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

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

Dolomite is a mineral, calcium magnesium carbonate, with the chemical formula CaMg(CO3)2. It is a principle component of various rock types sometimes also referred to as dolomite, including dolostone, dolomitic marble and dolomitic limestone (according to the composition of each type). Dolomite rock is found in sedimentary basins throughout the world, comprising approximately 2% of the Earth's crust. It is formed when lime mud or limestone encounters groundwater containing magnesium. Dolomite can contain elements such as lead, zinc and copper. Dolomite and limestone are used in various construction, landscaping and agricultural processes. This specimen was donated to the Burke Museum in 1868 by Alfred Selwyn as part of the Geological Survey of Victoria. It was donated to the Museum in 1868. Victoria and other regions of Australia were surveyed for sites of potential mineral wealth throughout the 19th Century. The identification of sites containing valuable commodities such as gold, iron ore and gemstones in a locality had the potential to shape the development and history of communities and industries in the area. The discovery of gold in Victoria, for instance, had a significant influence on the development of the area now known as 'the goldfields', including Beechworth; the city of Melbourne and Victoria as a whole. Dolomite and limestone are mined at several locations in Victoria, including sites in the North-East of the state in Bindi and Limestone Creek. There are notable dolomite deposits in most Australian states. The dolomitised form of the mineral tends to come from older limestone deposits, formed during the palaeozoic era in marine settings, so this specimen may have come from a deposit located along a coastline in Victoria or another state. The specimen is significant as an example of surveying activity undertaken to assess and direct the development of the mineral resource industries in Victoria and Australia, as well as the movement to expand human knowledge of earth sciences such as mineralogy and geology in the nineteenth century. 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 piece of pale pink dolomite (calcium magnesium carbonate) with dark grey rim and hollowed centre. geological specimen, geology, geology collection, burke museum, beechworth, dolomite, mineralogy, geological survey, alfred selwyn, limestone, calcium magnesium carbonate

Kaolin is also known as china clay. This specimen came from Dunolly, Victoria and was donated to the Museum in 1868 as part of the Geological Survey of Victoria. This survey helped map and study the geology of Victoria. In Victoria, Kaolin is particularly used as a filler and coating material in paper manufacture. It can also be used in paints, ceramics, rubbers and plastics. There are many kaolin deposits in Victoria but many of these have been mined out and there is not much Kaolin left. Rocks that have a high amount of Kaolinite and it can be formed through the decomposition of other materials. There are two types of Kaolin; hard and soft kaolin. Soft kaolin's are coarse but have a soapy texture. It can also break easily. The hard kaolins have an earthly texture and are finer grained. This means that they are harder to break, unlike the soft kaolin. Hard kaolin's are formed by flocculation in salt water, a process that in basic terms, bonds particles together. Kaolin is a common material in Victoria and that is why it is significant. While this specimen was mined in Dunolly, Victoria Kaolin can also be found Pittong, Pakenham, Bulla, Hallam and Ballarat as well as many other places throughout Victoria. This specimen represents the presence of Kaolin deposits in this region of Australia. It is also significant because Kaolin has many uses and is largely beneficial to many manufacturing processes in Victoria. 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.Two pieces of Kaolinite mineral with shades of white and graygeological specimen, geology, geology collection, burke museum, beechworth, kaolin, china clay, dunolly, geological survey of victoria, kaolinite, victoria, mining, mining deposits, geology of victoria, australia, filler, coating material, paper manufacture, paint, ceramics, rubbers, plastics, decomposition, materials, soft kaolin, hard kaolin, flocculation, particles, salt water

Malachite is a water soluble, crystalline, triphenyl methylene chloride salt. It has a close relationship to copper because it is common for Malachite and copper to come from the same ore. Malachite often has shades of green, making it also known as Malachite Green. As a result of it's colour, it is known for being a dye and has been used in the dye industry, the textile industry and in medical fields. Cobar in New South Wales is well known for it's mining. This is because of the number of important deposits present in the area and include three important mining belts where most of the materials are found. These are the 'Cobar belt', the 'Canbelego belt' and the 'Girilambone belt'. The 'Cobar belt' runs underneath the main town. Copper was first discovered in Cobar in 1869 and since then, many deposits of other materials have been found, including Malachite.This specimen is significant because it comes from Cobar, NSW and represents the many deposits of materials found there. Cobar has a long history of mining and is a source of Australia's copper minerals. Malachite is often found in copper deposits meaning that it is representative of Cobar's copper production. Malachite is known for it's vivid green colour and as a result, has many uses, such as meaning used as a dye. This makes it a valuable material and highly significant. 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 mineral with shades of brown , white and light green throughout.geological specimen, geology, geology collection, burke museum, beechworth, malachite, copper, water soluble, cobar, cobar mines, cobar mining, cobar nsw, nsw, new south wales, mining belts, ore, copper ore, malachite green, dye, green, dye industry, textile industry, desposits, canbelego, girilambone, alfred selwyn

