VSTA news article about the all girl rock group from Williamstown High School, touring the western District in 1988. Photocopy of original article.williamstown high school, music, 1987, rock groups, all girl band

Family Groups on rock face (possibly Grampians) Picnic at Concongella, In foreground Papa (J H) & Gran Rathgeber (Sarah Anne)

The low rolling hills of the Kimbolton countryside consist of ancient, hard and fractured Ordovician rock up to 65 million years old, which was originally deposited deep under the sea. Rocks mainly are sandstone, mudstone, black shale and quartz conglomerates. Marine fossils can be found in the area. Around seven million years ago a basalt flow buried the original bedrock along the along the Campaspe River. Ongoing weathering, wind and water movement over the following years has produced younger clay, sand, silt and gravel deposits throughout the area. Patches of White Hills Gravel are also found in the area. Another unique geological feature of this area is the Permian Glacial Pavement rocks north and south of Eppalock and glacial sediments (such as “Dunn’s Rock” and “Kellams Rock”). During the ice age (up to 280 million years ago) large glaciers moving over the countryside, scoured out sediments, pulverized bedrock, polished and cut grooves into bedrock in the direction of ice movement. When the ice melted boulders etc where left behind in areas of entirely different rock types, such as a 100 Tonne granite block known as ‘The Stranger’ near Derrinal. Dunn's Rock (Glaciated Pavement) Eppalock - Photos of the rock and a field group collecting date with Lake Eppalock (Knowsley) in the backgroundhistory, bendigo, dunn's rock eppalock, kimbolton forest, lake eppalock, gately collection

Series of Black & White Photos Total 4 depicting post war life for the Hill Family & Friends. The Hayes' Family Buick, 4 occupants and two men standing on offside of vehicle, two men in front seat are wearing dark suits and hats, two ladies in rear seat wear dark clothing, one has a hat, man standing beside the car in dark suit white shirt and black tie, other man nearer the back is wearing a grey suit, wooden cross in background near rear of vehicle, trellis fence left background, short white picket fence right background, 'Durvol'. This photo has two men in the front seat, both wearing grey suits white shirts and black ties, driver only wears a hat, in the rear seat are two ladies wearing dark clothing, one wears a hat, and a male wearing a dark suit white shirt and dark tie, Note anti kick guards below each door. At Hanging Rock family group, three gentlemen one lady and two young girls, standing next to a road bridge with wooden railings, two males are dressed in dark suits white shirts and dark ties, one wears a hat, man sitting on bridge rail wears a grey suit white shirt and dark tie, the two young girls are wearing light coloured clothing. Martin, Jack, Tom & Dolly the Horse, three boys wearing dark clothing, two boys are wearing white shirts and dark ties, Dolly is dark coloured, background shows gable roofed house with one chimney, end of veranda , large tree left background, wooden paling fence, 'Durvol' property Kyneton 1923.Hilda Hill Pesdonal Collectionaustralia, history, post war life

This particular geological specimen was found in Mount Franklin or Lalgambook in Djadjawurrung, located between Daylesford and Newstead, approximately ninety minutes drive from Melbourne. The mountain is an example of a breached scoria cone (a steep conical hill of loose pyroclastic fragments) which was created by a volcanic eruption about 470,000 years ago, a date which may indicate the age of this geological specimen. The volcanic eruptions of Mount Franklin were most likely witnessed by members of the Dja Dja Wurrung Aboriginal tribe, who referred to this country as the 'smoking grounds'. Mount Franklin and the surrounding area appears to have been a place of considerable religious significance to Aboriginal people, there is evidence which indicates that frequent large ceremonial gatherings took place in the area. Basalt is the most common rock on Earth’s surface, more than 90% of all volcanic rock on Earth is basalt. Basalt is an aphanitic extrusive igneous rock formed from the rapid cooling of low-viscosity lava exposed at or very near the surface of a rocky planet or moon. Specimens are black in colour and weather to dark green or brown. Basalt is rich in iron and magnesium and is mainly composed of olivine, pyroxene, and plagioclase. Olivine is the name of a group of rock-forming silicate minerals with compositions ranging between Mg2SiO4 and Fe2SiO4. Unlike other minerals, Olivine has a very high crystallisation temperature which makes it the first of the minerals to crystallise from magma. As magma cools, the crystals begin to form and settle on the bottom of the lava and form basalts that are abnormally enriched in olivine in the lower part of lava flows. According to H. M. King (on geology.com) "Olivine is thought to be an important mineral in Earth's mantle. Its presence as a mantle mineral has been inferred by a change in the behaviour of seismic waves as they cross the boundary between Earth's crust and mantle". Lava from Mount Franklin and other volcanoes in the area filled valleys and buried the gold bearing streams that became the renowned ‘deep leads’ of the gold mining era. In 1852, as part of the Victorian gold rush, gold was discovered in the immediate area, this gold was created by lava flows during the Newer Volcanic period, which were mined intensively during the nineteenth century. Around 1865 the presence of a deep lead in Mount Franklin was established. Deep lead mining was initially unsuccessful, and it was not until the late 1870s that the Franklinford Gold Mining Company mined at Mount Franklin on a significant scale. A few years later the Mount Franklin Estate Gold Mining Company also struck gold, followed by the Shakespeare and Great Western companies in the mid-1880s. By the late 1880s, however, deep lead mining had ceased in the area. Soon after gold was discovered in 1851, Victoria’s Governor La Trobe wrote to the Colonial Office in London, urging ‘the propriety of selecting and appointing as Mineral Surveyor for this Colony a gentleman possessed of the requisite qualifications and acquaintance with geological science and phenomena’. Alfred Selwyn was appointed geological surveyor in Australia in 1852 which began the Geological Survey of Victoria. In 1853-69 the Geological Survey issued under Selwyn's direction sixty-one geological maps and numerous reports; they were of such high standard that a writer in the Quarterly Journal of the Geological Society of London bracketed the survey with that of the United States of America as the best in the world. During his years spent in Australia, Selwyn collected numerous significant geological specimens, examples of which are held in collections such as the Burke Museum.This geological specimen is an example of basalt and olivine which shows the volcanic lava activity and geographical specific nature of Mt Franklin as a significant volcanic site. According to Agriculture Victoria 'The crater is one of the deepest in the Central Highlands area. It is a major megacryst site with some of the largest known Victorian examples of megacrysts of augite and an orthoclase. The small parasitic mound of Lady Franklin on the western flanks adds to the geological interest of the site'. This specimen also highlights the locality as a significant place for both indigenous activity and Victorian gold rush era mining practices. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.An angular, solid hand-sized piece of grey volcanic Basalt with green/brown Olivine phenocrysts along one flat edge.Olivine in basalt / - label is probably / correct. / C. Willman / 15/4/21burke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, mineralogy, basalt, igneous rock, igneous-volcanic, volcanic geology, volcanic, olivine, olivine specimen, basaltoid

