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The Beechworth Burke Museum
Geological specimen - Fossiliferous Mudstone, Unknown
... Geological specimen... of geological and mineral specimens collected from around Australia ...This specimen was found in Cape Patterson, Vic. Cape Paterson is a cape and seaside village located near the town of Wonthaggi, 132 kilometres southeast of Melbourne, in the Bass Coast Shire of Gippsland, Victoria, Australia. These dark, fossiliferous Mudstones were deposited in slow-moving water associated with sedimentary basins & continental shelves. They are rich in carbon which makes them almost black. This is typical of an anoxic, reducing environment such as deep water or stagnant conditions where carbon-rich material would remain unoxidised during subsequent deposition & diagenesis. it has an imprint of a leaf in the rock itself, displaying the fossil of the plant. This specimen is unique due to the leaf impression within the stone itself. Imprint fossils are formed from an organism moving in some way, leaving behind a trace or track. These tracks are preserved when the clay/silt dries slowly and is covered by other sediment. Plants can also leave imprint fossils when they are covered by sediment. The leaf tissue degrades, leaving an imprint of where the leaf once was. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.These dark, fossiliferous Mudstones were deposited in slow moving water associated with sedimentary basins & continental shelves. They are rich in carbon which makes them almost black. This is typical of an anoxic, reducing environment such as deep water or stagnant conditions where carbon rich material would remain unoxidised during subsequent deposition & diagenesis. FOSSILIFEROUS MUDSTONE / Locality: Cape Patterson, Victoria | Descriptive catalogue / Pg 27 No 95 / "Grey Clay, / Cape Paterson with leaf impressions' / 15/4/21 C. William /mudstone, cape patterson, leaf imprint, fossilised leaf, fossiliferous mudstone -
The Beechworth Burke Museum
Geological specimen - Granodiorite, Unknown
... Geological specimen... collection of geological and mineral specimens collected from around ...This specimen was found in Harcourt, Victoria. Harcourt is a small historic gold rush town located in a valley at the foot of Mount Alexander (741 m) in the Central Highlands of Victoria. In recent times the goldrush origins of the town have been replaced by a district known for apples, cider and wine. The Traditional owners of Harcourt are The Dja Dja Wurrung people. Granodiorite is a coarse-grained intrusive igneous rock similar to granite, but containing more plagioclase feldspar than orthoclase feldspar. Granodiorite has greater than 20% quartz by volume, and between 65% and 90% of the feldspar is plagioclase. This piece is of significance due to its provenance in Harcourt, Vic. Granodiorite is commonly produced in volcanic arcs, and in mountain buildings where it emplaces as large batholiths in mountain roots. Granodiorite is the plutonic equivalent of dacite. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.Granodiorite is a coarse-grained intrusive igneous rock similar to granite, but containing more plagioclase feldspar than orthoclase feldspar. According to the QAPF diagram, granodiorite has a greater than 20% quartz by volume, and between 65% and 90% of the feldspar is plagioclase.GRANDIORITE. / Locality: / Harcourt, Victoria / Other label: Geological survey / R S / Loc Harcourt quarries [?] Alexander / 1/4 Sheet. | 4 | Granite /granodiorite, granite, burke museum, harcourt, coarse-grained, igneous, plagioclase feldspar, orthoclase feldspar, quartz, mount alexander, the dja dja wurrung people, the traditional owners, central highlands of victoria, gold rush -
The Beechworth Burke Museum
Geological specimen - Greenstone / Gabbro, Unknown
