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Barbara Rawdon-Hastings, Marchioness Of Hastings
Barbara Rawdon-Hastings, Marchioness of Hastings, 20th Baroness Grey de Ruthyn (''née'' Yelverton; 20 May 1810 – 18 November 1858) was a fossil collector and geological author. Early life Born at Brandon House in Brandon, Warwickshire, Barbara Yelverton was the only child of Henry Yelverton, 19th Baron Grey de Ruthyn (1780–1810), and of his wife, Anna Maria Kellam (1792–1875). Her father was a friend of "mad, bad, and dangerous to know" Lord Byron, who referred to the new bride as "a rustic". At seven months, her father's death made her Baroness Grey de Ruthyn. Little is known of her early life or education.Dadley, Portia, ''Hastings, Barbara Rawdon ée Barbara Yelverton marchioness of Hastings and'' suo jure ''Baroness Grey de Ruthin (1810–1858), fossil collector and geological author'' in ''Oxford Dictionary of National Biography'' (Oxford University Press, 2004) In 1817, she was living in Derbyshire, in the (now lost) stately home Castlefields, owned by the Borrow ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
The Most Honourable
The honorific prefix "The Most Honourable" is a form of address that is used in several countries. In the United Kingdom, it precedes the name of a marquess or marchioness. Overview In Jamaica, Governors-General of Jamaica, as well as their spouses, are entitled to be styled "The Most Honourable" upon receipt of the Jamaican Order of the Nation."National Awards of Jamaica" Jamaica Information Service, accessed May 12, 2015. , and their spouses, are also styled this way upon receipt of the Order of the Nation, which is only given to Jamaican Governors-General and Prime Ministers. In |
Name Change
Name change is the legal act by a person of adopting a new name different from their current name. The procedures and ease of a name change vary between jurisdictions. In general, common law jurisdictions have loose procedures for a name change while civil law jurisdictions are more restrictive. A pseudonym is a name used in addition to the original or true name. This does not require legal sanction. Pseudonyms are generally adopted to conceal a person's identity, but may also be used for personal, social or ideological reasons. Reasons for changing one's name * Marriage or civil partnership (e.g. Tiffany Rodriguez marries Aanchal Chaudhari and assumes her surname, becoming Tiffany Chaudhari) * Adoption, or marriage of a custodial parent * Divorce or estrangement of parents * Immigration / adaptation of the name to a different language or script (e.g. Samantha Ogden became Shilpa Ojha on becoming an Indian national) * To evade the law or a debt or commit fraud * To avoid a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hordle
Hordle is a village and civil parish in the county of Hampshire, England. It is situated between the Solent coast and the New Forest, and is bordered by the towns of Lymington and New Milton. Like many New Forest parishes Hordle has no village centre. The civil parish includes the hamlets of Tiptoe and Everton as well as part of Downton. The parish was originally much larger; stretching from the New Forest boundary to Hurst Castle. The village Hordle has several shops including a post office, a pharmacy, and Co-operative Stores.History – HordlePC The village also has a primary school, and a : ''The Three Bells''. The present civil parish is somewhat smaller than the it used to c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Barton Beds
Barton Beds (now the Barton Group) is the name given to a series of grey and brown clays, with layers of sand, of Upper Eocene age (around 40 million years old), which are found in the Hampshire Basin of southern England. They are particularly well exposed in the cliffs at Barton-on-Sea, which is the type locality for the Barton Beds, and lends its name to the Bartonian age of the Eocene epoch. The clay is abundant in fossils, especially molluscs. The beds are found in the Hampshire Basin, and are well exposed in the cliffs of Barton, Hordle, and on the Isle of Wight.Archibald Geikie, (1903), ''Text-book of Geology, Volume 2'', page 1233. The cliffs at Barton are the world type locality for the Barton Beds.Janet M. Hooke, (1998), ''Coastal Defence and Earth Science Conservation'', pages 246-7. Geological Society. The beds consist of grey, greenish and brown clays with bands of sand and have long been well known for the abundance and excellent preservation of their fossils. More ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
William Buckland
William Buckland DD, FRS (12 March 1784 – 14 August 1856) was an English theologian who became Dean of Westminster. He was also a geologist and palaeontologist. Buckland wrote the first full account of a fossil dinosaur, which he named '' Megalosaurus''. His work proved that Kirkdale Cave in North Yorkshire had been a prehistoric hyena den, for which he was awarded the Copley Medal. It was praised as an example of how scientific analysis could reconstruct distant events. He pioneered the use of fossilised faeces in reconstructing ecosystems, coining the term coprolites. Buckland followed the Gap Theory in interpreting the biblical account of ''Genesis'' as two widely separated episodes of creation. It had emerged as a way to reconcile the scriptural account with discoveries in geology suggesting the earth was very old. Early in his career Buckland believed he had found evidence of the biblical flood, but later saw that the glaciation theory of Louis Agassiz gave a bet ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hugh Falconer
Hugh Falconer MD FRS (29 February 1808 – 31 January 1865) was a Scottish geologist, botanist, palaeontologist, and paleoanthropologist. He studied the flora, fauna, and geology of India, Assam,Burma,and most of the Mediterranean islands and was the first to suggest the modern evolutionary theory of punctuated equilibrium. He studied the Siwalik fossil beds, and may also have been the first person to discover a fossil ape. Early life Falconer was the youngest son of David Falconer of Forres, Elginshire. In 1826 Hugh Falconer graduated at the University of Aberdeen, where he studied natural history. Afterward, he studied medicine in the University of Edinburgh, taking the degree of MD in 1829.Arnold, David (2006) ''The Tropics and the Traveling Gaze: India, Landscape, and Science, 1800–1856'' University of Washington Press, Seattlepp. 156–157 During this period he zealously attended the botanical classes of Prof. R. Graham (1786–1845), and those on geology by Prof ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Charles Lyell
