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

Ilvaite has acquired its name from Ilva (Latin for Elba) Island, Greece, where Ilvaite is most commonly found. The geological setting in which Ilvaite occurs is through contact with magnetite, zinc and copper ore deposits, along with contact metamorphic deposits and zeolite zones. llvaite crystallizes in the form of black prismatic crystals and columns . This specimen was retrieved from Broken hill, known as the world's richest and largest zinc-lead ore deposit. Because of Ilvaite's often unaesthetic crystal formations compared to other minerals, Ilvaite is uncommon in most rock collections, particularly specimens that are not well formed, such as this one. Ilvaite is also a member of the Sorosilicate subclass of the silicate minerals, which have an unusual basic unit of Si2O7, making Ilvaite a unique mineral. Given that Ilvaite is not commonly found in Australia, it marks a unique contribution to an Australian collection of minerals. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A solid hand-sized ferrous iron analogue mineral with of black with shades of beige Ilvaite is a brittle, opaque rock formation that has acquired its name from Ilva (Latin for Elba) Island, Greece, where Ilvaite is most commonly found. The geological setting in which Ilvaite occurs is through contact with magnetite, zinc and copper ore deposits, along with contact metamorphic deposits and zeolite zones. llvaite crystallizes in the form of black prismatic crystals and columns rock, mineral, ilvaite, ilvaite specimen

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

This specimen was recovered from Creswick in Victoria. Basalt is dark in colour, often black and has a fine grain. It is composed of plagioclase and pyroxene minerals and an igneous rock. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A cylindrical fine-grained piece of igneous rockburke museum, geological survey of victoria, geological specimen, geology

This specimen was recovered from Wonthaggi in Victoria. Coal is a sedimentary rock which is composed of peat after it has been exposed over millions of years. This is an example of Australian black coal which is used as either thermal or coking coal for electricity generation or manufacturing processes. It is predominantly composed of Carbon which is 'C' on the periodic table of elements. This early example of a coal sample, shows the important role that coal played/plays in Australia's energy generation and manufacturing processes. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.Small piece of black coal with museum original labelGeological survey / R..... S...../ Locality Cape Patterson coal specimen, burke museum, geological survey of victoria, geological specimen, geology

This specimen was found in Cape Patterson, Vic. Cape Paterson is a cape and seaside village located near the town of Wonthaggi, 132 kilometres southeast of Melbourne, in the Bass Coast Shire of Gippsland, Victoria, Australia. These dark, fossiliferous Mudstones were deposited in slow-moving water associated with sedimentary basins & continental shelves. They are rich in carbon which makes them almost black. This is typical of an anoxic, reducing environment such as deep water or stagnant conditions where carbon-rich material would remain unoxidised during subsequent deposition & diagenesis. it has an imprint of a leaf in the rock itself, displaying the fossil of the plant. This specimen is unique due to the leaf impression within the stone itself. Imprint fossils are formed from an organism moving in some way, leaving behind a trace or track. These tracks are preserved when the clay/silt dries slowly and is covered by other sediment. Plants can also leave imprint fossils when they are covered by sediment. The leaf tissue degrades, leaving an imprint of where the leaf once was. 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.These dark, fossiliferous Mudstones were deposited in slow moving water associated with sedimentary basins & continental shelves. They are rich in carbon which makes them almost black. This is typical of an anoxic, reducing environment such as deep water or stagnant conditions where carbon rich material would remain unoxidised during subsequent deposition & diagenesis. FOSSILIFEROUS MUDSTONE / Locality: Cape Patterson, Victoria | Descriptive catalogue / Pg 27 No 95 / "Grey Clay, / Cape Paterson with leaf impressions' / 15/4/21 C. William /mudstone, cape patterson, leaf imprint, fossilised leaf, fossiliferous mudstone

This specimen was found in Harcourt, Victoria. Harcourt is a small historic gold rush town located in a valley at the foot of Mount Alexander (741 m) in the Central Highlands of Victoria. In recent times the goldrush origins of the town have been replaced by a district known for apples, cider and wine. The Traditional owners of Harcourt are The Dja Dja Wurrung people. Granodiorite is a coarse-grained intrusive igneous rock similar to granite, but containing more plagioclase feldspar than orthoclase feldspar. Granodiorite has greater than 20% quartz by volume, and between 65% and 90% of the feldspar is plagioclase. This piece is of significance due to its provenance in Harcourt, Vic. Granodiorite is commonly produced in volcanic arcs, and in mountain buildings where it emplaces as large batholiths in mountain roots. Granodiorite is the plutonic equivalent of dacite. 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.Granodiorite is a coarse-grained intrusive igneous rock similar to granite, but containing more plagioclase feldspar than orthoclase feldspar. According to the QAPF diagram, granodiorite has a greater than 20% quartz by volume, and between 65% and 90% of the feldspar is plagioclase.GRANDIORITE. / Locality: / Harcourt, Victoria / Other label: Geological survey / R S / Loc Harcourt quarries [?] Alexander / 1/4 Sheet. | 4 | Granite /granodiorite, granite, burke museum, harcourt, coarse-grained, igneous, plagioclase feldspar, orthoclase feldspar, quartz, mount alexander, the dja dja wurrung people, the traditional owners, central highlands of victoria, gold rush

