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Flodday Near Vatersay
Flodday ( gd, Flodaigh) is an uninhabited island, south west of Barra in the Western Islands of Scotland. Geography and geology Flodday is one of the Barra Isles, lying west of Sandray. It consists of three parts, with a natural rock arch between the larger two. Facing west there are black cliffs. Wildlife The island has a small grey seal The grey seal (''Halichoerus grypus'') is found on both shores of the North Atlantic Ocean. In Latin Halichoerus grypus means "hook-nosed sea pig". It is a large seal of the family Phocidae, which are commonly referred to as "true seals" o ... colony and is home to a subspecies of the dark green fritillary butterfly (''Argynnis aglaja scotica''). Notes and references Barra Isles Clan MacNeil Uninhabited islands of the Outer Hebrides Natural arches of Scotland {{WesternIsles-geo-stub ...
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Uist
"Uist" is a group of six islands and are part of the Outer Hebridean Archipelago, part of the Outer Hebrides of Scotland. North Uist and South Uist ( or ; gd, Uibhist ) are two of the islands and are linked by causeways running via the isles of Benbecula and Grimsay. From south to north, the inhabited islands in the island group are (Eriskay), (South Uist), Grimsay (South), (Benbecula), ( Flodaigh), ( Grimsay (North)), , (North Uist), (Baleshare) and ( Berneray). The islands, collectively, have a population of 4,723. Major settlements The main settlements in Uist are: South Uist * (Daliburgh) * (Lochboisdale) * ( Snishvale) * ( Stoneybridge) * ( Eochar) * ( Polochar) * (Eriskay) Benbecula * (Balivanich) * ( Creagorry) * ( Liniclate) North Uist * ( Carinish) * ( Bayhead) * (Sollas) * (Lochmaddy) * (Balemore) 16th century Geography Writing in 1549, Sir Donald Monro, High Dean of the Isles stated of "Ywst" that it was a fertile country full of ...
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Barra
Barra (; gd, Barraigh or ; sco, Barra) is an island in the Outer Hebrides, Scotland, and the second southernmost inhabited island there, after the adjacent island of Vatersay to which it is connected by a short causeway. The island is named after Saint Finbarr of Cork. In 2011, the population was 1,174. Gaelic is widely spoken, and at the 2011 Census, there were 761 Gaelic speakers (62% of the population). Geology In common with the rest of the Western Isles, Barra is formed from the oldest rocks in Britain, the Lewisian gneiss, which dates from the Archaean eon. Some of the gneiss in the east of the island is noted as being pyroxene-bearing. Layered textures or foliation in this metamorphic rock is typically around 30° to the east or northeast. Palaeoproterozoic age metadiorites and metatonalites forming a part of the East Barra Meta-igneous Complex occur around Castlebay as they do on the neighbouring islands of Vatersay and Flodday. A few metabasic dykes intrude ...
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Na H-Eileanan Siar
The Outer Hebrides () or Western Isles ( gd, Na h-Eileanan Siar or or ("islands of the strangers"); sco, Waster Isles), sometimes known as the Long Isle/Long Island ( gd, An t-Eilean Fada, links=no), is an island chain off the west coast of mainland Scotland. The islands are geographically coextensive with , one of the 32 unitary council areas of Scotland. They form part of the archipelago of the Hebrides, separated from the Scottish mainland and from the Inner Hebrides by the waters of the Minch, the Little Minch, and the Sea of the Hebrides. Scottish Gaelic is the predominant spoken language, although in a few areas English speakers form a majority. Most of the islands have a bedrock formed from ancient metamorphic rocks, and the climate is mild and oceanic. The 15 inhabited islands have a total population of and there are more than 50 substantial uninhabited islands. The distance from Barra Head to the Butt of Lewis is roughly . There are various important preh ...
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Outer Hebrides
The Outer Hebrides () or Western Isles ( gd, Na h-Eileanan Siar or or ("islands of the strangers"); sco, Waster Isles), sometimes known as the Long Isle/Long Island ( gd, An t-Eilean Fada, links=no), is an island chain off the west coast of mainland Scotland. The islands are geographically coextensive with , one of the 32 unitary council areas of Scotland. They form part of the archipelago of the Hebrides, separated from the Scottish mainland and from the Inner Hebrides by the waters of the Minch, the Little Minch, and the Sea of the Hebrides. Scottish Gaelic is the predominant spoken language, although in a few areas English speakers form a majority. Most of the islands have a bedrock formed from ancient metamorphic rocks, and the climate is mild and oceanic. The 15 inhabited islands have a total population of and there are more than 50 substantial uninhabited islands. The distance from Barra Head to the Butt of Lewis is roughly . There are various important preh ...
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Scotland
Scotland (, ) is a Countries of the United Kingdom, country that is part of the United Kingdom. Covering the northern third of the island of Great Britain, mainland Scotland has a Anglo-Scottish border, border with England to the southeast and is otherwise surrounded by the Atlantic Ocean to the north and west, the North Sea to the northeast and east, and the Irish Sea to the south. It also contains more than 790 Islands of Scotland, islands, principally in the archipelagos of the Hebrides and the Northern Isles. Most of the population, including the capital Edinburgh, is concentrated in the Central Belt—the plain between the Scottish Highlands and the Southern Uplands—in the Scottish Lowlands. Scotland is divided into 32 Subdivisions of Scotland, administrative subdivisions or local authorities, known as council areas. Glasgow, Glasgow City is the largest council area in terms of population, with Highland (council area), Highland being the largest in terms of area. Limi ...
