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Flagstaff Hill Maritime Museum and Village
Geological specimen - Marble, 1873-1878
The Loch Ard got its name from ”Loch Ard” a loch that lies west of Aberfoyle, and east of Loch Lomond. It means "high lake" in Scottish Gaelic. The vessel belonged to the famous Loch Line which sailed many vessels from England to Australia. The Loch Ard was built in Glasgow by Barclay, Curdle and Co. in 1873, the vessel was a three-masted square-rigged iron sailing ship that measured 79.87 meters in length, 11.58 m in width, and 7 m in depth with a gross tonnage of 1693 tons with a mainmast that measured a massive 45.7 m in height. Loch Ard made three trips to Australia and one trip to Calcutta before its fateful voyage. Loch Ard left England on March 2, 1878, under the command of 29-year-old Captain Gibbs, who was newly married. The ship was bound for Melbourne with a crew of 37, plus 17 passengers. The general cargo reflected the affluence of Melbourne at the time. Onboard were straw hats, umbrella, perfumes, clay pipes, pianos, clocks, confectionery, linen and candles, as well as a heavier load of railway irons, cement, lead and copper. There were other items included that were intended for display in the Melbourne International Exhibition of 1880. The voyage to Port Phillip was long but uneventful. Then at 3 am on June 1, 1878, Captain Gibbs was expecting to see land. But the Loch Ard was running into a fog which greatly reduced visibility. Captain Gibbs was becoming anxious as there was no sign of land or the Cape Otway lighthouse. At 4 am the fog lifted and a lookout aloft announced that he could see breakers. The sheer cliffs of Victoria's west coast came into view, and Captain Gibbs realised that the ship was much closer to them than expected. He ordered as much sail to be set as time would permit and then attempted to steer the vessel out to sea. On coming head-on into the wind, the ship lost momentum, the sails fell limp and Loch Ard's bow swung back towards land. Gibbs then ordered the anchors to be released in an attempt to hold its position. The anchors sank some 50 fathoms - but did not hold. By this time the ship was among the breakers and the tall cliffs of Mutton Bird Island rose behind. Just half a mile from the coast, the ship's bow was suddenly pulled around by the anchor. The captain tried to tack out to sea, but the ship struck a reef at the base of Mutton Bird Island, near Port Campbell. Waves subsequently broke over the ship and the top deck became loosened from the hull. The masts and rigging came crashing down knocking passengers and crew overboard. When a lifeboat was finally launched, it crashed into the side of Loch Ard and capsized. Tom Pearce, who had launched the boat, managed to cling to its overturned hull and shelter beneath it. He drifted out to sea and then on the flood tide came into what is now known as Loch Ard Gorge. He swam to shore, bruised and dazed, and found a cave in which to shelter. Some of the crew stayed below deck to shelter from the falling rigging but drowned when the ship slipped off the reef into deeper water. Eva Carmichael a passenger had raced onto the deck to find out what was happening only to be confronted by towering cliffs looming above the stricken ship. In all the chaos, Captain Gibbs grabbed Eva and said, "If you are saved Eva, let my dear wife know that I died like a sailor". That was the last Eva Carmichael saw of the captain. She was swept off the ship by a huge wave. Eva saw Tom Pearce on a small rocky beach and yelled to attract his attention. He dived in and swam to the exhausted woman and dragged her to shore. He took her to the cave and broke the open case of brandy which had washed up on the beach. He opened a bottle to revive the unconscious woman. A few hours later Tom scaled a cliff in search of help. He followed hoof prints and came by chance upon two men from nearby Glenample Station three and a half miles away. In a complete state of exhaustion, he told the men of the tragedy. Tom then returned to the gorge while the two men rode back to the station to get help. By the time they reached Loch Ard Gorge, it was cold and dark. The two shipwreck survivors were taken to Glenample Station to recover. Eva stayed at the station for six weeks before returning to Ireland by steamship. In Melbourne, Tom Pearce received a hero's welcome. He was presented with the first gold medal of the Royal Humane Society of Victoria and a £1000 cheque from the Victorian Government. Concerts were performed to honour the young man's bravery and to raise money for those who lost family in the disaster. Of the 54 crew members and passengers on board, only two survived: the apprentice, Tom Pearce and the young woman passenger, Eva Carmichael, who lost her family in the tragedy. Ten days after the Loch Ard tragedy, salvage rights to the wreck were sold at auction for £2,120. Cargo valued at £3,000 was salvaged and placed on the beach, but most washed back into the sea when another storm developed. The wreck of Loch Ard still lies at the base of Mutton Bird Island. Much of the cargo has now been salvaged and some items were washed up into Loch Ard Gorge. Cargo and artefacts have also been illegally salvaged over many years before protective legislation was introduced in March 1982. One of the most unlikely pieces of cargo to have survived the shipwreck was a Minton majolica peacock- one of only nine in the world. The peacock was destined for the Melbourne 1880 International Exhibition. It had been well packed, which gave it adequate protection during the violent storm. Today the Minton peacock can be seen at the Flagstaff Hill Maritime Museum in Warrnambool. From Australia's most dramatic