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

Basalt is a common igneous rock that composes most of the Earth's surface and can be found on the Moon and other rocky planets of the Solar System. It is generally composed minerals such as calcic plagioclase, clinopyroxene and iron ore which form grains that are indistinguishable to the naked eye. It can be dark grey or black in colouring and sometimes may contain holes left by gas bubbles. Most of the Earth's basalt was produced in environments such as oceanic divergent boundaries, oceanic hotspots, and mantle plumes and hotspots beneath continents. Basalt is commonly used in construction where it is crushed and used for multiple purposes such as concrete aggregate, road base, or railroad ballast. Thin slabs of basalt can also be cut and used for floor tiles, stone monuments, and building veneer. This particular specimen was excavated from Talbot in Victoria, which was a small gold mining town established in 1852. As basalt is a common rock, it is not specific to Talbot. However, this specimen can be assumed to be of the Cainozoic age due to previous geomorphic surveys of the area. This particular type of Basalt was used mainly for roads due to the durability of the rock.Basalt holds significance due to the continued use of the rock from historic until present times. The rock has been utilised for many types of construction and is still used for the same purposes today. Basalt also has significance to the Earth and other rocky planets of the Solar System as it makes up most of the planet's surface. 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 smaller than hand sized rock specimen which is dark grey in colour with small holes and white deposits across its surface.Geological survey / [illegible] /burke museum, beechworth, geological specimen, geology, basalt, basalt specemin, indigo shire, talbot, cainozoic, igneous rock

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

Sphalerite or sphaelerite is named from the Greek word for 'treacherous' or 'deceiver' as specimens can vary widely in appearance, making them hard to visually identify. It is a zinc sulfide with the chemical composition (Zn,Fe)S, the most important ore of zinc. Specimens of sphalerite can contain iron as a substitute for up to 25% of the usual zinc present, as well as trace elements of gallium, cadmium, geranium and indium. Small amounts of arsenic and manganese may also be detected. Sphalerite is found in igneous, sedimentary and metamorphic rocks. It forms when carbonate rock encounters acidic, zinc-bearing fluid. It often forms in veins or in fissures of the existing rock, with colours and crystal shapes dependent on the composition of the the combining elements. It forms isometric crystal shapes including cubes, tetrahedrons, octahedrons, dodecahedrons. This specimen was collected in approximately 1852, in Broken Hill, NSW, as an adjunct to 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.The specimen is significant as an 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.A pipe-shaped specimen of sulfide-mineral zinc ore displaying patches of black, brown, beige and gold colouring. The main item has associated broken pieces. geological specimen, geology, geology collection, burke museum, beechworth, mineralogy, indigo shire, geological survey, sphalerite, sphaelerite, zinc ore, broken hill, nsw, victoria, galena, fluorite, chalcopyrite, lead, cadmium, gallium, germanium, indium, iron

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. Although relatively common and semi-precious, agate has been prized since at least 1450 BC - an intricately carved agate seal was found in the 2015 excavation of a grave belonging to a Mycenaeum priest or warrior near Pylos in Greece. Agate is also used in jewellery and other decorative or ritual purposes due to its often striking appearance. Quartz is found all over Australia, including Beechworth in Victoria. It is formed in deep-seated igneous rocks and crystallized through hot aqueous solutions. It can have two forms; Microcrystalline quartz or Crystalline quartz. Microcrystalline quartz is a fine grain quartz where crystalline quartz is often a large crystal. The colour of quartz can vary. These specimens were collected in Victoria in the vicinity of the Burke Museum. 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.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.Geological specimens of Agate and Quartz respectively; the fist-sized piece of Agate has peach/coral colouring with grey concentric patterning and the smaller piece of quartz is a uniform yellow/orange shade. Existing label: Local pebbles / (agate and / quartz / (yellowish) / egg-shaped). / BB geological specimen, geology, geology collection, burke museum, beechworth, agate, quartz, north-east victoria, indigo shire, geological surveys