This is a program of a concert organized by the Soldiers’ Christmas Comforts Group and the Red Cross in Warrnambool to raise funds for the soldiers on active service in World War One. The concert was held in the Warrnambool Town Hall in September 1916 and featured a Melbourne artist, Horace Wood, who gave several violin solos and the local Warrnambool orchestra of Miss Gertrude Rooney. The Rooneys were early settlers in the Dennington area and had the property, ‘White Rock’ in Dennington and a produce store in Warrnambool. Miss Gertrude Rooney was an accomplished musician and was prominent in musical circles in Warrnambool during the first half of the 20th century. This program is of interest as an example of the fund raising activities in Warrnambool during World War One and of the type of entertainment offered at concerts at that time. There are many well-known names listed among the orchestra members at the back of the program. This is a sheet of buff-coloured paper folded in two to make four pages. The front page has an ornate red edging and there is dark blue printing on the front and back pages. The front page has a large Red Cross emblem The inside two pages have the printed program of concert items in black print. There are also advertisements for local Warrnambool businesses. The edges of the program are torn and ragged. world war one, warrnambool in world war one, gertrude rooney, musical entertainments in early 20th century, warrnambool

The Grinton Collection. Children in Scotland. Refer Cat No. 1280 for Jack Grintons service details.Photograph framed. Photograph - black and white photograph on paper depicting seven children standing and sitting near or on a low rock wall. On left one child holding a bicycle, on right a child standing on stilts. Background - trees and buildings. Frame - timber, light varnish finish, Perspex front, cardboard backing."Group 3: Trip of a lifetime". "K. Children - Scotland". framed accessories, camera on the somme, ww1, 38th bn, grinton, scotland

This stone Grinder or pounder was used as part of an indigenous grinding food preparation method, by the original inhabitants of the Kiewa Valley and its region. In conjunction with its grinding stone was used not only to grind seeds and but also to dig up eatable roots and leaves and served with the regions Bogong moth. This method of food preparation has survived in its basic form for centuries and is still used by master chiefs in modern eateries. This item has been registered with Aboriginal Affairs in Wangaratta, Victoria. Dhudhuroa elder Alan Murray has examined this tool, in Feb 2015, and said it was also used for sharpening axe heads as well as pounding food items. This item has a very significant historical and social aspect to it. Firstly it demonstrates the division of labour within a indigenous tribe. It was an era when the female had a definitive role within the family and the broader social indigenous tribal group of, gathering and preparing non animal(hunted) food. Hunted food was the domain of the initiated males of the tribe.Secondly it demonstrates the ability to fashion implements from raw materials(rock) into effective tools for the purpose of preparing a meal for human consumption. This was in an era where inter family and intra family participation in an indigenous tribal social protective environment was at a very high level. The Kiewa Valley/Mount Bogong region was an area where annual "get together" indigenous tribes for feasting, bartering and settling of disputes highlighting the importance of a regional gathering. Grooved stone, carved to a cylindrical shape with a relative pointed end tip one side (grinding or pounding end) and a rough other end (holding end} Made from Rhyolite stoneThere is a worn grove in the top side due to this tool being used for axe sharpening. indigenous, aboriginal, stone grinding, meal preparation, natural environment, pounding stone

