This particular specimen was found in the Moorabool Slate quarries in Victoria. The Moorabool Slate quarries was established in the 1860’s by a company of Welshmen with a crew of six who purchased land by the riverside to mine for slate. Under the promise of adding to existing recourses the crew mined the slate which was used for paving and roofing. Slate is a fine-grained, low-grade metamorphic rock that is formed by the transformation of mudstone, shale or sometimes volcanic ash under low pressure and temperatures. It dark colour is due to carbonaceous material or to finely divided iron sulphide. It is believed that Evan Rowlands and Theophilus Williams of Ballarat were the first to discover the slate veins. Slate is a one of the most common natural stones in general use. Being used as paving, flooring, roofing and more. However, its history of being mined in Australia is not common as it is considered that the best places to mine slate is Spain and parts of the United Kingdom. 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 somewhat rectangular foliated metamorphic rock composed of quartz, sericite and minerals from the chlorite group that make up the compounds of slate. The rock is dark grey almost black.Geological survey / R S / Loc Moorabool /Slate quarries / 1/4 sheet | 78 | Roofing Slate /burke museum, beechworth, geological, slate, metamorphic, slate (metamorphic), geological specimen, slate specimen, indigo shire

Nicholas Caire was born on Guernsey in the Channel Islands in 1837. He arrived in Adelaide with his parents in about 1860. In 1867, following photographic journeys in Gippsland, he opened a studio in Adelaide. From 1870 to 1876 he lived and worked in Talbot in Central Victoria. In 1876 he purchased T. F. Chuck's studios in the Royal Arcade Melbourne. In 1885, following the introduction of dry plate photography, he began a series of landscape series, which were commercially successful. As a photographer, he travelled extensively through Victoria, photographing places few of his contemporaries had previously seen. He died in 1918. Reference: Jack Cato, 'Caire, Nicholas John (1837–1918)', Australian Dictionary of Biography.An original, rare photograph from the series 'Views of Victoria: General Series' by the photographer, Nicholas Caire (1837-1918). The series of 60 photographs that comprise the series was issued c. 1876 and reinforced a neo-Romantic view of the Australian landscape to which a growing nationalist movement would respond. Nicholas Caire was active as a photographer in Australia from 1858 until his death in 1918. His vision of the Australian bush and pioneer life had a counterpart in the works of Henry Lawson and other nationalist poets, authors and painters.Views of Victoria (General Series) No.33 / ‘Interior of the crater at Mount Franklin’ / Albumen silver photograph mounted on cardOn Reverse: ‘Mount Franklin is situated near Malmsbury, about ten or twelve miles distant. The most remarkable and interesting part of this Mountain is its Crater, which, from its immense size and great depth, denotes that a volcanic eruption of considerable magnitude must have taken place at some period in the past. Looking down from the summit, the large gum trees growing at the bottom of the Crater appear but small saplings.’nicholas caire (1837-1918), mount franklin, victoria - landscape photography

E560 N5 Dec 1979 A43 Boring mole pit near big box tree in 39 Burlock Avenue backyard Part of a 43-photo record of the MMBW�s engineering feat in drilling a 12 inch pipe line up to 40 feet deep through rock hardened by volcanic action associated with geological fault that occurs along the line. The work took place from October 1979 to May 1980 on the southern boundary of Hubbard Reserve, North Ringwood. The collection was presented to the Ringwood Historical Research Group by J Clarke on 9th June 1980.

E560 N24 Jan 1980 A43 Cover of mole pit near big box tree in 39 Burlock Avenue backyard Part of a 43-photo record of the MMBW�s engineering feat in drilling a 12 inch pipe line up to 40 feet deep through rock hardened by volcanic action associated with geological fault that occurs along the line. The work took place from October 1979 to May 1980 on the southern boundary of Hubbard Reserve, North Ringwood. The collection was presented to the Ringwood Historical Research Group by J Clarke on 9th June 1980.

