SCOTLAND INFO

Scotland (Scottish Gaelic: Alba) is a nation in northwest Europe and one of the four constituent countries of the United Kingdom. It occupies the northern third of the island of Great Britain and shares a land border to the south with England. It is bounded by the North Sea to the east, the Atlantic Ocean to the north and west, and the North Channel and Irish Sea to the southwest. Apart from the mainland, Scotland consists of over 790 islands. Edinburgh, the country's capital and second largest city, is one of Europe's largest financial centres. Scotland's largest city is Glasgow, which is the centre of the Greater Glasgow conurbation. Greater Glasgow is home to approximately 40% of Scotland's population. Scottish waters consist of a large sector of the North Atlantic and the North Sea, containing the largest oil reserves in the European Union. The Kingdom of Scotland was an independent state until 1 May 1707, when the Acts of Union resulted in a political union with the Kingdom of England to create the Kingdom of Great Britain. Scotland's legal system continues to be separate from those of England, Wales, and Northern Ireland, and Scotland still constitutes a discrete jurisdiction in public and in private international law. The continued independence of Scots law, the Scottish education system, and the Church of Scotland have been three factors contributing to the continuation of Scottish culture and Scottish national identity since the Union.

History of Scotland
Repeated glaciations, which covered the entire land-mass of modern Scotland, have destroyed any traces of human habitation before the mesolithic period. It is believed that the first post-glacial group(s) of hunter-gatherers arrived in Scotland around 11,000 years ago, as the ice sheet retreated after the last ice age. Groups of settlers began building the first permanent houses on Scottish soil around 9,500 years ago, and the first villages around 6,000 years ago. A site from this period is the well-preserved village of Skara Brae on the Mainland of Orkney. Neolithic habitation, burial and ritual sites are particularly common and well-preserved in the Northern Isles and Western Isles, where lack of trees led to most structures being built of local stone. The written history of Scotland began with the arrival of the Roman Empire in southern and central Great Britain, when the Romans occupied what is now England and Wales, administering it as a province called Britannia. Roman occupation of Scotland was a series of brief interludes. In 83/4 AD the general Gnaeus Julius Agricola defeated the Caledonians at the battle of Mons Graupius, and Roman forts were briefly set along the Gask Ridge close to the Highland Line (none are known to have ever been constructed beyond that line). Scotland is called Scotia in Latin. Three years after the battle the Roman armies had withdrawn to the Southern Uplands. They erected Hadrian's Wall to control tribes on both sides of the wall, but it effectively became the main northern border for the Romans throughout much of the later occupation of Britain, although they held the Antonine Wall in the Central Lowlands for two short periods. The last of these was during the time of Emperor Septimius Severus from 208 until 210. The extent of Roman occupation of any significant part of Scotland was limited to a total of about 40 years, although their influence on the southern section of the country occupied by Brythonic tribes such as the Votadini and Damnonii would still have been considerable. The Kingdom of the Picts (based in Fortriu by the 6th century) was the state which eventually became known as "Alba" or "Scotland". The development of "Pictland", according to the historical model developed by Peter Heather, was a natural response to Roman imperialism. Another view places emphasis on the Battle of Dunnichen, and the reign of Bruide mac Der Ilei (671-693), with another period of consolidation in the reign of Óengus mac Fergusa (732-761). The Kingdom of the Picts as it was in the early 8th century, when Bede was writing, was largely the same as the kingdom of the Scots in the reign of Alexander (1107-1124). However, by the tenth century, the Pictish kingdom was increasingly dominated by what we can recognise as Gaelic culture, and had developed an Irish conquest myth around the ancestor of the contemporary royal dynasty, Cináed mac Ailpín (Kenneth MacAlpin). The decisive victory of Robert the Bruce over the English at Bannockburn was a defining moment establishing the Bruce dynasty and hence the independence of the Kingdom of the Scots.From a base of territory in eastern Scotland north of the River Forth and south of the River Oykel, the kingdom acquired control of the lands lying to the north and south. By the 12th century, the kings of Alba had added to their territories the English-speaking land in south-east and attained overlordship of Galloway and Norse-speaking Caithness; by the end of the 13th century, the kingdom had assumed approximately its modern