Galena occurs in a range of deposit contexts, often in metalliferous veins, such as Broken Hill, Australia; Coeur d’Alene, Idaho, United States.; Clausthal Zellerfeld, Germany; and Cornwall, England. Large deposits also replace limestone, dolomite, or occasionally organic matter, or have a contact-metamorphic origin. Galena is additionally found in cavities, brecciated (fractured) zones in limestone and chert, and in coal beds. This specimen was recovered from Broken Hill NSW and is 60% lead with 8-12 oz/silver to the ton.Galena or 'lead glance' is a grey lead sulfide and the chief ore mineral of lead. It forms isometric crystals in which the ionic lattice is similar to sodium chloride. Galena is brittle and easily weathers to secondary lead minerals, with the upper part of mineral deposits often containing cerussite, anglesite, and pyromorphite. It usually contains silver, which is mined along with its lead content. Other commercially important minerals that form in close association with galena are antimony, copper, and zinc. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A small-sized solid specimen containing one mineral with a sparkly silver metallic lustre exterior and pastel-grey interior.geological specimen, geology, geology collection, burke museum, beechworth, galena, lead sulphide, alfred selwyn, broken hill

Anthracite typically occurs in geologically deformed areas due to extreme heating – with temperatures ranging from 170 to 250 °C – caused by igneous intrusions or high geothermal gradients. It is most commonly found in northeastern Pennsylvania in the United States; however, smaller amounts are also found in Australia, China, eastern Ukraine, South Africa, western Canada, and other countries. This specimen was recovered from Tasmania and is 85-95% carbon.Anthracite is the mineral name for hard coal and is the least plentiful of all coal types. It is clean to the touch and, when polished, is used for decorative purposes. Before natural gas and electricity, anthracite was used for domestic heating as it produces little dust, burns slowly, and gives off a minor amount of smoke. However, it is also limited in abundance and expensive. 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 highly metamorphosed coal mineral with a black/steel-grey shiny metallic lustre.geological specimen, geology, geology collection, burke museum, beechworth, indigo shire, geological, mineralogy, victoria, alfred selwyn, anthracite

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

Selwynite is a fine-grained, compact green rock made primarily of chromian muscovite (fuchsite) and diaspore. Corundum and fuchsite can occur together in the form of massive aggregates or nodules. Often, copper carbonates are found as earthy films or tiny crystals in joint planes. The mineral name honours the late A. R. C. Selwyn, founding Director of the Geological Survey of Victoria. The particular specimen, a mottled green stone suitable for carving was recovered and found in Heathcote, Victoria, Australia. The rarity and qualities of this mineral attracted commercial mining, which was not successful, but traces of the mine shafts still exist today, and it is still highly valued by mineral collectors.Selwynit is considered to be one of the rare forms of rock because it is composed of phosphate minerals containing zirconium. This is an extremely rare combination found in nature. 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 fine grained rock composed of mainly of chromian muscovite (fuchsite) diaspore and corundum.geological specimen, geology, geology collection, burke museum, beechworth, mineralogy, heathcote, mineral collectors, selwynite, green rock, rock specimen

A granular metamorphic rock, marble is derived from limestone or dolomite and composed of calcite or dolomite interlocking grains. Heat and pressure from overlying sediments form it from limestone buried deep in Earth's crust. Graphite, pyrite, quartz, mica, and iron oxides can affect rock texture and colour. This specimen was found in Carrara, Italy. Carrara marble is the most common marble found in Italy, and it gets its name from the region where it is located. The marble was also called Luna marble and was used as a decorative element in buildings and sculptures. It has been quarried since Roman times in the Lunigiana, the northernmost tip of Tuscany, just outside the city of Carrara in the province of Massa and Carrara.Marble is one of the most popular and expensive rocks used in sculpture, architecture, interior decorations, statues, table tops, and novelties. It is available in various colors and textures depending on the chemical composition. The strength of the rock and its ability to hold finer details have made it a favorite among designers. 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 Marble (metamorphic rock) predominantly white with specks light grey and ochre geological specimen, geology, geology collection, burke museum, beechworth, marble, carrara marble, italian marble, marble specimen, tuscany