The card enabled a person to attend the 'Popular Science Lectures' which were held in the lecture hall of the school. These were the Winter course of 1882. The Lectures were from 8p.m. They ran from June 9 through to October 11. The subjects were varied and a guest speaker was responsible for each session. G Foord (Royal Mint) - Alchemy; Rev Ick (Sandhurst) - The Wonders of Coral Life; R Ellery (Government Astronomer) - The Sun's Distances and the Transits of Venus; J Thomas (Geelong) - The Stellar Universe; J Usher (Doctor) - Physiology, Body and Bones; Baron Von Mueller (Government Botanist) - General observations on the Flora of Australia; Professor Mica Smith - Gold; Professor F Kraush - Volcanic rocks of the Ballarat District. This was organised by the School Councilwhen James Oddie was Vice-President.Beige coloured card written on both sidespopular science lectures, winter course 1882, guest speakers, g foord, royal mint, alchemy, reverend ick, sandhurst, coral life, r ellery, government astronomer, sun's distances, transits of venus, j thomas, stellar universe, baron von mueller, flora of australia, government botanist, mica smith, gold, f m kraush, volcanic rocks

Tower Hill is a volcanic formation believed to have erupted about 32,000 years ago. Its formation is known as a "nested maar" and it is the largest example of its type in Victoria. During formation, molten lava pushed its way up through the Earth’s crust and encountered a layer of water-bearing rock. Violent explosions followed creating a shallow crater which later filled with water to form the lake. Further eruptions occurred in the centre of this crater, creating the islands and cone shaped hills. In 1892 Tower Hill became Victoria’s first National Park. In 1961, Tower Hill became a State Game Reserve under the then Fisheries and Wildlife Department and a major re-vegetation program began. (https://www.towerhill.org.au/index.php/about-reserve/history, accessed 23 December 2019)Black and white image of Tower Hill, near Koroit, Victoria.tower hill, volcano, crater

Tower Hill is a volcanic formation believed to have erupted about 32,000 years ago. Its formation is known as a "nested maar" and it is the largest example of its type in Victoria. During formation, molten lava pushed its way up through the Earth’s crust and encountered a layer of water-bearing rock. Violent explosions followed creating a shallow crater which later filled with water to form the lake. Further eruptions occurred in the centre of this crater, creating the islands and cone shaped hills. In 1892 Tower Hill became Victoria’s first National Park. In 1961, Tower Hill became a State Game Reserve under the then Fisheries and Wildlife Department and a major re-vegetation program began. (https://www.towerhill.org.au/index.php/about-reserve/history, accessed 23 December 2019)Panaramic view of Tower Hill, Victoria.tower hill, volcano, crater

Tower Hill is a volcanic formation believed to have erupted about 32,000 years ago. Its formation is known as a "nested maar" and it is the largest example of its type in Victoria. During formation, molten lava pushed its way up through the Earth’s crust and encountered a layer of water-bearing rock. Violent explosions followed creating a shallow crater which later filled with water to form the lake. Further eruptions occurred in the centre of this crater, creating the islands and cone shaped hills. In 1892 Tower Hill became Victoria’s first National Park. In 1961, Tower Hill became a State Game Reserve under the then Fisheries and Wildlife Department and a major re-vegetation program began. (https://www.towerhill.org.au/index.php/about-reserve/history, accessed 23 December 2019)Black and white photograph of Tower Hill devoid of trees.tower hill, crossley, volcano

VFF is seeking an appropriate framework to ensure farmers do not bear the cost of infrastructure on their farms. Overhead powerlines are proposed through the rich volcanic soils around Ballarat. This land supports 1200 jobs in processing in Ballarat. The towers would impact on the ability to irrigate crops, to use tractors around them, on biosecurity and on ability to use emergency equipment near them. VFF wants assurances that the managing entry to farm policy position will be adhered to and that a statewide strategic plan for renewable energy is prepared. https://www.vff.org.au/wp-content/uploads/2021/09/PS210901LG-Managing-Entry-to-Farms-adopted.pdf https://www.vff.org.au/wp-content/uploads/2021/09/VFF-Renewable-Energy-and-Energy-Efficiency-Policy-Statement-Meeting-172-June-2021.pdfadvocacy, renewable energy, farmers, protest, rally, managing entry to farm, victorian farmers federation, ballarat

VFF is seeking an appropriate framework to ensure farmers do not bear the cost of infrastructure on their farms. Overhead powerlines are proposed through the rich volcanic soils around Ballarat. This land supports 1200 jobs in processing in Ballarat. The towers would impact on the ability to irrigate crops, to use tractors around them, on biosecurity and on ability to use emergency equipment near them. VFF wants assurances that the managing entry to farm policy position will be adhered to and that a statewide strategic plan for renewable energy is prepared. https://www.vff.org.au/wp-content/uploads/2021/09/PS210901LG-Managing-Entry-to-Farms-adopted.pdf https://www.vff.org.au/wp-content/uploads/2021/09/VFF-Renewable-Energy-and-Energy-Efficiency-Policy-Statement-Meeting-172-June-2021.pdfadvocacy, renewable energy, farmers, protest, rally, managing entry to farm, victorian farmers federation, ballarat

