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Gorumna
Gorumna () is an island on the west coast of Ireland, forming part of County Galway. Geography Gorumna Island is linked with the mainland through the Béal an Daingin Bridge. Gorumna properly consists of three individual islands in close proximity, Lettermullen, Teeranea (Irish: ''Tír an Fhia'') and Lettermore. Contribution to Irish traditional music During the 1860s in South Boston, Massachusetts, Bríd Ní Mháille, an immigrant from the Gorumna village of Trá Bhán, composed the Irish-language '' caoine'' '' Amhrán na Trá Bháine'', which is about the drowning of her three brothers, whose ''currach'' was rammed and sunk while they were out at sea. Ní Mháille's lament for her brothers was first performed at a ceilidh in South Boston before being brought back to her native district in Connemara, where it continues to be passed down as both a work of oral poetry and as a very popular song among performers and fans of Irish traditional music. Geology Gorumna Islan ...
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Garmna (Gorumna) Island Church - Geograph
Gorumna () is an island on the west coast of Ireland, forming part of County Galway. Geography Gorumna Island is linked with the mainland through the Béal an Daingin Bridge. Gorumna properly consists of three individual islands in close proximity, Lettermullen, Teeranea (Irish: ''Tír an Fhia'') and Lettermore. Contribution to Irish traditional music During the 1860s in South Boston, Massachusetts, Bríd Ní Mháille, an immigrant from the Gorumna village of Trá Bhán, composed the Irish-language '' caoine'' '' Amhrán na Trá Bháine'', which is about the drowning of her three brothers, whose ''currach'' was rammed and sunk while they were out at sea. Ní Mháille's lament for her brothers was first performed at a ceilidh in South Boston before being brought back to her native district in Connemara, where it continues to be passed down as both a work of oral poetry and as a very popular song among performers and fans of Irish traditional music. Geology Gorumna Islan ...
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Lettermullen
Lettermullen, ( or possibly "the hill with the mill"), is a small island and village on the coast of southern Connemara in County Galway, Ireland. It is about west of Galway city, at the far western end of Galway Bay, Lettermullen is the westernmost of three islands; Lettermullen, Gorumna and Lettermore, along with smaller islands collectively known as Ceantar na nOileán ("District of the Islands") connected to the mainland by the bridges and causeways of R374. Lettermullen is in the parish of Kilcummin, barony of Moycullen, and province of Connaught. It forms one side of Kiegall Bay, and its northern end is part of the shore of Casheen Bay. The island comprises about of arable and pasture land. The inhabitants are chiefly employed in herring and cod fisheries and in the collection of seaweed for manure. Lettermullen is part of the Gaeltacht (Irish-speaking region of Ireland) and Irish is the most common spoken language. Accordingly, its official name is ''Leitir Mealláin'' ...
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Lettermore
Lettermore () is a Gaeltacht village in County Galway, Ireland. It is also the name of an island, linked by road to the mainland, on which the village sits. The name comes from the Irish ''Leitir Móir'' meaning ''great rough hillside'' (''leitir'' = ''rough hillside''). The main spoken language of the area is Irish. Lettermore island is in two halves. The eastern half is known as Lettermore, while the western half is known as Lettercallow (''Leitir Calaidh'', "rough hillside by a marshy area").Census of Ireland, 1911: Area, Houses, and Population : Also the Ages, Civil Or Conjugal Condition, Occupations, Birthplaces, Religion, and Education of the People. United Kingdom, H.M. Stationery Office, 1912. Demographics See also * List of towns in the Republic of Ireland * Darach O'Cathain * Gorumna * CLG Naomh Anna, Leitir Móir * Fiachra Breathnach * Seoighe Inish Bearachain * Peigín Leitir Móir References See also * List of towns in the Republic of Ireland This is ...
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Atlantic Ocean
The Atlantic Ocean is the second-largest of the world's five oceans, with an area of about . It covers approximately 20% of Earth's surface and about 29% of its water surface area. It is known to separate the " Old World" of Africa, Europe and Asia from the "New World" of the Americas in the European perception of the World. The Atlantic Ocean occupies an elongated, S-shaped basin extending longitudinally between Europe and Africa to the east, and North and South America to the west. As one component of the interconnected World Ocean, it is connected in the north to the Arctic Ocean, to the Pacific Ocean in the southwest, the Indian Ocean in the southeast, and the Southern Ocean in the south (other definitions describe the Atlantic as extending southward to Antarctica). The Atlantic Ocean is divided in two parts, by the Equatorial Counter Current, with the North(ern) Atlantic Ocean and the South(ern) Atlantic Ocean split at about 8°N. Scientific explorations of the A ...
