1.
Richter magnitude scale
–
The Richter magnitude scale assigns a magnitude number to quantify the size of an earthquake. As measured with a seismometer, an earthquake that registers 5.0 on the Richter scale has a shaking amplitude 10 times greater than an earthquake that registered 4.0 at the same distance. This means that, for instance, an earthquake of magnitude 5 releases 31.6 times as energy as an earthquake of magnitude 4. In the United States, the Richter scale was succeeded in the 1970s by the moment magnitude scale, the moment magnitude scale is now the scale used by the United States Geological Survey to estimate magnitudes for all modern large earthquakes. Richter derived his earthquake-magnitude scale from the apparent magnitude scale used to measure the brightness of stars and that fixed measure was chosen to avoid negative values for magnitude, given that the slightest earthquakes that could be recorded and located at the time were around magnitude 3.0. The Richter magnitude scale itself has no limit, and contemporary seismometers can register, record. M L was not designed to be applied to data with distances to the hypocenter of the earthquake that were greater than 600 km. Later, to express the size of earthquakes around the planet, Gutenberg and Richter developed a surface wave magnitude scale and these are types of waves that are recorded at teleseismic distances. The two scales were adjusted such that they were consistent with the M L scale and that adjustment succeeded better with the M s scale than with the M b scale. Each scale saturates when the earthquake is greater than magnitude 8.0, because of this, researchers in the 1970s developed the moment magnitude scale. The older magnitude-scales were superseded by methods for calculating the seismic moment, about the origins of the Richter magnitude scale, C. F. Richter said, I found a paper by Professor K. Wadati of Japan in which he compared large earthquakes by plotting the maximum ground motion against distance to the epicenter. I tried a similar procedure for our stations, but the range between the largest and smallest magnitudes seemed unmanageably large, dr. Beno Gutenberg then made the natural suggestion to plot the amplitudes logarithmically. I was lucky, because logarithmic plots are a device of the devil, the particular instrument used would become saturated by strong earthquakes and unable to record high values. The scale was replaced in the 1970s by the moment magnitude scale, for earthquakes adequately measured by the Richter scale, anything above 5 is classified as a risk by the USGS. Several scales have historically described as the Richter scale, especially the local magnitude M L. In addition, the body wave magnitude, m b, a couple of new techniques to measure magnitude are in the development stage by seismologists. All magnitude scales have been designed to give similar results
2.
Geographic coordinate system
–
A geographic coordinate system is a coordinate system used in geography that enables every location on Earth to be specified by a set of numbers, letters or symbols. The coordinates are chosen such that one of the numbers represents a vertical position. A common choice of coordinates is latitude, longitude and elevation, to specify a location on a two-dimensional map requires a map projection. The invention of a coordinate system is generally credited to Eratosthenes of Cyrene. Ptolemy credited him with the adoption of longitude and latitude. Ptolemys 2nd-century Geography used the prime meridian but measured latitude from the equator instead. Mathematical cartography resumed in Europe following Maximus Planudes recovery of Ptolemys text a little before 1300, in 1884, the United States hosted the International Meridian Conference, attended by representatives from twenty-five nations. Twenty-two of them agreed to adopt the longitude of the Royal Observatory in Greenwich, the Dominican Republic voted against the motion, while France and Brazil abstained. France adopted Greenwich Mean Time in place of local determinations by the Paris Observatory in 1911, the latitude of a point on Earths surface is the angle between the equatorial plane and the straight line that passes through that point and through the center of the Earth. Lines joining points of the same latitude trace circles on the surface of Earth called parallels, as they are parallel to the equator, the north pole is 90° N, the south pole is 90° S. The 0° parallel of latitude is designated the equator, the plane of all geographic coordinate systems. The equator divides the globe into Northern and Southern Hemispheres, the longitude of a point on Earths surface is the angle east or west of a reference meridian to another meridian that passes through that point. All meridians are halves of great ellipses, which converge at the north and south poles, the prime meridian determines the proper Eastern and Western Hemispheres, although maps often divide these hemispheres further west in order to keep the Old World on a single side. The antipodal meridian of Greenwich is both 180°W and 180°E, the combination of these two components specifies the position of any location on the surface of Earth, without consideration of altitude or depth. The grid formed by lines of latitude and longitude is known as a graticule, the origin/zero point of this system is located in the Gulf of Guinea about 625 km south of Tema, Ghana. To completely specify a location of a feature on, in, or above Earth. Earth is not a sphere, but a shape approximating a biaxial ellipsoid. It is nearly spherical, but has an equatorial bulge making the radius at the equator about 0. 3% larger than the radius measured through the poles, the shorter axis approximately coincides with the axis of rotation
3.
England
–
England is a country that is part of the United Kingdom. It shares land borders with Scotland to the north and Wales to the west, the Irish Sea lies northwest of England and the Celtic Sea lies to the southwest. England is separated from continental Europe by the North Sea to the east, the country covers five-eighths of the island of Great Britain in its centre and south, and includes over 100 smaller islands such as the Isles of Scilly, and the Isle of Wight. England became a state in the 10th century, and since the Age of Discovery. The Industrial Revolution began in 18th-century England, transforming its society into the worlds first industrialised nation, Englands terrain mostly comprises low hills and plains, especially in central and southern England. However, there are uplands in the north and in the southwest, the capital is London, which is the largest metropolitan area in both the United Kingdom and the European Union. In 1801, Great Britain was united with the Kingdom of Ireland through another Act of Union to become the United Kingdom of Great Britain and Ireland. In 1922 the Irish Free State seceded from the United Kingdom, leading to the latter being renamed the United Kingdom of Great Britain, the name England is derived from the Old English name Englaland, which means land of the Angles. The Angles were one of the Germanic tribes that settled in Great Britain during the Early Middle Ages, the Angles came from the Angeln peninsula in the Bay of Kiel area of the Baltic Sea. The earliest recorded use of the term, as Engla londe, is in the ninth century translation into Old English of Bedes Ecclesiastical History of the English People. According to the Oxford English Dictionary, its spelling was first used in 1538. The earliest attested reference to the Angles occurs in the 1st-century work by Tacitus, Germania, the etymology of the tribal name itself is disputed by scholars, it has been suggested that it derives from the shape of the Angeln peninsula, an angular shape. An alternative name for England is Albion, the name Albion originally referred to the entire island of Great Britain. The nominally earliest record of the name appears in the Aristotelian Corpus, specifically the 4th century BC De Mundo, in it are two very large islands called Britannia, these are Albion and Ierne. But modern scholarly consensus ascribes De Mundo not to Aristotle but to Pseudo-Aristotle, the word Albion or insula Albionum has two possible origins. Albion is now applied to England in a poetic capacity. Another romantic name for England is Loegria, related to the Welsh word for England, Lloegr, the earliest known evidence of human presence in the area now known as England was that of Homo antecessor, dating to approximately 780,000 years ago. The oldest proto-human bones discovered in England date from 500,000 years ago, Modern humans are known to have inhabited the area during the Upper Paleolithic period, though permanent settlements were only established within the last 6,000 years
4.