... Geological specimen... of geological and mineral specimens collected from around Australia ...This specimen was recovered from Ceres West of Geelong, Victoria. Greenstone is the name for any metamorphosed basic igneous rock (in the case of this specimen, Gabbro) that gains its greenish colour to the presence of the minerals chlorite, actinolite, or epidote, hence the term 'green' and 'stone'. Greenstone is often formed through metamorphsis along a convergent plate boundary. In the rock cycle (the series of processes that creates the various types of rocks) there are identified three different types of rocks, which are the sedimentary, the igneous and the metamorphic. Metamorphic rocks started out as sedimentary, igneous or earlier metamorphic rocks but changed from their original condition under the effect of high heat, high pressure or hot, mineral-rich fluid. However, if pressure or heat is too high, then the rock will melt, resulting in the formation of an igneous rock. The name used to describe these types of rocks reflects this specific inherent trait of change, since the word “metamorphic” derives from the Greek word “metamorphosis”, meaning “change of form or structure”. Metamorphic rocks form in the Earth`s crust but can be also found on the surface, due to elevation of the Earth`s surface. They are divided into two categories: the foliated metamorphic and the non-foliated metamorphic rocks. Gabbro is a highly useful mineral that is often polished to create cemetery markers and kitchen benches. It is notable for its qualities of durability, being able to withstand extreme elements and wear. Whilst not rare, Gabbro is of great utility and has been highly desirable for its qualities. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.Greenstone is a solid hand-sized metamorphic mineral of a green colour. Greenstone is the name for any metamorphosed basic igneous rock (in the case of this specimen, Gabbro) that gains its greenish colour to the presence of the minerals chlorite, actinolite, or epidote, hence the term 'green' and 'stone'. Gabbro is a medium to coarse grained rocks that consist primarily of plagioclase feldspar and pyroxene. Greenstone is often formed through metamorphsis along a convergent plate boundary. Gabbro forms due to cooling and crystallization of magma underneath Earth's surface. Greenstone/Gabbro/from Ceres west/of Geelong. Has old Geological Survey label/and probably collected by/Richard Daintree in 1861/C.Willam 15/4/21/ Other label: 62 /greenstone, metamorphosed, igneous rock, gabbro, chlorite, actinolite, epidote, metamorphsis, rock cycle, various types of rocks, sedimentary, high heat, high pressure, mineral-rich fluid, metamorphosis, foliated metamorphic, non-foliated metamorphic, convergent plate boundary, greenish colour, minerals -
The Beechworth Burke Museum
Geological specimen - Cerussite, Unknown c.1890s
... Geological specimen... for further study of Australian geological specimens. Dundas Tasmania ...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 Beechworth Burke Museum
Geological specimen - Garnet (red crystals) in galena (silvery metallic) and green feldspar, Unknown
... Geological specimen... of boom and bust which continues today. This geological specimen ...Garnet is a popular gemstone used in jewellery due to its hardness and durability. There are about 5 varieties of Garnet, which distinguish the colour of each stone. In Australia mostly Pyrope and Aimandine varieties are found; Pyrope, which is blood-red to black and Aimadine, which is brownish-red to black. Other varieties are rarely found in Australia. The garnets visible in this specimen are likely Pyrope. Galnea is the natural mineral form of lead sulphide and has had various uses throughout history; from makeup to car batteries. It was first mined in South Australia in 1841. Green feldspar is an amazonite mineral, a variety of the potassium feldspar called microcline. This particular mineral is considered uncommon. It has been used in jewellery throughout history. It is likely that this specimen was found in Broken Hill, NSW, presumed due to findings of specimens with similar combinations. Broken Hill is Australia’s longest-lived mining city. The city’s fortunes have come and gone against an extreme economic background of boom and bust which continues today.This geological specimen is a rarity, given that is formed of three distinct minerals and the richness of colour that remains visible in this item attests to the strength of each structure. As we cannot pinpoint exactly where this specimen was found further research can only strengthen what is known about mining within Australia. As such the item is significant due to its scientific rarity and its ability to represent three specimens in one. A solid palm-sized mineral that features shades of grey, red and green. garnet, galnea, green feldspar, minerals, mining, rare specimen -
Flagstaff Hill Maritime Museum and Village
Geological specimen - Marble, 1873-1878
... Geological specimen... of the Loch Ard. Geological specimen Marble ...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 -
Warrnambool and District Historical Society Inc.