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

Laterite refers to both a rock and a soil type that is rich in clay, as well as Iron and Aluminium. It is created during a process that is called laterization, where high heat and seasonal heavy rainfall cause there to be wet and dry periods, which over time hardens the soil into rock. Because of this, most laterite is formed between tropics of Cancer and Capricorn. The iron oxide in laterite is what gives it it’s orange-red colouring. The largest religious complex in the world, Angkor Wat in Cambodia, is partially constructed of laterite, particularly its foundations, as laterite is porous and allows rainwater to drain. This specimen of laterite was collected from the Democratic Republic of Congo while it was colonised by Belgium in the 19th century. Laterite forms in many parts of the world, particularly between the tropics. It is used both for ore and as a building material, and comparing specimens from different parts of the world allows us to document the different compositions that this mineral can have when formed at different locations. 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 iron-aluminium oxide mineral specimen in shades of brown, orange and greyburke museum, beechworth, geological, geological specimen, laterite, laterite specimen, geology

Montmorillonite is a type of clay composed of aluminium silicate that forms very small particles that are not well-bonded to one another. This is why it is so soft. When in the presence of water, all types of clay swell. Montmorillonite swells even more than most types of clay, which is why it is often chosen over other types of clay in its practical uses. Montmorillonite has many different practical uses, including in the mining industry, as a soil additive, as a sealant, as a desiccant to draw water out of the air, to clean ponds, to make kitty litter and in cosmetics. Montmorillonite is a common mineral and, despite being named after Montmorillon, France, can be found all over the world, including many deposits in Australia. It is not known where this particular specimen originates from. Montmorillonite is an economically and socially significant material with a wide variety of uses. Having samples of common and important minerals allows collections, like the Burke Museum, to have a more complete view of the land on which they are located, and therefore a more complete view of heritage. 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 tennis-ball sized chunk of aluminium silicate clay. It is primarily white, accented with orange and brown.burke museum, beechworth, geological, geological specimen, clay, montmorillonite

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

It is made up of andalusite. Andalusite is a rock-forming mineral, sometimes found in granite or schist. It is often used to make glass, ceramic products, chemicals, and heat-resistant bricks as it can withstand high temperatures without changing. The chiastolite contains particles of graphite, which arranges in geometric patterns. When crystal growth occurs in the rock, the granite particles concentrate at crystal interfaces and can result in cross shapes. These ‘cross stones’ have been valued and used for their spiritual or religious meaning and used as charms, gems, or amulets. Chiastolite was first discovered in 1754, seen in a description in a published book by a palaeontologist, Franciscan priest, and Spanish author, Jose Torrubia. Deposits have been found in Australia, France, the USA, Chile, Canada, Spain, Brazil, Sri Lanka, and Russia. Deposits have been found in Western Australia and South Australia. This particular specimen was found in Bimbowrie, South Australia. Other chiastolite specimens have been found in Bimbowrie, along with jasper, quartz, and aventurine in the form of rolled pebbles or schist. This chiastolite specimen is socially and historically significant. It is a very rare sort of andalusite mineral. It is from one of only two locations where it is regularly found in Australia. The carbon cross has made it an important religious symbol in the past. Its ability to withstand high temperatures has made it a common ingredient in heat-resistant bricks and ceramics today. 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 metamorphic mineral consisting of andalusite, with a cross shaped graphite pattern in colours of grey, brown and yellowburke museum, beechworth, geological, geological specimen, andalusite, chiastolite, geometric, cross stone, spiritual, religious, australia, south australia, bimbowrie, quartz, jasper, aventurine, schist

