Ernest Heinrich Marcuse was born on the 1st of December 1900 to Hedwig and Siegmund Marcuse in Berlin Germany. While Marcuse's artistic talent was apparent from a younger age, his earliest existing artwork was from when he was approximately 20 years old. Ernest's formal art training commenced in 1918 with a three year course at the Berlin school of Interior design. After completion he found work until 1924 when Germany's Great Depression took effect. To broaden his career opportunities he undertook a further 12 months study of fashion, drawing and advertising at Berlin's Reiman school of art. From 1925 to 1934 Ernest was primarily a freelance press artist specialising in industrial, architectural and figurative drawing. Prominent newspaper The Berliner Morgenpost was his largest client along with Gross Deutsche Rundfunaustellung (Germany's organisation for major trade shows). During this period he would create many significant works. Two months after Hitler and the Nazi part came to power in 1933, Ernest received a life changing letter stating that being Jewish he could no longer continue employment in Germany. Up until 1938 he would only be able to undertake private commissions and occasional unofficial work as a book illustrator and games designer. This was by arrangement with non Jewish artists who claimed his work as their own, they would then share the income with Ernest. With increasing unrest in Germany during late 1938 Ernest decided to move to London and there he married his girlfriend Lotte. In late 1939 Ernest and Lotte Marcuse embarked on an eight week journey to their new home in Australia where they had been accepted as refugees. Shortly after arriving in Australia Ernest presented his portfolio to an editor at the Argus newspaper and gained employment as a war events illustrator. He soon became well respected and known in particular for his detailed illustrations and cross sections of ships , artillery and aircrafts. His detailed depictions of battles were displayed on the front pages of The Argus newspaper on a number of occasions. In May 1940 as the war intensified Ernest was dismissed from The Argus newspaper due to his Australian government classification of 'stateless person of enemy origin' and was considered a potential security risk. The editor of the time commented "don't blame us, blame Hitler". Marcuse then began to establish himself as a commercial artist. Ernest was de-classified as a 'stateless person of enemy origin' and in early 1942. The Australian army heard of Ernest's artistic abilities and began to utilize his designs for visual training aids and posters. Ernest became Private E.H Marcuse V377746, his first army posting was as staff artist at The infantry officer's training school at Bonegilla. When off duty he was inspired by the beauty of the surrounding area creating the works in North east Victoria 'Kiewa river bridge', 'Hume weir', ' Dried up river bed' and 'Hawksview gold reef mine' from his 1942-1943 period at Bonegilla Victoria. Ernest returned to the area to create drawings and paintings from 1948 to 1983 in locations including Bright, Wandilligong, Bogong High plains and Wallace's Hut, Mt Buffalo, Beechworth, Pretty valley, Kiewa Hydro, Yackandandah and Bontherambo homestead. These sketches were often completed on location, photographs were also taken onsite to assist the works back at the studio. Occasionally Marcuse also painted in the field. Ernest's preferred choice of medium was pencil and ink. Up until 1952 he would often incorporate watercolour into his work. Later into his career he began introducing pastels, acrylic and mixed media. In earlier years Ernest Marcuse often signed his work Mar, later on the signing of works ranged from Marcuse, E.Marcuse, Ernest Marcuse, EHM or simply EM . If a work was considered incomplete or Marcuse did not like the work it would remain unsigned. From Bonegilla Marcuse was transferred to Woodside South Australia before his final posting in Melbourne until the end of 1945. Ernest's work from within his army posting 'Troop Train at Night' from his 1945 exhibition Australia at War are part of the permanent collection at Canberra's War Museum. Between 1946 and 1969 Ernest largely worked from home and concentrated on a career as a freelance commercial artist and graphic designer. During that time he created work for well known household names including CRA/Conzinc, Vacuum oil (Caltex), Cottee's Brand (Schweppes and Heinz), Home Beautiful magazine Fulton garden supplies, International Iveco trucks, Ego pharmaceuticals, QV and Sunsense. After retirement Ernest concentrated on his true love of fine art and focused on painting images of personal interest both across Australia and Internationally. Earnest never drove a car. He would often walk or use public transport or enlist in the help of family or artist friends to drive him. Throughout his career Ernest Marcuse's artworks were purchase by private collectors these included ACTU, Melbourne City council, Holland Constructions, Melbourne Metropolitan Tramways Board, GJ Coles and Australian Resources Bank. Ernest Marcuse permanent collections can be viewed at The National Gallery of Victoria , Sydney Jewish Museum, Jewish Holocaust Centre Melbourne, Canberra's War Museum, City of Melbourne, Shire of Yarra ranges and now the Burke Museum. © 2020 Art by Marcuse https://www.artbymarcuse.com.au/aboutDonated to the Burke Museum through the Australian Government's Cultural Gifts Program by Peter and Evelyn MarcusePen and pencil landscape drawing on paper.Obverse: CHILTERN PHARMACY / Reverse: 025 / ernest marcuse, marcuse, art, artbymarcuse, beechworth, burke museum, indigo shire, landscape, illustration, drawing, pen and pencil, australian army, war events illustrator, the age, the sun, the argus, germany, refugee, industrial drawing, architectual drawing, figure drawing, berliner morgenpost, grosse deutsche rundfunaustellung, berlin’s reiman school of art., cultural gifts program

index, ill, maps, p.154.non-fictionA history of the building of the railway from Brisbane to Cairns in Queensland.railroad construction - australia - history, railroad construction - queensland - history

