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Sanda Island
Sanda Island ( gd, Sandaigh) is a small island in Argyll and Bute, Scotland, off the southern tip of the Kintyre peninsula, near Southend and Dunaverty Castle. On clear days Sanda can be seen from the southern tip of the Kintyre peninsula, from the Isle of Arran and from northeast County Antrim. It is known locally on Arran and on the Antrim coast as "Spoon Island" because of its resemblance to an upturned spoon. Population In the 2001 census Sanda was one of four Scottish islands with a population of just one person. However, since then there has been some development, and in 2008 the island had a population of 3. In August 2008 the island was put up for sale by the husband and wife owners as a result of their separation at a price of £3.2 million, and in January 2009 they announced that a sole caretaker would be resident until spring viewings re-commenced. The island was eventually sold to Swiss businessman Michi Meier for the reduced price of £2.5 million. The island's ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Firth Of Clyde
The Firth of Clyde is the mouth of the River Clyde. It is located on the west coast of Scotland and constitutes the deepest coastal waters in the British Isles (it is 164 metres deep at its deepest). The firth is sheltered from the Atlantic Ocean by the Kintyre peninsula, which encloses the outer firth in Argyll and Ayrshire. The Kilbrannan Sound is a large arm of the Firth of Clyde, separating the Kintyre Peninsula from the Isle of Arran. Within the Firth of Clyde is another major island – the Isle of Bute. Given its strategic location at the entrance to the middle and upper Clyde, Bute played a vital naval military role during World War II. Geography At its entrance, the firth is about wide. At one area in its upper reaches, it is joined by Loch Long and the Gare Loch. This area includes the large anchorage off of Greenock that is known as the Tail of the Bank. (The “Bank” is a reference to the sandbank and shoal that separates the firth from the estuary of the Ri ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glunimore Island
Glunimore Island is an uninhabited island around southeast of the Kintyre peninsula, Scotland. It lies alongside Sanda Island and Sheep Island The island is just long and rises to a height of . There is a cave on the shoreline at the north. A drying reef surrounds the island to the north and east. More of these dangerous reefs litter the sound between Glunimore, Sanda and Sheep Island. Paterson's Rock is yet another dangerous rock around 1.5 kilometres (a mile) to the east. Despite these obstacles the natural harbour formed by the three islands is still often used by boats rounding the Mull of Kintyre. Glunimore and neighbouring Sheep Island are the most important breeding grounds of puffins in the Clyde and the birds are now returning from here to Ailsa Craig another traditional breeding ground. Guillemots and razorbills also nest here. The island was visited in 1899 by two naturalists performing a survey for the Natural History Society of Glasgow. Glunimore Island len ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Galloway
Galloway ( ; sco, Gallowa; la, Gallovidia) is a region in southwestern Scotland comprising the historic counties of Wigtownshire and Kirkcudbrightshire. It is administered as part of the council area of Dumfries and Galloway. A native or inhabitant of Galloway is called a Gallovidian. The place name Galloway is derived from the Gaelic ' ("amongst the '"). The , literally meaning "Stranger-'"; the specific identity of whom the term was applied to is unknown, but the predominant view is that it referred to an ethnic and/or cultural identity such as the Strathclyde Britons or another related but distinct population. A popular theory is that it refers to a population of mixed Scandinavian and Gaelic ethnicity that may have inhabited Galloway in the Middle Ages. Galloway is bounded by sea to the west and south, the Galloway Hills to the north, and the River Nith to the east; the border between Kirkcudbrightshire and Wigtownshire is marked by the River Cree. The definition has ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Priory Of Whithorn
Whithorn Priory was a medieval Scottish monastery that also served as a cathedral, located at 6 Bruce Street in Whithorn, Wigtownshire, Dumfries and Galloway (54.7357N, 4.415954W; OS grid reference NX445405). History The priory was founded about the middle of the 12th century by Fergus, the Lord of Galloway, (died 1161) during the reign of King David I of Scotland (died 1153), initially for a community of Augustinian Canons Regular. Around 1175, the monks were replaced by Premonstratensian canons regular, referred to colloquially in Britain as the White Canons.Hunter-Blair, Oswald. "Whithorn Priory." The Catholic Encyclopedia Vol. 15. New York: Robert Appleton Company, 1912. 21 January 2019] Sometime before 1161, the Premonstratensians had been established at |
William Reeves (bishop)
William Reeves (16 March 1815 – 12 January 1892) was an Irish antiquarian and the Church of Ireland Bishop of Down, Connor and Dromore from 1886 until his death. He was the last private keeper of the Book of Armagh and at the time of his death was President of the Royal Irish Academy. Early life Born at Charleville, County Cork, on 16 March 1815, Reeves was the eldest child of Boles D'Arcy Reeves, an attorney, whose wife Mary was a daughter of Captain Jonathan Bruce Roberts, land agent to the 8th Earl of Cork. This grandfather had fought at the Battle of Bunker's Hill, and Reeves was born at his house in Charleville. From 1823, Reeves was educated at the school of John Browne in Leeson Street, Dublin, and after that at a school kept by Edward Geoghegan. In October 1830, he entered Trinity College Dublin, where he quickly gained a prize for Hebrew and was elected a Scholar in classics in 1833. In his third year, he became a scholar and went on to graduate BA in 1835. He procee ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Holy Well
