15cm x 10cm coloured photograph of the cutting at 91 Sydney Street, Melbourne Street at the top of the cutting which exposed the volcanic rock. Now is the site of the car wash and KFC.Written on the back: Exposed volcanic rock 91 Sydney St Kilmoreconstruction

15cm x 10cm coloured photograph of the cutting at 91 Sydney Street, Melbourne Street at the top of the cutting which exposed the volcanic rock. Now is the site of the car wash and KFC.written on the back of .1: cutting @ 91 Sydney St Kilmore Melbourne St 2 top of cutting late July 2016 Written on the back .2: Exposed volcanic rock look south west 91 Sydney St Kilmore late July 2016construction

This specimen was recovered from the Nigretta Falls (previously named the Upper Wannon Falls), Victoria. The falls are fed by the Wannon River that has its head waters in the Grampians mountains. Approx. 10km upstream of the Wannon Falls, Nigretta is a multi-channel segmented cascade of smaller drops and bounces guided by patterns of joints in a much older (Devonian) rhyolitic volcanic rock. Both the Wannon and Nigretta Falls are iconic landscape features, entrenched in the history and identity of the region. These falls are particularly rare as they are the product of volcanic activity, which is unique in the context of the Volcanic Plain of Victoria. Waterfalls of this capacity are generally associated with the Uplands areas of Victoria, rather than the edges of the Volcanic Plain. 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, dark grey mineral specimen with pale terracotta coloured inclusions. Rhyodacite is a volcanic rock intermediate in composition between dacite and rhyolite. Rhyodacites form from rapid cooling of lava relatively rich in silica and low in alkali metal oxides.GEOLOGICAL SURVEY / R / S 55 FELSTONE PORPHYburke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, porphyritic rhyodacite, lava, nigretta falls, upper wannon falls, dacite, rhyolite, volcanic geology

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

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

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

8304.1 - Curiously dark rhyolite or rhyolitic volcanic rock. Coarse-grained feldspar quartz crystals within five-grained dark groundmass.

Olivine is mostly found on the Earth's surface in igneous rocks that are dark-coloured. It is common at divergent plate boundaries and at warm spots, such as volcanic areas. It crystalises and forms during the cooling of magma. Olivine is used in refractory sand, bricks, and gemstones. Olivine has been found on a number of meteorites, which might have originated from large asteroids or the mantle of a now-destroyed planet. This olivine crystal is thought to originate from Mount Noorat, with speculation that it could have originated from Mount Shadwell. Mount Noorat is a dormant volcano cone located in the Newer Volcanics Province of Victoria. Mount Noorat belongs to the Kirrae Wuurong people, who used the Mount as a place for meetings and gatherings prior to European settlement. Contact was first made between European settlers and the Indigenous people in 1841. The Mount has mostly been used for cattle and sheep grazing. Mount Shadwell is a well-known source of olivine and is the highest of a gathering of volcanic cones. The New Volcanic Province is located in South East Australia and covers 15000 square kilometres. It contains 400 explosive vents and small shield volcanoes. The last eruption is thought to have occurred 5000 years ago at Mount Gambier and Mount Schank. This olivine crystal has been identified as a volcanic bomb, which is a molten rock which was pushed out and ejected into the air when a volcano reupts. A rock needs to be larger than 65 mm in diameter to be classified as a volcanic bomb. This olivine volcanic bomb and its locality is historically and socially significant. The olivine was found in the Newer Volcanic Province, an area which contains over 400 dormant volcanoes. This olivine is one part of a volcanic bomb, which would have ejected when magma erupted out of a volcano. 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 iron-magnesium silicate mineral with shades of green and brownburke museum, beechworth, geological, geological specimen, olivine, igneous rock, volcanic, gemstones, volcanic bomb, meteorites, asteroids, plantes, mount noorat, mount shadwell, indigenous, kirrae wuurong people, newer volcanics province, victoria, european settlement, eruption