Geological specimen - Pumice
... Geological specimen... substance. Geological specimen Pumice ...Pending further research and information nothing is known about this piece of pumice.This piece of pumice has no known local provenance but is retained for display purposes.This grey irregular shaped piece of pumice is pitted and has traces of a white substance.Nilpumice -
Federation University Historical Collection
Geological specimen - Rocks, Petrified Wood, New South Wales
... Geological specimen... South Wales Geological specimen Rocks ...From the Ballarat School of Mines.rocks, petrified wood -
Federation University Historical Collection
Geological specimen - Rocks, Copper Specimen, Broken Hill, New South Wales
... Geological specimen..., New South Wales Geological specimen Rocks ...From the Ballarat School of Mines.Copper Specimen, Broken Hill, New South Walesrocks, geology, copper, broken hill -
Federation University Historical Collection
Geological specimen - Rocks, Petrified Wood
... Geological specimen... wood with some water polish. Petrified Wood Geological specimen ...From the Ballarat School of Mines.Petrified wood with some water polish.rocks, geology, petrified wood -
Federation University Historical Collection
Geological specimen
... Geological specimen... E.J. Barker Library (top floor) Mount Helen goldfields Geology ...geology, rocks, sap hill cemment, golden point ballarat cement -
Federation University Historical Collection
Geological specimen, Petrified
... Geological specimen... petrified wood rock geology 14 specimens of petrified wood. Some ...14 specimens of petrified wood. Some smooth some rough.petrified wood, rock, geology -
Federation University Historical Collection
Geological specimen, Jaspar
... Geological specimen... Geological specimen ...Six pieces of Jaspar (or jaspar like) rocks.jaspar, geology -
Federation University Historical Collection
Geological specimen, Selwynite, n/a
... Geological specimen... E.J. Barker Library (top floor) Mount Helen goldfields geology ...Green and brown rock known as Selwynite. It was found at Lady's pass near HEathcote, Victoria, and was identified by Peter Dalhaus in August 2008.geology, rock, selwynite -
Federation University Historical Collection
Geological specimen, Petrified wood
... Geological specimen... wood Geological specimen ...Three speimens of petrified wookpetrified wood, geology -
Glenelg Shire Council Cultural Collection
Geological specimen - Whale bones, n.d
... Geological specimen... Geological specimen Whale bones ...Believed to be confiscated by Department of Natural Resources from members of the public who had the bones in violation of the law. | 19/4/2000Various whale bones including |1 x top skull bone of Southern Right Whale |1 x jaw bone |1 x vertebrae |1 x rib |1 x eardrum -
Glenelg Shire Council Cultural Collection
Geological specimen - Black Pitch, n.d
... Geological specimen... specimen 5 pieces of black pitch. Geological specimen Black Pitch ...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 -
Glenelg Shire Council Cultural Collection
Geological specimen - Zebra Coral, n.d
... Geological specimen... branch of black and white striped coral. Geological specimen ...Displayed in History House.One branch of black and white striped coral.natural history, coral, marine ecology, southern reef -
Glenelg Shire Council Cultural Collection
Geological specimen - Brick - Glen Iris 1956 Olympics Brick, n.d
... Geological specimen... House Unknown Geological specimen Brick - Glen Iris 1956 ...Displayed at History HouseUnknown -
Ringwood and District Historical Society
Geological specimen - Concrete block, Rough grey/black concrete block, part of Eastland demolition during November 2014
... Geological specimen... of Eastland demolition during November 2014 Geological specimen ...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 -
Ringwood and District Historical Society
Geological specimen - Core sample, Section of core sample taken from Eastland Stage 5 - November 2014, Nov-14
... Geological specimen... from Eastland Stage 5 - November 2014 Geological specimen Core ...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 -
Ringwood and District Historical Society
Geological specimen - Rock fragments, Five rock fragments showing reference no.141484198821 - parts of Eastland excavation in November 2014
... Geological specimen... excavation in November 2014 Geological specimen Rock fragments ...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 -
Federation University Historical Collection
Geological specimen, Five Different Coloured sands
... Geological specimen... samples of sand Five Different Coloured sands Geological specimen ...^ plastic cylindrical containers housing five different samples of sandsand, geology -
