1.
Old English
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Old English or Anglo-Saxon is the earliest historical form of the English language, spoken in England and southern and eastern Scotland in the early Middle Ages. It was brought to Great Britain by Anglo-Saxon settlers probably in the mid 5th century, Old English developed from a set of Anglo-Frisian or North Sea Germanic dialects originally spoken by Germanic tribes traditionally known as the Angles, Saxons, and Jutes. As the Anglo-Saxons became dominant in England, their language replaced the languages of Roman Britain, Common Brittonic, a Celtic language, Old English had four main dialects, associated with particular Anglo-Saxon kingdoms, Mercian, Northumbrian, Kentish and West Saxon. It was West Saxon that formed the basis for the standard of the later Old English period, although the dominant forms of Middle. The speech of eastern and northern parts of England was subject to strong Old Norse influence due to Scandinavian rule, Old English is one of the West Germanic languages, and its closest relatives are Old Frisian and Old Saxon. Like other old Germanic languages, it is different from Modern English. Old English grammar is similar to that of modern German, nouns, adjectives, pronouns, and verbs have many inflectional endings and forms. The oldest Old English inscriptions were using a runic system. Old English was not static, and its usage covered a period of 700 years, from the Anglo-Saxon settlement of Britain in the 5th century to the late 11th century, some time after the Norman invasion. While indicating that the establishment of dates is a process, Albert Baugh dates Old English from 450 to 1150, a period of full inflections. Perhaps around 85 per cent of Old English words are no longer in use, Old English is a West Germanic language, developing out of Ingvaeonic dialects from the 5th century. It came to be spoken over most of the territory of the Anglo-Saxon kingdoms which became the Kingdom of England and this included most of present-day England, as well as part of what is now southeastern Scotland, which for several centuries belonged to the Anglo-Saxon kingdom of Northumbria. Other parts of the island – Wales and most of Scotland – continued to use Celtic languages, Norse was also widely spoken in the parts of England which fell under Danish law. Anglo-Saxon literacy developed after Christianisation in the late 7th century, the oldest surviving text of Old English literature is Cædmons Hymn, composed between 658 and 680. There is a corpus of runic inscriptions from the 5th to 7th centuries. The Old English Latin alphabet was introduced around the 9th century, with the unification of the Anglo-Saxon kingdoms by Alfred the Great in the later 9th century, the language of government and literature became standardised around the West Saxon dialect. In Old English, typical of the development of literature, poetry arose before prose, a later literary standard, dating from the later 10th century, arose under the influence of Bishop Æthelwold of Winchester, and was followed by such writers as the prolific Ælfric of Eynsham. This form of the language is known as the Winchester standard and it is considered to represent the classical form of Old English
2.
Anna of East Anglia
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Anna was king of East Anglia from the early 640s until his death. He was a member of the Wuffingas family, the dynasty of the East Angles. He was one of the three sons of Eni who ruled the kingdom of East Anglia, succeeding some time after Ecgric was killed in battle by Penda of Mercia, little is known of Annas life or his reign, as few records have survived from this period. In 631 he may have been at Exning, close to the Devils Dyke, in 645 Cenwalh of Wessex was driven from his kingdom by Penda and, due to Annas influence, he was converted to Christianity while living as an exile at the East Anglian court. Upon his return from exile, Cenwalh re-established Christianity in his own kingdom, around 651 the land around Ely was absorbed into East Anglia, following the marriage of Annas daughter Æthelthryth. Anna richly endowed the monastery at Cnobheresburg, in 651, in the aftermath of an attack by Penda on Cnobheresburg, Anna was forced to flee into exile, perhaps to the western kingdom of the Magonsæte. Anna was succeeded by his brother, Æthelhere, botolphs monastery at Iken may have been built in commemoration of the king. After Annas reign, East Anglia seems to have been eclipsed by its powerful neighbour. The kingdom of East Anglia was a small independent Anglo-Saxon kingdom that comprised what are now the English counties of Norfolk and Suffolk and perhaps the eastern part of the Cambridgeshire Fens. Anna was the son of Eni, a member of the ruling Wuffingas family, East Anglia was an early and long-lived Anglo-Saxon kingdom in which a duality of a