This specimen was recovered from Ceres West of Geelong, Victoria. Greenstone is the name for any metamorphosed basic igneous rock (in the case of this specimen, Gabbro) that gains its greenish colour to the presence of the minerals chlorite, actinolite, or epidote, hence the term 'green' and 'stone'. Greenstone is often formed through metamorphsis along a convergent plate boundary. In the rock cycle (the series of processes that creates the various types of rocks) there are identified three different types of rocks, which are the sedimentary, the igneous and the metamorphic. Metamorphic rocks started out as sedimentary, igneous or earlier metamorphic rocks but changed from their original condition under the effect of high heat, high pressure or hot, mineral-rich fluid. However, if pressure or heat is too high, then the rock will melt, resulting in the formation of an igneous rock. The name used to describe these types of rocks reflects this specific inherent trait of change, since the word “metamorphic” derives from the Greek word “metamorphosis”, meaning “change of form or structure”. Metamorphic rocks form in the Earth`s crust but can be also found on the surface, due to elevation of the Earth`s surface. They are divided into two categories: the foliated metamorphic and the non-foliated metamorphic rocks. Gabbro is a highly useful mineral that is often polished to create cemetery markers and kitchen benches. It is notable for its qualities of durability, being able to withstand extreme elements and wear. Whilst not rare, Gabbro is of great utility and has been highly desirable for its qualities. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.Greenstone is a solid hand-sized metamorphic mineral of a green colour. Greenstone is the name for any metamorphosed basic igneous rock (in the case of this specimen, Gabbro) that gains its greenish colour to the presence of the minerals chlorite, actinolite, or epidote, hence the term 'green' and 'stone'. Gabbro is a medium to coarse grained rocks that consist primarily of plagioclase feldspar and pyroxene. Greenstone is often formed through metamorphsis along a convergent plate boundary. Gabbro forms due to cooling and crystallization of magma underneath Earth's surface. Greenstone/Gabbro/from Ceres west/of Geelong. Has old Geological Survey label/and probably collected by/Richard Daintree in 1861/C.Willam 15/4/21/ Other label: 62 /greenstone, metamorphosed, igneous rock, gabbro, chlorite, actinolite, epidote, metamorphsis, rock cycle, various types of rocks, sedimentary, high heat, high pressure, mineral-rich fluid, metamorphosis, foliated metamorphic, non-foliated metamorphic, convergent plate boundary, greenish colour, minerals

‘Ropy lava’ is known for its sculptural and layered qualities. It occurs in specific lava flows that are slow moving and slow cooling, allowing for unique formations to be created out of the motion. Ropy Lava is a flow that has a hardened crust with molten material underneath, the tension between these states is what creates its characteristic form. The brown/red hue of the stone is an indication of age, as it is oxidised iron deposits. This rock deposit is thought to be sourced from the area by Talbot, in western Victoria. This area has a rich mineral history and experienced the gold rush in the 1850's. The traditional owners of this area are the Dja Dja Wurrung people.This geological specimen shows the conditions in which the Australian landscape was created as well as provides an indication as to how these events occurred. It is representative of a common natural process that contextualises the formation of Australia with the formation of other landmasses. 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.Hand sized specimen in brown/red hues42 / victoria, talbot, lava, ropy, ropy lava, mineral, geological specimen, geological, geological heritage, natural stone, natural history

