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The Beechworth Burke Museum
Photograph, 1990s--estimated
Taken in 1990, this photograph depicts a row of shops in Beechworth, with the shopfront of watchmaker and jewellers, William Turner and C.F. Falck, in the foreground, and newsagent and bookseller James Ingram's shop in the background.This photograph is of social significance to the Beechworth community in depicting the Street of Shops, the creation of curator, Roy Harvey, which opened in 1979 at Burke Museum. According to the Indigo Shire Council webpage for Burke Museum, this addition 'began a new period of collecting with Roy Harvey calling to the community for donations. The response resulted in an influx of material adding to the town history/ development and local identities collections. The Shops and their contents reflect another period in museology.' The historic shopfronts in this image portray those of local settlers, William Turner and CF Falck's Watchmaker and Jeweller store, and James Ingram's news agency and bookshop. William Turner was originally a goldfields official who became a commissioner on the Ovens goldfield, and later a resident warden, at times performing magisterial duties and chairing the Local Court. Charles Frederick Falck, born in Korlin, Germany, in 1833, a skilled watchmaker and jeweller, ran the jewellery business from 1862. Along with William Turner and Melbourne barrister, George Milner Stephen, he prepared a dazzling display of gems and jewellery from Beechworth for the Royal Society's Exhibition in Melbourne in 1865. This act signposted Beechworth's progress as a nineteenth-century gold rush town with a population of around 3000. In the mid-1850s, newsagent James Ingram established a newsagency and supplied papers and stationary to the goldfields. He and bookseller R.T. Vale stocked a wide range of literary, historical and religious works, textbooks, periodicals and newspapers, as well as hosting a reading and writing room on Camp Street{?}. James Ingram was a 'devoted instigator and supporter of the town's welfare institutions', who raised funds for to establish a hospital, primary school and benevolent asylum, and assisted people who'd fallen on hard times with his wife. He was also a mainstay of the early Baptist church, holding meetings in his house. He died in 1928, six weeks short of his 100th birthday. Ingram's Rock, north-west of Beechworth near where he lived in later life, was named after him. Colour rectangular photograph printed on matte photographic paper.Obverse: FALCK 1880 / maker & Jeweller/ WARDENS OFFICE/COACHING OFFICE/ EST. ??55/ ????ON HOUSE/ JAMES INGRAM/ NEWS?????? AND BOOKSELLER/ TOYS visible above shopfront in left foreground. Reverse: Catalogue item number 3305 pencilled in top right-hand corner.beechworth, beechworth historic shops, william turner, cf falck, james ingram, turner and falck watchmaker and jeweller, james ingram newsagent and bookseller, burke museum, promoting settlement, marketing and retailing, living in country towns, making regional centres, preserving traditions and commemorating, beechworth founders, victorian gold rush towns, beechworth pioneers, ingram's rock, 1860s beechworth, street of shops, roy harvey -
The Beechworth Burke Museum
Geological specimen - Ilvaite
Ilvaite has acquired its name from Ilva (Latin for Elba) Island, Greece, where Ilvaite is most commonly found. The geological setting in which Ilvaite occurs is through contact with magnetite, zinc and copper ore deposits, along with contact metamorphic deposits and zeolite zones. llvaite crystallizes in the form of black prismatic crystals and columns . This specimen was retrieved from Broken hill, known as the world's richest and largest zinc-lead ore deposit. Because of Ilvaite's often unaesthetic crystal formations compared to other minerals, Ilvaite is uncommon in most rock collections, particularly specimens that are not well formed, such as this one. Ilvaite is also a member of the Sorosilicate subclass of the silicate minerals, which have an unusual basic unit of Si2O7, making Ilvaite a unique mineral. Given that Ilvaite is not commonly found in Australia, it marks a unique contribution to an Australian collection of minerals. 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 ferrous iron analogue mineral with of black with shades of beige Ilvaite is a brittle, opaque rock formation that has acquired its name from Ilva (Latin for Elba) Island, Greece, where Ilvaite is most commonly found. The geological setting in which Ilvaite occurs is through contact with magnetite, zinc and copper ore deposits, along with contact metamorphic deposits and zeolite zones. llvaite crystallizes in the form of black prismatic crystals and columns rock, mineral, ilvaite, ilvaite specimen -
The Beechworth Burke Museum
Geological specimen - Porphyritic Rhyodacite
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 -
The Beechworth Burke Museum
Geological specimen - Gold-Sulphide Ore
This particular specimen was recovered from two hundred feet down in the Golden Mile in Kalgoorlie, Western Australia. The Golden Mile, named after the estimated sixty million ounces of gold worth around one hundred billion dollars, was the birthplace of the largest gold rush in Australia almost one hundred and thirty years ago when William Brookman and Samuel Pearce leased the Great Boulder mine. The Golden Mile is also the home of the Super Pit, Australia's most well-known mine.The majority of gold deposits will form as a native metal, however, on occasion, it can form a compound with another element, in this case, sulphur. Therefore, this specimen is a rare example of gold naturally forming into a compound mineral with sulphur. 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 gold-sulphide ore mineral specimen in shades of silver and grey with flecks of gold. Precious metals are often found in Sulphide Ores, as sulphides usually bind to these metals. They are also extremely symmetrical in crystaline form. Gold-Sulphide Ore occurs when gold forms a natural compound with other elements. In this form, gold can be present in one of two ways. It can be fully immersed in the sulphide, or a portion may be partially free. This specimen has minimal gold visible, with only a few flecks being partially visible.burke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, mineralogy, gold-sulphide ore -
The Beechworth Burke Museum
Geological specimen - Spotted Slate, Unknown
This specimen was recovered from Sedgwick, VIC. Spotted slate is a fine-grained porphyroblastic metamorphic rock with a number of compounds including muscovite, quartz, graphite with cordierite poikiloblasts and more. The cordierite poikiloblasts are rounded crystals that size up to 2.5 mm. the growth of these crystals is in response to metamorphism of low to medium intensity. The town Sedgwick was named after British geologist Adam Sedgwick 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 rectangular hand-sized spotted slate specimen in a shade of light grey with darker flecks throughout Spotted Slate / Locality: Sedgwick Victoria | This is an early specimen / from the Quarter sheet / map. See sample 62 / page 18. Described as 'Spotted Slate' but these / days we would call it spotted hornfels / C. William 15/4/21 slate, spotted slate, victoria, beechworth, burke museum, geological specimen, mineralogy, sedgwick, sedgwick victoria, spotted slate specimen -