shipwreck, it has now become Australia's most valuable shipwreck artifact and is one of very few 'objects' on the Victorian State Heritage Register. The shipwreck of the Loch Ard is of significance for Victoria and is registered on the Victorian Heritage Register ( S 417). Flagstaff Hill has a varied collection of artefacts from Loch Ard and its collection is significant for being one of the largest accumulation of artefacts from this notable Victorian shipwreck. The collections object is to also give us a snapshot into history so we can interpret the story of this tragic event. The collection is also archaeologically significant as it represents aspects of Victoria's shipping history that allows us to interpret Victoria's social and historical themes of the time. The collections historically significance is that it is associated unfortunately with the worst and best-known shipwreck in Victoria's history. Rectangular piece of cream coloured marble fireplace surround, with an embedded section of wrought iron in one end. Recovered from the wreck of the Loch Ard. Noneflagstaff hill, warrnambool, shipwrecked coast, flagstaff hill maritime museum, maritime museum, shipwreck coast, flagstaff hill maritime village, great ocean road, loch line, loch ard, captain gibbs, eva carmichael, tom pearce, glenample station, mutton bird island, loch ard gorge, marble fireplace, wrought iron, fireplace surround -
The Beechworth Burke Museum
Geological specimen - Galena Chalcopyrite, Unknown
... The Beechworth Burke Museum Loch Street Beechworth high ...Galena Chalcopyrite is the earth's primary ore of lead and is mined from a large number of deposits in many countries. It is also an important source of silver. Galena Chalcopyrite is one of the most abundant and widely distributed sulfide minerals across the world. The mineral is found in igneous and metamorphic rocks in medium- to low-temperature hydrothermal veins. This specific specimen was recovered from the mines in Broken Hill, New South Wales. The mines in Broken Hill were first established after Charles Rasp discovered a large amount of silver-lead-zinc ore-body in the area in 1883. BHP (Broken Hill Proprietary) mining company was then established in 1885 and quickly became the lead in Australia's mining industry after they began excavating and exporting the country's largest amount of lead, silver, and zinc. This feat generated over $100 billion in wealth for the company.Galena Chalcopyrite is signifiant as it represents the catalyst for the rise of Australia's most influential mining companies - BHP. The mineral was one of the first to be mined in the country and after being made into lead, was used for a variety of things such as paint, batteries, ammunition, and plumbing materials before it was known to be harmful to humans. 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 grey, solid hand-sized lead sulfide mineral with a silver metallic luster.burke museum, beechworth, geological, geological specimen, galena, galena chalcopyrite, chalcopyrite, broken hill, bhp, bhp mining, broken hill mine, mine, australia mine, lead, lead mine -
The Beechworth Burke Museum
Geological specimen - Feldspathic Sandstone
... feldspathic sandstone burke museum geology geological geological ...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 -
The Beechworth Burke Museum
Geological specimen - Ilvaite
Ilvaite has acquired its name from Ilva (Latin for Elba) Island, Greece, where Ilvaite is most commonly found. The geological setting in which Ilvaite occurs is through contact with magnetite, zinc and copper ore deposits, along with contact metamorphic deposits and zeolite zones. llvaite crystallizes in the form of black prismatic crystals and columns . This specimen was retrieved from Broken hill, known as the world's richest and largest zinc-lead ore deposit. Because of Ilvaite's often unaesthetic crystal formations compared to other minerals, Ilvaite is uncommon in most rock collections, particularly specimens that are not well formed, such as this one. Ilvaite is also a member of the Sorosilicate subclass of the silicate minerals, which have an unusual basic unit of Si2O7, making Ilvaite a unique mineral. Given that Ilvaite is not commonly found in Australia, it marks a unique contribution to an Australian collection of minerals. 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 hand-sized ferrous iron analogue mineral with of black with shades of beige Ilvaite is a brittle, opaque rock formation that has acquired its name from Ilva (Latin for Elba) Island, Greece, where Ilvaite is most commonly found. The geological setting in which Ilvaite occurs is through contact with magnetite, zinc and copper ore deposits, along with contact metamorphic deposits and zeolite zones. llvaite crystallizes in the form of black prismatic crystals and columns rock, mineral, ilvaite, ilvaite specimen -
The Beechworth Burke Museum
Geological specimen - Loellingite in Rhodonite
... The Beechworth Burke Museum Loch Street Beechworth high ...Rhodonite is a reddish-pink manganese silicate material and often contains iron, magnesium and calcium. It is usually found in metamorphic rocks (rocks which have been altered by heat, pressure or chemical process). It can range in size from tiny to massive. Because of their composition they are not suitable for use in jewellery because they are hard enough. It is quite rare to find, though has been found in Australia, North America, South America and Europe.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. This specimen is a palm shaped piece of loellingite within rhodonite. It is mostly reddish-pink coloured, with flecks of light and dark grey. Loellingite is a grey iron arsenide which often forms into crystal shapes. It is mostly found in mesothermal veins (caused by immense heat) with sulfides or in limestone. It is toxic when heated or struck. rhodonite, loellingite, burke museum, beechworth, geological survey of victoria -
