A printed book published in paperback edition. 21 pages, with illustrations and portraits. BMDHS Location: AR/SU5 Pamphlets Box 4non-fictionA brief history of the Bacchus Marsh Rifle Club written to celebrate its 125th anniversary. The club was preceded by an association which formed in 1868 with 14 initial members. It later formed into a club. According to this book rifle shooting is the oldest organised sporting activity in the district of Bacchus Marsh and this work documents this long history up to 1993. The club continues to exist in 2024. Citation: Club Number 4: A Short History of the Bacchus Marsh Rifle Club. Written by John Tidey with additional research by C.D. (Doug) Watson. Published by Bacchus Marsh Rifle Club, Bacchus Marsh, Vic., 1993.bacchus marsh rifle club, rifle clubs, shooting

An A4 size spiral bound publication detailing the work of John Gordon and his sons William and Charles. It includes a speech transcript as well as articles and images.John Gordon was born in Chelsea, London in 1826. He and his wife Eliza migrated to Australia in mid-1853. They settled originally in Sydney where John practiced his profession of carpenter. By 1868 John was advertising himself as an architect. In May 1876 he and George Sheppard of Wagga announced they had entered into partnership, adopting the name "Gordon and Sheppard". John drowned in the Murrumbidgee River at Wagga on the 19 December 1880 when aged 54, leaving a wife Eliza, two sons William Joseph and Charles Goodwin and a daughter, Ada Martin. In 1881 William and Charles established the firm Gordon & Gordon. Gordon & Gordon's practice initially covered southern Riverina, however by 1890 it was very Victorian orientated having offices in Melbourne, Corowa, Rutherglen, Mansfield, Benalla, Euroa, Wangaratta, Albury, Seymour and Wodonga. This publication documents many of the buildings designed by William and Charles Gordon, including images of many of them. Some of the more well-known ones were St. Patrick's Church in Albury, Fairfield villa at Brown’s Plains for G F Morris, the Wodonga Shire Hall of 1890, A. Schlink's Store in High Street, Wodonga, Old Tallangatta Shire Offices and Butter Factory, St. Joseph's Convent, Wodonga, "Cambourne" and the de Kerilleau Homestead.gordon and gordon architects, building albury & wodonga

non-fictionA history of the Glass Family and the development of "Redlands" farm and homestead at Allan's Flat, Northeast Victoria. Jesse Glass was born in Bratton, Wiltshire, England and married Elizabeth Smyth in 1868 in Beechworth. They established Redlands in Allan's Flat and their descendants became pioneers of the surrounding district. He passed away at "Redlands" in 1916.glass family, redlands farm, allan's flat pioneers, yackandandah

Index, p.626.non-fictionThe experiences of Gertrude Bell during her times in the Middle eastmiddle east - politics and government, gertrude bell 1868-1926

Stapled printed softcover booklet. 20 pages. 200mm x 290mm. Facsimile reproduction of a real estate booklet originally produced in 1947 by Sands and McDougall Pty Ltd for sale of the Underbank and Parwan Park properties in Bacchus Marsh. Facsimile reprint of original publication. Date of reprint copy c.2022. Original copy, printed 1947, is also held by Bacchus Marsh and District Historical Society. BMDHS Location: AR/SU4non-fictionSolomon (Sol) Green was a major bookmaker, businessman, real estate investor, racehorse owner and trainer, and philanthropist. His connection to Bacchus Marsh was through his ownership of the Underbank Stud property which he purchased in 1924. He also owned the Parwan Park property for some time. Both of these properties were put up for sale in 1947 just a year before the death of Sol Green in 1948. solomon green 1868-1948, bookmakers, parwan park, underbank stud, land sales bacchus marsh

