Brick house for auction 23 November 1996Pamphlet on the auction of a house in Vermont auctions, orion street, vermont, no 13

A fund-raising card explaining the donation of 'Bethany', the property of Miss 'Birdie' Kirkpatrick, 10 Orion Street Vermont as a site for homes for elderly people in 1969. The card depicts an illustration of 'Kirkpatrick'kirkpatrick homes, kirkpatrick, birdie, miss, vermont elderly peoples homes, faggetter, pat, orion street, vermont no. 10, mitcham community opportunity shop

Drawing by Bette Jones, the sketch was on the front of greeting sold to raise funds for Vermont Elderly Peoples Homes.Sketch of Miss Kirkpatrick's Home, 10 Orion Street, Vermont.kirkpatrick, miss, jones. bette, vermont elderly peoples homes

Article on the development plan of the Hale Estate, Mitcham.Article on the development planhale estate, mitcham, glenburnie road, orion street, vermont, grey street, malvern street, land subdivision

The Spring Gully Gold Mining property consists of Gold Mining Lease No. 2986, Castlemaine, of about 21 acres situated on the Emu Reef, in Spring Gully Fryers. There are two shafts, distant about 300 feet from each other. From one of them large quantities of gold were obtained in former years by previous companies. ( Prospectus of the Spring Gully Mining CompanyMaroon hard cover book, brown leather binding on spine and corners, three hundred and eighty pages. Written on spine of book in gold leaf : 'Minute Book'. Handwritten minute entries from 14th September 1903 to 30th August 1915. Affixed to first page, newspaper clipping from the 'Herald' 13/9/05, with information about the Spring Gully Mine Fryerstown. Page eighty-one has two quotes affixed from 'The Yarraville Chlorination and Ore Reduction Works' High Street Yarraville, July 1905, for works associated with pyrites and blanket sand. Page nine, a handwritten letter affixed to minutes, applying for a block of land 250 feet north of main shaft. Signed by J.S. Potter, H. Hancock, G Murray and T. Tumney. 1.Page one hundred and one: three quotes from 'Edwards' Metallurgical Works' Specimen Hill, Bendigo for pyrites and blanket sand. 2.Page one hundred and fifty five: handwritten letter (copy) from A. Schonfelder re shaft work on the mine and mention of tributors 3. Affixed to inside cover: letter from the 'United Shire of Mount Alexander' April 15th. 1907, regarding the reconstruction of the Vaughan bridge over the Loddon River. 'the benefit that the mines in your district derive from the bridge being open for wood waggons and this being the main traffic and this being the principal cause of the bridges present condition'. 4. Prospectus of the Spring Gully Mining Company, Spring Gull, Fryerstown, two page folded document enclosed inside back cover of book. Prospectus incomplete. (10746.93a) 5. Carbon copy of letter to D.E. Williams Esq, Castlemaine from GlenAthol, Casewick Road, London, January 25th, 1907 regarding two gentlemen who were 'called upon to carry the 'Spring Gullys' through - Mr. H. 'is making a determined effort to bring the matter to a successful issue' Letter signed by George Allan. (10746.93b. 6. Carbon copy of letter from E. Williams, London re proposed new company to acquire the properties of Spring G.M. Coy, Spring Gully G.M. Coy. No. 1, Sth Spring Gully G.M. Coy, Sth Spring Gully G.M. Coy Extended (10746.93c) 7. Handwritten letter to the Chairman and Directors of the Spring Gully G.M. Co. re the appointment of 'Mr. Samuel Morse Battery Manager at once, or accept my resignation as Mining Manager, for we can't agree any longer' Signed by A. Schonfelder. 8. Notice of extraordinary meeting of shareholders in Spring Gully Gold Mining Company No Liability, 22nd November 1906 at Beehive Chambers, Bendigo. Signed W.G. Blackham (Blackham & Garvin) Manager of the Company. (10746.93e) The Minute Book is part of the Margaret Roberts Collection of mining documents.bendigo, margaret roberts, , goldmining, castlemaine, spring gully gold mine, fryertown

Malachite is a green copper carbonate hydroxide mineral and was one of the first ores used to make copper metal. Malachite has been utilised as a gemstone and sculptural material in the past as its distinctive green color does not fade when exposed to light or after long periods of time. Malachite is formed at shallow depths in the ground, in the oxidizing zone above copper deposits. The material has also been used as a pigment for painting throughout history. This particular specimen was recovered from the Burra Burra Copper Mine in Burra, South Australia. Otherwise known as the 'Monster Mine', the Burra Burra Copper Mine was first established in 1848 upon the discovery of copper deposits in 1845. Within a few short years, people from around the world migrated to Burra to lay their claim in the copper economy. By April 1848 the mine was employing over 567 people and supporting a population of 1,500 in the local township. Up until 1860, the mine was the largest metals mine in Australia, producing approximately 50,000 tonnes of copper between 1845 to its closure in 1877. The Burra Burra Mine was also famous for a number of other specimens, including; crystalline azurite, cuprite, and botryoidal and malachite.Malachite is considered a rare gemstone in that the original deposits for the stones have been depleted leaving behind very few sources. In addition, the use of Malachite as gemstones and sculptural materials remains just as popular today as they were throughout history. It is quite common to cut the stone into beads for jewellery. The fact that Malachite has such a rich colour and one that does not fade with time or when exposed to light makes it particularly rare. 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 carbonate hydroxide mineral with shades of yellow, blue, and light green throughout.geological, geological specimen, burke museum, indigo shire, malachite, malachite specimen, burra burra mine, burra, south australia, australian mines, mines, monster mine