The Beechworth Burke Museum
Geological specimen - Copper Ore
This specimen was recovered from Silverton Mine in Broken Hill, New South Wales. Otherwise known as the 'Day Dream Mine', the Silverton Mine was first established in 1883, when silver and lead deposits where discovered. Within a few short years, the population of Broken Hill reached 3000 people. As of today the Silverton Mine is still open, and has produced over 200 million tonnes of ore, which has generated over $100 billion. The Silverton Mine was also famous for a number of specimens such as silver, iron and zinc.Copper is considered to be a rare ore in that finding it in its pure form is rare. Nowadays when mining for Copper it is often found in mixed in with other minerals or it is recycled from use. Moreover, Copper is found in a range of everyday uses such as coins, cookware, pipes, heating conductors and anything that generate electricity. The fact that Copper is heat a heat conductor, electricity conductor and it does not corrode easily, makes this ore a versatile and useful. 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 hand-sized cube-shaped sulfide and oxide with shades of green, grey and brown throughout. Copper is typically found as nuggets in the ground. It can be found in a range of forms such as its native state; mixed with other ores, such as zinc and iron; as porphyry copper deposits; and as major deposits. Porphyry deposits are when the mineral is scattered evenly throughout the rock. Major deposits are when the mineral is scattered amongst other minerals.burke museum, beechworth, indigo shire, beechworth musum, geological, geological specimen, mineraology, copper, copper ore, copper ore speciment, broken hill, new south wales -
The Beechworth Burke Museum
Geological specimen - Basalt, Unknown
... further study. burke museum Beechworth Geological Specimen geology ...Basalt is a common igneous rock that composes most of the Earth's surface and can be found on the Moon and other rocky planets of the Solar System. It is generally composed minerals such as calcic plagioclase, clinopyroxene and iron ore which form grains that are indistinguishable to the naked eye. It can be dark grey or black in colouring and sometimes may contain holes left by gas bubbles. Most of the Earth's basalt was produced in environments such as oceanic divergent boundaries, oceanic hotspots, and mantle plumes and hotspots beneath continents. Basalt is commonly used in construction where it is crushed and used for multiple purposes such as concrete aggregate, road base, or railroad ballast. Thin slabs of basalt can also be cut and used for floor tiles, stone monuments, and building veneer. This particular specimen was excavated from Talbot in Victoria, which was a small gold mining town established in 1852. As basalt is a common rock, it is not specific to Talbot. However, this specimen can be assumed to be of the Cainozoic age due to previous geomorphic surveys of the area. This particular type of Basalt was used mainly for roads due to the durability of the rock.Basalt holds significance due to the continued use of the rock from historic until present times. The rock has been utilised for many types of construction and is still used for the same purposes today. Basalt also has significance to the Earth and other rocky planets of the Solar System as it makes up most of the planet's surface. 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 smaller than hand sized rock specimen which is dark grey in colour with small holes and white deposits across its surface.Geological survey / [illegible] /burke museum, beechworth, geological specimen, geology, basalt, basalt specemin, indigo shire, talbot, cainozoic, igneous rock -
The Beechworth Burke Museum
Geological specimen - Chalcopyrite
... indigo shire beechworth museum geology geological specimen ...This specimen originated from Mount Lyell on the west coast of Tasmania, where a large group of open cut and underground copper-silver-gold mines began operating in 1883. Between 1893-1994, the Mt Lyell Mining and Railway Company were responsible for operations. The Mt Lyell copper-gold mines produce some excellent crystallised specimens of chalcopyrite and other minerals. The deposits are generally considered to be of Cambrian volcanic origin, but there are indications of Devonian granitic influence on the ores, plus local remobilisation during Devonian deformation. Over 120 million tonnes of ore was produced from several workings, including the main Prince Lyell mine and the North Lyell mine, which was also of great importance. The Mount Lyell mines have a long history of human and environmental disasters, including the 1912 North Lyell fire that killed 42 miners, and two separate incidents in 2013 in which three people lost their lives. The environmental impacts from this complex of mines are extensive, with waste tailings and heavy metal contamination flowing directly into the King and Queen River catchments. In 1954, the eminent Australian historian, Geoffrey Blainey, published 'The Peaks of Lyell' which delves into the history of the 1912 North Mount Lyell Disaster.Chalcopyrite does not contain the most copper in its structure relative to other minerals, but it is the most important copper ore since it can be found in many localities and occurs in a variety of ore types. The brassy-yellow colours in Chalcopyrite mean it is often confused with pyrites and gold, leading to use of the term, "fool's gold." Chalcopyrite has been the primary ore of copper since smelting began five thousand years ago. 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.This hand sized solid mineral specimen has shades of brass-yellow with spots of iridescent green-black tarnish. Chalcopyrite is a copper iron sulphide mineral and a major ore of copper common in sulphide veins and disseminated in igneous rocks. Chalcopyrite has a hardness of 3.5-4 on the Mohs Scale. It is a member of the tetragonal crystal system and has metallic lustre and opaque transparency.burke museum, beechworth, indigo shire, beechworth museum, geology, geological specimen, chalcopyrite, copper pyrites, copper mining, tasmanian geology, mount lyell, mount lyell mines, fools gold, mohs scale, crystals, minerals, historical geological collection, victorian geological survey, a.r.c selwyn, gold rush, van diemans land -