.7) Back row, Len STEVENS, Len TRIPP, Charles WOODWARD - ? 1st row, Les WARREN - ? Leonard Jordan TRIPP VX25096 2/24 BATT A.I.F K.I.A Alamein 24/10/42 Refer Cat No 205P for Len Tripps full service details..1) Photo, B&W on steel frame, photo surrounded by yellow edging, photo has plastic covering. Photo re L.J. TRIPP. .2) - .4) Photos, sepia colour, potrait re L.J. TRIPP. .5) Photo, B&W, shows group of 8 soldiers in Tin Hats and webbing. .6) Photo, B&W, shows group of 7 soldiers standing by a large rock. .7) Postcard photo, B&W, shows group of 6 soldiers outside a tent. .8) Postcard, cartoon B&W, with central inset photo of L.J. TRIPP..2) - .4) "Seymour 14.9.40" .7) "Merry Xmas & Happy New Year"photography-photographs, documents - postcards, military history

Inspected by Joanna Freslov, archaeologist 2.6.22008. Grinding stones are slabs of stone that Aboriginal people used to grind and crush different materials. Bulbs, berries, seeds, insects and many other things were ground between a large lower stone and a smaller upper stone. This is the lower stone.Large grinding stones such as this one were designed to be left at a camp site for use the next time the group moved there. Smaller grinding stones were carried between sites. Grinding stones were not abandoned when they became worn and smooth through use. The stone would simply be roughened again so it was once again suitable for its function. This is an example of a food preparation utensil used by the Early Indigenous people of Eastern Australia.A large flat rock with grind hole in top. Rock has split. gridstone aboriginal stone-artefact

Vassilieff dynamited rock from his own property to build his house. Stonygrad is reminiscent of a grotto and in parts, of a sculpture. Covered under Heritage Overlay, Nillumbik Planning Scheme. Published: Nillumbik Now and Then /​ Marguerite Marshall 2008; photographs Alan King with Marguerite Marshall.; p135 Stonygrad, the home built by Expressionist painter and sculptor Danila Vassilieff, is reminiscent of a grotto and in parts, of a sculpture. Vassilieff, who amongst others influenced painter Sydney Nolan and Albert Tucker, was a member of the artists group the Angry Penguins. He was also a highly regarded art teacher at the nearby Koornong Experimental School and taught at Eltham High School. Art critic Robert Hughes described Vassilieff’s painting as ‘lyrical without social commentary’, and said Vassilieff was ‘the most oddly neglected artist in recent Australian History’. Vassilieff, who was born in 1897 in Russia, had an unusually adventurous life before he settled in Warrandyte. The 12th of 18 children, he lived on a farm in the Don Basin. Vassilieff trained with the Imperial Military Academy at St Petersburg and fought in World War One as an officer in the White Russian Army against the communists. In 1920 he was captured, then escaped from prison, stole a horse and rode bareback 150 miles to the Black Sea, helped at first by Tartar freebooters. He then travelled to India, Shanghai and arrived in Queensland as a refugee in 1923 where he began painting. He and his wife Anisia bought a sugar farm near Ingram, and later he constructed railway lines at Mataranka, in the Northern Territory.4 In 1929 Vassilieff went to Brazil for formal art training from former fellow-officer Dmitri Ismailovich, but he soon left to travel up the Amazon River. He then worked as a sidewalk artist in the West Indies and travelled for two years in England, France and Spain. In 1937 he arrived in Melbourne where he lived until his death in 1958. His first major Australian series was the Carlton streetscapes and from 1951 he sculpted in local hard limestone. Vassilieff rejected all dogma and regarded religious subjects as suitable only for decorative arts. In 1944 he helped defeat a communist attempt to take over the Contemporary Art Society. For a short time, from around 1955, Vassilieff taught at various Victorian schools. The Angry Penguins painted mainly between 1937 and 1947, and included Arthur Boyd, Albert Tucker, Sidney Nolan and Joy Hester. The group formed as they felt isolated from European thought and art (including Surrealism) from which their work was derived. They were also angry at what they considered to be the complacency and insularity of their society. They maintained Australians at first were scarcely aware of the threats of the Wall Street Crash and Hitler and were little interested in the Spanish Civil War. The Angry Penguins also objected to the White Australia Policy. Hughes said although most of the Melbourne Expressionists in the 1940s were unskilled and their work crude in style, they helped jolt Australian painting from its pastoral complacency. Their style influenced nearly every painting produced by significant figurative artists in Melbourne in the 1950s such as Charles Blackman. From 1939 Vassilieff built Stonygrad, mainly with local stone. The house stands at the end of a private road surrounded by trees with the quiet occasionally broken by the sounds of bellbirds. To build his house Vassilieff dynamited rock and cut trees from his own property. The original section of the three-level house is of irregular-shaped pieces of solid stone, exposed inside like the exterior. Vassilieff later built sections with timber and brick. Inside is rustic and cave-like, and several rooms are linked by arched openings with no doors. One undulating wall was carved out of rock from which two sculptured heads protrude. Several ceilings are of rough-hewn logs and the built-in table and bookcase are rough, as is a timber ladder leading to a bedroom. Not for the elderly or unsteady! Yet the general impression in the muted light is beautiful, with artistic originality.This collection of almost 130 photos about places and people within the Shire of Nillumbik, an urban and rural municipality in Melbourne's north, contributes to an understanding of the history of the Shire. Published in 2008 immediately prior to the Black Saturday bushfires of February 7, 2009, it documents sites that were impacted, and in some cases destroyed by the fires. It includes photographs taken especially for the publication, creating a unique time capsule representing the Shire in the early 21st century. It remains the most recent comprehenesive publication devoted to the Shire's history connecting local residents to the past. nillumbik now and then (marshall-king) collection, danila vassilieff, hamilton road, north warrandyte, stonygrad

