Flora and fauna found through the Otway Ranges interspersed with historical references from aboriginal occupation to the present day.The Otway Ranges.Trevor Pescott. 1st ed. Belmont (Vic); Yaugher Print; 1998. 112 p.; illus, map, bibliography. Soft cover. ISBN 0 9586562 1 5otway ranges; natural history; description; travel; geology; timber;

The Report describes and assesses the natural resources of public land in the Corangamite study area, and provides a factual basis on which members of the community may base their submissions to the Council.Report on the Corangamite study area. Land Conservation Council. Melbourne; Land Conservation Council; May 1976. x, 310 p.; illus, maps (separate). Soft cover.land conservation council; corangamite; geology; physiography; climate; water resources; soils; vegetation; fauna;

Prospectus of the Victorian Gold Association N.L. Based on a report by Messrs H. W. Gepp Consultant on Development to the Commonwealth Government and W. Baragwanath, Director of the Geological Survey of Victoria. Dated 1931 This company was formed to investigate the Deborah Mine, The Central Nell Gwynne Mine and the Monument Hill Mine. 12 pages including maps and Transverse Sections of the MinesThe Commonwealth and Victorian State Governments. E. Whitehead & Co., Pty., Ltd Printers 21 Equitale Place, Melbourne, C1.gold, mining, prospectus, bendigo, gold mines, victorian gold associatian, deborah mine, central nell gwynne mine, monument hill mine.

Gwen McWilliam is well known as an authority on the history of Boroondara and the author of a large number of books and pamphlets about the City. She was awarded the medal of the Order of Australia in 2001 ‘for service to the community of Hawthorn and district, particularly through the research, documentation and publication of its history.’ This map from her collection was donated to the Kew Historical SocietyPlan of Heidelberg, annotated with details about the occupancy pre and post European settlement. The plan also contains geological references. The plan is included and analysed in volume 2 of the Heidelberg Conservation Study (1985). The original plan was published created in 1982. Printed annotationscity of heidelberg, yarra valley, historic plans -- heidelberg

1914 Handbook prepared for the members of the "British Association for the advancement of science" on the occasion of their visit to Victoria, under the direction of the Victorian Executive Committee. Hard covered green handbook, gold leaf lettering. Printed text with Illustrations, Maps, Plans and Diagrams.Stamped: "WITH THE COMPLEMENTS OF THE GOVERNMENT STATIST." victoria, 1914, education, population, immigration, mining, geology, land, law, government, forestry, maps, public works.

Colour Copy of Plan of the General Survey from the Town of Malmsbury to the Porcupine Inn, from the sources of Forest Creek to Golden Point, shewing (sic) the Alexandrian Range also Sawpit Gully Bendigo and Bullock Creeks. Handwritten note under the title a follows '' Forwarded to the Colonial Secretary with my letter No A 53/105 dated 30th March 1853 for transmission to the Geological Surveyor. R Hoddle Surveyor General. ' Stamped by Department of Mines Victoria with record#123 in Top right Hand corner. Also contains a catalogue number 2053/M/2. Part of the Contents of a DVD entitled 'Mapping Great Change' - Archival Maps, produced to support an exhibition in the Post Office Gallery Bendigo. A description of the Map, its history and implications for both historical and future discussions is contained in an Essay 'Mapping Great Changes' : The landscape of central Victoria by Gerry Gill.R. Hoddlemap, bendigo, country lands