The Beechworth Burke Museum
Geological specimen - Chalcedony
... further study. burke museum beechworth geological geological ...This specimen was recovered from Philip Island in Victoria. Chalcedony is composed of Quartz and Silicon Dioxide represented as SIO2. It has and is still used as a gemstone for thousands of years. This is an excellent specimen Chalcedony that shows its aesthetic 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. Uniquely shaped piece of Chalcedony with opening in the centerburke museum, beechworth, geological, geological specimen -
The Beechworth Burke Museum
Geological specimen - Rhodonite with Galena and Sphalerite
... The Beechworth Burke Museum Loch Street Beechworth high ...This specimen is from Broken Hill, NSW. Galena is a natural mineral form of lead sulphide and is often found associated with sphalerite, calcite, and fluorite. Galena is an important lead ore mineral, and, in some regions, it is also an important mineral associated with silver ore. Sphalerite is a sulphide mineral that is the main ore of zinc. Rhodonite is an uncommon mineral once used as an ore of manganese in India, however today the scarcity and fragility of the crystals mean it is primarily used as lapidary materials or mineral specimens. In 1883, Charles Rasp who was a boundary rider at the time, discovered what he thought were deposits of tin but were in fact samples of silver and lead. He and six others went on to set up the first mining company in Broken Hill (BHP). The ore body became the largest and richest of its kind in the world mining ore worth more than 42,000 pounds in its first year. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study. Galena contains lead and silver, Sphalerite contains zinc. 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 piece of Sphalerite and Galena with Rhodonite crystalsburke museum, beechworth, geological, geological specimen, galena, rhodonite, sphalerite, silver ore, manganese, lead sulphide, lead ore, zinc ore, lapidary, mineral specimen, broken hill, nsw -
The Beechworth Burke Museum
Geological specimen - Mangan Hedenbergite
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 -
The Beechworth Burke Museum
Geological specimen - Fossiliferous Mudstone, Unknown
This specimen was found in Cape Patterson, Vic. Cape Paterson is a cape and seaside village located near the town of Wonthaggi, 132 kilometres southeast of Melbourne, in the Bass Coast Shire of Gippsland, Victoria, Australia. These dark, fossiliferous Mudstones were deposited in slow-moving water associated with sedimentary basins & continental shelves. They are rich in carbon which makes them almost black. This is typical of an anoxic, reducing environment such as deep water or stagnant conditions where carbon-rich material would remain unoxidised during subsequent deposition & diagenesis. it has an imprint of a leaf in the rock itself, displaying the fossil of the plant. This specimen is unique due to the leaf impression within the stone itself. Imprint fossils are formed from an organism moving in some way, leaving behind a trace or track. These tracks are preserved when the clay/silt dries slowly and is covered by other sediment. Plants can also leave imprint fossils when they are covered by sediment. The leaf tissue degrades, leaving an imprint of where the leaf once was. 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.These dark, fossiliferous Mudstones were deposited in slow moving water associated with sedimentary basins & continental shelves. They are rich in carbon which makes them almost black. This is typical of an anoxic, reducing environment such as deep water or stagnant conditions where carbon rich material would remain unoxidised during subsequent deposition & diagenesis. FOSSILIFEROUS MUDSTONE / Locality: Cape Patterson, Victoria | Descriptive catalogue / Pg 27 No 95 / "Grey Clay, / Cape Paterson with leaf impressions' / 15/4/21 C. William /mudstone, cape patterson, leaf imprint, fossilised leaf, fossiliferous mudstone -
The Beechworth Burke Museum
Geological specimen - Granodiorite, Unknown
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 -
The Beechworth Burke Museum
Geological specimen - Slate (Metamorphic), Unknown
... further study. burke museum beechworth geological slate ...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 -
The Beechworth Burke Museum
Geological specimen - Chalcopyrite, Unknown
