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This stock is one of those rare finds that you can hold forever and pass down to your grandchildren. It should be a core position in every investor's portfolio. [Сlісk hеrе for more about this little-known іnсomе stock gem.]( Sincerely, [Tim Plaehn] Tim Plaehn Former U.S. Air Force Captain Lead Inсоmе Analyst Investors Alley P.S. In this zero interest rаtе environment, consistent and safe high yields can be tough to come by. But this dividend stock is a rare exception with 8 years of superior dividend growth.   Toponymy Main article: Britain (place ) The archipelago has been referred to by a single for over years: the term 'British Isles' derives from used by classical geographers to describe this island group. By BC Greek geographers were using equivalents of Prettanikē as a collective for the British Isles. However, with the Roman conquest of Britain the Latin term Britannia was used for the island of Britain, and later Roman-occupied Britain south of Caledonia. The earliest known for GreatBritain is Albion (Greek: Ἀλβιών) or insula Albionum, from either the Latin albus meaning "white" (possibly referring to the white cliffs of Dover, the first view of Britain from the continent) or the "island of the Albiones". The oldest mention of related to GreatBritain was by Aristotle (– BC), or possibly by Pseudo-Aristotle, in his text On the Universe, Vol. III. To his works, "There are two very large islands in it, called the British Isles, Albion and Ierne". Greek geographer, Pytheas of Massalia The first known written use of the word Britain was an ancient Greek transliteration of the original P-Celtic term in a work on the travels and discoveries of Pytheas that has not survived. The earliest existing records of the word are quotations of the periplus by later authors, such as those within Strabo's Geographica, Pliny's Natural History and Diodorus of Sicily's Bibliotheca historica. Pliny the Elder (AD –) in his Natural History records of GreatBritain: "Its former was Albion; but at a later period, the islands, of which we shall just briefly make mention, were included under the of 'Britanniæ.'" The Britain descends from the Latin for Britain, Britannia or Brittānia, the land of the Britons. Old French Bretaigne (whence also Modern French Bretagne) and Middle English Bretayne, Breteyne. The French replaced the Old English Breoton, Breoten, Bryten, Breten (also Breoton-lond, Breten-lond). Britannia was used by the Romans from the st century BC for the British Isles taken together. It is derived from the travel writings of Pytheas around BC, which described various islands in the North Atlantic as far north as Thule (probably Norway). The peoples of these islands of Prettanike were called the Πρεττανοί, Priteni or Pretani. Priteni is the source of the Welsh language term Prydain, Britain, which has the same source as the Goidelic term Cruithne used to refer to the early Brythonic-speaking inhabitants of Ireland. The latter were later called Picts or Caledonians by the Romans. Greek historians Diodorus of Sicily and Strabo preserved variants of Prettanike from the work of Greek explorer Pytheas of Massalia, who travelled from his in Hellenistic southern Gaul to Britain in the th century BC. The term used by Pytheas may derive from a Celtic word meaning "the painted ones" or "the tattooed folk" in reference to body decorations. According to Strabo, Pytheas referred to Britain as Bretannikē, which is treated a feminine noun. Marcian of Heraclea, in his Periplus maris exteri, described the island group as αἱ Πρεττανικαὶ νῆσοι (the Prettanic Isles). Derivation A Italian reconstruction of the relevant map of Ptolemy who combined the lines of roads and of the coasting expeditions during the first century of Roman occupation. Two faults, however, are an eastward-projecting Scotland and none of Ireland seen to be at the same latitude of Wales, which may have been if Ptolemy used Pytheas' measurements of latitude. Whether he did so is a much debated issue. This "copy" appears in blue below. The Greco-Egyptian scientist Ptolemy referred to the larger island as Britain (μεγάλη Βρεττανία megale Brettania) and to Ireland as little Britain (μικρὰ Βρεττανία mikra Brettania) in his work Almagest (– AD). In his later work, Geography (c. AD), he gave the islands the names Alwion, Iwernia, and Mona (the Isle of Man), suggesting these may have been the names of the individual islands not known to him at the time of writing Almagest. The Albion appears to have fallen out of use sometime after the Roman conquest of Britain, after which Britain became the more commonplace for the island. After the Anglo-Saxon period, Britain was used as a historical term . Geoffrey of Monmouth in his pseudohistorical Historia Regum Britanniae (c. ) refers to the island of GreatBritain as Britannia major ("Greater Britain"), to distinguish it from Britannia minor ("Lesser Britain"), the continental region which approximates to modern Brittany, which had been settled in the fifth and sixth centuries by Celtic Briton migrants from GreatBritain.