This specimen was recovered from Mica Schist, Canada. Chalcopyrite is a copper iron sulfide mineral with a chemical composition of CuFeS2. Its name derives from the Greek words for copper (chalco-) and brass (pyrite). It can be found in shades of yellow, green and grey, and, when exposed to acid, it can change to purple, blue, violet and yellow tones. Weathering can cause loss of its metallic luster and its brass-yellow colour. Chalcopyrite forms under various conditions, with the most significant deposits being hydrothermal in their origin. It is known globally as the most important ore of copper for thousands of years, and is thus considered a very important mineral formation. Given its golden appearance, it is often confused for the mineral gold, earning it the popular reputation as 'fool's gold' or 'yellow copper'. However, it can be straightforwardly distinguished from gold; the latter is soft, with higher specific gravity and a yellow streak, whereas chalcopyrite is brittle, easily scratched by a nail, and has a greenish grey streak. Copper was the first metal that was used by people. It was discovered by the Neolithic man about 9,000 years ago and it gradually replaced stone as it was easier to be shaped. In Australia, search for copper began after the European settlement, leading to the discovery of substantial deposits, like the one at the Olympic Dam in South Australia, which is regarded as one of the largest copper deposits in the world. Chalcopyrite has been used for copper since smelting processes began approximately five thousand years ago. Although by no means rare, this the specimen of this mineral can be used to reflect a wider history of industrial uses of copper for a significant portion of human history. 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 copper iron sulfide mineral of brass yellow, often with an iridescent tarnish, with greenish-black streak and submetallic luster. Chalcopyrite can be formed in several ways, including crystalizing from accessory minerals in igneous rocks, or from magma or within volcano sulfide deposits. Most commonly, chalcopyrite are found in hydrothermal conditions, where it forms in hydrothermal veins. As a member of the tetragonal crystal system, it often takes the shape of tetra-headed crystals, often with striations along the sides of the crystals. #18 Copper pyrites/(chalcopyrite) in/Laurentian Slate/(page 315 of inventory)/page missing from/descriptive catalogue/ Other label: 81 /fool's gold, chalcopyrite, mineral, rock, geology, geological, hydrothermal, neolithic, european settlement, olympic dam, south australia, stone, deposits, specific gravity, greenish grey streak, brittle, mineral gold, metallic luster, cufes2, greek words

BHS CollectionPart of a map of the Bendigo Gold Field - Golden Square. Geological Survey of Victoria. Shown are reefs, faults and anticlines. Many of the mines are shown on the map. Gullies, hills and streets are also shown.bendigo, history, long gully history group, the long gully history group - bendigo gold field - golden square geological survey of victoria, north bendigo state school reserve, hospital reserve, benevolent asylum reserve, empire hill, richmond hill, raes hill, south end hill, victoria hill, new chum hill, iron bark hill, redan hill, view hill, hustlers hill, camp hill

The Osborne Peninsula on the Yarra River at Warrandyte accommodates a limited number of properties and residents (70 households). The area is rich in geology and ecology, and an unusually rich endowment of human, built and creative history. Contents: Welcome: The landform: The River: Aboriginal occupation: The Miners: North Warrandyte :The Subdivision: The Lowes: The Osbornes: The Last Osborne: The Elders: The Relics: Dray Track: Water Wheel"Kauri Plaque: River track: Pines: Windmill Creek Bridge: The Koornong School: The Houses" Man Cave: MidCentury Classic: Enduring Original" Masterwork: The Muddies: The State Park: The Saving of Koornong Reserve: The Landcare Story: Flora and Fauna: The Vulnerable, Endangered and threatened: Birds: Mammals: "Waring" the wombat: Reptiles: Fish: Invertebrates: Flora: Fire. Published by the North Warrandyte (Osborne Peninsula) Landcare Group. Includes photos from EDHS collection.64 p. : ill., map ; 29.7 x 21 cm. (2 copies)yarra river, birrarung, dray track, fauna, geology, houses, indigenous history, koornong reserve, koornong school, lowe family, mining, mudbrick houses, north warrandyte, osborne family, warrandyte state park, water wheel, north warrandyte (osborne peninsula) landcare group, osborne peninsula

Printed foolscap size book. Softcover. 112 pages. Colour and black and white photos. Maps, figures, tables. Index. Publication details. Graham Simpson (Publisher, Bacchus Marsh, Victoria, 2021. Lead authors Graham Simpson, Jeanette McGonegal and Alan Morton.This book contains a collection of articles written by landholders, local residents and members of corporate and volunteer organisations describing their roles in the restoration of Rowsley Valley. The historical scope of this book encompasses the geological and environmental history of the area prior to human habitation, occupation by the Wadawurrung people prior to European colonisation, and the colonial and post colonial eras. This introductory contextual background is complemented by the rest of the book which describes the various aspects of the environmental restoration of the Rowsley Valley from the latter part of the 20th century continuing to the present day.environmental restoration projects, rowsley valley victoria environmental history, conservation of natural resources, aboriginal australians bacchus marsh region history, wadawurrung people history