Federation University Historical Collection
Geological specimen, Rock
... Geological specimen... Geological specimen ... -
Federation University Historical Collection
Geological specimen - Ethnographic, Rock Blanks
... Geological specimen... rocks Aboriginal Rock Blanks Rock Blanks Geological specimen ...Rock Blanks blanks, rocks, aboriginal -
Flagstaff Hill Maritime Museum and Village
Geological specimen - Slate, c. 1908
... Geological specimen... of HALLADALE Geological specimen Slate ...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 -
Flagstaff Hill Maritime Museum and Village
Geological specimen - Slate, c. 1908
... Geological specimen... the wreck of the Falls of Halladale. Geological specimen Slate ...The iron-hulled, four-masted barque, the Falls of Halladale, 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. ABOUT THE ‘FALLS OF HALLADALE’ (1886 - 1908) Built: in1886 by Russell & Co., Greenock shipyards, River Clyde, Scotland, UK. The company was founded in 1870 (or 1873) as a partnership between Joseph Russell (1834-1917), Anderson Rodger and William Todd Lithgow. During the period 1882-92 Russell & Co., standardised designs, which sped up their building process so much that they were able to build 271 ships over that time. In 1886 they introduced a 3000 ton class of sailing vessel with auxiliary engines and brace halyard winches. In 1890 they broke the world output record. Owner: Falls Line, Wright, Breakenridge & Co, 111 Union Street, Glasgow, Scotland. Configuration: Four masted sailing ship; iron-hulled barque; iron masts, wire rigging, fore & aft lifting bridges. Size: Length 83.87m x Breadth 12.6m x Depth 7.23m, Gross tonnage 2085 ton Wrecked: the night of 14th November 1908, Curdies Inlet, Peterborough south west Victoria Crew: 29 The Falls of Halladale was a four-masted sailing ship built-in 1886 in Glasgow, Scotland, for the long-distance cargo trade and was mostly used for Pacific grain trade. She was owned by Wright, Breakenridge & Co of Glasgow and was one of several Falls Line ships, all of which were named after waterfalls in Scotland. The lines flag was of red, blue and white vertical stripes. The Falls of Halladale had a sturdy construction built to carry maximum cargo and able to maintain full sail in heavy gales, one of the last of the ‘windjammers’ that sailed the Trade Route. She and her sister ship, the Falls of Garry, were the first ships in the world to include fore and aft lifting bridges. Previous to this, heavily loaded vessels could have heavy seas break along the full length of the deck, causing serious injury or even death to those on deck. The new, raised catwalk-type decking allowed the crew to move above the deck stormy conditions. This idea is still used today on the most modern tankers and cargo vessels and has proved to be an important step forward in the safety of men at sea. On 4th August 1908, with new sails, 29 crew, and 2800 tons of cargo, the Falls of Halladale left New York, bound for Melbourne and Sydney via the Cape of Good Hope. The cargo on board was valued at £35,000 and included 56,763 tiles of American slate roof tiles (roof slates), 5,673 coils of barbed wire, 600 stoves, 500 sewing machines, 6,500 gallons of oil, 14,400 gallons of benzene, plumbing iron, 117 cases of crockery and glassware and many other manufactured items. The Falls of Halladale had been at sail for 102 days when, at 3 am on the night of 14th November 1908, under full sail in calm seas with a six knots breeze behind and misleading fog along the coast, the great vessel rose upon an ocean swell and settled on top of a submerged reef near Peterborough on the south-west Victoria’s coast. The ship was jammed on the rocks and began filling with water. The crew launched the two lifeboats and all 29 crew landed safely on the beach over 4 miles away at the Bay of Islands. The postmistress at Peterborough, who kept a watch for vessels in distress, saw the stranding and sent out an alert to the local people. A rescue party went to the aid of the sailors and the Port Campbell rocket crew was dispatched, but the crew had all managed to reach shore safely by the time help arrived. 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 valuable cargo was largely lost, despite two salvage attempts in 1908-09 and 1910. Further salvage operations were made from 1974-1986, during which time 22,000 slate tiles were recovered with the help of 14 oil drums to float them, plus personal artefacts, ship fittings, reams of paper and other items. The Court of Marine Inquiry in Melbourne ruled that the foundering of the ship was entirely due to Captain David Wood Thomson’s navigational error, not too technical failure of the Clyde-built ship. 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).Californian, American, rectangular blue roof slate tile, recovered from the wreck of the Falls of Halladale. flagstaff hill, warrnambool, shipwrecked-coast, flagstaff-hill, flagstaff-hill-maritime-museum, maritime-museum, shipwreck-coast, flagstaff-hill-maritime-village, falls of halladale., slate, roof slate, russell & co. -
