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Nairn V The University Court Of The University Of St Andrews
Nairn (; gd, Inbhir Narann) is a town and royal burgh in the Highland (council area), Highland council areas of Scotland, council area of Scotland. It is an ancient fishing port and market town around east of Inverness, at the point where the River Nairn enters the Moray Firth. It is the traditional county town of county of Nairn, Nairnshire. At the 2011 United Kingdom census, 2011 census, Nairn had a population of 9,773, making it the third-largest settlement in the Highland council area, behind Inverness and Fort William, Highland, Fort William. Nairn is best known as a seaside resort, with two golf courses, award-winning beaches, a community centre and arts venue, a small theatre (called The Little Theatre) and one small museum, providing information on the local area and incorporating the collection of the former Fishertown museum. History The History of Nairn is a broad and diverse topic spanning its Palaeolithic and Mesolithic roots before recorded history, to the Pict ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Highland (council Area)
Highland ( gd, A' Ghàidhealtachd, ; sco, Hieland) is a council area in the Scottish Highlands and is the largest local government area in the United Kingdom. It was the 7th most populous council area in Scotland at the 2011 census. It shares borders with the council areas of Aberdeenshire, Argyll and Bute, Moray and Perth and Kinross. Their councils, and those of Angus and Stirling, also have areas of the Scottish Highlands within their administrative boundaries. The Highland area covers most of the mainland and inner-Hebridean parts of the historic counties of Inverness-shire and Ross and Cromarty, all of Caithness, Nairnshire and Sutherland and small parts of Argyll and Moray. Despite its name, the area does not cover the entire Scottish Highlands. Name Unlike the other council areas of Scotland, the name ''Highland'' is often not used as a proper noun. The council's website only sometimes refers to the area as being ''Highland'', and other times as being '' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Seaside Resort
A seaside resort is a town, village, or hotel that serves as a vacation resort and is located on a coast. Sometimes the concept includes an aspect of official accreditation based on the satisfaction of certain requirements, such as in the German ''Seebad''. Where a beach is the primary focus for tourists, it may be called a beach resort. History Seaside resorts have existed since antiquity. In Roman times, the town of Baiae, by the Tyrrhenian Sea in Italy, was a resort for those who were sufficiently prosperous. Barcola in northern Italy, with its Roman luxury villas, is considered a special example of ancient leisure culture by the sea. Mersea Island, in Essex, England was a seaside holiday destination for wealthy Romans living in Colchester. The development of the beach as a popular leisure resort from the mid-19th century was the first manifestation of what is now the global tourist industry. The first seaside resorts were opened in the 18th century for the ari ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jurassic
The Jurassic ( ) is a geologic period and stratigraphic system that spanned from the end of the Triassic Period million years ago (Mya) to the beginning of the Cretaceous Period, approximately Mya. The Jurassic constitutes the middle period of the Mesozoic Era and is named after the Jura Mountains, where limestone strata from the period were first identified. The start of the Jurassic was marked by the major Triassic–Jurassic extinction event, associated with the eruption of the Central Atlantic Magmatic Province. The beginning of the Toarcian Stage started around 183 million years ago and is marked by an extinction event associated with widespread oceanic anoxia, ocean acidification, and elevated temperatures likely caused by the eruption of the Karoo-Ferrar large igneous provinces. The end of the Jurassic, however, has no clear boundary with the Cretaceous and is the only boundary between geological periods to remain formally undefined. By the beginning of the Jurassi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Permian–Triassic Extinction Event
The Permian–Triassic (P–T, P–Tr) extinction event, also known as the Latest Permian extinction event, the End-Permian Extinction and colloquially as the Great Dying, formed the boundary between the Permian and Triassic geologic periods, as well as between the Paleozoic and Mesozoic eras, approximately 251.9 million years ago. It is the Earth's most severe known extinction event, with the extinction of 57% of biological families, 83% of genera, 81% of marine species and 70% of terrestrial vertebrate species. It was the largest known mass extinction of insects. There is evidence for one to three distinct pulses, or phases, of extinction. The scientific consensus is that the main cause of extinction was the large amount of carbon dioxide emitted by the volcanic eruptions that created the Siberian Traps, which elevated global temperatures, and in the oceans led to widespread anoxia and acidification. Proposed contributing factors include: the emission of much additi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alluvial Plain
An alluvial plain is a largely flat landform created by the deposition of sediment over a long period of time by one or more rivers coming from highland regions, from which alluvial soil forms. A floodplain is part of the process, being the smaller area over which the rivers flood at a particular period of time, whereas the alluvial plain is the larger area representing the region over which the floodplains have shifted over geological time. As the highlands erode due to weathering and water flow, the sediment from the hills is transported to the lower plain. Various creeks will carry the water further to a river, lake, bay, or ocean. As the sediments are deposited during flood conditions in the floodplain of a creek, the elevation of the floodplain will be raised. As this reduces the channel floodwater capacity, the creek will, over time, seek new, lower paths, forming a meander (a curving sinuous path). The leftover higher locations, typically natural levees at the margins o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
North Sea