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Barra Isles
The Barra Isles, also known as the Bishop's Isles, are a small archipelago in the Outer Hebrides of Scotland. They lie south of the island of Barra, for which they are named. The group consists of nine islands and numerous rocky islets, skerries, and sea stacks. In 1427, the Lords of the Isles awarded Lairdship of Barra (and its associated islands) to Clan MacNeil of Barra. However, following acts of piracy by the MacNeils, king James VI transferred ownership of the southern archipelago to the Bishop of the Isles, hence the islands became known as the ''Bishop's Isles''.Murray, W.H. (1966) ''The Hebrides''. London. Heinemann. p. 230 Murray writes that they belonged "to the Bishop of the Isles ''de jure'' although to MacNeil ''de facto''". Many of the islands are extremely small; only the largest, Vatersay – which is now linked by causeway to Barra – remains inhabited. Berneray (also known as Barra Head), Pabbay, Sandray and Mingulay have been inhabited in the past. The ...
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Sandray
Sandray ( gd, Sanndraigh) is one of the Barra Isles in the Outer Hebrides of Scotland. It never had a large population, and has been uninhabited since 1934. It is now known for its large seabird colony. Geography Sandray is half a mile due south of Vatersay, and east of Flodaigh, north east of Lingeigh and Pabaigh. Maol Domhnaigh/ Muldoanich is to the north east of it. There are three main peninsulas on the south end of Sandray, they are called Meanish, Leehinish and Rubha Pabbach. See also * List of islands of Scotland This is a list of islands of Scotland, the mainland of which is part of the island of Great Britain. Also included are various other related tables and lists. The definition of an offshore island used in this list is "land that is surrounded by ... Footnotes Barra Isles Uninhabited islands of the Outer Hebrides {{WesternIsles-geo-stub ...
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Natural Arch
A natural arch, natural bridge, or (less commonly) rock arch is a natural landform where an arch has formed with an opening underneath. Natural arches commonly form where inland cliffs, coastal cliffs, fins or stacks are subject to erosion from the sea, rivers or weathering (subaerial processes). Most natural arches are formed from narrow fins and sea stacks composed of sandstone or limestone with steep, often vertical, cliff faces. The formations become narrower due to erosion over geologic time scales. The softer rock stratum erodes away creating rock shelters, or alcoves, on opposite sides of the formation beneath the relatively harder stratum, or caprock, above it. The alcoves erode further into the formation eventually meeting underneath the harder caprock layer, thus creating an arch. The erosional processes exploit weaknesses in the softer rock layers making cracks larger and removing material more quickly than the caprock; however, the caprock itself continues to e ...
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Grey Seal
The grey seal (''Halichoerus grypus'') is found on both shores of the North Atlantic Ocean. In Latin Halichoerus grypus means "hook-nosed sea pig". It is a large seal of the family Phocidae, which are commonly referred to as "true seals" or "earless seals". It is the only species classified in the genus ''Halichoerus''. Its name is spelled gray seal in the US; it is also known as Atlantic seal and the horsehead seal. Taxonomy There are two recognized subspecies of this seal: The type specimen of ''H. g. grypus'' (Zoological Museum of Copenhagen specimen ZMUC M11-1525, caught off the island of Amager, Danish part of the Baltic Sea) was believed lost for many years but was rediscovered in 2016, and a DNA test showed it belonged to a Baltic Sea specimen rather than from Greenland, as had previously been assumed (because it was first described in Otto Fabricius' book on the animals in Greenland: ''Fauna Groenlandica''). The name ''H. g. grypus'' was therefore transferred to the ...
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Dark Green Fritillary
The dark green fritillary (''Speyeria aglaja'') is a species of butterfly in the family Nymphalidae. The insect has a wide range in the Palearctic realm - Europe, Morocco, Iran, Siberia, Central Asia, China, Korea, and Japan. Description in Seitz The large fritillary is fiery reddish yellow above, the basal area of the male being always duller. The markings are constant: a black margin, a row of deep black but thin marginal arcs, a very straight, central row of dots, of which only the last one of the forewing is shifted distad; between this row of dots and the base there are six thin black transverse bands extending from the subcostal vein into the wing. The underside of the hindwing is characteristic; it bears numerous silver-spots on a partly verdigris partly leather-yellow ground, but never a row of ocelli in the marginal area, as is the case in the forms of the Niobe fritillary (''Fabriciana niobe'') and high brown fritillary (''F. adippe''). Seitz. A. in Seitz, A. ed. Band ...
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Clan MacNeil
Clan MacNeil, also known in Scotland as Clan Niall, is a highland Scottish clan of Irish origin. According to their early genealogies and some sources they're descended from Eógan mac Néill and Niall of the Nine Hostages. The clan is particularly associated with the Outer Hebridean island of Barra. The early history of Clan MacNeil is obscure, however despite this the clan claims to descend from the legendary Irish King Niall of the Nine Hostages, who is counted as the 1st Clan Chief, the current Clan Chief being the 47th. The clan itself takes its name from a ''Niall'' who lived in the 13th or early 14th century, and who belonged to the same dynastic family of Cowal and Knapdale as the ancestors of the Lamonts, MacEwens of Otter, Maclachlans, and the MacSweens. While the clan is centred in Barra in the Outer Hebrides, there is a branch of the clan in Argyll (McNeill/MacNeill) that some historians have speculated was more senior in line, or possibly even unrelated. However, ...
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