Showing 764 items
matching type forms
-
City of Moorabbin Historical Society (Operating the Box Cottage Museum)
Accessory - Clothing, bow tie, black , spring clip, 20thC
The Bow Tie is a type of men's necktie that consists of a ribbon of fabric tied around the collar in a symmetrical manner such that the two opposite ends form loops. Ready-tied Bow ties are available, in which the distinctive Bow is sewn and a band goes around the neck and clips to secure. Bow ties may be made of any fabric material, but most are made from silk, polyester, cotton, or a mixture of fabrics. The Bow tie originated among Croatian mercenaries during the Prussian wars of the 17th century when the Croat mercenaries used a scarf around the neck to hold together the opening of their shirts. This was soon adopted under the name cravat, derived from the French for "Croat", by the upper classes in France, then a leader in fashion, and flourished in the 18th and 19th centuries. The most traditional Bow ties are usually of a fixed length and are made for a specific size neck. Sizes can vary between approximately 14 and 20 inches just like a comparable shirt collar. Fixed-length Bow ties are preferred when worn with the most formal wing-collar shirts, so as not to expose the buckle or clasp of an adjustable Bow tie. Bow ties are worn by magicians, country doctors, paediatricians, lawyers, professors musicians and by people hoping to look like the above and clowns also wear oversized ones. In the 1980’s fashionable and professional women wore a type of Bow tie. Most men only wear Bow ties with formal dress. A man's pre-tied black bow tie with a metal spring clip to attach to the shirt collar. The 2 spring clips have 'alligator teeth' to grip the collaron spring clip MADE IN AUSTRALIA SPRINGmenswear, clothing, bow ties, cheltenham, moorabbin, bentleigh, early settlers, pioneers, market gardeners, male neckwear -
City of Moorabbin Historical Society (Operating the Box Cottage Museum)
Clothing - Clothing, bow tie, white , elastic clip, 20thC
The Bow Tie is a type of men's necktie that consists of a ribbon of fabric tied around the collar in a symmetrical manner such that the two opposite ends form loops. Ready-tied Bow ties are available, in which the distinctive Bow is sewn and a band goes around the neck and clips to secure. Bow ties may be made of any fabric material, but most are made from silk, polyester, cotton, or a mixture of fabrics. The Bow tie originated among Croatian mercenaries during the Prussian wars of the 17th century when the Croat mercenaries used a scarf around the neck to hold together the opening of their shirts. This was soon adopted under the name cravat, derived from the French for "Croat", by the upper classes in France, then a leader in fashion, and flourished in the 18th and 19th centuries. The most traditional Bow ties are usually of a fixed length and are made for a specific size neck. Sizes can vary between approximately 14 and 20 inches just like a comparable shirt collar. Fixed-length Bow ties are preferred when worn with the most formal wing-collar shirts, so as not to expose the buckle or clasp of an adjustable Bow tie. Bow ties are worn by magicians, country doctors, paediatricians, lawyers, professors musicians and by people hoping to look like the above and clowns also wear oversized ones. In the 1980’s fashionable and professional women wore a type of Bow tie. Most men only wear Bow ties with formal dress. A pre tied white Bow tie sewn on a neckband with an elastic clip fastenermenswear, clothing, bow ties, cheltenham, moorabbin, bentleigh, early settlers, pioneers, market gardeners, male neckwear -
City of Moorabbin Historical Society (Operating the Box Cottage Museum)
Clothing - Clothing, bow tie white, fixed length, 20thC
The Bow Tie is a type of men's necktie that consists of a ribbon of fabric tied around the collar in a symmetrical manner such that the two opposite ends form loops. Ready-tied bow ties are available, in which the distinctive bow is sewn and a band goes around the neck and clips to secure. Bow ties may be made of any fabric material, but most are made from silk, polyester, cotton, or a mixture of fabrics. The Bow tie originated among Croatian mercenaries during the Prussian wars of the 17th century when the Croat mercenaries used a scarf around the neck to hold together the opening of their shirts. This was soon adopted under the name cravat, derived from the French for "Croat", by the upper classes in France, then a leader in fashion, and flourished in the 18th and 19th centuries. The most traditional Bow ties are usually of a fixed length and are made for a specific size neck. Sizes can vary between approximately 14 and 20 inches just like a comparable shirt collar. Fixed-length Bow ties are preferred when worn with the most formal wing-collar shirts, so as not to expose the buckle or clasp of an adjustable bow tie. Bow ties are worn by magicians, country doctors, lawyers, paediatricians, professors musicians and by people hoping to look like the above and clowns also wear oversized ones. In the 1980’s fashionable and professional women wore a type of Bow tie. Most men only wear Bow ties with formal dress. This white bow tie is a 'fixed length' type that needs to be tied by the person wearing it. MAKO SIZE 15 1/2 menswear, clothing, shirts, collars, early settlers, fashion, cheltenham, moorabbin, dairy farmers, market gardeners, bow ties, mako pty ltd -