VFF is seeking an appropriate framework to ensure farmers do not bear the cost of infrastructure on their farms. Overhead powerlines are proposed through the rich volcanic soils around Ballarat. This land supports 1200 jobs in processing in Ballarat. The towers would impact on the ability to irrigate crops, to use tractors around them, on biosecurity and on ability to use emergency equipment near them. VFF wants assurances that the managing entry to farm policy position will be adhered to and that a statewide strategic plan for renewable energy is prepared. https://www.vff.org.au/wp-content/uploads/2021/09/PS210901LG-Managing-Entry-to-Farms-adopted.pdf https://www.vff.org.au/wp-content/uploads/2021/09/VFF-Renewable-Energy-and-Energy-Efficiency-Policy-Statement-Meeting-172-June-2021.pdfadvocacy, renewable energy, farmers, protest, rally, managing entry to farm, victorian farmers federation, ballarat

VFF is seeking an appropriate framework to ensure farmers do not bear the cost of infrastructure on their farms. Overhead powerlines are proposed through the rich volcanic soils around Ballarat. This land supports 1200 jobs in processing in Ballarat. The towers would impact on the ability to irrigate crops, to use tractors around them, on biosecurity and on ability to use emergency equipment near them. VFF wants assurances that the managing entry to farm policy position will be adhered to and that a statewide strategic plan for renewable energy is prepared. https://www.vff.org.au/wp-content/uploads/2021/09/PS210901LG-Managing-Entry-to-Farms-adopted.pdf https://www.vff.org.au/wp-content/uploads/2021/09/VFF-Renewable-Energy-and-Energy-Efficiency-Policy-Statement-Meeting-172-June-2021.pdfadvocacy, renewable energy, farmers, protest, rally, managing entry to farm, victorian farmers federation, ballarat

VFF is seeking an appropriate framework to ensure farmers do not bear the cost of infrastructure on their farms. Overhead powerlines are proposed through the rich volcanic soils around Ballarat. This land supports 1200 jobs in processing in Ballarat. The towers would impact on the ability to irrigate crops, to use tractors around them, on biosecurity and on ability to use emergency equipment near them. VFF wants assurances that the managing entry to farm policy position will be adhered to and that a statewide strategic plan for renewable energy is prepared. https://www.vff.org.au/wp-content/uploads/2021/09/PS210901LG-Managing-Entry-to-Farms-adopted.pdf https://www.vff.org.au/wp-content/uploads/2021/09/VFF-Renewable-Energy-and-Energy-Efficiency-Policy-Statement-Meeting-172-June-2021.pdfadvocacy, renewable energy, farmers, protest, rally, managing entry to farm, victorian farmers federation, ballarat

VFF is seeking an appropriate framework to ensure farmers do not bear the cost of infrastructure on their farms. Overhead powerlines are proposed through the rich volcanic soils around Ballarat. This land supports 1200 jobs in processing in Ballarat. The towers would impact on the ability to irrigate crops, to use tractors around them, on biosecurity and on ability to use emergency equipment near them. VFF wants assurances that the managing entry to farm policy position will be adhered to and that a statewide strategic plan for renewable energy is prepared. https://www.vff.org.au/wp-content/uploads/2021/09/PS210901LG-Managing-Entry-to-Farms-adopted.pdf https://www.vff.org.au/wp-content/uploads/2021/09/VFF-Renewable-Energy-and-Energy-Efficiency-Policy-Statement-Meeting-172-June-2021.pdfphotos of Lydiard St Stop Ausnet Rallyadvocacy, renewable energy, farmers, protest, rally, managing entry to farm, victorian farmers federation, ballarat

VFF is seeking an appropriate framework to ensure farmers do not bear the cost of infrastructure on their farms. Overhead powerlines are proposed through the rich volcanic soils around Ballarat. This land supports 1200 jobs in processing in Ballarat. The towers would impact on the ability to irrigate crops, to use tractors around them, on biosecurity and on ability to use emergency equipment near them. VFF wants assurances that the managing entry to farm policy position will be adhered to and that a statewide strategic plan for renewable energy is prepared. https://www.vff.org.au/wp-content/uploads/2021/09/PS210901LG-Managing-Entry-to-Farms-adopted.pdf https://www.vff.org.au/wp-content/uploads/2021/09/VFF-Renewable-Energy-and-Energy-Efficiency-Policy-Statement-Meeting-172-June-2021.pdfphotos of Lydiard St Stop Ausnet Rallyadvocacy, renewable energy, farmers, protest, rally, managing entry to farm, victorian farmers federation, ballarat

