Red hard cloth covered book of 845 pages. Includes contents and index.non-fictionThis volume includes Australasia, and lists each state seperately , as well as New Zealand, It also lists Bismoth, Chome iron ore, coal, copper, gold, lead, mineral industry growth, alumite, antinomy, cobalt, coke, copper ore, gold, iron, lead, limestone flux, managanese, shale, silver, silver-lead, tin and zinc mining, statistics, technology, trades, metal industry, minerals, united states, canada, china, france, germany, italy, japan, russia, south america, spain, sweden, united kingdom, ireland, coins, cuba, blast furnaces, gold, lead production, manganese, opals, silver, +, alumite, antinomy, cobalt, coke, copper ore, iron, lead, limestone flux, managanese, shale, silver-lead, tin, zinc, abrasives, chemical industry, gems, precious stones, dividends, akalies, salt, earthernware, glass, petroleum, aluminium, bismuth, tungsten

From the Ballarat School of Mines.Geological specimenrocks, geology, mica schist

Frank Wright was a renown resident of Smeaton, where he was born. He lived at Laura Villa, and attended Smeaton State School. His father William was a gold miner and his mother's name was Sarah. Their family won many singing and instrumental awards. Frank was tutored by Percy Code and became the Australian Open Cornet Champion by the age of eighteen. A year later, Frank conducted the City of Ballarat Band, and later the Ballarat Soldiers’ Memorial Band. He formed the Frank Wright Frisco Band and Frank Wright and his Coliseum Orchestra. These bands won many South Street awards, and Frank as conductor won many awards in the Australian Band Championship contest. In 1933 Frank Wright sailed to England to conduct the famous St Hilda’s Band and was later appointed Musical Director of the London County Council, where he organized many amazing concerts in parks, in and around the London district. He was made Professor of Brass and Military Band Scoring and conducted at the Guildhall of Music and Drama. Frank was often invited to adjudicate Brass Band Championships around Europe, in Australia, including South Street and in New Zealand. The Frank Wright Medal at the Royal South Street competition is awarded to an individual recognized as making an outstanding contribution to brass music in Australia..1) black and white photograph of two men, one sitting on a motorbike, dressed in boots, rolled up pants, shirt and tie and a belted jacket and the other man is sitting in an outfit (or sidecar). They are in front of a brick building with a circular window, the Hepburn Springs Pavilion. The one on the bike is Frank Wright. .2) sepia photograph of a man on a motorbike with outfit (or sidecar). He is on a country road with a trimmed hedge in the background. The man is Frank Wright..1) handwritten on the back - Hepburn Springs Pavilion. Printed on the back - Post Correspondence .2) printed on the back - Post Correspondencefrank wright, hepburn springs pavilion, motorbike, outfit, sidecar, transport, motorcycle, hepburn springs

Buildings - Hotel

Black and white photograph of Lake Daylesford.daylesford, mineral springs, camping, camping ground

Robert Mosely was an aerated water and cordial manufacturer. in 1909 Robert Mosley married Isabel Ethel Shepherd Stevens (or Steens). (Victorian Marriage Records, 1909) He died in 1936. MOSLEY. - On the 28th June at a private hospital, Melbourne, Robert, the dearly loved husband of Ethel Mosley, of 31 Ormond road, Moonee Ponds, loving father of Florrie (Mrs. Bayne), Jane, and Bessie (Mrs. Read), loving stepfather of Gladys (Mrs Myers) and Esma Campion, aged 75 years. — At rest. (The Argus, 29 June 1936) MOSLEY. — On the 28th June, at a private hospital, Melbourne, Robert Mosley, of 31 Ormond-road, Moonee Ponds. At rest. (The Age, 29 June 1936)Glass bottle made for Robert Mosely of Flemington Bridge, Melbourne. The 1896 Mosley bottles was manufactured in England and Victoria (t Mr Corfield's in Exhibition Street, Melbourne. )r. mosley, robert mosley, mineral water, flemington, globe mineral water works, flemington bridge

A number of people stand on a timber bridge which spans Spring Creek at Hepburn Springs. hepburn springs, spring creek, spring creek bridge, hepburn mineral spring, pavilion

Black and white postcard of Hard Hill Spring, Daylesford.hard hill spring, daylesford, mineral water

