The Star Hotel was built in 1863 as a private dwelling, by James Shackell who owned the Bond Store, next door. It was a small house consisting of only a couple of rooms. In 1867 Joseph Salomon bought the house and converted it into a hotel. He built an underground bar to "deal with the peculiarities of the Echuca climate". It was called 'The Shades'. In 1890 Jane Pygall bought the hotel, which was described by the Riverine Herald as having ' three parlours, seven bedrooms, underground bar, kitchen, bathroom, outhouses, small stables, and entrance from two streets." She changed the name to The Esplanade Hotel. In 1890 it was de-licensed along with many hotels in Echuca. It had been a very popular drinking place for all the wharf workers, who continued to to drink illegally in the underground bar. It was then that the escape tunnel to the laneway was built , so the drinkers could escape the Police raids. For many years it was a private dwelling, or an office. In 1973 the City of Echuca bought the Star Hotel and resored it. At the time this photograph was taken it was the main tourist information centre for the Port of Echuca. It now operates as a hotel, serving meals and providing performance opportunities for musicians.The Star Hotel is very significant in Echuca's history due to its proximity to the Echuca Wharf. It was the closest bar to the wharf. Despite Jane Pygall trying to improve the quality of her clientele, the wharf drinkers preferred to drink at The Star Hotel, as the Bridge Hotel catered for more upmarket clientele. After de-licensing in 1897, the workers continued to drink at The Shades Bar and even put in place elaborate strategies to enable them to drink illegally there. It is now a large eating and entertainment site, and the public are still able to visit 'The Shades Bar'.A coloured photograph of the Star Hotel building in Murray Esplanade. The photograph is taken from the east side of the street. The Shackell's Bond Store can be seen on the left of the photograph. Printed on the back are the words, "This paper manufactured by Kodak". Also on the back is green Port of Echuca stamp. Written across the front of the Bond Store are the words 'World In Wax Museum.' On a sign outside the Star Hotel are the words, "Port Information Centre. Ticket Sales. Souvenirs . Star Hotel 1867."port of echuca, star hotel, shackell, james, salomon, joseph, pygall, jane, esplanade hotel, 1863, underground bar, the shades, de-licensing of echuca hotels

Cloth sample book entitled "Collins Bros. Pty. Ltd. Woollen Manufacturers Geelong Shades for Slipper Socking and Scrim Felts" contains numerous coloured felt samples within two covers.Collins Bros. Pty. Ltd. Woollen Manufacturers Geelong Shades for Slipper Socking and Scrim Feltscollins bros mill pty ltd, felting

Pastel and fashion shades on wool with Erioclarite B - J.R. Geigy A.G., Basel (Schweiz)"Pastel and fashion shades on wool with Erioclarite B" - J.R. Geigy A.G., Basel (Schweiz)dyeing, j.r. geigy soc. an.

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

Tourmaline is a group of minerals belonging to the complex borosilicate mineral class. These minerals are known for their striking and varied colours, making them prized gemstones. Tourmaline crystals can come in various shades, including pink, green, blue, brown, black, and colourless. They are often transparent or translucent. Tourmaline's chemical composition is complex, but it typically includes elements such as aluminium, iron, magnesium, sodium, lithium, and potassium. The specific arrangement of these elements in the crystal lattice gives rise to the different colours and properties of tourmaline specimens. Tourmaline specimens from Beechworth, Victoria, Australia, are a notable part of the region's mineral heritage. These tourmalines are of interest to mineral collectors and enthusiasts. While the tourmaline found in Beechworth is not as well-known as some other tourmaline varieties, it has unique characteristics and a historical context associated with the gold mining areas in Beechworth.The significance of tourmaline in Beechworth, Victoria, Australia, lies in its unique geological and historical context, contributing to both scientific and cultural aspects. The tourmaline mined in Beechworth is a rare and unique variety of tourmaline that is primarily found in the historic gold mining areas surrounding Beechworth. Its occurrence is closely linked to the geological processes that shaped the region during the Gold Rush era. The discovery of tourmaline in Beechworth adds to the rich mineral heritage of the area, which was historically known for gold mining. The specimens serve as a tangible connection to the region's mining history and contribute to preserving its geological legacy. The presence of tourmaline in Beechworth showcases the mineralogical diversity of the area. Tourmaline is known for its wide range of colours and unique properties, making it a valuable subject of study for mineralogists and geologists. Tourmaline specimens from Beechworth have educational significance, providing opportunities for research and study. They offer insights into the geological processes and mineral formation in the region, contributing to a better understanding of Earth's geological history.A hand-sized solid mineral specimen in shades of brown, green, light grey and dark greyTOURMALINE (schorl) / (Silicate of boron and aluminum) burke museum, beechworth, indigo shire, geological, geological specimen, mineralogy, tourmaline

