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Noel Benson
William Noel Benson FRS FRGS (26 December 1885 – 20 August 1957) was an English-born research geologist and academic active first in Australia and then New Zealand. After studying geology at the University of Sydney, Benson worked temporarily at the University of Adelaide before returning to Sydney as a demonstrator. After winning an 1851 Exhibition Science Scholarship in 1910 he left Sydney to study at the University of Cambridge, where he worked until 1913. He returned to Sydney in 1914 as the Macleay Fellow in Geology, leaving in 1917 to become Chair of the Geology Department at the University of Otago, where for many years he was the only lecturer. During his lifetime he published over 100 papers and won several awards, including the Clarke Medal and the Lyell Medal. He died on 20 August 1957 following his retirement from academia in 1951. Early life and education Benson was born on 26 December 1885 in Anerley, London, England, to William Benson, see pages 27 and 29 a Qu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Anerley
Anerley () is an area of south east London, England, within the London Borough of Bromley. It is located south south-east of Charing Cross, to the south of Crystal Palace and Upper Norwood, west of Penge, north of Elmers End and South Norwood. History Origin and development Anerley has never existed as an independent entity, but rather as a general area. Prior to the enclosure in 1827 and the relocation of the Crystal Palace to Penge Place at the top of Sydenham Hill, Anerley was an unoccupied part of Penge Common, and did not develop until the 19th century. The government Act of 1827 stipulated that a 50 feet (15 metres) wide, new road, was to be set out from Elmers End Road to what is now Church Road, Upper Norwood.The London Encyclopaedia, p. 23 In 1827, a Scottish silk manufacturer named William Sanderson bought land on the former Penge Common and built the first house in the area, which he named "Anerly Lodge", a Scottish and Northern English dialect word meaning "soli ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Edgeworth David
Sir Tannatt William Edgeworth David (28 January 1858 – 28 August 1934) was a Welsh Australian geologist and Antarctic explorer. A household name in his lifetime, David's most significant achievements were discovering the major Hunter Valley coalfield in New South Wales and leading the first expedition to reach the South Magnetic Pole. He also served with distinction in World War I. Early life David was born on 28 January 1858, in St. Fagans near Cardiff, Wales, the eldest son of the Rev. William David, a fellow of Jesus College, Oxford, a classical scholar and naturalist and his wife Margaret Harriette (née Thomson). His mother's cousin, William A. E. Ussher of the Geological Survey, first interested David in what was to be his life work. At the age of 12, David went to Magdalen College School, Oxford in 1870. In 1876 he gained a classical scholarship to New College, Oxford. While there he was lectured by the famous John Ruskin and William Spooner. In 1878 he suff ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cenozoic
The Cenozoic ( ; ) is Earth's current geological era, representing the last 66million years of Earth's history. It is characterised by the dominance of mammals, birds and flowering plants, a cooling and drying climate, and the current configuration of continents. It is the latest of three geological eras since complex life evolved, preceded by the Mesozoic and Paleozoic. It started with the Cretaceous–Paleogene extinction event, when many species, including the non-avian dinosaurs, became extinct in an event attributed by most experts to the impact of a large asteroid or other celestial body, the Chicxulub impactor. The Cenozoic is also known as the Age of Mammals because the terrestrial animals that dominated both hemispheres were mammalsthe eutherians (placentals) in the northern hemisphere and the metatherians (marsupials, now mainly restricted to Australia) in the southern hemisphere. The extinction of many groups allowed mammals and birds to greatly diversify so that l ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
University Of Melbourne
The University of Melbourne is a public research university located in Melbourne, Australia. Founded in 1853, it is Australia's second oldest university and the oldest in Victoria. Its main campus is located in Parkville, an inner suburb north of Melbourne's central business district, with several other campuses located across Victoria. Incorporated in the 19th century by the colony of Victoria, the University of Melbourne is one of Australia's six sandstone universities and a member of the Group of Eight, Universitas 21, Washington University's McDonnell International Scholars Academy, and the Association of Pacific Rim Universities. Since 1872, many residential colleges have become affiliated with the university, providing accommodation for students and faculty, and academic, sporting and cultural programs. There are ten colleges located on the main campus and in nearby suburbs. The university comprises ten separate academic units and is associated with numerous institut ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sedgwick Museum Of Earth Sciences
The Sedgwick Museum of Earth Sciences, is the geology museum of the University of Cambridge , mottoeng = Literal: From here, light and sacred draughts. Non literal: From this place, we gain enlightenment and precious knowledge. , established = , other_name = The Chancellor, Masters and Schola .... It is part of the Department of Earth Sciences, University of Cambridge, Department of Earth Sciences and is located on the university's Downing Site in Downing Street, Cambridge, Downing Street, central Cambridge, England. The Sedgwick Museum is the oldest of the eight museums which make up the University of Cambridge Museums consortium. History Construction and opening John Woodward (naturalist), Dr John Woodward collected and catalogued over 35 years nearly 10,000 specimens in five walnut cabinets, two of which he bequeathed to the university in his will. The university later purchased another two, and the fifth was added in the 1840s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Thomas George Bonney