Essex
–
Essex /ˈɛsᵻks/ is a county in England immediately north-east of London. It borders the counties of Suffolk and Cambridgeshire to the north, Hertfordshire to the west, Kent across the estuary of the River Thames to the south, the county town is Chelmsford, which is the only city in the county. Essex occupies the part of the old Kingdom of Essex, before this. As well as areas, the county also includes London Stansted Airport, the new towns of Basildon and Harlow, Lakeside Shopping Centre, the port of Tilbury. Originally recorded in AD527, Essex occupied territory to the north of the River Thames, incorporating all of what later became Middlesex and its territory was later restricted to lands east of the River Lea. In changes before the Norman conquest the East Saxons were subsumed into the Kingdom of England and, following the Norman conquest, Essex became a county. During the medieval period, much of the area was designated a Royal forest, including the county in a period to 1204. Gradually, the subject to forest law diminished, but at various times included the forests of Becontree, Chelmsford, Epping, Hatfield, Ongar. County-wide administration Essex County Council was formed in 1889, however County Boroughs of West Ham, Southend-on-Sea and East Ham formed part of the county but were unitary authorities. 12 boroughs and districts provide more localised services such as rubbish and recycling collections, leisure and planning, parish-level administration – changes A few Essex parishes have been transferred to other counties. Before 1889, small areas were transferred to Hertfordshire near Bishops Stortford, Essex became part of the East of England Government Office Region in 1994 and was statistically counted as part of that region from 1999, having previously been part of the South East England region. Two unitary authorities In 1998 the boroughs of Southend-on-Sea and Thurrock were granted autonomy from the county of Essex after successful requests to become unitary authorities. Essex Police covers the county and the two unitary authorities. The county council chamber and main headquarters is at the County Hall in Chelmsford, before 1938 the council regularly met in London near Moorgate, which with significant parts closer to that point and the dominance of railways had been more convenient than any place in the county. It currently has 75 elected councillors, before 1965, the number of councillors reached over 100. The highest point of the county of Essex is Chrishall Common near the village of Langley, close to the Hertfordshire border, the pattern of settlement in the county is diverse. Epping Forest also acts as a barrier to the further spread of London. Part of the southeast of the county, already containing the population centres of Basildon, Southend and Thurrock, is within the Thames Gateway
5.
Virley
–
Virley is a village in the Colchester borough of Essex, England and forms part of the Winstred Hundred civil parish. According to the 2001 census it had a population of 61, the village is about seven miles south of Colchester. Virley is among the villages which suffered damage from the 1884 Colchester earthquake, the village church was destroyed in the quake
6.
Colchester
–
Colchester /ˈkoʊltʃɛstər/ is an historic large town and the largest settlement within the borough of Colchester in the county of Essex. As the oldest recorded Roman town in Britain, Colchester is claimed to be the oldest town in Britain and it was for a time the capital of Roman Britain, and is a member of the Most Ancient European Towns Network. Colchester is some 50 miles northeast of London and is connected to the capital by the A12 road and it is seen as a popular town for commuters, and is less than 30 miles away from Stansted Airport and 20 miles from the passenger ferry port of Harwich. Colchester is home to Colchester Castle and Colchester United Football Club and it has a Conservative Member of Parliament, Will Quince, who was elected in the 2015 General Election. The River Colne runs through the town and it is a widely held belief that the name Colchester is derived from the Latin words Colonia and Castra, meaning fortifications. The earliest forms of the name Colchester are Colenceaster and Colneceastre from the 10th century, in this way of interpreting the name, the River Colne which runs through the town takes its name from Colonia as well. Cologne also gained its name from a similar etymology, ekwall went as far as to say it has often been held that Colchester contains as first element colonia. This derivation is ruled out of court by the fact that Colne is the name of old villages situated a good many miles from Colchester. The identification of Colonia with Colchester is doubtful, from these deposits beneath the town have been found Palaeolithic flint tools, including at least six Acheulian handaxes. Further flint tools made by hunter gatherers living in the Colne Valley during the Mesolithic have been discovered and this included a pit found at Culver Street containing a ritually placed Neolithic grooved ware pot, as well as find spots containing later Deverel-Rimbury bucket urns. Before the Roman conquest of Britain it was already a centre of power for Cunobelin – known to Shakespeare as Cymbeline – king of the Catuvellauni, who minted coins there. Its Celtic name, Camulodunon, variously represented as CA, CAM, CAMV, CAMVL and CAMVLODVNO on the coins of Cunobelinus, during the 30s AD Camulodunon controlled a large swathe of Southern and Eastern Britain, with Cunobelin called King of the Britons by Roman writers. Camulodunon is considered one of possible sites around Britain for the legendary Camelot of King Arthur. Soon after the Roman conquest of Britain in AD43, a Roman legionary fortress was established, later, when the Roman frontier moved outwards and the twentieth legion had moved to the west, Camulodunum became a colonia named in a second-century inscription as Colonia Victricensis. This contained a large and elaborate Temple to the Divine Claudius, Colchester is home to two of the five Roman theatres found in Britain, the one at Gosbecks being the largest in Britain, able to seat 5,000. Camulodunum served as a provincial Roman capital of Britain, but was attacked and destroyed during Boudicas rebellion in AD61, sometime after the destruction, London became the capital of the province of Britannia. Colchesters town walls c.3,000 yd. long were built c. 65–80 A. D. when the Roman town was rebuilt after the Boudicca rebellion. In 2004, Colchester Archaeological Trust discovered the remains of a Roman Circus underneath the Garrison in Colchester, the Roman town of Camulodunum, officially known as Colonia Victricensis, reached its peak in the Second and Third centuries AD
7.