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

Chiltern Pharmacy, now called Dow's Pharmacy, opened in 1859 at a time when the township of Chiltern was experiencing a second-wave gold rush that redistributed the balance of commercial and social activity in the region. David McEwan, father of Prime Minister John McEwan, was one of the first pharmacists practicing at the business. It was purchased in 1929 by pharmacist Hilda Dow who ran the business with her apprentice and husband, Roy Dow, until they closed the business in 1968. In 1988, after founding the North East branch of the National Trust, the Dows donated the premises with its entire fittings and stock. Some of the more than 4,000 items in stock at the time of closure in 1968 were present in the shop when the Dows took charge in 1929 and date to the late Nineteenth Century (around the time this image was taken). Hilda Dow (nee Grey) was born in 1897, the daughter of a police magistrate. She enrolled to study at the Victorian College of Pharmacy in 1919 and worked initially for Poynton's Pharmacy in Morwell before purchasing the Chiltern Pharmacy that was later named after her. She was a member of the Pharmaceutical Society of Victoria, a hospital committee and Board, the Red Cross and the Infant Welfare Association and held office for the Chiltern branch of the Country Women's Association. Her sister Helene Grey received an OBE for her work as Lady Superintendent of the Royal Melbourne Hospital. Although Hilda Dow was not Australia's first female pharmacist (this was Caroline Copp in 1880) the preservation of the pharmacy and the stories it presents sheds light on the general issue of recognition for female medical pioneers in Australia. Lantern slides, sometimes called 'magic lantern' slides, are glass plates on which an image has been secured for the purpose of projection. Glass slides were etched or hand-painted for this purpose from the Eighteenth Century but the process became more popular and accessible to the public with the development of photographic-emulsion slides used with a 'Magic Lantern' device in the mid-Nineteenth Century. Photographic lantern slides comprise a double-negative emulsion layer (forming a positive image) between thin glass plates that are bound together. A number of processes existed to form and bind the emulsion layer to the base plate, including the albumen, wet plate collodion, gelatine dry plate and woodburytype techniques. Lantern slides and magic lantern technologies are seen as foundational precursors to the development of modern photography and film-making techniques.This image is significant as it provides insight into social and commercial infrastructure available in the North-East region of Victoria in the late Nineteenth and early Twentieth Centuries. The business pictured is also associated with a Prime Minister of Victoria and some of Victoria's first female medical and pharmaceutical practitioners. Thin translucent sheet of glass with a circular image printed on the front and framed in a black backing. It is held together by metals strips to secure the edges of the slide.burke museum, beechworth, lantern slide, slide, glass slide, plate, burke museum collection, photograph, monochrome, hilda dow, roy dow, chiltern pharmacy, dow's pharmacy, chiltern, indigo shire, north east victoria, history of pharmacies, women in pharmacy, women in medicine, women in business, david mcewan, john mcewan, national trust, national trust victoria, north-east victoria national trust, heritage buildings, industrial heritage, helene grey, pharmaceutical society of victoria, victorian college of pharmacy, country women's association, caroline copp, royal melbourne hospital, red cross, infant welfare association

Isabella Park Taylor, nee Dawson (1842-1929), friend of Western Victorian First Nations people, and student of their languages and customs. Isabella grew up at "Kangatong" (1844-1866) in the company of First Nations people and became fluent in their languages. With her father, James Dawson, she wrote the book "Australian Aborigines" (1881). She married William Andrew Taylor in 1877 and they built a fine homestead on their property at "Renny Hill'' near Camperdown, Victoria. Together they had two children, Effie, born 1878 and Katherine in 1880.Studio portrait of Isabella Taylor (nee Dawson) sitting at an occasional table.cdhs, cdhsfirstnations, djargurd wurrung, djargurdwurrung

Isabella Park Taylor, nee Dawson (1842-1929), friend of Western Victorian First Nations people, and student of their languages and customs. Isabella grew up at "Kangatong" (1844-1866) in the company of First Nations people and became fluent in their languages. With her father, James Dawson, she wrote the book "Australian Aborigines" (1881). She married William Andrew Taylor in 1877 and they built a fine homestead on their property at "Renny Hill'' near Camperdown, Victoria. Together they had two children, Effie, born 1878 and Katherine in 1880. She is pictured with her grandchildren, Jack and Katherine Thornton, Effie's children.Isabella Taylor (nee Dawson) seated with her two young grandchildren Jack and Katherine Thornton.cdhs, cdhsfirstnations, djargurd wurrung, djargurdwurrung