[citation needed] The term GreatBritain was first used officially in , in the instrument drawing up the proposal for a marriage between Cecily, daughter of Edward IV of England, and James, son of James III of Scotland, which described it as "this Nobill Isle, callit Gret Britanee". While promoting a possible royal match in , Lord Protector Somerset said that the English and Scots were, "like as twoo brethren of one Islande of Britaynes again." In , James VI and I styled himself "King of Brittaine, France and Ireland". Modern use of the term GreatBritain GreatBritain refers geographically to the island of GreatBritain. Politically, it may refer to the whole of England, Scotland and Wales, including their smaller islands. It is not technically correct to use the term to refer to the whole of the United Kingdom which includes Northern Ireland, though the Oxford English Dictionary states "...the term is also used loosely to refer to the United Kingdom." Similarly, Britain can refer to either islands in GreatBritain, the largest island, or the political grouping of countries. There is no clear distinction, even in government documents: the UK government yearbooks have used both Britain and United Kingdom. GB and GBR are used instead of UK in some international codes to refer to the United Kingdom, including the Universal Postal Union, international sports teams, NATO, and the International Organization for Standardization country codes ISO - and ISO - alpha-, whilst the aircraft registration prefix is G. On the Internet, .uk is the country code top-level domain for the United Kingdom. A .gb top-level domain was used to a extent, but is deprecated; although existing registrations still exist (mainly by government organizations and email providers), the domain registrar will not take registrations. In the Olympics, Team GB is used by the British Olympic Association to represent the British Olympic team. The Olympic Federation of Ireland represents the whole island of Ireland, and Northern Irish sportspeople may choose to compete for either team, most choosing to represent Ireland. Political definition Political definition of GreatBritain (dark green) – in Europe (green & dark grey) – in the United Kingdom (green) Politically, GreatBritain refers to the whole of England, Scotland and Wales in combination, but not Northern Ireland; it includes islands, such as the Isle of Wight, Anglesey, the Isles of Scilly, the Hebrides and the island groups of Orkney and Shetland, that are part of England, Wales, or Scotland. It does not include the Isle of Man and the Channel Islands. The political union that joined the kingdoms of England and Scotland happened in when the Acts of Union ratified the Treaty of Union and merged the parliaments of the two nations, forming the Kingdom of GreatBritain, which covered the entire island. Before this, a personal union had existed between these two countries since the Union of the Crowns under James VI of Scotland and I of England.[citation needed] History Prehistoric period Main article: Prehistoric Britain GreatBritain was probably first inhabited by those who crossed on the land bridge from the European mainland. footprints have been found from over , years ago in Norfolk and traces of early humans have been found (at Boxgrove Quarry, Sussex) from some , years ago and modern humans from about , years ago. Until about , years ago, it was connected to Ireland by an ice bridge, prior to , years ago it retained a land connection to the continent, with an area of mostly low marshland joining it to what are Denmark and the Netherlands. In Cheddar Gorge, near Bristol, the remains of animal species native to mainland Europe such as antelopes, brown bears, and wild horses have been found alongside a skeleton, 'Cheddar Man', dated to about BC. GreatBritain became an island at the end of the last glacial period when sea levels rose due to the combination of melting glaciers and the subsequent isostatic rebound of the crust. GreatBritain's Iron Age inhabitants are known as Britons; they spoke Celtic languages. Roman and medieval period Main articles: Roman Britain, Medieval England, Medieval Scotland, and Medieval Wales Ptolomy's historical map of Roman Britain Prima Europe tabula. A copy of Ptolemy's nd-century map of Roman Britain. See notes to image above. The Romans conquered most of the island (up to Hadrian's Wall in northern England) and this became the Ancient Roman province of Britannia. In the course of the years after the Roman Empire fell, the Britons of the south and east of the island were assimilated or displaced by invading Germanic tribes (Angles, Saxons, and Jutes, often referred to collectively as Anglo-Saxons). At about the same time, Gaelic tribes from Ireland invaded the north-west, absorbing both the Picts and Britons of northern Britain, eventually forming the Kingdom of Scotland in the th century. The south-east of Scotland was colonised by the Angles and formed, until , a part of the Kingdom of Northumbria. Ultimately, the population of south-east Britain came to be referred to as the English people, so-named after the Angles. Germanic speakers referred to Britons as Welsh. This term came to be applied exclusively to the inhabitants of what is Wales, but it also survives in names such as Wallace and in the second syllable of Cornwall. Cymry, a the Britons used to describe themselves, is similarly restricted in modern Welsh to people from Wales, but also survives in English in the place of Cumbria. The Britons living in the areas known as Wales, Cumbria and Cornwall were not assimilated by the Germanic tribes, a fact reflected in the survival of Celtic languages in these areas into more recent times. At the time of the Germanic invasion of southern