This image shows Bethanga Bridge, which was constructed between 1927 and 1930 in Albury, NSW. The bridge was a necessity due to the building of the Hume Dam (Wier), 1919-1936. Bethanga Bridge is a long, nine-span, riveted-steel, variable depth, Pratt Truss road bridge of nine principal spans of 82 metres and a total length of 752 metres over the flooded valley of the Murray River, now part of Hume Reservoir. Because of its unique location, over the waters of a dam with the border running down the centre of the body of water, the Bethanga bridge is the only built structure shared by both New South Wales and Victoria. It was built 1.6 kilometres upstream of the dam and in 1961 was raised 300mm, with a concrete deck replacing the original wooden deck. The State Rivers and Water Supply Commission of Victoria and the New South Wales Department of Public Works were responsible for the construction works for the Hume Weir under the River Murray Waters Agreement. It is apparent that a similar joint arrangement was made for the construction of the Bethanga Bridge as part of the Hume Weir works.This photograph of the Bethanga Bridge is of historical significance as it showcases the architectural skills of Percy Allen and Vincent Packer. Additionally, it reveals the environmental landscape of the 1920s-1930s, is linked to the Hume Dam and both New South Wales and Victorian heritage. Unmounted black and white rectangular photograph. Reverse: 1997.3196 84-20-3bethanga, bethanga bridge, hume dam, pratt truss, murray river, hume weir, transportation

This rectangle black and white photograph shows a bush scene with part of a suspension rope and wooden plank bridge visible in the middle of the image. It is likely this suspension bridge was used by the Tannery workers to move between the town and the Ovens Tannery located South-West of Beechworth due to its secluded bush location, the bridge likely spanned the gorge across Spring creek. The tannery itself was located alongside Gimlet Creek, about three kilometres from town, down what is now known as Malakoff and Old Tannery Road but which at the time was remote and accessed through bushland. The Ovens tannery was stablished in 1858 by Matthew Dodd and Hallahan and later Matthew and his brother Thomas Dodd in 1866 who developed it over the years. According to Doyle, 'we have little information about its early operations except the tannery itself comprised four small buildings' by 1870 ‘a small village with gardens of vines and fruit trees surrounded the tannery’ (Woods, 121), and by 1887 the Tannery employed fifteen men. The Ovens tannery was among several new businesses establishing themselves such as a foundry that brought industrial manufacturing alongside the developing township and which strengthened the economic stability of Beechworth after the receding mining surge. According to Woods (p. 121) in the 1860’s the government spent considerable sums to establish several public buildings such as the Benevolent Asylum, the Hospital and Insane Asylum to support those in need of care in the area directly after the Indigo gold rush which had left Beechworth, a fairly remote regional and newly formed township (Gold was first discovered in Beechworth in 1852) with a number of infirm and destitute people in its wake and which due to the support and establishment of these facilities ‘made Beechworth a significant social welfare centre in Victoria’ (Woods, p. 121). The tannery provided employment and connected the regional centre with other parts of Victoria and the wider colonial outposts and would have been a welcome opportunity for those seeking work after gold was no longer a source of income.A good example of the ingenuity of regional settlers to achieve what would have been a difficult and remote construction of a bridge as a means of access. This bridge is evidence of planning and forethought and shows dedication to establishing a life in a remote landscape.Black and white rectangular photograph printed on paperreverse: / 2983 / / BMM2983 /black and white photograph, bush, suspension bridge, rope bridge, tannery, spring creek, ovens tannery, bushland, gimlet creek, matthew dodd, beechworth

Taken during the construction of the Bethanga Bridge (1927-1930), this sepia photograph shows a view of the incomplete bridge taken from inside the structure and looking down the span of the bridge from where the photographer stands. The photograph depicts an incomplete deck, with loose-looking wooden planks/panels lain along the centre in groups of three. Once complete, the original decking of the bridge was made of timber before being replaced by cement in 1961 (Victorian Heritage Database).Bethanga Bridge is of historical significance to the Indigo Shire for its associations with the construction of Hume Dam, its associations with the River Murray Waters Agreement and the River Murray Commission, and illustration of the needs and influence of the farming communities along the river in this area - particularly in relation to the building of the Weir. It also represents the collaboration between New South Wales and Victoria on a large infrastructure project, being the only built structure shared by both New South Wales and Victoria due to its location. also reflecting on the Shire's geographical closeness to this neighboring state. This photograph is part of a series that documents the construction of this well-known heritage site of significance to the Indigo Shire. It reflects upon a period of growth and change in the area.Sepia, rectangular photograph printed on matt photographic paper, unmountedReverse: 1997.3190 / Another snap of the bridge. taken on the bridge showing huge steel sides / 84-19-4 / V [in circle] 354 / KODAK PRINTbethanga bridge, hume dam, bridges album, construction, road construction, hume weir

