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Islet
An islet ( ) is generally a small island. Definitions vary, and are not precise, but some suggest that an islet is a very small, often unnamed, island with little or no vegetation to support human habitation. It may be made of rock, sand and/or hard coral; may be permanent or tidal (i.e. surfaced reef or seamount); and may exist in the sea, lakes, rivers or any other sizeable bodies of water. Definition As suggested by its origin ''islette'', an Old French diminutive of "isle", use of the term implies small size, but little attention is given to drawing an upper limit on its applicability. The World Landforms website says, "An islet landform is generally considered to be a rock or small island that has little vegetation and cannot sustain human habitation", and further that size may vary from a few square feet to several square miles, with no specific rule pertaining to size. Other terms * Ait (/eɪt/, like eight) or eyot (/aɪ(ə)t, eɪt/), a small island. It is espe ...
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Rockall - Geograph
Rockall () is a high, uninhabitable granite islet in the North Atlantic Ocean. It is west of Soay, St Kilda, Scotland; northwest of Tory Island, Republic of Ireland, Ireland; and south of Iceland. The nearest permanently inhabited place is North Uist, east in Scotland's Outer Hebrides. Rockall was formed during the Paleogene period by magmatism, as part of the North Atlantic Igneous Province. Rockall's only named geographic location and occupiable area is Hall's Ledge. Rockall and Hasselwood Rock 200 metres North, are the only emergent parts of Helen's Reef and the Rockall Plateau. Rockall has appeared on maps since at least 1550 and in literature since at least 1698. Marine surveyors, scientists, adventurers, amateur radio operators and environmental activists, have variously landed on and/or briefly occupied the islet. The earliest documented landing on Rockall was in 1811 by a small Royal Navy party led by Basil Hall. The longest known continuous occupation is 45 days, ...
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Les Houmets
Les Houmets are tidal islands to the east of Guernsey in the Channel Islands. Their name derives from a diminutive of '' hou'', a Norman/Guernésiais word meaning islets. Among the islets are Houmet Benest/Houmet Benêt, Houmet Paradis and Houmet Hommetol (Omptolle). Although Victor Hugo suggests that they were heavily eroded by quarrying (which was certainly true in the case of Crevichon off Herm), Victor Coysh disagrees saying: Victor Hugo Victor Hugo who wrote about many of the Channel Islands in his books, described Les Houmets, in his work '' The Toilers of the Sea'' (''Les Travailleurs de la mer''). Gilliat, the main character lives on Houmet Paradis: :"This house was called the Bû de la Rue. It was situated on the point of a tongue of land, or rather of rock, that made a little separate harbour in the creek of Houmet Paradis. The water was very deep here. This house was all alone on the point, almost off the land, with just enough land for a small garden. The high ...
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Écréhous
The Écréhous (; or in Jèrriais: ''Êcrého'') are a group of islands and rocks situated north-east of Jersey, and from France. They form part of the Bailiwick of Jersey and are administratively part of the Parish of St Martin. Etymology The name 'Ecrehous' is Norse in origin. "Esker" as in Skerry meaning a stony bank and ' Hou', the toponym found also in Jethou, Lihou, Brecqhou, Burhou and other islets, derives from ''holm'', meaning ''island''. The first part of the name appears to be traced back to the Norse word ''sker'', meaning ''reef''. The Ecrehous are actually, geologically, part of the same island group as Les Dirouilles (west) and Les Pierres de Lecq ('the Paternosters') (further west). Islets The most significant islets in the group are: *Maîtr'Île *La Marmotchiéthe ('La Marmotière' in gallicized form) *Lé Bliantch'Île (''La Blanche Île'' in gallicized form); others include: *Les D'mies *La Grand' Naithe *L'Etchièrviéthe *Lé Fou *La Froutchie Al ...
