historic, coal miningB/w photograph, Victoria Company Lignite Mine, Lal Lal, c 1900lal lal, coal mine, lignite, victoria company

Latrobe valley.8370.1 - Small, irregularly shaped 'lump' of lignite/brown coal.

Black brooch in shape of two crossed racquets. Materials: Jet (Lignite), Metaltennis

This particular specimen was recovered from the Lal Lal Coal and Iron Mine in Victoria, 19km from Ballarat. Brown Coal was discovered here in 1857, just alongside the Geelong to Ballarat Railway line. This discovery of lignite (brown coal) was the first in Victoria, which would bring important benefits to the region and state, both of which had previously been reliant on coal imports. In the 1860s, iron ore was found just 5km from Lal Lal, and the area was converted into an Iron Ore Mine. The Lal Lal Iron Mining Company took over operations in 1874, who then peaked iron production in 1884. This mine continued operations until June 1884, when the blast furnace was extinguished and never recommenced. The blast furnace at Lal Lal is considered one of the most important and highly significant sites ion early industrial history in Australia, as it is the only remaining best furnace from the nineteenth century in the Southern Hemisphere. The furnace ruins are 17 metres high, and are clearly visible today on Iron Mine Road, Lal Lal, near the Bungal Dam. This specimen of Lignite (brown coal) is significant, as it was mined from the area where brown coal was first discovered in Victoria, leading to an important and controversial future of the mining and use of brown coal in this State. The Victorian Heritage Database has listed the Lal Lal Coal Mine with local significance, with their Statement of Significance stating: "The Lal Lal coal mine is historically significant as the site of the first discovery of lignite (brown coal) in Victoria, and one that promised important benefits to regional and state industries that were reliant on coal imports at the time. The significance of the stie is reduced by the poor state of preservation of the coal mining and processing fabric". 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 light-weight, soft and combustable sedimentary rock specimen, that is dark brown in colour. The specimen has jagged edges, as though parts of the rock have crumbled away. Brown coal, or Lignite, is formed naturally from compressed peat, and is typically found in natural basins. The stages to the formation of coal ('coalification') begin with plant material and wood, which will decay if it is not subjected to deep burial or heating, and turn into Peat. Peat, when sufficiently compressed naturally, will turn into Brown Coal (Lignite), and finally into Black Coal (sub-bituminous, bituminous and anthracite). Each successive stage has a higher energy content and lower water content. It is brownish-black in colour. Brown Coal has a high moisture content, between 50 and 75 percent, and a low carbon content. Some Brown Coals may be stratified, with layers of plant matter, which means little coalification has occurred beyond the peat natural processing stage. When Brown Coal is submerged in dilute nitric acid or boiling potassium hydroxide solution, it reacts to produce a reddish solution, of which higher-ranked coals do not. When brown coal is pulverised and burned in boilers, the steam is used to drive turbines, which generates electricity. It is the lowest rank of coal, as when burned, it creates a relatively low heat content, which in turn does not create a great output of steam. burke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, mineralogy, brown coal, brown coal specimen, lignite, lal lal, lal lal coal mine, lal lal iron mine, ballarat, blast furnace

Jet brooch in shape of a racquet and ball held by a hand. Materials: Metal, Jet (Lignite)tennis

Black brooch in shape of two crossed racquets and pair of shoes. Materials: Jet (Lignite), Metaltennis

Three pieces of Black Jet Mourning Jewellery - one small and one larger bracelet and one brooch. 1. Small bracelet narrower and overlapping at back, with ornately carved thistle centrefront in same black jet material. 2. Larger bracelet with gap at centre back, same ornate thistle on front as on smaller piece. 3. Carved black jet brooch, oval in shape depicting spray of flowers with metal clasp on back.bangle, brooch, black jet, lignite, mourning jewellery

The Ballarat School of Mines is a predecessor institution of Federation University Australia.Ballarat School of Mines Annual Report. The report includes: Ballarat Gaol Reserve and Endowment, Black Hill (F.M. Krause), Lal Lal Geology (F.M. Krause), Lal Lal Iron Ore Deposits (F.M. Krause) , Sedimentary Rocks of the Ballarat District (F.M. Krause), Skipton Lignite Deposit (F. M. Krause) The report includes the following Images: Ballarat School of Mines and Botanical Garden ballarat school of mines, ballarat court house, ballarat circuit court, skipton, coal, skipton coal, ballarat school of mines botanical gardens, ballarat gaol, w.h. shaw, ferdinand krause, black hill, lal lal, lal lal ore deposits, lal lal geology, sedimentary rocks of ballarat district, skipton lignite deposit, john ditchburn, john o'malley, john thompson mckenna, george samual gawler, henry henry keast, george james, donald mcgregor, george kidd, hachin gordon illingworth, john king, josiah curnow, john james patterson, john bailey bullen, john trevan, thomas james, patrick mcloughlin, patrick murray, john hore, henry ferdinand conrad