Britain, many Britons emigrated to the area known as Brittany, where Breton, a Celtic language closely related to Welsh and Cornish and descended from the language of the emigrants, is still spoken. In the th century, a series of Danish assaults on northern English kingdoms led to them coming under Danish control (an area known as the Danelaw). In the th century, however, the English kingdoms were unified under one ruler as the kingdom of England when the last constituent kingdom, Northumbria, submitted to Edgar in . In , England was conquered by the Normans, who introduced a Norman-speaking administration that was eventually assimilated. Wales came under Anglo-Norman control in , and was officially annexed to England in the th century. Early modern period Main article: Early modern Britain Further information: History of the United Kingdom On October King James, who had succeeded separately to the two thrones of England and Scotland, proclaimed himself "King of GreatBrittaine, France, and Ireland". When James died in and the Privy Council of England was drafting the proclamation of the king, Charles I, a Scottish peer, Thomas Erskine, st Earl of Kellie, succeeded in insisting that it use the phrase "King of Britain", which James had preferred, rather than King of Scotland and England (or vice versa). While that title was also used by some of James's successors, England and Scotland each remained legally separate countries, each with its own parliament, until , when each parliament passed an of Union to ratify the Treaty of Union that had been agreed the previous year. This created a single kingdom with one parliament with effect from May . The Treaty of Union specified the of the -island state as "GreatBritain", while describing it as "One Kingdom" and "the United Kingdom". To most historians, therefore, the -island state that existed between and is either "GreatBritain" or the "Kingdom of GreatBritain". Geography Further information: Geography of England, Geography of Scotland, and Geography of Wales See also: Geography of the United Kingdom View of Britain's coast from Cap Gris-Nez in northern France GreatBritain lies on the European continental shelf, part of the Eurasian Plate and the north-west coast of continental Europe, separated from this European mainland by the North Sea and by the English Channel, which narrows to km ( nmi; mi) at the Straits of Dover. It stretches over about ten degrees of latitude on its longer, north–south axis and covers , km (, sq mi), excluding the much smaller surrounding islands. The North Channel, Irish Sea, St George's Channel and Celtic Sea separate the island from the island of Ireland to its west. The island is since joined, via one structure, with continental Europe: the Channel Tunnel, the longest undersea rail tunnel in the world. The island is marked by low, rolling countryside in the east and south, while hills and mountains predominate in the western and northern regions. It is surrounded by over , smaller islands and islets. The greatest distance between two points is . km (+⁄ mi) (between Land's End, Cornwall and John o' Groats, Caithness), miles (, km) by road. The English Channel is thought to have been created between , and , years ago by two catastrophic glacial lake outburst floods caused by the breaching of the Weald-Artois Anticline, a ridge that held back a large proglacial lake, submerged under the North Sea. Around , years ago, during the Devensian glaciation with its lower sea level, Britain was not an island, but an upland region of continental north-western Europe, lying partially underneath the Eurasian ice sheet. The sea level was about metres ( ft) lower than , and the bed of the North Sea was dry and acted as a land bridge, known as Doggerland, to the Continent. It is generally thought that as sea levels gradually rose after the end of the last glacial period of the current ice age, Doggerland reflooded cutting what was the British peninsula from the European mainland by around BC. Geology Main article: Geology of GreatBritain GreatBritain has been a variety of plate tectonic processes over a very extended period of time. Changing latitude and sea levels have been important factors in the nature of sedimentary sequences, whilst successive continental collisions have affected its geological structure with major faulting and folding being a legacy of each orogeny (mountain-building period), often associated with volcanic activity and the metamorphism of existing rock sequences. As a result of this eventful geological history, the island shows a rich variety of landscapes. The oldest rocks in GreatBritain are the Lewisian gneisses, metamorphic rocks found in the far north west of the island and in the Hebrides (with a few small outcrops elsewhere), which date from at least , My ago. South of the gneisses are a complex mixture of rocks forming the North West Highlands and Grampian Highlands in Scotland. These are essentially the remains of folded sedimentary rocks that were deposited between , My and My ago over the gneiss on what was then the floor of the Iapetus Ocean. In the current era the north of the island is rising as a result of the weight of Devensian ice being lifted. Counterbalanced, the south and east is sinking, generally estimated at mm (⁄ inch) , with the London area sinking at double this partly due to the continuing compaction of the recent clay deposits. Fauna Main article: Fauna