Earthquake
–
An earthquake is the shaking of the surface of the Earth, resulting from the sudden release of energy in the Earths lithosphere that creates seismic waves. Earthquakes can range in size from those that are so weak that they cannot be felt to those violent enough to people around. The seismicity or seismic activity of an area refers to the frequency, type, Earthquakes are measured using measurements from seismometers. The moment magnitude is the most common scale on which earthquakes larger than approximately 5 are reported for the entire globe and these two scales are numerically similar over their range of validity. Magnitude 3 or lower earthquakes are mostly imperceptible or weak and magnitude 7 and over potentially cause damage over larger areas. The largest earthquakes in historic times have been of magnitude slightly over 9, intensity of shaking is measured on the modified Mercalli scale. The shallower an earthquake, the damage to structures it causes. At the Earths surface, earthquakes manifest themselves by shaking and sometimes displacement of the ground, when the epicenter of a large earthquake is located offshore, the seabed may be displaced sufficiently to cause a tsunami. Earthquakes can also trigger landslides, and occasionally volcanic activity, in its most general sense, the word earthquake is used to describe any seismic event — whether natural or caused by humans — that generates seismic waves. Earthquakes are caused mostly by rupture of faults, but also by other events such as volcanic activity, landslides, mine blasts. An earthquakes point of rupture is called its focus or hypocenter. The epicenter is the point at ground level directly above the hypocenter, tectonic earthquakes occur anywhere in the earth where there is sufficient stored elastic strain energy to drive fracture propagation along a fault plane. The sides of a fault move past each other smoothly and aseismically only if there are no irregularities or asperities along the surface that increase the frictional resistance. Most fault surfaces do have such asperities and this leads to a form of stick-slip behavior, once the fault has locked, continued relative motion between the plates leads to increasing stress and therefore, stored strain energy in the volume around the fault surface. This continues until the stress has risen sufficiently to break through the asperity, suddenly allowing sliding over the portion of the fault. This energy is released as a combination of radiated elastic strain seismic waves, frictional heating of the fault surface and this process of gradual build-up of strain and stress punctuated by occasional sudden earthquake failure is referred to as the elastic-rebound theory. It is estimated that only 10 percent or less of a total energy is radiated as seismic energy. Most of the energy is used to power the earthquake fracture growth or is converted into heat generated by friction
8.
United Kingdom
–
The United Kingdom of Great Britain and Northern Ireland, commonly known as the United Kingdom or Britain, is a sovereign country in western Europe. Lying off the north-western coast of the European mainland, the United Kingdom includes the island of Great Britain, Northern Ireland is the only part of the United Kingdom that shares a land border with another sovereign state—the Republic of Ireland. The Irish Sea lies between Great Britain and Ireland, with an area of 242,500 square kilometres, the United Kingdom is the 78th-largest sovereign state in the world and the 11th-largest in Europe. It is also the 21st-most populous country, with an estimated 65.1 million inhabitants, together, this makes it the fourth-most densely populated country in the European Union. The United Kingdom is a monarchy with a parliamentary system of governance. The monarch is Queen Elizabeth II, who has reigned since 6 February 1952, other major urban areas in the United Kingdom include the regions of Birmingham, Leeds, Glasgow, Liverpool and Manchester. The United Kingdom consists of four countries—England, Scotland, Wales, the last three have devolved administrations, each with varying powers, based in their capitals, Edinburgh, Cardiff and Belfast, respectively. The relationships among the countries of the UK have changed over time, Wales was annexed by the Kingdom of England under the Laws in Wales Acts 1535 and 1542. A treaty between England and Scotland resulted in 1707 in a unified Kingdom of Great Britain, which merged in 1801 with the Kingdom of Ireland to form the United Kingdom of Great Britain and Ireland. Five-sixths of Ireland seceded from the UK in 1922, leaving the present formulation of the United Kingdom of Great Britain, there are fourteen British Overseas Territories. These are the remnants of the British Empire which, at its height in the 1920s, British influence can be observed in the language, culture and legal systems of many of its former colonies. The United Kingdom is a country and has the worlds fifth-largest economy by nominal GDP. The UK is considered to have an economy and is categorised as very high in the Human Development Index. It was the worlds first industrialised country and the worlds foremost power during the 19th, the UK remains a great power with considerable economic, cultural, military, scientific and political influence internationally. It is a nuclear weapons state and its military expenditure ranks fourth or fifth in the world. The UK has been a permanent member of the United Nations Security Council since its first session in 1946 and it has been a leading member state of the EU and its predecessor, the European Economic Community, since 1973. However, on 23 June 2016, a referendum on the UKs membership of the EU resulted in a decision to leave. The Acts of Union 1800 united the Kingdom of Great Britain, Scotland, Wales and Northern Ireland have devolved self-government
9.