The photograph appears to depict the of the entrance to the Rocky Mountain Tunnel. The Rocky Mountain Tunnel runs from opening of the tunnel, underneath the Beechworth town, to the Gorge. This tunnel drained the excess water from the upper Spring Creek Goldfield to allow for mining access in the area. The Rocky Mountain Co. blasted through the granite rock to create the original 400ft-long tunnel in 1859, but between 1867 and 1871, the Rocky Mountain Gold Sluicing Co. widened and extended it. At its completion, it measured 14ft deep, 6ft wide, and almost half a mile long. The mining surveyor at Beechworth called it 'without doubt, the greatest undertaking of the kind in the colony'. When the company became the Rocky Mountain Extended Gold Sluicing Co. in the mid-1870s, they continued the tunnelling work. The work was reportedly vital to mining being able to continue at Beechworth and may have established world records in tunnelling through hard rock. The entrance at the Gorge side of the tunnel can be seen from the Beechworth Gorge Walk. The tunnel continues to be an outfall drain for the lake and the town.The search for gold is ingrained into the history of Victoria and therefore, images like this one which portray an open cut sluicing site can reveal important information for society and technology for the date when the photograph was taken. This image is of important historical significance for its ability to convey information about sluicing and the methods used to find gold in the late 1800s and early 1900s. It also shows a location where sluicing was undertook which provides insight into the impact of sluicing on the environment at a time when it was done. The Burke Museum is home to a substantial collection of Australian mining photographs which can be used to gain a deeper understanding into life on the gold fields, technology used in mining, the miners themselves and the impact of the gold digging on the environment.A black and white rectangular reproduced photograph printed on matte photographic paper.7814beechworth, beechworth museum, burke museum, australian museum, mining, rocky mountain mining co., rocky mountain mining company, mine, mining company, rocky mountain mine, mine entrance, rocky mountain, gold, gold mining

Lord Kitchener visited Seymour as part of his review of Australia's military capabilities. Lord Kitchener was Commander-in-Chief of the British Army at the time of his visit. At the invitation of Prime Minister Alfred Deakin, Kitchener visited Australia in 1909 to inspect the existing state of defence preparedness of the Commonwealth, and advise on the best means of providing Australia with a land defence. Kitchener’s report, submitted in February 1910, recommended the introduction of compulsory military training which was immediately adopted, as was the establishment of the Military College, Duntroon: It has been definitely decided that Seymour will be the site of the Kitchener camp. The troops which will make the strongest muster at the camp will be the Light Horse. This being so, the suitability of the chosen area for cavalry operations has necessarily had to be considered in selecting the site, and an additional factor is that Seymour is practically in the centre of the Light Horse districts. The country round Seymour is also suitable for artillery manoeurves, and there is no available area in the vicinity of Melbourne where these could be so well carried out. As it is considered that Field-Marshal Lord Kitchener will desire to see the troops on the move, the reason for choosing such a district as Seymour is apparent. The eight days to be devoted to the camp will be mainly occupied in moving the troops over a considerable area, and in carrying out certain tactical operations. Many of the sites recommended have been inspected by officers of the head quarter staff, and all that now remains is that the exact situation for the main camp should be selected, Major Luscombe will visit Seymour on Saturday to inspect the surround country, and select the most suitable places. The intention will be directed to sites closer to the town. Yea Chronicle (Yea, Vic), 9 December 1909. Black and white rectangular photograph printed on matte photographic paper and mounted on board.Obverse: Beechworth Light Horse (pen) / Kitchener Camp / Seymour / 1910 / Reverse: 8743 / Mrs R Scott / military album, burke museum, burke, beechworth, beechworth light horse, light horse, world war one, wwi, 1910

After gold was discovered to be deposited "for miles along Woolshed Valley" in the early 1850s, the Woolshed became a major site of mining activity in the north-east . This region was divided into large claims of 80 yards long, one of which was the one depicted in this photograph, called 'Big Johnson's Claim'. Claims such as this utilised a range of technology, including water wheels, steam engines, sluices and toms, most of which would not arrive until after 1856 when this photograph was taken. The Woolshed initially became prosperous in 1855, and labourers, such as the ones depicted in this photograph, engaged in sinking work for 7 pounds a week, whilst other mining labourers could earn up to nine. The search for gold is ingrained into the history of Victoria and therefore, images like this one which portray an open cut sluicing site can reveal important information for society and technology for the date when the photograph was taken. This image is of important historical significance for its ability to convey information about the operations of mining claims, particularly of the Woolshed Valley area that this photograph documents. This image is important for current research into the history of Woolshed, which was a major site of mining significance and operations. Therefore, this image has the capacity to be beneficial for research into society and the motivations of those living and working in this region during this period and therefore, has social significance. The Beechworth Burke Museum has additional images relating to gold sluicing and the Woolshed area which can be analysed and studied alongside images like this one. A black and white rectangular photograph printed on matte photographic paper.Reverse: 7791 / page 34. / 52% / Big Johnstone / Claim on Woolshed Goldfields / 1856 / Note canvas [illegible] building / Burke Museum /woolshed, mining, claims, mining claims, big johnson, gold