Two bronze commemorative plaques on rocks, unveiled by Wurundjeri Tribe Council Elders, mark two eastern boundaries of the former Warrandyte Aboriginal Reserve on the north and south sides of the Yarra. This project was initiated by Nillumbik Reconciliation Group in close association with Reconciliation Manningham and the Wurundjeri Tribe Council, as a means of commemorating the last great corroboree of the Kulin Nation which was held at Pound Bend in March 1852. This plaque is on the Nillumbuk side of the Yarra, accessed via The Boulevard, North Warrandyte. The plaque is set on a rock approximately 50 metres before the turning circle at the end of The Boulevard. Plaque : Warrandyte Aboriginal Reserve This commemorative rock marks an eastern boundary of the former Warrandyte Aboriginal Reserve established in 1852. Centred on Pound Bend, it covered 1,908 acres on both sides of the Yarra River (Birrarung). That same year saw the last great gathering of the Kulin nation here in Wurundjeri country which was celebrated over two weeks with traditional performance and games. For a few years longer the reserve intermittently served as a ration station.With gold having been discovered at Warrandyte, the Wurundjeri were moved on again but ultimately secured a permanent home at Coranderrk, Healesville. A second commemorative plaque and rock is located on the opposite bank of the Yarra and its confluence with Stony Creek. Melway ref : 23 C 9 Unveiled by Wurundjeri Elder, Uncle Bill Nicholson on 23rd March 2013 Funded by the Robert Bridgford Indigenous Trust (Nillumbik Community Fund) with assistance from Manningham City Council Small Grants Program Ref: Monument Autralia https://monumentaustralia.org.au/themes/culture/indigenous/display/99680-warrandyte-aboriginal-reserve-fay bridge collection, 2016-11-07, aboriginal reserve, north warrandyte, plaques, warrandyte aboriginal reserve

Blue and white photocopy of photograph taken outside of group of fourteen men, in front of brick building with six sash windows. All men wear hats, some carry folded umbrellas, some wear frock coats, most wear three piece suits. Large rock in foreground. Rails on L background. At L background is shield with spats, and under 'one and all' ( Cornish Symbol). Mounted on white board.person, group, males

Copy of an article from the Bendigo Advertiser 1/9/1990 mentioning the Cornish influence on Victorian gold mining during the 1880's and 1890's. Also mentioned is population growth, rock drills and miner's phthisis.bendigo, history, long gully history group, the long gully history group - cornishmen brought their mining skills to bendigo, bendigo advertiser 1/9/1990, dr charles fahey, cornish association of bendigo and district, bendigo college of advanced education, george lansell, the mining exchange, beehive building, eaglehawk fire station, george ellis

Two hand written pages with year dates and what took place at that time. Dates range from 1852 to 1950's. 1950's - mining stopped in Long /G. 1926 - First Teachers training College established. Taylor Horsefields Engineering works - Horsefield a genius. Pioneered local production of compressed air driven roak-drills, specialized in rock bores and drills exported them throughout the world. Harvester - for f/ter in Harvest equipment. 1856 - Anglican School opened held church as well as school. Manchester Arms, Admiral Arms both has pretentious music halls attracted large crowds. 1862 - Ironbark, Long Gully sought annexation by the Municipality of Sandhurst. 1872 - Long Gully Fire Brigade was formed. Keen rivals. 1850 - recognised Chinese camp. ? Long Gully - due to the sinking deeper and the rewards generally richer, became the heart of 'Little Cornwall' - Cornish people. * Tent Church services held in 1862. Long Gully Mine opened April 1852. On the back of the first page is written - Mines - Reefs. mines mentioned are New Chum Hill, the New Chum and Victoria, The Victoria HIll Ironbark, The North Old Chum, Lansell's Big 180, Ballerstadt's Open-Cut, and the Victoria Quartz Mine.bendigo, history, long gully history group, the long gully history group - 1852 to 1950's, first teachers training college, taylor horsefields engineering works, anglican school, manchester arms, admiral arms, municipality of sandhurst, long gully fire brigade, chinese camp, little cornwell, long gully mine

black and white photograph of two workmen seated on bush timber fitted between vertical rock faces. The ladder is probably from the level immediately below. The lamps are ' Bendigo bucket carbide lamps ' Some advisers consider consider that this photograph is posed as workers are not safely placed. In grey lead ' miners at work ' down below' in Bendigo ' a signature ' J.J. Stanistreet ' a caption ' Hercules Mine ' ? On back in black pen ' miners shaping shaft prior to ' boxing in' with red gum slabs - note white quartz reef on wall face ' On small paper inclusion ' Miners placing staging for stoping on spurs' Mining Revival C 1930's.. James Lerk 26 Nov. 1999 - not as described in ink on rear 'person, group, mining

