6-page document plus map, dated 21st September 1940, between the Crown and Herbert Jackson Leed, for the land shown on the accompanying map 'indicated by yellow colour' Depths indicated on lease document. On map: Mining District of Bendigo, County of Bendigo, Parish of Sandhurst. No. 11081. Net Area 24 acres, 3 roods, 3 perches. Signed by Herbert Leed and ?Walsh, Warden Clerk, Bendigo. Map shows lease holding 11081 coloured yellow. Other leases: no's. 9882 11081, 11034, 11080. Streets: Fletcher Street, and Belle Vue Road. Gullies: Derwenters Mistake Bully and Pig Face Gully on lease 11081. Quarry Hill Recreation Reserve marked and some residential allotments. Water race indicated on map. On back of document: ; Deborah United Gold Mining Company No Liability of Charing Cross Bendigo is now the proprietor of the within described estate by transfer registered on 21st November 1940 and numbered 1795202.bendigo, mining, deborah united gold mine, herbert jackson leed, deborah united gold mining. major general sir winston joseph dugan

6 page document plus map : Gold mining lease No. 11145 between Crown ( King George VI) and North Deborah Mining Company, Parish of Sandhurst, dated 14th February, 1941. Map: Lease No. 11145 'Mining District of Bendigo, County of Bendigo, Parish of Sandhurst. Total area 48 acres, 3 roods, 22 perches. Map has extensive colour key indicating depths below surface that will be mined. Crown land and surface excised shown in orange cross-hatching. Lease holdings on map: 10753, 11020, 1363 T.L., 1115 T.L., 11013, 11062, 11033, 9988. Dam shown on 11013. Railway line marked through centre of map. Map refers to central area of Bendigo and includes reference to Hargreaves Street, Violet Street, Lily Street, Breen Street and Sullivan Street.bendigo, mining, north deborah mining company, breen street, lilly street, hargreaves street, voilet street, sullivan street.

6 page document ' Gold Mining Lease Crown land Number 11307 Bendigo' plus map. Indenture document between Queen Elizabeth 11 and North Deborah Mining Company No Liability, Parish of Sandhurst, dated 20th November, 1952 re Vol 333, Folio 053. Land indicated by yellow on map and below ' a depth of one hundred and fifty feet from the surface of the land indicated by purple colour and delineated on the plan' Document signed by J. Stanistreet, Manager, North Deborah Mining Company No Liability. Map, fixed to document, heading ' Mining District of Bendigo, No. 11307, County of Bendigo, Parish of Sandhurst, Total area 13 acres 2 roods, 11 perches. Map shows large dam on Crown land, transmission line excised 150 ft., written on purple area. Underneath map ' provided that the dam indicated on the said plan is hereby reserved'.bendigo, mining, north deborah mining company

6 page document, Gold Mining Lease 11166, plus map. Indenture between Crown (King George VI) and Ronald Alexander Rankin of Bendigo, dated 24th June, 1941. Map No. 11166 Bendigo, Mining District of Bendigo, Parish of Sandhurst, County of Bendigo. Map shows lease 11166 marked in yellow with shaft, ore bins and tramway marked. Belle Vue Road , Adam Street and Griston Street shown on map. ( Golden Gully area) Dams indicated on lease holdings. Other lease holdings: 1675 T.L.9858, 10990, 11013, 11062, 11165, 11063 (void) 1172 W.R. (dam thereon) 9882 (void). Some residential lots marked along Belle Vue Road, and Adam Street. On bottom of map 21.8.41 in pencil. On last page of document : North Deborah Mining Company now the proprietor of the within described estate by transfer registered on 11th November 1914.bendigo, mining, north deborah lease, belle vue road, adams street, griston street, golden gully, ronald alexander rankin, north deborah mine.