This specimen was recovered from Mica Schist, Canada. Chalcopyrite is a copper iron sulfide mineral with a chemical composition of CuFeS2. Its name derives from the Greek words for copper (chalco-) and brass (pyrite). It can be found in shades of yellow, green and grey, and, when exposed to acid, it can change to purple, blue, violet and yellow tones. Weathering can cause loss of its metallic luster and its brass-yellow colour. Chalcopyrite forms under various conditions, with the most significant deposits being hydrothermal in their origin. It is known globally as the most important ore of copper for thousands of years, and is thus considered a very important mineral formation. Given its golden appearance, it is often confused for the mineral gold, earning it the popular reputation as 'fool's gold' or 'yellow copper'. However, it can be straightforwardly distinguished from gold; the latter is soft, with higher specific gravity and a yellow streak, whereas chalcopyrite is brittle, easily scratched by a nail, and has a greenish grey streak. Copper was the first metal that was used by people. It was discovered by the Neolithic man about 9,000 years ago and it gradually replaced stone as it was easier to be shaped. In Australia, search for copper began after the European settlement, leading to the discovery of substantial deposits, like the one at the Olympic Dam in South Australia, which is regarded as one of the largest copper deposits in the world. Chalcopyrite has been used for copper since smelting processes began approximately five thousand years ago. Although by no means rare, this the specimen of this mineral can be used to reflect a wider history of industrial uses of copper for a significant portion of human 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 solid hand-sized copper iron sulfide mineral of brass yellow, often with an iridescent tarnish, with greenish-black streak and submetallic luster. Chalcopyrite can be formed in several ways, including crystalizing from accessory minerals in igneous rocks, or from magma or within volcano sulfide deposits. Most commonly, chalcopyrite are found in hydrothermal conditions, where it forms in hydrothermal veins. As a member of the tetragonal crystal system, it often takes the shape of tetra-headed crystals, often with striations along the sides of the crystals. #18 Copper pyrites/(chalcopyrite) in/Laurentian Slate/(page 315 of inventory)/page missing from/descriptive catalogue/ Other label: 81 /fool's gold, chalcopyrite, mineral, rock, geology, geological, hydrothermal, neolithic, european settlement, olympic dam, south australia, stone, deposits, specific gravity, greenish grey streak, brittle, mineral gold, metallic luster, cufes2, greek words -
The Beechworth Burke Museum
Geological specimen - Greenstone / Gabbro, Unknown
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 -
The Beechworth Burke Museum
Geological specimen - Ropy Lava
‘Ropy lava’ is known for its sculptural and layered qualities. It occurs in specific lava flows that are slow moving and slow cooling, allowing for unique formations to be created out of the motion. Ropy Lava is a flow that has a hardened crust with molten material underneath, the tension between these states is what creates its characteristic form. The brown/red hue of the stone is an indication of age, as it is oxidised iron deposits. This rock deposit is thought to be sourced from the area by Talbot, in western Victoria. This area has a rich mineral history and experienced the gold rush in the 1850's. The traditional owners of this area are the Dja Dja Wurrung people.This geological specimen shows the conditions in which the Australian landscape was created as well as provides an indication as to how these events occurred. It is representative of a common natural process that contextualises the formation of Australia with the formation of other landmasses. 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.Hand sized specimen in brown/red hues42 / victoria, talbot, lava, ropy, ropy lava, mineral, geological specimen, geological, geological heritage, natural stone, natural history -
Eltham District Historical Society Inc
Book, Andrew Ross Museum, Kangaroo Ground: its Land and its People by Mick Woiwod published by Andrew Ross Museum, 2002
Kangaroo Ground's geology, original people, European settlers, plants used by Wurundjeri people26 leaves : ill., maps ; 30 cm.wurundjeri (australian people) -
Tatura Irrigation & Wartime Camps Museum
Document, Geological Plan, Eildon Dam Site, 1945
To record details of geological aspects of EildonA series of maps illustrating rock formations etc., locations, boundaries and planswater/irrigation, documents, maps -
Moorabbin Air Museum
Poster (Item) - Geology of America's north west, The shaping of a continent (USA)
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Koorie Heritage Trust
Journal - Serials, Birdsell, Joseph B. et al, Records of the Queen Victoria Museum Launceston. Contents - The racial origins of the Extinct Tasmanians. A survey of possible sea routes available to the Tasmanian Aborigines. The Tasmanians - a summary, 1949
Some of the points raised seem rather dated, but an interesting set of theories historically.105-145P.; plates; refs. figs.Some of the points raised seem rather dated, but an interesting set of theories historically.tasmanians - racial origins., australian aboriginals - origins., migration theories - tasmanians., bass strait - geology. -
Port Fairy Historical Society Museum and Archives
Postcard, A.C. Aberline, The Crags
This photograph is of “The Crags” an area on the coast half way between Port Fairy and Yambuk. The name is an abbreviation of McKechnies Craigs/Crags owners of property in the vicinity. it is close to ancient aboriginal campsites but these are not accessible to the public. Because of the nature of the geology in this area this photograph shows a seascape that it is not possible to see now.Hand coloured photograph used as postcardThe Crags Port Fairyseascape, sea, beach, the crags, mckechnie’s crags or craigs -
Port Fairy Historical Society Museum and Archives
Book, James Bonwick, Western Victoria It’s geography geology and social condition. The Narrative of an Educational Tour in 1857