The Beechworth Burke Museum
Geological specimen - Greenstone / Gabbro, Unknown
This specimen was recovered from Ceres West of Geelong, Victoria. Greenstone is the name for any metamorphosed basic igneous rock (in the case of this specimen, Gabbro) that gains its greenish colour to the presence of the minerals chlorite, actinolite, or epidote, hence the term 'green' and 'stone'. Greenstone is often formed through metamorphsis along a convergent plate boundary. In the rock cycle (the series of processes that creates the various types of rocks) there are identified three different types of rocks, which are the sedimentary, the igneous and the metamorphic. Metamorphic rocks started out as sedimentary, igneous or earlier metamorphic rocks but changed from their original condition under the effect of high heat, high pressure or hot, mineral-rich fluid. However, if pressure or heat is too high, then the rock will melt, resulting in the formation of an igneous rock. The name used to describe these types of rocks reflects this specific inherent trait of change, since the word “metamorphic” derives from the Greek word “metamorphosis”, meaning “change of form or structure”. Metamorphic rocks form in the Earth`s crust but can be also found on the surface, due to elevation of the Earth`s surface. They are divided into two categories: the foliated metamorphic and the non-foliated metamorphic rocks. Gabbro is a highly useful mineral that is often polished to create cemetery markers and kitchen benches. It is notable for its qualities of durability, being able to withstand extreme elements and wear. Whilst not rare, Gabbro is of great utility and has been highly desirable for its qualities. 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.Greenstone is a solid hand-sized metamorphic mineral of a green colour. Greenstone is the name for any metamorphosed basic igneous rock (in the case of this specimen, Gabbro) that gains its greenish colour to the presence of the minerals chlorite, actinolite, or epidote, hence the term 'green' and 'stone'. Gabbro is a medium to coarse grained rocks that consist primarily of plagioclase feldspar and pyroxene. Greenstone is often formed through metamorphsis along a convergent plate boundary. Gabbro forms due to cooling and crystallization of magma underneath Earth's surface. Greenstone/Gabbro/from Ceres west/of Geelong. Has old Geological Survey label/and probably collected by/Richard Daintree in 1861/C.Willam 15/4/21/ Other label: 62 /greenstone, metamorphosed, igneous rock, gabbro, chlorite, actinolite, epidote, metamorphsis, rock cycle, various types of rocks, sedimentary, high heat, high pressure, mineral-rich fluid, metamorphosis, foliated metamorphic, non-foliated metamorphic, convergent plate boundary, greenish colour, minerals -
The Beechworth Burke Museum
Geological specimen - Slate with Iron pyrites
This specimen was recovered from Moonambel, Donkey Hill, Victoria. Established in the early 1860's, Moonambel is a small town in the Pyrenees region of the Australian state of Victoria. In the 1850s the location of Moonambel was part of the ‘Mountain Creek’ pastoral run, but in 1860 reports began to appear of a gold-rush at McKinnon’s ‘Mountain Creek’ station. By 1861, a township had developed on the diggings site, and on 21 October 1861 the “municipal district of Moonambel, on Mountain Creek” was proclaimed. The name 'Moonambel' is believed to be an aboriginal word meaning 'hollow in the hills'. Slate is a stone with a fine grain that is noted for its persistent strength and ability to naturally split into slabs. It forms under low temperatures and is most often created from clay. Pyrite is a crystallising compound that occurs naturally in grey and blue-black slate that is colloquially referred to as slate-rust as it resembles regular rust. 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.Pyrite is iron sulphide (also known as “fool's gold”) which is commonly found in slates.Existing label: 53 /moonambel, slate, pyrite, burke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, mineralogy, victoria -
The Beechworth Burke Museum
Audio - Oral History, Jennifer Williams, Mr Albert (Bert) Nankervis, 15th March 2000
Mr Albert (Bert) Nankervis was born at Thougla, in the Upper Murray, in 1903. He had a large family and was one of eight children, four boys and four girls. He and his family moved to a farm in Wooragee named ‘Wattle Grove’ in 1918 after his father returned from serving as a soldier in World War One. The family established ‘Wattle Grove’ as a dairy farm as Beechworth has a high demand for milk and little supply. They had 25 milk cows that were hand milked every morning in order to provide milk for approximately 100 customers in the town, with any extra going to the butter factory at Springhurst. Albert married Floré Lilias Hardy in 1930 and they had two sons, Phillip and Barry. In this oral history, Albert discusses his life as a farmer in Wooragee, including his role in getting electricity to Beechworth, as well as his participation in the Young Farmer’s Association Immigration Scheme, which provided work experience to migrants in order for them to learn how to farm. This oral history recording was part of a project conducted by Jennifer Williams in the year 2000 to capture the everyday life and struggles in Beechworth during the twentieth century. This project involved recording seventy oral histories on cassette tapes of local Beechworth residents which were then published in a book titled: Listen to what they say: voices of twentieth century Beechworth. These cassette tapes were digitised in July 2021 with funds made available by the Friends of the Burke. Mr Albert (Bert) Nankervis’s account of his life in Wooragee and the local area, including Beechworth, during the early 20th century is historically and socially significant to the cultural heritage of the region. He details his life as a farmer and milkman in the early 20th century, particularly the interwar period (1918-1939), but also discusses life after the Second World War, including employing young migrant men to train them as farmers through the Young Farmer’s Association. This oral history account is socially and historically significant as it is a part of a broader collection of interviews conducted by Jennifer Williams which were published in the book 'Listen to what they say: voices of twentieth-century Beechworth.' While the township of Beechworth is known for its history as a gold rush town, these accounts provide a unique insight into the day-to-day life of the town's residents during the 20th century, many of which will have now been lost if they had not been preserved. This is a digital copy of a recording that was originally captured on a cassette tape. The cassette tape is black with a horizontal white strip and is currently stored in a clear flat plastic rectangular container. It holds up 45 minutes of recordings on each side.Mr Albert (Bert) Nankervis / albert nankervis, bert nankervis, nankervis, wattle grove, wooragee, dairy farm beechworth, dairy farm, dairy factories beechworth, dairying, milkman, oral history, springhurst, butter factory, electricity, rural life, farming and agriculture, farm, farm work, cow, cattle, jersey cattle, interwar period, first world war, second world war, wwi, wwii, greatest generation, centenarian, nonagenarian, 1920s, 1930s beechworth, thougla, upper murray, murray, lucyvale, benalla -
