Showing 517 items matching museum studies
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Federation University Historical Collection
Photograph - Colour, Deakin University Museum Studies Students of 1994-1997 Reunion, 09/10/1998
... Deakin University Museum Studies Students of 1994-1997...museum studies...Deakin University Museum Studies students of 1994-1997... Museum Studies. Names of people printed under the photograph... Photograph - Colour Deakin University Museum Studies Students of 1994 ...Deakin University Museum Studies students of 1994-1997 at the Old Castlemaine Gaol to celebrate 20 years of Museum Studies, 1979-1998. Most attendees arrived at Castlemaine on board a Steam train. In the back row is Clare Gervasoni who was the curator of the Federation University Art and Historical Collection.Coloured photograph mounted in a presentation folder showing students of 1994-1997 attendees at the Deakin University Museum Studies. Names of people printed under the photographmuseum studies, deakin university museum studies, margaret birtley, anne kewshaw, chris keeler, clare gervasoni, castlemaine gaol, rachel faggoter -
Moorabbin Air Museum
Document (Item) - Collection of Academic Theses Relating to Museum Studies, Notes on Caring for Collections
... Collection of Academic Theses Relating to Museum Studies... research on museum studies.... research on museum studies. Three large yellow envelopes containing ...The three theses relate to the Post Office Museum in Melbourne (by Sarah Therese Murphy), the collections of Barry Humphries and Dame Edna Everage (by Diane Soumilas), and the preservation of watercolour paintings (by Peter John Struthers). They may have been kept by Kevin Kerle as part of his own thesis research on museum studies. -
Moorabbin Air Museum
Document (Item) - Two copies of Kevin Kerle's Thesis Relating to Interpretation of Aircraft at Museums, Kevin Kerle, Thesis for Graduation in Diploma in Museum Studies by Kevin Kerle (1987), 1987
... Thesis for Graduation in Diploma in Museum Studies by Kevin...The thesis aims to show museums how they can create a more ...The thesis aims to show museums how they can create a more interactive and interpretive experience, connecting their audience with the aircraft on display.This thesis was written by an important donor to the museum, and contains useful advice for all aviation museums. -
University of Melbourne, Burnley Campus Archives
Document, Museum Collection, 1991
... museum studies...Correspondence with Victoria College Rusden re Museum... Correspondence with Victoria College Rusden re Museum Studies students ...Correspondence with Victoria College Rusden re Museum Studies students working with Burnley historical collection on 3-day projectmuseum collection, museum studies, rusden, students -
Whitehorse Historical Society Inc.
Photograph, Deakin students at Whitehorse Historical Society, 6th/03/2011
... are studying museum practice being shown museum practices and display... Deakin students who are studying museum practice being shown ...4 coloured photographs (a-d) showing Deakin students who are studying museum practice being shown museum practices and display methodsdeakin students, whitehorse historical society -
City of Moorabbin Historical Society (Operating the Box Cottage Museum)
Certificate - Certificate of General Nursing - Mary Beatrice Josephine Maggs, 1919
Mary Beatrice Josephine Maggs (1892-1960) came to Australia in 1914 and was a governess for Mr Alfred Rutter Clarke at his mansion "Merriwa" on Orrong Road, Toorak. Mary returned to England in 1919 and furthered her studies in nursing. When she returned to Australia in 1924 she was head nurse at a number of Hospitals, Private Hospital in Loch, Tatura Bush Nursing Home, Mooroopna. Certificate of General Nursing 1919 of Mary B MaggsThe Royal Victorian Trained Nurses Association / CERTIFICATE FOR GENERAL NURSING / Signed by President, Member of Council, Secretarymaggs mary, medicine, nursing, thompson jean, hospitals, early settlers, pioneers, melbourne hospital -
City of Moorabbin Historical Society (Operating the Box Cottage Museum)
Photograph, B/W Laminated of August Rietman Family c 1918, c1918
