This image was taken at the height of the Ballarat school of Mines world wide fame.Black and white photograph mounted onto green card showing an interior chemistry classroom at the Ballarat school of Mines. Chemicals and apparatus line one wall, and geological specimens are housed in glass cases. Posters line the wall. On lower section of photograph 'Section Chemistry Room S.M.B. mines Dept Vic.ballarat school of mines, mines department, geology, chemisty

Stapled folder containing handwritten inventory of historic items collected for school fund-raising exhibition.Column headings include name of collector, type of item, and record of payment of 3d/per item entry fee. Sample of exhibit items include personal and household items, geological specimens, weaponry, and taxidermry. (Prizes for oldest exhibit and most unusual or most original exhibit categories advertised but results not recorded.)

The Ballarat School of Mines had a 'Model Mine' that was used to teach students. Practical work was undertaken for a fee, supervised by laboratory superintendents. Copies of assays undertaken are compiled together in this book. Leatherbound ledger with transfer copies assay reports from the Ballarat School of Mines. Those seeking assaying work from the Ballarat School of Mines are listed in alphabetical order in the front of the ledger. The ledger contains 543 pages. .2) Foolscap assay report on foolscap Ballarat School of Mines letterhead, and signed by Alfred Mica Smith, Superintendent of Laboratories. The report was on eight samples of Quartz submitted by R.C. Morgan, Scotts, Hotel, Melbourne .3) Assay report on Ballarat School of Mines letterhead, dated 14 August 1985, and signed by Andrew Berry, Registrar. The assay was supervised by Professor Alfred Mica Smith, and undertaken for James Burke, Broken Hill, New South Wales. .4) Assay report on Ballarat School of Mines letterhead, dated 18 August 1988, and signed by Alfred Mica Smith, Superintendent of Laboratories. The assay was undertaken on samples of Limonite submitted by James Burke and others, Broken Hill, New South Wales. The report includes information the the Ballarat School of Mines museum and the search for geological specimens from all Australian colonies for the collection. .5) A 'rough' assay report on samples of stone submitted by H. Major Senr, Wilcannia, New South Wales. 5) A 'rough' assay report on sample quartz drillings from quartz reef submitted by H. Morris, Egerton, and an sample of quartz and pyrites for determination by Professor Krause submitted by R.M. Serjeant. ballarat school of mines, a.c. allan, brittania g.m. co., s. body, black horse company, john m. bickett, william bell, james barker, w. bliss, w. bailey, william barrou, w.h. batten, w. bechervaise, band and albion, budd bros, charles barker, i. cahir, a. chamber, w. cahill, james coglan, d. clarke, a.w. dobbie, john dosett, john dunstan, j.a. evans, l. eggleton, charles forbes, d. fitzpatrick, e. ford, michael goold, j. graham, john greenwood, james hayes, ed hardy, arthur harvey, george hodges, john hall, jubilee gold mining company, krause, luplau, lempiere, mt lyell co, john law, ed meadway, john murray, j.h. middleton, c.m. miles, m. muir, e. mcmillan, w. mcdougall, c. napier, w.r. nicholls, napier freehold, w.b, ochiltree, oakleigh gold mining company, dr pinnock, c. quin, james ross, c.b. retallack, e. rowlands, royal standard, linton, frank rabling, william russell, charles soloman, f. selby, w.j. scott, sulieman pasha co, south clunes united, h.w. sinclair, george selby, e.h. schroeder, horsham, e.w. spain, c.h. sheary, sir henry loch gold mining company, a. sutherland, saxon consols, j.b. triggs, h. townsend, harold turnley, c. taylor, melbourne, c. thorpe, a. vandenberg, charles walker, charles wilson, thomas wellington, a. wynne, r. warne, e. wattis, john wood, walter warner, armidale, c. winterbottom, w.l. willliams, j.c. young