Isabella Park Taylor, nee Dawson (1842-1929), friend of Western Victorian First Nations people, and student of their languages and customs. Isabella grew up at "Kangatong" (1844-1866) in the company of First Nations people and became fluent in their languages. With her father, James Dawson, she wrote the book "Australian Aborigines" (1881). She married William Andrew Taylor in 1877 and they built a fine homestead on their property at "Renny Hill'' near Camperdown, Victoria. Together they had two children, Effie, born 1878 and Katherine in 1880. William Taylor (1849-1927) was a farmer, Councillor and civic leader. In 1883 he gifted the world's oldest statue of Robert Burns to the people of Camperdown. William and Isabella Taylor (nee Dawson) seated together in the garden at "Renny Hill".cdhs, cdhsfirstnations, djargurd wurrung, djargurdwurrung

Isabella Park Taylor, nee Dawson (1842-1929), friend of Western Victorian First Nations people, and student of their languages and customs. Isabella grew up at "Kangatong" (1844-1866) in the company of First Nations people and became fluent in their languages. With her father, James Dawson, she wrote the book "Australian Aborigines" (1881). She married William Andrew Taylor in 1877 and they built a fine homestead on their property at "Renny Hill'' near Camperdown, Victoria. Together they had two children, Effie, born 1878 and Katherine in 1880.Studio portrait of Isabella Dawson as a young womancdhs, cdhsfirstnations, djargurd wurrung, djargurdwurrung

Charles Henry [Carl] Grove died on 17/4/1938 at Box Hill at the age of 88 and was buried in Orbost. Prior to coming to the Snowy River district, Carl worked as overseer on Buchan Station. In 1880, he selected land at Newmerella after first coming here in 1874 with early selector James A Robertson. He married Annie Robertson in 1876. Carl was a farmer, hop and seed grower and nurseryman. He was an elected Councillor of the newly formed Tambo Shire in 1882, and then in 1892 to the Orbost Shire where he served for many years filling varioius public roles. In 1911, he shifted to Queensland, but later returned to Victoria and died at Box Hill. (Ref. Nov 2014 Newsletter) Carl Grove was a prominent Orbost early settler. This document is a useful research tool.A document hand-written on foolscap sized paper. There is a "List of Species Collected by Mr Carl Grove" and a letter written by Carl Grove to the president and committee of the Mechanics Institute Orbost.document-species-list-orbost grove-carl

This is a photograph of Councillor Charles Henry Grove who represented South Riding on the Orbost Shire Council. from 1893 - 1901. He was president in 1893-1894, 1895-1896 and 1900-1901. He also served on the Tambo Shire prior to the formation of the Croajingolong / Orbost Shire. Charles Henry [Carl] Grove died on 17/4/1938 at Box Hill at the age of 88 and was buried in Orbost. Prior to coming to the Snowy River district, Carl worked as overseer on Buchan Station. In 1880, he selected land at Newmerella after first coming here in 1874 with early selector James A Robertson. He married Annie Robertson in 1876. Carl was a farmer, hop and seed grower and nurseryman. He was an elected Councillor of the newly formed Tambo Shire in 1882, and then in 1892 to the Orbost Shire where he served for many years filling various public roles. In 1911, he shifted to Queensland, but later returned to Victoria and died at Box Hill. (info. Newsletter 113)This item is associated with the Orbost Shire Council. The shire covered an area of 9,347 square kilometres and existed from 1892 until 1994 when it became part of the East Gippsland Shire Council. It is associated with Carl Grove, a prominent early Orbost citizen.A black / white head and shoulders portrait photograph of a bearded man in a suit. There is also a framed copy.grove-charles-henry grove-carl orbost-shire-council

This is a photograph of Councillor Charles Henry Grove who represented South Riding on the Orbost Shire Council. from 1893 - 1901. He was president in 1893-1894, 1895-1896 and 1900-1901. He also served on the Tambo Shire prior to the formation of the Croajingolong / Orbost Shire. Charles Henry [Carl] Grove died on 17/4/1938 at Box Hill at the age of 88 and was buried in Orbost. Prior to coming to the Snowy River district, Carl worked as overseer on Buchan Station. In 1880, he selected land at Newmerella after first coming here in 1874 with early selector James A Robertson. He married Annie Robertson in 1876. Carl was a farmer, hop and seed grower and nurseryman. He was an elected Councillor of the newly formed Tambo Shire in 1882, and then in 1892 to the Orbost Shire where he served for many years filling various public roles. In 1911, he shifted to Queensland, but later returned to Victoria and died at Box Hill. (info. Newsletter 113Carl Grove was a prominent early Orbost citizen.A small square head and shoulders photograph of a man. It is attached to a white card with tape.on front - "Mr C. Grove"grove-charles

