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Pabay Shale Formation
Pabay is a islands of Scotland, Scottish island just off the coast of Skye. The name Pabay is derived from an old Norse word meaning "priest's isle" and there are the remains of a 13th-century chapel. Geography Pabay is an island in the Inner Sound, Scotland, Inner Sound of Skye, lying north of Broadford, Skye, Broadford. It lies south of Longay and east of the larger Scalpay, Inner Hebrides, Scalpay. Like most others of the name, is a low grassy island. It is in size, diamond-shaped and predominantly flat. The highest point is above sea level, with cliffs on the North and East shores. The island is formed of fossil-containing limestone, with some micaceous shale, named Pabba Shale. It forms a flat plateau with cliffs on the North and East shores. The surrounding low reefs encroach on its shores and double the area at low water. The island gives its name to a group of Jurassic Sedimentary rocks which are seen across the Inner Hebredian area-Pabba Shales. These were laid down ...
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Papar
The Papar (; from Latin ''papa'', via Old Irish, meaning "father" or "pope") were, according to early Icelandic sagas, Irish monks who took eremitic residence in parts of what is now Iceland before that island's habitation by the Norsemen of Scandinavia, as evidenced by the sagas and recent archaeological findings. Origins The first Norsemen began settling in Iceland in 874 CE. The oldest Scandinavian source mentioning the existence of the Papar, however, the ''Íslendingabók'' ("Book of the Icelanders") by Icelandic chronicler Ari Þorgilsson, was written between 1122 and 1133, some time after the event. Ari writes of "Christian men", titled the 'Papar' by the Norsemen, who departed the isle because of their dislike of the 'heathen' Norse, pointing to the possibility of the Papar having arrived before the Norse. An earlier source that could possibly refer to the Papar is the work of Dicuil, an early 9th-century Irish monk and geographer, which included mention of the wa ...
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Gazetteer For Scotland
The ''Gazetteer for Scotland'' is a gazetteer covering the geography, history and people of Scotland. It was conceived in 1995 by Bruce Gittings of the University of Edinburgh and David Munro of the Royal Scottish Geographical Society, and contains 25,870 entries as of July 2019. It claims to be "the largest dedicated Scottish resource created for the web". The Gazetteer for Scotland provides a carefully researched and editorially validated resource widely used by students, researchers, tourists and family historians with interests in Scotland. Following on from a strong Scottish tradition of geographical publishing, the ''Gazetteer for Scotland'' is the first comprehensive gazetteer to be produced for the country since Francis Groome's ''Ordnance Gazetteer of Scotland'' (1882-6) (the text of which is incorporated into relevant entries). The aim is not to produce a travel guide, of which there are many, but to write a substantive and thoroughly edited description of the count ...
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Uninhabited Islands Of Highland (council Area)
The list of uninhabited regions includes a number of places around the globe. The list changes year over year as human beings migrate into formerly uninhabited regions, or migrate out of formerly inhabited regions. List As a group, the list of uninhabited places are called the "nonecumene". This is a special geography term which means the uninhabited area of the world. * Virtually all of the Ocean *Virtually all of Antarctica *Most of The Arctic *Most of Greenland *Most of The Sahara * Antipodes Islands * Ashmore and Cartier Islands * Bajo Nuevo Bank * Baker Island * Ball's Pyramid * Balleny Islands * Big Major Cay * Bouvet Island * Much of the interior of Brazil * Caroline Island * Clipperton Island * The semi-arid regions and deserts of Australia * Devon Island * Much of Eastern Oregon * Elephant Island * Elobey Chico * Ernst Thälmann Island * Much of Fiordland, New Zealand * Goa Island * Gough Island * Hans Island * Harmil * Hashima Island * Hatutu * Heard Island ...
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Martin Martin
Martin Martin (Scottish Gaelic: Màrtainn MacGilleMhàrtainn) (-9 October 1718) was a Scottish writer best known for his work '' A Description of the Western Islands of Scotland'' (1703; second edition 1716). This book is particularly noted for its information on the St Kilda archipelago. Martin's description of St Kilda, which he visited in 1697, had also been published some years earlier as ''A Late Voyage to St Kilda'' (1698). Life Martin was a native of Bealach, near Duntulm on Skye and he was born around 1660. He was a son of Donald Martin, who served with the MacDonalds of Sleat under James Graham, 1st Marquess of Montrose, and his wife Màiri, who was a niece of Dòmhnall Gorm Òg MacDonald, 1st Baronet of Sleat. He is thought to have had at least two brothers, Withers, Charles W.J. (1999), Introduction to ''A Description of the Western Islands of Scotland circa 1695'' by Martin Martin, Birlinn, Edinburgh, pp. 1 - 12, one of whom may have been tacksman at Flodigarry on ...
