テ四e De Groix
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テ四e De Groix
Groix (; br, Enez Groe) is an island and a commune in the Morbihan department of the region of Brittany in north-western France. Groix lies a few kilometres off the coast of Lorient. Several ferries a day run from Lorient to Groix. There are a few small towns on the island. High cliffs are on its north coast and sandy beaches in secluded coves on the south coast. Groix is also home to a wide variety of sea birds. Groix is also famous for hosting the only convex beach in Europe, which also moves following sea currents. During the last 15 years, the beach moved half a kilometer westbound. The geology of Groix is distinct from that of the nearby continent, and the east and south coasts have been designated a mineral nature reserve since 1982. More than 60 minerals can be found on the island, particularly blue glaucophane (observable on the surface), epidote or garnet. The island mainly consists of schist. A major naval battle between Britain and France took place off Groix in 17 ...
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Communes Of France
The () is a level of administrative division in the French Republic. French are analogous to civil townships and incorporated municipalities in the United States and Canada, ' in Germany, ' in Italy, or ' in Spain. The United Kingdom's equivalent are civil parishes, although some areas, particularly urban areas, are unparished. are based on historical geographic communities or villages and are vested with significant powers to manage the populations and land of the geographic area covered. The are the fourth-level administrative divisions of France. vary widely in size and area, from large sprawling cities with millions of inhabitants like Paris, to small hamlets with only a handful of inhabitants. typically are based on pre-existing villages and facilitate local governance. All have names, but not all named geographic areas or groups of people residing together are ( or ), the difference residing in the lack of administrative powers. Except for the municipal arrondi ...
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Schist
Schist ( ) is a medium-grained metamorphic rock showing pronounced schistosity. This means that the rock is composed of mineral grains easily seen with a low-power hand lens, oriented in such a way that the rock is easily split into thin flakes or plates. This texture (geology), texture reflects a high content of platy minerals, such as micas, talc, chlorite group, chlorite, or graphite. These are often interleaved with more granular minerals, such as feldspar or quartz. Schist typically forms during regional metamorphism accompanying the process of mountain building (orogeny) and usually reflects a medium Metamorphism#Metamorphic grades, grade of metamorphism. Schist can form from many different kinds of rocks, including sedimentary rocks such as mudstones and igneous rocks such as tuffs. Schist metamorphosed from mudstone is particularly common and is often very rich in mica (a ''mica schist''). Where the type of the original rock (the protolith) is discernible, the schist is us ...
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Islands Of Brittany
An island (or isle) is an isolated piece of habitat that is surrounded by a dramatically different habitat, such as water. Very small islands such as emergent land features on atolls can be called islets, skerries, cays or keys. An island in a river or a lake island may be called an eyot or ait, and a small island off the coast may be called a holm. Sedimentary islands in the Ganges delta are called chars. A grouping of geographically or geologically related islands, such as the Philippines, is referred to as an archipelago. There are two main types of islands in the sea: continental and oceanic. There are also artificial islands, which are man-made. Etymology The word ''island'' derives from Middle English ''iland'', from Old English ''igland'' (from ''ig'' or ''ieg'', similarly meaning 'island' when used independently, and -land carrying its contemporary meaning; cf. Dutch ''eiland'' ("island"), German ''Eiland'' ("small island")). However, the spelling of the word ...
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Yann-Ber Kalloc'h
Yann-Ber Kalloc'h (born ''Jean-Pierre Calloc'h'' in French; 21 July 1888 窶 10 April 1917) was a Breton war poet who wrote in both Breton and French. Life Yann-Ber Kalloc'h was born on the island of Groix, near Lorient, on July 24, 1888. He was the son of a fisherman (who was lost at sea in October 1902) and his wife. He describes his childhood in the autobiographical poem ''Me 'zo Ganet kreiz ar e mor'' '. Kalloc'h at first wanted to become a Roman Catholic priest and entered the minor seminary of Sainte Anne d'Auray in 1900, then the major seminary at Vannes in October 1905. He was forced to renounce his vocation after his two sisters and his younger brother revealed signs of mental illness, since canon law forbade the priesthood to those who had relatives suffering from such diseases. Yann-Ber had dreamed of being a missionary and his exclusion from the priesthood brought him great distress. He became tutor in various cities including Paris. During military service, Yann- ...
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Communes Of The Morbihan Department
The following is a list of the 249 communes of the Morbihan department of France. The communes cooperate in the following intercommunalities (as of 2022):BANATIC
Pテゥrimティtre des EPCI テ fiscalitテゥ propre. Accessed 15 March 2022.
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Battle Of Groix
The Battle of Groix was a large naval engagement which took place near the island of Groix off the Biscay coast of Brittany on 23 June 1795 ( 5 messidor an III) during the French Revolutionary Wars. The battle was fought between elements of the British Channel Fleet and the French Atlantic Fleet, which were cruising in the region on separate missions. The British fleet, commanded by Admiral Lord Bridport, was covering an invasion convoy carrying a French Royalist army to invade Quiberon, while the French under Vice-admiral Villaret de Joyeuse had sailed a week earlier to rescue a French convoy from attack by a British squadron. The French fleet had driven off the British squadron in a battle on 17 June known as Cornwallis's Retreat, and were attempting to return to their base at Brest when Bridport's force of 14 ships of the line appeared on 22 June. Villaret, believing that the stronger British fleet would destroy his own 12 ships of the line, ordered his force to fall back t ...