"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

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

A quarry was transformed into the Blue Lake. Published: Nillumbik Now and Then /​ Marguerite Marshall 2008; photographs Alan King with Marguerite Marshall.; p179 The dramatic steep-sided Plenty Gorge lies along the divide of two geological areas, and separates the Nillumbik Shire and the City of Whittlesea. On the Nillumbik side are undulating hills and sedimentary rock, and in Whittlesea, lies a basalt plain formed by volcanic action up to two million years ago. This provides the Plenty Gorge Park with diverse vegetation and habitats, making it one of Greater Melbourne’s most important refuges for threatened and significant species. The park, established in 1986, consists of around 1350 hectares, and extends 11 kilometres along the Plenty River, from Greensborough to Mernda. It provides a wildlife corridor for around 500 native plant and 280 animal species.1 The area’s plentiful food and water attracted the Wurundjeri Aboriginal people and then European settlers. By 1837 squatters had claimed large runs of land for their sheep and cattle. The Plenty Valley was among the first in the Port Phillip District to be settled - mainly in the less heavily timbered west - and was proclaimed a settled district in 1841.2 But by the late 1880s, the settlers’ extensive land clearing for animal grazing, then agriculture, depleted the Wurundjeri’s traditional food sources, which helped to drive them away. Many Wurundjeri artefacts remain (now government protected), and so far 57 sites have been identified in the park, including scarred trees, burial areas and stone artefacts. Pioneer life could be very hard because of isolation, flooding, bushfires and bushrangers. Following the Black Thursday bushfires of 1851, basalt was quarried to build more fire-resistant homes. Gold discoveries in the early 1850s swelled the population, particularly around Smugglers Gully; but food production made more of an impact. In the late 1850s wheat production supplanted grazing. In the 1860s the government made small holdings available to poorer settlers. These had the greatest effect on the district, particularly in Doreen and Yarrambat, where orchards were established from the 1880s to 1914. Links with a prominent early family are the remains of Stuchbery Farm, by the river’s edge bounded by Smugglers Gully to the north and La Trobe Road, Yarrambat, to the east. The Stuchberys moved to the valley in 1890, and the family still lives in the area. In 1890, Alfred and Ada first lived in a tent where four children were born, then Alfred built the house and outbuildings around 1896. They planted an orchard, then a market garden, and developed a dairy. The family belonged to the local Methodist and tennis communities. Their grandson Walter, opened the Flying Scotsman Model Railway Museum in Yarrambat, which his widow, Vi, continues to run. Wal was also the Yarrambat CFA Captain for 22 years until 1987. Walter sold 24 hectares in 1976 for development - now Vista Court - and in 1990, the remaining 22.6 hectares for the park. Remaining are an early stone dairy and remnants of a stone barn, a pig sty and a well.3 Until it was destroyed by fire in 2003, a slab hut stood on the Happy Hollow Farm site, at the southern end of the park. The hut is thought to have been built in the Depression around 1893. This was a rare and late example of a slab hut with a domestic orchard close to Melbourne. Emmet Watmough and his family first occupied the hut, followed by a succession of families, until the Bell family bought it around 1948. There they led a subsistence lifestyle for 50 years, despite encroaching Melbourne suburbia.4 The Yellow Gum Recreation Area includes the Blue Lake, coloured turquoise at certain times of the year. Following the 1957 bushfires, this area was quarried by Reid Quarries Pty Ltd for Melbourne’s first skyscrapers, then by Boral Australia. However in the early 1970s water began seeping into the quarry forming the Blue Lake and the quarry was closed. The State Government bought the site in 1997 and opened it as a park in 1999.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, blue lake, plenty gorge park