northern and a southern part existed, corresponding with the modern English counties of Norfolk and Suffolk. Anna was married, Bede refers to the saint Sæthryth as daughter of the wife of Anna, king of the East Angles. In Abbott Folcards Life of St Botolph, written in the 11th century, Botolph is described as having been at one time the chaplain to the sisters of a king, Æthelmund, folcard names two of Sæwaras kinsmen as Æthelhere and Æthelwold. The Liber Eliensis names Hereswith, the sister of Hild, abbess of Whitby, as Annas wife, historians now believe that Hereswith was Annas sister-in-law and that around the time that she married into the East Anglian royal family, Anna had already been king for a decade. In 631 Anna was probably at the Suffolk village of Exning, an important settlement with royal connections, and, according to the Liber Eliensis, by tradition, Æthelthryth is said to have been baptised at Exning in a pool known as St Mindreds Well. An early Anglo-Saxon cemetery discovered there suggests the existence of an important site nearby, during 632 or 633 Edwin of Northumbria, with his centre of Christian power north of the River Humber, was overthrown. Edwin was slain and Northumbria was ravaged by Cadwallon ap Cadfan, supported by the Mercian king, the Mercians then turned on the kingdom of the East Angles and their king, Ecgric. At an unknown date, they routed the East Anglian army and Ecgric, D. P. Kirby has suggested that as Sigeberht was alive when the Irish monk Fursey left for Gaul and found Erchinoald, Sigeberht was probably killed around 640 or 641. Pendas victory marked the end of the line of kings of the East Angles who were descended from Rædwald
3.
Picts
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The Picts were a tribal confederation of peoples who lived in what is today eastern and northern Scotland during the Late Iron Age and Early Medieval periods. They are thought to have been ethnolinguistically Celtic, where they lived and what their culture was like can be inferred from the geographical distribution of brochs, Brittonic place name elements, and Pictish stones. Picts are attested to in records from before the Roman conquest of Britain to the 10th century. Picts are assumed to have been the descendants of the Caledonii, Pictland, also called Pictavia by some sources, gradually merged with the Gaelic kingdom of Dál Riata to form the Kingdom of Alba. Alba then expanded, absorbing the Brittonic kingdom of Strathclyde and Northumbrian Lothian, Pictish society was typical of many Iron Age societies in northern Europe, having wide connections and parallels with neighbouring groups. Archaeology gives some impression of the society of the Picts, what the Picts called themselves is unknown. The Latin word Picti first occurs in a written by Eumenius in AD297 and is taken to mean painted or tattooed people. Their Old English name gave the modern Scots form Pechts and the Welsh word Fichti and it is generally accepted that this is derived from *Qritani, which is the Goidelic/Q-Celtic version of the Britonnic/P-Celtic *Pritani. From this came Britanni, the Roman name for those now called the Britons and it has been suggested that Cruthin referred to all Britons not conquered by the Romans—those who lived outside Roman Britannia, north of Hadrians Wall. A Pictish confederation was formed in Late Antiquity from a number of tribes—how, some scholars have speculated that it was partly in response to the growth of the Roman Empire. Pictland had previously described by Roman writers and geographers as the home of the Caledonii. These Romans also used names to refer to tribes living in that area, including Verturiones, Taexali. But they may have heard these other names only second- or third-hand, from speakers of Brittonic or Gaulish languages, Pictish recorded history begins in the Dark Ages. It appears that Picts were not the dominant power in Northern Britain for that entire period, the Gaels of Dál Riata controlled what is present day Argyll for a time, although they suffered a series of defeats in the first third of the 7th century. The Angles of Bernicia overwhelmed the adjacent British kingdoms, one of which, the Picts were probably tributary to Northumbria until the reign of Bridei mac Beli, when, in 685, the Anglians suffered a defeat at the Battle of Dun Nechtain that halted their northward expansion. The Northumbrians continued to dominate southern Scotland for the remainder of the Pictish period, a later Pictish king, Caustantín mac Fergusa, placed his son Domnall on the throne of Dál Riata. Pictish attempts to achieve a dominance over the Britons of Alt Clut were not successful. The Viking Age brought great changes in Britain and Ireland, no less in Scotland than elsewhere, in a major battle in 839, the Vikings killed the king of Fortriu, Eógan mac Óengusa, the king of Dál Riata Áed mac Boanta, and many others
4.