Thomas George Bonney (27 July 1833 – 10 December 1923) was an English geologist, president of the Geological Society of London. Career Bonney was born in Rugeley, Staffordshire, England, the eldest son of the Reverend Thomas Bonney, headmaster of Rugeley Grammar School. His uncle was the Australian explorer Charles Bonney, and one of his brothers, Frederic Bonney, is remembered for his photography and ethnology in Australia. Thomas was educated at Uppingham School and St John's College, Cambridge, where he graduated as 12th wrangler in 1856, and was ordained in the following year. From 1856 to 1861 he was mathematical master at Westminster School, and he pursued geology only as a recreational activity, mainly in Alpine regions. In 1868 he was appointed tutor at St John's College, Cambridge and lecturer in geology. His attention was specially directed to the study of the igneous and metamorphic rocks in Alpine regions and in various parts of England (e.g.: the Lizard in Cor ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alfred Harker
Alfred Harker FRS (19 February 1859 – 28 July 1939) was an English geologist who specialised in petrology and interpretive petrography. He was Lecturer in Petrology at the University of Cambridge for many years, and carried out field mapping for the Geological Survey of Scotland and geological studies of western Scotland and the Isle of Skye. He and other British geologists pioneered the use of thin sections and the petrographic microscope in interpretive petrology. Education and career Harker's father was the Yorkshire corn merchant Portas Hewart Harker, his mother Ellen Mary Harker. He attended Hull and East Riding College, and the private Clewer House School (Windsor) before enrolling as an undergraduate at St. John's College (Cambridge) from where he graduated with an M.A. on 18 January 1882. Whilst at Cambridge he was an early member of the Sedgwick Club. In 1884 he held the post of Demonstrator in the Geology Department under Thomas McKenny Hughes (whom he regarded ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
John Edward Marr
John Edward Marr FGS FRS (14 June 1857 – 1 October 1933) was a British geologist. After studying at Lancaster Royal Grammar School, he matriculated to St John's College, Cambridge, graduating with First Class Honours in 1878. Following undergraduate work in the Lake District, he travelled to Bohemia to investigate the fossil collection of Joachim Barrande, where his work won him the Sedgwick Prize in 1882. In 1886, Marr became lecturer at the University of Cambridge Department of Geology, a position he held for 32 years until he succeeded Thomas McKenny Hughes as Woodwardian Professor of Geology in 1917. Early life and education Marr was born in Poulton-le-Sands on 14 June 1857 to John Marr, a retired silk merchant, and his wife Mary Simpson. After the family stayed in Caernarfon in 1863, Marr became interested in geology, having discovered a fossil which was named after him. From 1867 to 1875 he studied at the Lancaster Royal Grammar School, where he met R. H. Tiddeman, who ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mount Lofty Ranges
The Mount Lofty Ranges are a range of mountains in the Australian state of South Australia which for a small part of its length borders the east of Adelaide. The part of the range in the vicinity of Adelaide is called the Adelaide Hills and defines the eastern border of the Adelaide Plains. Location and description The Mount Lofty Ranges stretch from the southernmost point of the Fleurieu Peninsula at Cape Jervis northwards for over before petering out north of Peterborough. In the vicinity of Adelaide, they separate the Adelaide Plains from the extensive plains that surround the Murray River and stretch eastwards to Victoria. The Heysen Trail traverses almost the entire length of the ranges, crossing westwards to the Flinders Ranges near Hallett. The mountains have a Mediterranean climate with moderate rainfall brought by south-westerly winds, hot summers and cool winters. The southern ranges are wetter (with of rain per year) than the northern ranges (). Southern rang ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geomorphology
Geomorphology (from Ancient Greek: , ', "earth"; , ', "form"; and , ', "study") is the scientific study of the origin and evolution of topographic and bathymetric features created by physical, chemical or biological processes operating at or near Earth's surface. Geomorphologists seek to understand why landscapes look the way they do, to understand landform and terrain history and dynamics and to predict changes through a combination of field observations, physical experiments and numerical modeling. Geomorphologists work within disciplines such as physical geography, geology, geodesy, engineering geology, archaeology, climatology, and geotechnical engineering. This broad base of interests contributes to many research styles and interests within the field. Overview Earth's surface is modified by a combination of surface processes that shape landscapes, and geologic processes that cause tectonic uplift and subsidence, and shape the coastal geography. Surface processes co ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Barossa Range
The Barossa Range (Kaurna: ''Yampoori'') is a mountain range located in the Australian state of South Australia. Location The range is a part of the southern Mount Lofty Ranges and the western slopes primarily fall into the Barossa Valley. As such, the range is the main source for the North Para River and its tributary Jacob's Creek. The highest point of the range is Mount Kaiser Stuhl with an elevation of and forms part of the Kaiserstuhl Conservation Park. Mengler Hill, another notable peak within the range, lies on the road route from Tanunda to Angaston. Naming The range was named by Colonel William Light in 1837 after Barrosa Hill (Cerro de Puerco) in the modern municipality of Chiclana de la Frontera, Spain, to which it he thought it similar. The Spanish location was the site of the Battle of Barrosa and was won by Light's friend Lord Lynedoch (Lt. Gen. Sir Thomas Graham) in 1811. The word ''barrosa'' (mis-spelt in the naming of the valley, two 'r' and one 's' b ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cambrian
The Cambrian Period ( ; sometimes symbolized C with bar, Ꞓ) was the first geological period of the Paleozoic Era, and of the Phanerozoic Eon. The Cambrian lasted 53.4 million years from the end of the preceding Ediacaran Period 538.8 million years ago (mya) to the beginning of the Ordovician Period mya. Its subdivisions, and its base, are somewhat in flux. The period was established as "Cambrian series" by Adam Sedgwick, who named it after Cambria, the Latin name for 'Cymru' (Wales), where Britain's Cambrian rocks are best exposed. Sedgwick identified the layer as part of his task, along with Roderick Murchison, to subdivide the large "Transition Series", although the two geologists disagreed for a while on the appropriate categorization. The Cambrian is unique in its unusually high proportion of sedimentary deposits, sites of exceptional preservation where "soft" parts of organisms are preserved as well as their more resistant shells. As a result, our understanding of the Ca ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