1857 tour of Western Victoria including Tower Hill, Belfast and Yambuk.non-fiction1857 tour of Western Victoria including Tower Hill, Belfast and Yambuk.colonial education, belfast, victoria 1857, book -
Flagstaff Hill Maritime Museum and Village
Geological specimen - Slate Roof Tiles
These rectangular slates of 'beautiful, unusual, expensive, green' American roof tiles were recovered from the wreck of the Falls of Halladale. Salvaging began in 1974 by volunteer divers, using local cray-fishing boats. An efficient system was devised to recover up to 4,000 of the still neatly packed slates a day. Many of the 22,000 salvaged slates can be seen on the roofs of eight Flagstaff Hill Maritime Village buildings. The iron-hulled, four-masted barque, the Falls of Halladale (1886 - 1908), was a bulk carrier of general cargo. She left New York in August 1908 on her way to Melbourne and Sydney. In her hold, along with 56,763 tiles of unusual beautiful green American slates (roof tiles), 5,673 coils of barbed wire, 600 stoves, 500 sewing machines, 6500 gallons of oil, 14400 gallons of benzene, and many other manufactured items, were 117 cases of crockery and glassware. Three months later and close to her destination, a navigational error caused the Falls of Halladale to be wrecked, grounded on a reef at Wreck Point, midway between Peterborough and the Bay of Islands, during the night of 14th November 1908. The captain and 29 crew members all survived, but her valuable cargo was largely lost, despite two salvage attempts in 1908-09 and 1910. The ship stayed in full sail on the rocky shelf for nearly two months, attracting hundreds of sightseers who watched her slowly disintegrate until the pounding seas and dynamiting by salvagers finally broke her back, and her remains disappeared back into deeper water. The shipwreck is a popular site for divers, about 300m offshore and in 3 – 15m of water. Some of the original cargo can be seen at the site, including pieces of roof slate and coils of barbed wire.The American slate tiles are significant as an example of cargo imported for use as building materials in Australia. The Falls of Halladale shipwreck is listed on the Victorian Heritage Register (No. S255). She was one of the last ships to sail the Trade Routes. She is one of the first vessels to have fore and aft lifting bridges. She is an example of the remains of an International Cargo Ship and also represents aspects of Victoria’s shipping industry The wreck is protected as a Historic Shipwreck under the Commonwealth Historic Shipwrecks Act (1976).Bundle of slate roof tiles (18); rectangular, green American slate roof tiles, some with red-brown stains. Two tiles both have two holes drilled through them. Two different tiles are thicker than the others. The tiles were salvaged from the wreck of Falls of Halladale. flagstaff hill, warrnambool, maritime village, maritime museum, shipwreck coast, great ocean road, cargo, slate, slate tile, green american slates, building material, wreck point, peterborough, bay of islands, russell & co., 1908 shipwreck, salvage, recover -
Federation University Historical Collection
Booklet, Ballarat School of Mines Annual Report, 1901
In 1901 Andrew Anderson was President of the Ballarat School of Mines. At the height of its world wide fame the annual report states: 'That the public recognises and appreciates the importance of the School, is evident by the large additions to the class rolls - (many of the students have come long distances, from England, India, South Africa, new South Wales, Queensland, West Australia, South Australia and Tasmania,) which give ample proof, if such were necessary, of the wide spread reputation of the School.'8 page booklet relating to the Ballarat School of Mines in the year 1901. It includes information on: Alfred Johnston's death during the Boer War, Thomas Bath's bequest to the Ballarat School of Mines, resignation of Theophilus Williams from the School Council, appointment of Richard Maddern and Isaiah Pearce to the School Council, Associateship courses, New mining metallurgical laboratory and a statement of receipts and expenditure ballarat school of mines, andrew anderson, thomas bath, alfred gresham johnston, boer war, rhenoster kop, south africa, richard maddern, isaiah pearce, salariesmining laboratory, metallurgical laboratory, wynne tables, tregurtha tables, halley's percussioina tables, wilfley concentrator, spitzkasten, jig, linkenback table, chilian mill, amalgamator, model agitation plant, slime vats, alfred mica smith, william gurr, thomas hart, museum, fees, mining plant, model mine, allendale excursion, daylesford excursion, botanical excursion, geological excursion, melbourne excursion, itonworkers' association -
Federation University Historical Collection
Booklet, The School of Mines, Ballaarat, Annual Report 1881, 1882
The School of Mines Ballaarat Annual Report 1881. Annual Report, Additional Examination Statute, Certificates Granted by the Council, Copy of letter received from the Honble. Francis Ormond, M.L.C., Extracts from the Visitors' Book, Fees, Form of Bequest, Life Governors, Museum - open to Visitors', Office Bearers, Paper of Particulars, Report of the Curator of the Museum and Library (with plans), Report of the Superintendent of Laboratories, Report of the Lecturer in Telegraphy, Report of the Lecturer in Mechanical Engineering, Statement of Receipts and Expenditure for the year 1881, Subjects and Lecturers, Subjects and Examiners, Subscriptions and Donations from 1st January to 31st December 1881, The Lignite Deposit at Skipton (with Section and Plan)Soft covered pale green booklet of 63 pages.annual report, additional examination statute, certificates granted by the council, copy of letter received from the honble. francis