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

Bailliere's Victorian Gazetteer and Road Guide. The most recent and accurate information as th every place in the colony. Second edition, with additions to date. Includes small hamlets postal villages and volcanic hills. Newspaper clipping refering to Marysville. Newspaper clipping referring to Harkaway. Clipping of sale of YMCA, sale of freehold at corner of High and Short Sts. Invitations from Bendigo and Northern District Hospital to H. Curnow. This item also has numerous references to other things that apply to the invitation. Old Post Office telegram form with notes on the back. Mixed amid inner pages is yellow card with typwritten description of the book's name. At front and back there are numerous pages of advertisements.Robt. P. Whitworthvictoria, history, people and places in victoria.

Thunderegg Agates are formed within rhyolite volcanic ash layers. They are rough spherical shapes, varying in size from less than an inch to over a metre long. Thundereggs usually contain centres of chalcedony which may have been fractured followed by deposition of agate, jasper or opal, either uniquely or in combination. A unique characteristic that these specimens have is the fact that they often look like ordinary rocks on the outside, but slicing them in half and polishing them may reveal intricate patterns and colours. These particular specimens are examples of thunderegg agates. Agate is a variety of chalcedony, a cryptocrystalline form of quartz. The agate component contributes to the intriguing internal patterns of the specimens. The specific locality of these specimens is unknown but they can be found in flows of rhyolite lava. They are formed in gas pockets in the lava, which act as moulds. These specimens can be found globally, with specific locations in Germany being particularly abundant. 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 small solid specimens with pale, sandy-coloured exteriors and fractured internal patterns. burke museum, beechworth, geological, geological specimen, thundereggs, thundereggs agate, agate, rhyolite, rhyolite lava, volcanic ash, chalcedony, cryptocrystalline

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

This specimen originated from Mount Lyell on the west coast of Tasmania, where a large group of open cut and underground copper-silver-gold mines began operating in 1883. Between 1893-1994, the Mt Lyell Mining and Railway Company were responsible for operations. The Mt Lyell copper-gold mines produce some excellent crystallised specimens of chalcopyrite and other minerals. The deposits are generally considered to be of Cambrian volcanic origin, but there are indications of Devonian granitic influence on the ores, plus local remobilisation during Devonian deformation. Over 120 million tonnes of ore was produced from several workings, including the main Prince Lyell mine and the North Lyell mine, which was also of great importance. The Mount Lyell mines have a long history of human and environmental disasters, including the 1912 North Lyell fire that killed 42 miners, and two separate incidents in 2013 in which three people lost their lives. The environmental impacts from this complex of mines are extensive, with waste tailings and heavy metal contamination flowing directly into the King and Queen River catchments. In 1954, the eminent Australian historian, Geoffrey Blainey, published 'The Peaks of Lyell' which delves into the history of the 1912 North Mount Lyell Disaster.Chalcopyrite does not contain the most copper in its structure relative to other minerals, but it is the most important copper ore since it can be found in many localities and occurs in a variety of ore types. The brassy-yellow colours in Chalcopyrite mean it is often confused with pyrites and gold, leading to use of the term, "fool's gold." Chalcopyrite has been the primary ore of copper since smelting began five thousand years ago. 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.This hand sized solid mineral specimen has shades of brass-yellow with spots of iridescent green-black tarnish. Chalcopyrite is a copper iron sulphide mineral and a major ore of copper common in sulphide veins and disseminated in igneous rocks. Chalcopyrite has a hardness of 3.5-4 on the Mohs Scale. It is a member of the tetragonal crystal system and has metallic lustre and opaque transparency.burke museum, beechworth, indigo shire, beechworth museum, geology, geological specimen, chalcopyrite, copper pyrites, copper mining, tasmanian geology, mount lyell, mount lyell mines, fools gold, mohs scale, crystals, minerals, historical geological collection, victorian geological survey, a.r.c selwyn, gold rush, van diemans land