Amazonite is classed as a Tectosilicate and is part of the Feldspar group of minerals. Amazonite forms in a triclinic crystal structure and its chemical formula is K(AlSi3O8). In appearance, Amazonite can range from shades of green to green blue to blue, and often with white streaks or veining. The greenish colour is believed to come from the small amount of lead contained in its composition. Amazonite is named after the Amazon River due to its colour and similarities to another rock found along the riverbanks, although Amazonite is not actually found at or near the Amazon. Although less commonly used in jewellery today, Amazonite has been mined and used by humans for thousands of years and Amazonite jewellery from at least 2000BCE have been discovered in North Africa. Amazonite is found in many locations around the world including Brazil, Peru, Ethiopia, Canada, Russia, Mozambique, Myanmar, Pakistan, China, Madagascar, and the United States of America. This specimen most probably comes from the U.S.A., Amazonite is found in several US states particularly in Colorado, Virginia, Pennsylvania. This specimen is of both scientific and historic significance as a striking blue green example of Amazonite mined prior to 1868 in the United States of America, most likely from Colorado, Virginia, or Pennsylvania. These three states are all locations of significant Amazonite deposits. 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 palm-sized Feldspar mineral specimen from the Tectosilicate class in shades of blue-green with white veining.Existing label: green/blue Feldspar / "amazonite" / possibly USA geological specimen, geology, geology collection, burke museum, beechworth, tectosilicate, amazonite, feldspar, triclinic crystal structure, amazonite usa, amazonite colorado, amazonite virginia, amazonite pennsylvania

Galena is the natural compound of lead and classed as a sulphide, it crystallises in a cubic pattern and its chemical formula is PbS. Galena is a primary source of both lead and silver. This specimen of Galena comes from Broken Hill. Broken Hill has one of the world’s largest and most significant deposit of ore for the production of lead. Mining of Galena at Broken Hill began with the staking of land by Charles Rasp in 1883. By the following year, in 1884, Rasp and six others had formed Broken Hill Mining Company. Broken Hill Mining Company eventually evolved into BHP group limited and is currently the largest mining company in the world and the largest company in Australia. There is archaeological evidence from artefacts discovered in Turkey that humans have been extracting lead from galena by the process of smelting since at least 6500 BCE. This specimen also has quartz on the top surface which is frequently discovered alongside Galena. This mineral specimen is of historic significance as a sample of Galena extracted from Broken Hill during the 19th century. Mining for Galena in Broken Hill begin in 1883 by Charles Rasp and evolved into the world’s largest mining company – BHP Group Limited. Broken Hill is one of the world’s most significant deposits of ore for the production of lead. 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 flat, hand-sized, grey sulphide specimen that is the natural compound of lead with a quartz formation on the top surface. Existing Label: GALENA / (with quartz) / Locality: Broken Hill / N.S.W 120 x 70 x 29geological specimen, geology, geology collection, burke museum, beechworth, galena, galena quartz, quartz, charles rasp, broken hill mining company, bhp group limited, bhp, lead, ore, lead sulphide, sulphide, silver, broken hill

Galena occurs in a range of deposit contexts, often in metalliferous veins, such as Broken Hill, Australia; Coeur d’Alene, Idaho, United States.; Clausthal Zellerfeld, Germany; and Cornwall, England. Large deposits also replace limestone, dolomite, or occasionally organic matter, or have a contact-metamorphic origin. Galena is additionally found in cavities, brecciated (fractured) zones in limestone and chert, and in coal beds. This specimen was recovered from Broken Hill NSW and is 60% lead with 8-12 oz/silver to the ton.Galena or 'lead glance' is a grey lead sulfide and the chief ore mineral of lead. It forms isometric crystals in which the ionic lattice is similar to sodium chloride. Galena is brittle and easily weathers to secondary lead minerals, with the upper part of mineral deposits often containing cerussite, anglesite, and pyromorphite. It usually contains silver, which is mined along with its lead content. Other commercially important minerals that form in close association with galena are antimony, copper, and 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 small-sized solid specimen containing one mineral with a sparkly silver metallic lustre exterior and pastel-grey interior.geological specimen, geology, geology collection, burke museum, beechworth, galena, lead sulphide, alfred selwyn, broken hill