This large, leather bound journal was made for the Public Library and Burke Museum in Beechworth by book manufacturer, William Detmold in 1875. It was commissioned by the President of the Library and Burke Museum committee, Dr Antoine Mousse, for the purpose of cataloguing all the items in the collection. The cataloguer was the curator at that time, William Morton, whose hand-writing appears in the journal today. When William Morton first started recording in this journal in 1875, there were already a number of existing items in the institution. The Public Library and Burke Museum in Beechworth had actually been operating since the 1850s; first as a Young Men’s Association in 1856, then as Beechworth Athenaeum in 1858, then as the Beechworth Public Library in 1860. Then in 1861 when news of the death of Beechworth’s former police superintended, Robert O’Hara Burke, reached the town, it was agreed that the Public Library would also become a museum to tribute his legacy, renaming it as the ‘Public Library and Robert O’Hara Burke Memorial Museum, Beechworth’. Many of the items from the early institutions would have been used to form the nucleus of this new organisation. Plus, the additional items that were either collected or donated to develop it into a museum. The catalogue is extensive. There are exactly 461 pages of recorded items, each page detailing the various collections the museum acquired in the late 19th century. Collections recorded in this catalogue include a large collection of geological specimens, that were given to the museum in 1868 by the Geological Survey Department of Victoria. A large collection of taxidermy mounts, that were given to the museum as skins by the Museum of Australia in 1865. An extensive collection of Aboriginal artefacts that were purchased from amateur anthropologist R. E . Johns in 1868. As well as artworks, charts, photographs, machinery, maps etc., all of which have been held in the museum since. This catalogue also details the governance and management of the organisation. There were originally 30 rules that governed the actions for the management committee and, while anyone could read in the free library, only subscribers could borrow two books and one periodical. At first, subscriptions rates were 7/6 a quarter. This was later changed to £1 per annum, paid quarterly in advance. This was a considerable amount; 7/6 per quarter meant that the annual fee was £1.10. This was equivalent to about £650.00 or about $1,182.00AUD today, while the reduced subscription fee of £1 a year was the equivalent to £450.00 or about $818.00AUD today. Membership of the athenaeum would have been the reserve of the town's notable citizens. The vale of the catalogue lies not only in its historical connect with the establishment of the Athenaeum and the current museum, but also in its record of the names and positions of all members of the institution's committees of management from 1875-1876. This is a unique object that contains important records for a notable country town. Large brown leather bound book made in 1875 for the Beechworth library and museum by William Detmond. Inside is a comprehensive and detailed itemised listing of the paintings, drawings, charts, photographs, specimens and books that entered the institution from 1850 -1882. non-fictionCover: RULES / CATALOGUE OF BOOKS / INVENTORY OF PICTURES, DRAWINGS, / MAPS, CHARTS, FURNITURE, SPECIMENS / OF THE / PUBLIC LIBRARY AND BURKE MUSEUM / BEECHWORTHburke museum, beechworth, catalogue, museum catalogue, 1875, william morton, william detmold, exposition universelle, ferdinand von mueller, public library, collection, book, leather bound, restored, digitised, robert o'hara burke, hand-written

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

Rhodonite is a reddish-pink manganese silicate material and often contains iron, magnesium and calcium. It is usually found in metamorphic rocks (rocks which have been altered by heat, pressure or chemical process). It can range in size from tiny to massive. Because of their composition they are not suitable for use in jewellery because they are hard enough. It is quite rare to find, though has been found in Australia, North America, South America and Europe.This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study. This specimen is a palm shaped piece of loellingite within rhodonite. It is mostly reddish-pink coloured, with flecks of light and dark grey. Loellingite is a grey iron arsenide which often forms into crystal shapes. It is mostly found in mesothermal veins (caused by immense heat) with sulfides or in limestone. It is toxic when heated or struck. rhodonite, loellingite, burke museum, beechworth, geological survey of victoria

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 found in Harcourt, Victoria. Harcourt is a small historic gold rush town located in a valley at the foot of Mount Alexander (741 m) in the Central Highlands of Victoria. In recent times the goldrush origins of the town have been replaced by a district known for apples, cider and wine. The Traditional owners of Harcourt are The Dja Dja Wurrung people. Granodiorite is a coarse-grained intrusive igneous rock similar to granite, but containing more plagioclase feldspar than orthoclase feldspar. Granodiorite has greater than 20% quartz by volume, and between 65% and 90% of the feldspar is plagioclase. This piece is of significance due to its provenance in Harcourt, Vic. Granodiorite is commonly produced in volcanic arcs, and in mountain buildings where it emplaces as large batholiths in mountain roots. Granodiorite is the plutonic equivalent of dacite. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.Granodiorite is a coarse-grained intrusive igneous rock similar to granite, but containing more plagioclase feldspar than orthoclase feldspar. According to the QAPF diagram, granodiorite has a greater than 20% quartz by volume, and between 65% and 90% of the feldspar is plagioclase.GRANDIORITE. / Locality: / Harcourt, Victoria / Other label: Geological survey / R S / Loc Harcourt quarries [?] Alexander / 1/4 Sheet. | 4 | Granite /granodiorite, granite, burke museum, harcourt, coarse-grained, igneous, plagioclase feldspar, orthoclase feldspar, quartz, mount alexander, the dja dja wurrung people, the traditional owners, central highlands of victoria, gold rush

