Portal:Scottish islands

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The Scottish Islands Portal
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Relief map of Scotland, showing some of the numerous offshore islands

Scotland has around 900 offshore islands, most of which are to be found in four main groups: Shetland, Orkney, and the Hebrides, sub-divided into the Inner Hebrides and Outer Hebrides. There are also clusters of islands in the Firth of Clyde, Firth of Forth, and Solway Firth, and numerous small islands within the many bodies of fresh water in Scotland including Loch Lomond and Loch Maree. The largest island is Lewis and Harris which extends to 2,179 square kilometres, and there are a further 200 islands which are greater than 40 hectares in area. Of the remainder, several such as Staffa and the Flannan Isles are well known despite their small size. Some 94 Scottish islands are permanently inhabited, of which 89 are offshore islands. Between 2001 and 2011 Scottish island populations as a whole grew by 4% to 103,702.

The geology and geomorphology of the islands is varied. Some, such as Skye and Mull, are mountainous, while others like Tiree and Sanday are relatively low lying. Many have bedrock made from ancient Archaean Lewisian Gneiss which was formed 3 billion years ago; Shapinsay and other Orkney islands are formed from Old Red Sandstone, which is 400 million years old; and others such as Rùm from more recent Tertiary volcanoes. Many of the islands are swept by strong tides, and the Corryvreckan tide race between Scarba and Jura is one of the largest whirlpools in the world. Other strong tides are to be found in the Pentland Firth between mainland Scotland and Orkney, and another example is the "Grey Dog" between Scarba and Lunga. (More on Scottish islands...)

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The Inner Hebrides of Scotland

The Inner Hebrides (/ˈhɛbrɪdz/ HEB-rid-eez; Scottish Gaelic: na h-Eileanan a-staigh, lit.'the Inner Isles') is an archipelago off the west coast of mainland Scotland, to the south east of the Outer Hebrides. Together these two island chains form the Hebrides, which experience a mild oceanic climate. The Inner Hebrides comprise 35 inhabited islands as well as 44 uninhabited islands with an area greater than 30 hectares (74 acres). Skye, Mull, and Islay are the three largest, and also have the highest populations. The main commercial activities are tourism, crofting, fishing and whisky distilling. In modern times the Inner Hebrides have formed part of two separate local government jurisdictions, one to the north and the other to the south. Together, the islands have an area of about 4,130 km2 (1,594 sq mi), and had a population of 18,948 in 2011. The population density is therefore about 4.6 inhabitants per square kilometre (12 inhabitants per square mile).

There are various important prehistoric structures, many of which pre-date the first written references to the islands by Roman and Greek authors. In the historic period the earliest known settlers were Picts to the north and Gaels in the southern kingdom of Dál Riada prior to the islands becoming part of the Suðreyjar kingdom of the Norse, who ruled for over 400 years until sovereignty was transferred to Scotland by the Treaty of Perth in 1266. Control of the islands was then held by various clan chiefs, principally the MacLeans, MacLeods and MacDonalds. The Highland Clearances of the 19th century had a devastating effect on many communities and it is only in recent years that population levels have ceased to decline.

Sea transport is crucial and a variety of ferry services operate to mainland Scotland and between the islands. The Gaelic language remains strong in some areas; the landscapes have inspired a variety of artists; and there is a diversity of wildlife. (Full article...)

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Proposed spaceport site at Lamma Ness, Unst
Proposed spaceport site at Lamma Ness, Unst

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The corn crake, corncrake or landrail (Crex crex) is a bird in the rail family. It breeds in Europe and Asia as far east as western China, and migrates to Africa for the Northern Hemisphere's winter. It is a medium-sized crake with buff- or grey-streaked brownish-black upperparts, chestnut markings on the wings, and blue-grey underparts with rust-coloured and white bars on the flanks and undertail. The strong bill is flesh-toned, the iris is pale brown, and the legs and feet are pale grey. Juveniles are similar in plumage to adults, and downy chicks are black, as with all rails. There are no subspecies, although individuals from the east of the breeding range tend to be slightly paler than their western counterparts. The male's call is a loud krek krek, from which the scientific name is derived. The corn crake is larger than its closest relative, the African crake, which shares its wintering range; that species is also darker-plumaged, and has a plainer face.

The corn crake's breeding habitat is grassland, particularly hayfields, and it uses similar environments on the wintering grounds. This secretive species builds a nest of grass leaves in a hollow in the ground and lays 6–14 cream-coloured eggs which are covered with rufous blotches. These hatch in 19–20 days, and the black precocial chicks fledge after about five weeks. This crake is in steep decline across much of its former breeding range because modern farming practices often destroy nests before breeding is completed. The corn crake is omnivorous but mainly feeds on invertebrates, the occasional small frog or mammal, and plant material including grass seed and cereal grain. Threats include dogs, cats, other introduced and feral mammals, large birds, various parasites and diseases.

Although numbers have declined steeply in western Europe, this bird is classed as least concern on the IUCN Red List because of its huge range and large, apparently stable, populations in Russia and Kazakhstan. Numbers in western China are more significant than previously thought, and conservation measures have facilitated an increased population in some countries which had suffered the greatest losses. Despite its elusive nature, the loud call has ensured the corn crake has been noted in literature, and garnered a range of local and dialect names. (Full article...)