Sir Charles Lyell, 1st Baronet, (14 November 1797 – 22 February 1875) was a Scottish geologist who demonstrated the power of known natural causes in explaining the earth's history. He is best known as the author of ''Principles of Geology'' (1830–33), which presented to a wide public audience the idea that the earth was shaped by the same natural processes still in operation today, operating at similar intensities. The philosopher William Whewell termed this gradualistic view "uniformitarianism" and contrasted it with catastrophism, which had been championed by Georges Cuvier and was better accepted in Europe. The combination of evidence and eloquence in ''Principles'' convinced a wide range of readers of the significance of "deep time" for understanding the earth and environment. Lyell's scientific contributions included a pioneering explanation of climate change, in which shifting boundaries between oceans and continents could be used to explain long-term variations ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Edward Forbes
Edward Forbes FRS, FGS (12 February 1815 – 18 November 1854) was a Manx naturalist. In 1846, he proposed that the distributions of montane plants and animals had been compressed downslope, and some oceanic islands connected to the mainland, during the recent ice age. This mechanism, which was the first natural explanation to explain the distributions of the same species on now-isolated islands and mountain tops, was discovered independently by Charles Darwin, who credited Forbes with the idea. He also incorrectly deduced the so-called azoic hypothesis, that life under the sea would decline to the point that no life forms could exist below a certain depth. Early years Forbes was born at Douglas on the Isle of Man. His father was a well-to-do banker. As a child, Forbes was very interested in collecting insects, shells, minerals, fossils, and plants. Due to poor health, he was unable to attend school from his 5th through his 11th years. In 1828, he started attending the At ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eocene
The Eocene ( ) Epoch is a geological epoch that lasted from about 56 to 33.9 million years ago (mya). It is the second epoch of the Paleogene Period in the modern Cenozoic Era. The name ''Eocene'' comes from the Ancient Greek (''ēṓs'', " dawn") and (''kainós'', "new") and refers to the "dawn" of modern ('new') fauna that appeared during the epoch. The Eocene spans the time from the end of the Paleocene Epoch to the beginning of the Oligocene Epoch. The start of the Eocene is marked by a brief period in which the concentration of the carbon isotope 13C in the atmosphere was exceptionally low in comparison with the more common isotope 12C. The end is set at a major extinction event called the ''Grande Coupure'' (the "Great Break" in continuity) or the Eocene–Oligocene extinction event, which may be related to the impact of one or more large bolides in Siberia and in what is now Chesapeake Bay. As with other geologic periods, the strata that define the start and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Richard Owen
Sir Richard Owen (20 July 1804 – 18 December 1892) was an English biologist, comparative anatomist and paleontologist. Owen is generally considered to have been an outstanding naturalist with a remarkable gift for interpreting fossils. Owen produced a vast array of scientific work, but is probably best remembered today for coining the word '' Dinosauria'' (meaning "Terrible Reptile" or "Fearfully Great Reptile"). An outspoken critic of Charles Darwin's theory of evolution by natural selection, Owen agreed with Darwin that evolution occurred, but thought it was more complex than outlined in Darwin's ''On the Origin of Species''. Owen's approach to evolution can be considered to have anticipated the issues that have gained greater attention with the recent emergence of evolutionary developmental biology. Owen was the first president of the Microscopical Society of London in 1839 and edited many issues of its journal – then known as '' The Microscopic Journal''. Owen als ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
British Museum
The British Museum is a public museum dedicated to human history, art and culture located in the Bloomsbury area of London. Its permanent collection of eight million works is among the largest and most comprehensive in existence. It documents the story of human culture from its beginnings to the present.Among the national museums in London, sculpture and decorative and applied art are in the Victoria and Albert Museum; the British Museum houses earlier art, non-Western art, prints and drawings. The National Gallery holds the national collection of Western European art to about 1900, while art of the 20th century on is at Tate Modern. Tate Britain holds British Art from 1500 onwards. Books, manuscripts and many works on paper are in the British Library. There are significant overlaps between the coverage of the various collections. The British Museum was the first public national museum to cover all fields of knowledge. The museum was established in 1753, largely b ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Crocodylus Hastingsae
''Diplocynodon'' is an extinct genus of alligatoroid that lived during the Paleocene to Middle Miocene in Europe. It looked very similar to the modern caiman in that it was small and had bony armour scutes covering its neck, back, belly, and tail. The longest ''Diplocynodon'' recovered was 4 feet in length and probably fed on small fish, frogs, and took insects when young. In the nineteenth century, ''D. steineri'' was named from Styria, Austria and ''D. styriacus'' was named from Austria and France. A third Austrian species, ''Enneodon ungeri'', was placed in its own genus. The Austrian and French species of ''Diplocynodon'' were synonymized with ''E. ungeri'' in 2011, and because the name ''Diplocynodon'' has priority over ''Enneodon'', the species is now called ''D. ungeri''. Other genera have recently been found to be synonymous with ''Diplocynodon''. ''Hispanochampsa muelleri'' of Spain was determined to be synonymous with ''Diplocynodon'' in 2006, and ''Baryphracta dep ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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