This image taken between 1920-1930 depicts open-cut hydraulic sluicing at the Three Mile Mine, located about five kilometres south of Beechworth. Alluvial, or surface, mining began on this site in the 1850s, but was soon replaced by hydraulic sluicing methods. By the start of 1880 it is estimated that nine hundred miles of water races had been cut though soil and rock in the Beechworth district. Hydraulic sluicing employs high pressure jets of water to blast away large areas of earth and wash it down to be run through a sluice box. Gold gets caught in the sluice and the remaining slurry is washed away. Large water quantities were required for hydraulic sluicing, and the long water races and deep tailraces that were constructed were considered great engineering feats. This method of mining is extremely effective, but causes significant environmental damage and impacts to waterways and agricultural operations. Miners at Beechworth built extensive networks of races and dams to secure reliable supplies of water on a scale far greater than elsewhere in Victoria. By the 1880s Beechworth's water barons continued to hold more than half of all the water right licences on issue and undertook sluicing operations on a massive scale. The manipulation of surface and ground water via race networks was well planned and recorded in detail by local mining surveyors. The maps that were created, combined with modern geo-spatial technologies, provide a vital key in understanding the great lengths to which miners went to capture and control critical water resources. Today, Three Mile mine is called Baarmutha. The Three Mile Mine was unproductive until 1865 when John Pund and three other miners secured a fifteen year license and constructed a water race from Upper Nine Mile Creek to Three Mile Creek. In the early twentieth century Pund & Co. averaged over one thousand ounces of gold per year from the mine. After Pund's death in 1915, GSG Amalgamated Co operated the site, continuing sluicing until 1950. This image of hydraulic sluicing methods shows the extent of water-works engineering in the landscape. This photograph has historic and research potential for understanding changes to the landscape, the evolution of mining methods, and the extensive construction, manipulation and management of water networks in the Beechworth district. Black and white rectangular photograph on matte paperReverse: 7597-1 / Sluice Mining / Copied from original on loan from Webb (Qld) / Donated Nov 2009 / Baarmutha Three Mile Mine c1920-1950 / Managed by the Plain Bros then Parkinsons / Current Location is: Beechworth Animal Shelter / used for Baarmuthaburke museum, beechworth museum, beechworth, gold fields, gold rush, victorian gold rush, hydraulic sluicing, spring creek, netwown falls, mining tunnels, water races, tailraces, gold ming history, colonial australia, australian gold rushes, mining technology, beechworth historic district, indigo gold trail, indigo shire, john pund, water manipulation, water engineering, three mile creek, three mile mine, water race, large-scale mining methods, historical mining construction, alluvial mining, mining environmental impacts, baarmutha, water barons

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

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

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 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

Coorongite is a dark, rubber-like, highly resilient structureless algal deposit. In the Coorong district of South Australia it occurs in moderate quantities associated with the coastal swamps and sand dunes which extend for a considerable distance east of the mouth of the Murray. This particular specimen was recovered from the south of the Coorong River, South Australia. A type of sediment rich in organic matter, Coorongite is the unlithified end-member of the sapropelic coal series. The members of the sapropelic coal series can be ranked in order as sapropel (the unlithified form), sapropelic-lignite, and sapropelic-coal (the lithified forms) based on increasing carbon content and decreasing volatile content. Sapropel (Coorongite) is an unlithified dark, pulpy, fine organic mud containing concentrations of algae and miospores that are more or less identifiable. Coorongite is typically found as an algae like substance, that can be found in irregular size pieces. Coorongite was believed to be dried up oil due to its rubber-like texture. The Coorongite is also soft to the point where it can be cut into with a knife or it can be broken and torn by hand. Otherwise known as 'Kurangk', the Coorong River is home to the Ngarrindjeri people, which acts as both a place for gathering food and a spiritual place. In 1852 the first sight of Coorongite was found along the Coorong River. The finders mistook the Coorongite for dried up oil, which lead to the belief that there were oil reserves under the Coorong River. Between the 1860s and the 1930s the Coorong River became a place where mining oil and Coorongite became precedent. Nowadays, the local council and the South Australian Government are working together with the Ngarrindjeri people to sustain and preserve the Coorong River and the culture that is with it. 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. Selwyn went on to collect geological samples and catalogue thousands of specimens around Australia. 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.Coorongite is considered to be a mineral with a unique texture, where it can be both hard and soft. Coorongite can also be considered to be a rare mineral, as it is only located along the Coorong River and due to the mining of it, has left very few sources. It was believed at one point that Coorongite could be used to replace oil. 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.Three solid varyingly hand-sized pieces of wooden appearing organic matter derived from the river in the Coorong District in South Australia. A rubber-like, highly resilient structureless algal deposit.Specimen 245 page 69 / in Descriptive Register / "Elcestic Bitumen, / Coorangite" South of / Coorung River, South Australia . / C. WIllman / 15/4/21burke museum, beechwoth, indigo shire, beechworth museum, geological, geological specimen, mineraology, coorong, coorong river, kurangk, ngarrindjeri, south australia, coorongite, coorongite specimen