"The dry stone walls provide a tangible link to the area’s white settlement, and they remain a symbol of the profound change in land usage from the original Kulin custodians to the European arrivals of the nineteenth century. The bulk of dry stone wall construction in Victoria occurred between the 1850s and 1880s. The gold rush of the early 1850s in particular inspired a flurry of construction. At this time, labour previously available for shepherding livestock dried up, as men gravitated to the goldfields to seek their fortunes. This necessitated the building of fencing to contain the district’s growing number of sheep, cattle and horses. An explosion in surveying, subdivision and the sale of Crown lands also contributed to a boost in construction. Government regulations that punished pastoralists for allowing their livestock to stray provided further incentive to fence-off previously open expanses of land. The major benefit of this type of fencing was that it utilised the materials at hand; the plentiful grey basalt that scattered the landscape. In the case of the dry stone walls built around Melton, the characteristic round or oval shape of the volcanic fieldstones on the western plains inspired some distinctive designs.54 Another advantage of dry stone walls was their ability to withstand the ravages of flood, fire and drought often experienced in the district. This durability accounts for the fact that many of these fences still exist today". Dry Stone Wall trail brochure/pamphlet for visitors provided by Melton Visitor Information Centrecouncil, landscapes of significance

The art of making glass can be traced back to 2600 BC in Mesopotamia. Egyptians practised making glass around 2500 BC. Artificial glass first appeared in the Egyptian or the Mesopotamian civilization, whereas they used tools made out of volcanic glass obsidian in the Stone Age. Ancient China, however, discovered how to make glass a little later. Glass beads are known to be one of the earliest products made out of glass. Their creation is thought to be primarily accidental. In the later Bronze Age, glassmaking came to a halt. Glass was a luxury material back then. Archaeological excavations suggest the use of glass in England during the middle ages. In the 10th century, stained glass found a place in cathedrals and windows of palaces. After the Renaissance, architectural methods changed substantially, leading to a decrease in stained glass as a building material. Domestic use of glass increased following the industrial revolution. Vessels, glass windows, and glass beads gained popularity in Europe during this period. During the 19th century, many people preferred glass windows and doors as a decorative option. In the late 19th century, some designers brought back stained glass in decorative windows. It was during this period that Mr Tiffany discovered several methods to make domed glass handicrafts. People discovered the true versatility of using glass as a building material only in the 20th century. With glassmaking technology receiving an industrial boom, you could produce several different types of glass. Toughened glass, laminated glass, bulletproof glass, and smart glass all boosted the use of glass in buildings. Today, several skyscrapers, small and big homes, and offices use glass in almost all aspects of construction and design. https://www.aisglass.com/glass-made-step-step-process/The invention and development of glass, both as domestic items and in building, has been nothing short of revolutionary. Prior to the use of glass for windows, the interior of buildings were extremely dark, even during sunny days. The use of glass domestic objects, that could be easily washed, led to improved hygiene.Cylindrical drinking glass with stepped relief around lipNoneflagstaff hill, warrnambool, shipwrecked-coast, flagstaff-hill, flagstaff-hill-maritime-museum, maritime-museum, shipwreck-coast, flagstaff-hill-maritime-village, glass

The art of making glass can be traced back to 2600 BC in Mesopotamia. Egyptians practised making glass around 2500 BC. Artificial glass first appeared in the Egyptian or the Mesopotamian civilization, whereas they used tools made out of volcanic glass obsidian in the Stone Age. Ancient China, however, discovered how to make glass a little later. Glass beads are known to be one of the earliest products made out of glass. Their creation is thought to be primarily accidental. In the later Bronze Age, glassmaking came to a halt. Glass was a luxury material back then. Archaeological excavations suggest the use of glass in England during the middle ages. In the 10th century, stained glass found a place in cathedrals and windows of palaces. After the Renaissance, architectural methods changed substantially, leading to a decrease in stained glass as a building material. Domestic use of glass increased following the industrial revolution. Vessels, glass windows, and glass beads gained popularity in Europe during this period. During the 19th century, many people preferred glass windows and doors as a decorative option. In the late 19th century, some designers brought back stained glass in decorative windows. It was during this period that Mr Tiffany discovered several methods to make domed glass handicrafts. People discovered the true versatility of using glass as a building material only in the 20th century. With glassmaking technology receiving an industrial boom, you could produce several different types of glass. Toughened glass, laminated glass, bulletproof glass, and smart glass all boosted the use of glass in buildings. Today, several skyscrapers, small and big homes, and offices use glass in almost all aspects of construction and design. https://www.aisglass.com/glass-made-step-step-process/The invention and development of glass, both as domestic items and in building, has been nothing short of revolutionary. Prior to the use of glass for windows, the interior of buildings were extremely dark, even during sunny days. The use of glass domestic objects, that could be easily washed, led to improved hygiene.Moulded patterned glass butter dish. Base has been broken.None.flagstaff hill, warrnambool, shipwrecked-coast, flagstaff-hill, flagstaff-hill-maritime-museum, maritime-museum, shipwreck-coast, flagstaff-hill-maritime-village, glass, kitchen item, butter