August Rietmann 1877-1951 and his wife Frieda 1878-1942 leased the Box Cottage in 1917 and raised 2 children Stefanie 1918-2006, and William 1920– 1997. August was a Monumental Mason / Potter / Sculptor and he was employed at Corbens Ltd Clifton Hill, to make the War Memorials for many towns post WW1. August purchased the property 1935,and established a pressed concrete business using the cottage as a workshop and storeroom After August died in 1951, William, his son, continued to work in the business from the site until the land was sold to Lewis Co. Ltd Timber Merchants in 1970. Rietman's Landscaping Ltd , managed by William's family, moved to Bay Road Highett 1953 and later to Carrum. The original small, pioneer cottage was built in the late 1840s to early1850s, by an unknown pioneer. It was located on part of a 30 Acre allotment that was originally part of Dendy’s Special Survey granted in 1841. The doors and window sashes, (made of red deal joinery timber), as well as the brass locks and fittings, are from the original cottage, and were imported from England. The fire-place bricks are from the original cottage, and are sun-dried, (not kiln fired), and are hand-made. Convict marks can be seen on two bricks. There is a small display of external cladding shingles from the original pioneer cottage. These shingles were hand-split, and most likely made from locally collected timber The nails included in this display were used to fasten the shingles on the original cottage, and are also hand-made. The cottage was occupied by William Box and family from 1865 until 1914 when it was sold to August Rietman . The enamel nameplate, “Colonial”, on the wall of the cottage, was the name chosen for the original pioneer cottage by Mr August Rietman, when he purchased the property in around 1915, for 1200 Pounds approximately. In 1974 Mr Lewis, a timber specialist, found the dilapidated building on property he had recently purchased in Jasper Rd and suggested it be reconstructed and relocated. Moorabbin Council agreed and the cottage was rebuilt just about 250 metres from its original site. The cost of the rebuild was met by 'Victoria's 150th Committee, plus a small grant from the City of Moorabbin, and Mr Laurie Lewis donated much of the timber for the reconstruction. The re-constructed cottage plan has followed faithfully the original dimensions, and plan of the original pioneer cottage, and as many original items from that cottage’s long occupation have been incorporated. The photographs in Album 1 record the progress of the reconstruction from February 1984 to the First Public Open Day November 18th 1984After the death of Elisa Box in 1914 the house was leased to August Rietmann, a potter / sculptor who with his wife Fieda raised their family there 1917 - 1951. Stefanie Rennick nee Rietman lived at the house until she left to study teaching 1937. August's son, William Rietman and family managed Rietman's Landscaping Ltd after moving to Bay Road Highett 1953 and later to Carrum. The Lewis Timber Company Ltd purchased the land with The Cottage c1970. i) A laminated, black and white, photograph of August Rietmann and Family c1918 at Box Cottage, Ormond, Molly the house cow is in foreground ii) Colour photograph of Rietman's Landscaping Ltd. Bay Road Highett c 1990brighton, moorabbin, cottages, pioneers, ormond, colonial, mckinnon, dendy henry, box william, box elizabeth, reitman august, convicts lewis timber co. ltd., deam h, museums, box alonzo, smith a, rietmann august, rietman august, rietmann frieda, rietman frieda, stonnington city town hall, war memorials, world war 1 1914-1918, rietman stefanie, rennick stefanie, francis stefanie, rietman william, rietman ray, mountford paul, malvern city town hall, box cottage museum ormond, joyce park ormond, rietman's landscaping pty ltd, bay road highett, macrobertson pty ltd, coleraine soldier memorial 1921, dendy, rietman agust, convicts, macrobertson, war memorial -
City of Moorabbin Historical Society (Operating the Box Cottage Museum)
Booklet - The Ridgway First Aid Chart - The Ridgway Society, c 1911
The Ridgway Society provided this booklet with a medical cabinet. "The Remedies in this Cabinet and the Dressings, will enable you to so care for minor injuries, that they will not develop into serious ones, and a study of the Chart will provide you, and your sons and daughters, with practical useable information, that will enable them to help their fellow men in distress, wherever they may be." 19 page document with instructions on how to treat medical emergencies and conditions, with illustrations and photos.first aid, medical, emergencies -
City of Moorabbin Historical Society (Operating the Box Cottage Museum)
Certificate - The Melbourne Hospital Certificate, Mary Beatrice Josephine Maggs