The Beechworth Burke Museum
Audio - Oral History, Jennifer Williams, Mrs Vanessa McDonald, 9 November 2000
Mrs. Vanessa McDonald was born in Beechworth in 1917. Christened, Agnes Bertha Collins, Vanessa changed her name in 1960. Mrs. McDonald's family's connection with gold mining in the district reach back to the first of Beechworth's gold rushes, when her great grandfather, a Dutchman who adopted the name Charles Collins, arrived in 1851-1852. Mrs. McDonald spent her childhood in the isolated hamlet of Stanley, in the area known as 'Little Scotland', where she recalls helping her mother to raise younger siblings, picking apples and walnuts on the family farm, and roaming the hills for wildflowers. As a young woman Mrs. McDonald attended religious and social gatherings in the local community. In 1940 she went to Melbourne to work as a mothercraft nurse during the Second World War. She met her husband at a Beechworth football match and was married at the Stanley Methodist Church in 1941. The gold diggings known as the 'Nine Mile' became the hamlet of Stanley, after the British Prime Minister, Lord Stanley, in 1858. By the late 1850s, Stanley boasted schools, an athenaeum, a church, a weekly newspaper and several hotels and other civic infrastructure to cater for a growing population. The area attracted large numbers of Chinese miners, whose presence was frequently resisted. Like other early Victorian mining settlements, Stanley was a hotbed of political and racial tensions during the gold rush. One side of the Nine Mile Creek was known as 'Little Scotland’, the other, 'Little Ireland'. A number of Christian denominations built congregations and churches in Stanley, including the Church of England, Methodist Church, the Catholic Church, and Presbyterian Church. Stanley became part of the United Shire of Beechworth in 1871. By 1880 timber was being cut and two sawmills were established by 1887. River-dredged gold mining consumed vast amounts of timber from the forests in the area, and in 1931 the first of several softwood plantations began. This oral history recording was part of a project conducted by Jennifer Williams in the year 2000 to capture the everyday life and struggles in Beechworth during the twentieth century. This project involved recording seventy oral histories on cassette tapes of local Beechworth residents which were then published in a book titled: 'Listen to what they say: voices of twentieth century Beechworth'. These cassette tapes were digitised in July 2021 with funds made available by the Friends of the Burke.Following the decline in the mining and associated industries during the early-mid-twentieth century, the Beechworth district experienced a period of general economic decline. On the east side of the Dingle Range, Mrs. McDonald's father, William Henry Collins, felled timber and the family were pioneer apple orchardists. The establishment of apple orchards in Stanley reflects changes to how land was used and contributes to our understanding of the historical development of rural communities following the gold rush. Mrs. McDonald's recollections are significant for understanding family and social life in a small rural town in years leading up to the Great Depression and prior to the Second World War. This oral history recording may be compared with other oral histories and items in the Burke Museum's collection. This oral history account is socially and historically significant as it is a part of a broader collection of interviews conducted by Jennifer Williams which were published in the book 'Listen to what they say: voices of twentieth-century Beechworth.' While the township of Beechworth is known for its history as a gold rush town, these accounts provide a unique insight into the day-to-day life of the town's residents during the 20th century, many of which will have now been lost if they had not been preserved.This is a digital copy of a recording that was originally captured on a cassette tape. The cassette tape is black with a horizontal white strip and is currently stored in a clear flat plastic rectangular container. It holds up 40 minutes of recordings on each side.Mrs Vanessa McDonald /listen to what they say, beechworth, oral history, burke museum, emigration, gold rush immigration, victorian gold rush, mining families, apple orchard, forestry, forest plantation, little scotland, stanley, twentieth century history, regional australia, rural australia, farming, harvest festival, great depression, dingle range, the nine mile, australian wildflowers, high country wildflowers, mothercraft nurse, rural and regional women, social history, collins, mrs. vanessa mcdonald, building community life, shaping cultural and creative life, fruit growers, family history, changes to land use in regional victoria -
The Beechworth Burke Museum
Audio - Oral History, Jennifer Williams, Gwendoline Warden, 1st June 2000
Gwendoline Warden was born in Ararat in 1913. When she was 13 years old, she moved to Wangaratta, where her parents owned the “Hibernian Hotel”. Her father`s name was William Lavender. When Gwen was around 16 years old, she moved to Beechworth, where she met her husband and they got married in 1935. They had their wedding reception at Warden`s Hotel and they had two children together, a boy and a girl. She recounts how difficult it was for them during the war to manage their grocery's shop and source the supplies they needed, having coupons for food and the black-market prevailing. They faced financial difficulties and, ultimately, they had to sell the shop. After the war she did a few other jobs and she retired when she was nearly sixty. Gwendoline portrays Beechworth as a quiet place, where people were happy and peaceful, enjoying the many opportunities they had for entertainment, such as dances and balls, or the celebrations for the New Year's Eve. She also witnessed the beginning of the famous wheelbarrow race, which started just outside the post office and a big crowd gathered to farewell the two barrowmen. When comparing the past with the present, she points out how much Beechworth has changed over the last decades, with many new people coming to town, making her feel as “the only one around”. She also remarked that young people have changed as well; in her day they were entertaining themselves but nowadays they want to be entertained. This oral history recording was part of a