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

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

Dendrites are deposits of black minerals, typically manganese oxides that precipitated from water seeping through fractures in fine-grain rocks like a sandstone or limestone. Dendrites are much less regular than plant fossils and lacks vein structures. The manganese cryztallizes through the process called 'supercooling'. Some samples of dendrites occur in volcanic rocks in the Lilydale district, east of Melbourne. Sandstones are made of tiny sand grains that may have been deposited in the sea and later formed together. Most sandstones are made of quartz which are chemically-resistant minerals. This particular specimen was donated by Alfred Selwyn in 1868 as part of the Geological Survey of Victoria. It is connected to the original 1875 catalogue on Geological Specimen with number 189 'Quartz Crystals_Quartz Crystals (two are polished)'Dendrites on sandstones This specimen is an important contribution to the geological history of Victoria, as well as its links to the 1868 Geological Survey of Victoria. This specimen is part of larger collection of significant geological specimens in the Burke Museum that was collected from around the world between 1868-1880. A large percentage of these specimens were collection as part of the Geological Survey of Victoria 1852-1974. The Geological Survey of Victoria was an organisation founded in response to the Victorian gold rush to explore the geological and mineral resources and to record a detailed map of the state. It 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 hand-sized slice of light brown sandstone with dendrites formed from crystallized manganese oxide.Existing label: Not sure what / 'Slica dondrites' / means. / Sample is sandstone and original label / identifies it as from / the Grampians near Stawell. / C. Willman / 15/4/21 Other label: [illegible] / stone [ illegible] / from Grampians Stawell / 1894 /geological specimen, geology, geology collection, burke museum, beechworth, dendrites, sandstones, quartz, lilydale district, geological survey of victoria, grampians, victoria rocks, minerals, rocks, manganese oxides, alfred selwyn

Native Sulphur in its solid form is a yellow crystalline mineral that forms near volcanic vents and fumaroles where it is the solid form of hot gases. It is also frequently found in the subsurface as a by-product of sulphide ore mineralization. In all its forms, sulphur is one of the most commonly occurring minerals on the planet, especially in natural gases, and is key to the make-up of a range of other minerals. It is essential to continuing life on earth, and was used in ancient societies as part of medical care, religious rites, and entertainment, and was key to the invention of gunpowder by the Chinese. Native Sulphur in its solid form is a yellow crystalline mineral that forms near volcanic vents and fumaroles where it is the solid form of hot gases. It is also frequently found in the subsurface as a by-product of sulphide ore mineralization. In all its forms, sulphur is one of the most commonly occurring minerals on the planet, especially in natural gases, and is key to the make-up of a range of other minerals. It is essential to continuing life on earth and was used in ancient societies as part of medical care, religious rites, and entertainment, and was key to the invention of gunpowder by the Chinese. The exact site of extraction for this specimen is unknown, but it was probably collected in New Zealand in the 1850s. Sulphur is significant both for its historical and current uses, and for its nature as one of the most abundant minerals on the planet. Sulphur's importance comes both from its abundance and its role in ensuring survival, creating other minerals, and daily human life. This specimen is significant as representative of sulphur's solid properties. 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, small, crystalline mineral specimen that is largely bright yellow, with some darker spotting. geological specimen, geology, geology collection, burke museum, beechworth, sulphur, native sulphur, new zealand, native sulphur specimen, sulphur specimen

Thunderegg Agates are formed within rhyolite volcanic ash layers. They are rough spherical shapes, varying in size from less than an inch to over a metre long. Thundereggs usually contain centres of chalcedony which may have been fractured followed by deposition of agate, jasper or opal, either uniquely or in combination. A unique characteristic that these specimens have is the fact that they often look like ordinary rocks on the outside, but slicing them in half and polishing them may reveal intricate patterns and colours. These particular specimens are examples of thunderegg agates. Agate is a variety of chalcedony, a cryptocrystalline form of quartz. The agate component contributes to the intriguing internal patterns of the specimens. The specific locality of these specimens is unknown but they can be found in flows of rhyolite lava. They are formed in gas pockets in the lava, which act as moulds. These specimens can be found globally, with specific locations in Germany being particularly abundant. 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 small solid specimens with pale, sandy-coloured exteriors and fractured internal patterns. burke museum, beechworth, geological, geological specimen, thundereggs, thundereggs agate, agate, rhyolite, rhyolite lava, volcanic ash, chalcedony, cryptocrystalline

