This specimen was donated in 1868 by Alfred Selwyn. Olivine is typically found in basic and ultra-basic igneous rocks around the world, in a variety of colours including yellowish green, olive green, greenish black and reddish brown with a transparent to translucent diaphaneity. The luster of the specimen is vitreous, the luminescence non-fluorescent and when fractured the mineral is very brittle producing small, conchoidal fragments. Chromian diopside is normally found in small sizes as the larger the size of the mineral the darker the colour is, almost black rather than green. Chromium is the element that gives chromian diopside and emeralds their rich green colour. Diopside is found across the world in multiple colours however gem-quality chromian diopside is mined in Siberia, Russia and prominent within the jewellery industry as a more affordable substitute to emeralds. Chromium-bearing diopside has been located across Australia. Chromium-bearing Diopside is located across the world found in North America, parts of South America, and across Australia, Africa, Europe and Asia. Chromium-bearing Diopside is mined in Siberia, Russia and is sold as a commercial substitute for emeralds. The stone is often turned into jewellery. This item is one of many geological and mineral specimens that constitute a broader collection obtained from various regions across Australia (as well as some international locales) and generously contributed to the Burke Museum between 1868 and 1880. A significant portion of these specimens originated from Victoria and were acquired as a result of the Geological Survey of Victoria, initiated in 1852 during the Gold Rush era. The primary objective of this survey was to investigate and chart the geological characteristics of Victoria. The procurement of geological specimens played a vital role in advancing our comprehension of the Earth's scientific composition and was instrumental in supporting research and educational institutions throughout Australia, including the Burke Museum, in their efforts to foster further exploration and study. A solid mineral specimen in shades of green, grey and brownburke museum, beechworth, geological, geological specimen

Back Row: Norris Stratton, Vic McGrath, Bob Hayward, Geoff Morrissey(?), Duncan McGregor, Trevor Shepherd, Wally Kerr, Max Howard(?), Dean Hart, Steve McGrath, David Bishop, Allan McCorkell. 3rd Row: Ron McCorkell, George Haddon, Gordon Mark, Bob Brody, Lyle Grigg, Geoff Morrissey (?), Roland Emmerson, Jack Culliver, Jim Culliver, Basil McDonald, Graham Smith. 2nd Row: Laurie Lancaster, Laurie Stevens, Noel Cluff, Lyle Fletcher, Mervyn McDonald, Carl Hoffman, Des Harris, Les Witton, Ian Morrissey, Graham Ching, Raymond Mark, Jim(?) Haddon. Front Row: Graeme McGregor, Colin Hearn, Vernon Broes, Graham Stevens, Stan Lancaster, Lindsay Witton, Stan Howard(?), Colin Nicol, Selwyn Hoffman, Les Mark.Black and white copy of a photograph of Linton State School boys taken in 1940."Linton School 880 1940"linton state school no. 880, vic mcgrath, bob hayward, geoff morrissey(?), duncan mcgregor, trevor shepherd, wally kerr, max howard(?), dean hart, steve mcgrath, david bishop, allan mccorkell, ron mccorkell, george haddon, gordon mark, bob brody, lyle grigg, roland emmerson, jack culliver, jim culliver, basil mcdonald, graham smith, laurie lancaster, laurie stevens, noel cluff, lyle fletcher, mervyn mcdonald, carl hoffman, des harris, les witton, ian morrissey, graham ching, raymond mark, jim(?) haddon, graeme mcgregor, colin hearn, vernon broes, graham stevens, stan lancaster, stan howard(?), colin nicol, selwyn hoffman, les mark., norris stratton, lindsay witton

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

Dolomite is a mineral, calcium magnesium carbonate, with the chemical formula CaMg(CO3)2. It is a principle component of various rock types sometimes also referred to as dolomite, including dolostone, dolomitic marble and dolomitic limestone (according to the composition of each type). Dolomite rock is found in sedimentary basins throughout the world, comprising approximately 2% of the Earth's crust. It is formed when lime mud or limestone encounters groundwater containing magnesium. Dolomite can contain elements such as lead, zinc and copper. Dolomite and limestone are used in various construction, landscaping and agricultural processes. This specimen was donated to the Burke Museum in 1868 by Alfred Selwyn as part of the Geological Survey of Victoria. It was donated to the Museum in 1868. Victoria and other regions of Australia were surveyed for sites of potential mineral wealth throughout the 19th Century. The identification of sites containing valuable commodities such as gold, iron ore and gemstones in a locality had the potential to shape the development and history of communities and industries in the area. The discovery of gold in Victoria, for instance, had a significant influence on the development of the area now known as 'the goldfields', including Beechworth; the city of Melbourne and Victoria as a whole. Dolomite and limestone are mined at several locations in Victoria, including sites in the North-East of the state in Bindi and Limestone Creek. There are notable dolomite deposits in most Australian states. The dolomitised form of the mineral tends to come from older limestone deposits, formed during the palaeozoic era in marine settings, so this specimen may have come from a deposit located along a coastline in Victoria or another state. The specimen is significant as an example of surveying activity undertaken to assess and direct the development of the mineral resource industries in Victoria and Australia, as well as the movement to expand human knowledge of earth sciences such as mineralogy and geology in the nineteenth century. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.Hand-sized piece of pale pink dolomite (calcium magnesium carbonate) with dark grey rim and hollowed centre. geological specimen, geology, geology collection, burke museum, beechworth, dolomite, mineralogy, geological survey, alfred selwyn, limestone, calcium magnesium carbonate