Feldspathic arenites are sandstones that contain less than 90% quartz, and more feldspar than unstable lithic fragments, and minor accessory minerals.Feldspathic sandstones are commonly immature or sub-mature.These sandstones occur in association with cratonic or stable shelf settings. Feldspathic sandstones are derived from granitic-type, primary crystalline, rocks. If the sandstone is dominantly plagioclase, then it is igneous in origin Sandstone features prominently in public buildings throughout Victoria. Most of the sandstone used as dimension stone in the State came from three sources: the Heatherlie quarry in the Grampians (Silurian), the Bacchus Marsh area (Permian), and the Barrabool Hills near Geelong (Cretaceous).Sandstone features prominently in public buildings throughout Victoria, making this specimen special as it shows the materials used by Victorian building companies. Sandstone can also be crushed, crushed stone is used in the construction of roadways and road structures such as bridges, and in buildings, both commercial and residential. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study. A feldspar-rich sandstone, a sandstone intermediate in composition between an arkosic sandstone and a quartz sandstone, containing 10% to 25% feldspar and less than 20% matrix material of clay, sericite, and chlorite. Feldspathic arenite containing less than 90 percent of the composition of quartz. Feldspar is the main composition. Feldspathic arenite may contain fragments of unstable rock, and a little amount of other minerals such as mica and heavy minerals. Some feldspathic arenite have pink or red color because of the presence of potassium feldspar or iron oxide. There are also colored light gray to white. These sandstones are usually medium to coarse grained and can contain a high percentage of granules with angular until subangular roundness. The content of the matrix can appear as the rest up to more than 15 percent, and sorting of grains can present as moderate to poorly sorted. Feldspathic sandstones are generally immature in textural maturity. Feldspathic arenite can not be judged from the structure of the sediment. Bedding can emerge from the laminate parallel to the crossbed. Fossils may appear in the layer deposited on the sea. Feldspathic arenites usually appear on the craton or the continental shelf, which can be associated with conglomerate, quartz lithic arenite, carbonate rock, or evaporites. This sandstone may also appear on the succession of sedimentary basins deposited on an unstable or deep sea, and moving arc setting. According to Pettijohn (1963) Arkose make up about 15 percent of all sandstones. Some Arkose formed in situ when the granite and related rocks disintegrate and generate granular sediments. Most of the material feldspathic sandstones derived from primary crystalline granitic rocks, such as granite or metasomatic rocks containing abundant potassium feldspar. Mineral contained in sandstones is mostly a form of plagioclase feldspar derived from quartz diorite or volcanic rock. Feldspar contained on this sandstone comes from arid to cool climates when the chemical weathering process is reduced.sandstone, natural stone, feldspathic sandstone, burke museum, geology, geological, geological specimen