Firth of Forth
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The Firth of Forth is the estuary of the River Forth in Scotland, where it flows into the North Sea, between Fife to the north and Lothian to the south. It was known as Bodotria in Roman times, in the Norse sagas it was known as the Myrkvifiörd. Geologically, the Firth of Forth is a fjord, formed by the Forth Glacier in the last glacial period, the Kincardine Bridge, the Clackmannanshire Bridge, the Forth Road Bridge and the Forth Bridge carry traffic across the firth. Queensferry Crossing, alongside the Forth Road Bridge, was expected to open in 2016 but has since been delayed until May 2017. From 1964 to 1982, a tunnel existed under the Firth of Forth, the shafts leading into the tunnel were filled and capped with concrete when the tunnel was closed, and it is believed to have filled with water or collapsed in places. In July,2007, a passenger service completed a two-week trial between Portobello, Edinburgh and Kirkcaldy, Fife. The trial of the service was hailed as an operational success. It was estimated the service would decrease congestion for commuters on the Forth road, despite the initial success, the project was cancelled in December,2011. Historic villages line the Fife shoreline, Limekilns, Charlestown and Culross, established in the 6th century, the firth is important for nature conservation and is a Site of Special Scientific Interest. The Firth of Forth Islands SPA is home to more than 90,000 breeding seabirds every year, there is a bird observatory on the Isle of May. The youngest person to swim across the Firth of Forth was 13-year-old Joseph Feeney, in 2008, a controversial bid to allow oil transfer between ships in the firth was refused by Forth Ports. SPT Marine Services had asked permission to transfer 7.8 million tonnes of oil per year between tankers, but the proposals were met with determined opposition from conservation groups
5.
River Tweed
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The River Tweed, or Tweed Water, is a river 97 miles long that flows east across the Border region in Scotland and northern England. Tweed derives its name from its association with the River Tweed, the Tweed is one of the great salmon rivers of Britain and the only river in England where an Environment Agency rod licence is not required for angling. Tweed is a British name of uncertain meaning and it flows primarily through the scenic Borders region of Scotland, and eastwards from the settlements on opposing banks of Birgham and Carham forms the historic boundary between Scotland and England. It rises in the Lowther Hills at Tweeds Well near where the Clyde, draining northwest, Annan, Tweed and Clyde rise oot the ae hillside is a saying from the Border region. East of Kelso, it becomes a section of the part of the border. Entering England, its reaches are in Northumberland, where it enters the North Sea at Berwick-upon-Tweed. The rivers valley floor is a field and the relic of a paleo-ice stream that flowed through the area during the last glaciation. Major towns through which the Tweed flows include Innerleithen, Peebles, Galashiels, Melrose, Kelso, Coldstream and Berwick-upon-Tweed, where it flows into the North Sea
6.