Red hard cloth covered book of 115 pages. INcludes contentsnon-fictionThis volume includes Australasia, and lists each state seperately , as well as New Zealand, It also lists Bismoth, Chome iron ore, coal, copper, gold, lead, mineral industry growth, alumite, antinomy, cobalt, coke, copper ore, gold, iron, lead, limestone flux, managanese, shale, silver, silver-lead, tin and zinc Lead production Manganese opals mining, statistics, technology, trades, metal industry, minerals, united states, canada, china, france, germany, italy, japan, russia, south america, spain, sweden, united kingdom, ireland, coins, cuba, blast furnaces, gold, lead production, manganese, opals, silver, +, alumite, antinomy, cobalt, coke, copper ore, iron, lead, limestone flux, managanese, shale, silver-lead, tin, zinc

Daylesford is a tourist towns with natural mineral water springsCentral Springs, one of many mineral water springs at Daylesford.daylesford, lake daylesford, central springs

Calcite is a common mineral and is found worldwide due to it being a primary component of many other rocks such as limestone and marble. It is a softer mineral that scratches easily and is often found colourless or with a cream/white shade but may show up in colours such as red, yellow, green, and violet. In sedimentary rocks calcite is often found in the form of invertebrate shells, making it an important biomineral. Calcite is used in many industries such as farming, building, and medicine. This particular specimen was found at Broken Hill mine in Broken Hill, New South Wales, Australia. Broken Hill mine is one of the largest mines working silver and lead in Australia and at its peak employed 6500 staff across 7.5km long of land. The site was founded in 1883 by Charles Rasp, where Rasp and 6 other men from various backgrounds came together to form the first BHP mine. It has become one of the most popular mining sites due to its abundance and longevity. The ore body was created 1685 million years ago due to volcanic activity causing heated seawater to flow up through the seafloor where it mixed with the cold water creating black sulphide precipitates. These then settled back onto the seafloor forming sediment layers rich in minerals. Over time the land eroded until it was discoverable by humans.Historically this specimen is significant due to the origin of its location. Broken Hill mine has a long history in both its location and its findings and has resulted in a variety of minerals being discovered at its site. It is beneficial in the understanding of the Australian landscape over millions of years. Due to its properties, calcite today is used in a multitude of different industries such as agriculture, construction, medicine, and farming.A small sized calcium, carbon and oxygen made mineral specimen in shades cream and greycalcite, mineral, limestone, marble, sedimentary, invertebrate shells, biomineral, farming, medicine, broken hill, broken hill mine, new south wales, charles rasp, syndicate of seven, volcanic activity, black sulphide precipitates, calcite crystals, beechworth museum, indigo shire, beechworth

Native Sulphur in its solid form is a yellow crystalline mineral that forms near volcanic vents and fumaroles where it is the solid form of hot gases. It is also frequently found in the subsurface as a by-product of sulphide ore mineralization. In all its forms, sulphur is one of the most commonly occurring minerals on the planet, especially in natural gases, and is key to the make-up of a range of other minerals. It is essential to continuing life on earth, and was used in ancient societies as part of medical care, religious rites, and entertainment, and was key to the invention of gunpowder by the Chinese. Native Sulphur in its solid form is a yellow crystalline mineral that forms near volcanic vents and fumaroles where it is the solid form of hot gases. It is also frequently found in the subsurface as a by-product of sulphide ore mineralization. In all its forms, sulphur is one of the most commonly occurring minerals on the planet, especially in natural gases, and is key to the make-up of a range of other minerals. It is essential to continuing life on earth and was used in ancient societies as part of medical care, religious rites, and entertainment, and was key to the invention of gunpowder by the Chinese. The exact site of extraction for this specimen is unknown, but it was probably collected in New Zealand in the 1850s. Sulphur is significant both for its historical and current uses, and for its nature as one of the most abundant minerals on the planet. Sulphur's importance comes both from its abundance and its role in ensuring survival, creating other minerals, and daily human life. This specimen is significant as representative of sulphur's solid properties. 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, crystalline mineral specimen that is largely bright yellow, with some darker spotting. geological specimen, geology, geology collection, burke museum, beechworth, sulphur, native sulphur, new zealand, native sulphur specimen, sulphur specimen

This specimen was recovered from Broken Hill, NSW. It was given the name Mangan Hedenbergite in 1819 by Jöns Jakob Berzelius in honor of Mr. Anders Ludvig of Hedenberg who was the first to define hedenbergite as a mineral. Hedenbergite, belongs in the pyroxene group having a monoclinic crystal system. The mineral is extremely rarely found as a pure substance. Mangan Hedenbergite is a manganese bearing variety of Hedenbergite. Manganese is the world’s fourth most used mineral after iron, aluminium, and copper primarily because it has no satisfactory substitute in its major applications. Globally, the steel industry is the primary user of manganese metal, utilizing it as an alloy to enhance the strength and workability of steel and in the manufacture of tin cans. Manganese is a key component of certain widely used aluminium alloys and, in oxide form, dry cell batteries used in electric vehicles. These batteries are in high demand. Another potential use for manganese may as an additive to help coat and protect a car’s engine. Manganese is also used for non-metallurgical purposes such as plant fertilizers, animal feed, and colorants for bricks. 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 hand-sized mineral specimen in shades of silver and blackmanganese, open cut mine, manganese ore processing, bell bay, tasmania, northern territory, steel industry, zinc-carbon batteries, alkaline batteries, tin cans

