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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] |
Marilyn (hill)
This is a list of Marilyn hills and mountains in the United Kingdom, Isle of Man and Republic of Ireland, Ireland by height. Lists of mountains and hills in the British Isles#Marilyns, Marilyns are defined as peaks with a topographic prominence, prominence of or more, regardless of height or any other merit (e.g. topographic isolation, as used in Lists of mountains and hills in the British Isles#Munros, Munros). Thus, Marilyns can be mountains, with a height above , or relatively small hills. there were 2,011 recorded Marilyns. Definition The Marilyn classification was created by Alan Dawson in his 1992 book ''The Relative Hills of Britain''. The name Marilyn was coined by Dawson as a punning contrast to the ''Munro'' classification of Scottish mountains above , but which has no explicit prominence threshold, being homophonous with (Marilyn) ''Marilyn Monroe, Monroe''. The list of Marilyns was extended to Ireland by Clem Clements. Marilyn was the first of several subsequen ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Book Of Leinster
The Book of Leinster ( mga, Lebor Laignech , LL) is a medieval Irish manuscript compiled c. 1160 and now kept in Trinity College, Dublin, under the shelfmark MS H 2.18 (cat. 1339). It was formerly known as the ''Lebor na Nuachongbála'' "Book of Nuachongbáil", a monastic site known today as Oughaval. Some fragments of the book, such as the ''Martyrology of Tallaght'', are now in the collection of University College, Dublin. Date and provenance The manuscript is a composite work and more than one hand appears to have been responsible for its production. The principal compiler and scribe was probably Áed Ua Crimthainn,Hellmuth, "''Lebor Laignech''", pp. 1125-6. who was abbot of the monastery of Tír-Dá-Glas on the Shannon, now Terryglass (County Tipperary), and the last abbot of that house for whom we have any record. Internal evidence from the manuscript itself bears witness to Áed's involvement. His signature can be read on f. 32r (p. 313): ''Aed mac meic Crimthaind ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Triassic
The Triassic ( ) is a geologic period and system which spans 50.6 million years from the end of the Permian Period 251.902 million years ago ( Mya), to the beginning of the Jurassic Period 201.36 Mya. The Triassic is the first and shortest period of the Mesozoic Era. Both the start and end of the period are marked by major extinction events. The Triassic Period is subdivided into three epochs: Early Triassic, Middle Triassic and Late Triassic. The Triassic began in the wake of the Permian–Triassic extinction event, which left the Earth's biosphere impoverished; it was well into the middle of the Triassic before life recovered its former diversity. Three categories of organisms can be distinguished in the Triassic record: survivors from the extinction event, new groups that flourished briefly, and other new groups that went on to dominate the Mesozoic Era. Reptiles, especially archosaurs, were the chief terrestrial vertebrates during this time. A specialized subgroup of archo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Permian
The Permian ( ) is a geologic period and stratigraphic system which spans 47 million years from the end of the Carboniferous Period million years ago (Mya), to the beginning of the Triassic Period 251.9 Mya. It is the last period of the Paleozoic Era; the following Triassic Period belongs to the Mesozoic Era. The concept of the Permian was introduced in 1841 by geologist Sir Roderick Murchison, who named it after the region of Perm in Russia. The Permian witnessed the diversification of the two groups of amniotes, the synapsids and the sauropsids ( reptiles). The world at the time was dominated by the supercontinent Pangaea, which had formed due to the collision of Euramerica and Gondwana during the Carboniferous. Pangaea was surrounded by the superocean Panthalassa. The Carboniferous rainforest collapse left behind vast regions of desert within the continental interior. Amniotes, which could better cope with these drier conditions, rose to dominance in place of their am ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Erosion
Erosion is the action of surface processes (such as water flow or wind) that removes soil, rock, or dissolved material from one location on the Earth's crust, and then transports it to another location where it is deposited. Erosion is distinct from weathering which involves no movement. Removal of rock or soil as clastic sediment is referred to as ''physical'' or ''mechanical'' erosion; this contrasts with ''chemical'' erosion, where soil or rock material is removed from an area by dissolution. Eroded sediment or solutes may be transported just a few millimetres, or for thousands of kilometres. Agents of erosion include rainfall; bedrock wear in rivers; coastal erosion by the sea and waves; glacial plucking, abrasion, and scour; areal flooding; wind abrasion; groundwater processes; and mass movement processes in steep landscapes like landslides and debris flows. The rates at which such processes act control how fast a surface is eroded. Typically, physical erosion procee ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Granite
Granite () is a coarse-grained (phaneritic) intrusive igneous rock composed mostly of quartz, alkali feldspar, and plagioclase. It forms from magma with a high content of silica and alkali metal oxides that slowly cools and solidifies underground. It is common in the continental crust of Earth, where it is found in igneous intrusions. These range in size from dikes only a few centimeters across to batholiths exposed over hundreds of square kilometers. Granite is typical of a larger family of ''granitic rocks'', or ''granitoids'', that are composed mostly of coarse-grained quartz and feldspars in varying proportions. These rocks are classified by the relative percentages of quartz, alkali feldspar, and plagioclase (the QAPF classification), with true granite representing granitic rocks rich in quartz and alkali feldspar. Most granitic rocks also contain mica or amphibole minerals, though a few (known as leucogranites) contain almost no dark minerals. Granite is nearly alway ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Paleogene
