Showing 120 items matching fossil
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Churchill Island Heritage Farm
Photograph - Photograph of a half-buried skeleton
Churchill Island Heritage Farm has a large photograph collection dating from the nineteenth century. Photograph of a half-buried skeleton in sand in a corrugated iron shedCatalogue number on reverse in pencil.photograph, fossil -
Churchill Island Heritage Farm
Photograph - Photograph of a dinosaur skeleton's front arms
Churchill Island Heritage Farm has a large photograph collection dating from the nineteenth century. Photograph of a dinosaur skeleton's front arms behind a glass screen in front of a corrugated steel wallCatalogue number on reverse in pencil.photograph, fossil -
Coal Creek Community Park & Museum
Mudstone with wood
8348.1 - Roughly triangle-sided prism in shape; pieces of fossil wood; one face seems to have slip-surfaces. -
Coal Creek Community Park & Museum
Mudstone with woody fragments
8334.1 - Roughly oblong in shape mudstone with large woody plant fossil on one face, and small woody fragments on others. -
Orbost & District Historical Society
fossils
These were found at Red Bluff at Lake Tyers. Inspected by George Rawlings 6.2.2013.Two lumps of shell fossils. The smaller, .1, is a shell and the larger .2 is a cast of spondylus, a genus of bivalve molluscs, gasteropodes. This is in calcite.fossils shells red-bluff bivalve molluscs spondylus -
Coal Creek Community Park & Museum
Mudstone with plant fragments
8325.1 - Flattened mudstones, shaped like a square with one corner smoothly shaved away, and showing low-quality wood fossils -
Orbost & District Historical Society
shells, Lavell, Edgar and Alan, first half 20th century
Shells were collected by Edgar lavell and son, alan.The fossils paint a vivid picture of life below a sea that once covered parts of East Gippsland. They reflect the geological history of the area.Square shaped wooden display case with glass front. Holds a collection of fossil shells on cork. Shells are from the Middle Miocene Age.shells natural-history middle-miocene fossils -
Orbost & District Historical Society
fossils
Inspected by George Rawlings 6.2.2013.Fossils are among the most valuable sources of information about the Earth's history.Two fossils in Gippsland limestone. .1 has scallop shells - pectens .2 has calcified wood. Both are from the Miocene Era.fossils miocene scallops petrified-wood -
Orbost & District Historical Society
fossils
Three small fossils. .1 and .2 are corals. .3 is a gastropod - barnacle. They are from the Miocene Era. The inside structure of the coral can be seen.fossils gastropod-barnacle coral shell -
Greensborough Historical Society
Newspaper Clipping, Commuters support move to eco-friendly Vehicles and Cars, 02/12/2015
A community group supported Banyule Council's move to stop directly investing in companies allied to fossil fuels.News clipping, black text, colour image. Date written on pagemontmorency community group, banyule city council -
Orbost & District Historical Society
fossils
Inspected by George Rawlings 6.2.2012. Found at Toorloo Arm (near Lakes Entrance in East Gippsland).Three bowl-shaped fossils from the Miocene Era. They are Bryzoan types of coral. .1 is part of a shell. .2 is a cup coral and .3 is a coral.fossils coral miocene bryzoan -
Coal Creek Community Park & Museum
Mudstone with plant fossils
8340.1 - Grey, triangular, mid-large, thin mudstone contains carbonised plant fossils, most prominently a small, partial, but well preserved frond. -
Coal Creek Community Park & Museum
Large piece of mudstone with fossils
8318.1 - Roughly rectangular mudstone with fragments of fossil wood and plant matter, notably large ovoid cross section through a piece of fossilised wood. -
Flagstaff Hill Maritime Museum and Village
Book, Our Common British Fossils
This item is from the ‘Pattison Collection’, a collection of books and records that was originally owned by the Warrnambool Mechanics’ Institute, which was founded in Warrnambool in 1853. By 1886 the Warrnambool Mechanics’ Institute (WMI) had grown to have a Library, Museum and Fine Arts Gallery, with a collection of “… choice productions of art, and valuable specimens in almost every branch and many wonderful national curiosities are now to be seen there, including historic relics of the town and district.” It later included a School of Design. Although it was very well patronised, the lack of financial support led the WMI in 1911 to ask the City Council to take it over. In 1935 Ralph Pattison was appointed as City Librarian to establish and organise the Warrnambool Library as it was then called. When the WMI building was pulled down in 1963 a new civic building was erected on the site and