Sand goannas are the second largest species of carnivorous lizards found across mainland Australia. They can grow up to 160cm in length and can weigh as much as 6kg. Their common name is derived from "iguana", since early European bush settlers in Australia likened goannas to the South American lizards. Goannas retain special cultural and historic significance within Australian folklore and Indigenous culture. They were an important traditional native food source and are commonly represented in Aboriginal Dreamtime stories. In some Aboriginal languages, the sand goanna is called "bungarra"; a term also commonly used by non-Aboriginal people in Western Australia. In Pitjantjatjara and other central Australian languages, goannas are called "tingka". This specimen is part of a collection of almost 200 animal specimens that were originally acquired as skins from various institutions across Australia, including the Australian Museum and the National Museum of Victoria, as well as individuals such amateur anthropologist Reynell Eveleigh Johns between 1860-1880. These skins were then mounted by members of the Burke Museum Committee and put-on display in the formal space of the Museum’s original exhibition hall where they continue to be on display. This display of taxidermy mounts initially served to instruct visitors to the Burke Museum of the natural world around them, today it serves as an insight into the collecting habits of the 19th century. This specimen is part of a significant and rare taxidermy mount collection in the Burke Museum. This collection is scientifically and culturally important for reminding us of how science continues to shape our understanding of the modern world. They demonstrate a capacity to hold evidence of how Australia’s fauna history existed in the past and are potentially important for future environmental research. This collection continues to be on display in the Museum and has become a key part to interpreting the collecting habits of the 19th century.Small goanna with a streamlined body and textured scaly skin in different shades of olive and brown. It has a long neck and a long tail which narrows towards the tip. The goanna has four short, stocky legs which meet with large, curled claws. Its mouth is slightly slightly open, and it has two black glass eyes.On tag: BMM / 5892 /taxidermy mount, taxidermy, animalia, burke museum, beechworth, australian museum, skin, reynell eveleigh johns, lizard, goanna, sand goanna, monitor lizard, various gouldii

There is no known information about the species of snake that this skin belongs to. However, generally speaking, Australia has over two hundred known species of snakes. They are elongated, legless and carnivorous reptiles with scaly, textured skin. Snakes are especially important in Aboriginal dreaming, representing one of the great and powerful forces of nature and spirit. In the Rainbow Serpent Dreamtime story, they are considered the great life giver and protector of water, which is their spiritual home. This specimen is part of a collection of almost 200 animal specimens that were originally acquired as skins from various institutions across Australia, including the Australian Museum and the National Museum of Victoria, as well as individuals such amateur anthropologist Reynell Eveleigh Johns between 1860-1880. These skins were then mounted by members of the Burke Museum Committee and put-on display in the formal space of the Museum’s original exhibition hall where they continue to be on display. This display of taxidermy mounts initially served to instruct visitors to the Burke Museum of the natural world around them, today it serves as an insight into the collecting habits of the 19th century. This specimen is part of a significant and rare taxidermy mount collection in the Burke Museum. This collection is scientifically and culturally important for reminding us of how science continues to shape our understanding of the modern world. They demonstrate a capacity to hold evidence of how Australia’s fauna history existed in the past and are potentially important for future environmental research. This collection continues to be on display in the Museum and has become a key part to interpreting the collecting habits of the 19th century.Caramel coloured long snake skin curled around in an oval shape.taxidermy mount, taxidermy, animalia, burke museum, beechworth, australian museum, skin, reynell eveleigh johns, snake skin, snake, reptile