Wivenhoe
–
Wivenhoe is a town and civil parish in north eastern Essex, England, approximately 3 miles south east of Colchester. At the 2001 census, the town had a population of over 7,221, the towns history centres on fishing, ship building, and smuggling. Much of lower Wivenhoe is also a conservation area, with many streets being of particular architectural interest. The place-name Wivenhoe is Saxon in origin, deriving from the personal name Wifas or Wifes spur or promontory, the place-name is now usually pronounced Wivvenho, but the Essex accent would traditionally have rendered it as Wivvenhoo. According to folk etymology, the derived from Wyvernhoe, originating from the mythical beast called a wyvern. The towns football team, Wivenhoe Town FC, is nicknamed The Wyverns, the church of St Mary the Virgin is in the High Street and existed by 1254 when Simon Battle was the patron. The North and South aisles were built in 1340 and 1350, the walls are of rubble, which includes some Roman tile, with ashlar dressings. Elizabeth de Vere, widow of John, 13th earl of Oxford, the tower was plastered in 1563. It became an important port for trade for Colchester and developed shipbuilding, commerce, the period of greatest prosperity for the town came with the arrival of the railway in 1863. In 1884 the town suffered significant damage when it lay close to the epicentre of one of the most destructive UK earthquakes of all time – the 1884 Colchester earthquake. In 1890, there was a population of about 2,000 mostly engaged in fishing for oysters and sprats and in ship and yacht building. A dry dock was built in 1889 and extended in 1904, making it one of the largest on the East Coast, in the 1960s, Wivenhoe Park was chosen as the location for the University of Essex. Wivenhoe Park, bordering on the town of Colchester, is the location for the University of Essex, the site was the home for several centuries of the Rebow family, descendants of Flemish clothweavers from Colchester. Wivenhoe House was designed for Isaac Rebow in 1759 by Thomas Reynolds and it was remodelled in 1846-7 by T. Hopper. A view of the house across the lake was painted by John Constable painting on a visit to Major-General Francis Slater Rebow in 1816 for a fee of 100 guineas. Wivenhoe station is served by a rail service to and from London Liverpool Street via Colchester railway station currently provided by Abellio Greater Anglia. There is a bus connection to Colchester, Wivenhoe is just over one hour from Stansted Airport and 30 minutes from Harwich International Port. Wivenhoe has a population of nine and ten thousand people with a mixture of students from the University of Essex, a long-standing artistic community
10.
Abberton, Essex
–
Abberton is a village in Essex, England. It is located approximately 0.62 mi east of Abberton Reservoir and is 4.2 mi south of Colchester, the village is in the borough of Colchester and in the parliamentary constituency of North Essex. The town is served by Abberton and Langenhoe Parish Council, there is a post office in the village. Abberton is among the villages which suffered damage from the 1884 Colchester earthquake, the Church at Abberton is St Andrew. It is located at the end of Rectory Lane approximately three hundred yards from Abberton Reservoir
11.
Peldon
–
Peldon is a village in the Colchester borough of Essex, England and forms part of the Winstred Hundred civil parish. Other nearby villages include, Little Wigborough and Langenhoe, the parish church is dedicated to St Mary the Virgin and is a grade I listed building. The population of the parish as of the 2011 census is 559, in 1870-72 John Marius Wilsons Imperial Gazetteer of England and Wales described Peldon as, Peldon, a parish and a sub-district in Lexden district, Essex. The parish lies near Mersea Island, 4½ miles S W of Wivenhoe r. station, and 5½ S by W of Colchester, houses,106 The property is much subdivided. During the Iron Age and Roman periods the marshes around Peldon were home to a thriving salt-production industry, Peldon was originally around 2,200 acres of land, equating to approximately 8.9 square kilometres. This land was established by William the Conqueror in 1086 and was passed on to Sir Thomas Darcy by King Henry VIII. The strongest earthquake to strike the UK occurred on the 22nd April 1884. It measured to a 5.1 magnitude on the Richter scale and rendered much of the area around, in total, it damaged around 1250 buildings including churches, houses and cottages. It was reported at the time every single building in Peldon was damaged in some way, including the local church. Peldon was also affected by World War One, on September the 24th 1916, German Zeppelin L33 was damaged during a bombing attack on London, and later crashed near the church in Peldon. The crew of the thought that landing at see would be far too risky. The ship turned around and began to descend into the Essex area, the aircraft landed in a field next to the Peldon church, where the crew managed to escape before the wreckage burst into flames. According to the 2011 Census there was a population of 559, of these 559 residents,282 are residents between the ages of 16 and 74 and are in employment. The main source of employment for the population of Peldon is the repair of vehicles and motor cycles. The age structure of Peldon is primarily made up of people over the age of 45, of the 422 residents of Peldon that are aged between 16 and 74, only three people are unemployed. This means that 419 residents in this age bracket are employed and economically active, the St. Marys Church in Peldon generally dates back to the 11th century, with Anglo Saxon origin. The nave originates from the 12th century, the tower the 14th century, the church also has a tower that leans in a southwesterly direction, originally thought to have been caused by the 1884 earthquake. However, the tower was reportedly already leaning when the earthquake occurred, it was noted in a book, ‘Mehalah
12.
France
–
France, officially the French Republic, is a country with territory in western Europe and several overseas regions and territories. The European, or metropolitan, area of France extends from the Mediterranean Sea to the English Channel and the North Sea, Overseas France include French Guiana on the South American continent and several island territories in the Atlantic, Pacific and Indian oceans. France spans 643,801 square kilometres and had a population of almost 67 million people as of January 2017. It is a unitary republic with the capital in Paris. Other major urban centres include Marseille, Lyon, Lille, Nice, Toulouse, during the Iron Age, what is now metropolitan France was inhabited by the Gauls, a Celtic people. The area was annexed in 51 BC by Rome, which held Gaul until 486, France emerged as a major European power in the Late Middle Ages, with its victory in the Hundred Years War strengthening state-building and political centralisation. During the Renaissance, French culture flourished and a colonial empire was established. The 16th century was dominated by civil wars between Catholics and Protestants. France became Europes dominant cultural, political, and military power under Louis XIV, in the 19th century Napoleon took power and established the First French Empire, whose subsequent Napoleonic Wars shaped the course of continental Europe. Following the collapse of the Empire, France endured a succession of governments culminating with the establishment of the French Third Republic in 1870. Following liberation in 1944, a Fourth Republic was established and later dissolved in the course of the Algerian War, the Fifth Republic, led by Charles de Gaulle, was formed in 1958 and remains to this day. Algeria and nearly all the colonies became independent in the 1960s with minimal controversy and typically retained close economic. France has long been a centre of art, science. It hosts Europes fourth-largest number of cultural UNESCO World Heritage Sites and receives around 83 million foreign tourists annually, France is a developed country with the worlds sixth-largest economy by nominal GDP and ninth-largest by purchasing power parity. In terms of household wealth, it ranks fourth in the world. France performs well in international rankings of education, health care, life expectancy, France remains a great power in the world, being one of the five permanent members of the United Nations Security Council with the power to veto and an official nuclear-weapon state. It is a member state of the European Union and the Eurozone. It is also a member of the Group of 7, North Atlantic Treaty Organization, Organisation for Economic Co-operation and Development, the World Trade Organization, originally applied to the whole Frankish Empire, the name France comes from the Latin Francia, or country of the Franks
13.