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Channel Islands
The Channel Islands are an archipelago in the English Channel, off the French coast of Normandy. They are divided into two Crown Dependencies: the Jersey, Bailiwick of Jersey, which is the largest of the islands; and the Bailiwick of Guernsey, consisting of Guernsey, Alderney, Sark, Herm and some smaller islands. Historically, they are the remnants of the Duchy of Normandy. Although they are not part of the United Kingdom, the UK is responsible for the defence and international relations of the islands as it is for the other Crown Dependency, the Isle of Man, and the British Overseas Territories. The Crown Dependencies are neither members of the Commonwealth of Nations, nor part of the European Union. They have a total population of about , and the bailiwicks' Capital city, capitals, Saint Helier and Saint Peter Port, have populations of 33,500 and 18,207 respectively. "Channel Islands" is a geographical term, not a political unit. The two bailiwicks have been administered sepa ...
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Caribbean
The Caribbean ( , ; ; ; ) is a region in the middle of the Americas centered around the Caribbean Sea in the Atlantic Ocean, North Atlantic Ocean, mostly overlapping with the West Indies. Bordered by North America to the north, Central America to the west, and South America to the south, it comprises numerous List of Caribbean islands, islands, cays, islets, reefs, and banks. It includes the Lucayan Archipelago, Greater Antilles, and Lesser Antilles of the West Indies; the Quintana Roo Municipalities of Quintana Roo#Municipalities, islands and Districts of Belize#List, Belizean List of islands of Belize, islands of the Yucatán Peninsula; and the Bay Islands Department#Islands, Bay Islands, Miskito Cays, Archipelago of San Andrés, Providencia and Santa Catalina, Archipelago of San Andrés, Providencia, and Santa Catalina, Corn Islands, and San Blas Islands of Central America. It also includes the coastal areas on the Mainland, continental mainland of the Americas bordering the ...
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Lihou
Lihou () is a small tidal island just off the west coast of the island of Guernsey, in the English Channel, between Great Britain and France. Administratively, Lihou forms part of the Parish of St Peter's in the Bailiwick of Guernsey, and is now owned by the parliament of Guernsey (the States of Guernsey), although there have been a number of owners in the past. Since 2006 the island has been jointly managed by the Guernsey Environment Department and the Lihou Charitable Trust. In the past the island was used by locals for the collection of seaweed for use as a fertiliser, but today Lihou is mainly used for tourism, including school trips. Lihou is also an important centre for conservation, forming part of a Ramsar wetland site for the preservation of rare birds and plants as well as historic ruins of a priory and a farmhouse. Etymology In common with several nearby islands, such as Jethou and Brecqhou, the name contains the Norman suffix '' -hou'', which means a small hil ...
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Tatihou
Tatihou is an islet of Normandy in France with an area of . It is located to the east of the Cotentin peninsula just off the coast near Saint-Vaast-la-Hougue. It is almost uninhabited, and is usually reached by amphibious craft although, being a tidal island, it is also possible to walk there over the local oyster beds at low tide. Access to the island is limited to 500 visitors per day. History Tatihou, like many of the islets of the Channel Islands contains the ''-hou'' suffix. In 1692 the naval Battle of La Hougue took place between the English and the French close to the island of Tatihou. In 1756 the surroundings of La Hougue were defended by many batteries and forts, but the lack of regular maintenance ensured that these quickly fell into disrepair. In 1720 Tatihou was used for Quarantine, quarantining plague victims from Marseille. On 10 December 1803, the 36-gun frigate HMS Shannon (1803), HMS ''Shannon'' grounded on Tatihou. All her crew survived to be captured by troo ...
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Reef
A reef is a ridge or shoal of rock, coral, or similar relatively stable material lying beneath the surface of a natural body of water. Many reefs result from natural, abiotic component, abiotic (non-living) processes such as deposition (geology), deposition of sand or wave erosion planning down rock outcrops. However, reefs such as the coral reefs of tropical waters are formed by biotic component, biotic (living) processes, dominated by corals and coralline algae. Artificial reefs, such as shipwrecks and other man-made underwater structures, may occur intentionally or as the result of an accident. These are sometimes designed to increase the physical complexity of featureless sand bottoms to attract a more diverse range of organisms. They provide shelter to various aquatic animals which help prevent extinction. Another reason reefs are put in place is for aquaculture, and fish farmers who are looking to improve their businesses sometimes invest in them. Reefs are often quite n ...