project conducted by Jennifer Williams in the year 2000 to capture the everyday life and struggles in Beechworth during the twentieth century. This project involved recording seventy oral histories on cassette tapes of local Beechworth residents which were then published in a book titled: Listen to what they say: voices of twentieth century Beechworth. These cassette tapes were digitised in July 2021 with funds made available by the Friends of the Burke.Gwendoline Warden's account of her life in Beechworth and the local area during the 20th century is historically and socially significant as it offers valuable information about the business activity in the region and provides a deeper insight into the way hotels and grocery shops were operating during the first half of the previous century. Additionally, along with all the details provided for many aspects of social life, her personal account of the war period is of great importance, offering vital information to research on the way the Australian society experienced WWII. This is a digital copy of a recording that was originally captured on a cassette tape. The cassette tape is black with a horizontal white strip and is currently stored in a clear flat plastic rectangular container. It holds up 40 minutes of recordings on each side.Mrs Gwendoline Warden/ararat, wangaratta, hibernian hotel, gwendoline warden, william lavender, beechworth, warden`s hotel, grocery`s shop, coupons, black-market, war, dances, new year`s eve, balls, new people, listen to what they say: voices of twentieth century beechworth, jennifer williams, cassette tapes, friends of the burke, oral histories -
The Beechworth Burke Museum
Photograph, 1973
Taken in 1973, this photograph features 13 men in suits, most of whom are council members of the United Shire of Beechworth, as well as a secretary and engineer. The photo is taken in a formal setting, suggesting there may have been an occasion at this time (potentially surrounding or related to the August council meeting). Previously a district (1856), then a borough (1863) and separate shire (1866) at this time the Local Government Area (LGA) had been known by this name for approximately two years, after having amalgamated with the still-existing borough. Beechworth amalgamated with Rutherglen and Chiltern Yackandandah to become the Indigo Shire Council in 1994. Little has been found about the men in the photograph, however this was at also around the time that women were becoming more widely accepted into positions on Victorian council (such as Valerie Mason, who was elected the first President of the United Shire of Beechworth council 6 years after this photograph.) The photograph has been taken in front of the Beechworth Shire Hall. The Hall was designed by architects J.J. Coe and Thomas Dalziel and is dated to 1859. Originally the building was used as the Shire Offices but also doubled as a fire station and a courthouse, with still surviving cells underneath. The Town Hall is now home to the Visitor Information Centre, is the starting point for historical Precinct walking tours and is available for hire for events or community meetings.The Beechworth Town Hall is one of five distinctive granite buildings on Ford Street that comprise the Justice Precinct, and is listed on the Victorian Heritage register. This photograph captures the ongoing importance and use of the Beechworth Town Hall and its ties to Council operations in the 1970s.Black and white rectangular photograph print matt photographic paperReverse - written in pencil upper right corner: 1997.2602; stamped in black ink across centre margin: Beechworth shire council Aug.1973/ Crs.H.H.Warner, H.C.Lucas, L.W. Powell, L. Leentjes, R.C. Sewell, T.J. Carroll/ G.Gray (Secry), Crs.R.P. O'Connor, D. Nankervis, D. McKenzie-McHaig, J.J. Macaulay, H.R. Sinclair/ D.Pope (Engineer), Absent Cr.J.V.Diffey; written in pencil in cursive lower left margin: Absent J Diffey; written in pencil bottom right edge: BMMA02602beechworth shire council, crs.h.h.warner, h.c.lucas, l.w. powell, l. leentjes, r.c. sewell, t.j. carroll, g.gray (secry), crs.r.p. o'connor, d. nankervis, d. mckenzie-mchaig, j.j. macaulay, h.r. sinclair, d.pope (engineer), cr.j.v.diffey, beechworth town hall -
The Beechworth Burke Museum
Postcard, 1910 - 1912
This photograph is taken of Lake Kerferd in around 1910. The photograph shows the road circling around the large lake and the jetty on the lake. On the other side, there is a written message from Fred Pulling to Win Pulling. Fred seems to have gone away and was not sure when he would return. He was also glad to hear about a gentlemen called Perc, who he stated to be a 'decent enough chap'.This postcard is significant because Lake Kerferd itself is significant within Beechworth's history. This lake was constructed in 1862 and was named after the former Beechworth Mayor, Hon. G B Kerferd. This lake was originally constructed to supply the town with water. Fred's correspondence with Win demonstrates a glimpse into what life was like during this time. Black and white rectangular postcard printed on cardObverse: (113) Lake Kerferd Beechworth / Reverse: Beechworth / 29.11.19 / [ Stamped: POST CARD / KODAK AUSTRALIA / Dear Win / Gald to hear that you / have made up your mind about / Perc / He seems a decent enough chap / too / Anyway, Thanks for the letter / Dont exactly know when we are / returning / will write later. Regards / to Nell of course, and H. (indecipherable) / Lots of love / Fred / lake kerferd, jetty, chap, postcard, letter, trees, lake, horse drawn carriage, horse drawn cart, kodak, australia, gum trees, gravel road, beechworth, kerferd -
The Beechworth Burke Museum
Photograph - Postcard, c1900
The construction on Lake Kerferd began in 1862 however it wasn't completed until 1874 due to engineering and funding issues. The lake was named after George Briscoe Kerferd (1831–1889) who was responsible for Beechworth's water scheme. George Briscoe Kerferd was born on 21 January 1831 in Liverpool, England and arrived in Melbourne April 1853. He spent his first years in Australia in Bendigo before settling down in Beechworth as a wine and spirits merchant. He married Ann Martindale on 17th December 1853 at St James Cathedral, Melbourne and between them they had three sons and five daughters. Kerferd began his political and legal career in Beechworth when he was first elected to the Municipal Council in May 1857. Later he would be elected to the Legislative Assembly for the Ovens District in November 1864, and continued to represent the area until February 1886. This photograph is historically significant as it provides insight into the water reserves of Victoria. It also demonstrates the political identity of George Briscoe Kerferd and the Beechworth Municipal Council.Sepia rectangular postcard printed on paperObverse: Reverse: 83-131-1/ Post Card/ Correspondence / Address Only / BMM2997 / 53 / [Kodak Australia Stamp] lake kerferd, beechworth, water scheme, water reserve, reservoir, legislative assembly, hon. george briscoe kerferd, catchments, beechworth water reserve, beechworth catchments, municipal council, st. james cathedral, lakes, reserve, water supply, political projects -
