2004 Les Saintes Earthquake
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2004 Les Saintes Earthquake
The 2004 Les Saintes earthquake occurred at on November 21, 2004 with a moment magnitude of 6.3 and maximum European macroseismic intensity of VIII (''Heavily damaging''). The shock was named for Îles des Saintes "Island of the Saints", a group of small islands to the south of Guadeloupe, which is an overseas department of France. Although it occurred near the Lesser Antilles subduction zone, this was an intraplate, normal fault event. It resulted in one death, 13 injuries, and 40 people being made homeless, but the overall damage was considered moderate. A small, nondestructive tsunami was reported, but run-up and inundation distances were difficult to measure due to a storm that occurred on the day of the event. Unusual effects at a volcanic lake on Dominica were also documented, and an aftershock caused additional damage three months later. Tectonic setting While the northern and southern boundaries of the Caribbean Plate are complex and diffuse, with zones of seismici ...
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Fault (geology)
In geology, a fault is a planar fracture or discontinuity in a volume of rock across which there has been significant displacement as a result of rock-mass movements. Large faults within Earth's crust result from the action of plate tectonic forces, with the largest forming the boundaries between the plates, such as the megathrust faults of subduction zones or transform faults. Energy release associated with rapid movement on active faults is the cause of most earthquakes. Faults may also displace slowly, by aseismic creep. A ''fault plane'' is the plane that represents the fracture surface of a fault. A ''fault trace'' or ''fault line'' is a place where the fault can be seen or mapped on the surface. A fault trace is also the line commonly plotted on geologic maps to represent a fault. A ''fault zone'' is a cluster of parallel faults. However, the term is also used for the zone of crushed rock along a single fault. Prolonged motion along closely spaced faults can blur the ...
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Fault Scarp
A fault scarp is a small step or offset on the ground surface where one side of a fault has moved vertically with respect to the other. It is the topographic expression of faulting attributed to the displacement of the land surface by movement along faults. They are exhibited either by differential movement and subsequent erosion along an old ''inactive'' geologic fault (a sort of old rupture), or by a movement on a recent active fault. Characteristics Fault scarps often contain highly fractured rock of both hard and weak consistency. In many cases, bluffs form from the upthrown block and can be very steep. The height of the scarp formation is equal to the vertical displacement along the fault. Active scarps are usually formed by tectonic displacement, e.g. when an earthquake changes the elevation of the ground and can be caused by any type of fault, including strike-slip faults, whose motion is primarily horizontal. This movement is usually episodic, with the height of the bluf ...
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Christmas Day
Christmas is an annual festival commemorating the birth of Jesus Christ, observed primarily on December 25 as a religious and cultural celebration among billions of people around the world. A feast central to the Christian liturgical year, it is preceded by the season of Advent or the Nativity Fast and initiates the season of Christmastide, which historically in the West lasts twelve days and culminates on Twelfth Night. Christmas Day is a public holiday in many countries, is celebrated religiously by a majority of Christians, as well as culturally by many non-Christians, and forms an integral part of the holiday season organized around it. The traditional Christmas narrative recounted in the New Testament, known as the Nativity of Jesus, says that Jesus was born in Bethlehem, in accordance with messianic prophecies. When Joseph and Mary arrived in the city, the inn had no room and so they were offered a stable where the Christ Child was soon born, with angels proclaim ...
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Stratovolcano
A stratovolcano, also known as a composite volcano, is a conical volcano built up by many layers (strata) of hardened lava and tephra. Unlike shield volcanoes, stratovolcanoes are characterized by a steep profile with a summit crater and periodic intervals of explosive eruptions and effusive eruptions, although some have collapsed summit craters called calderas. The lava flowing from stratovolcanoes typically cools and hardens before spreading far, due to high viscosity. The magma forming this lava is often felsic, having high-to-intermediate levels of silica (as in rhyolite, dacite, or andesite), with lesser amounts of less-viscous mafic magma. Extensive felsic lava flows are uncommon, but have travelled as far as . Stratovolcanoes are sometimes called composite volcanoes because of their composite stratified structure, built up from sequential outpourings of erupted materials. They are among the most common types of volcanoes, in contrast to the less common shield volca ...