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River Thames
The River Thames ( ), known alternatively in parts as the The Isis, River Isis, is a river that flows through southern England including London. At , it is the longest river entirely in England and the Longest rivers of the United Kingdom, second-longest in the United Kingdom, after the River Severn. The river rises at Thames Head in Gloucestershire and flows into the North Sea near Tilbury, Essex and Gravesend, Kent, via the Thames Estuary. From the west, it flows through Oxford (where it is sometimes called the Isis), Reading, Berkshire, Reading, Henley-on-Thames and Windsor, Berkshire, Windsor. The Thames also drains the whole of Greater London. The lower Reach (geography), reaches of the river are called the Tideway, derived from its long Tidal river, tidal reach up to Teddington Lock. Its tidal section includes most of its London stretch and has a rise and fall of . From Oxford to the estuary, the Thames drops by . Running through some of the drier parts of mainland Bri ...
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-hou
''-hou'' or ''hou'' is a place-name element found commonly in the Norman toponymy of the Channel Islands and continental Normandy. Etymology and signification Its etymology and meaning are disputed, but most specialists think it comes from Saxon or Anglo-Saxon ''hōh'' "heel", sometimes ''hō'', then "heel-shaped promontory", "rocky steep slope", "steep shore". This toponymic appellative appears as a final ''-hou'' or associated with the Romance definite article ''le Hou''. It can be found everywhere in Normandy, but more in the western part of it. The English toponymy uses this Saxon or Anglo-Saxon element the same way, but its result is phonetically ''-hoo'' or ''-hoe'', sometimes ''-(h)ow'' or ''-ho'' e. g. : Northoo (Suffolk); Poddinghoo (Worcestershire); Millhoo (Essex); Fingringhoe (Essex); Rainow (Cheshire); Soho (London); etc. Eilert Ekwall, ''The Concise Oxford Dictionary of English Place-names'' (4th edition), Oxford University Press, Oxford, 1960, p. 244b. As ...
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Bahamas
The Bahamas, officially the Commonwealth of The Bahamas, is an archipelagic and island country within the Lucayan Archipelago of the Atlantic Ocean. It contains 97 per cent of the archipelago's land area and 88 per cent of its population. It comprises more than 3,000 islands, cays and islets in the Atlantic Ocean, and is located north of Cuba and north-west of the island of Hispaniola (split between the Dominican Republic and Haiti) and the Turks and Caicos Islands, southeast of the U.S. state of Florida and east of the Florida Keys. The capital and largest city is Nassau on the island of New Providence. The Royal Bahamas Defence Force describes the Bahamas' territory as encompassing of ocean space. The Bahama islands were inhabited by the Arawak and Lucayans, a branch of the Arawakan- speaking Taíno, for many centuries. Christopher Columbus was the first European to see the islands, making his first landfall in the "New World" in 1492 when he landed on the ...
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Seamount
A seamount is a large submarine landform that rises from the ocean floor without reaching the water surface (sea level), and thus is not an island, islet, or cliff-rock. Seamounts are typically formed from extinct volcanoes that rise abruptly and are usually found rising from the seafloor to in height. They are defined by oceanographers as independent features that rise to at least above the seafloor, characteristically of conical form.IHO, 2008. Standardization of Undersea Feature Names: Guidelines Proposal form Terminology, 4th ed. International Hydrographic Organization and Intergovernmental Oceanographic Commission, Monaco. The peaks are often found hundreds to thousands of meters below the surface, and are therefore considered to be within the deep sea. During their evolution over geologic time, the largest seamounts may reach the sea surface where wave action erodes the summit to form a flat surface. After they have subsided and sunk below the sea surface, such flat-top ...
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