This photograph shows a piece of gold mining equipment identified as a mine winch, possibly an air winch cylinder of 1870s RG Ford's Patent design. Throughout the history of mining for gold and other precious materials, the windlass or winch (pictured) was used to bring up buckets full of soil from the bottom of a mine. This soil was then searched for gold/metals before being relocated to a different area. Due to the size and complexity of this particular piece of equipment, this winch may have been used to raise and lower mine carts to the entrance of the mine (often used in coal mining) and could have been used in raising cages up and down (acting as elevators) containing miners if the mine was particularly deep. The actual use of this particular item in the Beechworth locality is undocumented but these are some possibilities based on the use of these pieces of equipment in other mining locations. Mining can have a largely detrimental impact to the environment and therefore, the study of machinery like the one depicted in this photograph can help researches to reconstruct the methods and technologies used in the late 1800s and early 1900s. This particular item appears to have been removed from it's original site where it would have been used to assist with mining. It is possible that this photograph has been taken for recording purposes or as part of a machinery exhibition. Prior documentation records that this piece of equipment had connections to the Rocky Mountains Mining Company. Today, the Rocky Mountains Gold Mining company is famous in Beechworth for having been instrumental in the creation of the Rocky Mountain tunnel. Construction for this tunnel began in 1859 when a group of 12 men blasted a 400ft long tailrace though the rock beneath the town of Beechworth. Today, the 800ft tunnel, completed in 1871, is a popular tourist attraction but during the decades of gold mining, the purpose of this tunnel was to divert water away from the main sluicing operations so miners could better access gold and precious materials. The tunnel was used for this purpose for many years, later becoming useful for the Zwar Brother's tannery and currently as an outfall drain for Lake Sambell. This area continued to be mined until the early 1900s. The period when this item was in use is unclear but it is estimated to have been in the 1870s based on the design and appearance of the image. The gold works at the Rocky Mountain Tunnel closed in the early 1920s but the impact of mining remains in Beechworth today and therefore the study of photographs like this one which contain mining equipment can further understanding of mining in this region.This photograph has historic and research potential for study on the gold mining of the Beechworth region and types of equipment used to locate gold after the initial gold rush of 1853-1854 which resulted in the discovery of the surface gold and required miners to dig deeper to access precious metals. The clarity of the photo, and its good preserved condition, means it can continue to be used for research. This photo is part of a collection of six photos all within the Burke Museum Collection which depict mining equipment.Square black and white photograph on card.7793.1beechworth, mining, goldmining, goldmining equipment, beechworth burke museum

This image is a reproduction of an 1899 original depicting the 'Williams Good Luck Mine' on the Mopoke Reef (also called 'Morepork Gully') in the Dingle Ranges, approximately three miles from Beechworth. A large opening to a mine can be seen behind the men in the photograph, with a wheeled cart on a track leading to the men's position, where the soil and rocks have been hauled away. This photograph interestingly contains dogs alongside the miners. While dogs have been recorded as deterrents to thieves in the Victorian goldfields, these dogs appear as companions to these men. Following the discovery of gold at Beechworth in 1852, rushes quickly followed at surrounding creeks and gullies in the district. In the late nineteenth and early twentieth centuries, small syndicates of miners continued to work old or abandoned quartz reefs, often persisting without the assistance of heavy machinery to remove the large amounts of rock, in order to obtain yields at ever greater depths. The group of miners in this photograph are Mr. Roger Williams and Sons, who revived operations at the ‘Old Good Luck’ mine on the Mopoke Reef in the Dingle Range near Beechworth around 1892, working the site for more than two decades. An emigrant from Cornwall with experience in the tin mining industry, 19 year old Roger Williams senior sailed to New Zealand in 1840, then to Australia where he spent time in the Bendigo Gold Fields before settling in Beechworth in the early 1860s. Mr Williams senior worked on various mining activities in the district, including the Rocky Mountain Tunnel project. Conversant with the character of gold-bearing reefs in the area, the syndicate dug an eight hundred foot tunnel, digging down as far down as two hundred feet with little capital save their labour, to connect and provide better working access to the mass of reefs and veins in the vicinity. Progress was hampered by poor air quality charged with fumes from dynamite and large quantities of rock had to be crushed to obtain payable yields. The Victorian Goldfields are filled with ruins and remnants of the area's rich mining history, ranging from small alluvial diggings to the remains of huge mining companies. Site names often changed several times throughout the nineteenth and twentieth centuries. Some sites were abandoned and forgotten, others were worked continuously over many decades. The names of mines were often repeated at different locations throughout the Victorian Goldfields. For example, there is a Mopoke Gully heritage mine near Fryers Creek, Victoria. 'Mopoke' is a common onomatopoeic name for Morepork and Australian Boobook owls.This image has historical, social and research significance for patterns of emigration during of the Victorian Gold Rush, and the historical, social and environmental impacts of mining at Beechworth at the turn of the nineteenth and twentieth centuries. As gold became scarce and government support and large company investment waned, poor hard-working miners laboured intensively to make a living through periods of high unemployment. This image can be compared and studied alongside other historical mining photographs and objects in the Burke Museum Collection. It has potential to improve our understanding of miners working conditions and the shifting character of mining in the Beechworth district.Sepia coloured rectangular photograph printed on gloss photographic paper mounted on card. Obverse: Williams/ Good/ Luck Reverse: A02498/ 1997. 2498/ Good Luck/ Mine/ 1899/ Mopoke. burke museum, beechworth museum, beechworth, gold fields, gold rush, victorian gold rush, gold ming history, colonial australia, australian gold rushes, mining technology, beechworth historic district, indigo gold trail, migration, indigo shire, good luck gold mine, victorian goldfields, mining syndicates, gold fever, quartz-mining, small-scale mining, old good luck mine, mopoke gully, quartz reefs beechworth