Belgium
–
Belgium, officially the Kingdom of Belgium, is a sovereign state in Western Europe bordered by France, the Netherlands, Germany, Luxembourg, and the North Sea. It is a small, densely populated country which covers an area of 30,528 square kilometres and has a population of about 11 million people. Additionally, there is a group of German-speakers who live in the East Cantons located around the High Fens area. Historically, Belgium, the Netherlands and Luxembourg were known as the Low Countries, the region was called Belgica in Latin, after the Roman province of Gallia Belgica. From the end of the Middle Ages until the 17th century, today, Belgium is a federal constitutional monarchy with a parliamentary system of governance. It is divided into three regions and three communities, that exist next to each other and its two largest regions are the Dutch-speaking region of Flanders in the north and the French-speaking southern region of Wallonia. The Brussels-Capital Region is a bilingual enclave within the Flemish Region. A German-speaking Community exists in eastern Wallonia, Belgiums linguistic diversity and related political conflicts are reflected in its political history and complex system of governance, made up of six different governments. Upon its independence, declared in 1830, Belgium participated in the Industrial Revolution and, during the course of the 20th century, possessed a number of colonies in Africa. This continuing antagonism has led to several far-reaching reforms, resulting in a transition from a unitary to a federal arrangement during the period from 1970 to 1993. Belgium is also a member of the Eurozone, NATO, OECD and WTO. Its capital, Brussels, hosts several of the EUs official seats as well as the headquarters of major international organizations such as NATO. Belgium is also a part of the Schengen Area, Belgium is a developed country, with an advanced high-income economy and is categorized as very high in the Human Development Index. A gradual immigration by Germanic Frankish tribes during the 5th century brought the area under the rule of the Merovingian kings, a gradual shift of power during the 8th century led the kingdom of the Franks to evolve into the Carolingian Empire. Many of these fiefdoms were united in the Burgundian Netherlands of the 14th and 15th centuries, the Eighty Years War divided the Low Countries into the northern United Provinces and the Southern Netherlands. The latter were ruled successively by the Spanish and the Austrian Habsburgs and this was the theatre of most Franco-Spanish and Franco-Austrian wars during the 17th and 18th centuries. The reunification of the Low Countries as the United Kingdom of the Netherlands occurred at the dissolution of the First French Empire in 1815, although the franchise was initially restricted, universal suffrage for men was introduced after the general strike of 1893 and for women in 1949. The main political parties of the 19th century were the Catholic Party, French was originally the single official language adopted by the nobility and the bourgeoisie
14.
Ipswich
–
Ipswich is the county town of Suffolk, England, located on the estuary of the River Orwell, about 60 miles north east of London. The town has been occupied since the Saxon period. It has also known as Gyppewicus and Yppswyche. Ipswich is one of Englands oldest towns, if not the oldest, the claim has also been made of the Essex town of Colchester, but that town was abandoned for some time, leaving Ipswich to claim to be the oldest continuously inhabited town in England. Under the Roman empire, the area around Ipswich formed an important route inland to towns and settlements via the rivers Orwell. A large Roman fort, part of the defences of Britain, stood at Walton near Felixstowe. The modern town took shape in Anglo-Saxon times around Ipswich dock, gipeswic ) arose as the equivalent to these, serving the Kingdom of East Anglia, its early imported wares dating to the time of King Rædwald, supreme ruler of the English. The famous ship-burial and treasure at Sutton Hoo nearby is probably his grave, the Ipswich Museum houses replicas of the Roman Mildenhall and Sutton Hoo treasures. A gallery devoted to the towns origins includes Anglo-Saxon weapons, jewellery, the 7th-century town was centred near the quay. Towards 700 AD, Frisian potters from the Netherlands area settled in Ipswich and their wares were traded far across England, and the industry was unique to Ipswich for 200 years. With growing prosperity, in about 720 AD a large new part of the town was out in the Buttermarket area. Ipswich was becoming a place of national and international importance, parts of the ancient road plan still survive in its modern streets. After the invasion of 869 Ipswich fell under Viking rule, the earth ramparts circling the town centre were probably raised by Vikings in Ipswich around 900 to prevent its recapture by the English. The town operated a mint under royal licence from King Edgar in the 970s, the abbreviation Gipes appears on the coins. King John granted the town its first charter in 1200, laying the foundations of its modern civil government. In the next four centuries it made the most of its wealth, Five large religious houses, including two Augustinian Priories, and those of the Greyfriars, Ipswich Whitefriars and Ipswich Blackfriars, stood in medieval Ipswich. The last Carmelite Prior of Ipswich was the celebrated John Bale, there were also several hospitals, including the leper hospital of St Mary Magdalene, founded before 1199. During the Middle Ages the Marian Shrine of Our Lady of Grace was a pilgrimage destination
15.
Layer de la Haye
–
Layer de la Haye is a small village of around 2,000 people, measured at 1,767 in the 2011 Census, near Colchester in Essex, England. The village is thought to have founded in Saxon times, with its original name, Legra. Its elevation made it a vantage point for the Saxons against raiding parties from the coast. Later its name changed to Leire or Leger, meaning mud, a Norse word, this is likely to have referred to the soil and marshland around the village. During the time of the Norman Conquests, the village was owned by the de la Hayes, Layer was ravaged by the Black Plague of the 14th Century. The Church became derelict until it was restored by monks, in 1289, John de Rye donated 160 acres of land to St Johns Abbey in Colchester. As a token of appreciation, a manor and farm were named after him, at the end of the 15th century, the Abbey built a toll-gate house, now called the Greate House near Malting Green. Layer Mill is mentioned in the Domesday Book as a water-mill, the mill wheel was powered by water from the Roman River. Layer de la Haye is among the villages which suffered damage from the 1884 Colchester earthquake, in 1950 its population was under 700, by 1975 it was over 1,000 and in 1990 it was just short of 2,000. However, the proximity of Colchester, with its range of shops and facilities. The Layer Village Store was reopened by new owners in 2015, despite concerns over vandalism and ASB the village is generally regarded as a safe and happy place to be. Societies and clubs such as The Shoestring Theatre Company provide entertainment for the village community. The Layer Parish Council has created a website for the village, the website contains information about all the services, attractions and facilities in the village. Village Website 1, Layer de la Haye Village Appraisal,2003 Media related to Layer de la Haye at Wikimedia Commons
16.