The School of Mines Ballaarat Annual Report 24 January 1882, Additional Examination Statute, Certificates Granted by Council, Copy of letter received from the Honble. Francis Ormond MLC, Extracts from Visitors' Book, Fees, Form of Bequest, Life Governors, Museum open to Visitors, Office Bearers, Paper of Particulars, Report of the Curator of the Museum and Library (with plans), Report of the Superintendent of Laboratories, Report of the Lecturer in Telegraphy, Report of the Lecturer in Mechanical Engineering, Statement of Receipts and Expenditure for the year 1881, Subjects and Lecturers, Subjects and Examiners, Subscriptions and Donations from 1 January to 31 December 1881, The Lignite Deposit at Skipton (with Section and Plan)Ballarat School of Mines Annual Report. Pale brown booklet of 64 pages. A plan of the Ballarat School of Mines shows the position of the Botanical Gardens, and the Ballarat School of Mines Museum. Geological Sketch Map of Country in the Neighbourhood of Skipton and Plan showing site of Coal Discovery. Skipton Coal Discovery - Section of Windlass Shaft. .2) is a leatherbound copyballarat school of mines, coal, plan, ballarat school of mines botanical gardens, ballarat school of mines museum, museum, annual report, james oddie, w. p. bechervaise, s. e. friggis, f. j. martell, w. h. nicholls,, e. i. rosenblum, h. r. caselli, thomas mann, theos. williams, f. m. krause, alf. mica smith, walter d. campbell, w. h. shaw, charles kent, andw. berry, robert adam, wm. lant carpenter, henry parkinson, h. b. de la poer wall, w. h. brockenshire, arthur parker, c. davies, simon richards, c. r. blackett, david jones, wilberforce dyke, kr. r. krauel, duncan love, william ralph heaton, edward dowling, octavius vaughan morgan, william denton, e. h. grimwade, james hunter, the honble. francis ormond, ferdinand krause, a.a. buley, j. cosmo newberry, w.c. kernot, john lewis, j.m. bickett, james bickett, fees, annie barnett, annette budden, isabel clinton, john dimsey, agnes pobjoy, charlotte shaw, bernard o'dowd, bernard patrick o'dowd, josiah wasley, ferdinand von mueller, william kernot, john lynch, william henderson, henry richards caselli, w.p. berchervaise, e.i. rosenblum, w.h. nicholls, lignate, samuel figgis, mary drury, w. longley, botanical reserve, botanical gardens, francis ormond, george russell, william foster stawell, w.j. clarke, rivett henry bland, john warrington rogers, j. lonie, s.e. figgis, r.f. hudson, w. robertson, e.l. rosenblum, theophilus williams, andrew berry, henry sutton, h. rosales, state school classes, calcutta international exhibition, examinations, h.b.m ship bounty, certicates, walter charles kernot, william tunbridge, mary skelton, cartherine moran, mary rose usher, margaret ellen brophy, william burbridge, andrea tuxen, elizabeth curnow, francis campigi, james s. morrison, arthur hogue

Coorongite is a dark, rubber-like, highly resilient structureless algal deposit. In the Coorong district of South Australia it occurs in moderate quantities associated with the coastal swamps and sand dunes which extend for a considerable distance east of the mouth of the Murray. This particular specimen was recovered from the south of the Coorong River, South Australia. A type of sediment rich in organic matter, Coorongite is the unlithified end-member of the sapropelic coal series. The members of the sapropelic coal series can be ranked in order as sapropel (the unlithified form), sapropelic-lignite, and sapropelic-coal (the lithified forms) based on increasing carbon content and decreasing volatile content. Sapropel (Coorongite) is an unlithified dark, pulpy, fine organic mud containing concentrations of algae and miospores that are more or less identifiable. Coorongite is typically found as an algae like substance, that can be found in irregular size pieces. Coorongite was believed to be dried up oil due to its rubber-like texture. The Coorongite is also soft to the point where it can be cut into with a knife or it can be broken and torn by hand. Otherwise known as 'Kurangk', the Coorong River is home to the Ngarrindjeri people, which acts as both a place for gathering food and a spiritual place. In 1852 the first sight of Coorongite was found along the Coorong River. The finders mistook the Coorongite for dried up oil, which lead to the belief that there were oil reserves under the Coorong River. Between the 1860s and the 1930s the Coorong River became a place where mining oil and Coorongite became precedent. Nowadays, the local council and the South Australian Government are working together with the Ngarrindjeri people to sustain and preserve the Coorong River and the culture that is with it. Soon after gold was discovered in 1851, Victoria’s Governor La Trobe wrote to the Colonial Office in London, urging ‘the propriety of selecting and appointing as Mineral Surveyor for this Colony a gentleman possessed of the requisite qualifications and acquaintance with geological science and phenomena’. Alfred Selwyn was appointed geological surveyor in Australia in 1852 which began the Geological Survey of Victoria. Selwyn went on to collect geological samples and catalogue thousands of specimens around Australia. In 1853-69 the Geological Survey issued under Selwyn's direction sixty-one geological maps and numerous reports; they were of such high standard that a writer in the Quarterly Journal of the Geological Society of London bracketed the survey with that of the United States of America as the best in the world. During his years spent in Australia, Selwyn collected numerous significant geological specimens, examples of which are held in collections such as the Burke Museum.Coorongite is considered to be a mineral with a unique texture, where it can be both hard and soft. Coorongite can also be considered to be a rare mineral, as it is only located along the Coorong River and due to the mining of it, has left very few sources. It was believed at one point that Coorongite could be used to replace oil. 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.Three solid varyingly hand-sized pieces of wooden appearing organic matter derived from the river in the Coorong District in South Australia. A rubber-like, highly resilient structureless algal deposit.Specimen 245 page 69 / in Descriptive Register / "Elcestic Bitumen, / Coorangite" South of / Coorung River, South Australia . / C. WIllman / 15/4/21burke museum, beechwoth, indigo shire, beechworth museum, geological, geological specimen, mineraology, coorong, coorong river, kurangk, ngarrindjeri, south australia, coorongite, coorongite specimen

8362.1 - Irregularly shaped piece of brown coal.