Flagstaff Hill Maritime Museum and Village
Geological specimen - Slate
... Geological specimen.... Geological specimen Slate ...The iron-hulled, four-masted barque, the Falls of Halladale, 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. ABOUT THE ‘FALLS OF HALLADALE’ (1886 - 1908) Built: in1886 by Russell & Co., Greenock shipyards, River Clyde, Scotland, UK. The company was founded in 1870 (or 1873) as a partnership between Joseph Russell (1834-1917), Anderson Rodger and William Todd Lithgow. During the period 1882-92 Russell & Co., standardised designs, which sped up their building process so much that they were able to build 271 ships over that time. In 1886 they introduced a 3000 ton class of sailing vessel with auxiliary engines and brace halyard winches. In 1890 they broke the world output record. Owner: Falls Line, Wright, Breakenridge & Co, 111 Union Street, Glasgow, Scotland. Configuration: Four masted sailing ship; iron-hulled barque; iron masts, wire rigging, fore & aft lifting bridges. Size: Length 83.87m x Breadth 12.6m x Depth 7.23m, Gross tonnage 2085 ton Wrecked: the night of 14th November 1908, Curdies Inlet, Peterborough south west Victoria Crew: 29 The Falls of Halladale was a four-masted sailing ship built-in 1886 in Glasgow, Scotland, for the long-distance cargo trade and was mostly used for Pacific grain trade. She was owned by Wright, Breakenridge & Co of Glasgow and was one of several Falls Line ships, all of which were named after waterfalls in Scotland. The lines flag was of red, blue and white vertical stripes. The Falls of Halladale had a sturdy construction built to carry maximum cargo and able to maintain full sail in heavy gales, one of the last of the ‘windjammers’ that sailed the Trade Route. She and her sister ship, the Falls of Garry, were the first ships in the world to include fore and aft lifting bridges. Previous to this, heavily loaded vessels could have heavy seas break along the full length of the deck, causing serious injury or even death to those on deck. The new, raised catwalk-type decking allowed the crew to move above the deck stormy conditions. This idea is still used today on the most modern tankers and cargo vessels and has proved to be an important step forward in the safety of men at sea. On 4th August 1908, with new sails, 29 crew, and 2800 tons of cargo, the Falls of Halladale left New York, bound for Melbourne and Sydney via the Cape of Good Hope. The cargo on board was valued at £35,000 and included 56,763 tiles of American slate roof tiles (roof slates), 5,673 coils of barbed wire, 600 stoves, 500 sewing machines, 6,500 gallons of oil, 14,400 gallons of benzene, plumbing iron, 117 cases of crockery and glassware and many other manufactured items. The Falls of Halladale had been at sail for 102 days when, at 3 am on the night of 14th November 1908, under full sail in calm seas with a six knots breeze behind and misleading fog along the coast, the great vessel rose upon an ocean swell and settled on top of a submerged reef near Peterborough on the south-west Victoria’s coast. The ship was jammed on the rocks and began filling with water. The crew launched the two lifeboats and all 29 crew landed safely on the beach over 4 miles away at the Bay of Islands. The postmistress at Peterborough, who kept a watch for vessels in distress, saw the stranding and sent out an alert to the local people. A rescue party went to the aid of the sailors and the Port Campbell rocket crew was dispatched, but the crew had all managed to reach shore safely by the time help arrived. 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 valuable cargo was largely lost, despite two salvage attempts in 1908-09 and 1910. Further salvage operations were made from 1974-1986, during which time 22,000 slate tiles were recovered with the help of 14 oil drums to float them, plus personal artefacts, ship fittings, reams of paper and other items. The Court of Marine Inquiry in Melbourne ruled that the foundering of the ship was entirely due to Captain David Wood Thomson’s navigational error, not too technical failure of the Clyde-built ship. 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. SIGNIFICANCE 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). Californian, American, blue roof slate tile, rectangular shape, recovered from the wreck of the Falls of Halladale.flagstaff hill, warrnambool, shipwrecked-coast, flagstaff-hill, flagstaff-hill-maritime-museum, maritime-museum, shipwreck-coast, flagstaff-hill-maritime-village, falls of halladale, slate, roof slate, russell & co. -