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

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

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

This particular specimen was recovered from the Lal Lal Coal and Iron Mine in Victoria, 19km from Ballarat. Brown Coal was discovered here in 1857, just alongside the Geelong to Ballarat Railway line. This discovery of lignite (brown coal) was the first in Victoria, which would bring important benefits to the region and state, both of which had previously been reliant on coal imports. In the 1860s, iron ore was found just 5km from Lal Lal, and the area was converted into an Iron Ore Mine. The Lal Lal Iron Mining Company took over operations in 1874, who then peaked iron production in 1884. This mine continued operations until June 1884, when the blast furnace was extinguished and never recommenced. The blast furnace at Lal Lal is considered one of the most important and highly significant sites ion early industrial history in Australia, as it is the only remaining best furnace from the nineteenth century in the Southern Hemisphere. The furnace ruins are 17 metres high, and are clearly visible today on Iron Mine Road, Lal Lal, near the Bungal Dam. This specimen of Lignite (brown coal) is significant, as it was mined from the area where brown coal was first discovered in Victoria, leading to an important and controversial future of the mining and use of brown coal in this State. The Victorian Heritage Database has listed the Lal Lal Coal Mine with local significance, with their Statement of Significance stating: "The Lal Lal coal mine is historically significant as the site of the first discovery of lignite (brown coal) in Victoria, and one that promised important benefits to regional and state industries that were reliant on coal imports at the time. The significance of the stie is reduced by the poor state of preservation of the coal mining and processing fabric". 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 light-weight, soft and combustable sedimentary rock specimen, that is dark brown in colour. The specimen has jagged edges, as though parts of the rock have crumbled away. Brown coal, or Lignite, is formed naturally from compressed peat, and is typically found in natural basins. The stages to the formation of coal ('coalification') begin with plant material and wood, which will decay if it is not subjected to deep burial or heating, and turn into Peat. Peat, when sufficiently compressed naturally, will turn into Brown Coal (Lignite), and finally into Black Coal (sub-bituminous, bituminous and anthracite). Each successive stage has a higher energy content and lower water content. It is brownish-black in colour. Brown Coal has a high moisture content, between 50 and 75 percent, and a low carbon content. Some Brown Coals may be stratified, with layers of plant matter, which means little coalification has occurred beyond the peat natural processing stage. When Brown Coal is submerged in dilute nitric acid or boiling potassium hydroxide solution, it reacts to produce a reddish solution, of which higher-ranked coals do not. When brown coal is pulverised and burned in boilers, the steam is used to drive turbines, which generates electricity. It is the lowest rank of coal, as when burned, it creates a relatively low heat content, which in turn does not create a great output of steam. burke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, mineralogy, brown coal, brown coal specimen, lignite, lal lal, lal lal coal mine, lal lal iron mine, ballarat, blast furnace

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 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

This specimen is from Barefoot Hills, Victoria. Sandstones are economically important as major reservoirs for both petroleum and water, as building materials, and as valuable sources of metallic ores. Most significantly, they are the single most useful sedimentary rock type for deciphering Earth 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 sedimentary rock composed mostly of quartz sand. Sandstone is the second most common sedimentary rock after shale. Sandstones consist of sand-sized grains principally quartz, feldspar and rock fragments. The two major classes of sandstone are arenite and wacke. the colour of sandstone varies from grey, yellow, red and white reflecting the variation in mineral content and cement and is gritty to touch (like sandpaper).Geological survey / R.... S 61 / Loc Bareboot Hills / Sheet / 24SE / 94 /burke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, mineralogy, sandstone, yellow sandstone, victoria, barefoot hills

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

Although it is not known where these specimens were collected, Victoria and other regions of Australia were surveyed for sites of potential mineral wealth throughout the 19th Century. The identification of sites containing valuable commodities such as gold, iron ore and gemstones in a locality had the potential to shape the development and history of communities and industries in the area. The discovery of gold in Victoria, for instance, had a significant influence on the development of the area now known as 'the goldfields', including Beechworth; the city of Melbourne and Victoria as a whole. Agate occurs when amygdales (gas pockets) form in the upper levels of basaltic lava flows. If these pockets or bubbles are iniltrated by water bearing silica in solution, the fluid dries and hardens in layers, forming round or egg shaped nodules or geodes within the rocky matrix. Agate is formed of a silica mineral chalcedony similar to quartz. The term carnelian primarily refers to the reddish shading of the stone; whether the stone is termed an agate or chalcedony type is often influenced by the degree of colour banding the specimen shows. The specimens are significant as examples of surveying activity undertaken to assess and direct the development of the mineral resource industries in Victoria and Australia, as well as the movement to expand human knowledge of earth sciences such as mineralogy and geology in the nineteenth century.Three small geological specimens that appear visually consistent with images of rough or unpolished Carnelian Agate or Chalcedony. geological specimen, geology, geology collection, burke museum, beechworth, indigo shire, north-east victoria, gemstones, agate, carnelian