This image shows the Punt (a kind of small boat) that took residents of Bethanga across the Murray River before the Bethanga Bridge was built. Bethanga Bridge was built between 1927 and 1930, and was made a necessity by the building of the Hume Dam. The Hume Dam, formerly known as the Hume Weir, was in construction between 1919 and 1936, which swelled the Murray River into the floodplain to the East of the dam permanently, creating Lake Hume, and isolating the residents of Bethanga and nearby towns, for whom the trip all the way around the new lake to another river crossing was a massive undertaking. The person who wrote on the back of this card instead chose to cross the river on a boat until the Bethanga Bridge became available. Interestingly, partially submerged trees can be seen in the lake in the background of this photograph, illustrating that the dam had already begun to fill the floodplain even before the bridge was built. This photograph shows the methods the residents of Bethanga used while the Bethanga Bridge was being built. This record is associated with the Heritage Listed sites of the Hume Dam and the Bethanga Bridge, and shows the environment during the process of construction and the creation of Lake HumeSepia rectangular photograph printed on matte photographic paperReverse: 1997.3189 / 84 -19 -1 / This is the snap of the Punt. / Our only means of getting out / of Bethanga for the present / Until the bridge is completed / it is 2 miles above the junction / of the Mitta + Murray. It is / 1/2 a mile wide + runs across / the Murray into NSW / Kodak Print / bethanga, bethanga bridge, hume, hume dam, artificial lake, lake hume, hume weir, flood, floodplain, boat, punt, weir, pier, dock, transport, transportation

Taken on 25 October 1930, various houses with the Hume Dam under construction are depicted in the background. The construction of the Hume Dam took place from 1919 to 1936. At the time of construction, it was the second largest dam in the world. It was also one of the earliest civil projects developed after the Federation. Some of the Dam workers consisted of World War I veterans. Dam workers often settled their families in Mitta Junction Village and Wodonga. Archaeological surveys were completed by Austral Archaeology, which was done when the Department of Land & Water Conservation was doing work to improve Hume Dam. The archaeological report that came out of the survey recommended three sites of interest where archaeological excavation should be done: Camp Ganger’s Quarters, Stableman’s Quarters, and the Industrial Dump. The excavation uncovered artefacts. Mitta Mitta: Mitta Mitta is situated between Mount Welcome and Mount Misery. It is named after the river that explorers Hume and Hovell discovered in 1824. The town would eventually become a huge gold mining town. Mitta Mitta is called Midamodunga by the local Indigenous peoples Wodonga: Wodonga is situated on the Murray River and is part of North East Victoria. Hume and Hovell: Hamilton Hume (1979-1873) and William Hilton Hovell (1786-1875). W. H. Hovell was born in Norfolk England and Hume was born in Parramatta, New South Wales Hovell and Hume undertook an exploration journey in 1824 and thought they discovered a river, which turned out to be the Murray River. They returned home in 1825, but returned to the area in 1826 and discovered coal in the area. This photo is historically significant as it shows the Hume Dam under construction in 1930. The Dam was named after Hamilton Hume, who is an important historical figure for this area as he helped discover the area where resources were found.Sepia rectangular photograph printed unmountedReverse: 84-19-5 / 1997.3185/ Values & spillway. / When completed the wall / will be as high as the / scaffolding. [featuring trademark: kodak print]construction, houses, veterans, mitta junction village, hume dam, world war i, federation, wodonga, archaeological survey, excavation, austral archaeology, department of land & water conservation, camp ganger's quarter's, stableman's quarters, industrial dump, artefacts, mitta mitta, mount welcome, mount misery, murray river, hamilton hume, william hilton hovell, hume and hovell expedition

Taken on 25 October 1930, various houses with the Hume Dam under construction are depicted in the background. The construction of the Hume Dam took place from 1919 to 1936. At the time of construction, it was the second largest dam in the world. It was also one of the earliest civil projects developed after the Federation. Some of the Dam workers consisted of World War I veterans. Dam workers often settled their families in Mitta Junction Village and Wodonga. Archaeological surveys were completed by Austral Archaeology, which was done when the Department of Land & Water Conservation was doing work to improve Hume Dam. The archaeological report that came out of the survey recommended three sites of interest where archaeological excavation should be done: Camp Ganger’s Quarters, Stableman’s Quarters, and the Industrial Dump. The excavation uncovered artefacts. Mitta Mitta: Mitta Mitta is situated between Mount Welcome and Mount Misery. It is named after the river that explorers Hume and Hovell discovered in 1824. The town would eventually become a huge gold mining town. Mitta Mitta is called Midamodunga by the local Indigenous peoples Wodonga: Wodonga is situated on the Murray River and is part of North East Victoria. Hume and Hovell: Hamilton Hume (1979-1873) and William Hilton Hovell (1786-1875). W. H. Hovell was born in Norfolk England and Hume was born in Parramatta, New South Wales Hovell and Hume undertook an exploration journey in 1824 and thought they discovered a river, which turned out to be the Murray River. They returned home in 1825, but returned to the area in 1826 and discovered coal in the area.This photo is historically significant as it shows the Hume Dam under construction in 1930. The Dam was named after Hamilton Hume, who is an important historical figure for this area as he helped discover the area where resources were found.Sepia rectangular photograph printed unmountedReverse: 84-19-2/ 1997.3188/ These are the four / release valves they are / not always open (illegible) this / when closed the water flows / over the spillway. [featuring trademark: kodak print] photograph number: 354construction, houses, veterans, mitta junction village, hume dam, world war i, federation, wodonga, archaeological survey, excavation, austral archaeology, department of land & water conservation, camp ganger's quarter's, stableman's quarters, industrial dump, artefacts, mitta mitta, mount welcome, mount misery, murray river, hamilton hume, william hilton hovell, hume and hovell expedition