Coldingham
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Coldingham is a village and parish in Berwickshire, Scottish Borders, on Scotlands southeast coastline, north of Eyemouth. The parish lies in the east of the Lammermuir district and is the second largest civil parish by area in the county of Berwickshire and it was included in the former Berwickshire District of Borders Region, by the Local Government Act 1973, from 1975 to 1996. Before the Reformation a vaguely defined jurisdiction known as Coldinghamshire was linked to Coldingham Priory, by 15th century there is some indication that the civil administration was gradually attaining paramount sway with the consent of the Church itself. The barony of Coldingham, which included Eyemouth and other adjacent to the parish of Coldingham continued as a jurisdiction into the 17th and 18th centuries. Because of the size of the parish, a chapel was set-up for the interior or western part of the parish in 1794. Houndwood was made a parish for the western part of Coldingham in 1851. This parish is now linked to Ayton and is served by places of worship at Reston, the church itself became a crematorium in 2015 A Parochial Board was established under the Poor Law Act 1845. Civil parishes in Scotland, as units of government, were abolished in 1929 but have been used later for census. In 1891 a Boundary Commission transferred a portion of Oldhamstocks parish, namely Butterdean. It was already in Berwickshire, despite its mother parish being in East Lothian, the civil parish has an area of 25,379 acres and a population of 1,919. The settlement of Coldingham has a population of 563, bede describes it as the Monastery of Virgins and states that in 679 the monastery burnt down. It was rebuilt, but was destroyed by fire at the hands of a raiding party of Danes in 870. This time the ruins were not rebuilt, it would appear, until 1098 and it became the caput for the Barony of Coldingham, with the prior as the feudal lord. The priory continued in its religious purposes until 1560, when it was destroyed during the Scottish Reformation. However, a portion of it continued its religious activities until 1650, after a siege of two days, the main tower in which the besieged defended themselves was so shattered by artillery that they were forced to capitulate. This great tower of the original priory finally collapsed about 1777, the ruins of about 40% of the original priory church were rebuilt in 1855, it is today used as the parish church, and is the most notable building in the parish. Nearby Coldingham Bay has a secluded beach popular with surfers. RCAHMS entry for Coldingham Scran, The Bogan, Coldingham Scran, Coldingham Shore 1868 Ordnance Gazetteer of Scotland, 1882-1885 coldingham. info Coldingham Priory
7.
Ireland
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Ireland is an island in the North Atlantic. It is separated from Great Britain to its east by the North Channel, the Irish Sea, Ireland is the second-largest island of the British Isles, the third-largest in Europe, and the twentieth-largest on Earth. Politically, Ireland is divided between the Republic of Ireland, which covers five-sixths of the island, and Northern Ireland, in 2011, the population of Ireland was about 6.4 million, ranking it the second-most populous island in Europe after Great Britain. Just under 4.6 million live in the Republic of Ireland, the islands geography comprises relatively low-lying mountains surrounding a central plain, with several navigable rivers extending inland. The island has lush vegetation, a product of its mild, thick woodlands covered the island until the Middle Ages. As of 2013, the amount of land that is wooded in Ireland is about 11% of the total, there are twenty-six extant mammal species native to Ireland. The Irish climate is moderate and classified as oceanic. As a result, winters are milder than expected for such a northerly area, however, summers are cooler than those in Continental Europe. Rainfall and cloud cover are abundant, the earliest evidence of human presence in Ireland is dated at 10,500 BC. Gaelic Ireland had emerged by the 1st century CE, the island was Christianised from the 5th century onward. Following the Norman invasion in the 12th century, England claimed sovereignty over Ireland, however, English rule did not extend over the whole island until the 16th–17th century Tudor conquest, which led to colonisation by settlers from Britain. In the 1690s, a system of Protestant English rule was designed to materially disadvantage the Catholic majority and Protestant dissenters, with the Acts of Union in 1801, Ireland became a part of the United Kingdom. Northern Ireland saw much civil unrest from the late 1960s until the 1990s and this subsided following a political agreement in 1998. In 1973 the Republic of Ireland joined the European Economic Community while the United Kingdom, Irish culture has had a significant influence on other cultures, especially in the fields of literature. Alongside mainstream Western culture, an indigenous culture exists, as expressed through Gaelic games, Irish music. The culture of the island shares many features with that of Great Britain, including the English language, and sports such as association football, rugby, horse racing. The name Ireland derives from Old Irish Eriu and this in turn derives from Proto-Celtic *Iveriu, which is also the source of Latin Hibernia. Iveriu derives from a root meaning fat, prosperous, during the last glacial period, and up until about 9000 years ago, most of Ireland was covered with ice, most of the time
8.