This particular geological specimen was found in Mount Franklin or Lalgambook in Djadjawurrung, located between Daylesford and Newstead, approximately ninety minutes drive from Melbourne. The mountain is an example of a breached scoria cone (a steep conical hill of loose pyroclastic fragments) which was created by a volcanic eruption about 470,000 years ago, a date which may indicate the age of this geological specimen. The volcanic eruptions of Mount Franklin were most likely witnessed by members of the Dja Dja Wurrung Aboriginal tribe, who referred to this country as the 'smoking grounds'. Mount Franklin and the surrounding area appears to have been a place of considerable religious significance to Aboriginal people, there is evidence which indicates that frequent large ceremonial gatherings took place in the area. Basalt is the most common rock on Earth’s surface, more than 90% of all volcanic rock on Earth is basalt. Basalt is an aphanitic extrusive igneous rock formed from the rapid cooling of low-viscosity lava exposed at or very near the surface of a rocky planet or moon. Specimens are black in colour and weather to dark green or brown. Basalt is rich in iron and magnesium and is mainly composed of olivine, pyroxene, and plagioclase. Olivine is the name of a group of rock-forming silicate minerals with compositions ranging between Mg2SiO4 and Fe2SiO4. Unlike other minerals, Olivine has a very high crystallisation temperature which makes it the first of the minerals to crystallise from magma. As magma cools, the crystals begin to form and settle on the bottom of the lava and form basalts that are abnormally enriched in olivine in the lower part of lava flows. According to H. M. King (on geology.com) "Olivine is thought to be an important mineral in Earth's mantle. Its presence as a mantle mineral has been inferred by a change in the behaviour of seismic waves as they cross the boundary between Earth's crust and mantle". Lava from Mount Franklin and other volcanoes in the area filled valleys and buried the gold bearing streams that became the renowned ‘deep leads’ of the gold mining era. In 1852, as part of the Victorian gold rush, gold was discovered in the immediate area, this gold was created by lava flows during the Newer Volcanic period, which were mined intensively during the nineteenth century. Around 1865 the presence of a deep lead in Mount Franklin was established. Deep lead mining was initially unsuccessful, and it was not until the late 1870s that the Franklinford Gold Mining Company mined at Mount Franklin on a significant scale. A few years later the Mount Franklin Estate Gold Mining Company also struck gold, followed by the Shakespeare and Great Western companies in the mid-1880s. By the late 1880s, however, deep lead mining had ceased in the area. Soon after gold was discovered in 1851, Victoria’s Governor La Trobe wrote to the Colonial Office in London, urging ‘the propriety of selecting and appointing as Mineral Surveyor for this Colony a gentleman possessed of the requisite qualifications and acquaintance with geological science and phenomena’. Alfred Selwyn was appointed geological surveyor in Australia in 1852 which began the Geological Survey of Victoria. In 1853-69 the Geological Survey issued under Selwyn's direction sixty-one geological maps and numerous reports; they were of such high standard that a writer in the Quarterly Journal of the Geological Society of London bracketed the survey with that of the United States of America as the best in the world. During his years spent in Australia, Selwyn collected numerous significant geological specimens, examples of which are held in collections such as the Burke Museum.This geological specimen is an example of basalt and olivine which shows the volcanic lava activity and geographical specific nature of Mt Franklin as a significant volcanic site. According to Agriculture Victoria 'The crater is one of the deepest in the Central Highlands area. It is a major megacryst site with some of the largest known Victorian examples of megacrysts of augite and an orthoclase. The small parasitic mound of Lady Franklin on the western flanks adds to the geological interest of the site'. This specimen also highlights the locality as a significant place for both indigenous activity and Victorian gold rush era mining practices. 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.An angular, solid hand-sized piece of grey volcanic Basalt with green/brown Olivine phenocrysts along one flat edge.Olivine in basalt / - label is probably / correct. / C. Willman / 15/4/21burke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, mineralogy, basalt, igneous rock, igneous-volcanic, volcanic geology, volcanic, olivine, olivine specimen, basaltoid

