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Old Town, Edinburgh
The Old Town ( sco, Auld Toun) is the name popularly given to the oldest part of Scotland's capital city of Edinburgh. The area has preserved much of its medieval street plan and many Reformation-era buildings. Together with the 18th/19th-century New Town, and West End, it forms part of a protected UNESCO World Heritage Site. Royal Mile The "Royal Mile" is a name coined in the early 20th century for the main street of the Old Town which runs on a downwards slope from Edinburgh Castle to Holyrood Palace and the ruined Holyrood Abbey. Narrow '' closes'' (alleyways), often no more than a few feet wide, lead steeply downhill to both north and south of the main spine which runs west to east. Significant buildings in the Old Town include St. Giles' Cathedral, the General Assembly Hall of the Church of Scotland, the National Museum of Scotland, the Old College of the University of Edinburgh and the Scottish Parliament Building. The area contains underground vaults and hidden pass ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Edinburgh
Edinburgh ( ; gd, Dùn Èideann ) is the capital city of Scotland and one of its 32 council areas. Historically part of the county of Midlothian (interchangeably Edinburghshire before 1921), it is located in Lothian on the southern shore of the Firth of Forth. Edinburgh is Scotland's second-most populous city, after Glasgow, and the seventh-most populous city in the United Kingdom. Recognised as the capital of Scotland since at least the 15th century, Edinburgh is the seat of the Scottish Government, the Scottish Parliament and the highest courts in Scotland. The city's Palace of Holyroodhouse is the official residence of the British monarchy in Scotland. The city has long been a centre of education, particularly in the fields of medicine, Scottish law, literature, philosophy, the sciences, and engineering. It is the second-largest financial centre in the United Kingdom, and the city's historical and cultural attractions have made it the UK's second-most visited tourist d ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
National Museum Of Scotland
The National Museum of Scotland in Edinburgh, Scotland, was formed in 2006 with the merger of the new Museum of Scotland, with collections relating to Scottish antiquities, culture and history, and the adjacent Royal Scottish Museum (opened in 1866 as the Edinburgh Museum of Science and Art, renamed in 1904, and for the period between 1985 and the merger named the Royal Museum of Scotland or simply the Royal Museum), with international collections covering science and technology, natural history, and world cultures. The two connected buildings stand beside each other on Chambers Street, by the intersection with the George IV Bridge, in central Edinburgh. The museum is part of National Museums Scotland. Admission is free. The two buildings retain distinctive characters: the Museum of Scotland is housed in a modern building opened in 1998, while the former Royal Museum building was begun in 1861 and partially opened in 1866, with a Victorian Venetian Renaissance facade and a gr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
South Bridge, Edinburgh
South Bridge is a road bridge and street in Edinburgh, Scotland, between the High Street and Chambers Street/Infirmary Street. It extends to North Bridge at the north and Nicolson Street at the south, forming a level roadway over the steep valley scoured parallel to the High Street when the crag and tail landscape was formed. The Cowgate roadway along the bottom of the valley runs under the largest arch of the bridge. The South Bridge Act 1785 was passed in the House of Commons of the United Kingdom on 21 April 1785 and in 1789 taxes were raised to fund the South Bridge to a plan prepared by Robert Adam. The bridge was completed in 1788. It is constructed of nineteen arches, but is almost entirely enclosed by buildings on both sides, exposing only the largest arch where the street crosses the Cowgate. Below deck level are many buildings and vaults, the latter are now something of a tourist attraction. Most of the buildings on the deck level have separate entrances (and somet ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
North Bridge, Edinburgh
North Bridge is a road bridge and street in Edinburgh linking the High Street with Princes Street, and the Old Town with the New Town. The current bridge was built between 1894 and 1897. A previous North Bridge, built between 1763 and 1772, stood until 1896. Current North Bridge The current North Bridge is long and has three spans of arched girders each feet in length. It is wide. It was constructed from 1894 to 1897 by Sir William Arrol & Co., the company also noted for construction of the Forth Bridge. The design of the ornamentation was by the City architect of the time, Robert Morham. The foundation stone was laid on 25 May 1896 by the Lord Provost, the Rt. Hon Andrew McDonald, with Masonic ceremonial. A medal was struck commemorating the opening of the bridge on 15 September 1897. The medal shows a view of the bridge with trains underneath and on the obverse a bust of the by then knighted Sir Andrew McDonald. Situated on the bridge is a war memorial, by sculptor Wi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Edinburgh Town Walls
There have been several town walls around Edinburgh, Scotland, since the 12th century. Some form of wall probably existed from the foundation of the royal burgh in around 1125, though the first building is recorded in the mid-15th century, when the King's Wall was constructed. In the 16th century the more extensive Flodden Wall was erected, following the Scots' defeat at the Battle of Flodden in 1513. This was extended by the Telfer Wall in the early 17th century. The walls had a number of gates, known as ports, the most important being the Netherbow Port, which stood halfway down the Royal Mile. This gave access from the Canongate which was, at that time, a separate burgh. The walls never proved very successful as defensive structures, and were easily breached on more than one occasion. They served more as a means of controlling trade and taxing goods, and as a deterrent to smugglers. By the mid 18th century, the walls had outlived both their defensive and trade purposes, a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nor Loch