Quartz is an extremely common mineral to find across the world. Quartz can have two forms; Microcrystalline quartz or Crystalline quartz. Microcrystalline quartz is a fine grain quartz where crystalline quartz is often a large crystal. This specimen is a crystalline quartz. Made of silicon oxide, this specimen is called smokey quartz crystals because of its brownish colour. However, the colour of quartz can vary. In addition, quartz are formed in deep-seated igneous rocks and crystallized through hot aqueous solutions. This type of crystal can be found all over Australia, including Beechworth in Victoria. Other places quartz can be found is the Ashburton River area in Western Australia, Marlborough in Queensland, the Lune River area in Tasmania and Kingsgate in New South Wales. This specimen is significant because it is common to find this kind of mineral. While the location of where this specimen was originally from is unknown, it highlights the many places in Australia where quartz is found. It demonstrates that quartz makes up a large portion of Australia's geology. In addition, quartz itself can vary in its colour and shape. This specimen represents one of these variations. That being smoky quartz crystals. 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 large hand-sized quartz mineral with shades of brown and gray throughout.Smoky quartz / crystals /locality/ unknown / (needs a wash) /BBgeological specimen, geology, geology collection, burke museum, beechworth, microcrystalline, quartz, quartz mining, quartz reefs beechworth, smokey quartz crystals, crystals, crystalline, silicon oxide, brown, colour, igneous rocks, magma, ashburton river, western australia, marlborough, queensland, lune river, tasmania, kingsgate, new south wales, nsw

Kaolin is also known as china clay. This specimen came from Dunolly, Victoria and was donated to the Museum in 1868 as part of the Geological Survey of Victoria. This survey helped map and study the geology of Victoria. In Victoria, Kaolin is particularly used as a filler and coating material in paper manufacture. It can also be used in paints, ceramics, rubbers and plastics. There are many kaolin deposits in Victoria but many of these have been mined out and there is not much Kaolin left. Rocks that have a high amount of Kaolinite and it can be formed through the decomposition of other materials. There are two types of Kaolin; hard and soft kaolin. Soft kaolin's are coarse but have a soapy texture. It can also break easily. The hard kaolins have an earthly texture and are finer grained. This means that they are harder to break, unlike the soft kaolin. Hard kaolin's are formed by flocculation in salt water, a process that in basic terms, bonds particles together. Kaolin is a common material in Victoria and that is why it is significant. While this specimen was mined in Dunolly, Victoria Kaolin can also be found Pittong, Pakenham, Bulla, Hallam and Ballarat as well as many other places throughout Victoria. This specimen represents the presence of Kaolin deposits in this region of Australia. It is also significant because Kaolin has many uses and is largely beneficial to many manufacturing processes in 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.Two pieces of Kaolinite mineral with shades of white and graygeological specimen, geology, geology collection, burke museum, beechworth, kaolin, china clay, dunolly, geological survey of victoria, kaolinite, victoria, mining, mining deposits, geology of victoria, australia, filler, coating material, paper manufacture, paint, ceramics, rubbers, plastics, decomposition, materials, soft kaolin, hard kaolin, flocculation, particles, salt water

Malachite is a water soluble, crystalline, triphenyl methylene chloride salt. It has a close relationship to copper because it is common for Malachite and copper to come from the same ore. Malachite often has shades of green, making it also known as Malachite Green. As a result of it's colour, it is known for being a dye and has been used in the dye industry, the textile industry and in medical fields. Cobar in New South Wales is well known for it's mining. This is because of the number of important deposits present in the area and include three important mining belts where most of the materials are found. These are the 'Cobar belt', the 'Canbelego belt' and the 'Girilambone belt'. The 'Cobar belt' runs underneath the main town. Copper was first discovered in Cobar in 1869 and since then, many deposits of other materials have been found, including Malachite.This specimen is significant because it comes from Cobar, NSW and represents the many deposits of materials found there. Cobar has a long history of mining and is a source of Australia's copper minerals. Malachite is often found in copper deposits meaning that it is representative of Cobar's copper production. Malachite is known for it's vivid green colour and as a result, has many uses, such as meaning used as a dye. This makes it a valuable material and highly significant. 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 mineral with shades of brown , white and light green throughout.geological specimen, geology, geology collection, burke museum, beechworth, malachite, copper, water soluble, cobar, cobar mines, cobar mining, cobar nsw, nsw, new south wales, mining belts, ore, copper ore, malachite green, dye, green, dye industry, textile industry, desposits, canbelego, girilambone, alfred selwyn

It is not known where this opal originated. Common Opal is formed from silica-rich water entering the earths crust and hardening into a gel of water and silica-spheres, layered through the specimen. Common opal differs from precious opal in colouration and appearance, with precious opal including more colours, and having a translucent or glossy appearance, where common opal shows less colour and is typically opaque. It scores high on the Mohs hardness scale, and is common throughout the world, especially in Australia, where it is far more prevalent than the highly-prized precious opal. Australia is also the highest producer of opals in the modern world. 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, silica-based mineral specimen of Common Opal in shades of grey, green, and yellow, with a thick grey vein running through the centre. geological specimen, geology, geology collection, burke museum, beechworth, opal, common opal, gemstone, mining