Mary Beatrice Josephine Maggs (1892-1960) came to Australia in 1914 and was a governess for Mr Alfred Rutter Clarke at his mansion "Merriwa" on Orrong Road, Toorak. Mary returned to England in 1919 and furthered her studies in nursing. When she returned to Australia in 1924 she was head nurse at a number of Hospitals, Private Hospital in Loch, Tatura Bush Nursing Home, Mooroopna.Certificate of Nursing 8 July 1918The Melbourne Hospital - Melbournemaggs mary, medicine, nursing, thompson jean, hospitals, early settlers, pioneers, melbourne hospital -
City of Moorabbin Historical Society (Operating the Box Cottage Museum)
Certificate - General Nursing Council for England and Wales Certificate England, Mary Beatrice Josephine Maggs, 20 July 1923
Mary Beatrice Josephine Maggs (1892-1960) came to Australia in 1914 and was a governess for Mr Alfred Rutter Clarke at his mansion "Merriwa" on Orrong Road, Toorak. Mary returned to England in 1919 and furthered her studies in nursing. When she returned to Australia in 1924 she was head nurse at a number of Hospitals, Private Hospital in Loch, Tatura Bush Nursing Home, Mooroopna.Certificate of General NursingGeneral Nursing Council for England and Walesmaggs mary, medicine, nursing, thompson jean, hospitals, early settlers, pioneers, melbourne hospital -
City of Moorabbin Historical Society (Operating the Box Cottage Museum)
Certificate - City of London Maternity Hospital May 1920, Mary Beatrice Maggs, 18 May 1920
Mary Beatrice Josephine Maggs (1892-1960) came to Australia in 1914 and was a governess for Mr Alfred Rutter Clarke at his mansion "Merriwa" on Orrong Road, Toorak. Mary returned to England in 1919 and furthered her studies in nursing. When she returned to Australia in 1924 she was head nurse at a number of Hospitals, Private Hospital in Loch, Tatura Bush Nursing Home, Mooroopna.CertificateCity of London Maternity Hospitalmaggs mary, medicine, nursing, thompson jean, hospitals, early settlers, pioneers, melbourne hospital -
City of Moorabbin Historical Society (Operating the Box Cottage Museum)
Certificate - Certificate of Registration Midwives Board of Victoria 1925, Mary Beatrice Josephine Maggs, 4 September 1925
Mary Beatrice Josephine Maggs (1892-1960) came to Australia in 1914 and was a governess for Mr Alfred Rutter Clarke at his mansion "Merriwa" on Orrong Road, Toorak. Mary returned to England in 1919 and furthered her studies in nursing. When she returned to Australia in 1924 she was head nurse at a number of Hospitals, Private Hospital in Loch, Tatura Bush Nursing Home, Mooroopna.maggs mary, medicine, nursing, thompson jean, hospitals, early settlers, pioneers, melbourne hospital -
City of Moorabbin Historical Society (Operating the Box Cottage Museum)
Certificate - Central Midwives Board Certificate England August 1920, Mary Beatrice Josephine Maggs, 14 August 1920
Mary Beatrice Josephine Maggs (1892-1960) came to Australia in 1914 and was a governess for Mr Alfred Rutter Clarke at his mansion "Merriwa" on Orrong Road, Toorak. Mary returned to England in 1919 and furthered her studies in nursing. When she returned to Australia in 1924 she was head nurse at a number of Hospitals, Private Hospital in Loch, Tatura Bush Nursing Home, Mooroopna.maggs mary, medicine, nursing, thompson jean, hospitals, early settlers, pioneers, melbourne hospital, midwives registration, midwives -
City of Moorabbin Historical Society (Operating the Box Cottage Museum)
Leisure object - The Rose Stereograph Cards, Coronation of King George V, 1911
This collection of Stereograph card depicts scenes from the Coronation of King George V. Produced by 'The Rose Stereographs. George Rose was born in Clunes, Victoria in 1861 and later worked in his father’s boot-making business in Prahran while studying photography. In 1880 he founded the Rose Stereograph Company and became famous for producing stereographs, or stereoviews, which gave the illusion of being in 3D when seen through a hand-held viewer. Some of the pioneers of Moorabbin were staunch supporters of the Monarchy of England. This collection of cards was donated by one of the founding pioneer families.Stereograph cards - 25 cards produced by Rose Stereographs. - black and whiteDescription of each card written on bottomcoronation, king george v, england, monarchy, moorabbin, london, westminster abbey, trafalgar square, boy scouts, crystal palace, queen mary -
City of Moorabbin Historical Society (Operating the Box Cottage Museum)
The Rose Stereograph Cards, Various pictures of European sites, 1911