Four page fold out booklet containing coloured fabric samples and printed text. front: [printed] Fashion Shades / Autumn 1933. / SANDOZfabric samples, textile industry, fashion, sandoz, switzerland, autumn

These glasses appear to be mainly sunglasses or ones for outdoors as the tinted glass and the shades indicate this. They would have been used commonly in the past (100 years ago or more) by those able to afford the cost of the item. Eye glasses were first used in the 13th century and bi-focals were invented in the late 18th century.These items have no known local significance and are kept as interesting souvenirs of eye glasses used in the past.This is a pair of spectacles or glasses in a case. The glasses are made of thin metal and contain dark tinted glass. The eye-glass pieces are oval in shape. On the outer rims of the eye-glass pieces are two curved metal mesh covers attached to the metal rims by two screws on each side. These act as shades for the sun and side protection for the eyes and fold down when not in use. One of the shades is detached from its metal rim. The glasses case is made of cardboard and has a black mottled outer covering and a light brown inside lining. The case is much scuffed. household items, history of warrnambool, spectacles

Amazonite is classed as a Tectosilicate and is part of the Feldspar group of minerals. Amazonite forms in a triclinic crystal structure and its chemical formula is K(AlSi3O8). In appearance, Amazonite can range from shades of green to green blue to blue, and often with white streaks or veining. The greenish colour is believed to come from the small amount of lead contained in its composition. Amazonite is named after the Amazon River due to its colour and similarities to another rock found along the riverbanks, although Amazonite is not actually found at or near the Amazon. Although less commonly used in jewellery today, Amazonite has been mined and used by humans for thousands of years and Amazonite jewellery from at least 2000BCE have been discovered in North Africa. Amazonite is found in many locations around the world including Brazil, Peru, Ethiopia, Canada, Russia, Mozambique, Myanmar, Pakistan, China, Madagascar, and the United States of America. This specimen most probably comes from the U.S.A., Amazonite is found in several US states particularly in Colorado, Virginia, Pennsylvania. This specimen is of both scientific and historic significance as a striking blue green example of Amazonite mined prior to 1868 in the United States of America, most likely from Colorado, Virginia, or Pennsylvania. These three states are all locations of significant Amazonite deposits. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A palm-sized Feldspar mineral specimen from the Tectosilicate class in shades of blue-green with white veining.Existing label: green/blue Feldspar / "amazonite" / possibly USA geological specimen, geology, geology collection, burke museum, beechworth, tectosilicate, amazonite, feldspar, triclinic crystal structure, amazonite usa, amazonite colorado, amazonite virginia, amazonite pennsylvania

The firm of Harbig was a Melbourne millinery company owned by Mr and Mrs Richard Ernest Harbig. In 1949, an article in the West Australian newspaper reported their return from the United States. It records that: 'FEATHERS SYDNEY, Sept. 14: Mr. and Mr. Richard Harbig, Melbourne milliners who reached Sydney by air tonight from America, gave these details of hat trends for next winter. Shapes: Head-hugging cloches to suit short hair, cut away at the back to clear high collars, and built up and out at the front to give height. Materals: Felts, velours, velvets, and a new long-haired fur fabric called flamond. Colours: Muted pastels, few jewel shades, and no vivid colours. Trimmings: Little veiling, "but feathers and feathers and feathers".'The Kew Historical Society’s fashion and design collection is comprised of costumes, hats, shoes and personal accessories. Many of these items were purchased or handmade in Victoria; some locally in Kew. The extensive hat collection comprises items dating from the 1860s to the 1970s. While most of the hats in the collection were created by milliners for women, there are a number of early and important men’s hats in the collection. The headwear collection is particularly significant in that it includes the work of notable Australian and international milliners.Pale green woman’s hat created by Harbig of Melbourne with a large border of flowers and leaves in shades of green. The crown of the hat is swathed with pale green silk gauze.Label: Harbig. Melbourne, New York, Parismilliners -- harbig, women's clothing -- hats, floral hats