The Freshwater Crocodile can measure up to 3 meters and is generally not considered to be a threat to humans. They reside in Northern Australia, Western Australia and the northern part of Cape York Peninsula in Queensland. They live in freshwater environments and make burrows among the roots of trees which fringe the waters they can be found in. This species of Crocodile mainly feed on invertebrate and vertebrate prey which includes insects, spiders, frogs, fish and small birds and mammals. They are also recognized as "cannibalistic" with the older Freshwater Crocodile occasionally preying on young hatchlings. These crocodiles are known for their "high walk" which they do to move on land. It is named "high walk" because the animal lifts their body off the ground using their long legs for height. They are able to walk considerable distances on land using this technique. In captivity, Freshwater Crocodiles are known to be hostile and aggressive to others of its species. This specimen is part of a collection of almost 200 animal specimens that were originally acquired as skins from various institutions across Australia, including the Australian Museum and the National Museum of Victoria, as well as individuals such amateur anthropologist Reynell Eveleigh Johns between 1860-1880. These skins were then mounted by members of the Burke Museum Committee and put-on display in the formal space of the Museum’s original exhibition hall where they continue to be on display. This display of taxidermy mounts initially served to instruct visitors to the Burke Museum of the natural world around them, today it serves as an insight into the collecting habits of the 19th century.This specimen is part of a significant and rare taxidermy mount collection in the Burke Museum. This collection is scientifically and culturally important for reminding us of how science continues to shape our understanding of the modern world. They demonstrate a capacity to hold evidence of how Australia’s fauna history existed in the past and are potentially important for future environmental research. This collection continues to be on display in the Museum and has become a key part to interpreting the collecting habits of the 19th century.The Freshwater Crocodile has a slender snout which is much smaller and thinner than its Saltwater counterpart. This specimen has dark grey and brown colouring with the darker colours concentrated around the face and upper torso of the Crocodile. There are darker stripes along the tail which features triangular scales and is long in length. The teeth are visible and bright yellow glass has been used to replace the eyes of this particular specimen. The crocodile has long but thin limbs which protrude from the sides of the body.taxidermy mount, taxidermy, animalia, burke museum, beechworth, australian museum, skin, reynell eveleigh johns, crocodile, freshwater crocodile, johnstone's crocodile

The Thylacine or Tasmanian Tiger, was a large nocturnal carnivorous marsupial now believed to be extinct that was native to both Australia and New Guinea. The Thylacine is believed to have first appeared over two million years ago with documentation of the species appearing on rock-art that have been dated as far back as 1,000BC. This specimen is part of a collection of almost 200 animal specimens that were originally acquired as skins from various institutions across Australia, including the Australian Museum and the National Museum of Victoria, as well as individuals such amateur anthropologist Reynell Eveleigh Johns between 1860-1880. These skins were then mounted by members of the Burke Museum Committee and put-on display in the formal space of the Museum’s original exhibition hall where they continue to be on display. This display of taxidermy mounts initially served to instruct visitors to the Burke Museum of the natural world around them, today it serves as an insight into the collecting habits of the 19th century. The Burke Museum Thylacine is of great historic, scientific and cultural significance as Australia's most notable example of a species made extinct within living memory. Poignant images of the last known thylacine linger in national consciousness and remain an evocative symbol of the impact of humankind on the natural environment. The Burke Museum thylacine has immense social significance not only for its ability to tell a story to present and future generations, but also for embodying the mythic tiger that lives on elusively, we hope, in the Tasmanian wilderness. Attempts to clone the thylacine from material held in museums attest to the passion that this iconic animal evokes in the scientific as well as mainstream community. Medium sized lean female thylacine with four stocky legs and a stiff tail. The fur is short and coarse and in a light brown-yellow colour with 15 dark brown stripes across the width of the body. The head is long and narrow with two small pointy ears and a large jaw with up to 30 visible teeth.taxidermy mount, taxidermy, animalia, burke museum, beechworth, australian museum, skin, reynell eveleigh johns, thylacine, tasmanian tiger, rare