City of Moorabbin Historical Society (Operating the Box Cottage Museum)
Clothing - Clothing, Bow tie, black, elastic, clip, c1960
The Bow Tie is a type of men's necktie that consists of a ribbon of fabric tied around the collar in a symmetrical manner such that the two opposite ends form loops. Ready-tied bow ties are available, in which the distinctive bow is sewn and a band goes around the neck and clips to secure. Bow ties may be made of any fabric material, but most are made from silk, polyester, cotton, or a mixture of fabrics. The Bow tie originated among Croatian mercenaries during the Prussian wars of the 17th century when the Croat mercenaries used a scarf around the neck to hold together the opening of their shirts. This was soon adopted under the name cravat, derived from the French for "Croat", by the upper classes in France, then a leader in fashion, and flourished in the 18th and 19th centuries. The most traditional Bow ties are usually of a fixed length and are made for a specific size neck. Sizes can vary between approximately 14 and 20 inches just like a comparable shirt collar. Fixed-length Bow ties are preferred when worn with the most formal wing-collar shirts, so as not to expose the buckle or clasp of an adjustable bow tie. Bow ties are worn by magicians, country doctors, lawyers, paediatricians, professors musicians and by people hoping to look like the above and clowns also wear oversized ones. In the 1980’s fashionable and professional women wore a type of Bow tie. Most men only wear Bow ties with formal dress. A man's pre-tied black bow tie with neckband and elastic tape with a clip. fastenermenswear, bow ties, fashion, melbourne, moorabbin, bentleigh, cheltenham, polyester, rayon -
City of Moorabbin Historical Society (Operating the Box Cottage Museum)
Accessory - Clothing, black bow tie, c1960
The Bow Tie is a type of men's necktie that consists of a ribbon of fabric tied around the collar in a symmetrical manner such that the two opposite ends form loops. Ready-tied bow ties are available, in which the distinctive bow is sewn and a band goes around the neck and clips to secure. Bow ties may be made of any fabric material, but most are made from silk, polyester, cotton, or a mixture of fabrics. The Bow tie originated among Croatian mercenaries during the Prussian wars of the 17th century when the Croat mercenaries used a scarf around the neck to hold together the opening of their shirts. This was soon adopted under the name cravat, derived from the French for "Croat", by the upper classes in France, then a leader in fashion, and flourished in the 18th and 19th centuries. The most traditional Bow ties are usually of a fixed length and are made for a specific size neck. Sizes can vary between approximately 14 and 20 inches just like a comparable shirt collar. Fixed-length Bow ties are preferred when worn with the most formal wing-collar shirts, so as not to expose the buckle or clasp of an adjustable bow tie. Bow ties are worn by magicians, country doctors, lawyers, paediatricians, professors musicians and by people hoping to look like the above and clowns also wear oversized ones. In the 1980’s fashionable and professional women wore a type of Bow tie. Most men only wear Bow ties with formal dress. A man's pre tied black bow tie with an elastic fastening clipmenswear, neckties, bow ties, cheltenham. moorabbin, bentleigh -
City of Moorabbin Historical Society (Operating the Box Cottage Museum)
Manufactured Object, 'Crest' Home Hair Perm Kit in box, c1950
A permanent hairstyle, commonly called a perm or "permanent" is a hairstyle consisting of styles set into the hair lasting a number of months using thermal or chemical means. In the latter method, chemicals are applied to the hair, which is then wrapped around forms / rods to produce hairstyles with varying degrees of wave or curls. Usually this styling is performed by Hairdressers, in Beauty Salons, however, manufacturers appealing to the 'thriftiness' of the post world war 2 women produced products that could be used at home. It became very popular for women in the new estates to gather with their neighbours to give each other this new 'Home perm' with some success and failure. Gladys Reed used this type of Home perm while a resident of City of Moorabbin c 1950Typical Home Hair Perming equipment used to style their own hair by women in City of Moorabbin c1950A cardboard box containing solution, equipment and instruction booklet for home treatment of hair to produce permanent waves.hairdressers, hairdressing equipment, permanent wave, hair fashion, hair styling 1950, grooming, personal effects, early settlers, post world war 2 estates moorabbin, reed gladys. reed george, clark judy, bentleigh, moorabbin, highett, ormond. -