Malachite is a copper carbonate hydroxide mineral. It has a chemical composition of Cu2(CO3)(OH)2. It often forms within limestone where a subsurface chemical environment favourable for the formation of carbonate minerals can occur. It is a substance that can be found in many different parts of the world including: Australia, USA, Russia and the Democratic Republic of Congo. Malachite has historically been used to produce copper, with mining of the mineral dating back over a period of four thousand years. Due to its beautiful green colourations, it is also commonly used for aesthetic purposes such as in the production of sculptures and jewellery. This particular specimen was collected from the town of Burra, South Australia as part of a geological survey undertaken during the nineteenth century. The locality (located on Ngadjuri Country) has a long history of mining, particularly in copper mining, as the area is rich in copper deposits. The first significant discovery of this was made in Burra (Burra Burra Mine) in 1845 and, at the time, the mine was the largest and richest of its kind in the world, producing nearly five percent of the total world copper output. This specimen is significant as it is considered to be a rare gemstone, as many of the original deposits for the stones are significantly depleted, leaving behind very few sources. 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 palm-sized copper carbonate hydroxide mineral with patterns of green colourations Existing Label: MALACHITE / Locality: Burra / S. Aust. Other Label: Confirmed / as Malachite / C. Willman / 15/4/1 / + Bill Birch burke museum, beechworth, geological, geological specimen, malachite, gemstone, green gemstone, burra, burra burra mine, burra south australia, carbonate mineral, copper, copper mining, copper mining burra, carbonate hydroxide mineral, copper carbonate, malachite mining, malachite burra, monster mine

Arsenopyrite is one of the most common arsenic sulfide minerals, alongside orpiment and realgar. In its purest form, it becomes toxic as a result of a 46.0% arsenic makeup. Arsenopyrite occurs naturally in sulfide-bearing mineral deposits and is commonly found alongside gold deposits. This specimen was discovered in Maldon, Victoria, in the Maldon gold field. This mine is an important gold producer which was first mined in 1857. Between this initial date and 1926, 58 tonnes of gold was produced. The town of Maldon was designated Australia's first notable town, and has maintained its 19th-century appearance since the says of the gold rush. This mineral makes up a small part of the large amounts of minerals which has been excavated from the Maldon gold mines. The Maldon Goldfield alone has produced an excess of 1.7 million ounces of Australia's highest grade gold. This mineral represents not only the richness of the area, but also the significant impacts the gold rush had on the town.A solid iron arsenic sulfide mineral with shades of white, grey and blackburke museum, mineral, arsenopyrite, victoria, maldon, maldon victoria

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

Used for separating gold particles from alluvial deposits. After washing the alluvial gravel in water the gold is trapped in a ring on the side of the pan. This pan has a ring half way round the rim of the pan.Typical gold pan that would have been used in gold fields of North East VictoriaUsed gold pan. 300mm diametergold, gold pan, goldfields

According to the 1912 Department of Mines Bulletin of the Geological Survey of Victoria, basalt covers a considerable portion of the Macedon area including Mount Macedon. Basalt is the most common form of rock underlying the earth's surface and is found in three kinds of rock forming environments: ocean divergent boundaries, oceanic hotspots, and mantle plumes and hotspots beneath continents.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 mass, geological specimen in shades of grey and white. Hyalite is a colourless variety of opal. It occurs as globular and botryoidal masses and irregular crusts in volcanic and pegmatite environments where the silica deposits from the gas phase. Basalt is dark in colour, fine-grained igneous rock composed of plagioclase and pyroxene minerals. It is commonly formed as an extrusive rock, such as lava flow. It is one of the most common forms of rock underlying the earth's surface.burke museum, geological specimen, department of mines, geological survey of victoria, basalt, mount macedon, beechworth

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

This particular specimen was recovered from two hundred feet down in the Golden Mile in Kalgoorlie, Western Australia. The Golden Mile, named after the estimated sixty million ounces of gold worth around one hundred billion dollars, was the birthplace of the largest gold rush in Australia almost one hundred and thirty years ago when William Brookman and Samuel Pearce leased the Great Boulder mine. The Golden Mile is also the home of the Super Pit, Australia's most well-known mine.The majority of gold deposits will form as a native metal, however, on occasion, it can form a compound with another element, in this case, sulphur. Therefore, this specimen is a rare example of gold naturally forming into a compound mineral with sulphur. 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 gold-sulphide ore mineral specimen in shades of silver and grey with flecks of gold. Precious metals are often found in Sulphide Ores, as sulphides usually bind to these metals. They are also extremely symmetrical in crystaline form. Gold-Sulphide Ore occurs when gold forms a natural compound with other elements. In this form, gold can be present in one of two ways. It can be fully immersed in the sulphide, or a portion may be partially free. This specimen has minimal gold visible, with only a few flecks being partially visible.burke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, mineralogy, gold-sulphide ore