A fossil refers to any remains or traces of past life that are preserved in the rock. It could be remains of plants or animals. Fossil leaves are commonly found on different types of rocks. These fossils can go as far back as the Triassic Age just like the series of fossil plants collected at Denmark Hill, Ipswich in Queensland. Fossils leaves are formed when dead plants get buried by sediments like mud, sand, or volcanic ash. Often, it gets detached cleanly from stems along a special layer of weak cells, then twigs, and, less commonly, cones of conifers and fruits and seeds of flowering plants. Over time, the leaves or pieces of leaves get buried by more sediments and eventually gets 'lithified' or hardened into a rock. Erosions and mining can cause the rocks to break and reveal the fossils buried in it. Fossilisation frequently takes place at sites in the lowlands where deposits of clay, silt, sand are found. This is usually due to weathering and erosion of rocks. Fossil leaves can provide information about ancient Australia's way of living. It contributes to Victorian biodiversity records and its botanical collections. It also contributes information on the geographical profile of Victoria as fossilisation usually occur at estuaries and deltas of rivers, river flood plains, ponds and lakes. 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.Piece of light brown rock with fossilised leaves in shades of golden yellow and brown.Existing label: Fossil Leaves / Locality unknown / might be worth checking if this is Glossopteris, a Permian age plant. / C. William 16/4/21 geological specimen, geology, geology collection, burke museum, beechworth, fossil leaves, fossilization, 1868 geological survey of victoria, lithified, rocks, fossilised leaf, rock, fossils, leaves

Galena is the natural compound of lead and classed as a sulphide, it crystallises in a cubic pattern and its chemical formula is PbS. Galena is a primary source of both lead and silver. This specimen of Galena comes from Broken Hill. Broken Hill has one of the world’s largest and most significant deposit of ore for the production of lead. Mining of Galena at Broken Hill began with the staking of land by Charles Rasp in 1883. By the following year, in 1884, Rasp and six others had formed Broken Hill Mining Company. Broken Hill Mining Company eventually evolved into BHP group limited and is currently the largest mining company in the world and the largest company in Australia. There is archaeological evidence from artefacts discovered in Turkey that humans have been extracting lead from galena by the process of smelting since at least 6500 BCE. This specimen also has quartz on the top surface which is frequently discovered alongside Galena. This mineral specimen is of historic significance as a sample of Galena extracted from Broken Hill during the 19th century. Mining for Galena in Broken Hill begin in 1883 by Charles Rasp and evolved into the world’s largest mining company – BHP Group Limited. Broken Hill is one of the world’s most significant deposits of ore for the production of lead. 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 flat, hand-sized, grey sulphide specimen that is the natural compound of lead with a quartz formation on the top surface. Existing Label: GALENA / (with quartz) / Locality: Broken Hill / N.S.W 120 x 70 x 29geological specimen, geology, geology collection, burke museum, beechworth, galena, galena quartz, quartz, charles rasp, broken hill mining company, bhp group limited, bhp, lead, ore, lead sulphide, sulphide, silver, broken hill

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

Mining & Geological Journal, March 1941, Vol.2, No.4. Published by Department of Mines Victoria, 136 pages of Mine Reports, articles on mines, photographs, illustrations, maps & advertisements. Name on cover A.Richardson 29 Harrison St Bendigo.Dept of Mines Victoriagold mines, mining, mining - mines - mining equipment, axedale - fletchers mine.

A party of surveyors camped by Yuille's Swamp (later Lake Wendouree) and surveyed the countryside for a map to be produced by the Geological Survey of Victoria. In November 2004 the Central Highlands Regional Library presented a special edition of 200 copies of the 1861 map reproduced from a copy in their collection. Original 1861 map of Ballarat showing streets and leads. Blue dots indicate gold leads, and red lines indicate auriferous quartz reef and outcrops of quartz veins."Compiled & Drawn from the Survey of Mining Surveyors Davidson, Fitzpatrick and Cowan & the Plans in the Surveyor General's Office by J. Brahe, 21st October 1861. R. Brough Smyth, Secretary for Mines. The Honourable J.B. Humffray, M.L.A. Commr of Mines.”ballarat, map, ballarat east, lake wendouree, survey, mines, robert davidson, ballarat gold field 1861, yuille's swamp, wendouree swamp, little bendigo diggings, gold leads, old post office hill, specimen hill, bakery hill, black hill, dead horse creek, brown hill, pennyweight hill, clayton hill, soldiers hill, golden point, gum tree flat, white flat, poverty hill, chinese village, robert brough smyth, ballarat map 1861, ballaarat vineyard, dead horse gully, deadhorse creek, invermay, black hill flat, gaelic church, police reserve, magpie range, dalton's flat, caadian lead, rifle butts, powder magazine, bathing house, government camp, gold office, chinese, llanberrris, victoria theatre, charlie napier hotel, united states hotel, grape's hoel, clayton's hill, cattleyard hill, free trade hotel, esmond lead, bakery hill, black hill lead, juvenile reformatory, ballarat orphanage, lady barkly lead, triffet's slaughter yard, little bendigo, melbourne road, t. cowan, thomas cowan