The Beechworth Burke Museum
Photograph, Christmas 1941
Taken on Christmas of 1941, shown is a track to Lake Kerferd with forest on both sides. The construction on Lake Kerferd began in 1862 however it wasn't completed until 1874 due to engineering and funding issues. The lake was named after George Briscoe Kerferd (1831–1889) who was responsible for Beechworth's water scheme. George Briscoe Kerferd was born on 21 January 1831 in Liverpool, England and arrived in Melbourne April 1853. He spent his first years in Australia in Bendigo before settling down in Beechworth as a wine and spirits merchant. He married Ann Martindale on 17th December 1853 at St James Cathedral, Melbourne and between them they had three sons and five daughters. Kerferd began his political and legal career in Beechworth when he was first elected to the Municipal Council in May 1857. Later he would be elected to the Legislative Assembly for the Ovens District in November 1864, and continued to represent the area until February 1886.This photograph is historically significant as it provides insight into surrounding areas of the water reserves of Victoria. It is also linked to political identity of George Briscoe Kerferd and the Beechworth Municipal Council.Black and white rectangular photograph printed on matte photographic paper.Obverse: Reverse: 8163/ Back track to Lake Kerford/ Beechworth/ Xmas 1941lake kerferd, beechworth, water scheme, water reserve, forest track, forest pathway, reservoir, legislative assembly, hon. george briscoe kerferd, catchments, beechworth water reserve, beechworth catchments, municipal council, st. james cathedral, lakes, reserve, water supply, political projects -
The Beechworth Burke Museum
Photograph - Post Card, 1920-1930's
Taken between 1920-1930s, shown is the banks of Lake Kerferd with wooden man-made fencing. The construction on Lake Kerferd began in 1862 however it wasn't completed until 1874 due to engineering and funding issues. The lake was named after George Briscoe Kerferd (1831–1889) who was responsible for Beechworth's water scheme. George Briscoe Kerferd was born on 21 January 1831 in Liverpool, England and arrived in Melbourne April 1853. He spent his first years in Australia in Bendigo before settling down in Beechworth as a wine and spirits merchant. He married Ann Martindale on 17th December 1853 at St James Cathedral, Melbourne and between them they had three sons and five daughters. Kerferd began his political and legal career in Beechworth when he was first elected to the Municipal Council in May 1857. Later he would be elected to the Legislative Assembly for the Ovens District in November 1864, and continued to represent the area until February 1886.The postcard holds Historic significance due to its connection to Beechworth and its Lake Kerford. It demonstrates the interactions between nature and colonialists, especially how the lake has somewhat been 'protected' with the man made fencing. It also presents information on the environmental development or degradation for the area, with possible changes to the environment that may have been caused by human physical forces, natural decay or Global Warming.Black and white rectangular postcard printed on paper.Obverse: Lake Kerferd, Beechworth / Reverse: 8164 / Post Card / Correspondence / Address Only / Kodak Austral [Kodak Australia Stamp] /lake kerferd, beechworth, water scheme, water reserve, reservoir, legislative assembly, hon. george briscoe kerferd, catchments, beechworth water reserve, beechworth catchments, municipal council, st. james cathedral, lakes, reserve, water supply, political projects, man-made fence, environmental changes -
The Beechworth Burke Museum
Photograph - Post Card, Rose Series Stereograph Co. Postcard
The construction on Lake Kerferd began in 1862 however it wasn't completed until 1874 due to engineering and funding issues. The lake was named after George Briscoe Kerferd (1831–1889) who was responsible for Beechworth's water scheme. George Briscoe Kerferd was born on 21 January 1831 in Liverpool, England and arrived in Melbourne April 1853. He spent his first years in Australia in Bendigo before settling down in Beechworth as a wine and spirits merchant. He married Ann Martindale on 17th December 1853 at St James Cathedral, Melbourne and between them they had three sons and five daughters. Kerferd began his political and legal career in Beechworth when he was first elected to the Municipal Council in May 1857. Later he would be elected to the Legislative Assembly for the Ovens District in November 1864, and continued to represent the area until February 1886. The postcard holds Historic significance due to its connection to Beechworth and its Lake Kerford. It demonstrates the interactions between nature and colonialists, especially how the lake has somewhat been 'protected' with the man made fencing. It also presents information on the environmental development or degradation for the area, with possible changes to the environment that may have been caused by human physical forces, natural decay or Global Warming.Sepia rectangular postcard printed on paper.Obverse: The Rose Series P. 10542 / Copyright / Evening lights, Lake Kerferd, Beechworth, VIC Reverse: Farley / Published by the Rose Stereograph Co., / Armadale Victoria. / 84-132-1 / Post card / The "Rose" Series De Luxe / A Real Photograph Produced in Australia / BMM299 lake kerferd, beechworth, water scheme, water reserve, reservoir, legislative assembly, hon. george briscoe kerferd, catchments, beechworth water reserve, beechworth catchments, municipal council, st. james cathedral, lakes, reserve, water supply, political projects, rose series, postcard, rose series stereograph -
The Beechworth Burke Museum
Photograph, 1960s
Taken around 1960s, this photograph shows the banks of Lake Sambell. Lake Sambell is named after Mr. L. H. Sambell who was instrumental in the lake's formation. Lake Sambell is the original site of the open sluice operation of Rocky Mountain Mining Company in the 1800s and the early 1900s. In the early 1920s, it was reconstructed as a recreational lake and was formally opened to public on 6 October 1928. The opening event was attended by townspeople and Beechworth's Minister of Lands Mr. Bailey. In the late 1930s to early 1940s, Lake Sambell redeveloped. The first development aimed to raise the banks by six feet to double its present area and to make the water cleaner. Another redevelopment in the 1940s was made possible by the Beechworth and District Progress Association. It involved raising the banks to five feet to provide swimming facilities, paddling pool and caravan park. This photograph holds Historic significance because of its connection to the development of Beechworth district.Sepia rectangular photograph printed on matte photographic paperObverse: Reverse: 3533 /beechworth, water scheme, water reserve, catchments, beechworth water reserve, beechworth catchments, municipal council, lakes, reserve, water supply, political projects, environmental changes, mr. l. h. sambell, sambell, rocky mountain mining company, recreational lake, minister of lands, mr. bailey, swimming pool, paddling pool, caravan park, swimming facilities, lake redevelopment, funding -