Bede
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He is well known as an author and scholar, and his most famous work, Ecclesiastical History of the English People gained him the title The Father of English History. Bedes monastery had access to a library which included works by Eusebius, Orosius. Almost everything that is known of Bedes life is contained in the last chapter of his Ecclesiastical History of the English People, a history of the church in England. It was completed in about 731, and Bede implies that he was then in his fifty-ninth year, a minor source of information is the letter by his disciple Cuthbert which relates Bedes death. Bede, in the Historia, gives his birthplace as on the lands of this monastery, Bede says nothing of his origins, but his connections with men of noble ancestry suggest that his own family was well-to-do. Bedes first abbot was Benedict Biscop, and the names Biscop, Bedes name reflects West Saxon Bīeda. It is an Anglo-Saxon short name formed on the root of bēodan to bid, the name also occurs in the Anglo-Saxon Chronicle, s. a. 501, as Bieda, one of the sons of the Saxon founder of Portsmouth, the Liber Vitae of Durham Cathedral names two priests with this name, one of whom is presumably Bede himself. Some manuscripts of the Life of Cuthbert, one of Bedes works, mention that Cuthberts own priest was named Bede, at the age of seven, Bede was sent to the monastery of Monkwearmouth by his family to be educated by Benedict Biscop and later by Ceolfrith. Bede does not say whether it was intended at that point that he would be a monk. Monkwearmouths sister monastery at Jarrow was founded by Ceolfrith in 682, in 686, plague broke out at Jarrow. The two managed to do the service of the liturgy until others could be trained. The young boy was almost certainly Bede, who would have been about 14, when Bede was about 17 years old, Adomnán, the abbot of Iona Abbey, visited Monkwearmouth and Jarrow. Bede would probably have met the abbot during this visit, in about 692, in Bedes nineteenth year, Bede was ordained a deacon by his diocesan bishop, John, who was bishop of Hexham. There might have been minor orders ranking below a deacon, in Bedes thirtieth year, he became a priest, with the ordination again performed by Bishop John. In about 701 Bede wrote his first works, the De Arte Metrica and De Schematibus et Tropis and he continued to write for the rest of his life, eventually completing over 60 books, most of which have survived. Not all his output can be dated, and Bede may have worked on some texts over a period of many years. His last-surviving work is a letter to Ecgbert of York, a former student, Bede may also have worked on one of the Latin bibles that were copied at Jarrow, one of which is now held by the Laurentian Library in Florence
9.
Cuthbert
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Saint Cuthbert was a saint of the early Northumbrian church in the Celtic tradition. He was a monk, bishop and hermit, associated with the monasteries of Melrose, and the South East of Scotland. After his death he became one of the most important medieval saints of Northern England, Cuthbert is regarded as the patron saint of northern England. His feast days are 20 March and 4 September, Cuthbert grew up near Melrose Abbey, a daughter-house of Lindisfarne, today in Scotland. He had decided to become a monk after seeing a vision on the night in 651 that St. Aidan, the founder of Lindisfarne, died, but seems to have seen some military service first. He was quickly made guest-master at the new monastery at Ripon, soon after 655, about 662 he was made prior at Melrose, and around 665 went as prior to Lindisfarne. In 684 he was bishop of Lindisfarne but by late 686 resigned and returned to his hermitage as he felt he was about to die. This was around 635, about the time Cuthbert was born, Cuthbert himself, though educated in the Celtic tradition, followed his mentor Eata in accepting the Roman forms without apparent difficulty after the Synod of Whitby in 664. Unlike Wilfrid, his style of life was austere, and when he was able to he lived the life of a hermit, fostering is possibly a sign of noble birth, as are references to his riding a horse when young. One night while still a boy, employed as a shepherd, he had a vision of the soul of Aidan being carried to heaven by angels, and later found out that Aidan had died that night. Edwin Burton finds a suggestion of lowly parentage in the fact that as a boy he used to tend sheep on the mountain-sides near that monastery and he appears to have had military service but at some point joined the very new monastery at Melrose, under the prior Boisil. Upon Boisils death in 661, Cuthbert succeeded him as prior, Saint Cuthbert was possibly a second cousin of King Aldfrith of Northumbria, which may have been the reason for his later proposal that Aldfrith should be crowned as monarch. Cuthberts fame for piety, diligence, and obedience quickly grew, when Alchfrith, king of Deira, founded a new monastery at Ripon, Cuthbert became its praepositus hospitum or guest master under Eata. When Wilfrid was given the monastery, Eata and Cuthbert returned to Melrose, illness struck the monastery in 664 and while Cuthbert recovered, the prior died and Cuthbert was made prior in his place. He spent much time among the people, ministering to their needs, carrying out missionary journeys, preaching. After the Synod of Whitby, Cuthbert seems to have accepted the Roman customs and he is also said to have founded St Cuthberts Church in Edinburgh. Cuthbert retired in 676, moved by a desire for the contemplative life, shortly afterwards, Cuthbert removed to Inner Farne island off the Northumbrian coast, where he gave himself up to a life of great austerity. At first he received visitors, but later he confined himself to his cell and he could not refuse an interview with the holy abbess and royal virgin Elfleda, the daughter of Oswiu of Northumbria, who succeeded St. Hilda as abbess of Whitby in 680
10.
