Inspected by George Rawlings on 6.12.2013. This fossil was probably found at the Newmerella cutting.Fossils are among the most valuable sources of information about the Earth's history. This fossil is part of the geological history of the Orbost area.A gastropod fossil from the Miocene Era.fossils gastropods shells

Photograph of a stone with a fossil imprint found by Mr Des Johnson in Goodman Creek bed in Comaida district.fossil

NoneAbstract image. Centre image is a human (shown without skin) climbing a narrow mound/hill form. At the top is a screen supported by three poles. The screen reproduces a photograph of what appears to be a classical narrative bas-relief sculpture. On each side of the hill are Celtic and Norse carvings/gilded artefacts/metalworks mounted on long poles. Abstract could patterns are at the top of the print. No matt. Silver metal frame.Front: 1/10 (lower left) Ikon to a Fossil King (lower centre) Allan Mann (lower right) (pencil) Back: (no inscriptions)

This fossil was found by Peter Cook just west of East Cape at Cape Conran (east of Orbost),. Original correspondence re its identification came from Andy Murray - Conservation & Natural Resources, Orbost. It was on display at the Orbost Visitor Information Centre - the Slab Hut.A fossil tooth from a marine species. It may be from a an extinct ziphiid or beaked whale (Warneke Marine Mammal Services 20.10.1993). It may be a fossil from a large species of subadult seal (Ewan Fordyce Senior Lecturer in Geology, University of Otago 11.10.1993).fossil-tooth whale seal marine cape-conran

Coloured LinocutSigned and dated 'A. ORTON 1999' in lower right corner under printed image. Titled 'Fossil Landscape' centred under print. Edition in lower left corner under printed image - illegible.

Inspected by George Rawlings 6.2.2013. It is a fossil of a Murray Cod (maccullochella macquariensis) from diatomaceous earths in New South Wales.A very fragile chalk fossil of a fresh water fish. It is aged about 20 million years and was found in the locality of a chalk mine at Bugaldie in New South Wales (near Coonabarrabran).fossil murray-cod chalk-mine bugaldie

This limestone rock containing many marine fossils, crustacean imprints and embedded shells, bivalves, and two imprints of spiny oyster, Pelecypos and Spondylus from the Miscene Age 10-20 million years BP. It was collected in the Orbost region, possibly at Newmerella when the railway was being constructed in 1915-16. An example of marine fossils, collected near Orbost. this fossil is part of the geological history of the Orbost area.A large piece of yellow/ochre coloured rock (East Gippsland limestone) containing many marine fossils. marine-fossils miscene-fossils east-gippsland-fossils

Found at Newmerella. Inspected by George Rawlings 6.2.2013Fossils are among the most valuable sources of information about the Earth's history. This fossil is part of the geological history of the Orbost district.A gastropod fossil from the Miocene Era.gastropod fossil miocene

Found at Point Hicks. Probably part of the root of the tree. This is a type of petrified wood that has had all of the wood cells replaced with calcite mineral. After exposure to the ultraviolet light of the sun for a few years, the petrified wood has turned dark. Inspected by George Rawlings 6.2.2013.One piece of fossil of a calcified tea tree.fossil tea-tree petrified-wood calcification

Inspected by George Rawlings 6.2.2013Fossils are among the most valuable sources of information about the Earth's history.Half of a gastropod fossil - cypraea. Possibly limestone from the Myocene era.fossil gastropod cypraea cowrie shell

Inspected by George Rawlings 6.2.2013A gastropod fossil which is probably Gippsland limestone from the Myocene Era.fossil gastropod myocene

Fossils are among the most valuable sources of information about the Earth's history.A fossil of a fern -probably a cycad from the Triassic Period. Order - cycadales.fossil fern cycad

Inspected 6.2.2013 by George Rawlings and confirmed.A large shell fossil. Genus Pterospira. Species Validostrata .Gippsland limestone.fossil pterospira validostrata

Inspected by George Rawlings 6.2 2013.A piece of rock which is calcified vegetation.fossil

Inspected by George Rawlings 6.2.2013.Fossils are among the most valuable sources of information about the Earth's history.A large oyster shell fossil from the Miocene Era. There is evidence of borers. It is a Mother-of-Pearl flap.oyster fossil mother-of-pearl miocene

Estimated date: c. 40 million years ago.Fossil cycad frond. Name: Pterostoma Zamioiedes Hill (possibly in the Zamiaceae family or even a separate one).cycad, pterostoma zamioiedes hill, alcoa power station

Found at the Pyramids , Buchan. Inspected by George Rawlings on 6.2.2013.A heavily calcified fossil rock. Genus Spinella Buchanesis . Devonian age 419.2–358.9 million years ago. It contains blastoids from the echinoid family.fossil spinella buchan devonian

Local Tutor in ceramicsGlazed Ceramic

My sculpture, Fossil, is a ‘skeleton’ of a tree trunk, constructed in stainless steel. Depicted in a ruined state, the trunk has been ‘broken’ from the top. While Fossil acknowledges architecture through the use of the constructed cross-bracing motif, its primary reference is to the Romantic artists’ use of the solitary ruined tree in the Sublime landscape. The heroic decay of mighty trees is a subject explored by painters and photographers of the mid nineteenth century who were searching for the ‘picturesque’. A solitary, damaged tree stands as evidence of the physical power of the landscape and natural forces such as storms and lightning strikes. It is trying to suggest itself to be an archaeological artifact of the future, a fossil of the future that speaks of how we view the world’s natural resources at this point in time. public art