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

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

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

‘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

The photo depicts one shift of mine hands at Hanlon Consols Mine Rokewod in 1901. ist on the left is George Edgar Yung. George was born in Ararat the son of Yohann Godlip and Christina (b Weller)Yung. They lived at Happy Valley near Linton. and Piggoreet. Yohann was a miner and died in the All Nations Mine collapse at Derwnt Jack's in 1877. Interesting to note in the following information that the Hanlon Consol mamager, William Maughan was also the manager of the Try Again Mine in Piggoreet. He was also on the six man school committee of Piggoreet Common School No. 726. (Is this why George Yung ended up working in Rokewood because of a previous connection at Piggoreet? George married Clara Emma Smith from Happy Valley and worked in a mine at Allendale. They later moved to Yendon) About the Hanlon gold mining company near Rokewood. 1901 - Information Bendigo Prospecting Club, 21/08/2020. Information provided once again by Peter McCarthy. Christopher Hanlon had put down a line of bores south of the Rokewood main street, looking for a continuation of the Break O’Day lead which had been worked for two or three miles with highly payable results, though in a primitive manner. Ground was being paddocked 30 feet deep and made to pay. The bores suggested the sinking would be about 70 feet and a shaft site was selected at the back of Stanbrook’s Hotel. The Hanlon Gold Mining Company was formed in March 1895 and the shaft was bottomed at 68 feet, getting just over an ounce of gold from the shaft bottom. By January 1896, the poppet heads were up, and steam plant was nearly ready. The mine produced 846 oz by September, which was not as good as expected, but they installed a second puddling machine. The mine was profitable for the next three years, with periods of prospecting and the need to install steam pumps in 1897. A second shaft was sunk in 1899, which bottomed at 86 feet on good wash and was sunk on to 109 feet. 1743 oz of gold had been produced in six months to September 1899, but the No1 shaft was let on tribute as the No2 workings were opened and machinery installed the following year. The No1 shaft tributors broke even in 1900 and in 1901 the shaft was shut down, with the No1 shaft machinery sold late in 1902. By September 1901, the mine had produced gold worth £66,124 and the No2 shaft main drive was in 346 feet, with gold being found mainly in crevices in the hard floor. Mining continued, but once the No2 shaft workings met up with the old No1 shaft workings at the end of 1902 there was not much wash remaining. The mine was let on tribute in June 1903 and a drive was put in to test deeper ground. The company was wound up in February 1904 and the plant sold. From what they discovered, the manager concluded that the mine sat at the edge of an ancient coastline and the gold was in a beach deposit. The total gold production from the mine was worth £73,294. J Lee Archer JP, shareholder, was the manager of the Bank of Victoria in Ballarat. Born in Tasmania, he came to Victoria with his parents and first came to Ballarat in 1855 as a junior clerk with the bank. He died in 1902 aged 64. Alexander J. Peacock was a legal manager and a share broker. In 1897 Peacock, born in Creswick, had been elected as one of the Victorian delegates to the Constitutional Convention which wrote the Australian Constitution. He later became a politician, state treasurer and three times state premier of Victoria and was knighted KCGM. He died in 1933 aged 72. William Maughan, director, was an English miner who came to Victoria in the 1850s and became a mine manager, managing the Try Again at Piggoreet, Ryan’s Freehold and the Madam Berry, among others. He died in Williamstown in 1915 aged 85. Sepia photographRhs front of photo: R. Millist Phto & Lanternist Geelong Verso (upside down): ONE SHIFT OF MINE HANDS HANLON CONSOLS MINE ROKEWOOD 1901 Grandfather Yung 1st on left rokewood, hanlon consols mine, shift of mine workers 1901, gold mines, george edgar godlip yung, william maughan

Map included with book "Victoria: Gold and Minerals" issued by Mines Department Victoria, 1935Fold out coloured mapYellow mark indicating depositsvictoria, auriferous areas, mineral localities, department of mines, tin, antimony, copper, silver lead, tungsten, manganese, platinum, iron

Panning dishes were used for washing fine gold from river sediments or from the residue trapped in cradles and puddling tubs. They were often used on the edge of streams/rivers to sift gold from alluvial soil or crushed quartz. This simple pan would have been filled with sand and gravel which might have contained gold. The pan was submerged in the water and shaken to sort the gold from the gravel and other material, with the lighter material gradually being washed over the lip until only the heavy deposits, such as gold, remained at the bottom. (ref. Museum Victoria) This pan was used by George Henry Douglas Russell Snr. As a young man prior to his enlistment in WW1 he panned for gold using this dish. During the war he became a vet sergeant in charge of horse lines.Gold panning is the oldest and simplest method of extracting gold. Gold pans had widespread use in alluvial gold fields where water is available. This item is an example of the type of pan commonly used on Victorian gold fields.A circular dull metal panning dish which has a wide rolled top lip which tapers down to a smaller diameter for the base which is flat. The pan has been made from ironmetal which has a coating of another metal with a matte grey finish. It has a small hanging hole and a reinforcing ring all around the top.russell-doug gold-panning mining

