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

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 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

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

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 photograph depicts the Great Southern Mine located in Rutherglen as it was during the 1900. After the initial Gold Rush of 1853-1854, Gold was discovered deeper under the surface of the earth in the 1860 after the discovery of another deep lead system. Due to the discovery of Gold in Rutherglen, Rutherglen developed into a community in its own right, possessing a population of 6600 by December 1860 and developed into a municipality in 1862. The Great Southern Mine depicted in this photograph required the use of a range of modern technologies, including the hydraulic pumps, in order to reach gold. This photo depicts the mining operations as they were undertaken around the turn of the century.The search for gold is ingrained into the history of Victoria and therefore, images like this one which portray a modern mining operation undertaken in the 1860s, 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 methods used to extract gold in 1900. It is significant as most mining operations around the region, particularly earlier on in the period, used different technologies such as water races. This image is important for current research into the history of Rutherglen more generally, a town which developed singlehandedly due to the discovery of minerals and mining, as depicted here in this photograph, thus indicating an element of social significance as well as historic. The Beechworth Burke Museum has additional images relating to mining and Rutherglen which can be analysed and studied alongside images like this one.A black and white rectangular photograph printed on matte photographic paper.Reverse: $ 3.00 19972503 / a02503 / Great Southern Mine Rutherglen 1900rutherglen mine, rutherglen, great southern mine, beechworth, mine, mining, post goldrush, victoria, gold, 1860s, sluicing, hydrolic sluicing

Depicted in the photograph are ten miners standing at a cliff face using a high pressure hose, in Beechworth, Victoria. The miners are located in the Three Mile Creek division, in the Beechworth Mining District established January 4th 1858 under An Act for Amending the Laws Relating to the Goldfields by the Governor-in-Council. The Ovens Gold Rush began at Beechworth in February 1852 and was followed by Yackandandah and the 'Indigo Goldfield'. The strategies applied to mining in Beechworth were distinct in comparison to other goldfields in Victoria such as Bendigo and Ballarat. The miners in Beechworth utlised 'hydraulic sluicing' to remove washdirt, the long water races and deep tailraces constructed through solid rock with an estimated 900 miles of water races cut through the Beechworth fields by 1880, demonstrating great engineering feats. The photograph taken is significant as it is a visual representation of the mining strategy, 'hydraulic sluicing' that was particularly unique to the Beechworth mines, particularly in Victoria and an engineering feat.Black and white rectangular photograph printed on matte photographic paper, unmounted print.beechworth mining district, mining, three mile creek division, three mile creek

The photograph printed on this postcard comes from the collection of the Mitchell Library in Sydney. It is sepia in tone and depicts seven men standing and sitting around a mine shaft in the Beechworth region. The photograph has been dated to approximately 1872. This period in history post-dates the Victorian gold rushes which occurred 1852-1853 in Ballarat, Bendigo and Beechworth. During this period, in the 1870s, the surface alluvial gold had been discovered and removed from location. Therefore, in order to reach the deeper and less accessible alluvial gold, diggers began to dig shafts into the earth. These shafts sunk below the ground level by 20 to 30 feet and required timber structures around the entrance and winches to bring the paydirt to the top. The top of this wooden structure is visible behind the man standing in the upper right of the image. This type of mining was highly dangerous as mines often caved in which injured the minors and often resulted in death. Thus, following this period, in the early 1900s, miners opted instead for hydrolic slucing which cut away the earth without the devastating consequences of a mine cave in. This particular group of miners appear to have been unable to afford a horse (then worth around 50 pounds) which were generally used at mines like this to help pull buckets attached to ropes up and down the mine. Instead, this group brought the buckets up and down by windlass. The windlass was a wooden structure mounted over the mining shaft and fitted with a hand-cranked winch which enabled the bucket attached to the rope to be brought up and down.Gold was first discovered in Beechworth in Spring and Reid's Creek in the summer of 1852-1853. At its popularity, this region had approximately 8000 people on the gold fields searching for gold on the banks of these creeks. These periods did not require the use of heavy machinery or the digging of deep mining shafts like the one depicted in this image. Therefore, this image has important connotations for the technologies associated with mining during the approximated 1870s when gold was harder to access. This is a later period in gold history which does not fit into the "gold rush" period. Instead, it occurred after the surface gold had disappeared and therefore, is essential for researchers who are investigating the mining techniques and structures used to reach the alluvial gold which was located deeper under ground in the 1870s. This period predates the use of big heavy machinery used to mine in the 1900s which include dredges. Images such as this one can also impart essential information as to the wardrobe and fashion of men during this period. It also imparts knowledge about the landscape of Beechworth which is useful for people researching the environment and impact of gold mining in the north-east region of Victoria. In addition, since this image is a postcard reproduction of an early Australian image which may date to approximately 1990 it can impart knowledge as to the interests of people during this time period when there may have been an increase into Australian history.A sepia tone facsimile of an early Australian photograph (circa 1872) printed as a postcard.Obverse: BEECHWORTH / Victoria, Australia / Reverse: GM 2 3275 / CORRESPONDENCE / AUSTRALIAN / YESTERYEAR / CARDS / ADDRESS / Published by George Symons (057) 65 3240 / THE MINEHEAD C. 1872 / The easily gleaned gold of the early fields did / not last very long. In order to reach less / accessible alluvial gold diggers began sinking shafts as much as twenty to thirty feet down / and the mines required timbering and winches / to bring the paydirt to the top. / This syndicate has been unable to afford the / luxury of a horse (about 50 pounds) and so everything / must go up and down by windlass and rawhide / bucket. / Photo: Mitchell Library, Sydney / A sepia tone facsimile of / an early Australian photographmining album, gold mine, beechworth, burke museum, mine shaft, postcard, australian yesteryear cards, george symons, the minehead, gold fields, alluvial gold, early australia, c.1872, 1872, gold diggers, north east victoria