After a quiet period, interest in bookplates in Australia began to increase in the early 1970s, Entrepreneurial art and book collectors such as Edwin Jewell and others commissioned multiple Bookplate designs from a range of well known fine artists. At a 1997 meeting in Melbourne of the Ephemera Society of Australia Edwin Jewell and others announced the formation of the Australian Bookplate Society. The society was instrumental in promoting the art of the bookplate through establishment of the Australian Bookplate Design competition. The competition includes a design award for secondary schools students.shades of black and white tree in landscape.Signed beneath plate in pencil Olivia Moroney. 2020

White Glass Light Shades (5 in Box)stawell

Sixteen page knitting pattern book featuring a woman wearing a black, grey and white knitted jumper on the cover.front: [printed] SHADES OF / WINTER / 5 FREE FASHION PATTERNS FOR YOU TO KNIT / THOROBRED / scheepjeswolthorobred scheepjeswol, fashion, design, knitwear, home made, wool, pattern book

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

This piece of petrified wood was found at the sand quarry between Sunbury and Bulla.A petrified piece of wood showing various shades of brown.smith, kevin, john, wood, george evans collection

Property of Miss O.A. SebireEuropean Castilani style bangle with cameos of different shades.bangles

This specimen was recovered from Broken Hill, NSW. It was given the name Mangan Hedenbergite in 1819 by Jöns Jakob Berzelius in honor of Mr. Anders Ludvig of Hedenberg who was the first to define hedenbergite as a mineral. Hedenbergite, belongs in the pyroxene group having a monoclinic crystal system. The mineral is extremely rarely found as a pure substance. Mangan Hedenbergite is a manganese bearing variety of Hedenbergite. Manganese is the world’s fourth most used mineral after iron, aluminium, and copper primarily because it has no satisfactory substitute in its major applications. Globally, the steel industry is the primary user of manganese metal, utilizing it as an alloy to enhance the strength and workability of steel and in the manufacture of tin cans. Manganese is a key component of certain widely used aluminium alloys and, in oxide form, dry cell batteries used in electric vehicles. These batteries are in high demand. Another potential use for manganese may as an additive to help coat and protect a car’s engine. Manganese is also used for non-metallurgical purposes such as plant fertilizers, animal feed, and colorants for bricks. 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 mineral specimen in shades of silver and blackmanganese, open cut mine, manganese ore processing, bell bay, tasmania, northern territory, steel industry, zinc-carbon batteries, alkaline batteries, tin cans

This specimen was donated in 1868 by Alfred Selwyn. Olivine is typically found in basic and ultra-basic igneous rocks around the world, in a variety of colours including yellowish green, olive green, greenish black and reddish brown with a transparent to translucent diaphaneity. The luster of the specimen is vitreous, the luminescence non-fluorescent and when fractured the mineral is very brittle producing small, conchoidal fragments. Chromian diopside is normally found in small sizes as the larger the size of the mineral the darker the colour is, almost black rather than green. Chromium is the element that gives chromian diopside and emeralds their rich green colour. Diopside is found across the world in multiple colours however gem-quality chromian diopside is mined in Siberia, Russia and prominent within the jewellery industry as a more affordable substitute to emeralds. Chromium-bearing diopside has been located across Australia. Chromium-bearing Diopside is located across the world found in North America, parts of South America, and across Australia, Africa, Europe and Asia. Chromium-bearing Diopside is mined in Siberia, Russia and is sold as a commercial substitute for emeralds. The stone is often turned into jewellery. This item is one of many geological and mineral specimens that constitute a broader collection obtained from various regions across Australia (as well as some international locales) and generously contributed to the Burke Museum between 1868 and 1880. A significant portion of these specimens originated from Victoria and were acquired as a result of the Geological Survey of Victoria, initiated in 1852 during the Gold Rush era. The primary objective of this survey was to investigate and chart the geological characteristics of Victoria. The procurement of geological specimens played a vital role in advancing our comprehension of the Earth's scientific composition and was instrumental in supporting research and educational institutions throughout Australia, including the Burke Museum, in their efforts to foster further exploration and study. A solid mineral specimen in shades of green, grey and brownburke museum, beechworth, geological, geological specimen