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A cave on Garbh Eilean in the Shiant Isles. In 1549, Donald Monro wrote that "through the arch we used to row or sail with our boats, for fear of the horrible break of the sea that is on the outward side of the point".

Description of the Western Isles of Scotland is the oldest known account of the Hebrides and the Islands of the Clyde, two chains of islands off the west coast of Scotland. The author was Donald Monro, a clergyman who used the title of "Dean of the Isles" and who lived through the Scottish Reformation. Monro wrote the original manuscript in 1549, although it was not published in any form until 1582 and was not widely available to the public in its original form until 1774. A more complete version, based on a late 17th-century manuscript written by Sir Robert Sibbald, was first published as late as 1961. Monro wrote in Scots and some of the descriptions are difficult for modern readers to render into English. Although Monro was criticised for publishing folklore and for omitting detail about the affairs of the churches in his diocese, Monro's Description is a valuable historical account and has reappeared in part or in whole in numerous publications, remaining one of the most widely quoted publications about the western islands of Scotland.

Monro also wrote a brief description of the five main branches of Clan Donald that existed in his day under the title "The Genealogies Of The Chief Clans Of The Iles", and this work was included when Description was first published as a stand-alone volume in 1805. The Sibbald manuscript also contains details about the "Council of the Isles" that operated from Eilean na Comhairle in Loch Finlaggan on the island of Islay. This is the most detailed extant account of the supreme judiciary body that had existed under the Lordship of the Isles until its demise in the late fifteenth century. (Full article...)

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Eilean Donan Castle

Eilean Donan (Scottish Gaelic: Eilean Donnain) is a small tidal island situated at the confluence of three sea lochs (Loch Duich, Loch Long and Loch Alsh) in the western Highlands of Scotland, about 1 kilometre (58 mi) from the village of Dornie. It is connected to the mainland by a footbridge that was installed early in the 20th century and is dominated by a picturesque castle that frequently appears in photographs, film and television. The island's original castle was built in the thirteenth century; it became a stronghold of the Clan Mackenzie and their allies, the Clan MacRae. In response to the Mackenzies' involvement in the Jacobite rebellions early in the 18th century, government ships destroyed the castle in 1719. The present-day castle is Lieutenant-Colonel John Macrae-Gilstrap's 20th-century reconstruction of the old castle.

Eilean Donan is part of the Kintail National Scenic Area, one of 40 in Scotland. In 2001, the island had a recorded population of just one person, but there were no "usual residents" at the time of the 2011 census.

Eilean Donan, which means simply "island of Donnán", is named after Donnán of Eigg, a Celtic saint who was martyred in 617. Donnán is said to have established a church on the island, though no trace of this remains. (Full article...)

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Skaill House, Orkney

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The Quiraing

Trotternish (Scottish Gaelic: Tròndairnis) is the northernmost peninsula of the Isle of Skye in Scotland, beginning at Portree and terminating at Rubha Hunish. The Trotternish escarpment runs almost the full length of the peninsula, some 30 kilometres (20 miles), and contains such landmarks as the Old Man of Storr and the Quiraing. The summit of The Storr, overlooking the Old Man, is the highest point of the peninsula. The north-eastern part of the peninsula around Quiraing is designated as a National Scenic Area and the entire escarpment is a Special Area of Conservation.

Dinosaur footprints have been found at An Corran, which is also a Mesolithic hunter-gatherer site dating to the 7th millennium BC. The ruins of the 14th–15th-century Duntulm Castle stand at the northern end of the peninsula.

The three major settlements on Trotternish are Portree, generally regarded as the capital of Skye, Uig, a ferry terminus, and Staffin. Trotternish is the strongest Gaelic-speaking area of Skye. (Full article...)

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John Crichton-Stuart, 2nd Marquess of Bute, KT, FRS (10 August 1793 – 18 March 1848), styled Lord Mount Stuart between 1794 and 1814, was a wealthy Scottish aristocrat and industrialist in Georgian and early Victorian Britain. He developed the coal and iron industries across South Wales and built the Cardiff Docks.

Bute's father, John, Lord Mount Stuart, died a few months after he was born and as a young child he was brought up first by his mother, the former Lady Elizabeth McDouall-Crichton, and later by his paternal grandfather, John Stuart, 1st Marquess of Bute. He travelled widely across Europe before attending Cambridge University. He contracted an eye condition and remained partially sighted for the rest of his life.

Having inherited large estates across Britain, he married his first wife, Lady Maria North, in 1818, and together they lived a relatively secluded life in Mount Stuart House in Scotland, one of Bute's four seats. Bute was dour but industrious, with a flair for land management. He focused his daily routine around extensive correspondence with his estate managers, making biennial tours of his lands around the country. The couple did not conceive any children, and Maria died in 1841. Bute remarried four years later, to Lady Sophia Rawdon-Hastings, and she gave birth to Bute's only child, John, in 1847.

Bute was a member of the House of Lords and controlled the votes of several members of the House of Commons. He was a political and religious conservative, a follower of the Duke of Wellington, but rarely took part in national debates unless his own commercial interests were involved. Early on, Bute realised the vast wealth that lay in the South Wales coalfields and set about commercially exploiting them through local ironmasters and colliers. (Full article...)

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Castle Stalker, Loch Laich
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