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

Malachite is a green copper carbonate hydroxide mineral and was one of the first ores used to make copper metal. Malachite has been utilised as a gemstone and sculptural material in the past as its distinctive green color does not fade when exposed to light or after long periods of time. Malachite is formed at shallow depths in the ground, in the oxidizing zone above copper deposits. The material has also been used as a pigment for painting throughout history. Malachite is considered a rare gemstone in that the original deposits for the stones have been depleted leaving behind very few sources. In addition, the use of Malachite as gemstones and sculptural materials remains just as popular today as they were throughout history. It is quite common to cut the stone into beads for jewellery. The fact that Malachite has such a rich colour and one that does not fade with time or when exposed to light makes it particularly rare. Although there is no indication available of the locality from which the specimen was sourced, it is likely that the specimen was collected either in South Australia in the vicinity of the Burra Burra mines or in Victoria as part of programs of geological surveying undertaken in the Nineteenth and Twentieth centuries. 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 carbonate hydroxide mineral with quartz pebbles in red conglomorate matrix presenting shades of cream, brown and green.Existing label: Malachite / (green) in / conglomerate / (white quartz / pebbles / in red matrix /geological specimen, geology, geology collection, burke museum, beechworth, geological, indigo shire, malachite, malachite specimen, australian mines, mines, geological survey, conglomorate, matrix

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

This specimen is Cassiterite in Quartz. Cassiterite is a tin oxide metal that forms in thin crystals which can have a beautiful lustre. Quartz is made of silicon dioxide, also known as silica, and is one of the most common minerals on earth. Cassiterite has been a fundamental source of tin ore for humans throughout history, including today. Tin is an important metal that has a wide variety of human uses in different areas, from dying fabric, to making mirrors, and their most well-known use ‘tin’ cans. Tin cans are primarily made of steel and are coated with tin in order to take advantage of tin’s property of being non-corroding. This is a massive step in the history of food preservation. Tinned food first reached Australia in 1815 with early settlers, and it began to be manufactured here in the 1840s. It was incredibly popular, and was a highly exported product, which would be a contributing factor to the ‘tin mining boom’ of the early 1880s. This specimen was collected at Jingellic, New South Wales, in about 1852. Although the Goldfields of the 1800s are much more well-known, tin mines existed alongside the gold mines which began in the mid 19th century and extended almost one hundred years, to the mid 20th century. Specimens like this would have been used as evidence to justify tin mining operations in the region as an investment. 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. The Geological Survey of Victoria was headed by British geologist, Alfred Richard Cecil Selwyn (1824-1902), who was responsible for issuing over 60 geological maps during his 17 years as director. These maps were all hand-drawn and coloured and became the benchmark for accuracy for geological mapping. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study. A fist-sized solid geological specimen made on one half of tin oxide, which is dark grey, and on the other side of silica, which is brown and cream.burke museum, beechworth, geological, geological specimen