Ken Arnold is a Bendigo author and publisher.A series of one hundred and thirty-five articles written by Ken Arnold and published in the Bendigo Weekly between 2000 and 2003. Each article has a topic or theme and includes historical information and details. Each article includes a photograph. The articles are stored in a red vinyl covered two ring A5 folder. Index below. Number Article Name Date 1. Centenary of Victoria 19.5.00 2. Storm Water Drain 26.5.00 3. Granite Rollers 2.6.00 4. Poverty Mine 9.6.00 5. Golden Monument. St Arnaud 16.6.00 6. Turner Statue 7.7.00 7. Gold Monument. High St Golden Square 30.6.00 8. Gold Monument. Howard Square Bendigo 14.7.00 9. Lansell Statue 21.7.00 10. Shelbourne West School 18.8.00 11. Mologa’s State Schools 25.8.00 12. Salinity Stone. Pyramid Hill 1.9.00 13. Cairn. Carisbrook 8.9.00 14. Commemorative Markers. Taradale 15.9.00 15. Burke Monument. Castlemaine 22.9.00 16. Cairn. Harcourt area 29.9.00 17. Cairn Marks Gold Route 6.10.00 18. Volcanic Rock Cairn. Woodstock 13.10.00 19. Garfield Water Wheel 20.10.00 20. Anticline. Castlemaine 27.10.00 21. Lawson Bridge 10.11.00 22. Plaque. Sutton Grange area 17.11.00 23. Memorial Cairn. Maryborough 1.12.00 24. Lonely Grave 8.12.00 25. Moonlight Flat Church 5.1.01 26. Historic Church. Near Tullaroop reservoir 12.1.01 27. Granite Statue. Castlemaine 19.1.01 28. Marker. Near Tullaroop reservoir 25.1.01 29. Church Site. Mologa 2.2.01 30. Church Site. Mologa 9.2.01 31. Plaque. Mologa 16.2.01 32. Mincha School 23.2.01 33. Historic Marker. Mincha 2.3.01 34. Expedition Marker. Pyramid Hill 9.3.01 35. Irrigation Marker. Tragowel 16.3.01 36. Mologa School Sites 23.3.01 37. Cairn. Pyramid Hill 30.3.01 38. Plaque. Pyramid Hill 6.4.01 39. Bristol Hill Lookout Tower. Maryborough 12.4.01 40. Eppalock Reservoir 20.4.01 41. Colbinabbin Cairn 27.4.01 42. Mount Macedon Cross 4.5.01 43. Memorial Gateway. Macedon 11.5.01 44. Cairn. Daylesford 18.5.01 45. Grave. Carlsruhe 25.5.01 46. Water Tower. Elmore 1.6.01 47. State School Site. Glenalbyn 8.6.01 48. Cairn. Kanya 15.6.01 49. Lonely Grave. Wedderburn 22.6.01 50. Church Cairn. Glenalbyn 29.6.01 51. Kamarooka School 6.7.01 52. Granite Marker. Moyston 13.7.01 53. Memorial Park. Kerang 20.7.01 54. Water Plaque. Bears Lagoon 27.7.01 55. Cemetery. Bears Lagoon 3.8.01 56. Race Monument 10.8.01 57. Cairn. Pyalong 17.8.01 58. Cairn. In memory of Edward Parker 24.8.01 59. Mt Macedon 31.8.01 60. Mt Macedon Cairn 7.9.01 61. Expedition Pass. Chewton 14.9.01 62. Granite Archway. St Arnaud 21.9.01 63. Stuart Mill School Site 28.9.01 64. School Site. Beazley’s Bridge 5.10.01 65. Fosterville 12.10.01 66. Barnadown 19.10.01 67. Salisbury School Site 26.10.01 68. Cricket History at Wattle Flat 2.11.01 69. School Site. Waterloo Plains 9.11.01 70. Carapooee School Site 11.01 71. Turkish Gun. Maldon 11.01 72. Kooreh 30.11.01 73. Marnoo East School 7.12.01 74. Bulgana Site 14.12.01 75. Emu School 21.12.01 76. Kooroocheang 4.1.02 77. Church Site. Gre Gre North 11.1.02 78. Carmens Tunnel. Maldon 18.1.02 79. Monument. Maldon 25.1.02 80. Woodfull Plaques. Maldon 1.2.02 81. Carapooee. St Peters Anglican Church 8.2.02 82. Cairn. Kingower 15.2.02 83. Cob & Co Stopover. Rheola 22.2.02 84. Flynn Monument 1.3.02 85. The Welcome Stranger. Moliagul 8.3.02 86. Campbell’s Creek Reserve 15.3.02 87. Mine. Fryerstown 22.3.02 88. Escott Grave. Near Chewton 28.3.02 89. School No 808. Kurting area 5.4.02 90. Graves. Bendigo Creek 10.5.02 91. School. Fish Point, Benjeroop North 17.5.02 92. Old Township. Diggora 24.5.02 93. Diggora West (1) 31.5.02 94. Diggora West (2) 7.6.02 95. School No 2735. Gower East 14.6.02 96. Pannoomilloo 21.6.02 97. Kamarooka Settlement 28.6.02 98. Mincha West State School No 1931 5.7.02 99. Bridges. Arnold 12.7.02 100. Woodvale 19.7.02 101. A Famous Son of Raywood. Jack Donaldson 26.7.02 102. Tandarra Area Schools 2.8.02 103. Dingee 9.8.02 104. Avonmore 30.8.02 105. Myola East School 6.9.02 106. Colbinabbin West 13.9.02 107. Colbinabbin West School 20.9.02 108. Runnymede area 27.9.02 109. Wanalta 4.10.02 110. School Sites. Between Wanalta and Carop 11.10.02 111. Burramboot 18.10.02 112. Kangaroo Chair. 25.10.02 113. Mincha South 1.11.02 114. Woodlands Church 8.11.02 115. School site. Sylvaterre 15.11.02 116. Terrick Terrick 22.11.02 117. Leitchville 29.11.02 118. Pennyweight Cemetery. Castlemaine 6.12.02 119. Mincha Area 13.12.02 120. Musk School 20.12.02 121. Dowie Park. Carisbrook 3.1.03 122. Neereman School Site 10.1.03 123. Bald Rock 17.1.03 124. Sylvaterre School Site 24.1.02 125. Carlsruhe 31.1.02 126. Athenaeum. Maldon 7.2.03 127. School. Mincha West 14.2.03 128. Yarraberb 21.2.03 129. Settlement Marker. Ravenswood Estate 28.2.03 130. Comini Reserve. Ravenswood 7.3.03 131. Ironbark and Gold Track. Whroo 14.3.03 132. Burke and Wills Obelisk. Castlemaine 21.3.03 133. James Cook Statue. Myers St Bendigo 28.3.03 134. St Marys Church. Axedale 4 .4.03 135. Butter Factory Site. Warragamba 11.4.03 events, monuments, historical sites, landmarks