This collection of Stereograph card depicts scenes from various Euopean sites and buildings. Produced by 'The Rose Stereographs. George Rose was born in Clunes, Victoria in 1861 and later worked in his father’s boot-making business in Prahran while studying photography. In 1880 he founded the Rose Stereograph Company and became famous for producing stereographs, or stereoviews, which gave the illusion of being in 3D when seen through a hand-held viewer.Collection of one of the pioneer families of City of Moorabbin.11 Stereographic Cards - manufactured by The Rose Sterographics - Black and whiteDescription of each card on the bottomeurope, paris, church of mary magdalene, the louvre, cathedral of notre dame, palace of justice, palace of beautiful arts, champs elysees, boulevard du nord, jules anspach fountain, brussels belgium, cathedral of st gudule, brussels, moorabbin, stereograph cards -
City of Moorabbin Historical Society (Operating the Box Cottage Museum)
Photograph, Stefanie Rennick nee Reitman, c1990
'Box Cottage' is so named after the first recorded family to establish a house and market garden on the site in 1865. William and Elizabeth Box. After the death of Elizabeth Box in 1914 the house was leased to August Reitman a potter / sculptor who raised his family there 1917 - 1953. Stefanie Rennick nee Reitmann lived at the house until she left to study teaching. The Lewis Timber Company Ltd acquired the land with The Cottage c1970. The CMHS together with City of Moorabbin Council, a 150 Year Celebration Grant and assistance from Lewis Timber Merchants Pty Ltd reconstructed the original 'Box Cottage' on its present site May 1984. August Reitman 1877-1951 and his wife Frieda 1878- 1942 raised 2 children Stefanie 1918-2006 and William 1920-1997 whilst living at the Box Cottage site. .August was a monumental mason and sculptor and was employed to carve war memorials in Victoria after WW1. He moved his business to Highett in 1953 but continued to use the cottage as a workshop until he sold the property to Lewis Timber P/L c 1970. . William and his descendants have continued the family business to the present day. August Reitman 1877-1951 and his wife Frieda 1878- 1942 raised 2 children Stefanie 1918-2006 and William 1920-1997 whilst living at the Box Cottage site. .August was a monumental mason and sculptor and was employed to carve war memorials in Victoria after WW1. He moved his business to Highett in 1953 but continued to use the cottage as a workshop until he sold the property to Lewis Timber P/L c 1970. . William and his descendants have continued the family business to the present day. Stefanie Rennick , a daughter of August and Frieda Reitman resided in Box Cottage 1918 - 1953.A colour photograph of Stefanie Rennick , nee Reitman 1918 - 2001, who spent her childhood living in Box Cottage.box william, box elisabeth, reitman august, reitman stefanie, reitman frieda, city of moorabbin council, lewis timber merchants pty ltd, pottery, sculpture, market gardens, pioneers, early settlers, dendy henry, box cottage museum, moorabbin, brighton, bentleigh, mckinnon, ormond, reitman william, rietmann -
The Beechworth Burke Museum
Geological specimen - Smoky quartz crystals, unknown
Quartz is an extremely common mineral to find across the world. Quartz can have two forms; Microcrystalline quartz or Crystalline quartz. Microcrystalline quartz is a fine grain quartz where crystalline quartz is often a large crystal. This specimen is a crystalline quartz. Made of silicon oxide, this specimen is called smokey quartz crystals because of its brownish colour. However, the colour of quartz can vary. In addition, quartz are formed in deep-seated igneous rocks and crystallized through hot aqueous solutions. This type of crystal can be found all over Australia, including Beechworth in Victoria. Other places quartz can be found is the Ashburton River area in Western Australia, Marlborough in Queensland, the Lune River area in Tasmania and Kingsgate in New South Wales. This specimen is significant because it is common to find this kind of mineral. While the location of where this specimen was originally from is unknown, it highlights the many places in Australia where quartz is found. It demonstrates that quartz makes up a large portion of Australia's geology. In addition, quartz itself can vary in its colour and shape. This specimen represents one of these variations. That being smoky quartz crystals. 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 large hand-sized quartz mineral with shades of brown and gray throughout.Smoky quartz / crystals /locality/ unknown / (needs a wash) /BBgeological specimen, geology, geology collection, burke museum, beechworth, microcrystalline, quartz, quartz mining, quartz reefs beechworth, smokey quartz crystals, crystals, crystalline, silicon oxide, brown, colour, igneous rocks, magma, ashburton river, western australia, marlborough, queensland, lune river, tasmania, kingsgate, new south wales, nsw -