the new Warrnambool Library, on behalf of the City Council, took over all the holdings of the WMI. At this time some of the items were separated and identified as the ‘Pattison Collection’, named after Ralph Pattison. Eventually the components of the WMI were distributed from the Warrnambool Library to various places, including the Art Gallery, Historical Society and Flagstaff Hill. Later some were even distributed to other regional branches of Corangamite Regional Library and passed to and fro. It is difficult now to trace just where all of the items have ended up. The books at Flagstaff Hill Maritime Village generally display stamps and markings from Pattison as well as a variety of other institutions including the Mechanics’ Institute itself. RALPH ERIC PATTISON Ralph Eric Pattison was born in Rockhampton, Queensland, in 1891. He married Maude Swan from Warrnambool in 1920 and they set up home in Warrnambool. In 1935 Pattison accepted a position as City Librarian for the Warrnambool City Council. His huge challenge was to make a functional library within two rooms of the Mechanics’ Institute. He tirelessly cleaned, cleared and sorted a disarrayed collection of old books, jars of preserved specimens and other items reserved for exhibition in the city’s museum. He developed and updated the library with a wide variety of books for all tastes, including reference books for students; a difficult task to fulfil during the years following the Depression. He converted all of the lower area of the building into a library, reference room and reading room for members and the public. The books were sorted and stored using a cataloguing and card index system that he had developed himself. He also prepared the upper floor of the building and established the Art Gallery and later the Museum, a place to exhibit the many old relics that had been stored for years for this purpose. One of the treasures he found was a beautiful ancient clock, which he repaired, restored and enjoyed using in his office during the years of his service there. Ralph Pattison was described as “a meticulous gentleman whose punctuality, floorless courtesy and distinctive neat dress were hallmarks of his character, and ‘his’ clock controlled his daily routine, and his opening and closing of the library’s large heavy doors to the minute.” Pattison took leave during 1942 to 1942 to serve in the Royal Australian Navy, Volunteer Reserve as Lieutenant. A few years later he converted one of the Museum’s rooms into a Children’s Library, stocking it with suitable books for the younger generation. This was an instant success. In the 1950’s he had the honour of being appointed to the Victorian Library Board and received more inspiration from the monthly conferences in Melbourne. He was sadly retired in 1959 after over 23 years of service, due to the fact that he had gone over the working age of council officers. However he continued to take a very keen interest in the continual development of the Library until his death in 1969. The Pattison Collection, along with other items at Flagstaff Hill Maritime Village, was originally part of the Warrnambool Mechanics' Institute’s collection. The Warrnambool Mechanics’ Institute Collection is primarily significant in its totality, rather than for the individual objects it contains. Its contents are highly representative of the development of Mechanics' Institute libraries across Australia, particularly Victoria. A diversity of publications and themes has been amassed, and these provide clues to our understanding of the nature of and changes in the reading habits of Victorians from the 1850s to the middle of the 20th century. The collection also highlights the Warrnambool community’s commitment to the Mechanics’ Institute, reading, literacy and learning in the regions, and proves that access to knowledge was not impeded by distance. These items help to provide a more complete picture of our community’s ideals and aspirations. The Warrnambool Mechanics Institute book collection has historical and social significance for its strong association with the Mechanics Institute movement and the important role it played in the intellectual, cultural and social development of people throughout the latter part of the nineteenth century and the early twentieth century. The collection of books is a rare example of an early lending library and its significance is enhanced by the survival of an original collection of many volumes. The Warrnambool Mechanics' Institute’s publication collection is of both local and state significance. Our Common British Fossils and Where to Find Them Author: J E Taylor, Ph D. F.G.S. Publisher: Chatto and Windus Date: 1885Label on spine with typed text PAT 560.942 TAY Pastedown end page has sticker from Warrnambool Mechanics Institute and Free Library Front loose endpaper has a sticker from Corangamite Regional Library Servicewarrnambool, shipwrecked-coast, flagstaff-hill, flagstaff-hill-maritime-museum, maritime-museum, shipwreck-coast, flagstaff-hill-maritime-village, shipwrecked-artefact, book, warrnambool mechanics’ institute, pattison collection, warrnambool library, ralph eric pattison, warrnambool city librarian, mechanics’ institute library, victorian library board, warrnambool books and records, warrnambool children’s library, our common british fossils, j e taylor -