Hawthorn hedges are important reminders of Kangaroo Ground's Scottish heritage. They are Registered on the Victorian Heritage Register. They are "historically significant because the planting of hawthorn hedges reflects the adoption of Eurorpean farming techniques by the Kangaroo Ground population in the period following settlement and because the grid pattern of paddocks that the Hawthorn hedges define is very different to today's farm landscapes." Covered under Heritage Overlay, Nillumbik Planning Scheme. Published: Nillumbik Now and Then /​ Marguerite Marshall 2008; photographs Alan King with Marguerite Marshall.; p21 Hawthorn hedges bordering Kangaroo Ground’s gently rolling farmlands are important reminders of its Scottish heritage and are rare so close to Melbourne.1 As early as the 1840s newly arrived farmers from Scotland planted hawthorn hedges around their properties, to protect crops from the numerous kangaroos and wallabies. Many of these hedges survive today. These farmers had the good fortune to settle some of the most fertile land available for cropping in the Colony of Victoria. At that time the black volcanic soil could sustain an amazing two crops a year. By the mid 1850s, 500 acres (202ha) of wheat were growing in Kangaroo Ground. But the crops were threatened by kangaroos, which were so plentiful, that Surveyor-General, Robert Hoddle, named the district Kangaroo Ground in 1838. As post-and-rail fences proved inadequate barriers for the bounding kangaroos, the Scots planted hawthorn hedgerows as they had done in Scotland. Some also used the hedges to net birds, presumably for the table. Interestingly the farmers in the bordering townships of Panton Hill and Christmas Hills, did not plant hawthorn hedges around their properties. Perhaps it was because by the time they settled in the 1860s and 1870s most of the wildlife had been gunned down by residents.2 The canny Scots planted the hedges on public land outside their own farms, as the hedgerows could spread to about five yards (five m) in width. With this impenetrable barrier Kangaroo Ground’s industrious farmers flourished to gain the economic power that saw the Shire of Eltham governed from Kangaroo Ground for 79 years (1858-1937). The Scots jealously guarded their land, so hard to get in Scotland. That is why they refused to release any of it ‘for local roads to follow easier grades as was the case in surrounding districts where roads generally followed ridgelines or streams’.3 Instead the roads were built in accordance with the magnetic bearings of their first survey in 1847 whether that suited the steep topography or not. This could force traffic to diverge when wet through Greensborough and Diamond Creek. Until 1921, the Eltham-Yarra Glen Road beside Wellers Restaurant, ‘dipped down into the upper reaches of Stony Creek’.4 Later some corners were compulsorily cut for the increasing motor traffic. As late as the 1960s, corners were cut to form sweeping curves above and alongside the Kangaroo Ground Cemetery and opposite the Emergency Operations Centre. In the latter case, the farmers – understanding their hedgerows as important heritage – insisted upon their reinstatement to conform to the altered road alignment. Kangaroo Ground’s ancient manna gums also point to the district’s history and to that of the hedgerows. The Aboriginal people had transformed the original forests into grasslands with the fires they lit to attract kangaroos, (which the Scots were to exclude by planting hedgerows). But the Wurundjeri hunters left the gums (Eucalyptus vimminalis cygnetensis), on the grasslands as ‘stalking trees’ to hunt kangaroos. The hawthorn hedges in Kangaroo Ground were neglected for around 60 years from about the middle of the 20th century. Bushfires had created gaps and the hedgerows were not trimmed. Then in late 2005, local historian Mick Woiwod, formed a group to lobby the Nillumbik Shire to restore the hedges, which could last for many centuries. Some hedges in parts of Britain date back to AD 800.5 Although the original Scottish farmers have gone, the hedges are a reminder of when they flourished in the district, which has changed little in 150 years.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, eltham-yarra glen road, hawthorn hedgerow, kangaroo ground

