and Kingsgate in New South Wales. This specimen is significant because it is common to find this kind of mineral. While the location of where this specimen was originally from is unknown, it highlights the many places in Australia where quartz is found. It demonstrates that quartz makes up a large portion of Australia's geology. In addition, quartz itself can vary in its colour and shape. This specimen represents one of these variations. That being smoky quartz crystals. 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 large hand-sized quartz mineral with shades of brown and gray throughout.Smoky quartz / crystals /locality/ unknown / (needs a wash) /BBgeological specimen, geology, geology collection, burke museum, beechworth, microcrystalline, quartz, quartz mining, quartz reefs beechworth, smokey quartz crystals, crystals, crystalline, silicon oxide, brown, colour, igneous rocks, magma, ashburton river, western australia, marlborough, queensland, lune river, tasmania, kingsgate, new south wales, nsw

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. Quartz is found all over Australia, including Beechworth in Victoria. It is formed in deep-seated igneous rocks and crystallized through hot aqueous solutions. It can have two forms; Microcrystalline quartz or Crystalline quartz. Microcrystalline quartz is a fine grain quartz where crystalline quartz is often a large crystal. The colour of quartz can vary. These specimens were collected in Victoria in the vicinity of the Burke Museum. 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.Geological specimens of Agate and Quartz respectively; the fist-sized piece of Agate has peach/coral colouring with grey concentric patterning and the smaller piece of quartz is a uniform yellow/orange shade. Existing label: Local pebbles / (agate and / quartz / (yellowish) / egg-shaped). / BB geological specimen, geology, geology collection, burke museum, beechworth, agate, quartz, north-east victoria, indigo shire, geological surveys

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

Scales were used in the Tarnagulla area of Central Victoria by Albert Charles Nicholls, who was a licensed assayer. This information comes from David Gordon of the Tarnagulla.com web-site. “The Nicholls family were very well known and highly respected at Tarnagulla in the 1800s. Albert's father, William Nicholls, was a leading figure in the gold mining community, and he both managed and owned quartz processing facilities for decades. He was probably the leading mining expert at Tarnagulla in a town full of mining experts, and it was said that no man at Tarnagulla had handled more gold over the years that him. (think in terms of tons of gold!) I would imagine the assaying equipment was probably passed in due course by William to Albert Charles. There are records of Albert Charles mining at Tarnagulla with his father as a young man, but AC apparently came down to the city when the gold began to fade. There are records of him living in Kew up until his death in 1932. He was employed as a draper for a long period.” This item is a significant item which is part of the history of gold mining in Victory.Gold assayer's scales, a very sensitive balance used in the assaying of gold, silver, etc.The scales are comprised of two circular brass pans suspended via brass chains to a metal balance.scales gold technology assayers tarnagulla

The A1 Gold Mine is located north of Woods Point, near Jamieson, in the Upper Goulburn region of Victoria. Gold was discovered at the A1 site in 1861 and mining operations began in 1864. The A1 Mine Settlement refers to a small township known variously as Castle Reef, Castle Point, and Raspberry Creek, which developed in the 1860s around mining industry centred on a crushing machine that worked the three gold reefs in the area. Historically, the name "A1"referred to the high quality of gold found in the quartz reefs at depths of at least two thousand feet. Along with the Morning Star mine at Woods Point, the A1 gold mine produced almost sixty percent of Victoria's gold output in the 1950s to 1970s and continued operating until 1992 when it went into administration. Operations at the site were revived in 2016 and the A1 Mine is now considered one of Victoria's premier gold mines. The A1 mine is part of the extensive and prospective Lachlan Fold Belt, a north-west trending belt of tightly folded Early Devonian sedimentary rocks extending from New South Wales to Victoria. Mineralisation is hosted within or immediately adjacent to diorite dykes. Contemporary development of the 'Queens Lode' at the A1 mine signals a move from high-grade, narrow vein airleg mining into larger scale, mechanical mining designed to increase ore production volume. This original, undated photograph of the A1 Mine appears to depict an area or phase of disuse or abandonment. The aged and humble appearance of the cottage suggests association with the historical A1 Mine Settlement, therefore the image may have been taken prior to the 1950s-1970s revival period in which the A1 mine is known to have produced high gold yields. The photograph contributes to our understanding of the A1 Gold Mine's impact on the landscape and the social, environmental impacts of mining on communities and may be compared with others in the Burke Museum's extensive collection of mining photographs to deepen our understanding of mining in the Jamieson area.Black and white rectangular photograph printed on photographic paperReverse: 5577 / A1 Mine / Near Jamieson / Vic. /burke museum, beechworth museum, beechworth, gold fields, gold rush, victorian gold rush, mining tunnels, gold ming history, colonial australia, australian gold rushes, mining technology, beechworth historic district, indigo gold trail, indigo shire, upper goulburn shire, jamieson, woods point-walhalla goldfield, a1 gold mine, victorian high country, modern mining methods, orogenic gold province, gold mineralisation, devonian, dykes