This specimen was recovered from Mica Schist, Canada. Chalcopyrite is a copper iron sulfide mineral with a chemical composition of CuFeS2. Its name derives from the Greek words for copper (chalco-) and brass (pyrite). It can be found in shades of yellow, green and grey, and, when exposed to acid, it can change to purple, blue, violet and yellow tones. Weathering can cause loss of its metallic luster and its brass-yellow colour. Chalcopyrite forms under various conditions, with the most significant deposits being hydrothermal in their origin. It is known globally as the most important ore of copper for thousands of years, and is thus considered a very important mineral formation. Given its golden appearance, it is often confused for the mineral gold, earning it the popular reputation as 'fool's gold' or 'yellow copper'. However, it can be straightforwardly distinguished from gold; the latter is soft, with higher specific gravity and a yellow streak, whereas chalcopyrite is brittle, easily scratched by a nail, and has a greenish grey streak. Copper was the first metal that was used by people. It was discovered by the Neolithic man about 9,000 years ago and it gradually replaced stone as it was easier to be shaped. In Australia, search for copper began after the European settlement, leading to the discovery of substantial deposits, like the one at the Olympic Dam in South Australia, which is regarded as one of the largest copper deposits in the world. Chalcopyrite has been used for copper since smelting processes began approximately five thousand years ago. Although by no means rare, this the specimen of this mineral can be used to reflect a wider history of industrial uses of copper for a significant portion of human history. 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 copper iron sulfide mineral of brass yellow, often with an iridescent tarnish, with greenish-black streak and submetallic luster. Chalcopyrite can be formed in several ways, including crystalizing from accessory minerals in igneous rocks, or from magma or within volcano sulfide deposits. Most commonly, chalcopyrite are found in hydrothermal conditions, where it forms in hydrothermal veins. As a member of the tetragonal crystal system, it often takes the shape of tetra-headed crystals, often with striations along the sides of the crystals. #18 Copper pyrites/(chalcopyrite) in/Laurentian Slate/(page 315 of inventory)/page missing from/descriptive catalogue/ Other label: 81 /fool's gold, chalcopyrite, mineral, rock, geology, geological, hydrothermal, neolithic, european settlement, olympic dam, south australia, stone, deposits, specific gravity, greenish grey streak, brittle, mineral gold, metallic luster, cufes2, greek words

The log book from the ship Isabella Brown on a voyage from Melbourne to Singapore in 1867.The Isabella Brown was a wooden two masted brig launched in Scotland in 1840 for general cargo work. The log covers a voyage with general cargo from Melbourne to Singapore via Newcastle in 1867 plus another voyage carrying live sheep in 1868-69.Entries in pen and ink throughout.log book, isabella brown, melbourne, singapore., newcastle

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

Native Sulphur in its solid form is a yellow crystalline mineral that forms near volcanic vents and fumaroles where it is the solid form of hot gases. It is also frequently found in the subsurface as a by-product of sulphide ore mineralization. In all its forms, sulphur is one of the most commonly occurring minerals on the planet, especially in natural gases, and is key to the make-up of a range of other minerals. It is essential to continuing life on earth, and was used in ancient societies as part of medical care, religious rites, and entertainment, and was key to the invention of gunpowder by the Chinese. Native Sulphur in its solid form is a yellow crystalline mineral that forms near volcanic vents and fumaroles where it is the solid form of hot gases. It is also frequently found in the subsurface as a by-product of sulphide ore mineralization. In all its forms, sulphur is one of the most commonly occurring minerals on the planet, especially in natural gases, and is key to the make-up of a range of other minerals. It is essential to continuing life on earth and was used in ancient societies as part of medical care, religious rites, and entertainment, and was key to the invention of gunpowder by the Chinese. The exact site of extraction for this specimen is unknown, but it was probably collected in New Zealand in the 1850s. Sulphur is significant both for its historical and current uses, and for its nature as one of the most abundant minerals on the planet. Sulphur's importance comes both from its abundance and its role in ensuring survival, creating other minerals, and daily human life. This specimen is significant as representative of sulphur's solid properties. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A solid, small, crystalline mineral specimen that is largely bright yellow, with some darker spotting. geological specimen, geology, geology collection, burke museum, beechworth, sulphur, native sulphur, new zealand, native sulphur specimen, sulphur specimen