Flagstaff Hill Maritime Museum and Village
Geological specimen - Slate, c. 1908
... Geological specimen... of the Falls of Halladale. Geological specimen Slate ...The iron-hulled, four-masted barque, the Falls of Halladale, 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. ABOUT THE ‘FALLS OF HALLADALE’ (1886 - 1908) Built: in1886 by Russell & Co., Greenock shipyards, River Clyde, Scotland, UK. The company was founded in 1870 (or 1873) as a partnership between Joseph Russell (1834-1917), Anderson Rodger and William Todd Lithgow. During the period 1882-92 Russell & Co., standardised designs, which sped up their building process so much that they were able to build 271 ships over that time. In 1886 they introduced a 3000 ton class of sailing vessel with auxiliary engines and brace halyard winches. In 1890 they broke the world output record. Owner: Falls Line, Wright, Breakenridge & Co, 111 Union Street, Glasgow, Scotland. Configuration: Four masted sailing ship; iron-hulled barque; iron masts, wire rigging, fore & aft lifting bridges. Size: Length 83.87m x Breadth 12.6m x Depth 7.23m, Gross tonnage 2085 ton Wrecked: the night of 14th November 1908, Curdies Inlet, Peterborough south west Victoria Crew: 29 The Falls of Halladale was a four-masted sailing ship built-in 1886 in Glasgow, Scotland, for the long-distance cargo trade and was mostly used for Pacific grain trade. She was owned by Wright, Breakenridge & Co of Glasgow and was one of several Falls Line ships, all of which were named after waterfalls in Scotland. The lines flag was of red, blue and white vertical stripes. The Falls of Halladale had a sturdy construction built to carry maximum cargo and able to maintain full sail in heavy gales, one of the last of the ‘windjammers’ that sailed the Trade Route. She and her sister ship, the Falls of Garry, were the first ships in the world to include fore and aft lifting bridges. Previous to this, heavily loaded vessels could have heavy seas break along the full length of the deck, causing serious injury or even death to those on deck. The new, raised catwalk-type decking allowed the crew to move above the deck stormy conditions. This idea is still used today on the most modern tankers and cargo vessels and has proved to be an important step forward in the safety of men at sea. On 4th August 1908, with new sails, 29 crew, and 2800 tons of cargo, the Falls of Halladale left New York, bound for Melbourne and Sydney via the Cape of Good Hope. The cargo on board was valued at £35,000 and included 56,763 tiles of American slate roof tiles (roof slates), 5,673 coils of barbed wire, 600 stoves, 500 sewing machines, 6,500 gallons of oil, 14,400 gallons of benzene, plumbing iron, 117 cases of crockery and glassware and many other manufactured items. The Falls of Halladale had been at sail for 102 days when, at 3 am on the night of 14th November 1908, under full sail in calm seas with a six knots breeze behind and misleading fog along the coast, the great vessel rose upon an ocean swell and settled on top of a submerged reef near Peterborough on the south-west Victoria’s coast. The ship was jammed on the rocks and began filling with water. The crew launched the two lifeboats and all 29 crew landed safely on the beach over 4 miles away at the Bay of Islands. The postmistress at Peterborough, who kept a watch for vessels in distress, saw the stranding and sent out an alert to the local people. A rescue party went to the aid of the sailors and the Port Campbell rocket crew was dispatched, but the crew had all managed to reach shore safely by the time help arrived. 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 valuable cargo was largely lost, despite two salvage attempts in 1908-09 and 1910. Further salvage operations were made from 1974-1986, during which time 22,000 slate tiles were recovered with the help of 14 oil drums to float them, plus personal artefacts, ship fittings, reams of paper and other items. The Court of Marine Inquiry in Melbourne ruled that the foundering of the ship was entirely due to Captain David Wood Thomson’s navigational error, not too technical failure of the Clyde-built ship. 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).Californian, American, rectangular blue roof slate, recovered from the wreck of the Falls of Halladale. flagstaff hill, warrnambool, shipwrecked-coast, flagstaff-hill, flagstaff-hill-maritime-museum, maritime-museum, shipwreck-coast, flagstaff-hill-maritime-village, falls of halladale, slate, roof slate, russell & co. -