This photograph dates to 1899, towards the end of the gold rush in the Mopoke Gully area. 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. Mopoke Gully mines came under the 'Fryer's Creek' division of the Castlemaine District during the Gold Rush. After the Gold Rush began in Victoria with the discovery of gold at Ballarat in 1851, Gold was found in Castlemaine by December of that year. 20,000 diggers were spread across the Castlemaine region, and the area was yielding about 23,000 ounces of gold per week. Mopoke Gully was the site of the Mopoke Gully Water Wheel, operating under the Bendigo and Fryers Goldmining Company from 1887 until 1900. This Water Wheel was used in the gold mining technique of 'sluicing'. Hydraulic sluicing uses high pressure water jets to blast away the earth, which runs through a sluice box, catching the gold with all remaining slurry washing away. This Water Wheel was built the same year as the more famous 'Chewton Water Wheel', but was smaller in diameter (60ft as opposed to Chewton's 72ft). The Mopoke Water Wheel ruins are quite intact today, and are a registered archaeological site. The search for gold is ingrained into the history of Victoria and therefore, images like this one can reveal important information for society and technology for the date when the photograph was taken. This image is of important historical significance for its ability to convey information about sluicing and the methods used to find gold in 1899. This photograph reveals important information on the use of dogs on Victorian goldfields in 1899. Dogs were used both as companions, such as this photograph depicts, as well as deterrents to thieves. 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. beechworth, burke museum, gold, gold mining, 1899, castlemaine, mopoke gully, good luck mine, fryer's creek, gold rush, victorian gold rush, water wheel, sluicing, chewton

This photograph dates to 1899, towards the end of the gold rush in the Mopoke Gully area. A slurry of rocks after they have been broken up is depicted, and this is part of the hydraulic sluicing mining process. Four men are relaxing under a wooden structure, with a fifth bearded man standing near a stone wall. 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. Mopoke Gully mines came under the 'Fryer's Creek' division of the Castlemaine District during the Gold Rush. After the Gold Rush began in Victoria with the discovery of gold at Ballarat in 1851, Gold was found in Castlemaine by December of that year. 20,000 diggers were spread across the Castlemaine region, and the area was yielding about 23,000 ounces of gold per week. Mopoke Gully was the site of the Mopoke Gully Water Wheel, operating under the Bendigo and Fryers Goldmining Company from 1887 until 1900. This Water Wheel was used in the gold mining technique of 'sluicing'. Hydraulic sluicing uses high pressure water jets to blast away the earth, which runs through a sluice box, catching the gold with all remaining slurry washing away. Hydraulicking is the process of breaking up the rocks and suspending it in a slurry. This Water Wheel was built the same year as the more famous 'Chewton Water Wheel', but was smaller in diameter (60ft as opposed to Chewton's 72ft). The Mopoke Water Wheel ruins are quite intact today, and are a registered archaeological site.The search for gold is ingrained into the history of Victoria and therefore, images like this one which portray a sluicing site can reveal important information for society and technology for the date when the photograph was taken. This image is of important historical significance for its ability to convey information about sluicing and the methods used to find gold in 1899. It also shows a location where sluicing was undertook which provides insight into the impact of sluicing on the environment at a time when it was done. This photograph reveals important information on the use of dogs on Victorian goldfields in 1899. Dogs were used both as companions, such as this photograph depicts, as well as deterrents to thieves. 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. beechworth, burke museum, gold, gold mining, 1899, castlemaine, mopoke gully, good luck mine, fryer's creek, gold rush, victorian gold rush, water wheel, sluicing, chewton, slurry