Thunderegg Agates are formed within rhyolite volcanic ash layers. They are rough spherical shapes, varying in size from less than an inch to over a metre long. Thundereggs usually contain centres of chalcedony which may have been fractured followed by deposition of agate, jasper or opal, either uniquely or in combination. A unique characteristic that these specimens have is the fact that they often look like ordinary rocks on the outside, but slicing them in half and polishing them may reveal intricate patterns and colours. These particular specimens are examples of thunderegg agates. Agate is a variety of chalcedony, a cryptocrystalline form of quartz. The agate component contributes to the intriguing internal patterns of the specimens. The specific locality of these specimens is unknown but they can be found in flows of rhyolite lava. They are formed in gas pockets in the lava, which act as moulds. These specimens can be found globally, with specific locations in Germany being particularly abundant. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.Two small solid specimens with pale, sandy-coloured exteriors and fractured internal patterns. burke museum, beechworth, geological, geological specimen, thundereggs, thundereggs agate, agate, rhyolite, rhyolite lava, volcanic ash, chalcedony, cryptocrystalline

A fossil refers to any remains or traces of past life that are preserved in the rock. It could be remains of plants or animals. Fossil leaves are commonly found on different types of rocks. These fossils can go as far back as the Triassic Age just like the series of fossil plants collected at Denmark Hill, Ipswich in Queensland. Fossils leaves are formed when dead plants get buried by sediments like mud, sand, or volcanic ash. Often, it gets detached cleanly from stems along a special layer of weak cells, then twigs, and, less commonly, cones of conifers and fruits and seeds of flowering plants. Over time, the leaves or pieces of leaves get buried by more sediments and eventually gets 'lithified' or hardened into a rock. Erosions and mining can cause the rocks to break and reveal the fossils buried in it. Fossilisation frequently takes place at sites in the lowlands where deposits of clay, silt, sand are found. This is usually due to weathering and erosion of rocks. Fossil leaves can provide information about ancient Australia's way of living. It contributes to Victorian biodiversity records and its botanical collections. It also contributes information on the geographical profile of Victoria as fossilisation usually occur at estuaries and deltas of rivers, river flood plains, ponds and lakes. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.Piece of light brown rock with fossilised leaves in shades of golden yellow and brown.Existing label: Fossil Leaves / Locality unknown / might be worth checking if this is Glossopteris, a Permian age plant. / C. William 16/4/21 geological specimen, geology, geology collection, burke museum, beechworth, fossil leaves, fossilization, 1868 geological survey of victoria, lithified, rocks, fossilised leaf, rock, fossils, leaves

Ventifacts are sand-blasted rocks that are typically faceted and often display parallel grooves carved by wind-blown sand. They are useful indicators of wind direction and strength in environments such as deserts, mountains, and coastal areas because they are usually not hidden by later sediment, soil or vegetation cover. In Antarctica ventifaction is strongly related to the composition or type of rock. Ventifacts are important because they provide evidence for abraders such as sand, dust or snow and ice crystals, and offer a unique understanding of past wind processes that are effective in the reconstruction of past wind flow conditions and can provides clues to weather and climate changes in the past. Interestingly ventifacts have also been found on the surface of Mars. They were a threat to the NASA rover due to the sharp angles of the facets, created by the Martian wind over the course of millions of years. These Martian ventifacts act like weathervanes for past wind and weather patterns on the red planet in a similar manner to those found on earth.The Geological Survey of Victoria was instigated in response to the Victorian Gold Rush which began around 1851 in the Beechworth, Castlemaine, Daylesford, Bendigo and Ballarat areas. The survey was conducted by Alfred Richard Cecil Selwyn from his arrival in December 1852 until his resignation in 1869and during this time he trained many notable geologists, e.g. Aplin, Wilkinson, Daintree, who went on to other State survey senior positions. This specimen was among those donated to the Burke Museum in 1868.A hand-sized solid mineral specimen in shades of dark and light browns with light lines visible in all configurations and a groove on configuration 2.light lines visible in all configurations and a groove on configuration 2burke museum, beechworth, geological, geological specimen, ventifact, antarctic region, antarctic, alfred richard cecil selwyn, alfred selwyn, wind direction, wind strength, abraders, wind flow, climate change, reconstruction of wind flow conditions, weather change, mars