borders. However, processes of cultural and economic change beginning in the 12th century ensured Scotland looked very different in the later Middle Ages. The stimulus for this was the reign of King David I and the so-called Davidian Revolution. Feudalism, government reorganisation and the first legally defined towns, called burghs, began in this period. These institutions and the immigration of French and Anglo-French knights and churchmen facilitated a process of cultural osmosis, whereby the culture and language of the low-lying and coastal parts of the kingdom's original territory in the east became, like the newly-acquired south-east, English-speaking, while the rest of the country retained the Gaelic language. The death of Alexander III in 1286, followed by the death of his grand-daughter Margaret, Maid of Norway, broke the succession line of Scotland's kings. This led to the intervention of Edward I of England. Edward established John Balliol as a sub-king, but this relationship broke down, leading to an ultimately unsuccessful attempt at total takeover by the English crown. This was famously opposed by William Wallace and others in the Wars of Scottish Independence, and in the divided country Robert de Brus, Earl of Carrick, became king (as Robert I). Robert, also known as "Robert the Bruce," had been excommunicated for bringing about the death of one of his rivals in church, and this excommunication was eventually expanded to the entire country. War with England continued for several decades, and a civil war between the Bruce dynasty and the English-backed Balliols lasted until the middle of the 14th century. Although the Bruce dynasty was successful, David II's lack of an heir allowed his nephew Robert II to come to the throne and establish the Stewart Dynasty. The Stewarts ruled Scotland for the remainder of the Middle Ages. The country they ruled experienced greater prosperity from the end of the 14th century through the Scottish Renaissance to the Reformation. This was despite continual warfare with England, the increasing division between Highlands and Lowlands, and a large number of royal minorities. In 1603, James VI King of Scots inherited the throne of the Kingdom of England, and became also King James I of England. With the exception of a short period under The Protectorate, Scotland remained a separate state, but there was considerable conflict between the crown and the Covenanters over the form of church government. After the Glorious Revolution and the overthrow of the Roman Catholic James VII by William and Mary, Scotland briefly threatened to select a different Protestant monarch from England. In 1707, however, following English threats to end trade and free movement across the border, the Scots Parliament and the Parliament of England enacted the twin Acts of Union, which created the Kingdom of Great Britain. Two major Jacobite risings launched from the Highlands of Scotland in 1715 and 1745 failed to remove the House of Hanover from the British throne. The deposed Jacobite Stuart claimants had remained popular in the Highlands and north-east, particularly amongst non-Presbyterians. Following the Scottish Enlightenment and the Industrial Revolution, Scotland became one of the commercial, intellectual and industrial powerhouses of Europe. After World War II, Scotland experienced an industrial decline which was particularly acute. Only in recent decades has the country enjoyed something of a cultural and economic renaissance. Factors which have contributed to this recovery include a resurgent financial services and electronics sector, the proceeds of North Sea oil and gas, and latterly the devolved Scottish Parliament, established by the UK government under the Scotland Act 1998.

Geography & Natural History
Scotland comprises the northern third of the island of Great Britain, which lies off the coast of north west Europe. The total land mass is 78,772 km² (30,414 mi²). Scotland's only land border is with England, and runs for 96 kilometres (60 miles) between the River Tweed on the east coast and the Solway Firth in the west. The Atlantic Ocean borders the west coast and the North Sea is to the east. The island of Ireland lies only 30 kilometres (20 mi) from the south western peninsula of Kintyre, Norway is 400 kilometres (250 mi) to the north east, and the Faroes and Iceland are to the north. The geographical centre of Scotland lies a few miles from the village of Newtonmore in Badenoch, far to the north of the modern population heartlands. The territorial extent of Scotland is generally that established by the 1237 Treaty of York between Scotland and England and the 1266 Treaty of Perth between Scotland and Norway. Exceptions include: the Isle of Man, which is now a crown dependency outside the United Kingdom, the 15th century acquisitions of Orkney and Shetland from Norway; and Rockall, a small rocky islet in the North Atlantic which was annexed by the UK in 1955 and later declared part of Scotland by the Island of Rockall Act 1972.