Bituminous coal is the most common type of coal, abundantly found in ancient coal deposits which can be dated back millions of years. Often referred to as soft or black coal, this specimen exhibits a high carbon content, ranging from 76-86%. It also holds a relatively high energy density (27 MJ/kg) meaning that it releases significant amounts of energy when burned. Bituminous coal is most commonly used for electricity generation, as well as in the production of steel. This particular piece of coal was collected as part of the Geological Survey of Victoria in the nineteenth century. It originates from Cape Paterson, a seaside village located in South Gippsland, Victoria (located on Bunurong Country). The discovery of bituminous coal in this locality was first made in 1826 by explorer William Hovell. More discoveries were gradually made over the following decades and in 1859 the Victorian Coal Company commenced the first active coal mining operations in the state by sinking a number of shafts and bores near the area of Cape Paterson. Evidence of this coal-focused past can be found today at the State Coal Mine Museum in the nearby town of Wonthaggi. This specimen is significant as it was collected from the locality of Cape Paterson in Victoria, an area that has since become historically instrumental in the mining of coal and other substances in the state 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 hand-sized piece of bituminous coal with a shiny black-grey surface and jagged edges.Existing Label: BITUMINOUS COAL / Locality: Cape / Patterson, VIC. burke museum, beechworth, geological, geological specimen, state coal mine museum, wonthaggi coal mine, victorian coal company, bituminous coal, coal victoria, coal energy generation, william hovell, cape paterson, coal specimen

Malachite is a copper carbonate hydroxide mineral. It has a chemical composition of Cu2(CO3)(OH)2. It often forms within limestone where a subsurface chemical environment favourable for the formation of carbonate minerals can occur. It is a substance that can be found in many different parts of the world including: Australia, USA, Russia and the Democratic Republic of Congo. Malachite has historically been used to produce copper, with mining of the mineral dating back over a period of four thousand years. Due to its beautiful green colourations, it is also commonly used for aesthetic purposes such as in the production of sculptures and jewellery. This particular specimen was collected from the town of Burra, South Australia as part of a geological survey undertaken during the nineteenth century. The locality (located on Ngadjuri Country) has a long history of mining, particularly in copper mining, as the area is rich in copper deposits. The first significant discovery of this was made in Burra (Burra Burra Mine) in 1845 and, at the time, the mine was the largest and richest of its kind in the world, producing nearly five percent of the total world copper output. This specimen is significant as it is considered to be a rare gemstone, as many of the original deposits for the stones are significantly depleted, leaving behind very few sources. 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 copper carbonate hydroxide mineral with patterns of green colourations Existing Label: MALACHITE / Locality: Burra / S. Aust. Other Label: Confirmed / as Malachite / C. Willman / 15/4/1 / + Bill Birch burke museum, beechworth, geological, geological specimen, malachite, gemstone, green gemstone, burra, burra burra mine, burra south australia, carbonate mineral, copper, copper mining, copper mining burra, carbonate hydroxide mineral, copper carbonate, malachite mining, malachite burra, monster mine

This specimen is Cassiterite in Quartz. Cassiterite is a tin oxide metal that forms in thin crystals which can have a beautiful lustre. Quartz is made of silicon dioxide, also known as silica, and is one of the most common minerals on earth. Cassiterite has been a fundamental source of tin ore for humans throughout history, including today. Tin is an important metal that has a wide variety of human uses in different areas, from dying fabric, to making mirrors, and their most well-known use ‘tin’ cans. Tin cans are primarily made of steel and are coated with tin in order to take advantage of tin’s property of being non-corroding. This is a massive step in the history of food preservation. Tinned food first reached Australia in 1815 with early settlers, and it began to be manufactured here in the 1840s. It was incredibly popular, and was a highly exported product, which would be a contributing factor to the ‘tin mining boom’ of the early 1880s. This specimen was collected at Jingellic, New South Wales, in about 1852. Although the Goldfields of the 1800s are much more well-known, tin mines existed alongside the gold mines which began in the mid 19th century and extended almost one hundred years, to the mid 20th century. Specimens like this would have been used as evidence to justify tin mining operations in the region as an investment. 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. The Geological Survey of Victoria was headed by British geologist, Alfred Richard Cecil Selwyn (1824-1902), who was responsible for issuing over 60 geological maps during his 17 years as director. These maps were all hand-drawn and coloured and became the benchmark for accuracy for geological mapping. 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 fist-sized solid geological specimen made on one half of tin oxide, which is dark grey, and on the other side of silica, which is brown and cream.burke museum, beechworth, geological, geological specimen