City of Moorabbin Historical Society (Operating the Box Cottage Museum)
Tools, Chain pipe wrench c1900, c1900
The heavy duty chain wrench has a double jaw that gives fast, ratchet-like action in either direction The "cable chain" is preferable for working with fittings and other irregular forms related to pipe where flat chain is better suited for pipe. The side plates connect to the handle with dovetails; the bolt's primary function is to keep the jaws in position rather than carrying the strain. The free end of the chain connects to the handle behind the attachment point for the fixed end of the chain to avoid potential for the chain to "lock" on pipe. This chain pipe wrench is typical of the type used by early settlers in Moorabbin Shire c1900Heavy steel chain pipe wrench c1900wrenches, spanners, chain pipe wrench, early settlers, market gardeners, blacksmiths, tools, building equipment, hammers, moorabbin shire, bentleigh, mckinnon, highett, cheltenham,mcewan james pty ltd, melbourne, bunnings pty ltd, -
City of Moorabbin Historical Society (Operating the Box Cottage Museum)
Tool - Bow saw with blade, 20thC
Traditionally, a bow saw is a woodworking tool used for straight or curved cuts. A bow saw is a type of frame saw. Its thin blade is held in tension by a frame. In English and American vocabulary it denotes a toothed blade suspended between two long narrow handles called "cheeks" that are supported and separated by a thin stretcher in the centre of the handles, making a wide H shape (the cheeks form the uprights of the H, the stretcher the crossbar of the H). The blade is kept in tension with a turnbuckle or a twisted cord that runs parallel to the blade between the two cheeks but on the opposite side of the stretcher. If a cord is used, the cord is twisted with a toggle attached to one loop of the cord, adding tension. The toggle hits the stretcher, which keeps the cord from untwisting. A finer version of the saw uses a narrow blade (1/4" or less) with handles that allow the user to hold the saw and turn the blade. In this context it is also known as a turning saw[2] which is larger than a coping saw.Early settlers in Moorabbin Shire had to be self reliant and made their own clothes, tools and equipment as they established their market gardens and farms. A wooden Bow saw with tensioning string, toggle and bladetools, woodwork, metalwork, carpentry, pioneers, market gardeners, early settlers, moorabbin, cheltenham, bentleigh, ormond -
City of Moorabbin Historical Society (Operating the Box Cottage Museum)
Clothing - Clothing, lady's ribbon lace, shawl collar, c1950
A collar is the part of a shirt, dress, coat or blouse that fastens around or frames the neck and may be permanently attached to the main body of the garment (e.g. by stitching) or detachable. Names for specific styles of collars vary with the vagaries of fashion. In the 1930s and 1940s, especially, historical styles were adapted by fashion designers; thus the Victorian bertha collar, a cape-like collar fitted to a low scooping neckline, was adapted in the 1940s but generally attached to a V-neckline. This item is a type of shawl collar for a V-neckline that is extended to form lapels, often used to enhance cardigans, dinner jackets and women's blouses. A lady's, detachable, white, nylon machined ribbon lace shawl collar with lace trim C1950clothing, collars, ornamental collars, moorabbin, cheltenham, bentleigh, lacework, dressmaking, fashion, formal wear, shawl collar -
The Beechworth Burke Museum
Geological specimen - Unknown, possible Carnelian Agate or Chalcedony
Although it is not known where these specimens were collected, 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. Agate occurs when amygdales (gas pockets) form in the upper levels of basaltic lava flows. If these pockets or bubbles are iniltrated by water bearing silica in solution, the fluid dries and hardens in layers, forming round or egg shaped nodules or geodes within the rocky matrix. Agate is formed of a silica mineral chalcedony similar to quartz. The term carnelian primarily refers to the reddish shading of the stone; whether the stone is termed an agate or chalcedony type is often influenced by the degree of colour banding the specimen shows. The specimens are significant as examples 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.Three small geological specimens that appear visually consistent with images of rough or unpolished Carnelian Agate or Chalcedony. geological specimen, geology, geology collection, burke museum, beechworth, indigo shire, north-east victoria, gemstones, agate, carnelian -