Stuchbery Farm was situated on the Plenty River bounded by Smugglers Gully to the north and La trobe Road, Yarrambat, to the east. Alan and Ada Stutchbery moved to the valley in 1890, first living in a tent where four children were born. Alfred built a home and outbuildings around 1896. They planted an orchard, then a market garden and developed a dairy. Published: Nillumbik Now and Then /​ Marguerite Marshall 2008; photographs Alan King with Marguerite Marshall.; p179 The dramatic steep-sided Plenty Gorge lies along the divide of two geological areas, and separates the Nillumbik Shire and the City of Whittlesea. On the Nillumbik side are undulating hills and sedimentary rock, and in Whittlesea, lies a basalt plain formed by volcanic action up to two million years ago. This provides the Plenty Gorge Park with diverse vegetation and habitats, making it one of Greater Melbourne’s most important refuges for threatened and significant species. The park, established in 1986, consists of around 1350 hectares, and extends 11 kilometres along the Plenty River, from Greensborough to Mernda. It provides a wildlife corridor for around 500 native plant and 280 animal species.1 The area’s plentiful food and water attracted the Wurundjeri Aboriginal people and then European settlers. By 1837 squatters had claimed large runs of land for their sheep and cattle. The Plenty Valley was among the first in the Port Phillip District to be settled - mainly in the less heavily timbered west - and was proclaimed a settled district in 1841.2 But by the late 1880s, the settlers’ extensive land clearing for animal grazing, then agriculture, depleted the Wurundjeri’s traditional food sources, which helped to drive them away. Many Wurundjeri artefacts remain (now government protected), and so far 57 sites have been identified in the park, including scarred trees, burial areas and stone artefacts. Pioneer life could be very hard because of isolation, flooding, bushfires and bushrangers. Following the Black Thursday bushfires of 1851, basalt was quarried to build more fire-resistant homes. Gold discoveries in the early 1850s swelled the population, particularly around Smugglers Gully; but food production made more of an impact. In the late 1850s wheat production supplanted grazing. In the 1860s the government made small holdings available to poorer settlers. These had the greatest effect on the district, particularly in Doreen and Yarrambat, where orchards were established from the 1880s to 1914. Links with a prominent early family are the remains of Stuchbery Farm, by the river’s edge bounded by Smugglers Gully to the north and La Trobe Road, Yarrambat, to the east. The Stuchberys moved to the valley in 1890, and the family still lives in the area. In 1890, Alfred and Ada first lived in a tent where four children were born, then Alfred built the house and outbuildings around 1896. They planted an orchard, then a market garden, and developed a dairy. The family belonged to the local Methodist and tennis communities. Their grandson Walter, opened the Flying Scotsman Model Railway Museum in Yarrambat, which his widow, Vi, continues to run. Wal was also the Yarrambat CFA Captain for 22 years until 1987. Walter sold 24 hectares in 1976 for development - now Vista Court - and in 1990, the remaining 22.6 hectares for the park. Remaining are an early stone dairy and remnants of a stone barn, a pig sty and a well.3 Until it was destroyed by fire in 2003, a slab hut stood on the Happy Hollow Farm site, at the southern end of the park. The hut is thought to have been built in the Depression around 1893. This was a rare and late example of a slab hut with a domestic orchard close to Melbourne. Emmet Watmough and his family first occupied the hut, followed by a succession of families, until the Bell family bought it around 1948. There they led a subsistence lifestyle for 50 years, despite encroaching Melbourne suburbia.4 The Yellow Gum Recreation Area includes the Blue Lake, coloured turquoise at certain times of the year. Following the 1957 bushfires, this area was quarried by Reid Quarries Pty Ltd for Melbourne’s first skyscrapers, then by Boral Australia. However in the early 1970s water began seeping into the quarry forming the Blue Lake and the quarry was closed. The State Government bought the site in 1997 and opened it as a park in 1999.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, ada stuchbery, alan stuchbery, dairy, stuchbery farm, farm buildings, yarrambat, plenty gorge park