Coal Creek Community Park & Museum
Mudstone with leaves
8352.1 - Irregularly-shaped mudstone with some waved faces, displaying partial leaf fossils, prominently a nearly-totally carbonised taeniopteris leaf on one face. -
Coal Creek Community Park & Museum
Mudstone with fossils and secondary minsral
8343.1 - Irregularly shaped grey mudstone containing some carbonised plant fragments, but most prominently (most likely) secondary iron mineralisation pseudo fossils -
Coal Creek Community Park & Museum
Mudstone fossils
8326.1 - Medium-to-small mudstone in roughly prismatic shape, displaying numerous small plant leaf fossils, and possibly a prominently rounded conerstion on one face. -
Orbost & District Historical Society
coral
This fossil was possibly found in a quarry near the top of Mt Raymond near Orbost. Crushed rock was quarried from a government quarry ther.A lump of fossilised coral in limestone rock.fossil coral mount-raymond -
Coal Creek Community Park & Museum
Broken mudstone with leaves
8357.1 - Large piece of mudstone broken perpendicular to longest axis into two almost-exact-sized pieces; break bifurcates leaf fossils apparent on both largest faces. -
Coal Creek Community Park & Museum
Mudstone containing woody matter
8339.1 - Large, though thin almost rectangular mudstone containing numerous small fragments of carbonised plant matter (one large piece in particular) and some fossil leaves. -
Clunes Museum
Container - ENGRAVING & BOX
INFORMATION ON BOX LID-THE ENCLOSED IMPRESSION EXHIBITS A LIKENESS OF THE REV. JOHN WESLEY, ENGRAVED ON A FOSSIL ECHINUS, OR SEA-EGG, IN THE POSSESSION OF MR. JOHN HEY OF LONDON. THE CLEVER ARTIST WHOSE WORK IT IS, PRONOUNCED THE STONE TO BE HARDEST HE HAD EVER ENGRAVED.A LIKENESS OF THE REV. JOHN WESLEY, ENGRAVED ON A FOSSEL ECHINUS, OR SEA-EGG. IN A SMALL BOX"THE WORLD IS MY PARISH"engraving, wesley, rev john wesley -
Warrnambool and District Historical Society Inc.
Book, Star Printing Service Pty Ltd, Dear Adam and Jasmine, 2015
This book contains information on the environmental problems facing the world. The effects of climate change, over-population and fossil-fuel use are discussed and some alternatives to coal production and the use of nuclear power for peaceful purposes and for defence are proposed. The book has been written for, and is dedicated to, the author’s grandchildren. This book is retained as it was written by Graham Keith, a local Warrnambool resident who has had considerable experience in the engineering field.This is a soft cover book of 158 pages. It has a blue cover with black printing on the front and a colour photograph of two children on the back. The book has 18 chapters of text and an index. The book contains some black and white photographs and a sketch. environmental issues, warrnambool -
Coal Creek Community Park & Museum
Cloven pseudofossil
Formed by sedimentary processes. 8312.1 - Rock split in half lengthways, revealing in both kidney-shaped halves a sedimentary concretion, itself split into un equal halves via cross-sectional fractures. The larger concretion fragment reveals a small carbonised plant fossil. -
The Beechworth Burke Museum
Geological specimen - Actionlite and Pyrite
Actinolite is usually found in metamorphic rocks, such as contact aureoles surrounding cooled intrusive igneous rocks. It also occurs as a product of the metamorphism of magnesium-rich limestones. Pyrite is usually found with other sulfides or oxides in quartz veins, sedimentary rock, and metamorphic rock, as well coal beds, and as a replacement mineral in fossils. Actinolite is an amphibole silicate mineral. It is named after the Greek word "aktinos" meaning “ray” in allusion to the mineral's fibrous nature. Fibrous actinolite is a type of asbestos and was once mined along Jones Creek at Gundagai, New South Wales. Pyrite or "Fool's Gold" is the most common sulfide mineral. It is named after the Greek "pyr" meaning "fire" because it can be used to create sparks needed for a fire if struck against metal or a hard surface. Due to its gold colour, pyrite can be mistaken for gold and often forms alongside it, causing small amounts of gold to be present in rocks containing pyrite. Most importantly, pyrite is an ore of gold. Pyrite is sometimes used as a gemstone but is not great for jewellery as it easily tarnishes. In some fossils of ammonites – shelled cephalopods that died ~66 million years ago – pyrite also replaces the shell. 