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 - 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 - Tourmaline in Quartz, Unknown
Tourmaline specimens are members of a crystalline silicate mineral group based on boron but influenced by elements including aluminium, iron, magnesium, sodium, lithium, or potassium. Specimens present a wide variety of colours and forms according to the specific mix of these elements. Tourmalines are semi-precious gemstones with many applications, including commercial jewellery production. The word 'tourmaline' derives from the Sinhalese term for the carnelian or red-shaded specimens, "tōramalli". This specimen has been classified by geologists as 'Black Schoalou/Tourmaline in quartz'. Schoalou may equate to a common black-hued type of Tourmaline associated since around 1400 with mines in Saxony, Germany near a village called Schorl (today's Zchorlau). If this specimen is part of the 'Schorl' species of tourmaline it is a member of the most common group of Tourmalines, a divalent sodium ion influenced group accounting for 95% of specimens. On assessment, it was noted that the crossed lines (XIs) of this tourmaline have been fractured and rehealed by the quartz matrix in which the tourmaline rests. This item is significant as an example of its type of gemstone and the geological processes leading to its formation. A solid medium-sized piece of Black Schoalou/Tourmaline in a cream and peach coloured quartz matrix. Existing label: Black Schoalou / Tourmaline in / quartz. / Tourmalines XIs have / been fractured and / rehealed with / quartz / C. Willman / 15/4/21 /geological specimen, geology, geology collection, burke museum, beechworth, indigo shire, north-east victoria, tourmaline, quartz, boron, crystals, minerals, gemstones, semi-precious, black schoalou, zchorlau, schorl -
The Beechworth Burke Museum
Geological specimen - Laterite
Laterite refers to both a rock and a soil type that is rich in clay, as well as Iron and Aluminium. It is created during a process that is called laterization, where high heat and seasonal heavy rainfall cause there to be wet and dry periods, which over time hardens the soil into rock. Because of this, most laterite is formed between tropics of Cancer and Capricorn. The iron oxide in laterite is what gives it it’s orange-red colouring. The largest religious complex in the world, Angkor Wat in Cambodia, is partially constructed of laterite, particularly its foundations, as laterite is porous and allows rainwater to drain. This specimen of laterite was collected from the Democratic Republic of Congo while it was colonised by Belgium in the 19th century. Laterite forms in many parts of the world, particularly between the tropics. It is used both for ore and as a building material, and comparing specimens from different parts of the world allows us to document the different compositions that this mineral can have when formed at different locations. 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 solid iron-aluminium oxide mineral specimen in shades of brown, orange and greyburke museum, beechworth, geological, geological specimen, laterite, laterite specimen, geology -
The Beechworth Burke Museum
Geological specimen - Montmorillonite
Montmorillonite is a type of clay composed of aluminium silicate that forms very small particles that are not well-bonded to one another. This is why it is so soft. When in the presence of water, all types of clay swell. Montmorillonite swells even more than most types of clay, which is why it is often chosen over other types of clay in its practical uses. Montmorillonite has many different practical uses, including in the mining industry, as a soil additive, as a sealant, as a desiccant to draw water out of the air, to clean ponds, to make kitty litter and in cosmetics. Montmorillonite is a common mineral and, despite being named after Montmorillon, France, can be found all over the world, including many deposits in Australia. It is not known where this particular specimen originates from. Montmorillonite is an economically and socially significant material with a wide variety of uses. Having samples of common and important minerals allows collections, like the Burke Museum, to have a more complete view of the land on which they are located, and therefore a more complete view of heritage. 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 tennis-ball sized chunk of aluminium silicate clay. It is primarily white, accented with orange and brown.burke museum, beechworth, geological, geological specimen, clay, montmorillonite -
Montmorency/Eltham RSL Sub Branch
Weapon - 1855 Pattern Sappers and Miners Lancaster Sword Bayonet, Carl Reinhard KIRSCHBAUM, 1855 Pattern Sapper and Miners Lancaster Sword Bayonet, 1855