The sharpening stone can also be referred to as a whetstone, oil stone or honing stone. It is a well-worn double-sided sharpening stone retrieved from the wreck site of the Loch Ard. It is used to grind and hone the edges of metal blades and tools. ‘Natural’ sharpening stones like this one are quarried from ancient sedimentary rock that has metamorphosed from clay and volcanic ash to produce garnet crystals. Most modern stones are artificially produced, or ‘bonded’, abrasive stones, made by fusing clay and metal powder under heat and pressure. The softer yellow Corticule stone is found in thin vertical veins running through the more plentiful Belgian Blue rock. Coticule is a fine-grained and dense material that ‘cuts’ metal slowly but to a superior standard of sharpness and finish. The relatively coarser Belgian Blue is stronger and ‘cuts’ more quickly, but with a less polished finish. A double-sided whetstone is therefore valued for its increased durability (the harder BBW ‘backs’, or supports, the softer Coticule), and additional utility (the fine ‘grit’ of Coticule complements the coarser BBW to meet a range of sharpening needs). The blue-grey base of this stone is thinner than the remaining yellow Coticule on top. This suggests that the majority of grinding and honing work it has done on board the ship was for larger tools, rather than on surgical or shaving blades. Its rounded or spherical shaping may also be related to the ‘tumbling’ action of the sea on the ocean floor. History of the Loch Ard wreck: The Loch Ard got its name from ”Loch Ard” a loch that lies to the west of Aberfoyle, and the east of Loch Lomond. It means "high lake" in Scottish Gaelic. The vessel belonged to the famous Loch Line which sailed many vessels from England to Australia. The Loch Ard was built in Glasgow by Barclay, Curle & Co. in 1873, the vessel was a three-masted square-rigged iron sailing ship that measured 79.87 meters in length, 11.58 m in width, and 7 m in depth with a gross tonnage of 1693 tons with a mainmast that measured a massive 45.7 m in height. Loch Ard made three trips to Australia and one trip to Calcutta before its fateful voyage. Loch Ard left England on March 2, 1878, under the command of 29-year-old Captain Gibbs, who was newly married. The ship was bound for Melbourne with a crew of 37, plus 17 passengers. The general cargo reflected the affluence of Melbourne at the time. Onboard were straw hats, umbrellas, perfumes, clay pipes, pianos, clocks, confectionery, linen and candles, as well as a heavier load of railway irons, cement, lead and copper. There were other items included that were intended for display in the Melbourne International Exhibition of 1880. The voyage to Port Phillip was long but uneventful. Then at 3 am on June 1, 1878, Captain Gibbs was expecting to see land. But the Loch Ard was running into a fog which greatly reduced visibility. Captain Gibbs was becoming anxious as there was no sign of land or the Cape Otway lighthouse. At 4 am the fog lifted and a lookout aloft announced that he could see breakers. The sheer cliffs of Victoria's west coast came into view, and Captain Gibbs realised that the ship was much closer to them than expected. He ordered as much sail to be set as time would permit and then attempted to steer the vessel out to sea. On coming head-on into the wind, the ship lost momentum, the sails fell limp and Loch Ard's bow swung back towards land. Gibbs then ordered the anchors to be released in an attempt to hold their position. The anchors sank some 50 fathoms - but did not hold. By this time the ship was among the breakers and the tall cliffs of Mutton Bird Island rose behind. Just half a mile from the coast, the ship's bow was suddenly pulled around by the anchor. The captain tried to tack out to sea, but the ship struck a reef at the base of Mutton Bird Island, near Port Campbell. Waves subsequently broke over the ship and the top deck became loosened from the hull. The masts and rigging came crashing down knocking passengers and crew overboard. When a lifeboat was finally launched, it crashed into the side of Loch Ard and capsized. Tom Pearce, who had launched the boat, managed to cling to its overturned hull and shelter beneath it. He drifted out to sea and then on the flood tide came into what is now known as Lochard Gorge. He swam to shore, bruised and dazed, and found a cave in which to shelter. Some of the crew stayed below deck to shelter from the falling rigging but drowned when the ship slipped off the reef into deeper water. Eva Carmichael a passenger had raced onto the deck to find out what was happening only to be confronted by towering cliffs looming above the stricken ship. In all the chaos, Captain Gibbs grabbed Eva and said, "If you are saved Eva, let my dear wife know that I died like a sailor". That was the last Eva Carmichael saw of the captain. She was swept off the ship by a huge wave. Eva saw Tom Pearce on a small rocky beach and yelled to attract his attention. He dived in and swam to the exhausted woman and dragged her to shore. He took her to the cave and broke the open case of brandy which had washed up on the beach. He opened a bottle to revive the unconscious woman. A few hours later Tom scaled a cliff in search of help. He followed hoof prints and came by chance upon two men from nearby Glenample Station three and a half miles away. In a complete state of exhaustion, he told the men of the tragedy. Tom then returned to the gorge while the two men rode back to the station to get help. By the time they reached Loch Ard Gorge, it was cold and dark. The two shipwreck survivors were taken to Glenample Station to recover. Eva stayed at the station for six weeks before returning to Ireland by steamship. In Melbourne, Tom Pearce received a hero's welcome. He was presented with the first gold medal of the Royal Humane Society of Victoria and a £1000 cheque from the Victorian Government. Concerts were performed to honour the young man's bravery and to raise money for those who lost family in the disaster. Of the 54 crew members and passengers on board, only two survived: the apprentice, Tom Pearce and the young woman passenger, Eva Carmichael, who lost her family in the tragedy. Ten days after the Lochard tragedy, salvage rights to the wreck were sold at auction for £2,120. Cargo valued at £3,000 was salvaged and placed on the beach, but most washed back into the sea when another storm developed. The wreck of Lochard still lies at the base of Mutton Bird Island. Much of the cargo has now been salvaged and some items were washed up into Lochard Gorge. Cargo and artefacts have also been illegally salvaged over many years before protective legislation was introduced in March 1982. One of the most unlikely pieces of cargo to have survived the shipwreck was a Minton majolica peacock- one of only nine in the world. The peacock was destined for the Melbourne 1880 International Exhibition. It had been well packed, which gave it adequate protection during the violent storm. Today the Minton peacock can be seen at the Flagstaff Hill Maritime Museum in Warrnambool. From Australia's most dramatic shipwreck, it has now become Australia's most valuable shipwreck artifact and is one of very few 'objects' on the Victorian State Heritage Register. The shipwreck of the Loch Ard is of significance for Victoria and is registered on the Victorian Heritage Register ( S 417). Flagstaff Hill has a varied collection of artefacts from Loch Ard and its collection is significant for being one of the largest accumulation of artefacts from this notable Victorian shipwreck of which the subject items are a small part. The collections objects give us a snapshot of how we can interpret the story of this tragic event. The collection is also archaeologically significant as it represents aspects of Victoria's shipping history that allows us to interpret Victoria's social and historical themes of the time. Through is associated with the worst and best-known shipwreck in Victoria's history. A sharpening stone is also called a whetstone, oil, or honing stone. The stone is a worn double-sided rectangular block with rounded corners. There is a clear delineation between its coarser Belgian Blue base (grey colour) and its finer Belgian Coticule face (yellow colour). It bears sedimentary encrustation over one-third of its surface. flagstaff hill, warrnambool, shipwrecked coast, flagstaff hill maritime museum, maritime museum, shipwreck coast, flagstaff hill maritime village, great ocean road, loch line, loch ard, captain gibbs, eva carmichael, tom pearce, glenample station, mutton bird island, loch ard gorge, sharpening stone, whetstone, oilstone, double-sided stone, belgian coticule, belgian blue whetstone, oil stone, honing stone