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-medium-sized solid specimen with the minerals actinolite (dark green fibrous) and pyrite (brassy) with shades of brown, black/grey, and white. Actinolite is an amphibole mineral in the tremolite-actinolite series of calcium, magnesium, and iron silicates. Pyrite is an iron disulfide mineral.geological specimen, geology, geology collection, burke museum, beechworth, indigo shire, geological, mineralogy, pyrite, actinolite, victoria, sewyln, alfred selwyn -
The Beechworth Burke Museum
Geological specimen - Fossiliferous Mudstone, Unknown
This specimen was found in Cape Patterson, Vic. Cape Paterson is a cape and seaside village located near the town of Wonthaggi, 132 kilometres southeast of Melbourne, in the Bass Coast Shire of Gippsland, Victoria, Australia. These dark, fossiliferous Mudstones were deposited in slow-moving water associated with sedimentary basins & continental shelves. They are rich in carbon which makes them almost black. This is typical of an anoxic, reducing environment such as deep water or stagnant conditions where carbon-rich material would remain unoxidised during subsequent deposition & diagenesis. it has an imprint of a leaf in the rock itself, displaying the fossil of the plant. This specimen is unique due to the leaf impression within the stone itself. Imprint fossils are formed from an organism moving in some way, leaving behind a trace or track. These tracks are preserved when the clay/silt dries slowly and is covered by other sediment. Plants can also leave imprint fossils when they are covered by sediment. The leaf tissue degrades, leaving an imprint of where the leaf once was. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.These dark, fossiliferous Mudstones were deposited in slow moving water associated with sedimentary basins & continental shelves. They are rich in carbon which makes them almost black. This is typical of an anoxic, reducing environment such as deep water or stagnant conditions where carbon rich material would remain unoxidised during subsequent deposition & diagenesis. FOSSILIFEROUS MUDSTONE / Locality: Cape Patterson, Victoria | Descriptive catalogue / Pg 27 No 95 / "Grey Clay, / Cape Paterson with leaf impressions' / 15/4/21 C. William /mudstone, cape patterson, leaf imprint, fossilised leaf, fossiliferous mudstone -
Federation University Historical Collection
Book, Prodromus of the Palaeontology of Victoria No iv, 1876 (exact)
This publication consists of many Decades which contain "figuers and descriptions of the fossil organic remains to be used for the determination of the geological ages of the different geological formations of the country." (p. 3). Frederick McCoy was born in Dublin, Ireland in 1817. He was a Professor of Natural Sciences, University of Melbourne 1854-1899. McCoy lectured in geology, zoology, chemistry, mineralogy, geography and botany. In 1858 He became the Director of the National Museum of Victoria and the President of the Royal Society of Victoria in 1864. In 1888, McCoy was awarded FRS for work in Palaeontology in Ireland, England and Australia. He died in his office while correcting examination papers in 1899A Paperback cover book. Decade IV. Title is written in black on front cover and on title page. At head of title: Geological Survey of Victoria. Illustrations, plates in b/w; 32 p. It includes figures and descriptions of Victorian Organic Remains and contents of Decades on the back cover of the book.australia palaeobotany, victoria palaeontology, geological survey of victoria, frederick mccoy, organic remains -
Federation University Historical Collection
Book, Prodromus of the Palaeontology of Victoria, 1877 (exact)
This publication consists of many Decades which contain "figuers and descriptions of the fossil organic remains to be used for the determination of the geological ages of the different geological formations of the country." (p. 3). Frederick McCoy was born in Dublin, Ireland in 1817. He was a Professor of Natural Sciences, University of Melbourne 1854-1899. McCoy lectured in geology, zoology, chemistry, mineralogy, geography and botany. In 1858 He became the Director of the National Museum of Victoria and the President of the Royal Society of Victoria in 1864. In 1888, McCoy was awarded FRS for work in Palaeontology in Ireland, England and Australia. He died in his office while correcting examination papers in 1899.A Paperback cover book. Decade v. Title is written in black on front cover and on title page. At head of title: Geological Survey of Victoria. Illustrations, plates in b/w; 41 p. It includes figures and descriptions of Victorian Organic Remains and contents of Decades on back cover.Stamped Ballarat East Public Library"australia palaeobotany, victoria palaeontology, geological survey of victoria, frederick mccoy, organic remains, ballarat east library, ballarat east public library -
