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Rock Flat, New South Wales
Rock Flat is a rural locality in the Snowy Monaro Regional Council local government area of New South Wales, Australia. It is located south of Cooma, on either side of the Monaro Highway. The area now known as Rock Flat lies on the traditional lands of the Ngarigo people. Near the Monaro Highway crossing of Rock Flat Creek, there is a mineral spring that comes to the surface, on the bank of the creek. The spring water issues from near the base of a small rocky mount composed of highly inclined beds of quartzite and the surface of the flat in the vicinity of the spring is tufaceous limestone that has been deposited there by the spring water. The flow rate of the spring is about 245-litres per hour. The spring water has a pleasant taste and is carbonated. The water contains carbonates of calcium, sodium, and magnesium. It is likely that this spring is the one referred to as Richard Bourke's Spring by the explorer Dr J. Lhotsky in 1834. Lhotsky had thought highly enough of the s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Snowy Monaro Regional Council
The Snowy Monaro Regional Council is a local government area located in the Snowy Mountains and Monaro regions of New South Wales, Australia. The council was formed on 12 May 2016 through a merger of the Bombala, Cooma-Monaro and Snowy River shires. The council comprises an area of and occupies the higher slopes of the eastern side of the Great Dividing Range between the Australian Capital Territory to the north and the state boundary with Victoria to the south. At the time of its establishment the council had an estimated population of . Its population at the was 20,218. The Mayor of the Snowy Monaro Regional Council is Narelle Davis. Towns and localities The following towns are located within Snowy Monaro Regional Council: The following localities are located within Snowy Monaro Regional Council: Heritage listings The Snowy Monaro Region has a number of heritage-listed sites, including: * Bombala, Goulburn-Bombala railway: Bombala railway station * Bombala, 91 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Spring (hydrology)
A spring is a point of exit at which groundwater from an aquifer flows out on top of Earth's crust (pedosphere) and becomes surface water. It is a component of the hydrosphere. Springs have long been important for humans as a source of fresh water, especially in arid regions which have relatively little annual rainfall. Springs are driven out onto the surface by various natural forces, such as gravity and hydrostatic pressure. Their yield varies widely from a volumetric flow rate of nearly zero to more than for the biggest springs. Formation Springs are formed when groundwater flows onto the surface. This typically happens when the groundwater table reaches above the surface level. Springs may also be formed as a result of karst topography, aquifers, or volcanic activity. Springs also have been observed on the ocean floor, spewing hot water directly into the ocean. Springs formed as a result of karst topography create karst springs, in which ground water travels thr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bombala Railway Line
The Bombala railway line is a branch railway line in the south of New South Wales, Australia. The northern part of it forms part of the main line from Sydney to Canberra, but the southern part is closed. It branches off the Main South line at Joppa Junction, south of Goulburn. The line is used by NSW TrainLink Xplorer services running between Sydney Central and Canberra station. History The line was opened in stages to Tarago (January 1884), Bungendore (March 1885), Queanbeyan (September 1887), Michelago (December 1887), Cooma (May 1889), Nimmitabel (April 1912) and Bombala (November 1921). Queanbeyan The section of the line, between Bungendore and Queanbeyan, was the most challenging to construct, with three tunnels, a major sideling embankment along the Molonglo River gorge (also known as 'Pine Valley'), and two major bridges, across the Molonglo and Queanbeyan Rivers. The construction contract for the line from Bungendore to Michelago was awarded to Johnstone an ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
George Child Villiers, 8th Earl Of Jersey
George Henry Robert Child Villiers, 8th Earl of Jersey DL (2 June 1873 – 31 December 1923), was a British peer and Conservative politician from the Villiers family. Villiers was the son of Victor Child Villiers, 7th Earl of Jersey, and the Honourable Margaret Elizabeth, daughter of William Henry Leigh, 2nd Baron Leigh. Public life Villiers was educated at Eton College and at New College, Oxford for university. He succeeded his father in the earldom in 1915 and served briefly as a Lord-in-waiting under David Lloyd George between January and August 1919. He was a Justice of the peace and deputy lieutenant in Oxfordshire and an alderman and vice chairman for Oxfordshire County Council and a high steward for the city of Oxford. Also a J.P. and an Alderman for Middlesex. Lord Jersey sold the Child & Co bank, part of the family's inheritance since the 5th Earl married into the Child family, to Glyn, Mills & Co. Bank in 1923. He was a member of the Ancient Order of Druids since ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Osterley House