This image is a reproduction of an 1899 original depicting the 'Williams Good Luck Mine' on the Mopoke Reef (also called 'Morepork Gully') in the Dingle Ranges, approximately three miles from Beechworth. The foreground of the image is littered with piles of smashed rock and detritus, known as ‘mullock’, beside a reinforced mine shaft, a vertical access passageway allowing miners to enter the mine and haul ore out using lifting technology such as a poppet heads, whims or windlasses. A group of miners and a dog appear close to an open-sided miner’s hut. Following the discovery of gold at Beechworth in 1852, rushes quickly followed at surrounding creeks and gullies in the district. In the late nineteenth and early twentieth centuries, small syndicates of miners continued to work old or abandoned quartz reefs, often persisting without the assistance of heavy machinery to remove the large amounts of rock, in order to obtain yields at ever greater depths. The group of miners in this photograph are Mr. Roger Williams and Sons, who revived operations at the ‘Old Good Luck’ mine on the Mopoke Reef in the Dingle Range near Beechworth around 1892, working the site for more than two decades. An emigrant from Cornwall with experience in the tin mining industry, 19 year old Roger Williams senior sailed to New Zealand in 1840, then to Australia where he spent time in the Bendigo Gold Fields before settling in Beechworth in the early 1860s. Mr Williams senior worked on various mining activities in the district, including the Rocky Mountain Tunnel project. Conversant with the character of gold-bearing reefs in the area, the syndicate dug an eight hundred foot tunnel, digging down as far down as two hundred feet with little capital save their labour, to connect and provide better working access to the mass of reefs and veins in the vicinity. Progress was hampered by poor air quality charged with fumes from dynamite and large quantities of rock had to be crushed to obtain payable yields. The Victorian Goldfields are filled with ruins and remnants of the area's rich mining history, ranging from small alluvial diggings to the remains of huge mining companies. Site names often changed several times throughout the nineteenth and twentieth centuries. Some sites were abandoned and forgotten, others were worked continuously over many decades. The names of mines were often repeated at different locations throughout the Victorian Goldfields. For example, there is a Mopoke Gully heritage mine near Fryers Creek, Victoria. 'Mopoke' is a common onomatopoeic name for Morepork and Australian Boobook owls.This image has historical, social and research significance for patterns of emigration during of the Victorian Gold Rush, and the historical, social and environmental impacts of mining at Beechworth at the turn of the nineteenth and twentieth centuries. As gold became scarce and government support and large company investment waned, poor hard-working miners laboured intensively to make a living through periods of high unemployment. This image can be compared and studied alongside other historical mining photographs and objects in the Burke Museum Collection. It has potential to improve our understanding of miners working conditions and the shifting character of mining in the Beechworth district.Sepia coloured rectangular photograph printed on gloss photographic paper mounted on card.Obverse: Reverse: A02497/ 1997.2497/ 'Good/ Luck/ Mine'/ Morepork/ Gully/ Mrs Joyce/ Bright/ Tunnel/ 800 ft/ 1899. burke museum, beechworth museum, beechworth, gold fields, gold rush, victorian gold rush, gold ming history, colonial australia, australian gold rushes, mining technology, beechworth historic district, indigo gold trail, migration, indigo shire, good luck gold mine, victorian goldfields, mining syndicates, gold fever, quartz-mining, small-scale mining, old good luck mine, mopoke gully, quartz reefs beechworth

This particular specimen was found in the Moorabool Slate quarries in Victoria. The Moorabool Slate quarries was established in the 1860’s by a company of Welshmen with a crew of six who purchased land by the riverside to mine for slate. Under the promise of adding to existing recourses the crew mined the slate which was used for paving and roofing. Slate is a fine-grained, low-grade metamorphic rock that is formed by the transformation of mudstone, shale or sometimes volcanic ash under low pressure and temperatures. It dark colour is due to carbonaceous material or to finely divided iron sulphide. It is believed that Evan Rowlands and Theophilus Williams of Ballarat were the first to discover the slate veins. Slate is a one of the most common natural stones in general use. Being used as paving, flooring, roofing and more. However, its history of being mined in Australia is not common as it is considered that the best places to mine slate is Spain and parts of the United Kingdom. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A somewhat rectangular foliated metamorphic rock composed of quartz, sericite and minerals from the chlorite group that make up the compounds of slate. The rock is dark grey almost black.Geological survey / R S / Loc Moorabool /Slate quarries / 1/4 sheet | 78 | Roofing Slate /burke museum, beechworth, geological, slate, metamorphic, slate (metamorphic), geological specimen, slate specimen, indigo shire