The artefact is a white marble tile raised from the wreck of the LOCH ARD (1878). The cargo manifest of the sunken vessel has the entry “Marble £400”. This is placed directly following the entry “Glass (604 cases)”. This conjunction suggests the marble tile was originally part of a consignment intended for use in a ‘high end’ residential or public building project in the gold and wool rich Colony of Victoria. Traditionally, white or cream marble was imported into Britain from the Mediterranean region of Europe, where beds of sedimentary limestone (calcium and magnesium carbonate) had been buried over a long geological period of time. Deep in the earth’s crust, it had been subjected to immense pressures and high temperatures, sufficient to completely re-crystallise the original deposits. Marble beds began as layers of sediment at the bottom of ancient tropical seas, forming from the skeletal remains of calcareous fossils, shell, and coral fragments. The metamorphic process of prolonged compression and heating recrystallised this skeletal material, destroying all signs of the original sedimentary fabric. The resulting ‘true’ marbles of, for example, White Carrara (Tuscany, Italy), Verdi (green) Antico (Thessaly, Greece), and Rouge (red) Languadoc (Carcassone, France), were highly prized in classical decoration (sculpture and friezes) and architecture (temples and arches). Marble was found in nineteenth century Australia, but in small, uneconomic deposits, not suitable for commercial quarrying. The comparative expense of imported marble restricted its use in colonial buildings to carved fireplaces and mantel pieces, or outdoor ornaments such as fountains, statuary and grave stones. If Carrara marble floor tiles were used, they were used sparingly, as an arresting feature in entrance halls for instance. However, most prominent private and public construction used timber flooring, waxed or ‘japanned’, with carpet runners and rugs (for example the Austin’s Barwon Park Mansion, 1871), or laid tessellated and ceramic tiles of baked clay infused with colour (for example the Chirnside’s Werribee Park Mansion, 1878). HISTORY OF THE LOCH ARD The LOCH ARD belonged to the famous Loch Line which sailed many ships from England to Australia. Built in Glasgow by Barclay, Curdle and Co. in 1873, the LOCH ARD was a three-masted square rigged iron sailing ship. The ship measured 262ft 7" (79.87m) in length, 38ft (11.58m) in width, 23ft (7m) in depth and had a gross tonnage of 1693 tons. The LOCH ARD's main mast measured a massive 150ft (45.7m) in height. LOCH ARD made three trips to Australia and one trip to Calcutta before its final voyage. LOCH ARD left England on March 2, 1878, under the command of Captain Gibbs, a newly married, 29 year old. She was bound for Melbourne with a crew of 37, plus 17 passengers and a load of cargo. The general cargo reflected the affluence of Melbourne at the time. On board were straw hats, umbrella, perfumes, clay pipes, pianos, clocks, confectionary, linen and candles, as well as a heavier load of railway irons, cement, lead and copper. There were items included that intended for display in the Melbourne International Exhibition in 1880. The voyage to Port Phillip was long but uneventful. At 3am on June 1, 1878, Captain Gibbs was expecting to see land and the passengers were becoming excited as they prepared to view their new homeland in the early morning. But 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 4am the fog lifted. A man 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. 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 LOCH ARD was among the breakers and the tall cliffs of Mutton Bird Island rose behind the ship. 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 broke over the ship and the top deck was 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 had raced onto 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 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 state of exhaustion, he told the men of the tragedy. Tom 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, this time 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 LOCH ARD 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 all of 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 was washed up into what is now known as LOCH ARD Gorge. Cargo and artefacts have also been illegally salvaged over many years before protective legislation was introduced. One of the most unlikely pieces of cargo to have survived the shipwreck was a Minton porcelain peacock - one of only nine in the world. The peacock was destined for the Melbourne International Exhibition in 1880. 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 artefact and is one of very few 'objects' on the Victorian State Heritage Register. The wreck of the LOCH ARD is of State significance — Victorian Heritage Register S417 Flagstaff Hill’s collection of artefacts from LOCH ARD is significant for being one of the largest collections of artefacts from this shipwreck in Victoria. It is significant for its association with the shipwreck, which is on the Victorian Heritage Register (VHR S417). The collection is significant because of the relationship between the objects, as together they have a high potential to interpret the story of the LOCH ARD. The LOCH ARD collection is archaeologically significant as the remains of a large international passenger and cargo ship. The LOCH ARD collection is historically significant for representing aspects of Victoria’s shipping history and its potential to interpret sub-theme 1.5 of Victoria’s Framework of Historical Themes (living with natural processes). The collection is also historically significant for its association with the LOCH ARD, which was one of the worst and best known shipwrecks in Victoria’s history. A square marble tile retrieved from the wreck of the LOCH ARD. Most of its surface is covered by a thin layer of limestone and marine growth encrustation that is stained rust-red. The tile is ‘rough-worked’, cut to shape and size, but not smoothed or polished. There is a companion tile in similar condition in the Flagstaff Hill collection. From visual observation of the original surface (at low magnification) the tile appears to be of white Carrara-type marble.flagstaff 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, white marble, marble tile, carrara marble, imported marble, colonial architecture, victorian building materials