In 1905 Richard Squire was manager of the West Berry Consols at Allendale, and developed an improved system of mine ventilation, which was supported in "The Age." He was successful in combating and remedying the gas and ventilation troubles of the Deep Mines of Creswick and Allendale Districts after all had failed. MINE MANAGERS’ ASSOCIATION. Ballarat Branch. ... Mr R. B. Squire, manager of the West Berry Consols, at Allendale, submitted a paper detailing what he had done tor the betterment of ventilation in the alluvial mines of Smeaton and Mary borough districts- Members gave Mr Squire every credit for the results that he claimed to have effected; the adoption of his ideas had testified to their value to mine-owners. It was painted out, however, that for want of a thorough debate of the subject with experienced men the author had unwittingly included some general statements that required modifying in some points and extending in others, in justice to other workers among the earlier and the present day managers of mines. It was decided to invite the author to meet a sub-committee on this subject!Various handwritten Letters from Richard Squire to his son Tom 1935richard squire, tom squire, hazel squire, jack squire, jim squire, ned, mt mercer, basil, plant, skids, pump, c. hayes, illness, poppet, carburetor, shaft, balance weight, pearson, pulleys, syndicate, goon, suction, lease, reports, estimates, flat fields, reef, banagwanth, trucks, pipeclay, sandstone, suction pipe, valves, honeycomb rock, mr kermode, yarrowee, ballarat, reef combs, cheques, earthquake, yellow slate, leigh river, dyke, the madame bay coy, allendale, berry west, quartz, ballarat deep leads, ballarat deep leads extension, bore, reads, bedrock, j. hayes, harmen premier distributors, middletons, cemented sand, electricity commission, g m of a, gold mines of australia, dick harry, pearsons, hawksburn, crown wheel, rice's paddock, liz the car, volcanic ridge, lrg coy, mcnaughton's paddock, madison's lead, cameron & sutherland, crabhole, rokewood, glenfine, mrs gibbs, dobson, booth, shiels, thomas mitchell, mcpherson's reward, haddon, trunk lead mine, elaine, pitfield plains, mr clarke, daylesford, kuchel, shelford, geoff squire, lode, quartz reef, bladder attack, kidneys, income tax, reginald murray, grenville, blasting, john b. dennison, martin t. taylor, durham and buninyong deep lead, sebastopol plateau, mr wilkie, the premier petrol distributing agency of ballarat, lawaluk, ryan's western leads, mr nichol, mr hodge, knox schlapp and co., dr griffiths, state accident insurance office, magdala mine stawell, mining