The Kew Historical Society’s fashion and design collection is comprised of costumes, hats, shoes and personal accessories. Many of these items were purchased or handmade in Victoria; some locally in Kew. The extensive hat collection comprises items dating from the 1860s to the 1970s. Most of the hats in the collection were created by milliners for women. There are however a number of early and important men’s hats in the collection. The headwear collection is particularly significant in that it includes the work of notable Australian and international milliners.Faux wool woman’s hat made of 'polyacryl' and 'thermoplastisch' in shades of blue and yellow. While the hat is based on the shape of a fedora the design is softened by the varying shades of colour in the weave.Label: 70% Polyacryl 30% Thermoplastisch, Made in Italywomen's clothing -- hats, fedoras

Small salt glazed pottery ink well, shades of brown.domestic equipment, writing equipment, ink well

Rural City of Wangaratta Collection. Gift of the Wangaratta BPW Club for their 21st Anniversary.A landscape oil painting in shades of yellow, blue, green, and brown.Obverse: Marg Woollard 6.1977- (bottom right corner) Marg Woollard 'NATURE'S CORROBOREE'/ Y.M.C.A 1978 Art Show prize/ Presented by Wangaratta B.P.W. Club. for its 21st anniversary/ to the City of Wangaratta./ (plaque mounted on frame)wagaratta art gallery, margaret woollard, painting, landscape

Paper booklet in two shades of brown containing knitting instructions.P+B Knitting Made Easy 1941 Edition Patons + Baldwinsbooks, reference

Olivine is mostly found on the Earth's surface in igneous rocks that are dark-coloured. It is common at divergent plate boundaries and at warm spots, such as volcanic areas. It crystalises and forms during the cooling of magma. Olivine is used in refractory sand, bricks, and gemstones. Olivine has been found on a number of meteorites, which might have originated from large asteroids or the mantle of a now-destroyed planet. This olivine crystal is thought to originate from Mount Noorat, with speculation that it could have originated from Mount Shadwell. Mount Noorat is a dormant volcano cone located in the Newer Volcanics Province of Victoria. Mount Noorat belongs to the Kirrae Wuurong people, who used the Mount as a place for meetings and gatherings prior to European settlement. Contact was first made between European settlers and the Indigenous people in 1841. The Mount has mostly been used for cattle and sheep grazing. Mount Shadwell is a well-known source of olivine and is the highest of a gathering of volcanic cones. The New Volcanic Province is located in South East Australia and covers 15000 square kilometres. It contains 400 explosive vents and small shield volcanoes. The last eruption is thought to have occurred 5000 years ago at Mount Gambier and Mount Schank. This olivine crystal has been identified as a volcanic bomb, which is a molten rock which was pushed out and ejected into the air when a volcano reupts. A rock needs to be larger than 65 mm in diameter to be classified as a volcanic bomb. This olivine volcanic bomb and its locality is historically and socially significant. The olivine was found in the Newer Volcanic Province, an area which contains over 400 dormant volcanoes. This olivine is one part of a volcanic bomb, which would have ejected when magma erupted out of a volcano. 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 iron-magnesium silicate mineral with shades of green and brownburke museum, beechworth, geological, geological specimen, olivine, igneous rock, volcanic, gemstones, volcanic bomb, meteorites, asteroids, plantes, mount noorat, mount shadwell, indigenous, kirrae wuurong people, newer volcanics province, victoria, european settlement, eruption