The Guardian
–
The Guardian is a British daily newspaper, known from 1821 until 1959 as the Manchester Guardian. Along with its sister papers The Observer and The Guardian Weekly, The Guardian is part of the Guardian Media Group, the Scott Trust became a limited company in 2008, with a constitution to maintain the same protections for The Guardian. Profits are reinvested in journalism rather than to the benefit of an owner or shareholders, the Guardian is edited by Katharine Viner, who succeeded Alan Rusbridger in 2015. In 2016, The Guardians print edition had a daily circulation of roughly 162,000 copies in the country, behind The Daily Telegraph. The newspaper has an online UK edition as well as two international websites, Guardian Australia and Guardian US, the newspapers online edition was the fifth most widely read in the world in October 2014, with over 42.6 million readers. Its combined print and online editions reach nearly 9 million British readers, notable scoops include the 2011 News International phone hacking scandal, in particular the hacking of murdered English teenager Milly Dowlers phone. The investigation led to the closure of the UKs biggest selling Sunday newspaper, and one of the highest circulation newspapers in the world, in 2016, it led the investigation into the Panama Papers, exposing the then British Prime Minister David Camerons links to offshore bank accounts. The Guardian has been named Newspaper of the Year four times at the annual British Press Awards, the paper is still occasionally referred to by its nickname of The Grauniad, given originally for the purported frequency of its typographical errors. The Manchester Guardian was founded in Manchester in 1821 by cotton merchant John Edward Taylor with backing from the Little Circle and they launched their paper after the police closure of the more radical Manchester Observer, a paper that had championed the cause of the Peterloo Massacre protesters. They do not toil, neither do they spin, but they better than those that do. When the government closed down the Manchester Observer, the champions had the upper hand. The influential journalist Jeremiah Garnett joined Taylor during the establishment of the paper, the prospectus announcing the new publication proclaimed that it would zealously enforce the principles of civil and religious Liberty. Warmly advocate the cause of Reform, endeavour to assist in the diffusion of just principles of Political Economy and. Support, without reference to the party from which they emanate, in 1825 the paper merged with the British Volunteer and was known as The Manchester Guardian and British Volunteer until 1828. The working-class Manchester and Salford Advertiser called the Manchester Guardian the foul prostitute, the Manchester Guardian was generally hostile to labours claims. The Manchester Guardian dismissed strikes as the work of outside agitators –, if an accommodation can be effected, the occupation of the agents of the Union is gone. CP Scott made the newspaper nationally recognised and he was editor for 57 years from 1872, and became its owner when he bought the paper from the estate of Taylors son in 1907. Under Scott, the moderate editorial line became more radical, supporting William Gladstone when the Liberals split in 1886
17.
The Times
–
The Times is a British daily national newspaper based in London, England. It began in 1785 under the title The Daily Universal Register, the Times and its sister paper The Sunday Times are published by Times Newspapers, since 1981 a subsidiary of News UK, itself wholly owned by News Corp. The Times and The Sunday Times do not share editorial staff, were founded independently and have only had common ownership since 1967 and its news and its editorial comment have in general been carefully coordinated, and have at most times been handled with an earnest sense of responsibility. While the paper has admitted some trivia to its columns, its emphasis has been on important public affairs treated with an eye to the best interests of Britain. To guide this treatment, the editors have for long periods been in touch with 10 Downing Street. In these countries, the newspaper is often referred to as The London Times or The Times of London, although the newspaper is of national scope, in November 2006 The Times began printing headlines in a new font, Times Modern. The Times was printed in broadsheet format for 219 years, the Sunday Times remains a broadsheet. The Times had a daily circulation of 446,164 in December 2016, in the same period. An American edition of The Times has been published since 6 June 2006 and it has been heavily used by scholars and researchers because of its widespread availability in libraries and its detailed index. A complete historical file of the paper, up to 2010, is online from Gale Cengage Learning. The Times was founded by publisher John Walter on 1 January 1785 as The Daily Universal Register, Walter had lost his job by the end of 1784 after the insurance company where he was working went bankrupt because of the complaints of a Jamaican hurricane. Being unemployed, Walter decided to set a new business up and it was in that time when Henry Johnson invented the logography, a new typography that was faster and more precise. Walter bought the patent and to use it, he decided to open a printing house. The first publication of the newspaper The Daily Universal Register in Great Britain was 1 January 1785, unhappy because people always omitted the word Universal, Ellias changed the title after 940 editions on 1 January 1788 to The Times. In 1803, Walter handed ownership and editorship to his son of the same name, the Times used contributions from significant figures in the fields of politics, science, literature, and the arts to build its reputation. For much of its life, the profits of The Times were very large. Beginning in 1814, the paper was printed on the new steam-driven cylinder press developed by Friedrich Koenig, in 1815, The Times had a circulation of 5,000. Thomas Barnes was appointed editor in 1817
18.