The Beechworth Burke Museum
Photograph, 1960s
This photograph was taken in the 1960s at Lake Sambell and is a view across the lake from the east side, the photo was taken during a period of improvements to the lake and surrounding area. Lake Sambell is an artificial lake that was created on the site of the old Rocky Mountain Mining Company workings and was officially opened by Minister for Lands, Mr Baily, on October 5, 1928. The disused and unattractive remains of the mine were converted into a recreational area intended for swimming, boating, and fishing. The lake is named after Mr L.H. Sambell, shire engineer and secretary of the Forward Beechworth Committee, who advocated for the enhancement of Beechworth into a tourist destination and was central to the planning and establishment of the lake. Funding for the project was raised through both competition funds and donations. Since the construction in 1928 several engineering issues have arisen. In 1939 the water levels were low, and the lake was considered both an eyesore and ‘mudhole’, Beechworth Shire Council sort funding to raise the height of the lake six feet to improve the quality of water. Throughout the 1940s the Beechworth Swimming Club sort to address the structural engineering issues and improve swimming facilities at the lake. R.E. Carter, similar to L.H. Sambell, was a shire engineer who advocated the importance of positioning Beechworth as a tourist destination. Carter held the position of shire engineer from 1954-63 and organised many improvements to the Lake Sambell area including the caravan park in 1959, the lake swimming pool in 1961, water skiing and boating facilities, and increased the lake surface area in 1964. These improvements to the lake also reflect an increase in leisure time and access to travel during a period of post-war prosperity in Australia during the 1950s and 60s. This photograph is of historical significance as it documents Lake Sambell in the 1960s after a series of enhancements to the lake area to improve its appearance and usability for both the people of Beechworth and tourists. It is also of social significance in providing an insight into the increase in leisure time and access to travel during a period of post-war prosperity. Black and white rectangle photograph printed on photographic paper and unmounted.Reverse: 3534 C798lake sambell, l.h. sambell, r.e. carter, rocky mountain mining company, forward beechworth committee, beechworth swimming club, wallace park lake sambell development scheme, lake sambell caravan park, beechworth 1960s, lake sambell swimming pool, lake sambell boating, lake sambell fishing, swimming, boating, water skiing, fishing, post-war prosperity, minister of lands, artificial lake, open cut sluice mine, lake -
The Beechworth Burke Museum
Photograph, 1920
Taken in 1920, depicted are four people in a rowing boat on Lake Sambell, Beechworth. From left to right, it is believed that the names of the people are Eric Beard, Mrs Doris Beard, and S/L to Bert Beard. The last two figures are unknown. Lake Sambell is a beautiful Victorian recreation lake and urban park with a unique history. It was created in the mid-1800s by the Rocky Mountain Mining company during the gold rush era and used as a mining site until the early 1900s, which brought Europeans into the area. It was turned into a reserve for residents in 1920 and is considered an icon of Beechworth as it represents the development of the community, human endeavour, and the spirit of the landscape.This photograph represents the community's social use of the lake in 1920.Black and white rectangular photograph print on paper.Reverse: LAKE SAMBELL/ c 1920/ from LTOR/ 1 ERIC? - BERT'S SON/ 2 MRS DORIS BEARD/ 3 S/L TO BERT BEARD/ 4 #beechworth, lake sambell, lake sambell boating, beechworth lake, social, 1920, victoria -
The Beechworth Burke Museum
Geological specimen - Actionlite and Pyrite
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 -
The Beechworth Burke Museum
Geological specimen - Amazonite, unknown
Amazonite is classed as a Tectosilicate and is part of the Feldspar group of minerals. Amazonite forms in a triclinic crystal structure and its chemical formula is K(AlSi3O8). In appearance, Amazonite can range from shades of green to green blue to blue, and often with white streaks or veining. The greenish colour is believed to come from the small amount of lead contained in its composition. Amazonite is named after the Amazon River due to its colour and similarities to another rock found along the riverbanks, although Amazonite is not actually found at or near the Amazon. Although less commonly used in jewellery today, Amazonite has been mined and used by humans for thousands of years and Amazonite jewellery from at least 2000BCE have been discovered in North Africa. Amazonite is found in many locations around the world including Brazil, Peru, Ethiopia, Canada, Russia, Mozambique, Myanmar, Pakistan, China, Madagascar, and the United States of America. This specimen most probably comes from the U.S.A., Amazonite is found in several US states particularly in Colorado, Virginia, Pennsylvania. This specimen is of both scientific and historic significance as a striking blue green example of Amazonite mined prior to 1868 in the United States of America, most likely from Colorado, Virginia, or Pennsylvania. These three states are all locations of significant Amazonite deposits. 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 palm-sized Feldspar mineral specimen from the Tectosilicate class in shades of blue-green with white veining.Existing label: green/blue Feldspar / "amazonite" / possibly USA geological specimen, geology, geology collection, burke museum, beechworth, tectosilicate, amazonite, feldspar, triclinic crystal structure, amazonite usa, amazonite colorado, amazonite virginia, amazonite pennsylvania -
The Beechworth Burke Museum
Geological specimen - Anthracite crystal, Unknown
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 -
The Beechworth Burke Museum
Geological specimen - Greenstone, Hokitika Jade Company, unknown