Taken on 25 October 1930, various houses with the Hume Dam under construction are depicted in the background. The construction of the Hume Dam took place from 1919 to 1936. At the time of construction, it was the second largest dam in the world. It was also one of the earliest civil projects developed after the Federation. Some of the Dam workers consisted of World War I veterans. Dam workers often settled their families in Mitta Junction Village and Wodonga. Archaeological surveys were completed by Austral Archaeology, which was done when the Department of Land & Water Conservation was doing work to improve Hume Dam. The archaeological report that came out of the survey recommended three sites of interest where archaeological excavation should be done: Camp Ganger’s Quarters, Stableman’s Quarters, and the Industrial Dump. The excavation uncovered artefacts. Mitta Mitta: Mitta Mitta is situated between Mount Welcome and Mount Misery. It is named after the river that explorers Hume and Hovell discovered in 1824. The town would eventually become a huge gold mining town. Mitta Mitta is called Midamodunga by the local Indigenous peoples Wodonga: Wodonga is situated on the Murray River and is part of North East Victoria. Hume and Hovell: Hamilton Hume (1979-1873) and William Hilton Hovell (1786-1875). W. H. Hovell was born in Norfolk England and Hume was born in Parramatta, New South Wales Hovell and Hume undertook an exploration journey in 1824 and thought they discovered a river, which turned out to be the Murray River. They returned home in 1825, but returned to the area in 1826 and discovered coal in the area.This photo is historically significant as it shows the Hume Dam under construction in 1930. The Dam was named after Hamilton Hume, who is an important historical figure for this area as he helped discover the area where resources were found.Sepia rectangular photograph printed unmountedReverse: 84-19-6/ 1997.3187/ The spillway [featuring trademark: kodak print] construction, houses, veterans, mitta junction village, hume dam, world war i, federation, wodonga, archaeological survey, excavation, austral archaeology, department of land & water conservation, camp ganger's quarter's, stableman's quarters, industrial dump, artefacts, mitta mitta, mount welcome, mount misery, murray river, hamilton hume, william hilton hovell, hume and hovell expedition

Taken on 25 October 1930, various houses with the Hume Dam under construction are depicted in the background. The construction of the Hume Dam took place from 1919 to 1936. At the time of construction, it was the second largest dam in the world. It was also one of the earliest civil projects developed after the Federation. Some of the Dam workers consisted of World War I veterans. Dam workers often settled their families in Mitta Junction Village and Wodonga. Archaeological surveys were completed by Austral Archaeology, which was done when the Department of Land & Water Conservation was doing work to improve Hume Dam. The archaeological report that came out of the survey recommended three sites of interest where archaeological excavation should be done: Camp Ganger’s Quarters, Stableman’s Quarters, and the Industrial Dump. The excavation uncovered artefacts. Mitta Mitta: Mitta Mitta is situated between Mount Welcome and Mount Misery. It is named after the river that explorers Hume and Hovell discovered in 1824. The town would eventually become a huge gold mining town. Mitta Mitta is called Midamodunga by the local Indigenous peoples Wodonga: Wodonga is situated on the Murray River and is part of North East Victoria. Hume and Hovell: Hamilton Hume (1979-1873) and William Hilton Hovell (1786-1875). W. H. Hovell was born in Norfolk England and Hume was born in Parramatta, New South Wales Hovell and Hume undertook an exploration journey in 1824 and thought they discovered a river, which turned out to be the Murray River. They returned home in 1825, but returned to the area in 1826 and discovered coal in the area.This photo is historically significant as it shows the Hume Dam under construction in 1930. The Dam was named after Hamilton Hume, who is an important historical figure for this area as he helped discover the area where resources were found.Black and white rectangular photograph printer unmountedReverse: 84-20-1/ 1997.3147construction, houses, veterans, mitta junction village, hume dam, world war i, federation, wodonga, archaeological survey, excavation, austral archaeology, department of land & water conservation, camp ganger's quarter's, stableman's quarters, industrial dump, artefacts, mitta mitta, mount welcome, mount misery, murray river, hamilton hume, william hilton hovell, hume and hovell expedition