This bayonet and scabbard was made for the Charles Lancaster .577 calibre Oval Bore Carbine and was known as the Pattern 1855 'Sappers and Miners' bayonet because they were designed for use by the Corps of British Royal Sappers & Miners. The first model Sappers and Miners bayonet appeared in 1841 and differs significantly from this type. Pattern 1855 bayonets were issued to some volunteer units of the Victorian defence forces in the late 1850s, Stylised beaked-brass pommel with T- shaped attachment slot. A steel press stud operates the locking catch via a steel leaf spring on right side of hilt. Two-piece black chequered leather grips. Left grip has four small steel rivets, right grip three rivets and the leaf spring securing screw. Brass cross-guard with formed muzzle ring. Long single-edged, pipe backed, quill pointed 24 inch (615mm) steel blade. Original leather scabbard with brass locket and chape.Knight's Head stamping of the German Solingen-based firm Carl Reinhard KIRSCHBAUM bayonet, victorian defence forces, lancaster carbine -
Federation University Historical Collection
Correspondence, J.L. Treloar, Letter on Australian War Memorial Letterhead, 1937, 12/04/1937
.1) Foolscap typed letter outlining the Coronation portrait of King George by W.B. McInnes, and requesting the Ballarat School of Mines to purchase a framed copy. The letter is signed by the Director of the Australian War Memorial, J.L. treloar .2) blank order form re ordering a Coronation portrait of King George by W.B. McInnes,australian war memorial, king george, portrait, j.l. treloar, w.b. mcinnes -
Federation University Historical Collection
Correspondence, Correspondence concerning the Burke Family, 1954, 20/05/1954
Some possibility the author is writing about Robert O'Hara Burke, but he was not married.Two letters typed .1) An air letter form J.L. Lonergan of Eastern Pensylvania addressed to Ballaratt University, and eventuallty delivered to the Ballarat School of Mines. The letter requests information on a Mrs Burke of Ballarat, whose husband was lost in the Bush. Mrs Burke ran a boading house. The author worked for Morris Machine Works and remembered a Chief Engineery from Ballarat visiting the plant at the beginning of World War One. .2) A letter on University of Melbourne letterhead redurecting the letter to Ballarat. The letter was signed by F.G. Elford for F.H. Johnston (Registrar)/j.l. lonergan, robert o'hara burke, mrs burke, kearney, f.g. elford, letterhead, f.h. johnston, morris machine works, air letter, aerograme -
Federation University Historical Collection
Document - Document - Information, VIOSH: Health and Safety Unit; Overall Objectives
Victorian Institute of Occupational Safety and Health (VIOSH) Australia is the Asia-Pacific centre for teaching and research in occupational health and safety (OHS) and is known as one of Australia's leaders on the field. VIOSH has a global reputation for its innovative approach within the field of OHS management. VIOSH had its first intake of students in 1979. At that time the Institution was known as the Ballarat College of Advanced Education. In 1990 it became known as Ballarat University College, then in 1994 as University of Ballarat. It was 2014 that it became Federation University. VIOSH Australia students are safety managers, senior advisors and experienced OHS professionals. They come from all over Australia and industry. Students are taught active research and enquiry; rather than textbook learning and a one-size fits all approach. VIOSH accepts people into the Graduate Diploma of Occupational Hazard Management who have no undergraduate degree - on the basis of extensive work experience and knowledge. Description of the Aims of the Health and Safety Unit (Ballarat College of Advanced Education). Three overall objectives are listed. The way each of these can be achieved it would be necessary to a. run high quality courses b. produce high quality research and development in at least one area of Occupational Health and Safety c. act as advisors to State and Federal Governments, Trade Unions and Employers d. be seen as a focus of knowledge on the role and training and effective use of inspectorates e. be known for a number of major themes which are recognised as the Ballarat View Each of these points is expanded on. Two A4 pages type written. Done in point formviosh, victorian institute of occupational safety and health, health and safety unit, ballarat college of advanced education, major objectives, quality course, research, advisors, governments -
Federation University Historical Collection
Document, State Film Centre, State Film Centre Despatch Advice, 1960, 22/11/1960
Paper form with text in red ink, and typed details in black. The document is a despatch Advice from the State Film Centre to the Ballarat Junior Technical School Old Boys Club.ballarat junior technical school, film, state film centre, entertainment -
Federation University Historical Collection