Dry stone construction as a technique is used for much more than paddock walls. Across the volcanic plains of western Victoriaare marvelous sheep dips, stock loading ramps, huts, dams, retaining walls, and the rich and largely undiscovered heritage of indigenous dry stone structures. Dry stone walls indicate many aspects of our rural environment; the geological beginnings of the way the landscape was created, the patterns of early settlement by pastoralists and squatters, the types of stock that grazed the land and the methods of cattle and sheep management, of the efforts to thwart the spread of rabbits .... "For the casual but interested observer dry stone walls are good to look at, to photograph, to get up alongside and see the way they are constructed, to appreciate the varying shapes and sizes of stones and learn of the techniques of keeping often quite rounded stones in place. Apart from walls and other dry stone structures on grazing land we can also see dry stone techniques used in other places and in other phases of our history. Indigenous Australians have built, and continue to build, structures for shelter or hunting or trapping eels and fish in rivers and estuaries around the country. At spots around our coast line there is evidence of simple stone structures built by early maritime explorers. Prospectors in early mining encampments used dry stone construction to build retaining walls or the low walls of rudimentary shelters. If the future of dry stone walls in the Australian landscape is to be assured. wall owners and local governments have to accept and embrace their custodial role in assuring the preservation and celebration of walls. This is not an easy task, but, along with putting the necessary statutory mechanisms to ensure their retention, it is a task that must be pursued. The Dry Stone Walls Association of Australia has as its primary goal the increase in awareness of wall owners and local governments of the importance of dry stone walls. It also seeks to increase the level of training of skilled and semi skilled wallers, and the gaining of rudimentary skills by farmers so that they can maintain their own walls". Melton Star Weekly article about the Stone Wallslandscapes of significance

Six year old Judith Furphy was the first person known to have been buried at Kangaroo Ground Cemetery in May 1851. The cemetery is situated on an ancient river bed with exposed Nillumbik sands. The rest of the district is formed from black volcanic soil which was hard to dig. According to local historian Mick Woiwod (deceased) the site may have been a burial ground for the local Wurundjeri people as the exposed softer sands were always their prefered camping sites. The Hon. Ewen Hugh Cameron who lived at Pigeon Bank and was the Member for Evelyn for 40 years (1874-1914) was buried here in 1915. Published: Nillumbik Now and Then /​ Marguerite Marshall 2008; photographs Alan King with Marguerite Marshall.; p39 The Wurundjeri people might have buried their dead on the site of the Kangaroo Ground Cemetery, according to local historian Mick Woiwod. Kangaroo Ground was a premier hunting ground, but camping on the black volcanic soil would have been uncomfortable. Unlike most of Kangaroo Ground, its cemetery, on an ancient river bed, comprises a rare exposure of Nillumbik sands – always the preferred campsite for Aboriginal people. The cemetery area is the only place where the soil was soft enough to dig a grave easily.1 Six-year-old Judith Furphy was the first person known to have been laid to rest at the Kangaroo Ground Cemetery. She died on May 17, 1851, from a chill caught by resting on wet grass. Local Andrew Ross wrote ‘..no public burying place existed nearer than Melbourne. The case being considered urgent, a general meeting of the settlers took place on the evening of the 17th……. The result was the selection of unoccupied crown land …….which was subsequently granted by Government for a public cemetery.’2 Judith was buried the next day on May 18. Her grave was marked by the trustees with a plaque, which unfortunately states nine years old, when she was probably only six. Judith came from an illustrious family. Her brother, Joseph, was the author of Such is Life and other works. Another brother, John, developed and manufactured the famous Furphy water cart, which distributed water to World War One soldiers along with the latest rumours. Hence the name Furphy entered the Australian idiom, as synonymous with ‘rumour’. Judith’s father Samuel helped build the first Kangaroo Ground church school. Inside, near the entrance of the cemetery, on Yarra Glen Road, stand a rotunda and a water tank. Occasional benches invite mourners to pause and remember. The gate with wrought iron and brick supports, bears the inscription ‘Erected by Sir Ewen and Lady Cameron in memory of their daughter, Flora Margaret’. These are only two of the famous people connected with this cemetery. The Hon. Ewen Hugh Cameron JP and MLA from 1874 to1914, who lived at Pigeon Bank, Warrandyte Road, was buried here in 1915. Unrelated, but with the same name, was Sir Ewen Cameron who had been Minister for Health and was laid to rest there in 1964. Sir Herbert Gepp, a leading industrialist and the former owner of Garden Hill, at Yarra Glen Road, was buried there in 1954.3 Many of the more imposing tombstones belong to the earlier graves. Unfortunately bushfires have cracked several. But this adds to the melancholy attractiveness of the cemetery, graced by some beautiful eucalypts, cypress and pines. Early pioneering families represented at the cemetery include Armstrong, Barr, Bell, Harkness, Jardine, Johnston, Rogerson, Stevenson, Thomson and Walters. Armstrong and Bell were among the first families to come to the district and Stevenson owned the district’s first sheep station. It took in much of present day Christmas Hills, which was the name he gave his sheep station. Harkness was the first to suggest a Kangaroo Ground school be built, and one of the first to suggest establishing the Eltham District Road Board. Many of these families leased pastoral land before the mid-century and bought land when it came on sale in 1849. In the cemetery’s early days sections were devoted to the major Christian denominations (mainly the Protestant) and one section was set aside for ‘other’ or ‘non-believers’. However in modern times burial plots have not been placed in areas according to religious beliefs.This collection of almost 130 photos about places and people within the Shire of Nillumbik, an urban and rural municipality in Melbourne's north, contributes to an understanding of the history of the Shire. Published in 2008 immediately prior to the Black Saturday bushfires of February 7, 2009, it documents sites that were impacted, and in some cases destroyed by the fires. It includes photographs taken especially for the publication, creating a unique time capsule representing the Shire in the early 21st century. It remains the most recent comprehenesive publication devoted to the Shire's history connecting local residents to the past. nillumbik now and then (marshall-king) collection, kangaroo ground, eltham-yarra glen road, agnes bell cameron, agnes cameron (nee bell), cameron family, edward aubrey haughton, eugene cameron, evelyn florence cameron, ewen hugh cameron, gravestones, jane armstrong, jane bell, jessie agnes haughton (nee cameron), jessie cameron, john donald cameron, kangaroo ground cemetery, neville cameron, simon armstrong, vera cameron, william bell armstrong, wurundjeri