This specimen was recovered from Ceres West of Geelong, Victoria. Greenstone is the name for any metamorphosed basic igneous rock (in the case of this specimen, Gabbro) that gains its greenish colour to the presence of the minerals chlorite, actinolite, or epidote, hence the term 'green' and 'stone'. Greenstone is often formed through metamorphsis along a convergent plate boundary. In the rock cycle (the series of processes that creates the various types of rocks) there are identified three different types of rocks, which are the sedimentary, the igneous and the metamorphic. Metamorphic rocks started out as sedimentary, igneous or earlier metamorphic rocks but changed from their original condition under the effect of high heat, high pressure or hot, mineral-rich fluid. However, if pressure or heat is too high, then the rock will melt, resulting in the formation of an igneous rock. The name used to describe these types of rocks reflects this specific inherent trait of change, since the word “metamorphic” derives from the Greek word “metamorphosis”, meaning “change of form or structure”. Metamorphic rocks form in the Earth`s crust but can be also found on the surface, due to elevation of the Earth`s surface. They are divided into two categories: the foliated metamorphic and the non-foliated metamorphic rocks. Gabbro is a highly useful mineral that is often polished to create cemetery markers and kitchen benches. It is notable for its qualities of durability, being able to withstand extreme elements and wear. Whilst not rare, Gabbro is of great utility and has been highly desirable for its qualities. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.Greenstone is a solid hand-sized metamorphic mineral of a green colour. Greenstone is the name for any metamorphosed basic igneous rock (in the case of this specimen, Gabbro) that gains its greenish colour to the presence of the minerals chlorite, actinolite, or epidote, hence the term 'green' and 'stone'. Gabbro is a medium to coarse grained rocks that consist primarily of plagioclase feldspar and pyroxene. Greenstone is often formed through metamorphsis along a convergent plate boundary. Gabbro forms due to cooling and crystallization of magma underneath Earth's surface. Greenstone/Gabbro/from Ceres west/of Geelong. Has old Geological Survey label/and probably collected by/Richard Daintree in 1861/C.Willam 15/4/21/ Other label: 62 /greenstone, metamorphosed, igneous rock, gabbro, chlorite, actinolite, epidote, metamorphsis, rock cycle, various types of rocks, sedimentary, high heat, high pressure, mineral-rich fluid, metamorphosis, foliated metamorphic, non-foliated metamorphic, convergent plate boundary, greenish colour, minerals