The Beechworth Burke Museum
Geological specimen - Fossil Leaves
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 Beechworth Burke Museum
Geological specimen - Common Opal, unknown
Common Opal is a mineraloid that is non crystallising and is classed as an amorphous silicate, the chemical composition for Opal is SiO2 nH2O. Opals can develop in weathered sedimentary rock typical in arid regions where limited water enters small gaps in the rock, and the silicate is hydrated. Common opals, unlike precious opals, do not exhibit ‘play of colour’ in which the colour appears to change depending on the angle of view. While precious opals are highly valuable and cut as gemstones for jewellery, common opals can be cut into inexpensive gemstones and are also mined for various uses including as ingredients in ceramics, insulation, fillers, and abrasives. The source of this common opal specimen is unknown, but common opals are found around the world, notable deposits are found in Queensland, South Australia, New South Wales, Peru, Kenya, Nevada, Oregon, and Mexico. This common opal specimen is of historic and scientific significance due to its donation in 1868 as part of the Geological Survey of Victoria and as a typical example of uncut common opal. 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 palm-sized amorphous (non-crystallising) hydrated silicate mineraloid specimen in shades of brown, orange, and white.Existing label: Common Opal / Locality unknowngeological specimen, geology, geology collection, burke museum, beechworth, common opal, opal, mineraloid, amorphous silicates, hydrated silicate -
The Beechworth Burke Museum
Geological specimen - Dolomite
Dolomite is a mineral, calcium magnesium carbonate, with the chemical formula CaMg(CO3)2. It is a principle component of various rock types sometimes also referred to as dolomite, including dolostone, dolomitic marble and dolomitic limestone (according to the composition of each type). Dolomite rock is found in sedimentary basins throughout the world, comprising approximately 2% of the Earth's crust. It is formed when lime mud or limestone encounters groundwater containing magnesium. Dolomite can contain elements such as lead, zinc and copper. Dolomite and limestone are used in various construction, landscaping and agricultural processes. This specimen was donated to the Burke Museum in 1868 by Alfred Selwyn as part of the Geological Survey of Victoria. It was donated to the Museum in 1868. Victoria and other regions of Australia were surveyed for sites of potential mineral wealth throughout the 19th Century. The identification of sites containing valuable commodities such as gold, iron ore and gemstones in a locality had the potential to shape the development and history of communities and industries in the area. The discovery of gold in Victoria, for instance, had a significant influence on the development of the area now known as 'the goldfields', including Beechworth; the city of Melbourne and Victoria as a whole. Dolomite and limestone are mined at several locations in Victoria, including sites in the North-East of the state in Bindi and Limestone Creek. There are notable dolomite deposits in most Australian states. The dolomitised form of the mineral tends to come from older limestone deposits, formed during the palaeozoic era in marine settings, so this specimen may have come from a deposit located along a coastline in Victoria or another state. The specimen is significant as an example of surveying activity undertaken to assess and direct the development of the mineral resource industries in Victoria and Australia, as well as the movement to expand human knowledge of earth sciences such as mineralogy and geology in the nineteenth century. 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.Hand-sized piece of pale pink dolomite (calcium magnesium carbonate) with dark grey rim and hollowed centre. geological specimen, geology, geology collection, burke museum, beechworth, dolomite, mineralogy, geological survey, alfred selwyn, limestone, calcium magnesium carbonate -
The Beechworth Burke Museum
Geological specimen - Kaolin, unknown
