Yellow soft covered report of 95 pages . The contents of the report include: Parks, reference areas, wildlife reserves, water production, harwood production, softwood production, flora Reserves and Flora and Fauna reserves, bushland reserves, historic area and reserves, rivers and streams, Roadside conservation and Highway parks, Education areas and School Plantations, Lake Reserves, geological reserves, recreation, scenic reserves, agriculture, mineral and stone production, utilities and survey, township land, Uncommitted Land, military training, other reserves and public land. Maps include: The Study area 1: 250 000 Supplementary Mapsland conservation authority, ballarat, endowment plantations, pine plantations, langi ghiran state park, mount buangor state park, enfield state park, ballarat-creswick regional park, rossbridge, black lake, flax mill swamp, dereel lagoon, lake bolac, lake wongan, langi ghiran reservoir, gong gong reservoir, pincotts reservoir, beales reservoir, wilsons reservoir, moorabool reservoir, korweinguboora, korweinguborra reservoir, learmonth bores, sago hill, illabarook reservoir, ballarat water commission, dunneworthy, mount cole, mont lonarch, ben major, waterloo, trawalla, linton, ross creek, canadian, shepherds flat, lal lal, mount doran, raglan, chute, carngham, buninyong, watsons hill, enfield, cape clear, illabrook, rokewood junction, mount warrenheip, nerrina, jubilee, golden stream, australasian deep lead mine, happy valley school, piggoreet, berringa, bulldog, ballarat common, wildlife, water, timber, flora, rivers, geology, agriculture, warrenheip, biodiversity

Garnet is a popular gemstone used in jewellery due to its hardness and durability. There are about 5 varieties of Garnet, which distinguish the colour of each stone. In Australia mostly Pyrope and Aimandine varieties are found; Pyrope, which is blood-red to black and Aimadine, which is brownish-red to black. Other varieties are rarely found in Australia. The garnets visible in this specimen are likely Pyrope. Galnea is the natural mineral form of lead sulphide and has had various uses throughout history; from makeup to car batteries. It was first mined in South Australia in 1841. Green feldspar is an amazonite mineral, a variety of the potassium feldspar called microcline. This particular mineral is considered uncommon. It has been used in jewellery throughout history. It is likely that this specimen was found in Broken Hill, NSW, presumed due to findings of specimens with similar combinations. Broken Hill is Australia’s longest-lived mining city. The city’s fortunes have come and gone against an extreme economic background of boom and bust which continues today.This geological specimen is a rarity, given that is formed of three distinct minerals and the richness of colour that remains visible in this item attests to the strength of each structure. As we cannot pinpoint exactly where this specimen was found further research can only strengthen what is known about mining within Australia. As such the item is significant due to its scientific rarity and its ability to represent three specimens in one. A solid palm-sized mineral that features shades of grey, red and green. garnet, galnea, green feldspar, minerals, mining, rare specimen

Sphalerite or sphaelerite is named from the Greek word for 'treacherous' or 'deceiver' as specimens can vary widely in appearance, making them hard to visually identify. It is a zinc sulfide with the chemical composition (Zn,Fe)S, the most important ore of zinc. Specimens of sphalerite can contain iron as a substitute for up to 25% of the usual zinc present, as well as trace elements of gallium, cadmium, geranium and indium. Small amounts of arsenic and manganese may also be detected. Sphalerite is found in igneous, sedimentary and metamorphic rocks. It forms when carbonate rock encounters acidic, zinc-bearing fluid. It often forms in veins or in fissures of the existing rock, with colours and crystal shapes dependent on the composition of the the combining elements. It forms isometric crystal shapes including cubes, tetrahedrons, octahedrons, dodecahedrons. This specimen was collected in approximately 1852, in Broken Hill, NSW, as an adjunct to the Geological Survey of Victoria. It was donated to the Museum in 1868. Victoria and other regions of Australia were surveyed for sites of potential mineral wealth throughout the 19th Century. The identification of sites containing valuable commodities such as gold, iron ore and gemstones in a locality had the potential to shape the development and history of communities and industries in the area. The discovery of gold in Victoria, for instance, had a significant influence on the development of the area now known as 'the goldfields', including Beechworth; the city of Melbourne and Victoria as a whole.The specimen is significant as an examples of surveying activity undertaken to assess and direct the development of the mineral resource industries in Victoria and Australia, as well as the movement to expand human knowledge of earth sciences such as mineralogy and geology in the nineteenth century.A pipe-shaped specimen of sulfide-mineral zinc ore displaying patches of black, brown, beige and gold colouring. The main item has associated broken pieces. geological specimen, geology, geology collection, burke museum, beechworth, mineralogy, indigo shire, geological survey, sphalerite, sphaelerite, zinc ore, broken hill, nsw, victoria, galena, fluorite, chalcopyrite, lead, cadmium, gallium, germanium, indium, iron