This photo depicts a man standing next to a large piece of mining equipment identified as a hydraulic chisel (alternative name: drifter dill or power rock drill). This piece of machinery was used in mining to place holes in the walls of a mine which were then filled with dynamite or other explosives for rock blasting or to make holes for plug and feather quarrying. The additional tools to the right of the photograph and in front of the machinery can be identified as either picks or as feather and wedges, the latter of which were used to split stone drilled by the hydraulic or power chisel. Depending on the date of the photograph, which is not provided, this chisel was either powered by electricity or by hydraulics. The following is written on the drill "R.C. FORD'S PATENT No91 / MELBOURNE VICTORIA 1879". The man depicted in this photograph wears a wide brim hat, a loose fitting white shirt and loose pants. He wears boots and has a medium sized dark beard. This attire, along with his locality in the mine and proficiency with the mining equipment, identifies this man as a miner working in this particular, but unidentified, mine. It depicts an instance of hydraulic chiseling which makes this photograph valuable for the study of mining techniques from a date c1880.The search for gold is ingrained into the history of Victoria and therefore, images like this one which portray the types of machinery used in mining can reveal important information for technology and highlight the methods used to break apart the earth in order to obtain access to gold and other precious materials during the period this photograph was captured. Further research into RC Ford can potentially reveal even further information pertaining to this photograph. This image is of important historical significance for its ability to convey information about the methods and machinery used to access gold or mine more in general. It also highlights the size of machinery at the time and allows us to compare this to the size of the person standing besides the machinery to better understand the manpower which would have been required to use and set-up this macinery.A black and white rectangular reproduced photograph printed on matte photographic paper.Reverse: 7816/ copy 1/3gold, sluicing, gold sluicing, hydraulic sluicing, gold and tin mine, mining, gold mining, beechworth, burke museum, melbourne, victoria, hat, mining machinery, machinery, r. c. ford

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

Portrait of William Edward Peach in First World War military uniform, holding a crop in front of his thighs with military kit on the ground behind him. A Beechworth postal employee who enlisted in 1915, this photograph is probably taken in 1917, as he is a corporal in the photo and was promoted to this rank in May 1917. This photograph is of historic significance as it depicts William Edward Peach, a Beechworth postal assistant who enlisted in the Australian Imperial Force (AIF) on his nineteenth birthday, 5 August 1915, which required his parents' permission. He was decorated with the military medal for his courage in battle 4/5 October 1917 at the Battle of Broodseinde Ridge near Ypres, the most successful allied attack of the Third Battle of Ypres (31 July to 10 November 1917), also known as the Battle of Paschendale, which saw the greatest loss of human life during World War One, with almost half a million lives were lost on all sides. According to the recommendation for his military medal, Peach 'displayed conspicuous courage and initiative', taking charge after his platoon commander became a casualty, handling the men 'under heavy fire with great skill'. He also assisted the Company Commander in reorganising their military objectives. The photograph is of social as well as historic significance for the Beechworth community, because it provides a direct link between local, national and international histories in relation to Australia' s participation in one of WWI's best-known battles. The record has strong research potential given the ongoing public and scholarly interest in war, history, and especially the ANZAC legend, which is commemorated annually on 25 April, known as ANZAC Day. Peach is also one of the diarists of WWI, including of this significant period of Australian military history, from 1916 to 18, which can be accessed via the Australian War Memorial. Sepia rectangular photograph printed on gloss Kodak photographic paper mounted on board. Reverse: BMM 8779 item catalogue number pencilled in right-hand bottom corner.military medal, defending australia and victoria, military service, hmat a64 demosthenes, wipers, anzac, burke museum, beechworth, ypres, australian military services, beechworth post office, first world war, wartime, our boys, belgium, flanders fields, ww1, british war medal, victory medal, broodseinde, third battle of ypres

The photograph depicts a rocking chair, a kerosene lamp, a bottle holder, and two epergnes.The photograph contains historical and research significance of domestic life in Beechworth. Through the depiction of the historical rocking chair, the kerosene lamp, the bottle holder and the epergnes, the picture displays some of the everyday objects that would have been found within a Beechworth house. Although kerosene lamps and bottle holders are no longer in widespread use, this photograph not only acts as historical document and depiction of both, but it also displays the evolution of everyday tools. The interpretive capacity of the photograph extends its significance as it contains the potential to reveal information regarding the domestic life of Beechworth residents. Moreover, it also has protentional to demonstrate the shifting designs of rocking chairs, kerosene lamps, bottle holders and epergnes.Black and white rectangular photograph printed on paper.Reverse: BMM A03328/ 1997.3132/ 28 1/2 ems/ E32k491/ THE OVENS AND MURRAY ADVERTISERrocking chair, chair, lamp, kerosene lamp, bottle holder, burke museum, beechworth