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

Feldspar, derived from the German word feldspat, is a group of minerals which is the most common mineral group found on Earth, making up more than half of the planet's crust. The major rock-forming minerals in the Feldspar group include albite, anorthite, orthoclase and microcline. (Mindat, Feldspar Group). Orthoclase is part of the Feldspar Group subgroup, Alkaline Feldspar, which are known to be poor in calcium, and mostly rich in potassium. It is further also considered to be a K Feldspar, a subgroup of Alkaline Feldspar that are Potassium-dominant with variable crystal symmetry and Al-Si ordering state. Orthoclase are most commonly Colorless to white, Greenish white, Grayish yellow, or Pale pink and transparent to translucent with slightly pearly cleavage. The mineral rates at a 6 on the Mohs Hardness Scale. (cannot be scratched with a knife, but scratches glass with difficulty). The stronger green colour of this particular specimen is distinctive to the Broken Hill region (where it was found), and due to a small amount of lead. (BB) Its qualities find it misidentified at times as as microcline variety amazonite. Broken Hill is one of the world’s richest lead-zinc-silver deposits. The huge, 300-million-tonne orebody was discovered in 1883 and the superb mineral specimens attract collectors from around the world. (Australian Museum, Minerals from Australia: Australian mining regions)While feldspar is not by any means rare, this particular specimen has qualities distinctive to the Broken Hill mining district, with these properties leading at times to the mineral's misidentification. This creates potential for further study and identification of these mineral deposits through methods such as microscopic twinning, or using the position of certain d values in XRD patterns to calculate the degree of disorder of a K-feldspar, as discussed on the Mindat website (Mindat.com, Orthoclase:About Orthoclase). 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 aluminosilicate mineral composition which is primarily pale green and blue-grey in colour with traces of beige and white throughout. Note: green plumbian orthoclase (aka green feldspar) is an indicator mineral for the Broken Hill style lead-zinc deposits.N/Abroken hill mine, geological specimen, minerology

This specimen is a native copper specimen that is metallic. Copper is typically found in the earth's crust and is often found alongside other metals such as gold, zinc, lead and silver which all belong to the same group which is the Copper/Gold group. Copper is most commonly formed from large masses of molten lava rock which has solidified in the earth's crust and over time though different sizes and speeds of crystal growth has turned into large amounts of copper, stored in porphyry copper deposits. Copper has a distinctive colour, yet can sometime appear blue and greenish which is often caused by oxidisation or a mixture of copper and other metals. This specific specimen was recovered from Moonta, South Australia. The Moonta Mining Company was established in 1861, after a Shepard in the area noticed traces of copper. This lead to a rush in the copper mining industry which was relatively young in Australia at the time, making Moonta Mining Company one of the richest in Australia. By the 1860's, South Australia had been nicknamed the "Copper Kingdom" due to its vast amount of Large copper mines and resources. As of 2016, Australia was the second largest producer of Copper internationally, following behind Chile in first place. This copper specimen is significant historically and scientifically as it is such an important metal commonly used throughout the world in various ways. Copper is an invaluable recourse used in daily life, used in most electrical appliances as it is a great conductor of heat and electricity, as well as being soft and malleable, making it easy to bend and mould into delicate sheets and wires. Copper does not corrode and is therefore used in the production of water pipes among countless other significant necessities that are often overlooked in our society. Historically, Copper holds great significance as it was the first metal used by humans. It was discovered roughly 9000 years ago and was utilised by the Neolithic Man who learnt that heating the metal made it more malleable, thus tools and utensils were made which were far superior to the previous stone tools used by humans. This history and its connection to the current and ongoing relationship between humans and copper must be preserved and highlighted as it is integral to the history of all humankind. A small, palm-sized solid native copper mineral specimen with shades of browns, black and rustic tones throughout the specimen.NATIVE (metalic) COPPER / Locality: Moonta, South Australiabeechworth, burke museum, geological specimen, native specimen, geological, mineral, mineralogy, indigo shire, beechworth museum, copper, copper ore

Taken in c. 1902, depicted is a group of adults and children dressed in formal clothing, with some of the women in the crowd carrying parasols, standing and sitting around and upon the rock at Queen Victoria Park on the Ford Street side of the park. This group is celebrating the official opening of the park. On top of the rock is a gas lamp post.Originally known as the Beechworth Botanical Gardens, the Queen Victoria Park features a extensive collection of historic trees and plants, which have been listed on the Indigo Shire’s Significant Tree Register. Sepia rectangular photograph printed on matte photographic paperReverse: 3716 (in black pen)/ 97.2273 (in pencil)/entertainment album, beechworth, queen victoria park, gardens & parks, opening, burke museum

Taken in c. 1905, depicted is a large group of children and adults dressed in formal attire sitting and standing upon a granite rock that is located in the centre of Queen Victoria Park. In front of the group is a wooden picket wire fence that sides the granite rock. On top of the rock is a gas lamp post.Originally known as the Beechworth Botanical Gardens, the Queen Victoria Park features a extensive collection of historic trees and plants, which have been listed on the Indigo Shire’s Significant Tree Register.Black and white rectangular reproduced photograph printed on matte photographic paperReverse: 6956 (in pencil)/ ©/ DONALD HAYES/ BEECHWORTH (stamped in orange ink)/entertainment album, burke museum, beechworth, queen victoria park, park