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First French Republic
In the history of France, the First Republic (french: Premiティre Rテゥpublique), sometimes referred to in historiography as Revolutionary France, and officially the French Republic (french: Rテゥpublique franテァaise), was founded on 21 September 1792 during the French Revolution. The First Republic lasted until the declaration of the First Empire on 18 May 1804 under Napolテゥon Bonaparte, although the form of the government changed several times. This period was characterized by the fall of the monarchy, the establishment of the National Convention and the Reign of Terror, the Thermidorian Reaction and the founding of the Directory, and, finally, the creation of the Consulate and Napoleon's rise to power. End of the monarchy in France Under the Legislative Assembly, which was in power before the proclamation of the First Republic, France was engaged in war with Prussia and Austria. In July 1792, the Duke of Brunswick, commanding general of the Austro窶撤russian Army, issued his Bru ...
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Kingdom Of Great Britain
The Kingdom of Great Britain (officially Great Britain) was a Sovereign state, sovereign country in Western Europe from 1 May 1707 to the end of 31 December 1800. The state was created by the 1706 Treaty of Union and ratified by the Acts of Union 1707, which united the kingdoms of Kingdom of England, England (which included Wales) and Kingdom of Scotland, Scotland to form a single kingdom encompassing the whole island of Great Britain and its outlying islands, with the exception of the Isle of Man and the Channel Islands. The unitary state was governed by a single Parliament of Great Britain, parliament at the Palace of Westminster, but distinct legal systems 窶 English law and Scots law 窶 remained in use. The formerly separate kingdoms had been in personal union since the 1603 "Union of the Crowns" when James VI of Scotland became King of England and King of Ireland. Since James's reign, who had been the first to refer to himself as "king of Great Britain", a political un ...
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Garnet
Garnets () are a group of silicate minerals that have been used since the Bronze Age as gemstones and abrasives. All species of garnets possess similar physical properties and crystal forms, but differ in chemical composition. The different species are pyrope, almandine, spessartine, grossular (varieties of which are hessonite or cinnamon-stone and tsavorite), uvarovite and andradite. The garnets make up two solid solution series: pyrope-almandine-spessartine (pyralspite), with the composition range ; and uvarovite-grossular-andradite (ugrandite), with the composition range . Etymology The word ''garnet'' comes from the 14th-century Middle English word ''gernet'', meaning 'dark red'. It is borrowed from Old French ''grenate'' from Latin ''granatus,'' from ''granum'' ('grain, seed'). This is possibly a reference to ''mela granatum'' or even ''pomum granatum'' ('pomegranate', ''Punica granatum''), a plant whose fruits contain abundant and vivid red seed covers ( arils), whic ...
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Lorient Agglomテゥration
Communautテゥ d'agglomテゥration Lorient Agglomテゥration is the ''communautテゥ d'agglomテゥration'', an intercommunal structure, centred on the city of Lorient. It is located in the Morbihan department, in the Brittany region, northwestern France. It was created in January 2014.CA Lorient Agglomテゥration (Nツー SIREN : 200042174)
BANATIC, accessed 6 April 2022.
Its area is 738.7 km2. Its area is 666.7 km2. Its population was 204,107 in 2018, of which 57,084 in Lorient proper.Comparateur de territoire
INSEE, accessed 6 April 2022.


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Epidote
Epidote is a calcium aluminium iron sorosilicate mineral. Description Well developed crystals of epidote, Ca2Al2(Fe3+;Al)(SiO4)(Si2O7)O(OH), crystallizing in the monoclinic system, are of frequent occurrence: they are commonly prismatic in habit, the direction of elongation being perpendicular to the single plane of symmetry. The faces are often deeply striated and crystals are often twinned. Many of the characters of the mineral vary with the amount of iron present for instance, the color, the optical constants, and the specific gravity. The color is green, grey, brown or nearly black, but usually a characteristic shade of yellowish-green or pistachio-green. It displays strong pleochroism, the pleochroic colors being usually green, yellow and brown. Clinozoisite is green, white or pale rose-red group species containing very little iron, thus having the same chemical composition as the orthorhombic mineral zoisite. The name, due to Haテシy, is derived from the Greek word "epidos ...
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Glaucophane
Glaucophane is the name of a mineral and a mineral group belonging to the sodic amphibole supergroup of the double chain inosilicates, with the chemical formula 笘侵a2(Mg3Al2)Si8O22(OH)2. Glaucophane crystallizes in the monoclinic system. Name Glaucophane is named for its typical blue color. In Greek, ''glaucophane'' means "blue appearing". As the major mineral component, it is glaucophane's color that gives the "blueschist" metamorphic rock type its name. Characteristics The blue color is very diagnostic for this species. Glaucophane, along with the closely related mineral riebeckite, to which it forms a series with, and their intermediate crossite, are the only well known amphiboles that are commonly blue. Glaucophane forms a solid solution series with ferroglaucophane (). Glaucophane is the magnesium-rich endmember and ferroglaucophane is the iron-rich endmember. Ferroglaucophane is similar to glaucophane but is slightly denser and hence increased specific gravity. The two ...
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