This lantern slide shows the Ovens District Hospital (also called the Ovens Goldfields Hospital) in Beechworth in approximately 1900. The Hospital was built as part of a community push to develop the infrastructure needed for a permanent town in the 1850s. At the time there was no hospital located between Melbourne and the NSW town of Goulburn and it was recognised that the nature of mining and agricultural work predisposed people to serious injury. The community voted in 1853 to raise funds for a hospital and a voluntary committee elected from people who contributed £2 or more annually determined the organisation's management policies, which aimed to provide care for poor people at rates levied according to the person's means. Ongoing operations of the hospital were primarily supported by Government grants, however. The foundation stone was laid at a site in Church Street at a ceremony held 1st September 1856 which was attended by 2000 people using a locally crafted trowel with a tin ore handle and pure gold blade. The hospital, which was designed by J.H. Dobbyn, cost £2347. The hospital had two wards, a dispensary, apartments for a resident surgeon and the matron, an operating theatre and a board room. Further medical facilities including services to meet the cultural and health needs of the local Chinese community were later added, in addition to a Palladian-style cut-granite face built in 1862-63. It functioned as the region's primary hospital until surpassed by the Wangaratta Hospital in 1910. In the 1940s much of the building materials were salvaged and repurposed, with the exception of the facade which was restored in 1963 by the Beechworth Lions Club and still stands today. The facade featured on the covers of local history volume 'Beechworth: a Titan's Field' by Carole Woods and heritage-focused travel guide the 'Readers Digest Book of Historic Australian Towns'. Lantern slides, sometimes called 'magic lantern' slides, are glass plates on which an image has been secured for the purpose of projection. Glass slides were etched or hand-painted for this purpose from the Eighteenth Century but the process became more popular and accessible to the public with the development of photographic-emulsion slides used with a 'Magic Lantern' device in the mid-Nineteenth Century. Photographic lantern slides comprise a double-negative emulsion layer (forming a positive image) between thin glass plates that are bound together. A number of processes existed to form and bind the emulsion layer to the base plate, including the albumen, wet plate collodion, gelatine dry plate and woodburytype techniques. Lantern slides and magic lantern technologies are seen as foundational precursors to the development of modern photography and film-making techniques.This glass slide is significant because it provides insight into Beechworth's built environment and infrastructure in the early Twentieth Century, around the time of Australia's Federation. It is also an example of an early photographic and film-making technology in use in regional Victoria in the time period.Thin translucent sheet of glass with a round-edged square image printed on the front and framed in a black backing. It is held together by metal strips to secure the edges of the slide.Obverse: Y /burke museum, beechworth, lantern slide, slide, glass slide, plate, burke museum collection, photograph, monochrome, ovens district hospital, indigo shire, north-east victoria, hospital, palladian architecture, granite, community fundraising, community infrastructure, j.h. dobbyn, beechworth lions club, ovens goldfields hospital, chinese community

Named in 1845 by Wilhelm Karl von Haidinger cerussite takes its name from the Latin cerussa, meaning 'white lead'. When viewed under certain lighting conditions cerussite gives of fire and rainbow-like colours (due to its high dispersion) and it is quite sought after by geological collectors for this very reason. Cerussite is usually found in the oxidised zone of lead ore deposits. It is a very common weathering product of galena and other lead ore minerals. It is a secondary mineral, meaning it forms as a result of the alteration of pre-existing minerals in the Earth’s crust. The presence of lead in cerussite makes it potentially toxic. Historically, it has been an important source of lead, which has numerous industrial applications, including in batteries, construction materials, and radiation shielding. Cerussite has a crystal structure that belongs to the orthorhombic crystal system. Its crystal structure is characterized by a three-dimensional arrangement of atoms in a repeating pattern. The crystal lattice of cerussite consists of interconnected lead (Pb) and carbonate (CO3) ions. This crystal structure is visible in the specimen. This specimen was found in Dundas (formerly Mount Dundas), a historical mining locality, mineral field and railway located on the western foothills of the West Coast Range in Western Tasmania. During the 1890s Dundas swelled in numbers however it is now lost in a temperate rainforest and its population is now 2. The present Dundas Extended mine, about 1.5 km east of Dundas is presently worked for specimen material.Faceted cerussite gems are considered rare and valuable, given the softness of the mineral. This item is not a faceted gem however its historical and scientific research potential give it significance; mined in an Australian township, this cerussite could shed light on the now lost history of Dundas and the mining that occurred there. Additionally, the uses of this mineral in historical industrial processes give it scientific significance. Such knowledge can add to understandings of the geographical and geological nature of Western Tasmania and allow for further study of Australian geological specimens. A small lead carbonite mineral with shades of cream, white and brown throughout, flaky shards of white at base. CERUSSITE / (lead carbonite) / Locality: Dundas, W. Tasmaniadundas, tasmania, cerussite, lead, orthorhombic, geology, minerals, mining

