Red Rock, Alvie, near Colac, is a complex of approximately 30 volcanic eruption points and is the Southern most of a chain of three volcanoes, the others being Warrion Hill and Alvie Hill. It is arguably the youngest eruption point in Victoria at around 8000 years, especially since the age of Mt Napier has been progressively pushed back. The highest point (on the Northern side) has many interesting features, including some awesome spatter ramparts. Driving around the rim to the south, you can also see layered tuff. There are some good views out to Lake Corangamite and the lava flows (probably from Warrion Hill) can be seen where they have entered the lake. Most of Red Rock is in private land, with two lookout points with some interpretive information. The water depicted in this photograph is not evident in 2019. Type: Volcanic Complex Location: South of Alvie, Victoria Last Eruption: 8000 years ago Access: Mostly private land, but there is an access road and some interpretive signage Visited: Visited Colour photograph of sisters Clare Gervasoni (left), Ann Gervasoni (centre) and Lisa Gervasoni and Red Rock, Alvie clare gervasoni, lisa gervasoni, ann gervasoni, red rock alvie

Native Sulphur in its solid form is a yellow crystalline mineral that forms near volcanic vents and fumaroles where it is the solid form of hot gases. It is also frequently found in the subsurface as a by-product of sulphide ore mineralization. In all its forms, sulphur is one of the most commonly occurring minerals on the planet, especially in natural gases, and is key to the make-up of a range of other minerals. It is essential to continuing life on earth, and was used in ancient societies as part of medical care, religious rites, and entertainment, and was key to the invention of gunpowder by the Chinese. Native Sulphur in its solid form is a yellow crystalline mineral that forms near volcanic vents and fumaroles where it is the solid form of hot gases. It is also frequently found in the subsurface as a by-product of sulphide ore mineralization. In all its forms, sulphur is one of the most commonly occurring minerals on the planet, especially in natural gases, and is key to the make-up of a range of other minerals. It is essential to continuing life on earth and was used in ancient societies as part of medical care, religious rites, and entertainment, and was key to the invention of gunpowder by the Chinese. The exact site of extraction for this specimen is unknown, but it was probably collected in New Zealand in the 1850s. Sulphur is significant both for its historical and current uses, and for its nature as one of the most abundant minerals on the planet. Sulphur's importance comes both from its abundance and its role in ensuring survival, creating other minerals, and daily human life. This specimen is significant as representative of sulphur's solid properties. 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, small, crystalline mineral specimen that is largely bright yellow, with some darker spotting. geological specimen, geology, geology collection, burke museum, beechworth, sulphur, native sulphur, new zealand, native sulphur specimen, sulphur specimen

Copy of Rose Series postcard #385 showing the new Mt Dandenong Tourist Road with wooden railing fence on low side of road. Surface not yet made. This photograph has a detailed inscription on the back handwritten by John Lundy-Clarke in 1974.View downhill from the Windy Bend showing the site of the 1972 landslide. In this picture the road is running along the top edge of the wall 900’ thick of Kalorama Docite that plunges thousands of feet deep down into the earth below the Ranges and extends to Fern Tree Gully. It was once a horizontal terrace nearly ten miles square and tipped over to the left when the mountain subsided into its volcanic cauldron.mt dandenong road, rose series, windy bend, landslide

E560 N6 Dec 1979 A43 The back-hoe works on the beginnings of pit 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.

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

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

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

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

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