There are 17 opal fields in Australia. This opal bearing stone was found in Lightning Ridge, NSW over what is known as the Great Australian Basin. This basin was formed and covers an area of 1.7 million square kilometers in eastern Australia in the Cretaceous period. This basin used to contain an inland sea, which provided an environment where silcrete eventually formed when water levels changed. This eventually seeped into other structures, and eventually hardened and formed opal. Lightning Ridge has a population of around 2000 people, with about 80 000 visitors every year. It is a historic mining town, and is known for its deposits of a rare black opal. Mining started in the area in the late 1800s, early 1900s when the black opal was discovered. This opal-bearing stone is of social and historical significance. It is from Lightning Ridge, which is well-known for being a large producer of opal stones, most famously black opal. The history of the period dates back to 140 million years, with the discovery of black opal in the early 1900s causing interest in the area. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.***A palm-sized solid mineral specimen in shades of beige and light orange*** silica based? burke museum, beechworth, geological, geological specimen, opal, opal fields, australia, lightning ridge, new south wales, great australian basin, cretaceous, silcrete, black opal, mining

Digitised video (2.73GB). Duration: 58 minutes. Recorded July, 2024. (Video is available for viewing at Ringwood & District Historical Society Archives by appointment)Guest Speaker, Peter Hanson grew up in Warrandyte surrounded by signs of gold mining activities including in his own back yard. In this presentation, Peter talks about the numerous diggings in the area, with images, maps and drawings of the mines, tunnels, shafts and structures above and below ground.

Bivouac Hut was built in 1935 on the Northern end of Mt. Bogong, on the Staircase Spur, about halfway to the summit. It was funded by Cleve Cole and he arranged for Walter Maddison to build it. Cleve Cole dedicated his life to the mountains and wanted to make them safer to visit - more huts and improved maps, pole lines and tracks. He perished in the winter of 1936 after attempting to make the first winter crossing from Mt. Hotham to Mt. Bogong on skis. The two others with him, Howard Michell and Mick Hull survived. The weather conditions were extreme at the time and having made the summit of Mt. Bogong they then became disorientated in the blizzard and came down the southern end of Bogong instead of the northern end . Howard Michell made it out to Glen Valley, a small mining town, to get help. Mick and Cleve were carried out on rough bush stretchers and Cleve died a few hours later. The Summit Hut was funded by Howard Michell and built in the 1940's. It was deliberately burnt down in the early 1980's. Bivouac hut was rebuilt in the 1980's.These photographs are of historical significance. Both huts were funded by experienced bushwalkers to provide shelter from the weather and so make walking and skiing in the area safer. They are both now gone with Bivouac being replaced with a more modern structure but there is nothing left of the Summit Hut. 5 coloured photographs, A4 in size, 4 near the summit of Mt. Bogong (Three of the Summit Hut) and one of Bivouac Hut on the Staircase Spur leading up to the summit.1. Hand written in ink on back of Photo - "Mt. Bogong Sep. 1976' - all underlined. Below this "Staircase Spur Hut The bloke in the hat me (David Jones)". 2. Handwritten in ink on back of photo - "Mt. Bogong winter 1970" (underlined). Underneathe "Same old Hut". 3. Handwritten in ink "Mt. Bogong Jan. 1969" (Underlined) Underneath "Tawonga Saddle looking towards the Summit". 4.Handwritten in ink back of photo "Mt. Bogong Jan. 1969" (underlined) Old hut near Summit, since removed, at the top of Staircase Spur. View looking out over Kiewa Valley." 5.Hand written on back of photo "Mt. Bogong Jan. 1969" (Underlined). Underneath - " Same old Hut (Staircase Spur) early morning".mt. bogong, summit hut, bivouac hut

Commissioned by George W. Bell, designed by Anthony Harvey. An old gold mining and wine growing district eighteen miles from Melbourne, now notable for its arts, crafts, good food and historic buildings. On the reverse side printed in 8 panels (3 half-folds) advertising for Montsalvat, Eltham; Kutta Mahal Gallery, Warrandyte; Country Art Store, Eltham; Eltham Crafts. Monstsalvat, Eltham; Tantoon native plants and culinary herbs, Eltham; The Claypot, Warrandyte; Research Trading, Research; Potters Cottage, Warrandyte; Graeme Law & Associates Pty Ltd, Kew.. In addition is provided The Shire of Eltham Cenenary 1871-1971 , Centenary Celebrations Programme of events from March through to August 1971.44..8 x 57.5 cm (Four copies) On the reverse side (of one copy only) is printed in 8 panels (3 half-folds) advertising and Centenary Program.eltham, warrandyte, map, advertising, montsalvat, kutta mahal gallery, country art store, the claypot, research trading, potters cottage, graeme law & associates pty ltd, eltham crafts, tantoon, shire of eltham centenary, program