Woolshed is a small area about five kilometres north west of Beechworth, and almost about 225km north east of Melbourne. When gold was discovered at the nearby Spring Creek in February 1852, Woolshed was one of three settlements set up to house miners and their families. At its peak in 1857, Woolshed was also populated by 29 storekeepers and 14 hotels, as well as the Woolshed State School, which stood near where this photograph was taken. The school often played host to public meetings, as well as a public dance in 1897. The school was subject to some controversy in 1874 when one parent complained about the head of the school in the local newspaper, the Owens and Murray Advertiser, and at least three letters to the editor were exchanged between the two. According to the parent, C. O'Donoghue was not providing enough amusement for the children and was disrespectful to parents and staff. When the State Governor, Sir Reginald Talbot, visited Beechworth in 1906, the school organised a celebratory welcome. The Woolshed State School was ultimately closed in 1922 as miners had exhausted the Spring Creek gold supply and were moving elsewhere. This photograph, taken in about 2000, shows the trees that grew on or near the site of the original school. The Woolshed State School Honour Roll, with a list of the men from the school who served in the First World War, also still exists. It is stored in the Beechworth RSL as of 2015.This photograph is significant for its connection to an important site in Beechworth's gold mining history. Woolshed served a significant community of miners, with a population of at least 138 according to the 1911 census, with families that needed the school site to ensure their children's education. The image is also useful for prompting discussion about how Beechworth has changed over time, with the photograph taken 78 years after the school closed down.A colour rectangular photograph printed on glossy photographic paper.Woolshed State. / School site / 2000 / - remnant trees / / cobeechworth, burke museum, school, education, trees, nature, state school, woolshed, gold mining, teachers, over time, owens and murray advertiser, public meetings, public dance, c. o'donoghue, spring creek, state governor, sir reginald talbot, miners, honour roll, world war 1

Malachite is typically found as crystalline aggregates or crusts, often banded in appearance, like agates. It is also often found as botryoidal clusters of radiating crystals, and as mammillary aggregates as well. Single crystals and clusters of distinguishable crystals are uncommon, but when found they are typically acicular to prismatic. It is also frequently found as a pseudomorph after Azurite crystals, which are generally more tabular in shape. This particular specimen was recovered from the Burra Burra Copper Mine in Burra, South Australia. Otherwise known as the 'Monster Mine', the Burra Burra Copper Mine was first established in 1848 upon the discovery of copper deposits in 1845. Within a few short years, people from around the world migrated to Burra to lay their claim in the copper economy. By April 1848 the mine was employing over 567 people and supporting a population of 1,500 in the local township. Up until 1860, the mine was the largest metals mine in Australia, producing approximately 50,000 tonnes of copper between 1845 to its closure in 1877. The Burra Burra Mine was also famous for a number of other specimens, including; crystalline azurite, cuprite, and botryoidal and malachite. Malachite is considered a rare gemstone in that the original deposits for the stones have been depleted leaving behind very few sources. In addition, the use of Malachite as gemstones and sculptural materials remains just as popular today as they were throughout history. It is quite common to cut the stone into beads for jewellery. The fact that Malachite has such a rich colour and one that does not fade with time or when exposed to light makes it particularly rare. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study. A solid hand-sized copper carbonate hydroxide mineral with shades of blue and light green throughout. burke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, mineralogy, burra, burra burra mine, south australia, malachite, malachite specimen

Malachite is a green copper carbonate hydroxide mineral and was one of the first ores used to make copper metal. Malachite has been utilised as a gemstone and sculptural material in the past as its distinctive green color does not fade when exposed to light or after long periods of time. Malachite is formed at shallow depths in the ground, in the oxidizing zone above copper deposits. The material has also been used as a pigment for painting throughout history. This particular specimen was recovered from the Burra Burra Copper Mine in Burra, South Australia. Otherwise known as the 'Monster Mine', the Burra Burra Copper Mine was first established in 1848 upon the discovery of copper deposits in 1845. Within a few short years, people from around the world migrated to Burra to lay their claim in the copper economy. By April 1848 the mine was employing over 567 people and supporting a population of 1,500 in the local township. Up until 1860, the mine was the largest metals mine in Australia, producing approximately 50,000 tonnes of copper between 1845 to its closure in 1877. The Burra Burra Mine was also famous for a number of other specimens, including; crystalline azurite, cuprite, and botryoidal and malachite.Malachite is considered a rare gemstone in that the original deposits for the stones have been depleted leaving behind very few sources. In addition, the use of Malachite as gemstones and sculptural materials remains just as popular today as they were throughout history. It is quite common to cut the stone into beads for jewellery. The fact that Malachite has such a rich colour and one that does not fade with time or when exposed to light makes it particularly rare. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study. A solid hand-sized copper carbonate hydroxide mineral with shades of yellow, blue, and light green throughout.geological, geological specimen, burke museum, indigo shire, malachite, malachite specimen, burra burra mine, burra, south australia, australian mines, mines, monster mine

Galena Chalcopyrite is the earth's primary ore of lead and is mined from a large number of deposits in many countries. It is also an important source of silver. Galena Chalcopyrite is one of the most abundant and widely distributed sulfide minerals across the world. The mineral is found in igneous and metamorphic rocks in medium- to low-temperature hydrothermal veins. This specific specimen was recovered from the mines in Broken Hill, New South Wales. The mines in Broken Hill were first established after Charles Rasp discovered a large amount of silver-lead-zinc ore-body in the area in 1883. BHP (Broken Hill Proprietary) mining company was then established in 1885 and quickly became the lead in Australia's mining industry after they began excavating and exporting the country's largest amount of lead, silver, and zinc. This feat generated over $100 billion in wealth for the company.Galena Chalcopyrite is signifiant as it represents the catalyst for the rise of Australia's most influential mining companies - BHP. The mineral was one of the first to be mined in the country and after being made into lead, was used for a variety of things such as paint, batteries, ammunition, and plumbing materials before it was known to be harmful to humans. 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 grey, solid hand-sized lead sulfide mineral with a silver metallic luster.burke museum, beechworth, geological, geological specimen, galena, galena chalcopyrite, chalcopyrite, broken hill, bhp, bhp mining, broken hill mine, mine, australia mine, lead, lead mine