The North Sea lies between Great Britain, Norway, Denmark, Germany, the Netherlands and Belgium. An epeiric sea, epeiric sea on the European continental shelf, it connects to the Atlantic Ocean through the English Channel in the south and the Norwegian Sea in the north. It is more than long and wide, covering . It hosts key north European shipping lanes and is a major fishery. The coast is a popular destination for recreation and tourism in bordering countries, and a rich source of energy resources, including wind energy, wind and wave power. The North Sea has featured prominently in geopolitical and military affairs, particularly in Northern Europe, from the Middle Ages to the modern era. It was also important globally through the power northern Europeans projected worldwide during much of the Middle Ages and into the modern era. The North Sea was the centre of the Viking Age, Vikings' rise. The Hanseatic League, the Dutch Golden Age, Dutch Republic, and the Kingdom of Grea ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
David I Of Scotland
David I or Dauíd mac Maíl Choluim ( Modern: ''Daibhidh I mac haoilChaluim''; – 24 May 1153) was a 12th-century ruler who was Prince of the Cumbrians from 1113 to 1124 and later King of Scotland from 1124 to 1153. The youngest son of Malcolm III and Margaret of Wessex, David spent most of his childhood in Scotland, but was exiled to England temporarily in 1093. Perhaps after 1100, he became a dependent at the court of King Henry I. There he was influenced by the Anglo-French culture of the court. When David's brother Alexander I died in 1124, David chose, with the backing of Henry I, to take the Kingdom of Scotland ( Alba) for himself. He was forced to engage in warfare against his rival and nephew, Máel Coluim mac Alaxandair. Subduing the latter seems to have taken David ten years, a struggle that involved the destruction of Óengus, Mormaer of Moray. David's victory allowed expansion of control over more distant regions theoretically part of his Kingdom. After the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sigurd The Stout
Sigurd Hlodvirsson (23 April 1014), popularly known as Sigurd the Stout from the Old Norse ''Sigurðr digri'',Thomson (2008) p. 59 was an Earl of Orkney. The main sources for his life are the Norse Sagas, which were first written down some two centuries or more after his death. These engaging stories must therefore be treated with caution rather than as reliable historical documents. Sigurd was the son of Hlodvir Thorfinnsson and (according to the Norse sagas) a direct descendant of Torf-Einarr Rognvaldson. Sigurd's tenure as earl was apparently free of the kin-strife that beset some other incumbents of this title and he was able to pursue his military ambitions over a wide area. He also held lands in the north of mainland Scotland and in the '' Sudrøyar'', and he may have been instrumental in the defeat of Gofraid mac Arailt, King of the Isles. The ''Annals of Ulster'' record his death at the Battle of Clontarf in 1014, the earliest known reference to the earldom of Orkney ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gnaeus Julius Agricola
Gnaeus Julius Agricola (; 13 June 40 – 23 August 93) was a Roman general and politician responsible for much of the Roman conquest of Britain. Born to a political family of senatorial rank, Agricola began his military career as a military tribune under Governor Gaius Suetonius Paulinus. In his subsequent career, he served in a variety of political positions in Rome. In 64, he was appointed quaestor in Asia province. Two years later, he was appointed Plebeian Tribune, and in 68, he was made praetor. During the Year of the Four Emperors in 69, he supported Vespasian, general of the Syrian army, in his bid for the throne. When Vespasian became emperor, Agricola was made a patrician and appointed governor of Gallia Aquitania. In 77, he was made consul and governor of Britannia. As governor, he completed the conquest of what is today Wales and northern England, and led his army to the far north of Scotland, establishing forts across much of the lowlands. In 85, Agricola was reca ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Picts
The Picts were a group of peoples who lived in what is now northern and eastern Scotland (north of the Firth of Forth) during Late Antiquity and the Early Middle Ages. Where they lived and what their culture was like can be inferred from early medieval texts and Pictish stones. Their Latin name, , appears in written records from the 3rd to the 10th century. Early medieval sources report the existence of a distinct Pictish language, which today is believed to have been an Insular Celtic language, closely related to the Brittonic spoken by the Britons who lived to the south. Picts are assumed to have been the descendants of the Caledonii and other Iron Age tribes that were mentioned by Roman historians or on the world map of Ptolemy. The Pictish kingdom, often called Pictland in modern sources, achieved a large degree of political unity in the late 7th and early 8th centuries through the expanding kingdom of Fortriu, the Iron Age Verturiones. By the year 900, the resulti ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mesolithic
The Mesolithic ( Greek: μέσος, ''mesos'' 'middle' + λίθος, ''lithos'' 'stone') or Middle Stone Age is the Old World archaeological period between the Upper Paleolithic and the Neolithic. The term Epipaleolithic is often used synonymously, especially for outside northern Europe, and for the corresponding period in the Levant and Caucasus. The Mesolithic has different time spans in different parts of Eurasia. It refers to the final period of hunter-gatherer cultures in Europe and Western Asia, between the end of the Last Glacial Maximum and the Neolithic Revolution. In Europe it spans roughly 15,000 to 5,000 BP; in Southwest Asia (the Epipalaeolithic Near East) roughly 20,000 to 10,000 BP. The term is less used of areas farther east, and not at all beyond Eurasia and North Africa. The type of culture associated with the Mesolithic varies between areas, but it is associated with a decline in the group hunting of large animals in favour of a broader hunter-g ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Palaeolithic
The Paleolithic or Palaeolithic (), also called the Old Stone Age (from Greek: παλαιός ''palaios'', "old" and λίθος '' lithos'', "stone"), is a period in human prehistory that is distinguished by the original development of stone tools, and which represents almost the entire period of human prehistoric technology. It extends from the earliest known use of stone tools by hominins, 3.3 million years ago, to the end of the Pleistocene, 11,650 cal BP. The Paleolithic Age in Europe preceded the Mesolithic Age, although the date of the transition varies geographically by several thousand years. During the Paleolithic Age, hominins grouped together in small societies such as bands and subsisted by gathering plants, fishing, and hunting or scavenging wild animals. The Paleolithic Age is characterized by the use of knapped stone tools, although at the time humans also used wood and bone tools. Other organic commodities were adapted for use as tools, incl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