This image is a reproduction of an 1899 original depicting the 'Williams Good Luck Mine' on the Mopoke Reef (also called 'Morepork Gully') in the Dingle Ranges, approximately three miles from Beechworth. The foreground of the image is littered with piles of smashed rock and detritus, known as ‘mullock’, beside a reinforced mine shaft, a vertical access passageway allowing miners to enter the mine and haul ore out using lifting technology such as a poppet heads, whims or windlasses. A group of miners and a dog appear close to an open-sided miner’s hut. Following the discovery of gold at Beechworth in 1852, rushes quickly followed at surrounding creeks and gullies in the district. In the late nineteenth and early twentieth centuries, small syndicates of miners continued to work old or abandoned quartz reefs, often persisting without the assistance of heavy machinery to remove the large amounts of rock, in order to obtain yields at ever greater depths. The group of miners in this photograph are Mr. Roger Williams and Sons, who revived operations at the ‘Old Good Luck’ mine on the Mopoke Reef in the Dingle Range near Beechworth around 1892, working the site for more than two decades. An emigrant from Cornwall with experience in the tin mining industry, 19 year old Roger Williams senior sailed to New Zealand in 1840, then to Australia where he spent time in the Bendigo Gold Fields before settling in Beechworth in the early 1860s. Mr Williams senior worked on various mining activities in the district, including the Rocky Mountain Tunnel project. Conversant with the character of gold-bearing reefs in the area, the syndicate dug an eight hundred foot tunnel, digging down as far down as two hundred feet with little capital save their labour, to connect and provide better working access to the mass of reefs and veins in the vicinity. Progress was hampered by poor air quality charged with fumes from dynamite and large quantities of rock had to be crushed to obtain payable yields. The Victorian Goldfields are filled with ruins and remnants of the area's rich mining history, ranging from small alluvial diggings to the remains of huge mining companies. Site names often changed several times throughout the nineteenth and twentieth centuries. Some sites were abandoned and forgotten, others were worked continuously over many decades. The names of mines were often repeated at different locations throughout the Victorian Goldfields. For example, there is a Mopoke Gully heritage mine near Fryers Creek, Victoria. 'Mopoke' is a common onomatopoeic name for Morepork and Australian Boobook owls. This image has historical, social and research significance for patterns of emigration during of the Victorian Gold Rush, and the historical, social and environmental impacts of mining at Beechworth at the turn of the nineteenth and twentieth centuries. As gold became scarce and government support and large company investment waned, poor hard-working miners laboured intensively to make a living through periods of high unemployment. This image can be compared and studied alongside other historical mining photographs and objects in the Burke Museum Collection. It has potential to improve our understanding of miners working conditions and the shifting character of mining in the Beechworth district. Black and white rectangular reproduction photograph printed on matte photographic paper.Obverse: Williams Good Luck Mine Beechworth / Roger! / Reverse: 6858 / burke museum, beechworth museum, beechworth, gold fields, gold rush, victorian gold rush, gold ming history, colonial australia, australian gold rushes, mining technology, beechworth historic district, indigo gold trail, migration, indigo shire, good luck gold mine, victorian goldfields, mining syndicates, gold fever, quartz-mining, small-scale mining, old good luck mine, mopoke gully, quartz reefs beechworth

This lead ingot was donated to Flagstaff Hill Maritime Village in January 2015 by local residents who discovered the ingot in their garden after they purchased the property about 12 months ago The LOCH ARD cargo manifest lists “Pig lead 50 tons” comprising “944 pig and 37 rolls”. Subsequent classification has rendered this section of cargo as “Lead Ballast”. This could be true. The international price per ton of lead ore plunged from a high point of £17 in 1853 to a low of £8 in 1882. The cheaper price of lead at the time of the vessel’s loading in early 1878 may have meant it was considered as an alternative to other ballast material (traditionally stone) for the journey to Melbourne. Loch Line ships generally returned to Britain laden with Australian wool. Even though wool bales were “screwed in” to the hold to less than half their “pressed weight”, they still made an awkwardly light cargo for the passage around the Horn. The concentrated weight of lead pigs along the keel line would help steady and centre the ship, and perhaps the artefacts in this case were to be retained for this purpose, rather than being sold on to the ready colonial market. However this is conjecture. Demand for building materials in the gold and wool rich Colony of Victoria was high in the 1870s, and much of the LOCH ARD cargo was intended for the Melbourne International Exhibition in 1880, which was another example of buoyant economic conditions. In the nineteenth century lead was valued for its density (high ratio of weight to volume), flexibility (relative softness for working into shape), and durability (corrosion resistant and waterproofing properties). It was used for pipes and water tanks, roof flashing and guttering, window sealing and internal plumbing. Many large private residences and new public buildings were at planning or construction stage in the colony during this period. The LOCH ARD lead ingots could equally have been destined for this ready market. 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 shipwreck 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. Lead ingots (sometimes referred to as ‘lead ballast’ or ‘lead pigs), salvaged from the wreck of the LOCH ARD. Grey metal bars with flat base, rising in a curved moulded shape to form a smooth rounded upper face. The imprint of the maker runs along the upper surface in clearly legible capital lettering (height 3cm). Durable and heavy, with some marine staining, but in good condition. Stamped along curved surface, within oval border, "PONTIFEX & WOOD LONDON."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, lead pigs, lead ingots, lead ballast, pontifex and wood, london, lead smelters

A postcard in a series produced by the Rose Stereograph Company in Victoria, Australia as a souvenir of Marysville.A black and white photograph of the Wolfram Track which is part of the Wilks Creek Walking Track near Marysville in Victoria. The Wolfram Track is named after the Wilks Creek Wolfram Mine which opened in around 1894. Wolframite is one of the principle ores of tungsten. The discovery was made in Wolfram Creek by a Mr Robinson who was probably a local of the district. Four creeks eventually proved to carry alluvial deposits of the ore; Wolfram Creek, Opas Creek, Quartz Creek and Main Creek. These creeks run south-east into Deep Creek, a tributary of the O'Shannassy River which, in turn, runs into the Yarra River.POST CARD The "Rose" Series/ De Luxe A Real Photograph/ Produced in Australia Published by the Rose Stereograph Co.,/ Sydney and Melbourne.wolfram track, wilks creek walking track, marysville, victoria, p. 2332, walking track, rose series postcard, postcard, souvenir, wolframite, wolfram creek, opas creek, quartz creek, main creek, deep creek, o'shannassy river, yarra river, mining