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

This 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

Rhodonite is a reddish-pink manganese silicate material and often contains iron, magnesium and calcium. It is usually found in metamorphic rocks (rocks which have been altered by heat, pressure or chemical process). It can range in size from tiny to massive. Because of their composition they are not suitable for use in jewellery because they are hard enough. It is quite rare to find, though has been found in Australia, North America, South America and Europe.This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study. This specimen is a palm shaped piece of loellingite within rhodonite. It is mostly reddish-pink coloured, with flecks of light and dark grey. Loellingite is a grey iron arsenide which often forms into crystal shapes. It is mostly found in mesothermal veins (caused by immense heat) with sulfides or in limestone. It is toxic when heated or struck. rhodonite, loellingite, burke museum, beechworth, geological survey of victoria

This specimen was recovered from Silverton Mine in Broken Hill, New South Wales. Otherwise known as the 'Day Dream Mine', the Silverton Mine was first established in 1883, when silver and lead deposits where discovered. Within a few short years, the population of Broken Hill reached 3000 people. As of today the Silverton Mine is still open, and has produced over 200 million tonnes of ore, which has generated over $100 billion. The Silverton Mine was also famous for a number of specimens such as silver, iron and zinc.Copper is considered to be a rare ore in that finding it in its pure form is rare. Nowadays when mining for Copper it is often found in mixed in with other minerals or it is recycled from use. Moreover, Copper is found in a range of everyday uses such as coins, cookware, pipes, heating conductors and anything that generate electricity. The fact that Copper is heat a heat conductor, electricity conductor and it does not corrode easily, makes this ore a versatile and useful. 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 cube-shaped sulfide and oxide with shades of green, grey and brown throughout. Copper is typically found as nuggets in the ground. It can be found in a range of forms such as its native state; mixed with other ores, such as zinc and iron; as porphyry copper deposits; and as major deposits. Porphyry deposits are when the mineral is scattered evenly throughout the rock. Major deposits are when the mineral is scattered amongst other minerals.burke museum, beechworth, indigo shire, beechworth musum, geological, geological specimen, mineraology, copper, copper ore, copper ore speciment, broken hill, new south wales

According to the 1912 Department of Mines Bulletin of the Geological Survey of Victoria, basalt covers a considerable portion of the Macedon area including Mount Macedon. Basalt is the most common form of rock underlying the earth's surface and is found in three kinds of rock forming environments: ocean divergent boundaries, oceanic hotspots, and mantle plumes and hotspots beneath continents.This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A solid mass, geological specimen in shades of grey and white. Hyalite is a colourless variety of opal. It occurs as globular and botryoidal masses and irregular crusts in volcanic and pegmatite environments where the silica deposits from the gas phase. Basalt is dark in colour, fine-grained igneous rock composed of plagioclase and pyroxene minerals. It is commonly formed as an extrusive rock, such as lava flow. It is one of the most common forms of rock underlying the earth's surface.burke museum, geological specimen, department of mines, geological survey of victoria, basalt, mount macedon, beechworth

This particular specimen was recovered from the Lal Lal Coal and Iron Mine in Victoria, 19km from Ballarat. Brown Coal was discovered here in 1857, just alongside the Geelong to Ballarat Railway line. This discovery of lignite (brown coal) was the first in Victoria, which would bring important benefits to the region and state, both of which had previously been reliant on coal imports. In the 1860s, iron ore was found just 5km from Lal Lal, and the area was converted into an Iron Ore Mine. The Lal Lal Iron Mining Company took over operations in 1874, who then peaked iron production in 1884. This mine continued operations until June 1884, when the blast furnace was extinguished and never recommenced. The blast furnace at Lal Lal is considered one of the most important and highly significant sites ion early industrial history in Australia, as it is the only remaining best furnace from the nineteenth century in the Southern Hemisphere. The furnace ruins are 17 metres high, and are clearly visible today on Iron Mine Road, Lal Lal, near the Bungal Dam. This specimen of Lignite (brown coal) is significant, as it was mined from the area where brown coal was first discovered in Victoria, leading to an important and controversial future of the mining and use of brown coal in this State. The Victorian Heritage Database has listed the Lal Lal Coal Mine with local significance, with their Statement of Significance stating: "The Lal Lal coal mine is historically significant as the site of the first discovery of lignite (brown coal) in Victoria, and one that promised important benefits to regional and state industries that were reliant on coal imports at the time. The significance of the stie is reduced by the poor state of preservation of the coal mining and processing fabric". 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 light-weight, soft and combustable sedimentary rock specimen, that is dark brown in colour. The specimen has jagged edges, as though parts of the rock have crumbled away. Brown coal, or Lignite, is formed naturally from compressed peat, and is typically found in natural basins. The stages to the formation of coal ('coalification') begin with plant material and wood, which will decay if it is not subjected to deep burial or heating, and turn into Peat. Peat, when sufficiently compressed naturally, will turn into Brown Coal (Lignite), and finally into Black Coal (sub-bituminous, bituminous and anthracite). Each successive stage has a higher energy content and lower water content. It is brownish-black in colour. Brown Coal has a high moisture content, between 50 and 75 percent, and a low carbon content. Some Brown Coals may be stratified, with layers of plant matter, which means little coalification has occurred beyond the peat natural processing stage. When Brown Coal is submerged in dilute nitric acid or boiling potassium hydroxide solution, it reacts to produce a reddish solution, of which higher-ranked coals do not. When brown coal is pulverised and burned in boilers, the steam is used to drive turbines, which generates electricity. It is the lowest rank of coal, as when burned, it creates a relatively low heat content, which in turn does not create a great output of steam. burke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, mineralogy, brown coal, brown coal specimen, lignite, lal lal, lal lal coal mine, lal lal iron mine, ballarat, blast furnace