Viking Age
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The Viking Age is the period from the late 8th century to the mid-11th century in European history, especially Northern European and Scandinavian history, following the Germanic Iron Age. It is the period of history when Scandinavian Norsemen explored Europe by its seas and rivers for trade, raids, colonisation and conquest. Three Viking ships had beached in Weymouth Bay four years earlier, the Viking devastation of Northumbrias Holy Island was reported by the Northumbrian scholar Alcuin of York, who wrote, Never before in Britain has such a terror appeared. Vikings were portrayed as violent and bloodthirsty by their enemies. The chronicles of medieval England portrayed them as rapacious wolves among sheep, the first challenges to the many anti-Viking images in Britain emerged in the 17th century. Pioneering scholarly works on the Viking Age reached a readership in Britain. Archaeologists began to dig up Britains Viking past, linguistics traced the Viking-Age origins of rural idioms and proverbs. New dictionaries of the Old Norse language enabled more Victorians to read the Icelandic Sagas, the Vikings who invaded western and eastern Europe were chiefly pagans from Denmark, Norway and Sweden. They also settled in the Faroe Islands, Ireland, Iceland, peripheral Scotland, Greenland and their North Germanic language, Old Norse, became the mother-tongue of present-day Scandinavian languages. By 801, a central authority appears to have been established in Jutland. In Norway, mountainous terrain and fjords formed strong natural boundaries, communities there remained independent of each other, unlike the situation in Denmark which is lowland. By 800, some 30 small kingdoms existed in Norway, the sea was the easiest way of communication between the Norwegian kingdoms and the outside world. It was in the 8th century that Scandinavians began to build ships of war, the North Sea rovers were traders, colonisers and explorers as well as plunderers. There are various theories concerning the causes of the Viking invasions, for people living along the coast, it would seem natural to seek new land by the sea. Another reason was that during this period England, Wales and Ireland, the Franks, however, had well-defended coasts and heavily fortified ports and harbours. Pure thirst for adventure may also have been a factor, a reason for the raids is believed by some to be over-population caused by technological advances, such as the use of iron, or a shortage of women due to selective female infanticide. Although another cause could well have been caused by the Frankish expansion to the south of Scandinavia. Consequently, these Vikings became raiders, in search of subsistence, There is ongoing debate among scholars as to why the Scandinavians began to expand during the 8th through 11th centuries
11.
Iona
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Iona is a small island in the Inner Hebrides off the Ross of Mull on the western coast of Scotland. It was a centre of Gaelic monasticism for four centuries and is renowned for its tranquility. It is a popular tourist destination and a place for retreats and its modern Gaelic name means Iona of Columba. The Hebrides have been occupied by the speakers of languages since the Iron Age. Nonetheless few, if any, can have accumulated so many different names over the centuries as the now known in English as Iona. The earliest forms of the name enabled place-name scholar William J. Watson to show that the name meant something like yew-place. The element Ivo-, denoting yew, occurs in Ogham inscriptions and in Gaulish names and it is possible that the name is related to the mythological figure, Fer hÍ mac Eogabail, foster-son of Manannan, the forename meaning man of the yew. The possible confusion results from ì, despite its original etymology, eilean Idhe means the isle of Iona, also known as Ì nam ban bòidheach. The modern English name comes of yet another variant, Ioua, iouas change to Iona, attested from c.1274, results from a transcription mistake resulting from the similarity of n and u in Insular Minuscule. Iona lies about 2 kilometres from the coast of Mull and it is about 2 kilometres wide and 6 kilometres long with a resident population of 125. The geology of the island consists mainly of Precambrian Lewisian gneiss with Torridonian sedimentary rocks on the eastern side, like other places swept by ocean breezes, there are few trees, most of them are near the parish church. Ionas highest point is Dùn Ì,101 metres, an Iron Age hill fort dating from 100 BC – AD200. Ionas geographical features include the Bay at the Back of the Ocean and Càrn Cùl ri Éirinn, the main settlement, located at St. Ronans Bay on the eastern side of the island, is called Baile Mòr and is also known locally as The Village. The primary school, post office, the two hotels, the Bishops House and the ruins of the Nunnery are here. The Abbey and MacLeod Centre are a short walk to the north, port Bàn beach on the west side of the island is home to the Iona Beach Party. The steamer Cathcart Park carrying a cargo of salt from Runcorn to Wick ran aground on Soa on 15 April 1912, in the early Historic Period Iona lay within the Gaelic kingdom of Dál Riata. The island was the site of an important monastery during the Early Middle Ages. Columba and twelve companions went into exile on Iona and founded a monastery there, many satellite institutions were founded, and Iona became the centre of one of the most important monastic systems in Great Britain and Ireland
12.