According to the 1912 Department of Mines Bulletin of the Geological Survey of Victoria, basalt covers a considerable portion of the Macedon area including Mount Macedon. Basalt is the most common form of rock underlying the earth's surface and is found in three kinds of rock forming environments: ocean divergent boundaries, oceanic hotspots, and mantle plumes and hotspots beneath continents.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 mass, geological specimen in shades of grey and white. Hyalite is a colourless variety of opal. It occurs as globular and botryoidal masses and irregular crusts in volcanic and pegmatite environments where the silica deposits from the gas phase. Basalt is dark in colour, fine-grained igneous rock composed of plagioclase and pyroxene minerals. It is commonly formed as an extrusive rock, such as lava flow. It is one of the most common forms of rock underlying the earth's surface.burke museum, geological specimen, department of mines, geological survey of victoria, basalt, mount macedon, beechworth

This specimen was found in Harcourt, Victoria. Harcourt is a small historic gold rush town located in a valley at the foot of Mount Alexander (741 m) in the Central Highlands of Victoria. In recent times the goldrush origins of the town have been replaced by a district known for apples, cider and wine. The Traditional owners of Harcourt are The Dja Dja Wurrung people. Granodiorite is a coarse-grained intrusive igneous rock similar to granite, but containing more plagioclase feldspar than orthoclase feldspar. Granodiorite has greater than 20% quartz by volume, and between 65% and 90% of the feldspar is plagioclase. This piece is of significance due to its provenance in Harcourt, Vic. Granodiorite is commonly produced in volcanic arcs, and in mountain buildings where it emplaces as large batholiths in mountain roots. Granodiorite is the plutonic equivalent of dacite. 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.Granodiorite is a coarse-grained intrusive igneous rock similar to granite, but containing more plagioclase feldspar than orthoclase feldspar. According to the QAPF diagram, granodiorite has a greater than 20% quartz by volume, and between 65% and 90% of the feldspar is plagioclase.GRANDIORITE. / Locality: / Harcourt, Victoria / Other label: Geological survey / R S / Loc Harcourt quarries [?] Alexander / 1/4 Sheet. | 4 | Granite /granodiorite, granite, burke museum, harcourt, coarse-grained, igneous, plagioclase feldspar, orthoclase feldspar, quartz, mount alexander, the dja dja wurrung people, the traditional owners, central highlands of victoria, gold rush

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

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

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 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.

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.

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 N23 Jan 1980 A43 Compressor unit in backyard of 39 Burlock Avenue

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 N22Jan 1980 A43 Work on mole boring 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.E560 N10 Dec 1979 A43 Filling at 29 Burlock Avenue

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 N9 Dec 1979 A43 Filling behind 29 Burlock Avenue just off sewer line

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 N11 Dec 1979 A43 Filling at 29 Burlock Avenue

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 N31 Jan 1980 A43 Closeup of revolving airwinch near Hibberd's house

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 N25 Jan 1980 A43 Grating over hole 37 feet deep in Chalkley's 41 Burlock Avenue (lot 8)

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 N27 Jan 1980 A43 View along line work in Hibberd's and Chalkley's (lot 9 and 8)

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 N32 Feb 1980 A43 Truck-mounted posthole digger that tried to sink shafts on MMBW sewer line behind 29-39 Burlock Avenue. Four feet wide, the auger could only go down one metre and was nearly useless.

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 N26 Jan 1980 A43 View behind no. 39 Burlock Avenue showing compressor, mole pit cover and the big box tree