Federation University Historical Collection
Book, John Ferres, Government Printer, Prodromus of the Palaeontology of Victoria Decade vi, 1878 (exact)
This publication consists of many Decades which contain "figuers and descriptions of the fossil organic remains to be used for the determination of the geological ages of the different geological formations of the country." (p. 3). Frederick McCoy was born in Dublin, Ireland in 1817. He was a Professor of Natural Sciences, University of Melbourne 1854-1899. McCoy lectured in geology, zoology, chemistry, mineralogy, geography and botany. In 1858 He became the Director of the National Museum of Victoria and the President of the Royal Society of Victoria in 1864. In 1888, McCoy was awarded FRS for work in Palaeontology in Ireland, England and Australia. He died in his office while correcting examination papers in 1899.A Paperback cover book. Decade VI. Title is written in black on front cover and on title page. At head of title: Geological Survey of Victoria. Illustrations, plates in b/w; 42 p. It includes figures and descriptions of Victorian Organic Remains and contents of Decades at back of the book.australia palaeobotany, victoria palaeontology, geological survey of victoria, frederick mccoy, organic remains, john ferres -
Federation University Historical Collection
Book, Cassell, Petter, Galpin & Co, Popular Educator Vol. 5
Green/black clothcovered book of 412 pages. Includes illustrations and topics such as Knights Templar, Red Cross Knights, Lesson in Architecture, botany, arithmetic, algebra, static forces, Cambridge University, chemistry, latin, Euclid, fossils, geology, Greek, Electricity, German, Organic Chemistry, shells, pearls, North America, nightshades, the Thirty Years War, commerce, reflection of light, book-keeping, mosses, South America, hydrostatics, camera obscura, London UniversityStamped 'Springs Public Libray'cambridge university, knights templar, red cross knights, organic chemistry, north america, thirty years war, south america, camera obscura, london university, springs public library -
The Beechworth Burke Museum
Geological specimen - Slice Dendrites on Sandstone, Unknown
Dendrites are deposits of black minerals, typically manganese oxides that precipitated from water seeping through fractures in fine-grain rocks like a sandstone or limestone. Dendrites are much less regular than plant fossils and lacks vein structures. The manganese cryztallizes through the process called 'supercooling'. Some samples of dendrites occur in volcanic rocks in the Lilydale district, east of Melbourne. Sandstones are made of tiny sand grains that may have been deposited in the sea and later formed together. Most sandstones are made of quartz which are chemically-resistant minerals. This particular specimen was donated by Alfred Selwyn in 1868 as part of the Geological Survey of Victoria. It is connected to the original 1875 catalogue on Geological Specimen with number 189 'Quartz Crystals_Quartz Crystals (two are polished)'Dendrites on sandstones This specimen is an important contribution to the geological history of Victoria, as well as its links to the 1868 Geological Survey of Victoria. This specimen is part of larger collection of significant geological specimens in the Burke Museum that was collected from around the world between 1868-1880. A large percentage of these specimens were collection as part of the Geological Survey of Victoria 1852-1974. The Geological Survey of Victoria was an organisation founded in response to the Victorian gold rush to explore the geological and mineral resources and to record a detailed map of the state. It 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 hand-sized slice of light brown sandstone with dendrites formed from crystallized manganese oxide.Existing label: Not sure what / 'Slica dondrites' / means. / Sample is sandstone and original label / identifies it as from / the Grampians near Stawell. / C. Willman / 15/4/21 Other label: [illegible] / stone [ illegible] / from Grampians Stawell / 1894 /geological specimen, geology, geology collection, burke museum, beechworth, dendrites, sandstones, quartz, lilydale district, geological survey of victoria, grampians, victoria rocks, minerals, rocks, manganese oxides, alfred selwyn