ormond, m.l.c., extracts from visitors' book, fees, form of bequest, paper of particulars, life governors, museum, officer bearers, report of the curator of the museum and library, report of the lecturer in telegraphy, report of the lecturer in mechanical engineering, statement of receipts and expenditure for the year 1881, subjects and lecturers, subjects and examiners, subscriptions and donations from 1st january to 31st december 1881, the lignite deposit at skipton, james oddie, esq., j.p., alf. mica smith, lecturer in chemistry, natural philosophy and botany, f. m. krause, lecturer in geology, scientific mining, land, mining and engineering surveying, t. h. thompson, lecturer in practical mining, w. h. shaw, lecturer in mechanical engineering, h. reid, lecturer in mechanical engineering, a. a. buley, lecturer in mathematics, w. d. campbell, lecturer in telegraphy, j. f. usher, lecturer in materia medica, pharmacy and physiology, a.a. buley, w.d. campbell, j.f. usher, w.h. shaw, ferdinand krause, t.h. krause, skipton lignite deposit, skipton coal, ballarat school of mines annual report -
Federation University Historical Collection
Booklet, A. A. Herberte, "STAR' Printing Works, The School of Mines, Ballaarat, Annual Report 1884, 1885
The School of Mines Ballaarat Annual Report 1884. Annual Report, Balance Sheet, Certificates Granted by the Council, Examination Papers - Elementary Science Classes (Appendix), Fees, Honorary Correspondents, Life Governors, Museum - open to Visitors', Office Bearers, Report of the Curator of the Museum and Library, Report of the Lecturer in Mathematics, Report of the Lecturer in Mechanical Engineering, Report of the Lecturer in Electricity and Magnetism, Report of the Lecturer in Telegraphy, Report of the Lecturer in Botany, Report of the Lecturer in Materia Medica and Physiology, Report of the Lecturer in Astronomy, Scale of Charges for Assays and Analyses, Examinations Held, Statement of Receipts and Expenditure for the year 1884, Statement of Receipts and Expenditure for Special Funds, Subjects and Lecturers, Subjects and Examiners, Subscriptions and Donations from 1st January to 31st December 1884, Time TableSoft covered pale green booklet of 67 pages. The Ballarat School of Mines Annual Report for 1984.annual report, balance sheet, certificates granted by the council, examination papers - elementary science, fees, honorary correspondents, life governors, museum, officer bearers, report of the curator of the museum and library, report of the lecturer in telegraphy, report of the lecturer in mechanical engineering, report of the lecturer in astronomy, scale of charges for assays and analyses, examinations held, statement of receipts and expenditure for the year 1884, statement of receipts and expenditure for special funds, subjects and lecturers, subjects and examiners, subscriptions and donations from 1st january to 31st december 1884, time table, james oddie, esq., j.p., alf. mica smith, lecturer in chemistry, natural philosophy and botany, f. m. krause, lecturer in geology, scientific mining, land, mining and engineering surveying, t. h. thompson, lecturer in practical mining, j. sommers, lecturer in mechanical engineering, h. sutton, lecturer in mechanical applied electricity and magnetism, a. a. buley, lecturer in mathematics, w. d. campbell, lecturer in telegraphy, j. f. usher, lecturer in materia medica, pharmacy and physiology, geo. day, lecturer in botany, john wall, lecturer in astronomy, subscriptions, fonations, telegraphy, henry sutton, usher, george day -
Federation University Historical Collection
Booklet, W. B. Macdonald, The Ballarat School of Mines, Industries and Science, Annual Report 1890, 1890
The Ballarat School of Mines Annual Report 1890. Annual Report, Crown Grant, Affiliation Statute, Constitution, Examination Statutes, Associateship of The School, Department of Agriculture, Certificates Granted by Council, Fees, Form of Bequest, Gauge-Testing Apparatus, General Balance Sheet and Liabilities and Assets, Honorary Correspondents, Life Governors, Meteorological Observations, Number of Students attended The School of Mines, Office Bearers, Report of the Professor of Mineralogy and Geology and Curator of the Museum, Report of the Superintendent of Laboratories, Report of the Lecturer on Engineering and Surveying, Report of the Lecturer on Geometrical and Freehand Drawing, Report of the Lecturer on Telegraphy, Report of the Lecturer on Botany, Report of the Lecturer on Materia Medica and Physiology, Report of University Classes, Examinations Held, Scale of Charges for Assays and Analyses, Statement of Receipts and Expenditure for the year 1890 and Special Trust Funds, Statistics - Students attending Lectures, Subjects and Examiners, Subscriptions and Donations from 1st January to 31st December 1890, Time TableThe Ballarat School of Mines annual Report, 1890. Cover is browning around the edges, back cover partly detached and is torn, 184 pages. ballarat school of mines, annual report, andrew anderson j.p. - president (acting) and vice president, rivett henry bland - trustee, the hon. sir w. j. clarke - trustee, the hon. john warrington rogers - trustee, james oddie - trustee, the hon. henry cuthbert - honorary solicitor, i. j. jones - honorary treasurer, chas. kent - auditor, andrew berry - registrar, f. m. krause - professor of mineralogy and geology, and curator of the museum, alf. mica. smith - superintendent of laboratories, mr e. wattis - manager, mining laboratory, j. h. horwood - lecturer on engineering and surveyin, h. j. hall - lecturer geometrical and free-hand drawing, george day - botany, j. f. usher - materia medica and physiology, miss bella guerin - university classes, charles kent - auditor, henry krone - assistant registrar of titles, henry b. loch, d. e. martin - secretary for agriculture, r. hedger wallace - department of agriculture -