Gabo Island sits off the coast of East Gippsland in Victoria, with cliffs of granite in a relatively unique red/pink colour. Early attempts to build a lighthouse on the island were abandoned due to poor foundations, but when a ship ran aground on the nearby Tullaberga Island in 1853 and led to the death of 37 people, efforts were reignited. Construction of a new lighthouse was completed by 1858, using Gabo Island granite. The lighthouse is Australia's second tallest in Australia and continues to play an important role in guiding boats around the coast as they journey between Melbourne and Sydney. The distinct pink colour from the granite means the lighthouse continues to be a defining feature of the island. Gabo Island granite was also used to construct the Treasury Building at 117 Macquarie Street in Sydney, now the Intercontinental Hotel.Granite in the pink colour of this specimen is relatively rare. The connection to the lighthouse on Gabo Island also gives the specimen historic significance and social significance regarding the maritime history of Victoria. 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 palm-sized mineral, coloured by flecks of pink, red, and grey. Granite is formed by the slow crystallisation of magma below the earth's surface. It is typically composed of a mix of quartz, feldspar, and other minerals, though syenitic granite like this sample has a smaller amount of quartz than typical granite. This different mineral composition leads to the more distinct pink and red colouring.First sticker: [torn]logical survey / R........ S........ / Loc Gabo Island / 1/4 Sheet / Second Sticker: 15 Third Sticker: Syenitic Graniteburke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, mineralogy, gabo island, gabo island lighthouse, lighthouse, granite, coast, coastal, granite specimen, victoria, coastal cliffs

In Australia, precious opal is found in Cretaceous age sandstones and mudstones. These sedimentary rocks were deeply weathered and this weathering released silica into the groundwater.Australia is the only part of the world where opalised animal and plant fossils have been found. Opal artefacts several thousands of years old have been discovered in East Africa. As early as 250 BC the Romans prized opals, thought to have come from mines in Eastern Europe, the ancient world's main source of opals. There are many aboriginal dreamtime stories that feature opal. Australian opals discovered during the late 1800's found little favour with European markets but their commercial value increased in the 1900's and in 1932 Australia took over as the major producer of opals in the world and remains the largest producer to this day. Opal is found around the world (Brazil, Mexico, Honduras and the western US) however Australia produces 95% of the world's precious opal and it is our official national gemstone. Opal was first mined commercially at Listowel Downs in Queensland in 1875 and later at White Cliffs in NSW. Today, Coober Pedy (SA) is the main producer of white opal, though in recent years this field has expanded and all types of opals are found. Other centres in SA include Andamooka and Mintabe. Lightning Ridge (NSW) is renowned for black opal and formerly White Cliffs was a large producer of high quality opal. Boulder opals (opals in concretionary ironstone) are mined in Queensland from numerous localities in a zone extending from the Eulo and Cunnamulla district in the south and northwest for a distance of over 700 km to Kynuna in the north. The towns of Quilpie, Yowah and Winton are the main opal mining and wholesale centres. Opals are considered gemstones and have been used in jewellery for thousands of years.Throughout much of history, opals were actually believed to be good luck. The Romans thought that opals were one of the luckiest gemstones and a symbol of hope. In the Middle Ages, opals were believed to be bestowed with all the positive properties of coloured gemstones due to its rainbow-like play of colour. Finally, there is a superstition that you should not wear an opal unless it is your birthstone otherwise misfortune will befall you. This, of course, is far-fetched, but the notion could have been promoted in the late 19th and early 20th Centuries by diamond traders who were trying to increase sales of diamonds and deter people from buying opals. Possibly related to this is the thought that you should set opal jewellery with diamonds as their powers of good fortune will override any negativity held by the opal. The great majority of opal does not show play of colour and is called common opal or potch however this is not the case with a precious opal. Opal is a precious gemstone, like rubies, emeralds or diamonds. Opal is rare, and it is expensive to prospect and mine for.Silica is one of the most common minerals on the planet, but precious opal is very rare – far more rare than diamonds. Precious opal is rare because the natural processes that create it rarely occur.Most (at least 95%) of the opal found by miners is common opal without gem colour. In Australia we call it potch. It can be white, grey, black or amber coloured. Even when a miner finds gem-coloured opal, most of it can’t be cut into gemstones because it’s too thin, or sandy. 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.It is not known where this opal originated, except that it is probably from Victoria, as it has been recorded from many localities in the State. Common Opal is formed from silica-rich water circulating through rocks near the Earth’s surface. It consists of minute spheres of silica arranged in different ways. In common opal, the spheres are of different sizes and randomly arranged, unlike in precious opal where the spheres are of similar size and uniformly arranged in three dimensions. These differences account for common opal generally being translucent to opaque and without the play of colours, or opalescence, displayed by precious opal. Common opal is found in many localities and different geological environments throughout Australia and the world. Precious opal requires special conditions to form and is much less common. Australia produces most to the world’s precious opal. burke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, precious opal, opal, brazil, mexico, honduras, queensland, coober pedy, gemstones, jewellery, play-of-colour, light blue