Kaolin is also known as china clay. This specimen came from Dunolly, Victoria and was donated to the Museum in 1868 as part of the Geological Survey of Victoria. This survey helped map and study the geology of Victoria. In Victoria, Kaolin is particularly used as a filler and coating material in paper manufacture. It can also be used in paints, ceramics, rubbers and plastics. There are many kaolin deposits in Victoria but many of these have been mined out and there is not much Kaolin left. Rocks that have a high amount of Kaolinite and it can be formed through the decomposition of other materials. There are two types of Kaolin; hard and soft kaolin. Soft kaolin's are coarse but have a soapy texture. It can also break easily. The hard kaolins have an earthly texture and are finer grained. This means that they are harder to break, unlike the soft kaolin. Hard kaolin's are formed by flocculation in salt water, a process that in basic terms, bonds particles together. Kaolin is a common material in Victoria and that is why it is significant. While this specimen was mined in Dunolly, Victoria Kaolin can also be found Pittong, Pakenham, Bulla, Hallam and Ballarat as well as many other places throughout Victoria. This specimen represents the presence of Kaolin deposits in this region of Australia. It is also significant because Kaolin has many uses and is largely beneficial to many manufacturing processes in Victoria. 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.Two pieces of Kaolinite mineral with shades of white and graygeological specimen, geology, geology collection, burke museum, beechworth, kaolin, china clay, dunolly, geological survey of victoria, kaolinite, victoria, mining, mining deposits, geology of victoria, australia, filler, coating material, paper manufacture, paint, ceramics, rubbers, plastics, decomposition, materials, soft kaolin, hard kaolin, flocculation, particles, salt water -
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 - Malachite, unknown
Malachite is a water soluble, crystalline, triphenyl methylene chloride salt. It has a close relationship to copper because it is common for Malachite and copper to come from the same ore. Malachite often has shades of green, making it also known as Malachite Green. As a result of it's colour, it is known for being a dye and has been used in the dye industry, the textile industry and in medical fields. Cobar in New South Wales is well known for it's mining. This is because of the number of important deposits present in the area and include three important mining belts where most of the materials are found. These are the 'Cobar belt', the 'Canbelego belt' and the 'Girilambone belt'. The 'Cobar belt' runs underneath the main town. Copper was first discovered in Cobar in 1869 and since then, many deposits of other materials have been found, including Malachite.This specimen is significant because it comes from Cobar, NSW and represents the many deposits of materials found there. Cobar has a long history of mining and is a source of Australia's copper minerals. Malachite is often found in copper deposits meaning that it is representative of Cobar's copper production. Malachite is known for it's vivid green colour and as a result, has many uses, such as meaning used as a dye. This makes it a valuable material and highly significant. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A solid hand-sized mineral with shades of brown , white and light green throughout.geological specimen, geology, geology collection, burke museum, beechworth, malachite, copper, water soluble, cobar, cobar mines, cobar mining, cobar nsw, nsw, new south wales, mining belts, ore, copper ore, malachite green, dye, green, dye industry, textile industry, desposits, canbelego, girilambone, alfred selwyn -
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 -
The Beechworth Burke Museum
Geological specimen - Oil shale
This particular specimen is found in Wolgan Valley, New South Wales. It could be linked to the abandoned oil shale mining sites in Wolgan Valley such as Newnes. Newnes was an industrial complex operational in the early 20th century is now partly surrounded by Wollemi National Park. It produced motor spirit, kerosene, and gas oil. Newnes's Torbanite oil shale rock contained around 350 litres of oil shale per tonne. The Torbanite was mined by the Commonwealth Oil Corporation Ltd. Oil shale is a sedimentary rock and also a form of fossil fuel. It is often formed millions of years ago and usually contain fossilised remains of plants and/or animals. Oil shale is rich in kerogen that releases hydrocarbon when heated. These hydrocarbon can be used as an alternative petroleum or natural gas. The oil-shale rock was converted into oil by "destructive distillation"; the rock being heated until it broke down to form an oily vapour and an ash residue. Oil bearing shale is one of Australia's national assets. There are many oil companies established in Australia. It reflects Australia's rich natural resources as well as connection to the Australia's engineering and oil industry. The booming oil shale extraction businesses can be traced as far back as 1920s. 