No information is available on these two items which would have been collected and polished by someone, probably someone interested in lapidary. The quartz would probably not have come from our area (Western District of Victoria).These items have no known local significance and will be useful only for display. These are two white quartz crystals with gold and silvery encrustations and markings. They are rough on the top and cut into geometric shapes and polished on the bottom part. The larger piece seems to have been fused together or split at one stage. quartz crystals, warrnambool

The handbook was intended for those with little experience who wanted to prospect of fossick.Grey soft covered book of 90 pages. Includes fold out map of a portion of Victoria showing auriferous areas and mineral localities. Also show Counties of Victoria and localities of minerals such as tin, antimony, copper, silver lead, Malybdenite, tungsten ores, manganese, platinum, osmiridium and iron. Chapter heading s include: working alluvial deposits, equipment, geology of Victoria, gold deposits, quartz reefs, indicators, economic minerals, assistance to prospectors, Miners' Right, mining bye-law, mining leases, forest regulations and glossary. Descriptions are given of a god dish, puddling tub, cradle, puddling machine, ground sluicing, boring, windlass, whim, hand dollying, sweeping, California pump, and wing dam.mining, baragwanath, gold, prospector, geology, quartz reefs, alluvial deposits, indicators, victorian goldfields, miners rights, mining leases, forest regulations, sluicing, sluice box, puddling machine, miner's cradle, whim, whip, california pump, gold nuggets, saddle reef, ballarat indicators, state batteries

Typed copy of what appears to be a speech. Mentioned is that after 1910 the Commonwealth took over the minting it's own money. Gold mining was chosen for the one pound note and a Bendigo scene was chosen. The scene chosen shows boring operations in the Victoria Quartz Mine. The picture was taken by Vincent Kelly of the five figures but for engraving only three were shown. They were Mr W Healy, Mr J Smith and Mr James Beverage. James Beverage was a member of Bendigo's first fire brigade. He went to Beechworth for a demonstration and on the way home stopped at Christie's Hotel in Swanston Street. There was a fire at the hotel and Mr Beverage rescued Mrs Christie, her baby and a servant. At a later date Mr Beverage saved a woman from a burning building in Moore Street in Bendigo. He received the Royal Humane Society's Medal which is now housed at the Bendigo Fire Station in Hargreaves Street. In the City's formative years the area that deposited its rain water into the Long Gully Creek was considered to be in Long Gully and for many years the Victoria Quartz Mine deposited many thousands of gallons of water into the Long Gully Creek. Mr Steve Gibbons unveiled the plaque.bendigo, history, long gully history group, the long gully history group - banknotes and james beverage, victoria quartz mine, vincent kelly, shepard's bush, mr rickards, mr abraham, mr w healy, mr j smith, mr james beverage, south iron bark mine, rae's hill, sandhurst no 1 fire brigade, christie's hotel, mrs christie, royal humane society's medal, bendigo fire station, long gully history group, mr steve gibbons, department of environment water heritage, arts commnmoration of historic events and famous persons