Plans for the magazine site in Ringwood, located at Wonga Road, Ringwood. Magazine licence 2 pages. Area map showing Warrandyte, Ringwood and Deep Creek.

Office of Mines published progressive reports on the Geological Survey of parts of Victoria.This book includes a chapter on 'Dargo and Bogong' Pages 96 - 117 and includes a fold out map of this area. These pages show heavy use.Hard deep red cover with gold printed title located at the centre top. Bound with spine blank. 217 pages. Date 1878 First chapter and some pages have pencil marks including page 97.geological survey 1878, dargo, bogong

Basin Studies are studies to evaluate water supply and demand and help ensure reliable water supplies by identifying strategies to address imbalances in water supply and demand.Spiral Bound. 157 leaves in various foliations (some folded) : illustrated. (some colour.), maps (some colour.)aerial photographs, allendale road, arthurs creek mine, arthurs creek road bridge, arthurs creek, bald spur look-out, bank protection, bolton steet, bridge street bridge, bridge street, bridges, challenger street, chute street, construction, coolaroo drive, culvert, deep creek, diamond creek basin, diamond creek region, diamond creek, diamond street bridge, drainage works, eltham lower park, eltham town park, eltham trestle bridge, eltham west drains, eltham, erosion, flood management, floods, footbridge, glen katherine estate, gold mining, gum glade, hurstbridge, kangaroo ground, kinglake escarpment, kinglake national park, latiners hat factory, main road bridge, main road, masons falls, melbourne metropolitan board of works, monash bridge, mount sugarloaf, nillumbik park, orchards, railway culvert, railway line, ramptons road, real estate advertisement, research creek, st helena east drain, st helena road, st helena, storm sewers, stormwater, sugarloaf-preston transfer main crossing, susan street, union mine, village pond, water flow, watkins street, wattletree road, weidlich road, wingrove park, yarra river, zig zag road, water supply, basin study

A history of the town of Matlock, VictoriaPaperback. Green cover. Front cover has a drawing depicting two men with packs and walking poles walking through knee deep snow past a wooden hut. In the background are several tree stumps and a small town of wooden buildings.For/ James and Lucienne/ Bailey Stamp of the Marysville & District Historical Society Inc / P.O. Box 22 / Marysville 3779gold mining, gold mine, matlock, victoria, australia, history, anne bailey, robin bailey

A postcard in a series produced by the Rose Stereograph Company in Victoria, Australia as a souvenir of Marysville.A black and white photograph of the Wolfram Track which is part of the Wilks Creek Walking Track near Marysville in Victoria. The Wolfram Track is named after the Wilks Creek Wolfram Mine which opened in around 1894. Wolframite is one of the principle ores of tungsten. The discovery was made in Wolfram Creek by a Mr Robinson who was probably a local of the district. Four creeks eventually proved to carry alluvial deposits of the ore; Wolfram Creek, Opas Creek, Quartz Creek and Main Creek. These creeks run south-east into Deep Creek, a tributary of the O'Shannassy River which, in turn, runs into the Yarra River.POST CARD The "Rose" Series/ De Luxe A Real Photograph/ Produced in Australia Published by the Rose Stereograph Co.,/ Sydney and Melbourne.wolfram track, wilks creek walking track, marysville, victoria, p. 2332, walking track, rose series postcard, postcard, souvenir, wolframite, wolfram creek, opas creek, quartz creek, main creek, deep creek, o'shannassy river, yarra river, mining