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 dark gray oil bearing shale with shades of light brown and fossilised leavesExisting label: OIL BEARING SHALE with / FOSSILISED LEAVES / Locality: Wongan Valley, NSW / Donor: Miss M. Cambell geological specimen, geology, geology collection, burke museum, beechworth, oil shale, shale, fossil fuels, alfred selwyn, wolgen valley, 1868 geological survey of victoria, rocks, sedimentary rocks, newnes, torbanite, commonwealth oil corporation ltd -
The Beechworth Burke Museum
Geological specimen - Amazonite, unknown
Amazonite is classed as a Tectosilicate and is part of the Feldspar group of minerals. Amazonite forms in a triclinic crystal structure and its chemical formula is K(AlSi3O8). In appearance, Amazonite can range from shades of green to green blue to blue, and often with white streaks or veining. The greenish colour is believed to come from the small amount of lead contained in its composition. Amazonite is named after the Amazon River due to its colour and similarities to another rock found along the riverbanks, although Amazonite is not actually found at or near the Amazon. Although less commonly used in jewellery today, Amazonite has been mined and used by humans for thousands of years and Amazonite jewellery from at least 2000BCE have been discovered in North Africa. Amazonite is found in many locations around the world including Brazil, Peru, Ethiopia, Canada, Russia, Mozambique, Myanmar, Pakistan, China, Madagascar, and the United States of America. This specimen most probably comes from the U.S.A., Amazonite is found in several US states particularly in Colorado, Virginia, Pennsylvania. This specimen is of both scientific and historic significance as a striking blue green example of Amazonite mined prior to 1868 in the United States of America, most likely from Colorado, Virginia, or Pennsylvania. These three states are all locations of significant Amazonite deposits. 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 palm-sized Feldspar mineral specimen from the Tectosilicate class in shades of blue-green with white veining.Existing label: green/blue Feldspar / "amazonite" / possibly USA geological specimen, geology, geology collection, burke museum, beechworth, tectosilicate, amazonite, feldspar, triclinic crystal structure, amazonite usa, amazonite colorado, amazonite virginia, amazonite pennsylvania -
The Beechworth Burke Museum
Geological specimen - Malachite in Conglomerate, Unknown
Malachite is a green copper carbonate hydroxide mineral and was one of the first ores used to make copper metal. Malachite has been utilised as a gemstone and sculptural material in the past as its distinctive green color does not fade when exposed to light or after long periods of time. Malachite is formed at shallow depths in the ground, in the oxidizing zone above copper deposits. The material has also been used as a pigment for painting throughout history. Malachite is considered a rare gemstone in that the original deposits for the stones have been depleted leaving behind very few sources. In addition, the use of Malachite as gemstones and sculptural materials remains just as popular today as they were throughout history. It is quite common to cut the stone into beads for jewellery. The fact that Malachite has such a rich colour and one that does not fade with time or when exposed to light makes it particularly rare. Although there is no indication available of the locality from which the specimen was sourced, it is likely that the specimen was collected either in South Australia in the vicinity of the Burra Burra mines or in Victoria as part of programs of geological surveying undertaken in the Nineteenth and Twentieth centuries. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A solid hand-sized copper carbonate hydroxide mineral with quartz pebbles in red conglomorate matrix presenting shades of cream, brown and green.Existing label: Malachite / (green) in / conglomerate / (white quartz / pebbles / in red matrix /geological specimen, geology, geology collection, burke museum, beechworth, geological, indigo shire, malachite, malachite specimen, australian mines, mines, geological survey, conglomorate, matrix -