Chert is a sedimentary rock composed of microcrystalline or cryptocrystalline quartz. While usually biological in origin, chert may also occur as a chemical precipitate or a diagenetic replacement--the product of petrified trees. Chert, also known as flint, was a common tool for early peoples during the stone age. It forms in limestone and chalk sediments as silicon dioxide microcrystals which grow into nodules of chert. Chert is found in many mines across the Northern Territory, however this specimen is sourced from the Mount Todd gold mine in Katherine. Its use in weaponry, both during the Stone Age and during the 18th century. Chert produces a spark when struck against steel, meaning t hat it can be used to start fires and fire guns. Chert was thus used in flintlock firearms, in which the gunpowder is ignited by a flint hammer striking a steel plate. Chert was commonly used in the Stone Age as a result of conchoidal fracturing causing very sharp edges, allowing early peoples to fashion weapons and cutting tools. It also rates a 7 on the Mohs Scale, making it a very hard and durable stone that maintains its sharpness. As a result, the significance of chert as a signifier of early indigenous Australian life makes this specimen important. It is also known that chert is a valuable mineral that was used as a trading commodity. Chert has also been valuable during the 1700s, proving itself to a be an important historical specimen in matters of war. A solid silicon dioxide mineral in shades of brown, white, and beigeburke museum, northern territory, chert, flint, minerals, geological specimen, katherine, mount todd gold mine, katherine northern territory

Azurite is a secondary copper mineral made by the weathering of copper sulphide ore deposits. Azurite is formed from copper, carbon, oxygen and hydrogen. There are over 45 forms of azurite that are more well-known, however over 100 forms have been found. Azurite is also commonly found together with Malachite, and Azurite is often psuedomorphed to Malachite. This specimen was found at the Great Cobar Copper Mine in New South Wales, which was founded in 1870. At the time it was one of the largest mining operations in the world. It was the largest copper mine in Australia and housed the southern hemisphere’s tallest chimney stack. The international price of copper collapsed at the end of World War 1 which led to the closure of the Great Cobar Mine on March 16th 1919. A year later on March 10th 1920 an underground fire in the CSA (Cornish, Scottish, Australian) mine started and burned for 16 years. The closure of the mine and the fire left thousands jobless and many people left the area. These were factors in Cobar facing a long stretch of poverty, until a boom in the 1960s led to the reopening of the mine. The mine still operates today, obtained by Metals Acquisition Limited in June 2023. Azurite is considered an uncommon mineral. Named for its deep blue colour, azurite was historically used for pigment making and as a gemstone, despite its softness. This specimen was donated to the Burke Museum between 1868-1880 as part of a larger collection of geological and mineral specimens. Many of the specimens in this collection were obtained as part of the Geological Survey of Victoria, which started in 1852. The Survey aimed to map the scientific makeup of the earth.A solid copper mineral with shades of darker blues almost covering it.burke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, mineralogy, cobar mines, great cobar copper mine, cobar mining, new south wales, azurite, azurite specimen

From the collection of Bette JonesHardangar worked in 1970's colours of two shades of mustard and two shades of brown on beige cloth. Possibly cushion front, central cross within a diamond shape within a square.manchester, furnishings, handcrafts, needlework

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

Rural City of Wangaratta Collection, Wangaratta Art Prize 1978.A snowscape painted in oil using shades of brown, white, blue, and green. Obverse: colby/ (bottom right corner)wangaratta art gallery, shirley colby, painting, landscape

Rural City of Wangaratta Collection, Wangaratta Art Prize 1982.A watercolour landscape painting of a pastoral scene in shades of brown, green, and blue.Obverse: NEVILLE CONNOR/ (bottom left corner)wangaratta art gallery, neville connor, landscape, watercolour painting, gapsted, pastoral

Rural City of Wangaratta Collection, Wangaratta Art Prize 1988.A coastal landscape painted in watercolour using shades of blue, green, and brown.Obverse: HERMAN/ REKEL/ (bottom left corner) WANGARATTA ART SHOW - 1988/ 150th CELEBRATION SPECIAL AWARD/ GRAND WINNER - WATERCOLOUR/ (plaque mounted on frame)wangaratta art gallery, herman pekel, coastal, landscape, painting