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Great Cumbrae
Great Cumbrae ( sco, Muckle Cumbrae; gd, Cumaradh Mòr; also known as Great Cumbrae Island, Cumbrae or the Isle of Cumbrae) is the larger of the two islands known as The Cumbraes in the lower Firth of Clyde in western Scotland. The island is sometimes called Millport, after its main town. Home to the Cathedral of The Isles and the FSC Millport field study centre, the island has a thriving community of 1,300 residents. Geography The island is roughly long by wide, rising to a height of above sea level at The Glaid Stone, which is a large, naturally occurring rock perched on the highest summit on the island. There is a triangulation pillar nearby, as well as an orientation point which indicates the locations of surrounding landmarks. In clear conditions, views extend north over the upper Clyde estuary to Ben Lomond and the Arrochar Alps. To the west, the larger islands of Bute and Arran can be seen, while on the other side of Knapdale the Paps of Jura may be visible. Loo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Britons (historical)
The Britons ( *''Pritanī'', la, Britanni), also known as Celtic Britons or Ancient Britons, were people of Celtic language and culture who inhabited Great Britain from at least the British Iron Age and into the Middle Ages, at which point they diverged into the Welsh, Cornish and Bretons (among others). They spoke the Common Brittonic language, the ancestor of the modern Brittonic languages. The earliest written evidence for the Britons is from Greco-Roman writers and dates to the Iron Age.Koch, pp. 291–292. Celtic Britain was made up of many tribes and kingdoms, associated with various hillforts. The Britons followed an Ancient Celtic religion overseen by druids. Some of the southern tribes had strong links with mainland Europe, especially Gaul and Belgica, and minted their own coins. The Roman Empire conquered most of Britain in the 1st century, creating the province of Britannia. The Romans invaded northern Britain, but the Britons and Caledonians in the north ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ailsa Craig
Ailsa Craig (; sco, Ailsae Craig; gd, Creag Ealasaid) is an island of in the outer Firth of Clyde, west of mainland Scotland, upon which microgranite has long been quarried to make curling stones. The now-uninhabited island comprises the remains of a magmatic pluton formed during the same period of igneous activity as magmatic rocks on the nearby Isle of Arran. The island, colloquially known as " Paddy's milestone", was a haven for Catholics during the Scottish Reformation in the 16th century, but is today a bird sanctuary, providing a home for huge numbers of gannets and an increasing number of puffins. Etymology An early reference to the rock is made by Sir Donald Monro, Archdeacon of the Isles, who referred to the rock as "Elsay" in the 16th century. The modern name of the island is an anglicisation of the Gaelic, ''Aillse Creag'' meaning "fairy rock". An alternative Gaelic name is ''Creag Ealasaid'' meaning "Elizabeth's rock". The first element, ''Aillse'' may repres ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sedimentary Rock
Sedimentary rocks are types of rock that are formed by the accumulation or deposition of mineral or organic particles at Earth's surface, followed by cementation. Sedimentation is the collective name for processes that cause these particles to settle in place. The particles that form a sedimentary rock are called sediment, and may be composed of geological detritus (minerals) or biological detritus (organic matter). The geological detritus originated from weathering and erosion of existing rocks, or from the solidification of molten lava blobs erupted by volcanoes. The geological detritus is transported to the place of deposition by water, wind, ice or mass movement, which are called agents of denudation. Biological detritus was formed by bodies and parts (mainly shells) of dead aquatic organisms, as well as their fecal mass, suspended in water and slowly piling up on the floor of water bodies (marine snow). Sedimentation may also occur as dissolved minerals precipitate from ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carboniferous
The Carboniferous ( ) is a geologic period and system of the Paleozoic that spans 60 million years from the end of the Devonian Period million years ago ( Mya), to the beginning of the Permian Period, million years ago. The name ''Carboniferous'' means "coal-bearing", from the Latin '' carbō'' ("coal") and '' ferō'' ("bear, carry"), and refers to the many coal beds formed globally during that time. The first of the modern 'system' names, it was coined by geologists William Conybeare and William Phillips in 1822, based on a study of the British rock succession. The Carboniferous is often treated in North America as two geological periods, the earlier Mississippian and the later Pennsylvanian. Terrestrial animal life was well established by the Carboniferous Period. Tetrapods (four limbed vertebrates), which had originated from lobe-finned fish during the preceding Devonian, became pentadactylous in and diversified during the Carboniferous, including early amphibian line ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Devonian
The Devonian ( ) is a geologic period and system of the Paleozoic era, spanning 60.3 million years from the end of the Silurian, million years ago (Mya), to the beginning of the Carboniferous, Mya. It is named after Devon, England, where rocks from this period were first studied. The first significant adaptive radiation of life on dry land occurred during the Devonian. Free-sporing vascular plants began to spread across dry land, forming extensive forests which covered the continents. By the middle of the Devonian, several groups of plants had evolved leaves and true roots, and by the end of the period the first seed-bearing plants appeared. The arthropod groups of myriapods, arachnids and hexapods also became well-established early in this period, after starting their expansion to land at least from the Ordovician period. Fish reached substantial diversity during this time, leading the Devonian to often be dubbed the Age of Fishes. The placoderms began dominating ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mudstone