Feldspathic arenites are sandstones that contain less than 90% quartz, and more feldspar than unstable lithic fragments, and minor accessory minerals.Feldspathic sandstones are commonly immature or sub-mature.These sandstones occur in association with cratonic or stable shelf settings. Feldspathic sandstones are derived from granitic-type, primary crystalline, rocks. If the sandstone is dominantly plagioclase, then it is igneous in origin Sandstone features prominently in public buildings throughout Victoria. Most of the sandstone used as dimension stone in the State came from three sources: the Heatherlie quarry in the Grampians (Silurian), the Bacchus Marsh area (Permian), and the Barrabool Hills near Geelong (Cretaceous).Sandstone features prominently in public buildings throughout Victoria, making this specimen special as it shows the materials used by Victorian building companies. Sandstone can also be crushed, crushed stone is used in the construction of roadways and road structures such as bridges, and in buildings, both commercial and residential. 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 feldspar-rich sandstone, a sandstone intermediate in composition between an arkosic sandstone and a quartz sandstone, containing 10% to 25% feldspar and less than 20% matrix material of clay, sericite, and chlorite. Feldspathic arenite containing less than 90 percent of the composition of quartz. Feldspar is the main composition. Feldspathic arenite may contain fragments of unstable rock, and a little amount of other minerals such as mica and heavy minerals. Some feldspathic arenite have pink or red color because of the presence of potassium feldspar or iron oxide. There are also colored light gray to white. These sandstones are usually medium to coarse grained and can contain a high percentage of granules with angular until subangular roundness. The content of the matrix can appear as the rest up to more than 15 percent, and sorting of grains can present as moderate to poorly sorted. Feldspathic sandstones are generally immature in textural maturity. Feldspathic arenite can not be judged from the structure of the sediment. Bedding can emerge from the laminate parallel to the crossbed. Fossils may appear in the layer deposited on the sea. Feldspathic arenites usually appear on the craton or the continental shelf, which can be associated with conglomerate, quartz lithic arenite, carbonate rock, or evaporites. This sandstone may also appear on the succession of sedimentary basins deposited on an unstable or deep sea, and moving arc setting. According to Pettijohn (1963) Arkose make up about 15 percent of all sandstones. Some Arkose formed in situ when the granite and related rocks disintegrate and generate granular sediments. Most of the material feldspathic sandstones derived from primary crystalline granitic rocks, such as granite or metasomatic rocks containing abundant potassium feldspar. Mineral contained in sandstones is mostly a form of plagioclase feldspar derived from quartz diorite or volcanic rock. Feldspar contained on this sandstone comes from arid to cool climates when the chemical weathering process is reduced.sandstone, natural stone, feldspathic sandstone, burke museum, geology, geological, geological specimen