Murray's Bridge over the Diamond Creek on the Diamond Creek Trail just prior to demolition and replacement with a new steel bridge. Heritage advice obtained by Nillumbik Shire Council, following a suggestion by the Eltham District Historical Society (EDHS), is that the original bridge appears to have been a simplified version of the Country Roads Board’s (CRB) standard timber bridge design of the early-to-mid 1920s. In c1990 Murray’s bridge was renovated with three recycled steel girders as part of a bike/pedestrian path in the reserve. During these alterations many parts of the bridge were removed, and some were replaced. Heritage advice indicates the condition of Murray’s bridge is poor. The remaining original parts are all in poor condition, with severe weathering, splitting and rot, especially to the stringers retained on the bridge. Heritage advice is that Murray’s Bridge does not have sufficient significance in the cultural history of the Nillumbik area to warrant inclusion in the Nillumbik Shire Heritage Overlay and also does not have sufficient significance as a rare survivor to warrant inclusion in the Nillumbik Shire Heritage Overlay. There are no indications in the historical record that this site was individually important to the cultural history of this area. EDHS is comfortable with the heritage advice provided to Council and has worked closely on this project with Council. EDHS has suggested some of the removed timbers be used in the vicinity of the bridge for landscaping and possibly seating, so as to retain these remnants close to the site of the original bridge, which is the last old timber bridge along the lower reaches of the Diamond Creek. Mary (Sweeney) Murray and John Wright Murray selected 80 acres, Lot C Section 16 and Lot 5 Section 17 Parish of Nillumbik, under an occupation license in 1866. John died in 1867 and freehold was granted to his son John in 1873. The farm was known as ‘Laurel Hill’. John Junior was an Eltham Shire councillor and sometime president from 1887 up until 1897. He added Lot A Section 16 to the farm in ca1888. John and his younger brother James arranged to rent/purchase Lot B Section 17, across Diamond Creek to the west, in ca1900. It appears that John and James farmed separately for a few years, with a new homestead built for James ad family on the high point of Lot B Section 17 in ca1910. John sold off Lot 5 Section 17 in 1912. When John died in 1912 James took over the land on both sides of the Diamond Creek. The old homestead on the west side of the Creek disappeared. A farm bridge over Diamond Creek from this period may have been located close to the northern boundary of the farm. John Langlands, owner of the farm known as ‘Ihurst’ on the west side of Diamond Creek to the south of the Murray’s land, died in 1907. In 1909 his land was then subdivided into 100 lots to become the ‘Glen Park Estate’. Other similar subdivisions of nineteenth century farms around Eltham in this period included the ‘Franktonia (or Beard’s) Estate’ to the northeast and ‘Bonsack’s Estate’ between Eltham and Greensborough. Soon after the opening of the railway extension line from Eltham to Hurstbridge in 1912, Glen Park and nearby residents including James Murray agitated for a railway station or siding to be located half-way between Eltham and Hurstbridge, so that the Glen Park residents who used the railway daily did not have to walk into the Eltham or Hurstbridge stations. Some believed Coleman’s Corner (opposite Edendale Farm) was an appropriate spot for the platform. James Murray was among those who thought the railway should be located on his land, closer to half-way between Eltham and Hurstbridge stations. The Railways Commissioners warned that the locals would have to fund these works themselves. The Glen Park Estate residents initially had difficulty accessing Eltham by road, with only an old low-level bridge over Diamond Creek at the south end of their estate. A new timber trestle bridge across the creek, now on Wattletree Road, was opened in 1915. Road access to the north was gained in 1927 when the new Murray’s Road, which crossed the Murray’s land, was built. Residents continued to agitate for a Glen Park station. By 1926 the Railways Commissioners’ preferred site was on the Murray’s land. They arranged an estimate of cost of a full-length platform. The estimate was too much for the locals, who in 1928 argued unsuccessfully for a shorter and hence cheaper platform. By 1929 Murray had agreed to donate the land, but the locals would still have to fund the works. Murray decided, unilaterally it would appear, to commence work on a timber trestle road bridge over Diamond Creek to link the new Murray Road to the proposed station. Late in 1929 he stopped work on the bridge, for reasons unknown, but started work again and completed the bridge in 1931. There is no further newspaper evidence of the campaign for the Glen Park station until 1939, when Murray and another local, Mr Maxwell, met the Railways Commissioner. The Glen Park locale now included 45 homes on the west side of the creek and 20 on the Eltham side. Most of the residents used the train every day. The Commissioner remained adamant that only a full-length platform could be built for safety reasons. It appears the campaign dissolved at this point. The increasing move to cars may have had an impact. There is no evidence of Murray’s bridge ever being connected to Murray’s