New Zealand Greenstone, also called Pounamu is found on New Zealand’s South Island in riverbeds and boulders, and colours vary depending on the source, but always include green tones. It is a form of the mineral nephrite, also known as jade, and is a tough stone with a crystalline structure, made up of calcium magnesium and iron silicate. Its hardness means it is ideal for carving, and has been used for this purpose throughout history, especially by the Maori people of New Zealand. Greenstone features heavily in Maori mythology, and the traditional name for the South Island, Te-Wai-Pounamu, literally translates to waters of greenstone. Wearing of Greenstone pendants with different carvings is practiced by Maori to represent connection to land and ancestors, or to endow the wearer with certain attributes. The sticker on the base of the specimen identifies it as a product of Hokitika Jade Company. The company, which was active in the 1970s, sold jade and greenstone specimens and ornaments. Hokitika, which started life as an 1860s gold rush town, is the origin of most nephrite found in New Zealand, and the centre of the Greenstone carving industry. The object has scientific and research potential as part of the Burke Museum's Geology Collection, and as and example of New Zealand Greenstone. It also has spiritual significance for it's role in Maori beliefs and communities, where it is both traditionally worn and features in mythology. As a valuable stone regularly used in carving and jewellery, it has aesthetic significance. Sticker on base: "N.Z. Greenstone/ a product of/ Hokitika Jade Coy."geological specimen, geology, geology collection, burke museum, beechworth, new zealand, greenstone, hokitika, nephrite, jade -
The Beechworth Burke Museum
Geological specimen - Selwynite, Unknown
Selwynite is a fine-grained, compact green rock made primarily of chromian muscovite (fuchsite) and diaspore. Corundum and fuchsite can occur together in the form of massive aggregates or nodules. Often, copper carbonates are found as earthy films or tiny crystals in joint planes. The mineral name honours the late A. R. C. Selwyn, founding Director of the Geological Survey of Victoria. The particular specimen, a mottled green stone suitable for carving was recovered and found in Heathcote, Victoria, Australia. The rarity and qualities of this mineral attracted commercial mining, which was not successful, but traces of the mine shafts still exist today, and it is still highly valued by mineral collectors.Selwynit is considered to be one of the rare forms of rock because it is composed of phosphate minerals containing zirconium. This is an extremely rare combination found in nature. 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 fine grained rock composed of mainly of chromian muscovite (fuchsite) diaspore and corundum.geological specimen, geology, geology collection, burke museum, beechworth, mineralogy, heathcote, mineral collectors, selwynite, green rock, rock specimen -
The Beechworth Burke Museum
Geological specimen - Marble, Unknown
A granular metamorphic rock, marble is derived from limestone or dolomite and composed of calcite or dolomite interlocking grains. Heat and pressure from overlying sediments form it from limestone buried deep in Earth's crust. Graphite, pyrite, quartz, mica, and iron oxides can affect rock texture and colour. This specimen was found in Carrara, Italy. Carrara marble is the most common marble found in Italy, and it gets its name from the region where it is located. The marble was also called Luna marble and was used as a decorative element in buildings and sculptures. It has been quarried since Roman times in the Lunigiana, the northernmost tip of Tuscany, just outside the city of Carrara in the province of Massa and Carrara.Marble is one of the most popular and expensive rocks used in sculpture, architecture, interior decorations, statues, table tops, and novelties. It is available in various colors and textures depending on the chemical composition. The strength of the rock and its ability to hold finer details have made it a favorite among designers. 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 Marble (metamorphic rock) predominantly white with specks light grey and ochre geological specimen, geology, geology collection, burke museum, beechworth, marble, carrara marble, italian marble, marble specimen, tuscany -
The Beechworth Burke Museum
Photograph - Lantern Slide, c1900
This picture shows an angle of Beechworth Primary School (State School number 1560) which is also pictured in the building's entry in the Victorian Heritage Register (VHR record 1718). The school began as a national school in 1858 as an alternative to Wesleyan and Anglican schools already operating in the area. Its name was changed to Common School number 36 in 1862 and the Beechworth Academy prior to being taken over by the Education department in 1873. The new premises were built in 1875 utilising the skills of architect Henry Bastow though the original design may be attributable to the firm Wharton and Vickers. The design was used with modifications for other schools in Victoria, including the Competition School in Errol Street, North Melbourne. The school moved to the building pictured from its original premises in Loch Street, designed by Thomas Dalziel, which later became the office of the Ovens Advertiser. The school was opened on 2 July 1875 by former Beechworth resident G.B. Kerferd, who was then the Premier of Victoria. The image shows approximately ninety older students at the school in approximately 1900. There are approximately equal numbers of boys and girls pictured, with most of the individuals pictured appearing to be between the ages of twelve and fifteen. Although the school had more than 1000 students enrolled at its height, enrolments had declined to 304 in 1890. Also visible is a fringe of sequoia pines which were planted by the school children as a project lasting through to the late 1930s. Lantern slides, sometimes called 'magic lantern' slides, are glass plates on which an image has been secured for the purpose of projection. Glass slides were etched or hand-painted for this purpose from the Eighteenth Century but the process became more popular and accessible to the public with the development of photographic-emulsion slides used with a 'Magic Lantern' device in the mid-Nineteenth Century. Photographic lantern slides comprise a double-negative emulsion layer (forming a positive image) between thin glass plates that are bound together. A number of processes existed to form and bind the emulsion layer to the base plate, including the albumen, wet plate collodion, gelatine dry plate and woodburytype techniques. Lantern slides and magic lantern technologies are seen as foundational precursors to the development of modern photography and film-making techniques.The image is significant because it sheds light on the educational infrastructure present in Beechworth in the early part of the Twentieth Century, including the prevalence of education for students after current-day primary-school age and the education of girls. It also provides insight into the building and design practices used by Government departments at the time. Thin translucent sheet of glass with a circular image printed on the front and framed in a black backing. It is held together by metals strips to secure the edges of the slide.Obverse: L / burke museum, beechworth, lantern slide, slide, glass slide, plate, burke museum collection, photograph, monochrome, schools, education, high school, primary school, common school, state school, state school 1560, common school 36, beechworth academy, g.b. kerferd, thomas dalziel, henry bastow, victorian heritage register, beechworth primary school, girls education, boys education, public schools, education department, pines, trees, sequoias, competition school -