A postcard in a series produced by the Rose Stereograph Company in Victoria, Australia as a souvenir of Marysville.A black and white photograph of a part of the forest that the Wolfram Track, which is part of the Wilks Creek Walking Track, runs through. The Wilks Creek Walking Track is in Marysville in Victoria. The Wolfram Track is named after the Wilks Creek Wolfram Mine which opened in around 1894. Wolframite is one of the principle ores of tungsten. The discovery was made in Wolfram Creek by a Mr Robinson who was probably a local of the district. Four creeks eventually proved to carry alluvial deposits of the ore; Wolfram Creek, Opas Creek, Quartz Creek and Main Creek. These creeks run south-east into Deep Creek, a tributary of the O'Shannassy River which, in turn, runs into the Yarra River.POST CARD The "Rose" Series/ De Luxe A Real Photograph/ Produced in Australia Published by the Rose Stereograph Co.,/ Armadale, Victoria.wolfram track, wilks creek walking track, walking track, marysville, victoria, p. 2334, rose series postcard, postcard, souvenir, p. 2332, wolframite, wolfram creek, opas creek, quartz creek, main creek, deep creek, o'shannassy river, yarra river, mining

non-fictionThe men and ships of the New Zealand Shipping company and their participation in the British Merchant Navy during WWII. Includes details of the company's ships lost through enemy action, including the Turakina, victim of the German raider Orion in the Tasman Sea in August 1940 which was the first of the company's ships lost. Also covers the sinking of the Rangitane and Cambridge, as well as the salvage of the Hororata and the Battle of the Atlantic with the Essex in the Malta Convoy. keith oliver, ww2, merchant navy, new zealand shipping company, turakina, rangitane, hororata

A book highlighting Ballarat and surrounds for visiting tourists. Green, black and red soft covered book of 50 pages. The book includes many illustrations and advertisements. Themes of the book include: Ballarat and district, Lake Wendouree, Ballarat Botanical Gardens, Statues, gold and mining, Ballarat gold nuggets, Eureka Stockade, Ballarat School of Mines, Hepburn Lagoon, Emu River, race courses, Art gallery of Ballarat Advertisements include: Dr Lem Chinese Practictioner, Eureka Aerated Waters & Brewing Co., Sunshine Harvester, Gordon Bros., Long's biscuits, South Street, Grand National Eisteddfod of Australia, Lake View Hotel, Carlyon's Hotel, Clarendon Ladies' College, J.E. Sang Chinese Doctor and Herbalist, Reid's Ballarat Coffee Palace, Robert Sim & Co Timber Merchants, Cobb & C0 livery and stables Ballarat, Eagle Foundry, Fred A. Reed Tobacconist, Heinz bros butchers, J.J. Goller & Co. Illustrations include: Craig's Royal Hotel, McBride's Boots, John Lavis Cordial Manufacturer, R. Graham & Sons tanners, Lester's hotel, Sun Foundry, Central business College, Edwards Pyrites & Ore Reduction Co., George Farmer, Sturt Street (colour), Lake Wendouree, Ballarat East Town Hall, Lake Burrumbeet, Queen Victoria Statue, Fairy Land, Ballarat Botanical Gardens, Lal Lal Falls, Moorabool Falls, Kirks Dam, Lake Wendouree and paddle boat, Lydiard Street, Bopeep Creek, Star of the East Mine, Peter Lalor Statue, great Equatorial Telescopu at Oddie Observatory (Ballarat Observatory), Boer War monument, Entrance to Art Gallery of Ballarat, interior of Art Gallery of Ballarat, Old Curiosity Shop, Angus Rialto cafe, Ballarat Brewing Co, Royal Standard brwery, Phoenix Brewery Warrenheip, John MacLeod and Companyballarat, ballarat school of mines, buninyong, burrumbeet, cobb and co, eureka brewery, ballarat brewing co, sturt street, m1604, chinese, chinese medicine, d. lem, j.e. sang, brewery, tanners