Joan O'Shea Collection. Victoria Hill Bendigo Gold Mining on the Richest Quartz Reef in Bendigo, from 1854 to 1916. Colour and Black and White Booklet 16 Pages. Includes Maps of the Victoria Hill Area, photographs of the remains of a twenty head crushing battery, burnt ground from quartz roasting, The Victoria Quartz Mine Photograph from Australian Mining Standard June 1899, The compressor beds and concrete foundations for the poppet legs all that remain today of the Victoria Quartz Mine deepest mine on Bendigo Goldfield 4613 feet or 1406.04 metres. Also included photograph of the view of Victoria Hill from The New Chum Hill in the 1870s. The Location of the 3 mines Ballerstedt's open cut, North Old Chum and Lansell's 180 are marked. A depiction of Rae's Open Cut gives an understanding of the primitive nature of early workings on the Goldfields. The Booklet also provides a brief history of Victoria Hill itself.Bendigo Trust Publication March 1972. Printed in Bendigo Cambridge Press.bendigo, mining, victoria hill

Three pages numbered 18/19, 20/21 and 22/23 titled Victoria Hill. First page has some information on Victoria Hill, a sketch of W Rae's Home and Rae's Open cut. The second page has a map of the Victoria Hill Area showing streets and the New Chum Anticline, a sketch of Ballerstedt's Open Cut and a Key to Victoria Hill Area Map. The third page mentions the Victoria Quartz mine, Tributors and quartz roasting. It also has sketch of a 20 Head Crushing Battery, Victoria Hill.bendigo, history, long gully history group, the long gully history group - victoria hill, gold mines hotel, christopher ballerstedt, theodore ballerstedt, ballerstedt's open cut, lansell's 180 mine, little 180 mine, new chum syncline battery, victoria reef quartz mining co, victoria quartz, new chum drainage scheme, a roberts and sons, tributors, william rae's bon accord mine and open cut, william rae, adventure and advance open cuts, central nell gwynne, heinz butcher shop

Three page handwritten document outlining the history of the Victoria Hill area. The open cuts on Victoria Hill; Lansell's Big 180 Mine, Victoria Quartz Mine; Wittscheibe's 'Jewellers Shop', Luffman and Sterry, Central Nell Gwynne and New Chum Hill are mentioned in the article. A description of the suitability of the Victoria Hill site as a potential mining museum is discussed as 'it is centrla to both the northern and southern ends of the main portion of the Bendigo and Eaglehawk mines'. William Rae built two fine residences on Happy Valley Road, and also set up a 30 head battery out of his gains from Victoria Hill.bendigo, mining, victoria hill

South New Chum Syncline South New Chum Syncline Gold Mines, N.L., has been floated with a capital of £27,500 in 55,000 shares of 10/ each. Forty thousand have been issued at 1/,10,000 fully paid shares go to vendors, and 5000 will be held in reserve. - Messrs. Savage and Nicholas report that the issue was heavily over-subscribed. The property is situated in the central portion of the Bendigo field, adjoining such former producers as the Victoria Quartz. Lansell’s Big 180, North Old Chum and New Chum. (Bendigo Advertiser, 29th September 1932).Seven pages of correspondence detailing a 'Permit to Mine' in favour of Messrs W.J. Browell, A.W. Browell and A.R. Hannon, Golden Square, in respect of portion of the area held under Gold Mining Lease No. 9903. Letter dated 23rd February 1937 to J.J. Stanistreet, Legal Manager, South New Chum Syncline, Bendigo from Mines Department, Treasury Gardens, Melbourne confirms the permit held under Gold Mining Lease No. 9903, Bendigo. List of articles taken by Browell on 29th June, 1936, is attached. Draft copy of 'permit to mine' document attached. bendigo, gold mining, south new chum syncline gold mine, j.j. stanistreet, legal manager, margaret roberts collection,