Taken in c. 1903, depicted is a large group of adults and children dressed in formal attire gathered around and upon the granite rock in the centre of Queen Victoria Park.Originally known as the Beechworth Botanical Gardens, Queen Victoria Park features a extensive collection of historic trees and plants, which have been listed on the Indigo Shire’s Significant Tree Register.Black and white rectangular postcard printed on cardObverse: QUEEN'S ROCK VICTORIA PARK BEECHWORTH Reverse: 3701/ 3641 (this has been crossed out)/ Parks & Gardens/ 1998.00059/ entertainment album, burke museum, beechworth, queen victoria park, gardens & parks

This image is a reproduction of an 1899 original depicting the 'Williams Good Luck Mine' on the Mopoke Reef (also called 'Morepork Gully') in the Dingle Ranges, approximately three miles from Beechworth. The foreground of the image is littered with piles of smashed rock and detritus, known as ‘mullock’, beside a reinforced mine shaft, a vertical access passageway allowing miners to enter the mine and haul ore out using lifting technology such as a poppet heads, whims or windlasses. A group of miners and a dog appear close to an open-sided miner’s hut. Following the discovery of gold at Beechworth in 1852, rushes quickly followed at surrounding creeks and gullies in the district. In the late nineteenth and early twentieth centuries, small syndicates of miners continued to work old or abandoned quartz reefs, often persisting without the assistance of heavy machinery to remove the large amounts of rock, in order to obtain yields at ever greater depths. The group of miners in this photograph are Mr. Roger Williams and Sons, who revived operations at the ‘Old Good Luck’ mine on the Mopoke Reef in the Dingle Range near Beechworth around 1892, working the site for more than two decades. An emigrant from Cornwall with experience in the tin mining industry, 19 year old Roger Williams senior sailed to New Zealand in 1840, then to Australia where he spent time in the Bendigo Gold Fields before settling in Beechworth in the early 1860s. Mr Williams senior worked on various mining activities in the district, including the Rocky Mountain Tunnel project. Conversant with the character of gold-bearing reefs in the area, the syndicate dug an eight hundred foot tunnel, digging down as far down as two hundred feet with little capital save their labour, to connect and provide better working access to the mass of reefs and veins in the vicinity. Progress was hampered by poor air quality charged with fumes from dynamite and large quantities of rock had to be crushed to obtain payable yields. The Victorian Goldfields are filled with ruins and remnants of the area's rich mining history, ranging from small alluvial diggings to the remains of huge mining companies. Site names often changed several times throughout the nineteenth and twentieth centuries. Some sites were abandoned and forgotten, others were worked continuously over many decades. The names of mines were often repeated at different locations throughout the Victorian Goldfields. For example, there is a Mopoke Gully heritage mine near Fryers Creek, Victoria. 'Mopoke' is a common onomatopoeic name for Morepork and Australian Boobook owls. This image has historical, social and research significance for patterns of emigration during of the Victorian Gold Rush, and the historical, social and environmental impacts of mining at Beechworth at the turn of the nineteenth and twentieth centuries. As gold became scarce and government support and large company investment waned, poor hard-working miners laboured intensively to make a living through periods of high unemployment. This image can be compared and studied alongside other historical mining photographs and objects in the Burke Museum Collection. It has potential to improve our understanding of miners working conditions and the shifting character of mining in the Beechworth district. Black and white rectangular reproduction photograph printed on matte photographic paper.Obverse: Williams Good Luck Mine Beechworth / Roger! / Reverse: 6858 / burke museum, beechworth museum, beechworth, gold fields, gold rush, victorian gold rush, gold ming history, colonial australia, australian gold rushes, mining technology, beechworth historic district, indigo gold trail, migration, indigo shire, good luck gold mine, victorian goldfields, mining syndicates, gold fever, quartz-mining, small-scale mining, old good luck mine, mopoke gully, quartz reefs beechworth

The Parfett family regularly holidayed in the Halls Gap area c1920sRectangular black & white photograph in a thin wooden frame with gold edging. A party of 8 people grouped on a large rock in front of a waterfall. 3 men, standing, the first has a cigarette in his mouth and holds a hat, the second holds a hiking pole; 3 women, the third has her arm raised with her hand on the back of her head; and 2 youths, the bigger wears braces and sits at the front of the rock, feet crossed, hands in his lap. The Rock has letters B.P and t E (?) painted on it. "BIG FALLS, c. 1926 (Mackenzie Falls) BLC sticker "Framed by DOUG'S FRAMES professional Picture Frame 24 Magpie St Ballarat, just down from Sovereign Hill. Phone 053 - 32 8311 label on back of frame.parfett, mackenzie falls, waterfalls

The photo shows a woodchopping competition in an unknown location in the Grampians. The identity of the people in the photo is unknown.The photo shows a large group of men standing in a clearing , around a cut log with a crow bar lodged in it. Other similar logs lie around the clearing. Many of the men are holding axes. There is a woman in a large hat standing beside a post in the right foreground and a man standing on a rock or log behind her with a pipe in his mouth.recreation, woodchopping competition

The photo shows a woodchopping competition in an unknown location in the Grampians. The identity of the people in the photo is unknown.The photo shows a large group of men standing in a clearing, around a cut log. One man has his foot on the log and is holding an axe and a crow bar which are lodged in the log. There is a man holding a book standing on a rock in the centre.recreation, woodchopping competition