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Oral Poetry
Oral poetry is a form of poetry that is composed and transmitted without the aid of writing. The complex relationships between written and spoken literature in some societies can make this definition hard to maintain. Background Oral poetry is sometimes considered to include any poetry which is performed live. In many cultures, oral poetry overlaps with, or is identical with, song. Meanwhile, although the term oral etymologically means 'to do with the mouth', in some cultures oral poetry is also performed by other means, such as talking drums in some African cultures. Oral poetry exists most clearly within oral cultures, but it can survive, and indeed flourish, in highly literate cultures. Oral poetry differs from oral literature in general because oral literature encompasses linguistic registers which are not considered poetry. In most oral literature, poetry is defined by the fact that it conforms to metrical rules; examples of non-poetic oral literature in Western culture in ...
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Census
A census is the procedure of systematically acquiring, recording and calculating information about the members of a given population. This term is used mostly in connection with national population and housing censuses; other common censuses include censuses of agriculture, traditional culture, business, supplies, and traffic censuses. The United Nations (UN) defines the essential features of population and housing censuses as "individual enumeration, universality within a defined territory, simultaneity and defined periodicity", and recommends that population censuses be taken at least every ten years. UN recommendations also cover census topics to be collected, official definitions, classifications and other useful information to co-ordinate international practices. The UN's Food and Agriculture Organization (FAO), in turn, defines the census of agriculture as "a statistical operation for collecting, processing and disseminating data on the structure of agriculture, covering th ...
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Basalt
Basalt (; ) is an aphanite, aphanitic (fine-grained) extrusive igneous rock formed from the rapid cooling of low-viscosity lava rich in magnesium and iron (mafic lava) exposed at or very near the planetary surface, surface of a terrestrial planet, rocky planet or natural satellite, moon. More than 90% of all volcanic rock on Earth is basalt. Rapid-cooling, fine-grained basalt is chemically equivalent to slow-cooling, coarse-grained gabbro. The eruption of basalt lava is observed by geologists at about 20 volcanoes per year. Basalt is also an important rock type on other planetary bodies in the Solar System. For example, the bulk of the plains of volcanism on Venus, Venus, which cover ~80% of the surface, are basaltic; the lunar mare, lunar maria are plains of flood-basaltic lava flows; and basalt is a common rock on the surface of Mars. Molten basalt lava has a low viscosity due to its relatively low silica content (between 45% and 52%), resulting in rapidly moving lava flo ...
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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 ...
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Ordovician
The Ordovician ( ) is a geologic period and System (geology), system, the second of six periods of the Paleozoic Era (geology), Era. The Ordovician spans 41.6 million years from the end of the Cambrian Period million years ago (Mya) to the start of the Silurian Period Mya. The Ordovician, named after the Celtic Britons, Welsh tribe of the Ordovices, was defined by Charles Lapworth in 1879 to resolve a dispute between followers of Adam Sedgwick and Roderick Murchison, who were placing the same Rock (geology), rock beds in North Wales in the Cambrian and Silurian systems, respectively. Lapworth recognized that the fossil fauna in the disputed Stratum, strata were different from those of either the Cambrian or the Silurian systems, and placed them in a system of their own. The Ordovician received international approval in 1960 (forty years after Lapworth's death), when it was adopted as an official period of the Paleozoic Era by the International Union of Geological Sciences, Intern ...
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Silurian
The Silurian ( ) is a geologic period and system spanning 24.6 million years from the end of the Ordovician Period, at million years ago ( Mya), to the beginning of the Devonian Period, Mya. The Silurian is the shortest period of the Paleozoic Era. As with other geologic periods, the rock beds that define the period's start and end are well identified, but the exact dates are uncertain by a few million years. The base of the Silurian is set at a series of major Ordovician–Silurian extinction events when up to 60% of marine genera were wiped out. One important event in this period was the initial establishment of terrestrial life in what is known as the Silurian-Devonian Terrestrial Revolution: vascular plants emerged from more primitive land plants, dikaryan fungi started expanding and diversifying along with glomeromycotan fungi, and three groups of arthropods (myriapods, arachnids and hexapods) became fully terrestrialized. A significant evolutionary milestone during ...
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Caledonian Orogeny
The Caledonian orogeny was a mountain-building era recorded in the northern parts of the British Isles, the Scandinavian Mountains, Svalbard, eastern Greenland and parts of north-central Europe. The Caledonian orogeny encompasses events that occurred from the Ordovician to Early Devonian, roughly 490–390 million years ago ( Ma). It was caused by the closure of the Iapetus Ocean when the continents and terranes of Laurentia, Baltica and Avalonia collided. The orogeny is named for Caledonia, the Latin name for Scotland. The term was first used in 1885 by Austrian geologist Eduard Suess for an episode of mountain building in northern Europe that predated the Devonian period. Geologists like Émile Haug and Hans Stille saw the Caledonian event as one of several episodic phases of mountain building that had occurred during Earth's history. Current understanding has it that the Caledonian orogeny encompasses a number of tectonic phases that can laterally be diachronous. The n ...
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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 ...
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