Galena is the natural compound of lead and classed as a sulphide, it crystallises in a cubic pattern and its chemical formula is PbS. Galena is a primary source of both lead and silver. This specimen of Galena comes from Broken Hill. Broken Hill has one of the world’s largest and most significant deposit of ore for the production of lead. Mining of Galena at Broken Hill began with the staking of land by Charles Rasp in 1883. By the following year, in 1884, Rasp and six others had formed Broken Hill Mining Company. Broken Hill Mining Company eventually evolved into BHP group limited and is currently the largest mining company in the world and the largest company in Australia. There is archaeological evidence from artefacts discovered in Turkey that humans have been extracting lead from galena by the process of smelting since at least 6500 BCE. This specimen also has quartz on the top surface which is frequently discovered alongside Galena. This mineral specimen is of historic significance as a sample of Galena extracted from Broken Hill during the 19th century. Mining for Galena in Broken Hill begin in 1883 by Charles Rasp and evolved into the world’s largest mining company – BHP Group Limited. Broken Hill is one of the world’s most significant deposits of ore for the production of lead. 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 flat, hand-sized, grey sulphide specimen that is the natural compound of lead with a quartz formation on the top surface. Existing Label: GALENA / (with quartz) / Locality: Broken Hill / N.S.W 120 x 70 x 29geological specimen, geology, geology collection, burke museum, beechworth, galena, galena quartz, quartz, charles rasp, broken hill mining company, bhp group limited, bhp, lead, ore, lead sulphide, sulphide, silver, broken hill

This specimen was recovered from Broken Hill, NSW. It was given the name Mangan Hedenbergite in 1819 by Jöns Jakob Berzelius in honor of Mr. Anders Ludvig of Hedenberg who was the first to define hedenbergite as a mineral. Hedenbergite, belongs in the pyroxene group having a monoclinic crystal system. The mineral is extremely rarely found as a pure substance. Mangan Hedenbergite is a manganese bearing variety of Hedenbergite. Manganese is the world’s fourth most used mineral after iron, aluminium, and copper primarily because it has no satisfactory substitute in its major applications. Globally, the steel industry is the primary user of manganese metal, utilizing it as an alloy to enhance the strength and workability of steel and in the manufacture of tin cans. Manganese is a key component of certain widely used aluminium alloys and, in oxide form, dry cell batteries used in electric vehicles. These batteries are in high demand. Another potential use for manganese may as an additive to help coat and protect a car’s engine. Manganese is also used for non-metallurgical purposes such as plant fertilizers, animal feed, and colorants for bricks. 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 mineral specimen in shades of silver and blackmanganese, open cut mine, manganese ore processing, bell bay, tasmania, northern territory, steel industry, zinc-carbon batteries, alkaline batteries, tin cans

non-fictionDavid Boyle purchased land in Nunawading which he occupied in 1868boyle david, nunawading, pioneers, horticulture

One siix page handwritten and three typed copies of notes on the The Lazarus Mine including the Lazarus New Chum and the Lazarus No 1 on the New Chum Line of Reef. Notes include locality, depth of shafts, size of lease, plant, early history, the Lazarus Company, Prominence, Best Gold and Total Gold Yields. Notes prepared by Albert Richardson.document, gold, the lazarus mine, the lazarus mine, notes on the the lazarus mine, lazarus new chum, lazarus no 1, australian headquarters survey unit, george lansell, new chum hill, b c v 8 studios, sheepshead, central red white & blue, mr lazarus, lansell's 222, old chum mine, lazarus company, mr george gibbs, lansell's fortuna, ballerstedt, mr barnet lazarus, the black lead, the white lead, mount alvernia hospital, mines dept special edition 'australian mining standard' 1/6/1899, mines dept booklet 'bendigo goldfield' 1936, mines dept annual and quarterly reports, annals of bendigo mining sections 1868 - 1910, a richardson, the bendigo goldfield registry j n macartney 1/3/1871

Illustrated book with dust jacket that has been covered with a clear protective film. Dustjacket has a red background. Front cover has an oval photograph of a woman in Victorian dress (Lucy Osburn). This photo has a grey frame with swirls. Also, on the front, the title is printed in white and the author's name in black. Title (in white) and author's surname (in black) are also printed on the spine.non-fictionThis book is a historical account of the early days of nursing in Australia, specifically focusing on the Sydney Hospital and Lucy Osburn, who arrived in Sydney in March 1868.lucy osburn, sydney hospital-history, nursing-australia-history, alfred hospital nurses