The artefact is a white marble tile raised from the wreck of the LOCH ARD (1878). The cargo manifest of the sunken vessel has the entry “Marble £400”. This is placed directly following the entry “Glass (604 cases)”. This conjunction suggests the marble tile was originally part of a consignment intended for use in a ‘high end’ residential or public building project in the gold and wool rich Colony of Victoria. Traditionally, white or cream marble was imported into Britain from the Mediterranean region of Europe, where beds of sedimentary limestone (calcium and magnesium carbonate) had been buried over a long geological period of time. Deep in the earth’s crust, it had been subjected to immense pressures and high temperatures, sufficient to completely re-crystallise the original deposits. Marble beds began as layers of sediment at the bottom of ancient tropical seas, forming from the skeletal remains of calcareous fossils, shell, and coral fragments. The metamorphic process of prolonged compression and heating recrystallised this skeletal material, destroying all signs of the original sedimentary fabric. The resulting ‘true’ marbles of, for example, White Carrara (Tuscany, Italy), Verdi (green) Antico (Thessaly, Greece), and Rouge (red) Languadoc (Carcassone, France), were highly prized in classical decoration (sculpture and friezes) and architecture (temples and arches). Marble was found in nineteenth century Australia, but in small, uneconomic deposits, not suitable for commercial quarrying. The comparative expense of imported marble restricted its use in colonial buildings to carved fireplaces and mantel pieces, or outdoor ornaments such as fountains, statuary and grave stones. If Carrara marble floor tiles were used, they were used sparingly, as an arresting feature in entrance halls for instance. However, most prominent private and public construction used timber flooring, waxed or ‘jappaned’, with carpet runners and rugs (for example the Austin’s Barwon Park Mansion, 1871), or laid tessellated and ceramic tiles of baked clay infused with colour (for example the Chirnside’s Werribee Park Mansion, 1878). HISTORY OF THE LOCH ARD The LOCH ARD belonged to the famous Loch Line which sailed many ships from England to Australia. Built in Glasgow by Barclay, Curdle and Co. in 1873, the LOCH ARD was a three-masted square rigged iron sailing ship. The ship measured 262ft 7" (79.87m) in length, 38ft (11.58m) in width, 23ft (7m) in depth and had a gross tonnage of 1693 tons. The LOCH ARD's main mast measured a massive 150ft (45.7m) in height. LOCH ARD made three trips to Australia and one trip to Calcutta before its final voyage. LOCH ARD left England on March 2, 1878, under the command of Captain Gibbs, a newly married, 29 year old. She was bound for Melbourne with a crew of 37, plus 17 passengers and a load of cargo. The general cargo reflected the affluence of Melbourne at the time. On board were straw hats, umbrella, perfumes, clay pipes, pianos, clocks, confectionary, linen and candles, as well as a heavier load of railway irons, cement, lead and copper. There were items included that intended for display in the Melbourne International Exhibition in 1880. The voyage to Port Phillip was long but uneventful. At 3am on June 1, 1878, Captain Gibbs was expecting to see land and the passengers were becoming excited as they prepared to view their new homeland in the early morning. But 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 4am the fog lifted. A man 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. 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 LOCH ARD was among the breakers and the tall cliffs of Mutton Bird Island rose behind the ship. 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 broke over the ship and the top deck was 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 had raced onto 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 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 state of exhaustion, he told the men of the tragedy. Tom 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, this time 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 LOCH ARD 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 all of 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 was washed up into what is now known as LOCH ARD Gorge. Cargo and artefacts have also been illegally salvaged over many years before protective legislation was introduced. One of the most unlikely pieces of cargo to have survived the shipwreck was a Minton porcelain peacock - one of only nine in the world. The peacock was destined for the Melbourne International Exhibition in 1880. 