The Beechworth Burke Museum
Geological specimen - Galena (with quartz), unknown
Galena is the natural compound of lead and classed as a sulphide, it crystallises in a cubic pattern and its chemical formula is PbS. Galena is a primary source of both lead and silver. This specimen of Galena comes from Broken Hill. Broken Hill has one of the world’s largest and most significant deposit of ore for the production of lead. Mining of Galena at Broken Hill began with the staking of land by Charles Rasp in 1883. By the following year, in 1884, Rasp and six others had formed Broken Hill Mining Company. Broken Hill Mining Company eventually evolved into BHP group limited and is currently the largest mining company in the world and the largest company in Australia. There is archaeological evidence from artefacts discovered in Turkey that humans have been extracting lead from galena by the process of smelting since at least 6500 BCE. This specimen also has quartz on the top surface which is frequently discovered alongside Galena. This mineral specimen is of historic significance as a sample of Galena extracted from Broken Hill during the 19th century. Mining for Galena in Broken Hill begin in 1883 by Charles Rasp and evolved into the world’s largest mining company – BHP Group Limited. Broken Hill is one of the world’s most significant deposits of ore for the production of lead. 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 flat, hand-sized, grey sulphide specimen that is the natural compound of lead with a quartz formation on the top surface. Existing Label: GALENA / (with quartz) / Locality: Broken Hill / N.S.W 120 x 70 x 29geological specimen, geology, geology collection, burke museum, beechworth, galena, galena quartz, quartz, charles rasp, broken hill mining company, bhp group limited, bhp, lead, ore, lead sulphide, sulphide, silver, broken hill -
The Beechworth Burke Museum
Geological specimen - Galena (lead sulphide), Unknown
Galena occurs in a range of deposit contexts, often in metalliferous veins, such as Broken Hill, Australia; Coeur d’Alene, Idaho, United States.; Clausthal Zellerfeld, Germany; and Cornwall, England. Large deposits also replace limestone, dolomite, or occasionally organic matter, or have a contact-metamorphic origin. Galena is additionally found in cavities, brecciated (fractured) zones in limestone and chert, and in coal beds. This specimen was recovered from Broken Hill NSW and is 60% lead with 8-12 oz/silver to the ton.Galena or 'lead glance' is a grey lead sulfide and the chief ore mineral of lead. It forms isometric crystals in which the ionic lattice is similar to sodium chloride. Galena is brittle and easily weathers to secondary lead minerals, with the upper part of mineral deposits often containing cerussite, anglesite, and pyromorphite. It usually contains silver, which is mined along with its lead content. Other commercially important minerals that form in close association with galena are antimony, copper, and zinc. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A small-sized solid specimen containing one mineral with a sparkly silver metallic lustre exterior and pastel-grey interior.geological specimen, geology, geology collection, burke museum, beechworth, galena, lead sulphide, alfred selwyn, broken hill -
The Beechworth Burke Museum
Geological specimen - Anthracite crystal, Unknown
Anthracite typically occurs in geologically deformed areas due to extreme heating – with temperatures ranging from 170 to 250 °C – caused by igneous intrusions or high geothermal gradients. It is most commonly found in northeastern Pennsylvania in the United States; however, smaller amounts are also found in Australia, China, eastern Ukraine, South Africa, western Canada, and other countries. This specimen was recovered from Tasmania and is 85-95% carbon.Anthracite is the mineral name for hard coal and is the least plentiful of all coal types. It is clean to the touch and, when polished, is used for decorative purposes. Before natural gas and electricity, anthracite was used for domestic heating as it produces little dust, burns slowly, and gives off a minor amount of smoke. However, it is also limited in abundance and expensive. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A hand-sized highly metamorphosed coal mineral with a black/steel-grey shiny metallic lustre.geological specimen, geology, geology collection, burke museum, beechworth, indigo shire, geological, mineralogy, victoria, alfred selwyn, anthracite