Mudstone, a type of mudrock, is a fine-grained sedimentary rock whose original constituents were clays or muds. Mudstone is distinguished from '' shale'' by its lack of fissility (parallel layering).Blatt, H., and R.J. Tracy, 1996, ''Petrology.'' New York, New York, W. H. Freeman, 2nd ed, 529 pp. The term ''mudstone'' is also used to describe carbonate rocks (limestone or dolomite) that are composed predominantly of carbonate mud. However, in most contexts, the term refers to siliciclastic mudstone, composed mostly of silicate minerals. The NASA Curiosity rover has found deposits of mudstone on Mars that contain organic substances such as propane, benzene and toluene. Definition There is not a single definition of mudstone that has gained general acceptance,Boggs 2006, p.143 though there is wide agreement that mudstones are fine-grained sedimentary rocks, composed mostly of silicate grains with a grain size less than . Individual grains this size are too small to be disting ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sandstone
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar (both silicates) because they are the most resistant minerals to weathering processes at the Earth's surface. Like uncemented sand, sandstone may be any color due to impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Since sandstone beds often form highly visible cliffs and other topographic features, certain colors of sandstone have been strongly identified with certain regions. Rock formations that are primarily composed of sandstone usually allow the percolation of water and other fluids and are porous enough to store large quantities, making them valuable aquifers and petroleum reservoirs. Quartz-bearing sandstone can be changed into quartzite through metamorphism, usually related to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hákonar Saga Hákonarsonar
''Hákonar saga Hákonarsonar'' ("The Saga of Haakon Haakonarson") or ''Hákonar saga gamla'' ("The Saga of Old Haakon") is an Old Norse Kings' Saga, telling the story of the life and reign of King Haakon Haakonarson of Norway. Content and style The circumstances of the saga's composition are exceptionally well understood, as they are recorded in some detail in '' Sturlunga saga'' (particularly ''Sturlu þáttr''): the saga was written in the 1260s (apparently 1264–65) by the Icelandic historian and chieftain Sturla Þórðarson (nephew of the noted historian Snorri Sturluson). Sturla Þórðarson was at the court of Haakon's son Magnus Lagabøte when Magnus learned of his father's death in Kirkwall in Orkney. Magnus is said to have immediately commissioned Sturla to write his father's saga. This was awkward for Sturla: 'King Hákon had instigated the death of Sturla's uncle, Snorri Sturluson, in 1241. Sturla rightly regarded Hákon as his most dangerous enemy, for he had steadf ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kingdom Of Strathclyde
Strathclyde (lit. "Strath of the River Clyde", and Strað-Clota in Old English), was a Brittonic successor state of the Roman Empire and one of the early medieval kingdoms of the Britons, located in the region the Welsh tribes referred to as Yr Hen Ogledd (“the Old North"), which comprised the Brythonic-speaking parts of what is now southern Scotland and northern England. The kingdom developed during Britain's post-Roman period. It is also known as ''Alt Clut'', a Brittonic term for Dumbarton Castle, the medieval capital of the region. It may have had its origins with the Damnonii people of Ptolemy's ''Geography''. The language of Strathclyde is known as Cumbric, a language that is closely related to Old Welsh, and, among modern languages, is most closely related to Welsh, Cornish, and Breton. Scottish toponymy and archaeology points to some later settlement by Vikings or Norse–Gaels (see Scandinavian Scotland), although to a lesser degree than in neighbouring Galloway. A ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Brittonic Languages
The Brittonic languages (also Brythonic or British Celtic; cy, ieithoedd Brythonaidd/Prydeinig; kw, yethow brythonek/predennek; br, yezhoù predenek) form one of the two branches of the Insular Celtic language family; the other is Goidelic. The name ''Brythonic'' was derived by Welsh Celticist John Rhys from the Welsh word , meaning Ancient Britons as opposed to an Anglo-Saxon or Gael. The Brittonic languages derive from the Common Brittonic language, spoken throughout Great Britain during the Iron Age and Roman period. In the 5th and 6th centuries emigrating Britons also took Brittonic speech to the continent, most significantly in Brittany and Britonia. During the next few centuries the language began to split into several dialects, eventually evolving into Welsh, Cornish, Breton, Cumbric, and probably Pictish. Welsh and Breton continue to be spoken as native languages, while a revival in Cornish has led to an increase in speakers of that language. Cumbric and Pictish are ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Crocodile Rock
"Crocodile Rock" is a song written by Elton John and Bernie Taupin, and recorded in summer 1972 at the Château d'Hérouville studio in France (it was listed as "Strawberry Studios" in the album's credits), where John and his team had previously recorded the ''Honky Château'' album. It was released on 27 October 1972 in the UK and 20 November 1972 in the U.S., as a pre-release single from his forthcoming 1973 album ''Don't Shoot Me I'm Only the Piano Player'', and became his first U.S. number-one single, reaching the top spot on 3 February 1973, and staying there for three weeks. In the U.S., it was certified Gold on 5 February 1973 and Platinum on 13 September 1995 by the RIAA. In Canada, it topped the chart as well, remaining at number one on the ''RPM 100'' national singles chart for four weeks from 17 February through 10 March. It was the first song released as a single on the MCA label (catalogue #40000) after MCA dissolved its Uni, Decca, Kapp and Coral labels. (Joh ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fairlie, North Ayrshire
Fairlie is a village in North Ayrshire, Scotland. Location and status Fairlie sits on the eastern shore of the Firth of Clyde and looks across to the Isle of Arran and the Cumbraes. It is currently little more than a commuter village, with few businesses still running within Fairlie. These include the "Village Inn" (a pub and restaurant) and a petrol station According to the 2001 census, Fairlie counted 1,510 residents. Fairlie House near Gatehead, Ayrshire in East Ayrshire was named after the Fairlie family of Fairlie; it previous name had been Little Dreghorn. History King David I of Scotland appointed Sir Richard de Morville, a Norman, to hold land in Scotland. Thus he became High Constable of Scotland and Lord of Cunninghame, Largs and Lauderdale. This piece of land was later sub-divided among Richard's relatives and friends, and, in the 13th century, the land of Fairlie was held by the de Ros (or Ross) family of Tarbert, the land to the North was held by the Boyle famil ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Saunders_Quarry-1.jpg "Click for more on -> Sandstone")