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

The Loch Ard got its name from ”Loch Ard” a loch that lies west of Aberfoyle, and east of Loch Lomond. It means "high lake" in Scottish Gaelic. The vessel belonged to the famous Loch Line which sailed many vessels from England to Australia. The Loch Ard was built in Glasgow by Barclay, Curdle and Co. in 1873, the vessel was a three-masted square-rigged iron sailing ship that measured 79.87 meters in length, 11.58 m in width, and 7 m in depth with a gross tonnage of 1693 tons with a mainmast that measured a massive 45.7 m in height. Loch Ard made three trips to Australia and one trip to Calcutta before its fateful voyage. Loch Ard left England on March 2, 1878, under the command of 29-year-old Captain Gibbs, who was newly married. The ship was bound for Melbourne with a crew of 37, plus 17 passengers. The general cargo reflected the affluence of Melbourne at the time. Onboard were straw hats, umbrella, perfumes, clay pipes, pianos, clocks, confectionery, linen and candles, as well as a heavier load of railway irons, cement, lead and copper. There were other items included that were intended for display in the Melbourne International Exhibition of 1880. The voyage to Port Phillip was long but uneventful. Then at 3 am on June 1, 1878, Captain Gibbs was expecting to see land. But the Loch Ard was running into a fog which greatly reduced visibility. Captain Gibbs was becoming anxious as there was no sign of land or the Cape Otway lighthouse. At 4 am the fog lifted and a lookout aloft announced that he could see breakers. The sheer cliffs of Victoria's west coast came into view, and Captain Gibbs realised that the ship was much closer to them than expected. He ordered as much sail to be set as time would permit and then attempted to steer the vessel out to sea. On coming head-on into the wind, the ship lost momentum, the sails fell limp and Loch Ard's bow swung back towards land. Gibbs then ordered the anchors to be released in an attempt to hold its position. The anchors sank some 50 fathoms - but did not hold. By this time the ship was among the breakers and the tall cliffs of Mutton Bird Island rose behind. Just half a mile from the coast, the ship's bow was suddenly pulled around by the anchor. The captain tried to tack out to sea, but the ship struck a reef at the base of Mutton Bird Island, near Port Campbell. Waves subsequently broke over the ship and the top deck became loosened from the hull. The masts and rigging came crashing down knocking passengers and crew overboard. When a lifeboat was finally launched, it crashed into the side of Loch Ard and capsized. Tom Pearce, who had launched the boat, managed to cling to its overturned hull and shelter beneath it. He drifted out to sea and then on the flood tide came into what is now known as Loch Ard Gorge. He swam to shore, bruised and dazed, and found a cave in which to shelter. Some of the crew stayed below deck to shelter from the falling rigging but drowned when the ship slipped off the reef into deeper water. Eva Carmichael a passenger had raced onto the deck to find out what was happening only to be confronted by towering cliffs looming above the stricken ship. In all the chaos, Captain Gibbs grabbed Eva and said, "If you are saved Eva, let my dear wife know that I died like a sailor". That was the last Eva Carmichael saw of the captain. She was swept off the ship by a huge wave. Eva saw Tom Pearce on a small rocky beach and yelled to attract his attention. He dived in and swam to the exhausted woman and dragged her to shore. He took her to the cave and broke the open case of brandy which had washed up on the beach. He opened a bottle to revive the unconscious woman. A few hours later Tom scaled a cliff in search of help. He followed hoof prints and came by chance upon two men from nearby Glenample Station three and a half miles away. In a complete state of exhaustion, he told the men of the tragedy. Tom then returned to the gorge while the two men rode back to the station to get help. By the time they reached Loch Ard Gorge, it was cold and dark. The two shipwreck survivors were taken to Glenample Station to recover. Eva stayed at the station for six weeks before returning to Ireland by steamship. In Melbourne, Tom Pearce received a hero's welcome. He was presented with the first gold medal of the Royal Humane Society of Victoria and a £1000 cheque from the Victorian Government. Concerts were performed to honour the young man's bravery and to raise money for those who lost family in the disaster. Of the 54 crew members and passengers on board, only two survived: the apprentice, Tom Pearce and the young woman passenger, Eva Carmichael, who lost her family in the tragedy. Ten days after the Loch Ard tragedy, salvage rights to the wreck were sold at auction for £2,120. Cargo valued at £3,000 was salvaged and placed on the beach, but most washed back into the sea when another storm developed. The wreck of Loch Ard still lies at the base of Mutton Bird Island. Much of the cargo has now been salvaged and some items were washed up into Loch Ard Gorge. Cargo and artefacts have also been illegally salvaged over many years before protective legislation was introduced in March 1982. One of the most unlikely pieces of cargo to have survived the shipwreck was a Minton majolica peacock- one of only nine in the world. The peacock was destined for the Melbourne 1880 International Exhibition. It had been well packed, which gave it adequate protection during the violent storm. Today the Minton peacock can be seen at the Flagstaff Hill Maritime Museum in Warrnambool. From Australia's most dramatic shipwreck, it has now become Australia's most valuable shipwreck artifact and is one of very few 'objects' on the Victorian State Heritage Register. The shipwreck of the Loch Ard is of significance for Victoria and is registered on the Victorian Heritage Register ( S 417). Flagstaff Hill has a varied collection of artefacts from Loch Ard and its collection is significant for being one of the largest accumulation of artefacts from this notable Victorian shipwreck. The collections object is to also give us a snapshot into history so we can interpret the story of this tragic event. The collection is also archaeologically significant as it represents aspects of Victoria's shipping history that allows us to interpret Victoria's social and historical themes of the time. The collections historically significance is that it is associated unfortunately with the worst and best-known shipwreck in Victoria's history. Rectangular piece of cream coloured marble fireplace surround, with an embedded section of wrought iron in one end. Recovered from the wreck of the Loch Ard. Noneflagstaff hill, warrnambool, shipwrecked coast, flagstaff hill maritime museum, maritime museum, shipwreck coast, flagstaff hill maritime village, great ocean road, loch line, loch ard, captain gibbs, eva carmichael, tom pearce, glenample station, mutton bird island, loch ard gorge, marble fireplace, wrought iron, fireplace surround