This photograph is part of the Caulfield Historical Album 1972. This album was created in approximately 1972 as part of a project by the Caulfield Historical Society to assist in identifying buildings worthy of preservation. The album is related to a Survey the Caulfield Historical Society developed in collaboration with the National Trust of Australia (Victoria) and Caulfield City Council to identify historic buildings within the City of Caulfield that warranted the protection of a National Trust Classification. Principal photographer thought to be Trevor Hart, member of Caulfield Historical Society. Most photographs were taken between 1966-1972 with a small number of photographs being older and from unknown sources. All photographs are black and white except where stated, with 386 photographs over 198 pages. From: Glen Eira Heritage Management Plan (1996) by Andrew Ward and Associates Moore's Buildings", were built in 1891 and comprising 5 shops. In 1888, Hugh Moore, a gentleman, subdivided his land in Glen Huntly Road, north side between Selwyn Street and St Georges Road into 27 lots, with a right of way separating them from his property "Glenmoore". The subdivision was known as the "Glenmoore Estate". Purchases of land included local builders Corkill, French and Pugh. Moore retained five lots and W.W. Jamieson bought lots 11 to 14. "Moore' s Buildings are locally important for their association with the early Elsternwick land owner, Hugh Moore, whose home, "Glenmoore", at 1 St.Georges Road (qv) survives. They recall Elsternwick's role in the Land Boom and survive as a most prominent row in the Glen Huntly Road shops, enhanced by the survival of the unpainted stuccoed surfaces to nos. 307-311. 287-289 Glen Huntly Road: contributory to HO72, Elsternwick Estate and Environs, City of Glen Eira.Page 63 of Photograph Album with one landscape photograph of retail shops (Moore's Buildings).Hand written: 287-289 Glen Huntly Road [under photo] / 63 [bottom left] trevor hart, shop, grocer, stuccoed, terrace, victorian terrace, protruding parapet, ornate render, hugh moore, 1890's, moore's buildings, glenmoore, glenmoore estate, shopping centres, milk bars, cars, victorian style, glen huntly road, glenhuntly road, elsternwick

James Watkin (1805–86), Pioneer Missionary. James Watkin was born in Manchester in 1805. While still young he felt the call to preach and in 1830 was accepted as a candidate for the Wesleyan Ministry. In the same year he married Hannah Entwistle and they sailed with a missionary party to Tonga. The work of the mission was jeopardised by prolonged and involved struggles between Christian and non-Christian Tongan chiefs; Watkin faced alone the danger of tribal warfare, but the experience left him depressed and exhausted. On his removal with his family to Sydney in September 1837 he prayed for a return home to England. Instead, when John Jones offered a free passage for a missionary appointed to Waikouaiti, where Jones had a whaling station, Watkin was selected for the post and arrived there in May 1840. Here he established the first mission station in the South Island. Watkin found the whaling settlement of Waikouaiti a centre of violence, licentiousness, and drunken depravity. Thoroughly disliking the corrupted Maoris and convinced that they were doomed to extinction, and disgusted by the brutality and vices of his fellow Europeans, Watkin laboured without hope, in the bitterness of exile and with deepening depression and distress. In spite of an abhorrence for his situation he established schools at Waikouaiti and Matanaka, and stationed partly trained Maori teachers at Stewart Island and at Moeraki. He had a natural flair for languages, preached in Maori four months after his arrival, and compiled an elementary reading book to be printed in Ngai Tahu. In November 1840 Watkin was greatly disturbed by Bishop Pompallier's visit to Otago. When, however, this was followed by Anglican intrusion – for Bishop Selwyn visited Otago in January 1844 – Watkin thought of withdrawing his own Maori teachers and abandoning the field. Never reconciled to his position at Waikouaiti, Watkin was relieved by Charles Creed and in June 1844 he sailed for Wellington, leaving 227 church members in Otago. In 1855 Watkin settled in New South Wales, and was president of the National Methodist Conference at Adelaide in 1862. He retired in 1869 and died on 14 May 1886, at Ashfield, New South Wales. 'WATKIN, James', from An Encyclopaedia of New Zealand, edited by A. H. McLintock, originally published in 1966. Te Ara - the Encyclopedia of New Zealand URL: http://www.TeAra.govt.nz/en/1966/watkin-james (accessed 30 Apr 2018) B & W engraving from a photograph of the Rev. James Watkin.Revd. James Watkin, Australia Engraved by J. Cochran from a Photograph.