Hepburn Springs in a tourist town with natural mineral water springsA black and white photographic image of the pavilion in the Hepburn Springs Mineral Springs Reserve. hepburn springs, mineral water, pavilion

Hepburn Springs in a tourist town with natural mineral water springsA black and white photographic image of Locarno Spring in the Hepburn Springs Mineral Springs Reserve. hepburn springs, locarno mineral water spring, mineral water, locarno spring

Hepburn Springs in a tourist town with natural mineral water springsA black and white photographic image of Wyuna Spring in the Hepburn Springs Mineral Springs Reserve. hepburn springs, mineral water, wyuna spring

Hepburn Springs in a tourist town with natural mineral water springsA black and white photographic image of Locarno Spring in the Hepburn Springs Mineral Springs Reserve. hepburn springs, locarno mineral water spring, mineral water, locarno spring

Hepburn Springs in a tourist town with natural mineral water springsA black and white photographic image of Sulphur Spring in the Hepburn Springs Mineral Springs Reserve. hepburn springs, mineral water, sulphur spring

Hepburn Springs in a tourist town with natural mineral water springsA black and white photographic image of a metal spring in the Hepburn Springs Mineral Springs Reserve. hepburn springs, mineral water, bridge

Tourmaline is a group of minerals belonging to the complex borosilicate mineral class. These minerals are known for their striking and varied colours, making them prized gemstones. Tourmaline crystals can come in various shades, including pink, green, blue, brown, black, and colourless. They are often transparent or translucent. Tourmaline's chemical composition is complex, but it typically includes elements such as aluminium, iron, magnesium, sodium, lithium, and potassium. The specific arrangement of these elements in the crystal lattice gives rise to the different colours and properties of tourmaline specimens. Tourmaline specimens from Beechworth, Victoria, Australia, are a notable part of the region's mineral heritage. These tourmalines are of interest to mineral collectors and enthusiasts. While the tourmaline found in Beechworth is not as well-known as some other tourmaline varieties, it has unique characteristics and a historical context associated with the gold mining areas in Beechworth.The significance of tourmaline in Beechworth, Victoria, Australia, lies in its unique geological and historical context, contributing to both scientific and cultural aspects. The tourmaline mined in Beechworth is a rare and unique variety of tourmaline that is primarily found in the historic gold mining areas surrounding Beechworth. Its occurrence is closely linked to the geological processes that shaped the region during the Gold Rush era. The discovery of tourmaline in Beechworth adds to the rich mineral heritage of the area, which was historically known for gold mining. The specimens serve as a tangible connection to the region's mining history and contribute to preserving its geological legacy. The presence of tourmaline in Beechworth showcases the mineralogical diversity of the area. Tourmaline is known for its wide range of colours and unique properties, making it a valuable subject of study for mineralogists and geologists. Tourmaline specimens from Beechworth have educational significance, providing opportunities for research and study. They offer insights into the geological processes and mineral formation in the region, contributing to a better understanding of Earth's geological history.A hand-sized solid mineral specimen in shades of brown, green, light grey and dark greyTOURMALINE (schorl) / (Silicate of boron and aluminum) burke museum, beechworth, indigo shire, geological, geological specimen, mineralogy, tourmaline