Federation University Historical Collection
Booklet, Berry Anderson & Co, The Ballarat School of Mines, Calendar and Annual Report 1894, 1894
The Ballarat School of Mines Calendar and Annual Report 1894. Associateship of The School, Calendar for 1894, Certificates Granted by the Council 1893, Comparative Statement of Receipts and Expenditure, Departmental Expenditure, Examiners, Examination Papers, Examination Fees, Fees, Honorary Correspondents, Life Governors, Meteorological Observations, Mining Engineering Scholarship, Number of Certificates Granted since Inception, Number of Students attended The School of Mines, Office Bearers, Plant and Appliances, Practical Treatment of Ores, Professors and Lecturers, Report of the Professor of Mineralogy and Geology and Curator of the Museum, Report of the Superintendent of Laboratories, Report of the Lecturer on Engineering and Surveying, Report of the Lecturer on Mathematics, Report of the Instructor in Mechanical Drawing and Machine Construction and Design, Report of the Lecturer on Electrical Engineering and Telegraphy, Report of the Lecturer on Geometrical Model and Perspective Drawing, Report of the Lecturer on Botany, Report of the Lecturer on Biology, Pharmacy, Materia Medica, Scale of Charges for Assays and Analyses, State School Science Classes, Statement of Receipts and Expenditure for year 1893 and Serjeant Scholarship Fund, Statistics - Student attending Lectures, Subscriptions and Donations, Syllabus of Lecture Courses, Time TableThe Ballarat School of Mines Calendar and Annual Report, 1894. Green soft cover, 116 pages. ballarat school of mines, annual report, andrew anderson j.p. - president, f. j. martell - vice president, r. denham pinnock - vice president, rivett henry bland - trustee, the hon. sir w. j. clarke - trustee, the hon. john warrington rogers - trustee, james oddie - trustee, the hon. henry cuthbert - honorary solicitor, r. g. middleton - honorary treasurer, charles kent - auditor, andrew berry - registrar, professor alf. mica smith - chemistry, metallurgy, natural philosophy, professor krause - geology, mineralogy, principles of mining, professor j. h. horwood - mine and land surveying, mining mechanics, hydraulics, civil engineering, applied mechanics, j. a. dawson - electrical engineering, d. walker - chemistry and natural philosophy, w. e. bennetts - mathematics, henry j. hall - freehand and perspective drawing, a. e. c. kerr - mechanical drawing, george p. day - botany, e. gutheil - paleontology, zoology, materia medica, w. d. snowball - veterinary science -
Federation University Historical Collection
Booklet, Berry Anderson & Co, The Ballarat School of Mines, Calendar and Annual Report 1895, 1895
The Ballarat School of Mines Calendar and Annual Report 1895. Associateship of The School, Calendar for 1895, Certificates Granted by the Council 1894, Certificates Granted by the Education Department 1893, Comparative Statement of Receipts and Expenditure, Departmental Expenditure, Examiners, Examination Papers, Examination Fees, Fees, Honorary Correspondents, Life Governors, Meteorological Observations, Number of Students attended The School of Mines, Obituary, Office Bearers, Practical Treatment of Ores, Professors and Lecturers, Report of the Professor of Mineralogy and Geology and Curator of the Museum, Report of the Superintendent of Laboratories, Report of the Lecturer on Engineering and Surveying, Report of the Lecturer on Mathematics, Report of the Instructor in Engineering and Machine Construction and Design, Report of the Lecturer on Electrical Engineering, Report of the Lecturer on Geometrical Model and Perspective Drawing, Report of the Lecturer on Botany, Report of the Lecturer on Palaeontology, Materia Medica and Mining Ambulance, Scale of Charges for Assays and Analyses, Statement of Receipts and Expenditure for year 1894, Statistics - Student attending Lectures, Subscriptions and Donations, Syllabus of Lecture Courses, Time TableThe Ballarat School of Mines Calendar and Annual Report, 1895. Pale brown soft cover, 90 pages. ballarat school of mines, annual report, andrew anderson j.p. - president, f. j. martell - vice president, r. denham pinnock - vice president, the hon. sir w. j. clarke - trustee, the hon. john warrington rogers - trustee, the right reverend samuel thornton - trustee, andrew anderson - trustee, james millhinch - trustee, james oddie - trustee, the hon. henry cuthbert - honorary solicitor, r. g. middleton - honorary treasurer, charles kent - auditor, andrew berry - registrar, professor alf. mica smith - chemistry, metallurgy, natural philosophy, professor krause - geology, mineralogy, principles of mining, professor g. j. dawbarn - mine and land surveying, mining mechanics, hydraulics, civil engineering, applied mechanics, j. rowe - practical mining, j. a. dawson - electrical engineering, d. walker - chemistry and natural philosophy, w. e. bennett - mathematics, henry j. hall - freehand and perspective drawing, a. e. c. kerr - mechanical drawing (machine construction and design), george p. day - botany, e. gutheil - paleontology, zoology, materia medica, rivett henry bland - obituary, george gant scott - obituary, fiddian, bennett, r. allan, dawbarn, rosales, krause, joseph bryant, matthews, j. robinson, andrew robertson, john lynch, jonathan robinson, a.e.c. kerr, alfred mica smith, frederick mccoy, j. cosmo newberry, blackett, elelry, arnot, robert allan, bickett, kent, martin, mitchell, ferdinand von mueller, rivett henry bland, thomas bath, john rowe, museum, andrew anderson, george day, subscriptions and donations, examination papers