Rowhedge
–
Rowhedge is a village in the Colchester borough of Essex, England. It is located just over 3 miles southeast of Colchester town centre, Rowhedge is on the right bank of the tidal River Colne and is the first settlement downstream from Colchester. The small town of Wivenhoe is on the bank, but slightly farther downstream, Fingringhoe is just to the south. Throughout the 20th century, Rowhedge and Wivenhoe were linked by a ferry, a barrier, similar to the one on the River Thames which shields London, was completed on the Colne in 1994. Rowhedge, Wivenhoe and Colchester all benefit from its protection from flooding, the main thoroughfare in Rowhedge, the High Street, runs parallel to the Colne. At one time, it connected two areas of ship and boat construction and maintenance – the Upper Yard to the north, and these were often known as Up Street and Down Street respectively. With the decline of building, housing estates have been built in both areas. The history of Rowhedge is connected directly to the River Colne, ship or boat building, the Essex earthquake of 22 April 1884, damaged several buildings in the village, even shaking a man off his ladder while he was repairing the villages school clock. Colchester Rowing Club was established in the village in 1896 when the population was about 1,100, Rowhedge could boast of its own brewery. In response to a £1,000 prize being offered by the Daily Mail newspaper for the first Briton to fly a mile, an areohydroplane, was designed and constructed by Jack Humphrey of Halstead in 1909. Several unsuccessful attempts at flight were made, both from the sea and land, after which the contraption was broken up, its floats ending their days in Rowhedge Ironworks in the Upper Yard, fishing for sprats could be a relatively worthless business. One of the pre-First World War village characters was John Spitty – salvager, pub licensee, fisherman and his use of a bedroom in the Royal Oak public house when he was the licensee to hide boxes of Dutch cigars was brought to a halt by his wife. She put her foot down after the pub was unsuccessfully searched by customs men and he would also sometimes swap sprats for coal at sea after a rumbustious verbal exchange with an obliging colliers skipper, the fuel was used in his smacks shrimp boiler. During the First World War, a bridge was built across the river to enable members of the nearby Colchester garrison to board trains at Wivenhoe when on their way to Gallipoli and it was inspected by King George V in April 1916, but dismantled after the war. Lifeboats and small oil tankers were constructed and maintained at the two yards, contributing towards the economy in the 1920s and 30s. Many boats were fabricated in the Upper Yard for contracts in the Sudan and this took kit form, the various parts would be dismantled, crated or wired together, sent out to the African country and reassembled for use on the Nile. The extraction of sand and gravel near the village began in the 1930s, demand for such building materials increased after the Second World War to repair bomb-damaged buildings, particularly in London. During that conflict, various types of construction, apart from ships, including then secret Mulberry Harbour components for the D-Day landings, were also built, both in Rowhedge and Wivenhoe
19.
Palaeozoic
–
The Paleozoic Era is the earliest of three geologic eras of the Phanerozoic Eon, from 541 to 252.17 million years ago. It is the longest of the Phanerozoic eras, and is subdivided into six periods, the Cambrian, Ordovician, Silurian, Devonian, Carboniferous. The Paleozoic comes after the Neoproterozoic era of the Proterozoic and is followed by the Mesozoic, the Paleozoic was a time of dramatic geological, climatic, and evolutionary change. The Cambrian witnessed the most rapid and widespread diversification of life in Earths history, known as the Cambrian explosion, fish, arthropods, amphibians, anapsids, synapsids, euryapsids and diapsids all evolved during the Paleozoic. Life began in the ocean but eventually transitioned onto land, and by the late Paleozoic, Great forests of primitive plants covered the continents, many of which formed the coal beds of Europe and eastern North America. Towards the end of the era, large, sophisticated diapsids and synapsids were dominant, the Paleozoic Era ended with the largest extinction event in the history of Earth, the Permian–Triassic extinction event. The effects of this catastrophe were so devastating that it took life on land 30 million years into the Mesozoic Era to recover, recovery of life in the sea may have been much faster. The Paleozoic era began and ended with supercontinents and in between were the rise of mountains along the margins, and flooding and draining of shallow seas between. At its start, the supercontinent Pannotia broke up, paleoclimatic studies and evidence of glaciers indicate that central Africa was most likely in the polar regions during the early Paleozoic. During the early Paleozoic, the huge continent Gondwana formed or was forming, by mid-Paleozoic, the collision of North America and Europe produced the Acadian-Caledonian uplifts, and a subduction plate uplifted eastern Australia. There are six periods in the Paleozoic Era, Cambrian, Ordovician, Silurian, Devonian, Carboniferous, the Cambrian spans from 541 million years to 485 million years and is the first period of the Paleozoic era of the Phanerozoic. The Cambrian marked a boom in evolution in an event known as the Cambrian explosion in which the largest number of creatures evolved in any period of the history of the Earth. Creatures like algae evolved, but the most ubiquitous of that period were the armored arthropods, almost all marine phyla evolved in this period. During this time, the supercontinent Pannotia begins to break up, the Ordovician spanned from 485 million years to 443 million years ago. The Ordovician is a time in Earths history in many of the biological classes still prevalent today evolved, such as primitive fish, cephalopods. The most common forms of life, however, were trilobites, snails, more importantly, the first arthropods went ashore to colonize the empty continent of Gondwana. By the end of the Ordovican, Gondwana was at the pole, early North America had collided with Europe. Glaciation of Africa resulted in a drop in sea level
20.
Cretaceous
–
The Cretaceous is a geologic period and system that spans 79 million years from the end of the Jurassic Period 145 million years ago to the beginning of the Paleogene Period 66 Mya. It is the last period of the Mesozoic Era, the Cretaceous Period is usually abbreviated K, for its German translation Kreide. The Cretaceous was a period with a warm climate, resulting in high eustatic sea levels that created numerous shallow inland seas. These oceans and seas were populated with now-extinct marine reptiles, ammonites and rudists, during this time, new groups of mammals and birds, as well as flowering plants, appeared. The Cretaceous ended with a mass extinction, the Cretaceous–Paleogene extinction event, in which many groups, including non-avian dinosaurs, pterosaurs. The end of the Cretaceous is defined by the abrupt Cretaceous–Paleogene boundary, the name Cretaceous was derived from Latin creta, meaning chalk. The Cretaceous is divided into Early and Late Cretaceous epochs, or Lower and Upper Cretaceous series, in older literature the Cretaceous is sometimes divided into three series, Neocomian, Gallic and Senonian. A subdivision in eleven stages, all originating from European stratigraphy, is now used worldwide, in many parts of the world, alternative local subdivisions are still in use. As with other geologic periods, the rock beds of the Cretaceous are well identified. No great extinction or burst of diversity separates the Cretaceous from the Jurassic and this layer has been dated at 66.043 Ma. A140 Ma age for the Jurassic-Cretaceous boundary instead of the usually accepted 145 Ma was proposed in 2014 based on a study of Vaca Muerta Formation in Neuquén Basin. Víctor Ramos, one of the authors of the study proposing the 140 Ma boundary age sees the study as a first step toward formally changing the age in the International Union of Geological Sciences, due to the high sea level there was extensive space for such sedimentation. Because of the young age and great thickness of the system. Chalk is a type characteristic for the Cretaceous. It consists of coccoliths, microscopically small calcite skeletons of coccolithophores, the group is found in England, northern France, the low countries, northern Germany, Denmark and in the subsurface of the southern part of the North Sea. Chalk is not easily consolidated and the Chalk Group still consists of sediments in many places. The group also has other limestones and arenites, among the fossils it contains are sea urchins, belemnites, ammonites and sea reptiles such as Mosasaurus. In southern Europe, the Cretaceous is usually a marine system consisting of competent limestone beds or incompetent marls
21.