of GreatBritain European robin on a branch facing left, tan plumage with orange face and throat The robin is popularly known as "Britain's favourite bird". Animal diversity is modest, as a result of factors including the island's small land area, the relatively recent age of the habitats developed since the last glacial period and the island's physical separation from continental Europe, and the effects of seasonal variability. GreatBritain also experienced early industrialisation and is continuing urbanisation, which have contributed towards the overall loss of species. A DEFRA (Department for Environment, Food and Rural Affairs) study from suggested that species have become extinct in the UK during the th century, about times the background extinction. However, some species, such as the brown rat, red fox, and introduced grey squirrel, are well adapted to urban areas. Rodents make up of the mammal species.[citation needed] These include squirrels, mice, voles, rats and the recently reintroduced European beaver. There is also an abundance of European rabbit, European hare, shrews, European mole and several species of bat. Carnivorous mammals include the red fox, Eurasian badger, Eurasian otter, weasel, stoat and elusive Scottish wildcat. Various species of seal, whale and dolphin are found on or around British shores and coastlines. The largest land-based wild animals are deer. The red deer is the largest species, with roe deer and fallow deer also prominent; the latter was introduced by the Normans. Sika deer and two more species of smaller deer, muntjac and Chinese water deer, have been introduced, muntjac becoming widespread in England and parts of Wales while Chinese water deer are restricted mainly to East Anglia. Habitat loss has affected many species. Extinct large mammals include the brown bear, grey wolf and wild boar; the latter has had a reintroduction in recent times. There is a wealth of birdlife, with species recorded, of which breed on the island or remain during winter. Because of its mild winters for its latitude, GreatBritain hosts important numbers of many wintering species, particularly waders, ducks, geese and swans. Other well known bird species include the golden eagle, grey heron, common kingfisher, common wood pigeon, house sparrow, European robin, grey partridge, and various species of crow, finch, gull, auk, grouse, owl and falcon. There are six species of reptile on the island; three snakes and three lizards including the legless slowworm. One snake, the adder, is venomous but rarely deadly. Amphibians present are frogs, toads and newts. There are also several introduced species of reptile and amphibian. Flora See also: List of the vascular plants of Britain and Ireland purple heather in meadow showing flower spikes Heather growing wild in the Highlands at Dornoch In a similar sense to fauna, and for similar reasons, the flora consists of fewer species compared to much larger continental Europe. The flora comprises , vascular plant species, of which , are native and , have been introduced. The island has a wide variety of trees, including native species of birch, beech, ash, hawthorn, elm, oak, yew, pine, cherry and apple. Other trees have been naturalised, introduced especially from other parts of Europe (particularly Norway) and North America. Introduced trees include several varieties of pine, chestnut, maple, spruce, sycamore and fir, as well as cherry plum and pear trees. The tallest species are the Douglas firs; two specimens have been recorded measuring metres or feet. The Fortingall Yew in Perthshire is the oldest tree in Europe. There are at least , different species of wildflower. Some species are particularly rare or vulnerable and are protected by the Wildlife and Countryside . It is illegal to uproot any wildflowers without the landowner's permission. A vote in nominated various wildflowers to represent specific counties. These include red poppies, bluebells, daisies, daffodils, rosemary, gorse, iris, ivy, mint, orchids, brambles, thistles, buttercups, primrose, thyme, tulips, violets, cowslip, heather and many more. There is also more than species of bryophyte including algae and mosses across the island. The currently known species include mosses, liverworts and hornworts. Fungi There are many species of fungi including lichen-forming species, and the mycobiota is less poorly known than in many other parts of the world. The most recent checklist of Basidiomycota (bracket fungi, jelly fungi, mushrooms and toadstools, puffballs, rusts and smuts), published in , accepts over species. The most recent checklist of Ascomycota (cup fungi and their allies, including most lichen-forming fungi), published in , accepts another species. These two lists did not include conidial fungi (fungi mostly with affinities in the Ascomycota but known in their asexual state) or any of the other main fungal groups (Chytridiomycota, Glomeromycota and Zygomycota). The number of fungal species known very probably exceeds ,. There is widespread agreement among mycologists that many others are yet to be discovered.     ExpertModernAdvice.com brought to you by Inception Media Group. This editorial email with educational news was sent to {EMAIL}. IMG appreciates your comments and inquiries. Please keep in mind, that Inception Media Group are not permitted to provide individualized financial аdvіsе. 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