Entry No. 621 on page 856. Entry is a list of the Catherine Reef United Claimholders Gold Mining Company Shareholders with their address and the number of shares they hold. Manager was Thomas Eyre and the Company Office was at Peg Leg Gully, Eaglehawk. Names of Shareholders are: John Abern, Simon Albert, James Allen, William Allen, Alexander Anderson, William Anderson,Harry Leigh Atkinson, William Bannerman, Adolphus Barnett, Adolphus Robert Barnett, Alexander Bayne, Adam Beattie, Robert Bell, Gottfried Bermann, William Boncher, James Branagan, Carl Brecht, Frederick William Brinkmeyer, William Ruthford Brown, Joseph Burgoine, Thomas Burgoine, Thomas Burrows, Joseph Butler, John Thomas Caldwell, Philip Carr, Mary Jane Chantler, James Cobb, Edward Cook, Edward F Cooper, James Crameri, George Cudden, Jacob Ludwig Culmsec, Gustav Damkohler, Ellen Dithmer, William Dixon, William Doig, Robert Campbell Dow, Adam George Dunlop, Andrew McBride Dunlop, Hugh Ellis, Thomas Eyre, Richard Philip Eyre, William Farnsworth, Matthew Fawcett, Frederick John Fleming, John Forrest, Andrew Frei, Robert Gilmour, James Gray, Fordinand Gremelsbecher, Robert Grieve, John Grieve, William Grose, George Hagger, Andrew Hamilton,Hans Truchen Hansen, Thomas Harding, Abraham Harkness, Alexander Hay, Joseph A C Helm, John Hoole, George Hoole, Edward Hunt, Thomas Huston, Henry Jackson, Samuel Jackson, Eli James, Robert Jeffrey, Carl Heinrich Jensen, George Foster Johnson, Richard Kevern, William Kimber, Martin Kircher, Hay Kirkwood, Henry Koch, John Lamperd, Mary Anne Lawley, Charles Letheby, Joseph Lowery, Ninjan Mailor, William Marshall, Robert Marshall, Henry Adolphus Medlicott, John Mitchell, William Moore, Susan Murray, Andrew McGrigor, John Steele McNair, Thomas McCormack, Peter Nielson, William Parry Nicholls, Henry Boyns Nicholas, George Nicholson, John Noble, Daniel Noonan, John O'Keeffe, David Purves, William Rea, William Usher Reavely, Francis Robinson Reay, John Bellew Richards, Samuel Richardson, William Robinson, Henry John Rowe, Thomas Ruberg, John Rule, Thomas Rule, Joseph Rutherford, Edward B Ryal, John Snaith Rymer, Philip Seeber, Ferdinand Sahlberg, John Thomas Sanders, Edward Saunders, Charles Selwyn Savage, Charles Sayer, John Scanlon, William Schafer, James Sherson, William Simpson, Antony Smith, Samuel Snowdon, Peter Sorensen, Anders Neilsen Sorensen, Frederick Stahl, David Chaplin Sterry, James Steward, Louis Straub, Robert Suggett, George Suggett, John Talbot, Marion Taylor, John Thomas, Joseph Thomson, Thomas Treloar, William Trimble, George Turner, Alfred Wainwright, Charles Wallin, John Watson, Joseph Watson, Richard John Webb, Frederick Whitaker, John William Williams, Henry Williams, Robert Wills, Christian Weiss, John Wilson, William Winter, George Wisemann, Joseph Wood, James William Wood, Edward Wrixon, Thomas Young and Henry Young. Witness to Signature was J D Crofts.mining, business, shareholders, catherine reef united claimholders gold mining company shareholders, thomas eyre, mining partnerships limited liability act 1860, john abern, simon albert, james allen, william allen, alexander anderson, william anderson, harry leigh atkinson, william bannerman, adolphus barnett, adolphus robert barnett, alexander bayne, adam beattie, robert bell, gottfried bermann, william boncher, james branagan, carl brecht, frederick william brinkmeyer, william ruthford brown, joseph burgoine, thomas burgoine, thomas burrows, joseph butler, john thomas caldwell, philip carr, mary jane chantler, james cobb, edward cook, edward f cooper, james crameri, george cudden, jacob ludwig culmsec, gustav damkohler, ellen dithmer, william dixon, william doig, robert campbell dow, adam george dunlop, andrew mcbride dunlop, hugh ellis, thomas eyre, richard philip eyre, william farnsworth, matthew fawcett, frederick john fleming, john forrest, andrew frei, robert gilmour, james gray, fordinand gremelsbecher, robert grieve, john grieve, william grose, george hagger, andrew hamilton, hans truchen hansen, thomas harding, abraham harkness, alexander hay, joseph a c helm, john hoole, george hoole, edward hunt, thomas huston, henry jackson, samuel jackson, eli james, robert jeffrey, carl heinrich jensen, george foster johnson, richard kevern, william kimber, martin kircher, hay kirkwood, henry koch, john lamperd, mary anne lawley, charles letheby, joseph lowery, ninjan mailor, william marshall, robert marshall, henry adolphus medlicott, john mitchell, william moore, susan murray, andrew mcgrigor, john steele mcnair, thomas mccormack, peter nielson, william parry nicholls, henry boyns nicholas, george nicholson, john noble, daniel noonan, john o'keeffe, david purves, william rea, william usher reavely, francis robinson reay, john bellew richards, samuel richardson, william robinson, henry john rowe, thomas ruberg, john rule, thomas rule, joseph rutherford, edward b ryal, john snaith rymer, philip seeber, ferdinand sahlberg, john thomas sanders, edward saunders, charles selwyn savage, charles sayer, john scanlon, william schafer, james sherson, william simpson, antony smith, samuel snowdon, peter sorensen, anders neilsen sorensen, frederick stahl, david chaplin sterry, james steward, louis straub, robert suggett, george suggett, john talbot, marion taylor, john thomas, joseph thomson, thomas treloar, william trimble, george turner, alfred wainwright, charles wallin, john watson, joseph watson, richard john webb, frederick whitaker, john william williams, henry williams, robert wills, christian weiss, john wilson, william winter, george wisemann, joseph wood, james william wood, edward wrixon, thomas young, henry young, j d crofts