Osterley Park and House is a Georgian country estate in west London, that straddles the London boroughs of Ealing and Hounslow. Originally dating from the 1570s, the estate contains a number of Grade I and II listed buildings, with the park listed as Grade II*. The main house was remodelled by Robert Adam between 1761 and 1765. The National Trust took charge of Osterley in 1991 and the house and park are open to visitors. History Elizabethan The original building on this site was a manor house built in the 1570s for banker Sir Thomas Gresham, who purchased the manor of Osterley in 1562. The "faire and stately brick house" was completed in 1576. It is known that Queen Elizabeth visited. The stable block from that period remains at Osterley Park. Gresham was so wealthy that he also bought the neighbouring Manor of Boston in 1572. Child and Adam Two hundred years later the manor house was falling into disrepair, when, as the result of a mortgage default, it came into t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Damper (food)
Damper is a thick homemade soda bread traditionally prepared by early European settlers in Australia. The bread is different from bush bread, which has been made by Indigenous Australians for thousands of years and was traditionally made by crushing a variety of native seeds, nuts and roots, mixing them into a dough, and then baking the dough in the coals of a fire. There is ongoing investigation into whether this technique of various Aboriginal peoples influenced the development of colonial-era damper, similarly cooked in the ashes of a camp fire. Damper is a bread made from wheat-based dough. Flour, salt and water, with some butter if available, is lightly kneaded and baked in the coals of a campfire, either directly or within a camp oven. When cooked as smaller, individually-sized portions, these damper "bush scones" are often called "johnny cakes Johnnycake, also known as journey cake, johnny bread, hoecake, shawnee cake or spider cornbread, is a cornmeal flatbread, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
John Lhotsky
John Lhotsky (1795–1866) was a Galicia-born Austrian naturalist, lecturer, artist and author. He wrote and published on the topics of zoology, botany, geology, geography and politics. Lhotsky was active in the early colonies of New South Wales and Tasmania from 1832 until 1838. During his sojourn in Australia, Lhotsky described himself, and was known as, Polish. Early life Lhotsky, whose first name is also given as Joannes Lhotsky, Johann Lhotsky and Jan Lhotsky, was born in Lemberg, Galicia, Austrian Empire (now Lviv, Ukraine), the son of Joseph Lhotsky. He moved to Vienna in 1812 and was awarded his doctorate from the University of Jena. He became a member of the Bavarian Botanical Society during this period. In 1819 he published a botanical work ''Flora Conchica'', and other papers for scientific journals, however, his political writing led to a prison sentence of six years. He was released in 1828. Travel to Australia Lhotsky was commissioned, by Ludwig I of Bav ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Richard Bourke
General Sir Richard Bourke, KCB (4 May 1777 – 12 August 1855), was an Irish-born British Army officer who served as Governor of New South Wales from 1831 to 1837. As a lifelong Whig (Liberal), he encouraged the emancipation of convicts and helped bring forward the ending of penal transportation to Australia. In this, he faced strong opposition from the landlord establishment and its press. He approved a new settlement on the Yarra River, and named it Melbourne, in honour of the incumbent British prime minister, Lord Melbourne. Early life and career Born in Dublin, Ireland, Bourke was educated at Westminster and read law at Christ Church, Oxford. He was a cousin of Edmund Burke and spent school and university holidays at Burke's home, and thus acquired some influential friends. He joined the British Army as an ensign in the Grenadier Guards on 22 November 1798, serving in the Netherlands with the Duke of York before a posting in South America in 1807, where he participated ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Magnesium Carbonate
Magnesium carbonate, (archaic name magnesia alba), is an inorganic salt that is a colourless or white solid. Several hydrated and basic forms of magnesium carbonate also exist as minerals. Forms The most common magnesium carbonate forms are the anhydrous salt called magnesite (), and the di, tri, and pentahydrates known as barringtonite (), nesquehonite (), and lansfordite (), respectively. Some basic forms such as artinite (), hydromagnesite (), and dypingite () also occur as minerals. All of those minerals are colouress or white. Magnesite consists of colourless or white trigonal crystals. The anhydrous salt is practically insoluble in water, acetone, and ammonia. All forms of magnesium carbonate react with acids. Magnesite crystallizes in the calcite structure wherein is surrounded by six oxygen atoms. The dihydrate has a triclinic structure, while the trihydrate has a monoclinic structure. References to "light" and "heavy" magnesium carbonates actually refer t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sodium Carbonate
Sodium carbonate, , (also known as washing soda, soda ash and soda crystals) is the inorganic compound with the formula Na2CO3 and its various hydrates. All forms are white, odourless, water-soluble salts that yield moderately alkaline solutions in water. Historically, it was extracted from the ashes of plants growing in sodium-rich soils. Because the ashes of these sodium-rich plants were noticeably different from ashes of wood (once used to produce potash), sodium carbonate became known as "soda ash". It is produced in large quantities from sodium chloride and limestone by the Solvay process. Hydrates Sodium carbonate is obtained as three hydrates and as the anhydrous salt: * sodium carbonate decahydrate (natron), Na2CO3·10H2O, which readily effloresces to form the monohydrate. * sodium carbonate heptahydrate (not known in mineral form), Na2CO3·7H2O. * sodium carbonate monohydrate (thermonatrite), Na2CO3·H2O. Also known as crystal carbonate. * anhydrous sodium carbonate ( n ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