British Geological Survey
–
The BGS headquarters are in Keyworth, Nottinghamshire, England, United Kingdom. Its other centres are located in Edinburgh, Wallingford, Cardiff, the current motto of the BGS is, Gateway to the Earth. The Geological Survey was founded in 1835 as the Ordnance Geological Survey and this was the worlds first national geological survey. It remained a branch of the Ordnance Survey for many years, in 1965, it was merged with the Geological Museum and Overseas Geological Surveys, under the name of Institute of Geological Sciences. On 1 January 1984, the institute was renamed the British Geological Survey, the BGS advises the British government on all aspects of geoscience, as well as providing impartial advice on geological matters to the public, academics and industry. The core outputs of the BGS include geological, geophysical, geochemical and hydrogeological maps, descriptions, scientists at the BGS produced the first comprehensive map of African groundwater reserves. One of the key strategic aims for the decade is to complete the transition from 2-D mapping to a 3-D modelling culture. The BGS has a budget of £57M, about half of which comes from the Governments science budget, with the remainder coming from commissioned research from the public
22.
International Standard Book Number
–
The International Standard Book Number is a unique numeric commercial book identifier. An ISBN is assigned to each edition and variation of a book, for example, an e-book, a paperback and a hardcover edition of the same book would each have a different ISBN. The ISBN is 13 digits long if assigned on or after 1 January 2007, the method of assigning an ISBN is nation-based and varies from country to country, often depending on how large the publishing industry is within a country. The initial ISBN configuration of recognition was generated in 1967 based upon the 9-digit Standard Book Numbering created in 1966, the 10-digit ISBN format was developed by the International Organization for Standardization and was published in 1970 as international standard ISO2108. Occasionally, a book may appear without a printed ISBN if it is printed privately or the author does not follow the usual ISBN procedure, however, this can be rectified later. Another identifier, the International Standard Serial Number, identifies periodical publications such as magazines, the ISBN configuration of recognition was generated in 1967 in the United Kingdom by David Whitaker and in 1968 in the US by Emery Koltay. The 10-digit ISBN format was developed by the International Organization for Standardization and was published in 1970 as international standard ISO2108, the United Kingdom continued to use the 9-digit SBN code until 1974. The ISO on-line facility only refers back to 1978, an SBN may be converted to an ISBN by prefixing the digit 0. For example, the edition of Mr. J. G. Reeder Returns, published by Hodder in 1965, has SBN340013818 -340 indicating the publisher,01381 their serial number. This can be converted to ISBN 0-340-01381-8, the check digit does not need to be re-calculated, since 1 January 2007, ISBNs have contained 13 digits, a format that is compatible with Bookland European Article Number EAN-13s. An ISBN is assigned to each edition and variation of a book, for example, an ebook, a paperback, and a hardcover edition of the same book would each have a different ISBN. The ISBN is 13 digits long if assigned on or after 1 January 2007, a 13-digit ISBN can be separated into its parts, and when this is done it is customary to separate the parts with hyphens or spaces. Separating the parts of a 10-digit ISBN is also done with either hyphens or spaces, figuring out how to correctly separate a given ISBN number is complicated, because most of the parts do not use a fixed number of digits. ISBN issuance is country-specific, in that ISBNs are issued by the ISBN registration agency that is responsible for country or territory regardless of the publication language. Some ISBN registration agencies are based in national libraries or within ministries of culture, in other cases, the ISBN registration service is provided by organisations such as bibliographic data providers that are not government funded. In Canada, ISBNs are issued at no cost with the purpose of encouraging Canadian culture. In the United Kingdom, United States, and some countries, where the service is provided by non-government-funded organisations. Australia, ISBNs are issued by the library services agency Thorpe-Bowker
23.
Raphael Meldola
–
Raphael Meldola FRS was a British chemist and entomologist. He was Professor of Organic Chemistry in the University of London, born in Islington, London, he was descended from Raphael Meldola, a theologian who was acting minister of the Spanish and Portuguese Jews in London,1804. Meldola was the son of Samuel Meldola, married Ella Frederica. He was educated in chemistry at the Royal College of Chemistry, there is a portrait of Meldola by Solomon J. Solomon in the Royal Society collection, also a photograph by Maull & Fox, visiting card size. Meldola worked in the laboratory of John Stenhouse. He was appointed Lecturer, Royal College of Science and assisted Norman Lockyer with spectroscopy, Meldola was in charge of the British Eclipse Expedition to the Nicobar Islands and was Professor of Chemistry, Technical College, Finsbury. He was also an entomologist and natural historian and he was elected Fellow of the Royal Society in 1886, awarded the Davy Medal in 1913, and was Vice-President of the Council from 1914–1915. He was the first president of the Maccabaeans, 1891–1915, in his honour the Royal Society of Chemistry award the Meldola medal each year. He discovered the synthetic dye Meldolas Blue, Works by Raphael Meldola at Project Gutenberg Works by or about Raphael Meldola at Internet Archive