Built c.1868, St Andrew’s Anglican Church is Nillumbik Shire’s oldest timber church and is historically, socially, and spiritually significant to the Shire of Nillumbik. The church is historically significant because it may have given its name 'St Andrews' to the town (another suggestion is that the name came from the local hotel), it is also historically significant as one of only four buildings that remain from the Caledonian goldfields era of Queenstown (now St Andrews) and one of only a handful of buildings that survived the 1960s bushfires. The church is historically, socially, and spiritually significant because it has played an important part in community life for more than 150 years; a proposal to move the church in 1984 met with strenuous opposition. Much of the fires on Black Saturday 2009 were the north of the town. The town itself remained intact - as did this heritage building. Covered under Heritage Overlay, Nillumbik Planning Scheme. National Trust of Australia (Victoria) Local significance Published: Nillumbik Now and Then /​ Marguerite Marshall 2008; photographs Alan King with Marguerite Marshall.; p69 The St Andrews Anglican Church and former St Andrews Primary School, are two reminders of the district’s early days, when it was founded on gold. St Andrews, then called Queenstown, was the earliest goldfield in the Caledonia Diggings.1 It was the Upper Diamond Gold Mining and Administrative Centre, with 3000 miners. Queenstown was also the seat of the Court of Petty Sessions. The church and school then stood close to European and Chinese stores, three hotels, a brewery and a quartz mill.2 In 1861, Queenstown was officially proclaimed a township. From 1865, the name Queenstown was interchangeable with St Andrews, until 1952, when the town was officially named St Andrews. As gold declined from the early 1880s, Queenstown changed dramatically into a settlement of small farms. St Andrew’s Anglican Church, built in 1868, is the Shire’s oldest timber church and possibly gave its name to the township.3 The small timber church was opened on November 1, 1869, by the Dean of Melbourne. Anniversary tea meetings helped raise funds, and in 1889, a three-bedroom parsonage was built alongside. In 1910, the vicar, the Rev Selwyn Chase (and friend of the Scouting Movement’s founder, Baden Powell), established the 1st Queenstown Scout Troop, only two years after Scouting began in Australia. The church was important to the lives of many local residents who were baptised, married and had funeral services there. But by the 1950s the population had decreased and so did the weekly attendances. Around the mid-1960s the church closed, then fell into disrepair. So in the mid 1980s it was sold to the Education Department and was under threat of relocation or demolition. However this caused such opposition from locals,4 that instead, the Anglican church leased it as part of the Panton Hill parish5 and it was reconsecrated in 1987. Queenstown’s first school was held in a tent after transferring from Andersons Creek, Warrandyte.6 From 1858 a church school, Caledonia Diggings, stood west of the main road, a quarter of a mile (0.4km) before Buttermans Track. In 1882 the school was moved from a leased building, owned by headmaster Robert Harris, into a larger building on the corner of the School and the Heidelberg-Kinglake Roads. It had been moved from Smiths Gully and included a teacher’s three-roomed residence.7 In 1887 the school was replaced by the Queenstown State School No 128, although it was also called Caledonia Diggings until 1891. In 1956 it was renamed St Andrews. Still standing, this building is now used as the St Andrews Community Centre and the residence is leased for private use. The original timber-lined room remains alongside the extensions, and is distinctive with its high ceiling and tall small-paned windows. In 1984 a new school was built 500 metres west of the old school. Many residents have contributed much to St Andrews but one family that has done so for several generations is the Harris family. Robert Harris was an active member of the St Andrew’s Anglican Church, and worked hard at improving the town’s amenities until his death in 1887. He was a signatory to the successful 1863 petition to the Chief Commissioner of Police, against the proposed removal of the Court of Petty Sessions and police station at the Caledonia Diggings. The police station stayed in the town until 1917. Harris was Head Teacher of Queenstown State School from 1864 to 1874, then of the Smiths Gully school until it closed in 1882, and he continued teaching at Panton Hill until his death. His son, Robert Charles Harris, was editor and printer of the local newspaper, The Evelyn Observer, from 1873 until 1915. Robert’s son, William Shelley Harris, served in the Boer War and in World War One. In 1928 he became Kinglake National Park’s first park ranger. Robert’s daughter Elizabeth, taught needlework at Queenstown State School, and later ran the post office in Kinglake.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, st andrews, st andrews anglican church