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 artefact and is one of very few 'objects' on the Victorian State Heritage Register. HISTORY OF THE LOCH ARD The LOCH ARD belonged to the famous Loch Line which sailed many ships from England to Australia. Built in Glasgow by Barclay, Curdle and Co. in 1873, the LOCH ARD was a three-masted square rigged iron sailing ship. The ship measured 262ft 7" (79.87m) in length, 38ft (11.58m) in width, 23ft (7m) in depth and had a gross tonnage of 1693 tons. The LOCH ARD's main mast measured a massive 150ft (45.7m) in height. LOCH ARD made three trips to Australia and one trip to Calcutta before its final voyage. LOCH ARD left England on March 2, 1878, under the command of Captain Gibbs, a newly married, 29 year old. She was bound for Melbourne with a crew of 37, plus 17 passengers and a load of cargo. The general cargo reflected the affluence of Melbourne at the time. On board were straw hats, umbrella, perfumes, clay pipes, pianos, clocks, confectionary, linen and candles, as well as a heavier load of railway irons, cement, lead and copper. There were items included that intended for display in the Melbourne International Exhibition in 1880. The voyage to Port Phillip was long but uneventful. At 3am on June 1, 1878, Captain Gibbs was expecting to see land and the passengers were becoming excited as they prepared to view their new homeland in the early morning. But 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 4am the fog lifted. A man 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. 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 LOCH ARD was among the breakers and the tall cliffs of Mutton Bird Island rose behind the ship. 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 broke over the ship and the top deck was 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 had raced onto 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 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 state of exhaustion, he told the men of the tragedy. Tom 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, this time 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 LOCH ARD 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 all of 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 was washed up into what is now known as LOCH ARD Gorge. Cargo and artefacts have also been illegally salvaged over many years before protective legislation was introduced. One of the most unlikely pieces of cargo to have survived the shipwreck was a Minton porcelain peacock - one of only nine in the world. The peacock was destined for the Melbourne International Exhibition in 1880. 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 artefact and is one of very few 'objects' on the Victorian State Heritage Register. The wreck of the LOCH ARD is of State significance — Victorian Heritage Register S417 Flagstaff Hill’s collection of artefacts from LOCH ARD is significant for being one of the largest collections of artefacts from this shipwreck in Victoria. It is significant for its association with the shipwreck, which is on the Victorian Heritage Register (VHR S417). The collection is significant because of the relationship between the objects, as together they have a high potential to interpret the story of the LOCH ARD. The LOCH ARD collection is archaeologically significant as the remains of a large international passenger and cargo ship. The LOCH ARD collection is historically significant for representing aspects of Victoria’s shipping history and its potential to interpret sub-theme 1.5 of Victoria’s Framework of Historical Themes (living with natural processes). The collection is also historically significant for its association with the LOCH ARD, which was one of the worst and best known shipwrecks in Victoria’s history. A square marble tile retrieved from the wreck of the LOCH ARD. Most of its surface is covered by a thin layer of limestone and marine growth encrustation that is stained rust-red. There is a piece of corroded iron encrusted at an oblique angle on the tile’s rear face. The tile is ‘rough-worked’, cut to shape and size, but not smoothed or polished. There is a companion tile in similar condition in the Flagstaff Hill collection. From visual observation of the original surface (at low magnification) the tile appears to be of white Carrara-type marble.flagstaff 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, white marble, marble tile, carrara marble, colonial architecture, victorian building materials