Taken on 25 October 1930, various houses with the Hume Dam under construction are depicted in the background. The construction of the Hume Dam took place from 1919 to 1936. At the time of construction, it was the second largest dam in the world. It was also one of the earliest civil projects developed after the Federation. Some of the Dam workers consisted of World War I veterans. Dam workers often settled their families in Mitta Junction Village and Wodonga. Archaeological surveys were completed by Austral Archaeology, which was done when the Department of Land & Water Conservation was doing work to improve Hume Dam. The archaeological report that came out of the survey recommended three sites of interest where archaeological excavation should be done: Camp Ganger’s Quarters, Stableman’s Quarters, and the Industrial Dump. The excavation uncovered artefacts. Mitta Mitta: Mitta Mitta is situated between Mount Welcome and Mount Misery. It is named after the river that explorers Hume and Hovell discovered in 1824. The town would eventually become a huge gold mining town. Mitta Mitta is called Midamodunga by the local Indigenous peoples Wodonga: Wodonga is situated on the Murray River and is part of North East Victoria. Hume and Hovell: Hamilton Hume (1979-1873) and William Hilton Hovell (1786-1875). W. H. Hovell was born in Norfolk England and Hume was born in Parramatta, New South Wales Hovell and Hume undertook an exploration journey in 1824 and thought they discovered a river, which turned out to be the Murray River. They returned home in 1825, but returned to the area in 1826 and discovered coal in the area. This photo is historically significant as it shows the Hume Dam under construction in 1930. The Dam was named after Hamilton Hume, who is an important historical figure for this area as he helped discover the area where resources were found. Black and white rectangular photograph printer unmountedReverse: 1997.3145/ 84-20-2construction, houses, veterans, mitta junction village, hume dam, world war i, federation, wodonga, archaeological survey, excavation, austral archaeology, department of land & water conservation, camp ganger's quarter's, stableman's quarters, industrial dump, artefacts, mitta mitta, mount welcome, mount misery, murray river, hamilton hume, william hilton hovell, hume and hovell expedition

The photograph is a reproduction of a postcard from the Rocky Mountain Mining Company. In 1875, the Rocky Mountain Extended Gold Sluicing Company Ltd was created, utilising the previous Rocky Mountain claim for the area near Lake Sambell. The company employed A.L Martin to survey an area for a tunnel underneath Beechworth and Johnson Stephens to dig it. The tunnel was built at a rate of 40 feet a month and eventually measured 800 metres. The tunnel was a true accomplishment both in the present and during the 19th century. It was considered to be a marvelous engineering feat. Beechworth is renowned for its hydraulic sluice method of mining. This involved soil being exposed to torrents of water from high-pressure hoses. From 1876 until its closure in 1921, the mine produced an astounding 47,926 ozs of gold. Companies like this were the source of income for many Chinese gold-diggers who sought to make their fortune on the goldfields of Beechworth. During the height of the rush, the town had around 7,000 Chinese inhabitants living on the outskirts of town as they were not permitted to live within Beechworth itself.This image of the Rocky Mountain mine is historically significant as the mining complex is now non-existent, with the only remains being the tunnel built in 1880 by the company, which was considered one of the greatest engineering feats of the time. The image also provides a first-hand look into the social and cultural networks at play during the 19th century with racial segregation of the Chinese at the 'Chinese Camp', as well as an insight into Beechworth's origins during the Gold Rush.Black and white rectangular reproduced photograph printed on paperbeechworth, rocky mountain mine, sluicing, gold rush, mining, gold

Alma Isabell Ashcroft was born on the 11th of July 1920 in Newtown, Beechworth. Her father and four of her brothers worked at the Tannery, her mother was recognised as the ‘district nurse’ in the area and the family were well known and at the heart of the local community. Alma joined the Beechworth branch of the R.S.L. and at the time of the interview in 2000, had been with the R.S.L for 40-50 years. This oral history recording was part of a project conducted by Jennifer Williams in the year 2000 to capture the everyday life and struggles in Beechworth during the twentieth century. This project involved recording seventy oral histories on cassette tapes of local Beechworth residents which were then published in a book titled: Listen to what they say: voices of twentieth century Beechworth. These cassette tapes were digitised in July 2021 with funds made available by the Friends of the Burke.Alma Ashcroft’s story is significant because of her personal and familial connections with Beechworth. Her family were at the heart of the community, and Alma’s association with the RSL in Beechworth spanned 4-5 decades. During the interview with Jennifer Williams, Alma also provided a rich history of the town, the locals and her extensive family.This is a digital copy of a recording that was originally captured on a cassette tape. The cassette tape is black with a horizontal white strip and is currently stored in a clear flat plastic rectangular container. It holds up 40 minutes of recordings on each side.listen to what they say, beechworth, oral history, burke museum, jennifer williams, twentieth century, ashcroft, alma ashcroft, r.s.l, community