This specimen originated from Mount Lyell on the west coast of Tasmania, where a large group of open cut and underground copper-silver-gold mines began operating in 1883. Between 1893-1994, the Mt Lyell Mining and Railway Company were responsible for operations. The Mt Lyell copper-gold mines produce some excellent crystallised specimens of chalcopyrite and other minerals. The deposits are generally considered to be of Cambrian volcanic origin, but there are indications of Devonian granitic influence on the ores, plus local remobilisation during Devonian deformation. Over 120 million tonnes of ore was produced from several workings, including the main Prince Lyell mine and the North Lyell mine, which was also of great importance. The Mount Lyell mines have a long history of human and environmental disasters, including the 1912 North Lyell fire that killed 42 miners, and two separate incidents in 2013 in which three people lost their lives. The environmental impacts from this complex of mines are extensive, with waste tailings and heavy metal contamination flowing directly into the King and Queen River catchments. In 1954, the eminent Australian historian, Geoffrey Blainey, published 'The Peaks of Lyell' which delves into the history of the 1912 North Mount Lyell Disaster.Chalcopyrite does not contain the most copper in its structure relative to other minerals, but it is the most important copper ore since it can be found in many localities and occurs in a variety of ore types. The brassy-yellow colours in Chalcopyrite mean it is often confused with pyrites and gold, leading to use of the term, "fool's gold." Chalcopyrite has been the primary ore of copper since smelting began five thousand years ago. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.This hand sized solid mineral specimen has shades of brass-yellow with spots of iridescent green-black tarnish. Chalcopyrite is a copper iron sulphide mineral and a major ore of copper common in sulphide veins and disseminated in igneous rocks. Chalcopyrite has a hardness of 3.5-4 on the Mohs Scale. It is a member of the tetragonal crystal system and has metallic lustre and opaque transparency.burke museum, beechworth, indigo shire, beechworth museum, geology, geological specimen, chalcopyrite, copper pyrites, copper mining, tasmanian geology, mount lyell, mount lyell mines, fools gold, mohs scale, crystals, minerals, historical geological collection, victorian geological survey, a.r.c selwyn, gold rush, van diemans land