Inspected by George Rawlings 6.2.2013. Gastropods are molluscs which include snails and slugs, living in fresh water or the sea. These fossils are possibly from the Newmerella cutting.Three small gastropod fossils from the Miocene Era.fossils gastropods shells

A fossil refers to any remains or traces of past life that are preserved in the rock. It could be remains of plants or animals. Fossil leaves are commonly found on different types of rocks. These fossils can go as far back as the Triassic Age just like the series of fossil plants collected at Denmark Hill, Ipswich in Queensland. Fossils leaves are formed when dead plants get buried by sediments like mud, sand, or volcanic ash. Often, it gets detached cleanly from stems along a special layer of weak cells, then twigs, and, less commonly, cones of conifers and fruits and seeds of flowering plants. Over time, the leaves or pieces of leaves get buried by more sediments and eventually gets 'lithified' or hardened into a rock. Erosions and mining can cause the rocks to break and reveal the fossils buried in it. Fossilisation frequently takes place at sites in the lowlands where deposits of clay, silt, sand are found. This is usually due to weathering and erosion of rocks. Fossil leaves can provide information about ancient Australia's way of living. It contributes to Victorian biodiversity records and its botanical collections. It also contributes information on the geographical profile of Victoria as fossilisation usually occur at estuaries and deltas of rivers, river flood plains, ponds and lakes. 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.Piece of light brown rock with fossilised leaves in shades of golden yellow and brown.Existing label: Fossil Leaves / Locality unknown / might be worth checking if this is Glossopteris, a Permian age plant. / C. William 16/4/21 geological specimen, geology, geology collection, burke museum, beechworth, fossil leaves, fossilization, 1868 geological survey of victoria, lithified, rocks, fossilised leaf, rock, fossils, leaves

The fossil was found by Mrs. D. Lee in 1983 in Jacksons Creek near the Palmas Reserve.A fossil of a small shell in a layer of sedimentary rock, which has formed above basalt rock.fossils, shells, jacksons creek, sunbury

Inspected by George Rawlings on 6.2.2013. The smaller fossil is related to the modern starfish, has 5 petals, secreted eggs from holes at the top. The mouth was underneath with rows of teeth. 1641.1 is a large sea urchin fossil (echinoderm) originally covered in spines. It is possibly from Turkey and 4 million years old. Modae Louisato 1641.2 is a smaller sea urchin fossil - echinoidius gippslandicus

This booklet contains an article on the plant fossil deposits in Eastern Victoria. It has been written by Dr John Douglas in 1963. He published extensively on a range of geological and natural history themes. His major works included co-editing the Geological Society of Victoria’s Geology of Victoria and his PH.D. thesis for the University of Melbourne contained in two Geological Survey Memoirs on the Mesozoic floras of Victoria. He was also responsible for the Geology and Sport and Recreation chapters in the State Government’s Atlas of Victoria and wrote the booklet, What Fossil Plant is That? He was a Supervising Geologist with the Department of Minerals and Energy in Victoria for many years and lectured extensively at Botany and Geology conferences in Australia and overseas. This book is of some interest as it was written by a former resident of Warrnambool, Dr John Douglas (1997 to his death in 2007). He was an active member of the Warrnambool Field Naturalists’ Group and edited for this group the book, The Nature of Warrnambool. This is a small booklet of 16 pages reprinted from the Proceedings of the Royal Society of Victoria, Vol. 77, Part 1. It has a grey cover with the logo of the Royal Society of Victoria on the front cover. It has printed material on plant fossil deposits in eastern Victoria and several sketches and black and white plates of plant fossil photographs and cross-sections. The pages were stapled but the staples have been removed. There is some rust where the staples were removed. Front cover: ‘Royal Society of Victoria, New Bennettitalean Leaves from the Mesozoic of Eastern Australia by J. G. Douglas, reprinted from Proc. Roy. Soc. Victoria, Vol 77, Part 1, Issued separately, 13 December, 1963.’ micro- paleontology in eastern victoria, dr john douglas, warrnambool

Inspected by George Rawlings 6.2.2013.Fossils are among the most valuable sources of information about the Earth's history.A piece of conglomerate rock with shell (nautiloid?) and coral from the Miocene Era.fossil conglomerate miocene coral nautiloid

Inspected by George Rawlings 6.2.2013.A fossilised worm casting., as in a beach or sand worm of a large variety. The worm secretes organic substances that harden in the burrow and the ejected material is called castings.fossil worm-casting

Fossils are among the most valuable sources of information about the Earth's history.Three fossils. The largest .1 is a giant cowrie. Genus cucullata, species corioensis. The two smaller fossils are conus catus.fossils shells giant-cowrie cucullata conus-catus

Inspected by George Rawlings 6.2.2013.Fossils are among the most valuable sources of information about the Earth's history.Two gastropod fossils. Spiral shells.fossils gastropods shells