Mr. Braz Borschman was born in Beechworth on the 1st of July 1914 at his parents home. He played for many years in the Towns volunteer Brass Band, a popular local band of about 30 members. Braz played the coronet and later the trombone. His first job was for the post office, but he spend most of his working life at the Beechworth Tannery. His interview contains lots of information about the tanning processes, including the story of 'Young Thomas', who lost his arm in a tannery accident. Braz recalls the open-air picture theatres of Beechworth, the many dances and balls, and distinct lack of cars. His testimony is rich with detail and filled with many other side-stories, including 'Blind Tommy', a self-sufficient, opium-smoking blind man of Chinese descent. This oral history recording was part of a project conducted by Jennifer Williams in the year 2000 to capture the everyday life and struggles in Beechworth during the twentieth century. This project involved recording seventy oral histories on cassette tapes of local Beechworth residents which were then published in a book titled: Listen to what they say: voices of twentieth century Beechworth. These cassette tapes were digitised in July 2021 with funds made available by the Friends of the Burke.Braz' interview is significant for the many historical details it provides about life, work, and leisure in Beechworth, particularly in relation to the period of the depression and after, which is the context which Braz' interview focuses on. His detail about the Beechworth tannery and the many open-air picture gardens is particularly rare and insightful to any social history of Beechworth. The oral history project more broadly is significant for its capture of the lives of ordinary Beechworth residents from incredibly divergent backgrounds, which has led to a rich, nuanced and diverse range of accounts of Beechworth.This is a digital copy of a recording that was originally captured on a cassette tape. The cassette tape is black with a horizontal white strip and is currently stored in a clear flat plastic rectangular container. It holds up 40 minutes of recordings on each side.listen to what they say, beechworth, oral history, braz borschman, brass band

Sister Elizabeth McGovern, Sister Mary Lacey, Sister Mary Griffiths, and Sister Gerardus Thistlewaite were all nuns of the Brigidine Order in Beechworth in the second half of the twentieth century. They had backgrounds in teaching and office work. As nuns, their contributions to the community included teaching, running camps, being there for community members wishing to talk to them or pray, and visiting prisons and hospitals. During their time in the order, the role of the nuns in Beechworth shifted due to the closing down of the Priory School, and changes in where housing for nuns was provided. The oral history also includes stories of boarding at the convent in the 1950s, and reflections on how the experience of being a nun has changed due to increasing immersion in the modern world, and the move from convent to house. This oral history recording was part of a project conducted by Jennifer Williams in the year 2000 to capture the everyday life and struggles in Beechworth during the twentieth century. This project involved recording seventy oral histories on cassette tapes of local Beechworth residents which were then published in a book titled: Listen to what they say: voices of twentieth century Beechworth. These cassette tapes were digitised in July 2021 with funds made available by the Friends of the Burke.Sister Elizabeth McGovern, Sister Mary Lacey, Sister Mary Griffiths, and Sister Gerardus Thistlewaite's interview with Jennifer Williams is revealing of the history of the Brigidine order in Beechworth, and the role religion and nuns played in the wellbeing, education, and life of the community in the latter half of the twentieth century. It is significant both for what it illustrates about the lives and motivation of the Sisters, and for what it tells us about how the role of religious education and figures shifted in Beecjhworth from 1950 onward. It is especially illuminating about the experience of women in education. This oral history account is socially and historically significant as it is a part of a broader collection of interviews conducted by Jennifer Williams which were published in the book 'Listen to what they say: voices of twentieth-century Beechworth.' While the township of Beechworth is known for its history as a gold rush town, these accounts provide a unique insight into the day-to-day life of the town's residents during the 20th century, many of which will have now been lost if they had not been preserved.This is a series of digital recordings that were originally recorded on multiple cassette tapes. The cassette tapes are black with a horizontal white strip and are currently stored in a clear flat plastic rectangular container. They up to 40 minutes of recordings on each side.Sister Elizabeth McGovern, Sister Mary Lacey, Sister Mary Griffiths, Sister Gerardus Thistlewaitelisten to what they say, listen to what they say: voices of twentieth century beechworth, nuns, brigidine sisters, brigidine convent, school, religion, prison, boarding school, modernization, food, women's history, teaching, teachers, education, hospitals, beechworth hospital, charity, old priory, father stockdale, easter, beechworth 1950s