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Clan Mackinnon
Clan MacKinnon ( gd, Clann MhicFhionghain ) is a Highland Scottish clan from the islands of Mull and Skye, in the Inner Hebrides. Popular tradition gives the clan a Dalriadic Gaelic origin. The 19th-century historian W. F. Skene named the clan as one of the seven clans of Siol Alpin, who according to Skene could all trace their ancestry back to Alpin, father of Cináed mac Ailpín.Skene, pp. 258–260. Popular tradition has been until recently to consider Cináed mac Ailpín the first King of Scots and a Gael, however recent research speculates Cináed was a Pictish king and possibly even a Pict himself.Johnston, Ian"First king of the Scots? Actually he was a Pict". ''The Scotsman''. 2 October 2004. Retrieved on 16 November 2007 Sir Iain Moncreiffe of that Ilk speculated that Clan MacKinnon belonged to the kindred of Saint Columba, noting the MacKinnon Arms bore the hand of the saint holding the Cross, and the several Mackinnon abbots of Iona.Moncreiffe, pp. 70–71. The MacKin ...
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Shale
Shale is a fine-grained, clastic sedimentary rock formed from mud that is a mix of flakes of clay minerals (hydrous aluminium phyllosilicates, e.g. kaolin, Al2 Si2 O5( OH)4) and tiny fragments (silt-sized particles) of other minerals, especially quartz and calcite.Blatt, Harvey and Robert J. Tracy (1996) ''Petrology: Igneous, Sedimentary and Metamorphic'', 2nd ed., Freeman, pp. 281–292 Shale is characterized by its tendency to split into thin layers ( laminae) less than one centimeter in thickness. This property is called '' fissility''. Shale is the most common sedimentary rock. The term ''shale'' is sometimes applied more broadly, as essentially a synonym for mudrock, rather than in the more narrow sense of clay-rich fissile mudrock. Texture Shale typically exhibits varying degrees of fissility. Because of the parallel orientation of clay mineral flakes in shale, it breaks into thin layers, often splintery and usually parallel to the otherwise indistinguishable beddin ...
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Mica
Micas ( ) are a group of silicate minerals whose outstanding physical characteristic is that individual mica crystals can easily be split into extremely thin elastic plates. This characteristic is described as perfect basal cleavage. Mica is common in igneous and metamorphic rock and is occasionally found as small flakes in sedimentary rock. It is particularly prominent in many granites, pegmatites, and schists, and "books" (large individual crystals) of mica several feet across have been found in some pegmatites. Micas are used in products such as drywalls, paints, fillers, especially in parts for automobiles, roofing and shingles, as well as in electronics. The mineral is used in cosmetics and food to add "shimmer" or "frost." Properties and structure The mica group is composed of 37 phyllosilicate minerals. All crystallize in the monoclinic system, with a tendency towards pseudohexagonal crystals, and are similar in structure but vary in chemical composition. Micas are ...
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Limestone
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms when these minerals precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly dolomite, a closely related rock, which contains a high percentage of the mineral dolomite, . ''Magnesian limestone'' is an obsolete and poorly-defined term used variously for dolomite, for limes ...
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Scalpay, Inner Hebrides
Scalpay (; gd, Sgalpaigh) is an inhabited island in the Inner Hebrides of Scotland which has a population of 4. Geology The bedrock of Scalpay is largely the Neoproterozoic age sandstone and conglomerates of the Sithean Glac an Ime Member of the Applecross Formation and in the west, the Mullach nan Carn members of the Diabaig Formation, a unit of the Torridon Group, or informally the Torridonian sandstone. Outcrops of hornfelsed basalt of the Palaeocene age Skye Lava Group and the Palaeogene age Scalpay granite are found in the south and west of Scalpay. The Scalpay Sandstone and Pabay Shale formations found in the southeast of the island around Scalpay House are assigned to the Lias Group. The Staffin Shale and Staffin Bay formations are of late Jurassic age and found east of Rubha Aosail Sligneach at Caolas Scalpay. Quaternary deposits are represented by peat in the north, present day marine deposits and raised marine deposits along the southwestern shore and a restrict ...
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Isle Of Skye
The Isle of Skye, or simply Skye (; gd, An t-Eilean Sgitheanach or ; sco, Isle o Skye), is the largest and northernmost of the major islands in the Inner Hebrides of Scotland. The island's peninsulas radiate from a mountainous hub dominated by the Cuillin, the rocky slopes of which provide some of the most dramatic mountain scenery in the country. Slesser (1981) p. 19. Although has been suggested to describe a winged shape, no definitive agreement exists as to the name's origins. The island has been occupied since the Mesolithic period, and over its history has been occupied at various times by Celtic tribes including the Picts and the Gaels, Scandinavian Vikings, and most notably the powerful integrated Norse-Gaels clans of MacLeod and MacDonald. The island was considered to be under Norwegian suzerainty until the 1266 Treaty of Perth, which transferred control over to Scotland. The 18th-century Jacobite risings led to the breaking-up of the clan system and later cleara ...
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Longay
Longay ( gd, Longaigh) is a small uninhabited Geography of Scotland, Scottish island in the Inner Sound, Scotland, Inner Sound just off the coast of the Isle of Skye, north of Pabay and east of Scalpay, Inner Hebrides, Scalpay. In 1971, the Caledonian MacBrayne mailboat ''Loch Seaforth'' ran aground on the island, sustaining only minimal damage. References

Uninhabited islands of Highland (council area) {{Highland-geo-stub ...
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