The Nor Loch, also known as the Nor' Loch and the North Loch, was a man-made loch formerly in Edinburgh, Scotland, in the area now occupied by Princes Street Gardens and Waverley station which lie between the Royal Mile and Princes Street. Geological formation The depression, along with the parallel one now occupied by the Cowgate, was formed by glacial erosion during the last Ice Age, when the icepack was forced to divide by the volcanic plug now known as Castle Rock. Early history A marsh formed in the hollow and was part of the natural defence of the Old Town of Edinburgh. In 1460 King James III ordered the hollow to be flooded in order to complete the defences of the town and Edinburgh Castle. The loch was formed by creating an earthen dam to block the progress of the Tummel Burn, a stream that ran along the foot of the north side of the castle rock. The water level was controlled by a sluice in the dam which was at the foot of Halkerston's Wynd. Because the Old ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Loch
''Loch'' () is the Scottish Gaelic, Scots and Irish word for a lake or sea inlet. It is cognate with the Manx lough, Cornish logh, and one of the Welsh words for lake, llwch. In English English and Hiberno-English, the anglicised spelling lough is commonly found in place names; in Lowland Scots and Scottish English, the spelling "loch" is always used. Many loughs are connected to stories of lake-bursts, signifying their mythical origin. Sea-inlet lochs are often called sea lochs or sea loughs. Some such bodies of water could also be called firths, fjords, estuaries, straits or bays. Background This name for a body of water is Insular CelticThe current form has currency in the following languages: Scottish Gaelic, Irish, Manx, and has been borrowed into Lowland Scots, Scottish English, Irish English and Standard English. in origin and is applied to most lakes in Scotland and to many sea inlets in the west and north of Scotland. The word comes from Proto-Indo-Eur ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glacier
A glacier (; ) is a persistent body of dense ice that is constantly moving under its own weight. A glacier forms where the accumulation of snow exceeds its ablation over many years, often centuries. It acquires distinguishing features, such as crevasses and seracs, as it slowly flows and deforms under stresses induced by its weight. As it moves, it abrades rock and debris from its substrate to create landforms such as cirques, moraines, or fjords. Although a glacier may flow into a body of water, it forms only on land and is distinct from the much thinner sea ice and lake ice that form on the surface of bodies of water. On Earth, 99% of glacial ice is contained within vast ice sheets (also known as "continental glaciers") in the polar regions, but glaciers may be found in mountain ranges on every continent other than the Australian mainland, including Oceania's high-latitude oceanic island countries such as New Zealand. Between latitudes 35°N and 35°S, glaciers occur o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Crag And Tail
A crag (sometimes spelled cragg, or in Scotland craig) is a rocky hill or mountain, generally isolated from other high ground. Origin Crags are formed when a glacier or ice sheet passes over an area that contains a particularly resistant rock formation (often granite, a volcanic plug or some other volcanic structure). The force of the glacier erodes the surrounding softer material, leaving the rocky block protruding from the surrounding terrain. Frequently the crag serves as a partial shelter to softer material in the wake of the glacier, which remains as a gradual fan or ridge forming a tapered ramp (called the tail) up the leeward side of the crag. In older examples, or those latterly surrounded by the sea, the tail is often missing, having been removed by post-glacial erosion. Examples Examples of crag and tail formations include: * Castle Rock (the crag, site of Edinburgh Castle) and the Royal Mile (the tail), in Edinburgh, Scotland * Salisbury Crags and Arthur ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Extinct Volcano
A volcano is a rupture in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface. On Earth, volcanoes are most often found where tectonic plates are diverging or converging, and most are found underwater. For example, a mid-ocean ridge, such as the Mid-Atlantic Ridge, has volcanoes caused by divergent tectonic plates whereas the Pacific Ring of Fire has volcanoes caused by convergent tectonic plates. Volcanoes can also form where there is stretching and thinning of the crust's plates, such as in the East African Rift and the Wells Gray-Clearwater volcanic field and Rio Grande rift in North America. Volcanism away from plate boundaries has been postulated to arise from upwelling diapirs from the core–mantle boundary, deep in the Earth. This results in hotspot volcanism, of which the Hawaiian hotspot is an example. Volcanoes are usually not created where two tectonic plates sl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Castle Rock (Edinburgh)
Castle Rock ( gd, Creag a' Chaisteil, IPA: �kʰʲɾʲekˈaˈxaʃtʰʲɪl is a volcanic plug in the middle of Edinburgh upon which Edinburgh Castle sits. The rock is estimated to have formed some 350 million years ago during the early Carboniferous period. It is the remains of a volcanic pipe which cut through the surrounding sedimentary rock, before cooling to form very hard dolerite, a coarser-grained equivalent of basalt. Subsequent glacial erosion was resisted more by the dolerite, which protected the softer rock to the east, leaving a crag and tail formation. The summit of the castle rock is above sea level, with rocky cliffs to the south, west and north, rearing up to from the surrounding landscape. This means that the only readily accessible route to the castle lies to the east, where the ridge slopes more gently. The defensive advantage of such a site is clear, but the geology of the rock also presents difficulties, since basalt is an extremely poor aquifer An aquif ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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