Flagstaff Hill Maritime Museum and Village
Geological specimen - Slate, c. 1908
... Geological specimen... of the Falls of Halladale. Geological specimen Slate ...The iron-hulled, four-masted barque, the Falls of Halladale, 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. ABOUT THE ‘FALLS OF HALLADALE’ (1886 - 1908) Built: in1886 by Russell & Co., Greenock shipyards, River Clyde, Scotland, UK. The company was founded in 1870 (or 1873) as a partnership between Joseph Russell (1834-1917), Anderson Rodger and William Todd Lithgow. During the period 1882-92 Russell & Co., standardised designs, which sped up their building process so much that they were able to build 271 ships over that time. In 1886 they introduced a 3000 ton class of sailing vessel with auxiliary engines and brace halyard winches. In 1890 they broke the world output record. Owner: Falls Line, Wright, Breakenridge & Co, 111 Union Street, Glasgow, Scotland. Configuration: Four masted sailing ship; iron-hulled barque; iron masts, wire rigging, fore & aft lifting bridges. Size: Length 83.87m x Breadth 12.6m x Depth 7.23m, Gross tonnage 2085 ton Wrecked: the night of 14th November 1908, Curdies Inlet, Peterborough south west Victoria Crew: 29 The Falls of Halladale was a four-masted sailing ship built-in 1886 in Glasgow, Scotland, for the long-distance cargo trade and was mostly used for Pacific grain trade. She was owned by Wright, Breakenridge & Co of Glasgow and was one of several Falls Line ships, all of which were named after waterfalls in Scotland. The lines flag was of red, blue and white vertical stripes. The Falls of Halladale had a sturdy construction built to carry maximum cargo and able to maintain full sail in heavy gales, one of the last of the ‘windjammers’ that sailed the Trade Route. She and her sister ship, the Falls of Garry, were the first ships in the world to include fore and aft lifting bridges. Previous to this, heavily loaded vessels could have heavy seas break along the full length of the deck, causing serious injury or even death to those on deck. The new, raised catwalk-type decking allowed the crew to move above the deck stormy conditions. This idea is still used today on the most modern tankers and cargo vessels and has proved to be an important step forward in the safety of men at sea. On 4th August 1908, with new sails, 29 crew, and 2800 tons of cargo, the Falls of Halladale left New York, bound for Melbourne and Sydney via the Cape of Good Hope. The cargo on board was valued at £35,000 and included 56,763 tiles of American slate roof tiles (roof slates), 5,673 coils of barbed wire, 600 stoves, 500 sewing machines, 6,500 gallons of oil, 14,400 gallons of benzene, plumbing iron, 117 cases of crockery and glassware and many other manufactured items. The Falls of Halladale had been at sail for 102 days when, at 3 am on the night of 14th November 1908, under full sail in calm seas with a six knots breeze behind and misleading fog along the coast, the great vessel rose upon an ocean swell and settled on top of a submerged reef near Peterborough on the south-west Victoria’s coast. The ship was jammed on the rocks and began filling with water. The crew launched the two lifeboats and all 29 crew landed safely on the beach over 4 miles away at the Bay of Islands. The postmistress at Peterborough, who kept a watch for vessels in distress, saw the stranding and sent out an alert to the local people. A rescue party went to the aid of the sailors and the Port Campbell rocket crew was dispatched, but the crew had all managed to reach shore safely by the time help arrived. 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 valuable cargo was largely lost, despite two salvage attempts in 1908-09 and 1910. Further salvage operations were made from 1974-1986, during which time 22,000 slate tiles were recovered with the help of 14 oil drums to float them, plus personal artefacts, ship fittings, reams of paper and other items. The Court of Marine Inquiry in Melbourne ruled that the foundering of the ship was entirely due to Captain David Wood Thomson’s navigational error, not too technical failure of the Clyde-built ship. 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).Californian American rectangular blue roof slate, recovered from the wreck of the Falls of Halladale. flagstaff hill, warrnambool, shipwrecked-coast, flagstaff-hill, flagstaff-hill-maritime-museum, maritime-museum, shipwreck-coast, flagstaff-hill-maritime-village, californian blue roof slate, falls of halladale., californian blue roof slate, green american slate, slate, russell & co.