River Wear
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The River Wear in North East England rises in the Pennines and flows eastwards, mostly through County Durham to the North Sea in the City of Sunderland. At 60 mi long, it is one of the regions longest rivers, wends in a valley through the cathedral city of Durham and gives its name to Weardale in its upper reach. The Wear rises in the east Pennines, an upland area raised up during the Caledonian orogeny, specifically, the Weardale Granite underlies the headwaters of the Wear. Devonian Old Red Sandstone in age, this Weardale Granite does not outcrop but was surmised by early geologists and it is thought that the course of the River Wear, prior to the last Ice Age, was much as it is now as far as Chester-le-Street. This can be established as a result of boreholes, of which there have been many in the Wear valley due to coal mining, however, northwards from Chester-le-Street, the Wear may have originally followed the current route of the lower River Team. At about 14,000 years ago, retreat of the ice paused for maybe 500 years at the city of Durham and this can be established by the types of glacial deposits in the vicinity of Durham City. The confluence of the River Browney was pushed from Gilesgate, several miles south to Sunderland Bridge, the gorge cut by the river through the Permian Magnesian Limestone can be seen most clearly at Ford Quarry. In the 17th edition of Encyclopædia Britannica, reference is made to a pre-Ice Age course of the River Wear outfalling at Hartlepool and this may, in part, be due to the Pennine areas of Upper Weardale and Upper Teesdale being the site of the shrinking ice cap. The glaciation left behind many indications of its presence, including lateral moraines and material from the Lake District and Northumberland, after the Ice Age, the Wear valley became thickly forested, however during the Neolithic period and increasingly in the Bronze Age, were largely deforested for agriculture. Much of the River Wear is associated with the history of the Industrial Revolution and its upper end runs through lead mining country, until this gives way to coal seams of the Durham coalfield for the rest of its length. As a result of quarrying, lead mining and coal mining. The Weardale Railway continues to run services between Stanhope and Wolsingham. Mining of lead ore has been known in the area of the headwaters of the Wear since the Roman occupation, however, abandoned mines and their spoil heaps continue to contribute to heavy metal mineral pollution of the river and its tributaries. This has significance to fishing in times of low flow and infrastructure costs as the River Wear is an important source of drinking water for many of the inhabitants along its course. Fluorspar is another mineral sporadically co-present with Weardale Granite and became important in the manufacture of steel from the late 19th century into the 20th century, in many cases the steel industries were able to take fluorspar from old excavation heaps. Fluorspar explains why iron and steel manufacture flourished in the Wear valley, Consett, overlying are three Carboniferous minerals, limestone, Coal Measures as raw materials for iron and steel manufacture, and sandstone, useful as a refractory material. The last remaining flourspar mine closed in 1999 following legislation re water quality, a mine at Rogerley Quarry, Frosterley, is operated by an American consortium who occasionally work it for specimen minerals. Minco are currently exploring the North Pennines and the upper Wear catchment for potential reserves of zinc at lower levels and these sources were in due course depleted or became uneconomic