Road, or of it having wide use for any purpose by locals. James Murray died in 1947 and the farm was taken over by his son James (Jim). Jim started to sell off parts of the farm in the 1980s, retaining a few acres around the ca1910 homestead and building a new house there. Recreation reserves were established along the creek. In ca1990 Murray’s bridge was renovated with steel girders as part of a bike/pedestrian path in the reserve. The old farmhouse was demolished in ca2014. * * * A theory posted on local community Facebook groups was that the bridge was built in the 1860s and was built to be more robust than was necessary for the movement of cows from one side of the creek to the other. It was suggested the robustness was necessary to support the weight of gold ore being transferred from a mine on Murray’s land to a railway siding near Murrays Bridge (presumably for transfer and processing at Diamond Creek). Perhaps this may have been one of the motivators for Murray, who really knows? Knowing when mining operations ceased on his land and how that fits the overall timeline would be useful but at the time the bridge was built, local gold production was minimal at best. The known facts are: • The railway line came to Eltham in 1902. • The extension of the railway from Eltham to Hurstbridge was constructed in 1912 so no railway line even existed through Murray's property until 1912 and the Victorian Railways maps at the time show no such siding on Murray’s property. • In 1923 a new company was formed in anticipation of the old Diamond Creek Gold Mine being re-opened. The mine had been previously closed and flooded. It was noted in the press at the time that the mine was within a mile of the railway. Nothing really came of this. • Construction of Murrays Bridge was commenced by James Murray in early 1929 in anticipation of a proposed flag station being nominated on his land, but work ceased shortly afterwards. The proposed flag station was commonly referred to as Glen Park as the residents of the Glen Park Estate wanted Option 1, located near them with the platform adjacent to Colemans corner. This was probably never going to fly as it was virtually in eyesight of Eltham station. Allandale Road was the third option, but the Commissioners' preferred option was No. 2 - on Murray's property. • The Railway Commissioners were not going to finance any such station and the works had to be funded by private landowners and residents, hence Murray investing in this himself. • Murray recommenced work two years later and finished his bridge in 1931 but unfortunately for him, the proposed flag station never eventuated. The bluestone siding you reference may well have been built by Murray as part of the proposed station platform. • Up until then, apart from the Main Road bridge, which was washed away in 1924, virtually all local crossings over the Diamond Creek were low lying bridges – Kaylocks Bridge at Brougham Street, Diamond Street bridge, Glen Park Road bridge. It is expected that Murray also had a low-lying bridge to connect his land either side of the creek. These were all washed away or severely damaged multiple times in the 1920s. Lessons were learnt, and Murrays Bridge appears to have been built in accordance with Country Road Board standards of the time. Flood damage was ongoing, and even more recently constructed raised bridges kept getting washed away, e.g., the new Wattle Tree Road bridge in 1958 just months after completion. Murray’s bridge was reinforced with steel some 30 years ago presumably to provide additional floodwater resistance, given the history of bridges disappearing in floodwaters. • In March 1932 it was reported in the Advertiser that there were still some prospectors operating around Eltham North who apart from further scarring the face of the earth over the previous two years had gained significant experience but little gold - hardly a driving factor for constructing a dedicated railway siding and bridge to transfer gold ore. It is far more probable that James Murray was hoping to have the railway station located on his property and invested his money by building the bridge to lead to it as well as a station platform. Had the station eventuated, it may well have driven up the value of his land for subdivision and new housing estates like the Glen Park Estate. That did not eventuate. Whilst the bridge was indeed old (90 years), the core structure being completed in 1931, it had been modified substantially from original and hence had no significant historic value – i.e., it was not a representative example of its type, construction, and age. Given that the bridge was not worthy of saving, the Eltham District Historical Society with Council’s support, and the Eltham Woodworkers group endeavoured to see what suitable sized timbers were salvageable to fabricate a commemorative seat. Unfortunately, the experts at the Woodworkers group were unable to salvage any suitable length/width timbers to fabricate the seat due to the presence of rot. Last remaining wooden trestle bridge on the Diamond Creek Trail just prior to demolition and replacementBorn digital image (27)diamond creek (creek), diamond creek trail, murrays bridge, ‘laurel hill’, john wright murray, mary (sweeney) murra, john murray jnr, james murray, john langlands, ‘ihurst’, ‘glen park estate’, beard's estate, franktonia, bonsack's estate, glen park estate, glen park railway station