The nine postcards in this set were donated together and date to the early 1900s. All but one postcard in this set shows images of Warrnambool, in the Western District of Victoria; the other has a London image. The postcards were all printed in Great Britain according to that country’s postal regulations. The fronts of all cards have titles printed in red. Most of the images on the cards are attributed to photographer Joseph Jordan and belong to the Jordan Series. The back of these cards has an outline for a postage stamp, a vertical dividing line and a heading on each side of the line to separate the Correspondence from the Address. Postcards or ‘correspondence cards’ appeared in Britain in 1894. They were plain cards with a space for the message on one side and an address on the other; regulations didn’t allow anything but the address to be written on the ‘address’ side. In 1902 the British regulations then allowed a picture to be printed on the front and the address on the back, so messages had to be written on the picture side. Soon, the regulations changed and the back was divided for a message and the address. Tower Hill and Lake, Warrnambool – Tower Hill Wildlife Reserve is in the crater of a dormant volcano. In 1892 the area was declared a National Park, the first in Victoria, preserving native animals and Indigenous plants. The rich volcanic soil in the area attracted early settlers including the families of Henry Giles, born at Tower Hill in 1858 and his wife Mary Jane (born Freckleton) born nearby at Cooramook in 1860. Henry and Mary worked in the local area where they also raised their six children. For a time, Henry was employed as a labourer on the Warrnambool Breakwater. Joseph Jordan - Joseph Jordan was born in 1841 in Leicester England. When he was 16 he joined the 7th Queen's Own Hussars and was sent to India at the outbreak of the mutiny. He took part in the relief of Lucknow and remained in India for eleven years. It was during this time that he became interested in photography. He was posted to New Zealand and later came to Victoria, becoming a sergeant major of the Mounted Rifles. In the mid-1880s he came to the Western district where he was responsible for establishing units of the Mounted Rifles in various country towns such as Dunkeld, Mortlake, Panmure, Bushfield, Koroit etc. He resigned from the army in 1889 and set up a professional photography studio in Liebig Street, Warrnambool. He became very well known in the Western District for family photographs, official photographs of local councillors and groups as well as views of local scenery. In 1891 he photographed the wrecked barque ‘Fiji’ at ‘Wrecks Beach’ near Princetown. His business was taken over by his son Arthur around 1917. Joseph was a keen rifle shot and in 1924 he donated the "Jordan Shield" as a prize to the Victorian Rifle Association. He was made a "Life Honorary Member" of the Warrnambool Returned Soldiers League and in 1933 he was recognised as being the oldest living soldier in Victoria. Joseph died in 1935 aged 95.The postcard of Tower Hill and Lake is connected to the location near Warrnambool where many of our early settlers lived and worked. One of these settlers was the Giles family, whose son Henry was born at Tower Hill. His family has donated many Victorian-era items which are now on display at Flagstaff Hill. Tower Hill National Park is the first place in Victoria to be named a National Park. As in the times when coastal trading ships brought passengers and cargo to the Port of Warrnambool, it continues to be a popular place to visit. Joseph Jordan is a significant figure in Warrnambool history as he helped to establish early units of the Mounted Rifles (G Company) in local towns during the late 1880's and later, photographed local scenes, groups and citizens of early Warrnambool.Postcard, one of nine, landscape orientation, coloured print within a rectangle and an impressed line around the image on the front. The picture shows several islands close together with hills around them and bushland in the foreground. There are dead trees amongst the vegetation and a sandy shore at the foot of some of the hills. The lower left corner shows what appears to be two white rails, possibly a lookout fence. There is no correspondence written on the card. The title is printed in red on the front and the back has inscriptions and outlines for a postage stamp. Jordan Series, printed in Great Britain. Front, in red: “Tower Hill Lake, Warrnambool” Back in green: “Jordan Series” “POST CARD” “PRINTED IN GREAT BRITAIN” “For correspondence” “The Address only to be written here”flagstaff hill maritime museum, flagstaff hill maritime village, flagstaff hill maritime museum and village, maritime museum, warrnambool, great ocean road, warrnambool and district, warrnambool scenes, local scenes, views of warrnambool, joseph jordan, jordan series, jordan photography, postcard, souvenir, correspondence, cameo postcard, tower hill, tower hill national park, victoria's first national park, henry giles, mary jane freckleton, breakwater, early settlers