Five pages of handwritten notes with typed copies of same, on the Lazarus Mine including Lazarus New Chum and Lazarus No 1. Notes include locality, depth of shafts, size of lease and plant. Includes the history, prominence, best gold, Total Gold Yield and Dividends. Albert Richardson Collectionmining, parish map, lazarus mine, lazarus mine, lazarus new chum, lazarus no 1, george lansell, b. c. v. 8 studios, sheepshead, central red white & blue, mr b lazarus, mr george gibbs, black lead, lansell's fortuna, mr ballerstedt, mr barnet lazarus, white lead, mines department special edition 'australian mining standard' 1/6/1899, mines department booklet 'bendigo goldfield' 1936, mines dept. annual and quarterly reports, annals of bendigo mining sections 1868 - 1910, a richardson, the bendigo goldfield registry j n macartney 1/3/1871.

non-fictionjohn pascoe fawkner, melbourne, taffe fawkner collection, hymettus library, ballarat, kirsop, book collectors' society of australia

Book, hard cover. First edition. Melbourne, Vic., Melbourne University Publishing, 2009. By David Baillieu. 389 pages. BMDHS Location: AR/SU63/S2 non-fictionRobert Lawson was the first Principal of Scotch College in Melbourne. He was Principal of Scotch College from 1851 until 1856. He later acquired land in the Pentland Hills near Bacchus Marsh and operated a school at Blackwood which he called the Landsberg Mains School. It was also known as the Landsberg Academy. The school opened in 1857 and operated under Lawson's direction until 1868. The school building was an imposing bluestone structure which came to be known as Landsberg House.The school was very successful for a time in the 1860s attracting students from across Victoria. Lawson died in 1869 and the school continued to operate until 1880 under a different Principal. Lawson is considered a pioneer educationalist in Australia. This is a substantial and scholarly biography about Lawson and his wife Isabella Wilson. Several chapters explore the time Lawson spent operating his school at Blackwood. schools bacchus marsh region, schools blackwood victoria, landsberg academy, robert lawson 1826-1869, isabella lawson

Pyrite also known as iron Pyrite or fools gold is an iron sulfide with a chemical formula of FeS2 and is the most abundant sulfide mineral. Its metallic luster and pale brass-yellow hue give it a superficial resemblance to gold for which its nickname of Fools Gold comes from. There are a number of iron pyrite mines in Victoria and many would have been mined during Victoria's Gold Rush revolution in the 19th century. As it's lustrius yellow metallic look closely resembles gold, it is likely that it was often mistaken for gold as real gold was also often found in similar metamorphic and sedimentary rock. 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 collections were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush). Collecting these specimens was an important part of Australia's early Geoplogical scientific discovery for mapping the earth's surface. It is unknown where in Victoria this specimen was mined from however; it shows strong provenance connections to Victoria's gold mining history and represents through larger economic and cultural structures the impact the Gold Rush had on Victoria during the 19th century. A solid coin-sized Pyrite crystal in black slate in shades of beige with tiny crystal structures. Pyrite / crystals / BB / in black slate / probably / victoria / (nice specimen)geology, geological specimen

Produced as a family memorial card at Julia's death in 1927 and retained in the family ever since in her beloved home 'Hymettus'.Julia Taffe was born Julia Berkery at Bungaree in 1868 of pioneering Irish couple Patrick and Mary Berkery who arrived and settled in the district in1853. Proud of her pioneering family and close to her uncle, Daniel Brophy, Shire President of Bungaree, MLA and Mayor of Ballarat she requested the family home remain as such. Hymettus has been kept in accordance to her wishes.ballarat, bungaree, pioneer

xvi, 175 p.; 24 cmnon-fictionA History of the Shire of Berwick now the City of Berwick and the Shire of Pakenhamcity of berwick, shire of pakenham, shire of berwick, list of berwick shire presidents from 1868 to 1973, berwick road board presidents from 1862 to 1867, berwick quarry,