The Paleogene ( ; British English, also spelled Palaeogene or Palæogene; informally Lower Tertiary or Early Tertiary) is a geologic period, geologic period and system that spans 43 million years from the end of the Cretaceous Period million years ago (annum, Mya) to the beginning of the Neogene Period Mya. It is the beginning of the Cenozoic Era of the present Phanerozoic Eon. The earlier term Tertiary Period was used to define the span of time now covered by the Paleogene Period and subsequent Neogene Period; despite no longer being recognised as a formal stratigraphy, stratigraphic term, 'Tertiary' is still widely found in earth science literature and remains in informal use. Paleogene is often abbreviated "Pg" (but the United States Geological Survey uses the abbreviation PE for the Paleogene on the Survey's geologic maps). During the Paleogene, evolution of mammals, mammals diversified from relatively small, simple forms into a large group of diverse animals in the wake of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dailly
Dailly ( gd, Dail Mhaol Chiarain) is a village in South Ayrshire, Scotland. It is located on the Water of Girvan, south of Maybole, and east of Old Dailly. "New Dailly", as it was originally known, was laid out in the 1760s as a coal-mining village. In 1849 a fire broke out in Maxwell Colliery, one of the nearby mines, and continued to burn for 50 years. Notable people *Thomas Thomson FRSE (1768-1852) antiquary and friend of Walter Scott * Hamilton Paul (1773–1854), Presbyterian minister, poet and writer *Thomas's younger brother, John Thomson of Duddingston FRSE (1778 – 1840) minister at Dailly 1800-1805 and artist *Hew Ainslie (1792–1878), poet * Anne Hepburn, missionary was born here in 1925Thanksgiving Service for the life of Anne Hepburn rder of Service Motherhood of God Papers, New College Library. (Mrs Hepburn's papers relating to the Motherhood of God Controversy were donated to New College Library in 2016). *Tommy Lawrence, footballer *Ross McCrorie, footballer ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Girvan
Girvan ( gd, Inbhir Gharbhain, "mouth of the River Girvan") is a burgh and harbour town in Carrick, South Ayrshire, Scotland. Girvan is situated on the east coast of the Firth of Clyde, with a population of about 6,450. It lies south of Ayr, and north of Stranraer, the main ferry port from Scotland to Northern Ireland. Deriving its name from the river which runs through the landscape the etymology of Girvan has possible Brythonic origins, related to the Welsh: ''Gearafon'' or ''Gwyrddafon'', "river flowing through the green flourishing place, from afon or avon, a river, and Gwyrdd, green, flourishing"). Prehistory and archaeology The earliest evidence of human habitation in the Girvan area dates to the Mesolithic. Between 1996 and 1998, archaeological investigations were undertaken by GUARD archaeology (then part of the University of Glasgow) as part of an expansion of the William Grant & Sons distillery. This work discovered several burnt mounds that dated to the lat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ailsa Craig OS OpenData Map
Ailsa may refer to: People *Ailsa (name), including a list of people with the name *Marquess of Ailsa, title in the Peerage of the United Kingdom created in 1831 Places *Ailsa Craig, an island in the outer Firth of Clyde, Scotland *Ailsa Craig, Ontario, North Middlesex, Ontario, Canada *Ailsa Craig (South Orkney Islands) *Ailsa Farms, New Jersey, U.S. Other uses * Ailsa (car) (1907–1910), car manufactured in Glasgow by Hugh Kennedy & Company * Ailsa Bay Distillery, a whisky distillery, co-located with the Girvan distillery and owned by William Grant & Sons * Ailsa Course, a golf course in Scotland, near Ailsa Craig * ''Ailsa'' (film), a 1994 Irish film *Ailsa Craig Engines, manufacturer of marine and specialist made to order engines from 1891 to 1972 *Ailsa Shipbuilding Company, shipbuilding company based in Troon, Scotland * Ailsa Stewart, fictional character in the Australian soap opera ''Home and Away'' *Volvo Ailsa B55, double-decker bus chassis built in Scotland *''Ailsa C ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Firth Of Forth
The Firth of Forth () is the estuary, or firth, of several Scottish rivers including the River Forth. It meets the North Sea with Fife on the north coast and Lothian on the south. Name ''Firth'' is a cognate of ''fjord'', a Norse word meaning a narrow inlet. ''Forth'' stems from the name of the river; this is ''*Vo-rit-ia'' (slow running) in Proto-Celtic, yielding '' Foirthe'' in Old Gaelic and '' Gweryd'' in Welsh. It was known as ''Bodotria'' in Roman times. In the Norse sagas it was known as the ''Myrkvifiörd''. An early Welsh name is ''Merin Iodeo'', or the "Sea of Iudeu". Geography and economy Geologically, the Firth of Forth is a fjord, formed by the Forth Glacier in the last glacial period. The drainage basin for the Firth of Forth covers a wide geographic area including places as far from the shore as Ben Lomond, Cumbernauld, Harthill, Penicuik and the edges of Gleneagles Golf Course. Many towns line the shores, as well as the petrochemical complexes at Gr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bass Rock
The Bass Rock, or simply the Bass (), ( gd, Creag nam Bathais or gd, Am Bas) is an island in the outer part of the Firth of Forth in the east of Scotland. Approximately offshore, and north-east of North Berwick, it is a steep-sided volcanic rock, at its highest point, and is home to a large colony of gannets. The rock is uninhabited, but historically has been settled by an early Christian hermit, and later was the site of an important castle, which after the Commonwealth period was used as a prison. The island belongs to Hew Hamilton-Dalrymple, whose family acquired it in 1706, and before to the Lauder family for almost six centuries. The Bass Rock Lighthouse was constructed on the rock in 1902, and the remains of an ancient chapel survive. The Bass Rock features in many works of fiction, including ''Catriona'' by Robert Louis Stevenson, ''The Lion Is Rampant'' by the Scottish novelist Ross Laidlaw and ''The New Confessions'' by William Boyd. Most recently it feature ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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