Actinolite is usually found in metamorphic rocks, such as contact aureoles surrounding cooled intrusive igneous rocks. It also occurs as a product of the metamorphism of magnesium-rich limestones. Pyrite is usually found with other sulfides or oxides in quartz veins, sedimentary rock, and metamorphic rock, as well coal beds, and as a replacement mineral in fossils. Actinolite is an amphibole silicate mineral. It is named after the Greek word "aktinos" meaning “ray” in allusion to the mineral's fibrous nature. Fibrous actinolite is a type of asbestos and was once mined along Jones Creek at Gundagai, New South Wales. Pyrite or "Fool's Gold" is the most common sulfide mineral. It is named after the Greek "pyr" meaning "fire" because it can be used to create sparks needed for a fire if struck against metal or a hard surface. Due to its gold colour, pyrite can be mistaken for gold and often forms alongside it, causing small amounts of gold to be present in rocks containing pyrite. Most importantly, pyrite is an ore of gold. Pyrite is sometimes used as a gemstone but is not great for jewellery as it easily tarnishes. In some fossils of ammonites – shelled cephalopods that died ~66 million years ago – pyrite also replaces the shell. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study. A small-medium-sized solid specimen with the minerals actinolite (dark green fibrous) and pyrite (brassy) with shades of brown, black/grey, and white. Actinolite is an amphibole mineral in the tremolite-actinolite series of calcium, magnesium, and iron silicates. Pyrite is an iron disulfide mineral.geological specimen, geology, geology collection, burke museum, beechworth, indigo shire, geological, mineralogy, pyrite, actinolite, victoria, sewyln, alfred selwyn

Malachite is a water soluble, crystalline, triphenyl methylene chloride salt. It has a close relationship to copper because it is common for Malachite and copper to come from the same ore. Malachite often has shades of green, making it also known as Malachite Green. As a result of it's colour, it is known for being a dye and has been used in the dye industry, the textile industry and in medical fields. Cobar in New South Wales is well known for it's mining. This is because of the number of important deposits present in the area and include three important mining belts where most of the materials are found. These are the 'Cobar belt', the 'Canbelego belt' and the 'Girilambone belt'. The 'Cobar belt' runs underneath the main town. Copper was first discovered in Cobar in 1869 and since then, many deposits of other materials have been found, including Malachite.This specimen is significant because it comes from Cobar, NSW and represents the many deposits of materials found there. Cobar has a long history of mining and is a source of Australia's copper minerals. Malachite is often found in copper deposits meaning that it is representative of Cobar's copper production. Malachite is known for it's vivid green colour and as a result, has many uses, such as meaning used as a dye. This makes it a valuable material and highly significant. 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 hand-sized mineral with shades of brown , white and light green throughout.geological specimen, geology, geology collection, burke museum, beechworth, malachite, copper, water soluble, cobar, cobar mines, cobar mining, cobar nsw, nsw, new south wales, mining belts, ore, copper ore, malachite green, dye, green, dye industry, textile industry, desposits, canbelego, girilambone, alfred selwyn

This particular specimen is found in Wolgan Valley, New South Wales. It could be linked to the abandoned oil shale mining sites in Wolgan Valley such as Newnes. Newnes was an industrial complex operational in the early 20th century is now partly surrounded by Wollemi National Park. It produced motor spirit, kerosene, and gas oil. Newnes's Torbanite oil shale rock contained around 350 litres of oil shale per tonne. The Torbanite was mined by the Commonwealth Oil Corporation Ltd. Oil shale is a sedimentary rock and also a form of fossil fuel. It is often formed millions of years ago and usually contain fossilised remains of plants and/or animals. Oil shale is rich in kerogen that releases hydrocarbon when heated. These hydrocarbon can be used as an alternative petroleum or natural gas. The oil-shale rock was converted into oil by "destructive distillation"; the rock being heated until it broke down to form an oily vapour and an ash residue. Oil bearing shale is one of Australia's national assets. There are many oil companies established in Australia. It reflects Australia's rich natural resources as well as connection to the Australia's engineering and oil industry. The booming oil shale extraction businesses can be traced as far back as 1920s. 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 dark gray oil bearing shale with shades of light brown and fossilised leavesExisting label: OIL BEARING SHALE with / FOSSILISED LEAVES / Locality: Wongan Valley, NSW / Donor: Miss M. Cambell geological specimen, geology, geology collection, burke museum, beechworth, oil shale, shale, fossil fuels, alfred selwyn, wolgen valley, 1868 geological survey of victoria, rocks, sedimentary rocks, newnes, torbanite, commonwealth oil corporation ltd