Both patients and staff were in frequent possession of passports and bank books particularly during the 20th century. These objects give an insight into people lives. The objects belonging to Miss Isabella Beatrice White are significant as they show everyday objects used by both patients and staff of Aradale Mental Hospital. British Passport - bound in thick blue material with the British Coat of Arms embossed in gold. The Passport contains 32 pages. The State Savings Bank of Victoria Book - The bank book is grey with black printed type. The Passport has both printed and hand written information and personal details. The bank book contains account details and hand written deposits and withdrawals made.bank book, passport

Bendigo Advertiser article, 4th March,1995, titled 'There is gold in them thar hills'. Reef Mining geologist Brian Cuffley and Company Chairman, Richard Sandner, are pictured discussing plans proposed for the Tarnagulla goldfield, where it is expected that '150,000 ounces of gold will be extracted from 527,000 tonnes of mineable deposits discovered at the Tarnagulla goldfield'. Colour photo shows Brian Cuffley and Richard Sandner, looking at a book titled 'Reef Mining, Tarnagulla Gold Field'. They are standing near a head frame.gold mining, bendigo, western mining, tarnagulla, reef mining company, richard sandner, brian cuffley

Robert Brough Smyth (1830-1889), civil servant and mining engineer, was born on 18 February 1830 near Wallsend, Northumberland, England, son of Edward Smith, mining engineer, and his wife Elizabeth, née Brough. On 14 November 1852 Smyth arrived in Melbourne and went to the gold diggings, where he worked as a carter on the construction of roads at Sawpit Gully. Back in Melbourne, on 7 November 1853 he became a draftsman under the surveyor-general, Andrew Clarke, and soon was acting chief draftsman. Smyth compiled numerous reports and wrote catalogues for exhibitions of minerals and fossils. In November 1869 he superintended the establishment of a museum of economic geology, mineralogy and mining and published in Melbourne The Gold Fields and Mineral Districts of Victoria … Covertly involved in the controversy that led to the disbanding of the Geological Survey in 1869, he became its director on its reinstatement in 1871; he increased its part in the search for and proving of economic mineral and coal deposits. In 1875 he became chief inspector of mines and published the geological reports on John Forrest's Western Australian exploration. On 19 June 1860 Smyth had become honorary secretary to the Board for the Protection of Aborigines and in 1863 became a voting member. Zealous and determined, he assumed the role of chairman, which belonged ex officio to the chief secretary, and wielded great power, including the dubious dismissal of John Green, general inspector of Aborigines in 1861-75 with whom he had earlier collaborated. Smyth's compilation, The Aborigines of Victoria … (1878), arose from his efforts to gather information and artefacts of Victorian Aboriginal cultures at a time when their vestiges were fast disappearing. The work, still valuable though long since superseded, relied heavily upon others such as L. Fison, G. B. Halford, A. Howitt and J. Milligan. Press reports and a petition from officers in the Mining Department accused Smyth of 'tyrannical and overbearing conduct', and in February 1876 a board of inquiry was constituted and heard evidence until April. McCoy defended 'one of the best heads of department he had ever known' but the board found the charges of 'excessive severity … in the main substantiated', and reported that Smyth had been irritable, lacking self-control and over-fastidious, but acknowledged his 'unremitting energy and zealous labours in the public service'. On 4 May Smyth resigned all public offices except his membership of the Aborigines' board. Source: Australian Dictionary of Biography. https://adb.anu.edu.au/biography/smyth-robert-brough-4621Original map printed on paper on canvas; copy of map with original. Title: Sandhurst gold field [cartographic material] / surveyed and compiled under the direction of R. Brough Smyth and Thos. Couchman, Angus Mackay ; additions made to the survey under the same direction by Regd. A.F. Murray, April 1873. "Lithd. by R. Shepherd" Topographic map of Sandhurst gold field, with relief shown by hachures. Shows roads, railways and public buildings. "Note - blocks held under leasing regulations are outlined and numbered in red" Map is also available on State Library Victoria: https://find.slv.vic.gov.au/discovery/fulldisplay?vid=61SLV_INST:SLV&search_scope=slv_local&tab=searchProfile&context=L&docid=alma994975393607636 sandhurst, goldfield, lease holdings, gullies, brough smyth, state library of victoria

Victoria will be sliced in half during the next two years by earth scientists who expect to reveal hidden mineral wealth and better understand land degradation caused by salinity. By using instruments that send vibrations into the earth, geologists will peel back the surface layers to expose a hidden landscape of buried hills, valleys and fossil streams, undiscovered gold and mineral wealth, and giant extinct volcanos. The $3 million project, called the Victorian Geotraverse, will attempt to expose the processes that shaped the state and helped form its mineral wealth. The project will be discussed at a conference, Victoria Undercover, in Benalla this week. Project leader Neil Phillips, chief of CSIRO Exploration and Mining, said the project would attempt to discover where the rest of Victoria's gold deposits might be found and where the next salinity disaster might strike. Using this process they will cut a 500-kilometre swathe through the Grampians, Bendigo, Benalla and Wodonga, curving down to Mallacoota on the far east coast. The project will involve 12 earth science agencies including the Victorian Department of Natural Resources and Environment, Geoscience Australia, the Cooperative Research Centre for Landscape, Environments and Mineral Exploration and the CSIRO. ('Age' newspaper, 28th April, 2002. https://www.theage.com.au/national/going-to-ground-for-state-secrets-20020428-gdu5tz.html Scientists will send shocks through the Victorian earth which will be reflected back and recorded on instruments that will reveal the density of the rocks below.'Australian' newspaper article, 25/26th May, 2002, 'Geologists point to gold bonanza'. Article describes the $5 million Geotraverse research in Victoria, undertaken by CSIRO geologists, that 'estimate the northern plains of Victoria conceal up to 5000 tonnes of gold'. Image on bottom of article, possibly S.T. Gill watercolour, titled 'Victorian miners pan for gold in the mid-1800's'.bendigo mining n.l., bendigo, mining, gold, csiro, geologist, geology, victorian geotraverse project