The Beechworth Burke Museum
Geological specimen - Cerussite, Unknown c.1890s
... The Beechworth Burke Museum Loch Street Beechworth high ...Named in 1845 by Wilhelm Karl von Haidinger cerussite takes its name from the Latin cerussa, meaning 'white lead'. When viewed under certain lighting conditions cerussite gives of fire and rainbow-like colours (due to its high dispersion) and it is quite sought after by geological collectors for this very reason. Cerussite is usually found in the oxidised zone of lead ore deposits. It is a very common weathering product of galena and other lead ore minerals. It is a secondary mineral, meaning it forms as a result of the alteration of pre-existing minerals in the Earth’s crust. The presence of lead in cerussite makes it potentially toxic. Historically, it has been an important source of lead, which has numerous industrial applications, including in batteries, construction materials, and radiation shielding. Cerussite has a crystal structure that belongs to the orthorhombic crystal system. Its crystal structure is characterized by a three-dimensional arrangement of atoms in a repeating pattern. The crystal lattice of cerussite consists of interconnected lead (Pb) and carbonate (CO3) ions. This crystal structure is visible in the specimen. This specimen was found in Dundas (formerly Mount Dundas), a historical mining locality, mineral field and railway located on the western foothills of the West Coast Range in Western Tasmania. During the 1890s Dundas swelled in numbers however it is now lost in a temperate rainforest and its population is now 2. The present Dundas Extended mine, about 1.5 km east of Dundas is presently worked for specimen material.Faceted cerussite gems are considered rare and valuable, given the softness of the mineral. This item is not a faceted gem however its historical and scientific research potential give it significance; mined in an Australian township, this cerussite could shed light on the now lost history of Dundas and the mining that occurred there. Additionally, the uses of this mineral in historical industrial processes give it scientific significance. Such knowledge can add to understandings of the geographical and geological nature of Western Tasmania and allow for further study of Australian geological specimens. A small lead carbonite mineral with shades of cream, white and brown throughout, flaky shards of white at base. CERUSSITE / (lead carbonite) / Locality: Dundas, W. Tasmaniadundas, tasmania, cerussite, lead, orthorhombic, geology, minerals, mining -
The Beechworth Burke Museum
Accessory - Chatelaine, C. 1890
The exact creation date of this chatelaine is unknown, however the hallmarks and engravings on some of the attached objects indicate that this chatelaine was made in the late 1890s. The shark tooth and the liberty bell attached to the chatelaine suggest that the item once belonged to an Australian who had connections to America. The compact, scent bottle lid, and feminine design of the other objects suggest that this wasowned by a woman. The name on the plate indicates that this object may have belonged to someone with the surname Heine. The hallmarks on the scent bottle lid and the compact indicate that they were made in Birmingham, England in the late 1890s, and that the compact was made by H. Matthews. Chatelaines where used by both men and women, usually fastened to a belt or pocket, and small household objects were attached to the main body of the chatelaine by chains. They were only worn by the heads of the household as a display of position and power.The social history objects held in the Burke Museum's collection help to tell the stories of Beechworth's past by showing the social, cultural, and economic aspects of the town's history.A decorative silver belt hook with small household object attached by chains to a suspended name plate. There are 8 chains and 7 objects; a vesta case, scent bottle lid, compact, shark tooth, bell, button hook handle, container.HEINE/ [plate] CHERRY./ from/ LEO/ May 12th 1899/ [inscription on vesta case] L??S/ Anchor symbol/ x symbol/ lion symbol/ [Hallmark on scent bottle lid] R/ HM/ Anchor symbol/ Lion symbol/ m symbol/ [Hallmark on back of the compact] SYDNEY/ [inscription on shark tooth] Proclaim liberty throughout all the land unto all inhabitants thereof/ By order of the Assembly of the Province of Pensylvania for the State House in Philada/ [inscription on bell] A01176/ burke museum, silverware, social history, heine -
The Beechworth Burke Museum
Functional object - Vesta Case, Unknown
This detailed example of a match holding Vesta was owned by someone with the initials GBW but is otherwise difficult to identify ownership. Vestas are the historical name for what are now known as matches. They were named for the Roman goddess Vesta whose domain was the hearth and home. The Swan company began production of short matches, mostly useful for lighting pipes and cigarettes due to their deliberately short length. Due to their small size it became convenient to carry these Vestas within a Vesta Case kept somewhere on the person, large enough to contain enough matches for a days use. The cases prevented their contents from becoming damaged and damp while also stopping them from accidentally striking if held loose in a pocket. This example of a Vesta case is particularly ornate.The social history objects held in the Burke Museum's collection help to tell the stories of Beechworth's past by showing the social, cultural, and economic aspects of the town's history.A decorative silver coloured vesta or match book. It has detailed engraving across the obverse and reverse sides with delicate scrollwork and a monogram set in a circular setting in the centre. The vesta has a hinged top and side loop to allow for attachment.GBW/ A01171/burke museum, vesta case, vesta, matches, silver, social history, luxury -
The Beechworth Burke Museum
Functional object - Vesta Case, Unknown
Vestas are the historical name for what are now known as matches. They were named for the Roman goddess Vesta whose domain was the hearth and home. The Swan company began production of short matches, mostly useful for lighting pipes and cigarettes due to their deliberately short length. Due to their small size it became convenient to carry these Vestas within a Vesta Case kept somewhere on the person, large enough to contain enough matches for a days use. The cases prevented their contents from becoming damaged and damp while also stopping them from accidentally striking if held loose in a pocket. This is a simple example of a Vesta Case.The social history objects held in the Burke Museum's collection help to tell the stories of Beechworth's past by showing the social, cultural, and economic aspects of the town's history.A decorative silver coloured vesta or match book. It has a raised crosshatch pattern in a circular pattern on the obverse side. The vesta has a hinged top and side loop to allow for attachment.A01199/burke museum, vesta case, vesta, matches, silver, social history