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

Heritage site report and gazetteer by David Bannear, head consultant for archealogy for the Department of Natural Resources and Environment. Includes information on the Warrandyte Goldfield and the Caledonia Goldfield, Queenstown (now known as St Andrews), One Tree Hill, Kingston (now known as Panton Hill), Kangaroo Grounds, You You Hill, Kingstown, South Morang, Nillumbik, (now known as Diamond Creek), Steele's Creek, Yarrambet and Kinglake. Photocopy of map headed: Location of mines and reefs from Geological survey of Victoria, Yan Yean with the Diamond Creek prominant on the map. no date35 page report with map and print out of cover letter (email form) from donorcaledonian gold fields, caledonina gold field, david bannear, gold mining, harry gilham collection, queenstown, st andrews, warrandyte goldfield

A pictorial history of the heyday of the Walhalla-Wood's Point gold belt in the 1860's-1960'sHardcover. The cover is a gold colour. The front cover has a photograph of a group of miners in front of the entry to a mine. On the top entry timber piece is a sign saying "Old Mine". The beginning of the wording is obscured by one of the miners standing in front of the entry. There is also an old mining trolley standing on tracks which lead into the mine.There is also an old gold mining dish sitting on a rock to the left of the entry into the mine.On the back cover is a photograph of Walhalla in modern times as well as a photograph of the publisher of this book. There is also a blurb about the publisher.Stamp of the Marysville & District Historical Society Inc / P.O. Box 22 / Marysville 3779gold, gold fields, gold mining, a1 mine settlement, aberfeldy, beardmore, black river group, coopers creek, donnellys creek, enochs point, fulton creek, gaffneys creek, gooleys creek, jamieson, jordan valley, kevington, knockwood, matlock, ten mile, walhalla, wood's point, history, victoria

A history of a gold mining town in the Gippsland area of Victoria Paperback. Gold cover. Cover has a pencil sketch of a gold mining town as well as a large gum tree on the back cover. Cover illustration runs across the whole cover.Stamp of the Marysville & District Historical Society Inc / P.O. Box 22 / Marysville 3779. Sticker - DISTRIBUTED BY: / Paoletti's (Adventurer) Maps P/L / 15 Nirvana Close, / Langwarrin. 3910 / Tel: 03 9789 6985 / Fax: 03 9776 6798 / Email: [email protected] / Other products & information Website: http://users.netlink.com.au/~maptrapgold, gold mining, gold town, gippsland, victoria, australia, history, gold miner, morgan, dorothy, morgan, marjorie

A history of the Donnelly's Creek gold mine in VictoriaPaperback. Front cover has a drawing depicting two horses carrying packs followed by a man mounted on a horse. There is also two men on foot following with packs and walking poles. They are walking along a forest track that has some tree stumps alongside it.The back cover has two colour photographs. The top one is of an old wooden building with what appears to be an attached lean to. Both of the buildings have stone chimneys. There is a group of people sitting and standing outside the main building. The bottom photograph appears to be the ruins of a building and a fence. There are three people viewing the ruins.The captions accompanying the photographs are: History revisited - O'Sullivans Old Toombon Hotel Recreated and Remnants of a Bygone Mining Era.Stamp of the Marysville & District Historical Society Inc / P O Box 22 / Marysville 3779gold, gold miner, gold mining, gold field, gippsland, victoria, australia, history, fulton's creek, seaton, walhalla, aberfeldy, jericho, wood's point

A history of the Wood's Point and Jordan gold fieldsPaperback. Beige cover. Front cover has a black and white photograph of miners standing and sitting around a mine cart that is sitting on railway tracks at the entrance to a mine.Back cover has a cartoon drawing of a pack horse that has fallen down a cliff with his rider trying to pull him back up by his tail. Inside the cover is a drawn map entitled 'Map of the Mining District round Wood's point'.Stamp of the Marysville & District Historical Society Inc / P.O. Box 22 / Marysville 3779 gold, gold field, gold mining, gold town, wood's point, jordan goldfields, victoria, australia, history, r w christie

A history of the Wood's Point and Jordan gold fieldsPaperback. Beige cover. Front cover has a black and white photograph of miners standing and sitting around a mine cart that is sitting on railway tracks at the entrance to a mine.Back cover has a cartoon drawing of a pack horse that has fallen down a cliff with his rider trying to pull him back up by his tail. Inside the cover is a drawn map entitled 'Map of the Mining District round Wood's point'.Stamp of Marysville & District / Historical Society Inc / P.O. Box 22 / Marysville 3779 gold, gold field, gold mining, gold town, wood's point, jordan goldfields, victoria, australia, history, r w christie