Mrs. Hedwig Bruckner was born in Answar, Germany, in 1920. She emigrated to Beechworth in 1955 at age 32 with her two children. Her husband was a prisoner of war in Russia for 6 years. After emigrating, Hedwig worked at the Beechworth tannery, but worked for the majority (20+) of her working years as a housekeeper for Doctor Collins. Her husband worked the nightshift at the Forestry Commission. Hedwig's testimony paints the picture of a life that was "very hard". When they moved into their house in 1956, they had no money for doors. Their two eldest children were pulled out of the convent school due to lack of funds, and their son worked as a milkman from a young age to supplement the family's income. Hedwig's testimony notes language difficulties and the number of European emigrant families in Beechworth, with which the Bruckners formed community bonds. This oral history recording was part of a project conducted by Jennifer Williams in the year 2000 to capture the everyday life and struggles in Beechworth during the twentieth century. This project involved recording seventy oral histories on cassette tapes of local Beechworth residents which were then published in a book titled: Listen to what they say: voices of twentieth century Beechworth. These cassette tapes were digitised in July 2021 with funds made available by the Friends of the Burke.Mrs. Hedwig Bruckner's oral history is significant for its insight into the perspectives and experiences of European emigrant families to Beechworth, noting their unique experiences and hardships of language, food, work, forging community bonds, and adjusting to country Australian life. The oral history project more broadly is significant for its capture of the lives of ordinary Beechworth residents from incredibly divergent backgrounds, which has led to a rich, nuanced and diverse range of accounts of Beechworth.This is a digital copy of a recording that was originally captured on a cassette tape. The cassette tape is black with a horizontal white strip and is currently stored in a clear flat plastic rectangular container. It holds up 40 minutes of recordings on each side.listen to what they say, beechworth, oral history, burke museum, hedwig bruckner

Doug Craig was born in Beechworth but had lived in Stanley. His parents had been in Stanley since the 1850's. He went to secondary school in Beechworth. His family roots are from France and Scotland. Doug gave an account of his younger years as a student at Beechworth in the post war periods of 1959 to 1953, his employment and the culture within companies he worked for, the changes brought by the new drug era, working in the hospital, This oral history recording was part of a project conducted by Jennifer Williams in the year 2000 to capture the everyday life and struggles in Beechworth during the twentieth century. This project involved recording seventy oral histories on cassette tapes of local Beechworth residents which were then published in a book titled: Listen to what they say: voices of twentieth century Beechworth. These cassette tapes were digitised in July 2021 with funds made available by the Friends of the Burke.This oral history account is socially and historically significant as it is a part of a broader collection of interviews conducted by Jennifer Williams which were published in the book 'Listen to what they say: voices of twentieth-century Beechworth.' While the township of Beechworth is known for its history as a gold rush town, these accounts provide a unique insight into the day-to-day life of the town's residents during the 20th century, many of which will have now been lost if they had not been preserved.This is a digital copy of a recording that was originally captured on a cassette tape. The cassette tape is black with a horizontal white strip and is currently stored in a clear flat plastic rectangular container. It holds up 40 minutes of recordings on each side.beechworth, mental hospital, drugs, burke museum, stanley state, hospitals, hospital patients, cocky's loft, may day hills, may day

Ric Edwards was born in Melbourne, but moved to Beechworth in 1962. He had strong associations with Beechworth Prison, which is now called Beechworth Correctional Centre after 144 years. Ric had a strong role in creating the education program for the prisoners. This oral history recording was part of a project conducted by Jennifer Williams in the year 2000 to capture the everyday life and struggles in Beechworth during the twentieth century. This project involved recording seventy oral histories on cassette tapes of local Beechworth residents which were then published in a book titled: Listen to what they say: voices of twentieth century Beechworth. These cassette tapes were digitised in July 2021 with funds made available by the Friends of the Burke.Although Beechworth is famous for its history in gold, the project by Jennifer Williams is significant as it captures the everyday life and struggles of residents living in Beechworth during the twentieth century. Ric Edwards story is significant as his story brings to light the prison system in Beechworth and it gives insight into not only Ric's role in the prison, but it also gives insight into the psychology of the prisoners.This is a digital copy of a recording that was originally captured on a cassette tape. The cassette tape is black with a horizontal white strip and is currently stored in a clear flat plastic rectangular container. It holds up 40 minutes of recordings on each side.listen to what they say, beechworth, oral history, burke museum, edwards, ric edwards, beechworth prison, beechworth correctional centre