A postcard in a series produced by the Rose Stereograph Company in Victoria, Australia as a souvenir of Marysville.A black and white photograph of a part of the forest that the Wolfram Track, which is part of the Wilks Creek Walking Track, runs through. The Wilks Creek Walking Track is in Marysville in Victoria. The Wolfram Track is named after the Wilks Creek Wolfram Mine which opened in around 1894. Wolframite is one of the principle ores of tungsten. The discovery was made in Wolfram Creek by a Mr Robinson who was probably a local of the district. Four creeks eventually proved to carry alluvial deposits of the ore; Wolfram Creek, Opas Creek, Quartz Creek and Main Creek. These creeks run south-east into Deep Creek, a tributary of the O'Shannassy River which, in turn, runs into the Yarra River.POST CARD The "Rose" Series/ De Luxe A Real Photograph/ Produced in Australia Published by the Rose Stereograph Co.,/ Armadale, Victoria.wolfram track, wilks creek walking track, walking track, marysville, victoria, p. 2334, rose series postcard, postcard, souvenir, p. 2332, wolframite, wolfram creek, opas creek, quartz creek, main creek, deep creek, o'shannassy river, yarra river, mining

The photo depicts one shift of mine hands at Hanlon Consols Mine Rokewod in 1901. ist on the left is George Edgar Yung. George was born in Ararat the son of Yohann Godlip and Christina (b Weller)Yung. They lived at Happy Valley near Linton. and Piggoreet. Yohann was a miner and died in the All Nations Mine collapse at Derwnt Jack's in 1877. Interesting to note in the following information that the Hanlon Consol mamager, William Maughan was also the manager of the Try Again Mine in Piggoreet. He was also on the six man school committee of Piggoreet Common School No. 726. (Is this why George Yung ended up working in Rokewood because of a previous connection at Piggoreet? George married Clara Emma Smith from Happy Valley and worked in a mine at Allendale. They later moved to Yendon) About the Hanlon gold mining company near Rokewood. 1901 - Information Bendigo Prospecting Club, 21/08/2020. Information provided once again by Peter McCarthy. Christopher Hanlon had put down a line of bores south of the Rokewood main street, looking for a continuation of the Break O’Day lead which had been worked for two or three miles with highly payable results, though in a primitive manner. Ground was being paddocked 30 feet deep and made to pay. The bores suggested the sinking would be about 70 feet and a shaft site was selected at the back of Stanbrook’s Hotel. The Hanlon Gold Mining Company was formed in March 1895 and the shaft was bottomed at 68 feet, getting just over an ounce of gold from the shaft bottom. By January 1896, the poppet heads were up, and steam plant was nearly ready. The mine produced 846 oz by September, which was not as good as expected, but they installed a second puddling machine. The mine was profitable for the next three years, with periods of prospecting and the need to install steam pumps in 1897. A second shaft was sunk in 1899, which bottomed at 86 feet on good wash and was sunk on to 109 feet. 1743 oz of gold had been produced in six months to September 1899, but the No1 shaft was let on tribute as the No2 workings were opened and machinery installed the following year. The No1 shaft tributors broke even in 1900 and in 1901 the shaft was shut down, with the No1 shaft machinery sold late in 1902. By September 1901, the mine had produced gold worth £66,124 and the No2 shaft main drive was in 346 feet, with gold being found mainly in crevices in the hard floor. Mining continued, but once the No2 shaft workings met up with the old No1 shaft workings at the end of 1902 there was not much wash remaining. The mine was let on tribute in June 1903 and a drive was put in to test deeper ground. The company was wound up in February 1904 and the plant sold. From what they discovered, the manager concluded that the mine sat at the edge of an ancient coastline and the gold was in a beach deposit. The total gold production from the mine was worth £73,294. J Lee Archer JP, shareholder, was the manager of the Bank of Victoria in Ballarat. Born in Tasmania, he came to Victoria with his parents and first came to Ballarat in 1855 as a junior clerk with the bank. He died in 1902 aged 64. Alexander J. Peacock was a legal manager and a share broker. In 1897 Peacock, born in Creswick, had been elected as one of the Victorian delegates to the Constitutional Convention which wrote the Australian Constitution. He later became a politician, state treasurer and three times state premier of Victoria and was knighted KCGM. He died in 1933 aged 72. William Maughan, director, was an English miner who came to Victoria in the 1850s and became a mine manager, managing the Try Again at Piggoreet, Ryan’s Freehold and the Madam Berry, among others. He died in Williamstown in 1915 aged 85. Sepia photographRhs front of photo: R. Millist Phto & Lanternist Geelong Verso (upside down): ONE SHIFT OF MINE HANDS HANLON CONSOLS MINE ROKEWOOD 1901 Grandfather Yung 1st on left rokewood, hanlon consols mine, shift of mine workers 1901, gold mines, george edgar godlip yung, william maughan

Book with greenand white cover.non-fictionballarat, sebastopol hill, lydiard street, powder magazine, deep leads, james oddie, mortality, statistics, shares, stock market, alexander dewar, old gravel pits, koh-i-noor, cobb corner, wesleyan church, henry richards caselli, band of hope mine, sir william don, mine sites