Galena occurs in a range of deposit contexts, often in metalliferous veins, such as Broken Hill, Australia; Coeur d’Alene, Idaho, United States.; Clausthal Zellerfeld, Germany; and Cornwall, England. Large deposits also replace limestone, dolomite, or occasionally organic matter, or have a contact-metamorphic origin. Galena is additionally found in cavities, brecciated (fractured) zones in limestone and chert, and in coal beds. This specimen was recovered from Broken Hill NSW and is 60% lead with 8-12 oz/silver to the ton.Galena or 'lead glance' is a grey lead sulfide and the chief ore mineral of lead. It forms isometric crystals in which the ionic lattice is similar to sodium chloride. Galena is brittle and easily weathers to secondary lead minerals, with the upper part of mineral deposits often containing cerussite, anglesite, and pyromorphite. It usually contains silver, which is mined along with its lead content. Other commercially important minerals that form in close association with galena are antimony, copper, and zinc. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A small-sized solid specimen containing one mineral with a sparkly silver metallic lustre exterior and pastel-grey interior.geological specimen, geology, geology collection, burke museum, beechworth, galena, lead sulphide, alfred selwyn, broken hill

Anthracite typically occurs in geologically deformed areas due to extreme heating – with temperatures ranging from 170 to 250 °C – caused by igneous intrusions or high geothermal gradients. It is most commonly found in northeastern Pennsylvania in the United States; however, smaller amounts are also found in Australia, China, eastern Ukraine, South Africa, western Canada, and other countries. This specimen was recovered from Tasmania and is 85-95% carbon.Anthracite is the mineral name for hard coal and is the least plentiful of all coal types. It is clean to the touch and, when polished, is used for decorative purposes. Before natural gas and electricity, anthracite was used for domestic heating as it produces little dust, burns slowly, and gives off a minor amount of smoke. However, it is also limited in abundance and expensive. 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 hand-sized highly metamorphosed coal mineral with a black/steel-grey shiny metallic lustre.geological specimen, geology, geology collection, burke museum, beechworth, indigo shire, geological, mineralogy, victoria, alfred selwyn, anthracite

This specimen is Cassiterite in Quartz. Cassiterite is a tin oxide metal that forms in thin crystals which can have a beautiful lustre. Quartz is made of silicon dioxide, also known as silica, and is one of the most common minerals on earth. Cassiterite has been a fundamental source of tin ore for humans throughout history, including today. Tin is an important metal that has a wide variety of human uses in different areas, from dying fabric, to making mirrors, and their most well-known use ‘tin’ cans. Tin cans are primarily made of steel and are coated with tin in order to take advantage of tin’s property of being non-corroding. This is a massive step in the history of food preservation. Tinned food first reached Australia in 1815 with early settlers, and it began to be manufactured here in the 1840s. It was incredibly popular, and was a highly exported product, which would be a contributing factor to the ‘tin mining boom’ of the early 1880s. This specimen was collected at Jingellic, New South Wales, in about 1852. Although the Goldfields of the 1800s are much more well-known, tin mines existed alongside the gold mines which began in the mid 19th century and extended almost one hundred years, to the mid 20th century. Specimens like this would have been used as evidence to justify tin mining operations in the region as an investment. 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. The Geological Survey of Victoria 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 fist-sized solid geological specimen made on one half of tin oxide, which is dark grey, and on the other side of silica, which is brown and cream.burke museum, beechworth, geological, geological specimen

This item was used in Dicken's Store. Originally the Pardew Brothers store in Nicholson Street, Orbost, Frank Dicken purchased the shop business. It was a bakery and general store and was known as F.B. Dicken and Son. In 1948 they bought the shop freehold . The store remains today converted into two separate shops. The meat slicer was purchased from Henry Berry and Company a large wholesale grocers and general merchant company, first established in Melbourne in 1859.The Dicken store is a prominent Orbost building. Frank and May Dicken moved to Orbost in 1936 where Frank became manager of Pardew Brothers store in Nicholson Street. In 1945, Frank purchased the business and in 1947, formed a partnership with his son, Selwyn. The store was then called F.B. Dicken and Son. The premises are still retained by the Dicken family although the shop business was sold in 1981. (ref. In Times Gone By - Deborah Hall)A heavy commercial meat slicer which sits on bench. Frame is painted red. The tray moves as the handle turns. The main structure is cast iron. It has a circular steel blade. The chrome output tray is detachable. The movable carriage has a cast aluminium tray with spikes to hold the meat and there is an adjustable clamp to secure the meat.INVICTA Model No 302 21 HENRY BERRY PTY LTD MELBfood-preparation dicken-store meat-slicer

2 photo of number 4, Old fire stationelstrenwick, selwyn st, fire station, o’donnell, jenny