Certificate, Australian Military Forces: Junior Cadet Training, Third Military District, 31/05/1916
Off white printed form. Sections filled in with purple typing.'A.M.Form N. 6a' and 'SCHOOL "B" (Men Teachers) printed at top of page No. written in red pen; 2529 Official seal of Australian Military Forces Signed: W Buttner Captain, 13th Brigade T H H Capt. Chief Instructora w steane, junior cadet training, australian military forces, drill hall, st kilda, refresher course, w buttner, melbourne, physical training, marching drill, rifle shooting, swimming, running, first aid -
Federation University Historical Collection
Correspondence, A A W Steane - Letter written to a member of the Masonic Lodge, 1951, 10/01/1951
Personal letter written by Albert Steane to a fellow Freemason. Talks about his travels in 1908 and return to Ballarat and the introduction of the new phase in education - establishment of Technical Schools. He became the Head Master of the Ballarat Junior Technical School and remained in that position until his retirement in 1942. Other topics mentioned are connected with the various activities within the Lodge.Two typed sheets of yellow paper in the form of a letter. Paragraphed - double spacing between.Address of senderalbert steane, ballarat junior technical school, masonic lodge, retirement, head master, 1908, south street, south street competitions, freemasons, royal south street competitions -
Federation University Historical Collection
Book, Inorganic Chemistry for Upper Forms, 1928
Blue hardcover book, 548 pages. Includes illustrations and an index.non-fictioninorganic chemistry, science, p. w. oscroft, uppingham school, rutland county, science master -
Lara RSL Sub Branch
Photograph, RAAF 1912 Deperdussin Aircraft
In the early days of flying in France, Armand Deperdussin and his aircraft designer, M. Bechereau, formed the Societe Pour Appareils Deperdussin, and designed and produced Deperdussin monoplanes of advanced design for the period. In 1912, the Australian Government ordered from the British Deperdussin Aeroplane Company, two single-seat trainers, Type A with 35hp Anzani Y-type three cylinder engine. These two aircraft were in the first batch of four aircraft ordered by the Commonwealth Government (the other two aircraft were BE-type biplanes). The recorded cost of the Deperdussin was 480 pounds each. The serial number CFS 5 identifies this aircraft as the 5th Australian Military aircraft. It is the oldest existing Australian aircraft. either military or civilian. Rectangular shaped glass covered picture frame with photo of the plane and pilot.RAAF AIRCRAFT 1921-1981. FIRST FOREBEAR The 1912 Deperdussin was the first military monoplane ordered for the RAAFs ancestor, the Central Flying School, Point cook.This historic aircraft is retained at the Australian War Memorial as a symbol of the nation's airpower genesis.deperdussin monoplane, australian military aircraft, lara r.s.l. australian flying corps, 1912 aircraft. -
Federation University Historical Collection
Document - Document - Letter, Ballarat Junior Technical School: Letters to / from Mr A O'Toole of Wallace and L Garner, Head master, 1953
Letter written by Mr A O'Toole of Wallace wishing to enroll his son Robert at BJTS. He requested information of uniform, fees, etc. Mr Garner replied and explained that he must make an application through the Head Teacher at the Wallace State School Yellow paper typedballarat junior technical school, leslie garner, head master, mr a o'toole, wallace, application form, wallace head teacher, robert o'toole -
Federation University Historical Collection
Document - Document - Letter, Ballarat Junior Technical School: Letter from Mr Garner, Head Master, to Wing Commander Sleight, Commanding Officer, R A A F Station, Ballarat
Letter from Mr L Garner, Head Master, to Wing Commander Sleight, Commanding Officer of the R A A F Station, Ballarat, thanking him for allowing the visit of fourth form boys to the station. the staff and students informed me the visit arrangements were excellent. Second letter was confirming a conversation where the Wing Commander agreed to be the guest speaker at the speech night in December. . Yellow paper typedballarat junior technical school, l garnar, junior technical certificate, head master, wing commander sleight, commanding officer, r a a f station, fourth form visit, guest speaker, speech night -
Federation University Historical Collection
Document - Document - Letter, Ballarat Junior Technical School: Letter from Mr Garner, Head Master, to Mr John, Ballarat
Letter from Mr L Garner, Head Master, to Mr John of M B John Ltd, Ballarat. Letter conveys thanks for allowing fourth form boys to visit the foundry works. visit was interesting and informative.. Yellow paper typedballarat junior technical school, l garnar, junior technical certificate, head master, mr john, m b john ltd, foundry, fourth form visit