Geology of Scotland
The whole of Scotland was covered by ice sheets during the Pleistocene ice ages and the landscape is much affected by glaciation. From a geological perspective the country has three main sub-divisions. The Highlands and Islands lie to the north and west of the Highland Boundary Fault, which runs from Arran to Stonehaven. This part of Scotland largely comprises ancient rocks from the Cambrian and Precambrian which were uplifted during the later Caledonian Orogeny. These foundations are interspersed with many igneous intrusions of a more recent age, the remnants of which have formed mountain massifs such as the Cairngorms and Skye Cuillins. A significant exception to the above are the fossil-bearing beds of Old Red Sandstones found principally along the Moray Firth coast. The Highlands are generally mountainous and are bisected by the Great Glen. The highest elevations in the British Isles are found here, including Ben Nevis, the highest peak at 1,344 metres (4,409 ft). Scotland has over 790 islands, divided into four main groups: Shetland, Orkney, and the Hebrides, sub-divided into the Inner Hebrides and Outer Hebrides. There are numerous bodies of freshwater including Loch Lomond and Loch Ness. The Central Lowlands is a rift valley mainly comprising Paleozoic formations. Many of these sediments have economic significance for it is here that the coal and iron bearing rocks that fuelled Scotland's industrial revolution are to be found. This area has also experienced intense vulcanism, Arthur’s Seat in Edinburgh being the remnant of a once much larger volcano active in the Carboniferous period some 300 million years ago. Also known as the Midland Valley, this area is relatively low-lying, although even here hills such as the Ochils and Campsie Fells are rarely far from view. The Southern Uplands are a range of hills almost 200 km (125 miles) long, interspersed with broad valleys. They lie south of a second fault line running from Stranraer towards Dunbar. The geological foundations largely comprise Silurian deposits laid down some 4-500 million years ago.

Climate of Scotland
Ben Nevis, the highest peak in the British Isles, is in Lochaber, the wettest district in the British IslesThe climate of Scotland is temperate and oceanic, and tends to be very changeable. It is warmed by the Gulf Stream from the Atlantic, and as such has much milder winters (but cooler, wetter summers) than areas on similar latitudes, for example Oslo or Moscow. However, temperatures are generally lower than in the rest of the UK, with the coldest ever UK temperature of -27.2°C (-16.96°F) recorded at Braemar in the Grampian Mountains, on 11 February 1895 and 10 January 1982 and also at Altnaharra, Highland, on 30 December 1995. Winter maximums average 6°C (42.8°F) in the lowlands, with summer maximums averaging 18°C (64.4°F). The highest temperature recorded was 32.9°C (91.22°F) at Greycrook, Scottish Borders on 9 August 2003. In general, the west of Scotland is usually warmer than the east, due to the influence of the Atlantic ocean currents, and the colder surface temperatures of the North Sea. Tiree, in the Inner Hebrides, is one of the sunniest places in the country: it had 300 days of sunshine in 1975. Rainfall varies widely across Scotland. The western highlands of Scotland are the wettest place, with annual rainfall exceeding 3,000 mm (120 inches). In comparison, much of lowland Scotland receives less than 800 mm (31 inches) annually. Heavy snowfall is not common in the lowlands, but becomes more common with altitude. Braemar experiences an average of 59 snow days per year, while coastal areas have an average of fewer than 10 days.

Fauna of Scotland
Scotland's wildlife is typical of the north west of Europe although several of the larger mammals such as the Brown Bear, Wolf, Eurasian Lynx, Beaver, Reindeer, Elk and Walrus were hunted to extinction in historic times. A population of Wild Cats remains. There are important populations of seals and internationally significant nesting grounds for a variety of seabirds such as Northern Gannets. The Golden Eagle is something of a national icon, and White-tailed Eagles and Ospreys are recent re-colonisations. The Scottish Crossbill is Britain's only endemic bird. The flora of the country is varied incorporating both deciduous and coniferous woodlands, and moorland and tundra species. Significant remnants of the native Scots Pine forest, can be found in places

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