A holy well or sacred spring is a well, spring or small pool of water revered either in a Christian or pagan context, sometimes both. The water of holy wells is often thought to have healing qualities, through the numinous presence of its guardian spirit or Christian saint. They often have local legends associated with them; for example in Christian legends, the water is often said to have been made to flow by the action of a saint. Holy wells are often also places of ritual and pilgrimage, where people pray and leave votive offerings. In Celtic regions, strips of cloth are often tied to trees at holy wells, known as clootie wells. Names The term ''haeligewielle'' is in origin an Anglo-Saxon toponym attached to specific springs in the landscape; its current use has arisen through folklore scholars, antiquarians, and other writers generalising from those actual 'Holy Wells', which survived into the modern era. The term 'holy-hole' is sometimes employed.A. Ross, ''Pagan Celt ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Celtic Cross
The Celtic cross is a form of Christian cross featuring a nimbus or ring that emerged in Ireland, France and Great Britain in the Early Middle Ages. A type of ringed cross, it became widespread through its use in the stone high crosses erected across the islands, especially in regions evangelized by Irish missionaries, from the ninth through the 12th centuries. A staple of Insular art, the Celtic cross is essentially a Latin cross with a nimbus surrounding the intersection of the arms and stem. Scholars have debated its exact origins, but it is related to earlier crosses featuring rings. The form gained new popularity during the Celtic Revival of the 19th century; the name "Celtic cross" is a convention dating from that time. The shape, usually decorated with interlace and other motifs from Insular art, became popular for funerary monuments and other uses, and has remained so, spreading well beyond Ireland. Early history Ringed crosses similar to older Continental f ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hadrian's Wall
Hadrian's Wall ( la, Vallum Aelium), also known as the Roman Wall, Picts' Wall, or ''Vallum Hadriani'' in Latin, is a former defensive fortification of the Roman province of Britannia, begun in AD 122 in the reign of the Emperor Hadrian. Running from Wallsend on the River Tyne in the east to Bowness-on-Solway in the west of what is now northern England, it was a stone wall with large ditches in front of it and behind it that crossed the whole width of the island. Soldiers were garrisoned along the line of the wall in large forts, smaller milecastles and intervening turrets. In addition to the wall's defensive military role, its gates may have been customs posts. A significant portion of the wall still stands and can be followed on foot along the adjoining Hadrian's Wall Path. The largest Roman archaeological feature in Britain, it runs a total of in northern England. Regarded as a British cultural icon, Hadrian's Wall is one of Britain's major ancient tourist attract ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Saint Ninian
Ninian is a Christian saint, first mentioned in the 8th century as being an early missionary among the Pictish peoples of what is now Scotland. For this reason he is known as the Apostle to the Southern Picts, and there are numerous dedications to him in those parts of Scotland with a Pictish heritage, throughout the Scottish Lowlands, and in parts of Northern England with a Northumbrian heritage. He is also known as Ringan in Scotland, and as Trynnian in Northern England. Ninian's major shrine was at Whithorn in Galloway, where he is associated with the Candida Casa (Latin for 'White House'). Nothing is known about his teachings, and there is no unchallenged authority for information about his life. The nature of Ninian's identity is uncertain, and historians have identified the name "Ninian" with other historical figures. A popular hypothesis proposed by Thomas Owen Clancy, a researcher and professor of Celtic studies, posits that Ninian can be identified with three other hi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cave
A cave or cavern is a natural void in the ground, specifically a space large enough for a human to enter. Caves often form by the weathering of rock and often extend deep underground. The word ''cave'' can refer to smaller openings such as sea caves, rock shelters, and grottos, that extend a relatively short distance into the rock and they are called ''exogene'' caves. Caves which extend further underground than the opening is wide are called ''endogene'' caves. Speleology is the science of exploration and study of all aspects of caves and the cave environment. Visiting or exploring caves for recreation may be called ''caving'', ''potholing'', or ''spelunking''. Formation types The formation and development of caves is known as ''speleogenesis''; it can occur over the course of millions of years. Caves can range widely in size, and are formed by various geological processes. These may involve a combination of chemical processes, erosion by water, tectonic forces, microorgani ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cliff
In geography and geology, a cliff is an area of rock which has a general angle defined by the vertical, or nearly vertical. Cliffs are formed by the processes of weathering and erosion, with the effect of gravity. Cliffs are common on coasts, in mountainous areas, escarpments and along rivers. Cliffs are usually composed of rock that is resistant to weathering and erosion. The sedimentary rocks that are most likely to form cliffs include sandstone, limestone, chalk, and dolomite. Igneous rocks such as granite and basalt also often form cliffs. An escarpment (or scarp) is a type of cliff formed by the movement of a geologic fault, a landslide, or sometimes by rock slides or falling rocks which change the differential erosion of the rock layers. Most cliffs have some form of scree slope at their base. In arid areas or under high cliffs, they are generally exposed jumbles of fallen rock. In areas of higher moisture, a soil slope may obscure the talus. Many cliffs also fea ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