The platypus is a semi-aquatic, egg-laying mammal endemic to eastern Australia. It is the sole living representative of its family and genus. They can grow up to 63cm in length and weigh up to 3kg, and their life span is typically 6-15 years. The unique mix of physical features of the platypus make it an important subject in the study of evolutionary biology, and a recognisable and iconic symbol of Australia. Furthermore, the platypus is culturally significant to several Aboriginal peoples of Australia. The animal has also appeared as a mascot at national events and features on the reverse of the Australian twenty-cent coin, and is the animal emblem of the state of New South Wales. This specimen is part of a collection of almost 200 animal specimens that were originally acquired as skins from various institutions across Australia, including the Australian Museum and the National Museum of Victoria, as well as individuals such amateur anthropologist Reynell Eveleigh Johns between 1860-1880. These skins were then mounted by members of the Burke Museum Committee and put-on display in the formal space of the Museum’s original exhibition hall where they continue to be on display. This display of taxidermy mounts initially served to instruct visitors to the Burke Museum of the natural world around them, today it serves as an insight into the collecting habits of the 19th century. This specimen is part of a significant and rare taxidermy mount collection in the Burke Museum. This collection is scientifically and culturally important for reminding us of how science continues to shape our understanding of the modern world. They demonstrate a capacity to hold evidence of how Australia’s fauna history existed in the past and are potentially important for future environmental research. This collection continues to be on display in the Museum and has become a key part to interpreting the collecting habits of the 19th century.A long, stocky platypus with a streamlined body and a flat bill. The platypus has four short limbs with webbed feet, and the front-right foot is positioned upright. The hair is short and dense; the upperbody fur has an auburn tint, and the underbody fur is a silver/cream colour. The platypus has two beady black glass eyes.On tag: BMM / 5899 /taxidermy mount, taxidermy, animalia, burke museum, beechworth, australian museum, skin, reynell eveleigh johns, platypus, monotreme, mammal, ornithorhynchus anatinus

Four species of quoll occur in Australia: the northern, spotted-tailed, eastern and western quolls. Once, most parts of Australia were inhabited by at least one of the species.Captain Cook collected quolls along the east coast in 1770, and recorded "quoll" as their local Aboriginal name. Quolls were often seen by early settlers, who called them "native cat", "native polecat" and "spotted marten", names based on familiar European animals. Since 1770, all four species have declined dramatically in numbers. This is mainly because of habitat loss or change across Australia, and introduced predators such as foxes and cats. Quolls are carnivorous marsupials with a pointed snout, a long tail and brown to black fur distinctively spotted with white. They are lively, attractive animals, with bright eyes, a moist pink nose and many sharp teeth. Like most Australian mammals, quolls are mainly active at night. Typically, they spend the day in one of their many dens, although spotted-tailed quolls and northern quolls sometimes forage and bask in the sunshine. Their large home ranges can extend for several kilometres in each direction from a smaller core range, and the range of a male quoll often overlaps those of several females. An interesting feature of their behaviour is the use of shared latrine (toilet) sites in open spaces such as rock ledges, for marking their territory and other social functions. Male quolls travel widely during the breeding season, with mating occurring during winter. All four species have a gestation period of 21 days. Because they are marsupial mammals, their young are born tiny and undeveloped and must work their way to the pouch, where they attach themselves to a teat to feed. Only the spotted-tailed quoll has a true pouch. In the other species, the young are protected by shallow folds of skin around the teats. As the pups grow, they dangle from the mother's belly; later, she carries them on her back. Quolls reach sexual maturity at one year. They have a naturally short life span, with smaller quolls living an average of only two years, and the larger spotted-tailed quoll about four to five years. The northern quoll is particularly short-lived. This specimen is part of a collection of almost 200 animal specimens that were originally acquired as skins from various institutions across Australia, including the Australian Museum and the National Museum of Victoria, as well as individuals such amateur anthropologist Reynell Eveleigh Johns between 1860-1880. These skins were then mounted by members of the Burke Museum Committee and put-on display in the formal space of the Museum’s original exhibition hall where they continue to be on display. This display of taxidermy mounts initially served to instruct visitors to the Burke Museum of the natural world around them, today it serves as an insight into the collecting habits of the 19th century. This specimen is part of a significant and rare taxidermy mount collection in the Burke Museum. This collection is scientifically and culturally important for reminding us of how science continues to shape our understanding of the modern world. They demonstrate a capacity to hold evidence of how Australia’s fauna history existed in the past and are potentially important for future environmental research. This collection continues to be on display in the Museum and has become a key part to interpreting the collecting habits of the 19th century.Average sized quoll with brown fur with white spots on body but absence on the long tail which is furry unlike the smooth body fur. The quoll has a small had with a pointed snout lined with sharp teeth, and thin membraned ears that are slightly covered in fur. The forelegs of the quoll are slightly smaller than the hindlegs, with all four legs featuring sharp clawed paws.On mounting board: BMM5984/ On Catalogue Tag (attached to left hindleg): Native Cat./ Catalogue. Page 50./ burke museum, taxidermy, taxidermy mount, fauna, animal, animalia, reynell eveleigh johns, quoll, native cat, dasyurus