This medal, dated 1858, was awarded to local farmer Marcus Macartney by the Victorian Agricultural Society on the 21 April 1858, for the prize 'PotatoesThe medal is of local historical significance"for its association with the early promotion of agriculture in Victoria through public shows and competitions in the 1850's; and its link to the emergence of the Koroit-Tower Hill area,with its rich volcanic soil, as a properous farming district, especially for potato-growing." (Helen Doyle, Significance Assesment: Koroit & District Historical Society.)Circular medal with small knob on top.Äround circumference/""EXTRA PRIZE VICTORIAN AGRICULTUREAL SOCIETY. Engraving on medal "Potatoes/Awarded To/Mr Marcus Macartney /April 21st/1858 Reverseägricultural shows, potatoes, koroit, tower hill

Thomas S. Hart was a teacher at the Ballarat School of Mines, and a member of the Ballarat Field Naturalists ClubArticle with illustrations published by the Royal Society of Victoria by Thomas S. Hart. The following plates are included: Fig 1. The Main Divide and some of the transverse ridges Fig 2. Hills on and near the Divide at the Ercildoun and Ascot Gaps Fig. 3. Profile of the Divide at Ascot Gap. Fig. 4. Sketch of the Hills west and north-west from Mt Buninyong - - The divide in Ascot Gap from Mt Blowhard (Serra Range, Mt William, Mt Ararat, Larne Gerin, Ben Major, Mt Cole, Mt Misery, Mt Bolton) Fig. 5. Diagram to illustrate the possible courses of the leads south of the present Divide - Burrumbeet Basin (Smythesdale, Ballarat, Lal Lal , Mt Doran, egerton, Parwan Creet, Rowsley Fault, Eastern Plateau) Fig. 6. Diagramatic cross section of the grampians, south of Hall's Gap. Profile of the Pyranees, from maiden Hill - Diagramatic Section of the Grampians south of Hall's Gap. (Mt Cole, Mt Mitchell, Ben Major, Ben More, Avoca Hill, Hall's Gap.) Fig. 7. Profile of the Pyrenees as seen from Maiden Hill near Waubra.thomas hart, thomas s. hart, ballarat school of mines, ballarat field naturalists club, royal society of victoria, western victoria, ballarat, great dividing range, mt william, volcano, volcanic plains, waterways, lal lal basin, yarrowee creek, ballarat common, lava flow, wendouree, warrenheip, ballarat plateau, mt elephant, grampians, t.s. hart, mt buangor, mt beckworth, mt misery, mt bolton, lal lal iron ored, mt ararat, mt wiliam, mt cole, burrumbeet, mt warrenheip, daylesford, waubra, ercildoun gap, smythesdale, lal lal falls, parwan valley, burrumbeet creek, staffordshire reef, pyranees, bacchus marsh, rowsley fault, ben nevis, avoca hill, landsborough hill, mt blowhard, weatherboard, mclean's hill, fyan's creek, thomas stephen hart, lal lal

Contour map of the Queenstown area in Tasmania, Australia.department of mines tasmania, volcanics, mount read, queesntown, whip spur, mining, king river, gormanston, mt owen, lynchford

Canola in bloom near Newlynnewlyn, agriculture, horticulture, volcanic hills, mammalian hills

cape bridgewater, geology, ocean, coastal, landscape, seascape, blowhole, volcanic rock

Colour photograph of the coastline at Cape Bridgewater, Victoria. cape bridgewater, geology, ocean, coastal, landscape, seascape, blowhole, volcanic rock

cape bridgewater, geology, ocean, coastal, landscape, seascape, blowhole, volcanic rock