Emerging from the base of Wombat Creek Sutton Spring has two mineral water pumps. The spring is named after the Sutton brothers of Cornwell, who discovered it while looking for alluvial gold along Wombat Creek in the 1850s. By 1900, a trench had been dug to expose the spring, and a pipe had been driven through the spring eye. Sandstone rockwork encircled the trench. On 27 February 1907 the Sutton Mineral Spring Reserve was gazetted. By that time the trench had been enlarged and rendered, and a lean-to shelter had been built over the approach track. In 1927 Wombat Creek was rerouted allowing the land around the spring to be cleared and pipework repaired. Five bores were dug in 1929 and equipped with hand pumps. The bores were all shallower than 9.7 m. An attempt was made to replace one of these bores with a new bore, however it was not possible due to ground instability. These two bores are the oldest of all the mineral springs open to the public. Also in 1929 Council contemplated encouraging private enterprise to establish a ‘hydrobath’ similar to those in Europe, after mineral water had been discovered flowing from several other vents in sandstone and slate strata below the typical level of the creek. However, the option was not enacted although at the time to capture the flow another bore to a depth of 15m was sunk. In 1936 architect P. Scott Williams adopted a similar notion and examined the prospect of establishing a Hydropathic establishment above Sutton Springs, assuming a reliable mineral water supply could be found. That idea also lapsed. In October 1997 the Sutton Spring trench was restored to enable the public to again take mineral water at the spring. The restoration included clearing the sides of the creek and removing willow root growth. In 2002 a major overhaul of the trench and its underground works was undertaken and all plumbing replaced. This involved re-routing the creek through sandbagging, covering the spring eye with geofabric and then concrete. Unfortunately due to ongoing water quality issues, public access to take water from the trench was closed, however the trench can still be viewed.A mineral water spring at Daylesford is surrounded by a drystone wall. mineral water, sutton spring, daylesford, central springs, p. scott williams

Gold usually is found as a native metal, but it also forms minerals with tellurium, sulphur, or selenium. The gold-bearing minerals that contain tellurium are called tellurides. Kalgoorlie, Western Australia contains greater than 1500 tonnes of gold.Seventy to seventy-five percent of the deposit occurs as native gold, but a further twenty percent appears as tellurides. What remains is in the form of 'invisible' gold. Extracting gold from telluride minerals, such as calaverite, which contains around forty-two percent gold, has produced approximately three hundred tonnes of gold. Prior to 1896, rocks containing tellurides were not recognised as rich gold ores, and were discarded.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 hand-sized silvery to pyrite-yellow striated mineral containing tellurium and goldburke museum, beechworth, beechworth museum, geological, geological specimen, mineralogy, telluride, tellurite, gold-bearing, kalgoorlie, tellurium

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

Quartz is one of the most common minerals in the world. It is formed by a 3d structure of silicon and oxygen. While it is a simple mineral, it can come in a variety of shapes and colours. When quartz is pure it is colourless, transparent and can appear glass-like. Better known and more rare variations of quartz include amethyst and smoky quartz. This specimen is a vein of quartz in Breccia Conglomerate. Breccia is coarse-grained clastic rock which is made up of broken rock fragments and held together by mineral cement. The locality of this specimen is unknown. While quartz is a very common mineral and does not have rarity, it is an important material in industrial settings. One of it's physical and chemical properties is that it is piezoelectric, which means it can be used to generate an electric charge. This has made it useful in the manufacturing of timekeeping devices. This specimen was donated to the Burke Museum between 1868-1880 among a larger collection of geological specimens. It was collected as part of the Geological Survey of Victoria which begun in 1852 as a response to the Gold Rush. Collections were distributed to organisations across Australia to encourage the further study of the scientific makeup of the Earth. A solid egg-shaped rock with a mineral vein forming a ring around the rock in shades of brown and beige.burke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, 1852 geological survey of victoria, mineralogy, quartz, breccia, breccia conglomerate, conglomerate

Actinolite is usually found in metamorphic rocks, such as contact aureoles surrounding cooled intrusive igneous rocks. It also occurs as a product of the metamorphism of magnesium-rich limestones. Pyrite is usually found with other sulfides or oxides in quartz veins, sedimentary rock, and metamorphic rock, as well coal beds, and as a replacement mineral in fossils. Actinolite is an amphibole silicate mineral. It is named after the Greek word "aktinos" meaning “ray” in allusion to the mineral's fibrous nature. Fibrous actinolite is a type of asbestos and was once mined along Jones Creek at Gundagai, New South Wales. Pyrite or "Fool's Gold" is the most common sulfide mineral. It is named after the Greek "pyr" meaning "fire" because it can be used to create sparks needed for a fire if struck against metal or a hard surface. Due to its gold colour, pyrite can be mistaken for gold and often forms alongside it, causing small amounts of gold to be present in rocks containing pyrite. Most importantly, pyrite is an ore of gold. Pyrite is sometimes used as a gemstone but is not great for jewellery as it easily tarnishes. In some fossils of ammonites – shelled cephalopods that died ~66 million years ago – pyrite also replaces the shell. 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 small-medium-sized solid specimen with the minerals actinolite (dark green fibrous) and pyrite (brassy) with shades of brown, black/grey, and white. Actinolite is an amphibole mineral in the tremolite-actinolite series of calcium, magnesium, and iron silicates. Pyrite is an iron disulfide mineral.geological specimen, geology, geology collection, burke museum, beechworth, indigo shire, geological, mineralogy, pyrite, actinolite, victoria, sewyln, alfred selwyn