The Donation Book relates to the Ballarat School of Mines Museum which opened in 1872. Very few of these items are still held by Federation University. The Museum was emptied in the 1960s with items being distrubuted to the Ballarat Historical Society, returned to original lenders (ie Pern Collection), of disposed of. Donations to the Ballarat School of Mines include: 34. M. Hamburger, Ballarat - bunsen burner 41. W.H. Shaw, Phoenix Foundry - 81 nos of 'Engineer' 89. Juvenile Industrial Exhibition Association Committee per Joseph Flude - dies used for striking medals awarded to successful exhibits. 165. Ferdinand Von Mueller 172 Ferdinand Von Mueller o hortus siccus 6 197. James Stoddart 203. Edward Gazzard, North Creswick - Model of safety Cage invented and made by donor 218. E. Morey 222. Alfred Lestor 228. J.J. Sleep, Ballarat, patent Lever escarpment Clock (displayed in laboratories) 237. Bernard Smith (Warden) per favor of James M. Bickett - Bust of Mr John Lynch, Smythesdale. (Note: This item is not in the present Federation University Historical Collection) 241. James Oddie, J.P., Ballarat, Copy of 'the Chemist and Druggist' 267. John Lynch Junior, Smythesdale - Cast of "Golden Age" nugget, found at Browns by Co-operative party, 12 men. Weight 75 oz, 12 dwts, 12 grs.(Note: This item is not in the present Federation University Historical Collection) 270. Isaac Davis, Main Road, Ballarat 294. W. H. Shaw, Ballarat - 94 nos of 'The Engineer' 295. Rivett Henry Bland, Clunes - Specimen of water pipe from the Port Phillip Company's mine encrusted with carbonites of lime and magnesium (Note: This item is not in the present Federation University Historical Collection) 299. D.J. Williams, Queenscliff - 1 case shells from Fiji 305. C. Retallack, Ballarat 314. William Henry Shaw, Ballarat - glass case 323. W. Longley, Ballarat - Botanical Specimen (Note: This item is not in the present Federation University Historical Collection) 327. W. H. Angove, Perth 337. J. Cosmo Newbery, B Sc, Melbourne 343. James Hector, M.D., New Zealand 353. R.S. Mitchell, Ballarat - 8 specimens live plants (medicinal) (for the Ballarat School of Mines Garden) 355. W. Magee, Ballarat - Sugar cane plants and seeds (for the Ballarat School of Mines Garden) 363. James Hector, Wellington, new Zealand 371. William Wesley, 28 Essex St, Strand, London - Scientific book circular 380. Jacob Upfold (deceased) per favor of the trustees - bequest of steam engine indicator and belongings (boothe and case) 381. Joseph Mitchell, 22 Macarthur Street, Ballarat - sod of turf cut from Warboy's High Few, County Huntingdon, England, 1872. 394. W.H. Barnard 401. James Orr 418. F. Ratte, Sydney 440. Alfred Mica Smith, Sandhurst (Bendigo), Inaugural Address, delivered to the Bendigo School of Mines Science Society, June 20. 1881 by P.H. Macgillivray, MA, MRCS, FLS, President. (Note: This item is not in the present Federation University Historical Collection) (Note: This item is not in the present Federation University Historical Collection) 446. C. C. Shoppee, Ballarat 462. Dr Bunce, Ballarat 468. James Black, Mining Manager "Kerrit Bureet' 479. J.S. North, Mining Manager No. 2 Queen Co, Black Hill Ballarat. 505. Smith Tibbitts - A block of ancient leaves from the Nigtingbool Estate near Haddon on the Ballarat district from shaft 80 feet deep. (Note: This item is not in the present Federation University Historical Collection) 512. F.W. Niven, Ballarat - "A Handy Book to Tasmania" 522. James Hector, Wellington, New Zealand 549. C.E. Grainger, Manager Ballarat Woollen Mills - samples of dyed and raw wools 600. (4 July 1882) Henry Sutton, Ballarat - 13th annual report of the Aeronautical Society of Great Britain; 2 papers from the Proceedings of the Royal Society, nos 217 and 218- 1882, "One a new electrical storage battery by Henry Sutton, Ballarat, Victoria. 608. H. Glenny J.P., Ballarat - Specimen of Asbestos from Tasmania 610. M.H. Edelmann, Munich, Germany 674. W.H. Shaw, Phoenix Foundry - Steel boring 95 feet long taken from bed-plate of locomotive engine. 