11 photographs of Glen Huntly Road, Elsternwick, from horsedrawn carriage days to the 1980s: A black and white photograph (200mm x 253mm) of Hulbert Gorrie standing outside the shop front of Rankin and Eyval Chemists at 35 Glen Huntly Road Elsternwick. Date and photographer unknown. Three black and white photographs (107mm x 130mm; 88mm x 140mm; 88mm x 88mm) of shop fronts on Glen Huntly Road taken in different eras. A horse drawn vehicle and women in long dresses are shown in one of the photographs. The other two most likely date to the 1960s. Exact dates and photographers unknown. Seven colour photographs of advertising signs revealed when a building on Glen Huntly Road was demolished in the 1980s to build the Bank of New South Wales.gorrie hulbert, rankin and eyval chemists, cast iron work, pharmacies, balconies, chemists, architectural features, advertising signs, selwyn street, p calandro and co, estate agents, elsternwick, chinese café, j higgins, glen huntly road

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."[4] 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!A variety of Letters written by Richard Squire to his son Tom Squire about the goings on at Mt Mercer Mine 1937richard squire, tom squire, hazel squire, jack squire, jim squire, ned, mt mercer, plant, skids, pump, poppet, carburetor, shaft, balance weight, pulleys, syndicate, suction, lease, reports, estimates, flat fields, reef, trucks, pipeclay, sandstone, suction pipe, valves, honeycomb rock, yarrowee, ballarat, reef combs, cheques, yellow slate, leigh river, dyke, quartz, ballarat deep leads, ballarat deep leads extension, bore, reads, bedrock, cemented sand, g m of a, gold mines of australia, liz the car, geoff squire, lode, cameron and sutherland, hayes timber, alan squire, ethel, ross creek field, ross creek gold mining co., frank herman, lillas, jack hayes, eyres brothers, g.gay & co, buninyong, glenfine, the star mine of avoca fields, talbot alluvials, guildford plateau, a.b.c. special supply store, geological branch, shell coy, lawaluk, almanac, mcbinny, bingley's paddock, cargaire valley and lead, stand and deliver demands, sheehan's, smeaton hotel, john charleson, aleck charleson, ted brown, billy jordan, mr banks, ballarat main lead, binney, goon, illabrook, mrs trenery, bre, max, june, mary, len, barry, hunter, herman, martin, aunt annie, bella, pitfield coy, mcnaughtons, donaldson, dereel, hogan, the bay leads, avoca field, ballarat alluvials, neil cameron, haddon field, courier, tom cotton, llewellen, stanley hunter, mr leonard, tom mitchell, school of mines, bryant, a.c. connely, dodson, constable mcmullins, adam ronaldson, bewick mining & co., reginald murray, r.c. selwyn, craig's hotel, broken hill syndicate, morrison's lead, wilkinson, j. hayes, mr nichol, burglary, baragwanath, wilkinson ross, creswick, seville, mr. ross, o'connor, c. mcgrath, alfred mica smith, henderson ross, angus kelly, a. r. dodson, duke of wellington plant, the moorabool lead, williams, paralysis, woodlock, squire, whipp, joe williams, peacock, moran, buchanan, hoare, bree kutchel, kohinoor band and alluvian, star of the east, bonshaw, epidemic, polio, mining

Percy Richards taught Architecture and Building Construction at The Ballarat Art School - a division of Ballarat School of Mines from 1918-1921. He was responsible for the design of a number of buildings in the district. This item is the "Specification of work required to be done and materiaals required for construction of the new A.N.A. Building at the corner of Sturt, Albert and Lewis Streets, Ballarat. Prepared by and to the satisfaction of P.S. Richards, A.R.V.I.A. Architect and subject to the General Conditions of Contract." "BALLARAT CITY A.N.A. BALLARAT, Wednesday — The Ballarat City branch, A.N.A., which was formed nearly 50 years ago, ranks fourth on the association records, but several of the members were prominent in establishing the association in Melbourne a year or two earlier. On the past half-year's operations the total funds increased by £1558/18/3 to £29.389/11/11. The membership now totals 949. The committee recommended that as the property at the corner of Sturt and Albert Streets, which had been intended as the site of a new hall, had been sold, steps should he taken to remodel the present hall, and bring It up to date. The report was adopted." (The Herald, 18 June 1924)Fourteen detailed drawings showing the specifications for each section of the new A.N.A. building for Ballarat. A 24 page document submitted to the Public Health Department, Victoria, received 15 January 1918 and a 3 page document related to Reinforced Concrete Particulars. All contained in a labelled black metal cylinder.A.N.A.4. PLANS painted on side and lid. Signature of P.S. Richards.ana, australian natives' association, architecture, percy richards, building specifications, ballarat, technical art school ballarat, materials, construction, p.s. richards, percival selwyn richards