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

The Great Crested Grebe is a medium to large sized bird located in Australia, New Zealand, Europe, Asia and in parts of Africa. They reside in large bodies of fresh water and are renowned for their elaborate mating dances. When breeding, the Great Crested Grebe has tawny cheek "fans" and black crests; however, in the non-breading seasons the plumage of this bird turns white. This specimen is part of a collection of almost 200 animal specimens that were originally acquired as skins from various institutions across Australia, including the Australian Museum and the National Museum of Victoria, as well as individuals such amateur anthropologist Reynell Eveleigh Johns between 1860-1880. These skins were then mounted by members of the Burke Museum Committee and put-on display in the formal space of the Museum’s original exhibition hall where they continue to be on display. This display of taxidermy mounts initially served to instruct visitors to the Burke Museum of the natural world around them, today it serves as an insight into the collecting habits of the 19th century. This specimen is part of a significant and rare taxidermy mount collection in the Burke Museum. This collection is scientifically and culturally important for reminding us of how science continues to shape our understanding of the modern world. They demonstrate a capacity to hold evidence of how Australia’s fauna history existed in the past and are potentially important for future environmental research. This collection continues to be on display in the Museum and has become a key part to interpreting the collecting habits of the 19th century.The Great Crested Grebe is a medium to large sized bird. It typically has cheek "fans" on the sides of the face and elaborate crest feathers which are shed after breeding, as is the case for this specimen. This bird is in a tall standing position with its neck stretched upwards and facing left. The small dark eyes have been made from glass and a large pointed bill. It has a metal tag tied to its left leg engraved with the numbers "4401". The skin surrounding the toes are flat which assists the bird when swimming.On tag 4401taxidermy mount, taxidermy, animalia, burke museum, beechworth, australian museum, skin, reynell eveleigh johns, great crested grebe, bird

The Red-Necked Grebe is a medium sized bird with a long neck and pointed bill. During the non-breeding months, this bird has grey, white and brown plumage. During the breeding seasons, the Red-necked Grebe has a rusty red coloured fore-neck and breast with a black bill and white cheeks. This species can be located in freshwater lakes of the northern hemisphere. This specimen is part of a collection of almost 200 animal specimens that were originally acquired as skins from various institutions across Australia, including the Australian Museum and the National Museum of Victoria, as well as individuals such amateur anthropologist Reynell Eveleigh Johns between 1860-1880. These skins were then mounted by members of the Burke Museum Committee and put-on display in the formal space of the Museum’s original exhibition hall where they continue to be on display. This display of taxidermy mounts initially served to instruct visitors to the Burke Museum of the natural world around them, today it serves as an insight into the collecting habits of the 19th century. This specimen is part of a significant and rare taxidermy mount collection in the Burke Museum. This collection is scientifically and culturally important for reminding us of how science continues to shape our understanding of the modern world. They demonstrate a capacity to hold evidence of how Australia’s fauna history existed in the past and are potentially important for future environmental research. This collection continues to be on display in the Museum and has become a key part to interpreting the collecting habits of the 19th century.A Red-Necked Grebe of medium size stylised in a standing position with the face positioned forward. The bird stands on a wooden pedestal with two tags around its legs. One tag is paper and documents cataloguing information and the second is metal and lists the number 4403. This Red-Necked Grebe has pale feathers of white, grey and browns typical of this species in the non-breeding months. The face is positioned towards the front and the small eyes are made from dark glass.On metal tag 4403. On paper tag "32. Red-Necked Grebe.Catalogue, page, 43"taxidermy mount, taxidermy, animalia, burke museum, beechworth, australian museum, skin, reynell eveleigh johns, bird, red-necked grebe