675 - H.R. Hancock J.P. pre favour Mr James Pryor, Moonta Mines 676. Baron Ferdinand Von Mueller KCMG, etc, Melbourne 678. E.F.A. Gaunt, Royal Navy, H.M.S. Nelson, per favour Lyde Gaunt - Specimen of manganese ore from the mines - Russell - New Zealand 728. Dr Pinnock, Ballarat 760. Simon Morrison, Ballarat 784. James Shugg, Hamilton - 1 case fossils from Muddy Creek, near Hamilton. (Note: This item is not in the present Federation University Historical Collection) 786. W. Bolam (inspector of Schools), Melbourne - 2 spears and 1 fishing prong Fijian 806. James Oddie, Ballarat 708. Henry G. Hanks, San Francisco 786. W. Bolam (Inspector of Government Schools Melbourne) - 2 spears and one fishing prong Fijian 824. Henrique Gorceixm Onro Preto, Brazil 840. W. Laplau, Ballarat - Gas furnace with a large assortment of fittings, also large gas holder and oil-heating apparatus 854. Robert Borch, Main Road, Ballarat - Improved safety chain (Note: This item is not in the present Federation University Historical Collection) 928. James Oddie 944. James P. Munroe, Registrar, Massachusetts 952. L.E. Cutter per favour of Mr F.J. Martell - Unexploded bomb shell from the Eureka Stockade 957. H. Glenny, Hobart 962. George Hart, Ballarat - eagle 976. Henry Sutton, Ballarat - 1 volume "Plattner on the Blowpipe" 978. J.W. Flatow, 45 Madeline Street, Carlton, Melbourne 984. Charles C Shoppee Ballarat - Copies of ancient coins 989-95 - Specimens from Moonta, South Australia 985. W.H. Wooster BOlwarra - books microscope related 1179. James Oddie - Live hedgehog 1181 C. Crisp, Bacchus Marsh, Portugal Copper Coin, 1785 1248 James Oddie, Solomon Islands - Bow and arrows & Spears 1285. C. Colyer, Smythesdale 1327. John L. McKenna, Smeaton - Fragment of Stone Axe. 1395. Mrs O. Skoglund, Nerrina 1428. Daniel Brophy, Ballarat - Collection of mineral specimen form Silverton (Collected by Mrs James Murray) 1442. Henry Sutton, Ballarat - Specimens of fossil fruits collected at Haddon by Charles Brown. 1444. Mining Department - Underground Mine Workings from Band of Hope and others. 1517. W.H. Wooster, Ballarat 1592. Bishop of Ballarat - Stone Axe and other native items 1669. H. McHaffier, Napoleons - 1 Spanish silver coin 1681. James Oddie, Dunedin 1688. W. Burbridge, Ballarat - Native Tomahawk from Metung 1708. A. Doepel, Ballarat 1712. Marty Guerin, Ballarat 1735. Bella Guerin. M.A., Ballarat - Copy Wide Awake Vol 1 No 7 May 28th 1887 and The Bulletin, March 19th 1887. 1747. Bella Geurin M.A., Ballarat - Copy Wide Awake Vol 1 No 8 June 4 1887 1751. Bella Geurin M.A., Ballarat - Copy Wide Awake Vol 1 No 9 June 11th 1887 1842. Linnean Society, London England - Charter, By Laws, Proceedings, Transactions, Journals 1853. W.J. Corbould, Silverton, NSW - chloride of silver from Pinnacles, Broken Hill, Silverton 1888. W. J. Corbould, Sample of metallic silver from Silverton, NSW 1928. E. Morey, Ballarat - Steam Engine 1937. Henry Sutton A.S.I.E., Ballarat - Plate Electric Machine, chimes and Sportman (number crossed out) 1951. Henry Sutton A.S.I.E., Ballarat - Plate Electric Machine, chimes and Sportman 1981. Harrie Wood (per W.H.B.[Barnard?), Ballarat 1996. W.H. Shaw, Phoenix Foundry - Papers "The Vict Engineer July 1887, May June July August 1888 and others 2014. Harrie Wood, Sydney - Report Department of Mines, 18872027. W.J. Bechervaise - Copy of Book by Baldwin Spencer 2034. A.G. Randall - Native Hatchet 2045. W.H. Corbould, Silverton, Collection of silver ores 2051. Fowler, Tarnagulla - Native Tomahawk 2123-2131. James Oddie, London 2163. Roff. F. Taplier, Sturt Street - Native Tomahawk 2178. Syd. Johnson, Meredith - Native Tomahawk, Greenstone 2184. Mr Tupp for Hall - Native Spear and Club 2292. Emmanuel Steinfeld, Melbourne 2313. A. Atwood, Rowlands Factory, Dana Street 2361. Dr Pinnock, Ballarat - Collection of Living Sponges 2363. P. Curnow, Ballarat - Piece of wood with stone naturally embedded 2364. R. Dowling, Waubra 2875. Mrs C, Flude, Ballarat - Collection of (5) mineral specimens 3460. Joseph Weir, Ballarat - Sample of rolled Annibar 3466. J. Hart, Ballarat - Native Shield - supposed to have been made by King Billy 4784. Mr. O. Woolnaugh, Pleasant Street - Four Native Tomahawks 6469. L. Balhausen, Ballarat 3472. John English, Smeaton - three samples of auriferous wash dirt 3607. Columbia College, New York - Handbook of Information of the Columbia College in the Ciry of New York 1892-3. 3672. L.A. Samuels, Bendigo 3724. P. Paperhagen 3736. The Late Rivett Henry Bland per John Noble Wilson - Collection of mineral specimens and fossils 3752. G.A. Denny, South Africa 3755. J. Carroll, Ballarat - Specimen of Native bread found in Ballarat East. 4765. J. Donnelly, Springs, Bungaree I. Fowler, Coolgardie, Specimen of Gold Bearing Quartz ballarat school of mines, doantions, museum, ballarat school of mines museum, safety cage, botanical garden, materia medica garden, library, bella guerin, james oddie, phoenix foundry, w.h. shaw, john lynch, henry sutton, aboriginal, stone axe, tomahawk, geological specimens, moonta, fedinand krause, oddie collection of minerals, thomas bath, spears, solomon islands, king billy, bows and arrows, ancient coins, birds eggs, snakes