From the Ballarat School of Mines.rocks, petrified wood

From the Ballarat School of Mines.Copper Specimen, Broken Hill, New South Walesrocks, geology, copper, broken hill

From the Ballarat School of Mines.Petrified wood with some water polish.rocks, geology, petrified wood

Three speimens of petrified wookpetrified wood, geology

Pitch may be made from petroleum or plant sources. Petroleum derived pitch is also known as bitumen whereas plant derived pitch is known as resin. Pitch derived from plant resin however is known as rosin. Tar and pitch are often used interchangeably.5 pieces of black pitch.natural history, pitch, natural specimen

Displayed in History House.One branch of black and white striped coral.natural history, coral, marine ecology, southern reef

Displayed at History HouseUnknown

Part of Eastland demolition obtained through Probuild building contractors by Terry Ahern.Rough grey/black concrete block, part of Eastland demolition during November 2014 +Additional Keywords: Eastland / Probuild / Terry AhernPart of the old Eastland

Section of core sample taken from Eastland Stage 5 Nov 2014 - Donated by Terry Ahern, obtained through Probuild building contractorsSection of core sample taken from Eastland Stage 5 November 2014 +Additional Keywords: Eastland / Ahern, Terry / Probuild

Rock fragments excavated during construction work on Eastland shopping centre extensions.Five rock fragments showing reference no.141484198821 - parts of Eastland excavation in November 2014 donated by Terry Ahern, obtained through Probuild building contractors. +Additional Keywords: Eastland / Terry Ahern / ProbuildPart of the old Eastland

^ plastic cylindrical containers housing five different samples of sandsand, geology

Rock Blanks blanks, rocks, aboriginal

These rectangular slates of 'beautiful, unusual, expensive, green' American roof tiles were recovered from the wreck of the Falls of Halladale. Salvaging began in 1974 by volunteer divers, using local cray-fishing boats. An efficient system was devised to recover up to 4,000 of the still neatly packed slates a day. Many of the 22,000 salvaged slates can be seen on the roofs of eight buildings in the Flagstaff Hill Maritime Village. The iron-hulled, four-masted barque, the Falls of Halladale (1886 - 1908), was a bulk carrier of general cargo. She left New York in August 1908 on her way to Melbourne and Sydney. In her hold, along with 56,763 tiles of unusual beautiful green American slates (roof tiles), 5,673 coils of barbed wire, 600 stoves, 500 sewing machines, 6500 gallons of oil, 14400 gallons of benzene, and many other manufactured items, were 117 cases of crockery and glassware. Three months later and close to her destination, a navigational error caused the Falls of Halladale to be wrecked on a reef off the Peterborough headland at 3 am on the morning of the 15th of November, 1908. The captain and 29 crew members all survived, but her valuable cargo was largely lost, despite two salvage attempts in 1908-09 and 1910. The ship stayed in full sail on the rocky shelf for nearly two months, attracting hundreds of sightseers who watched her slowly disintegrate until the pounding seas and dynamiting by salvagers finally broke her back, and her remains disappeared back into deeper water. The shipwreck is a popular site for divers, about 300m offshore and in 3 – 15m of water. Some of the original cargo can be seen at the site, including pieces of roof slate and coils of barbed wire.The Falls of Halladale shipwreck is listed on the Victorian Heritage Register (No. S255). She was one of the last ships to sail the Trade Routes. She is one of the first vessels to have fore and aft lifting bridges. She is an example of the remains of an International Cargo Ship and also represents aspects of Victoria’s shipping industry The wreck is protected as a Historic Shipwreck under the Commonwealth Historic Shipwrecks Act (1976).Rectangular slates of green American roof tiles, some with a red-brown stain. These are a sample of hundreds of slate roof tiles salvaged from the vessel FALLS of HALLADALENoneflagstaff hill, warrnambool, maritime museum, maritime village, great ocean road, shipwreck coast, cargo, slate, slate tile, green american slates, building material, wreck point, peterborough, bay of islands, russell & co., 1908 shipwreck, salvage, recover