Basalt is a common igneous rock that composes most of the Earth's surface and can be found on the Moon and other rocky planets of the Solar System. It is generally composed minerals such as calcic plagioclase, clinopyroxene and iron ore which form grains that are indistinguishable to the naked eye. It can be dark grey or black in colouring and sometimes may contain holes left by gas bubbles. Most of the Earth's basalt was produced in environments such as oceanic divergent boundaries, oceanic hotspots, and mantle plumes and hotspots beneath continents. Basalt is commonly used in construction where it is crushed and used for multiple purposes such as concrete aggregate, road base, or railroad ballast. Thin slabs of basalt can also be cut and used for floor tiles, stone monuments, and building veneer. This particular specimen was excavated from Talbot in Victoria, which was a small gold mining town established in 1852. As basalt is a common rock, it is not specific to Talbot. However, this specimen can be assumed to be of the Cainozoic age due to previous geomorphic surveys of the area. This particular type of Basalt was used mainly for roads due to the durability of the rock.Basalt holds significance due to the continued use of the rock from historic until present times. The rock has been utilised for many types of construction and is still used for the same purposes today. Basalt also has significance to the Earth and other rocky planets of the Solar System as it makes up most of the planet's surface. 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 smaller than hand sized rock specimen which is dark grey in colour with small holes and white deposits across its surface.Geological survey / [illegible] /burke museum, beechworth, geological specimen, geology, basalt, basalt specemin, indigo shire, talbot, cainozoic, igneous rock

This specimen was recovered from Creswick in Victoria. Basalt is dark in colour, often black and has a fine grain. It is composed of plagioclase and pyroxene minerals and an igneous rock. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these 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 cylindrical fine-grained piece of igneous rockburke museum, geological survey of victoria, geological specimen, geology

This specimen was recovered from Wonthaggi in Victoria. Coal is a sedimentary rock which is composed of peat after it has been exposed over millions of years. This is an example of Australian black coal which is used as either thermal or coking coal for electricity generation or manufacturing processes. It is predominantly composed of Carbon which is 'C' on the periodic table of elements. This early example of a coal sample, shows the important role that coal played/plays in Australia's energy generation and manufacturing processes. 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.Small piece of black coal with museum original labelGeological survey / R..... S...../ Locality Cape Patterson coal specimen, burke museum, geological survey of victoria, geological specimen, geology

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

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

This specimen is from Barefoot Hills, Victoria. Sandstones are economically important as major reservoirs for both petroleum and water, as building materials, and as valuable sources of metallic ores. Most significantly, they are the single most useful sedimentary rock type for deciphering Earth history. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A sedimentary rock composed mostly of quartz sand. Sandstone is the second most common sedimentary rock after shale. Sandstones consist of sand-sized grains principally quartz, feldspar and rock fragments. The two major classes of sandstone are arenite and wacke. the colour of sandstone varies from grey, yellow, red and white reflecting the variation in mineral content and cement and is gritty to touch (like sandpaper).Geological survey / R.... S 61 / Loc Bareboot Hills / Sheet / 24SE / 94 /burke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, mineralogy, sandstone, yellow sandstone, victoria, barefoot hills

This specimen was recovered from Philip Island in Victoria. Chalcedony is composed of Quartz and Silicon Dioxide represented as SIO2. It has and is still used as a gemstone for thousands of years. This is an excellent specimen Chalcedony that shows its aesthetic properties. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study. Uniquely shaped piece of Chalcedony with opening in the centerburke museum, beechworth, geological, geological specimen