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La Grande Soufrière
La Grande Soufrière ( en, "big sulfur outlet"), is an active stratovolcano on the French island of Basse-Terre, in Guadeloupe. It is the highest mountain peak in the Lesser Antilles, rising 1,467 m high. The last magmatic eruption was in 1580±50 during which the current lava dome was emplaced. More recent eruptions have been phreatic in type. On February 8, 1843, an eruption of La Grande Soufrière caused by an earthquake killed over 5,000 people. Significant seismic activity in 1976 led to a mass evacuation of the island's 72,000 residents. There was a bitter, and well-publicized, controversy between scientists Claude Allègre and Haroun Tazieff on whether evacuation should occur. Allègre held that inhabitants should be evacuated, just in case, while Tazieff held that the ''Soufrière'' was harmless. The prefect decided to evacuate, erring on the side of covering his back. The volcano erupted on August 30, 1976, but much less severely than predicted by the Allègre side ...
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Bureau De Recherches Géologiques Et Minières
Bureau ( ) may refer to: Agencies and organizations * Government agency *Public administration * News bureau, an office for gathering or distributing news, generally for a given geographical location * Bureau (European Parliament), the administrative organ of the Parliament of the European Union * Federal Bureau of Investigation, the leading internal law enforcement agency in the United States * Service bureau, a company which provides business services for a fee * Citizens Advice Bureau, a network of independent UK charities that give free, confidential help to people for money, legal, consumer and other problems Furniture * Desk, a piece of furniture, typically a table used for office work * Chest of drawers, a piece of furniture that has multiple, stacked, parallel drawers Geography * Bureau County, Illinois * Bureau Lake, a body of water in the Gouin Reservoir, in Quebec, Canada People * Bernard Béréau (1940–2005), French footballer * Bernard Bureau (born 1959), Fre ...
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Saint-Louis, Guadeloupe
Saint-Louis is a commune in the overseas department of Guadeloupe. Saint-Louis lies on the north of the island of Marie-Galante, and is the island's largest commune. Many beaches lie on the west coast of the commune. Population Education Public preschools and primary schools include:LISTE DES ECOLES PUBLIQUES ET PRIVEES SOUS CONTRAT
" . Retrieved on 10 March 2018.
* Ecole primaire Léopold Lubino * Ecole maternelle Guy Dramort Public junior high schools include:Établissements du 2nd degré PUBLIC 2017-2018 ...
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Color-tagged Structure
A color-tagged structure is a structure which has been classified by a color to represent the severity of damage or the overall condition of the building. The exact definition for each color may be different in different countries and jurisdictions. A structure has been severely damaged to the degree that the structure is too dangerous to inhabit. Similarly, a structure is if it has been moderately damaged to the degree that its habitability is limited (only during the day, for example). A structure may mean the building is either undamaged or has suffered slight damage, although differences exist at local levels when to use a green tag. Tagging is performed by government building officials, or, occasionally during disasters, by engineers deputized by the building official. Natural disasters such as earthquakes, floods and mudslides are among the most common causes of a building being red-, yellow- or green-tagged. Usually, after such incidents, the local government Local ...
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Marie-Galante
Marie-Galante ( gcf, label=Antillean Creole, Mawigalant) is one of the islands that form Guadeloupe, an overseas department of France. Marie-Galante has a land area of . It had 11,528 inhabitants at the start of 2013, but by the start of 2018 the total was officially estimated to be 10,655, with a population density of . Administration Marie-Galante is divided into three communes (with populations at 1 January 2013): * Grand-Bourg (5,564 residents), * Capesterre-de-Marie-Galante (3,389) and * Saint-Louis (2,575). These three communes formed an intercommunal entity in 1994: the Community of Communes of Marie-Galante (french: communauté de communes de Marie-Galante). This is the oldest intercommunal structure of the overseas regions of France. History The Huecoids are the oldest known civilizations to have occupied Marie-Galante, followed by Arawaks, and then by the Island Caribs circa 850. The island was called ''Aichi'' by the Caribs and ''Touloukaera'' by the Arawak ...
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Grand-Bourg
Grand-Bourg is a commune on the island of Marie-Galante, in the French overseas region and department of Guadeloupe in the Lesser Antilles Caribbean. It is located in the southwest of Marie-Galante, and is the most populous of the three communes on the island. Grand-Bourg hosts the headquarters of the communal association of Marie-Galante. The Marie-Galante Airfield is located in Grand-Bourg. History The Marais Folle Anse, a vast fresh water reserve, allowed habitation by native Arawaks at the beginning of the 1st millennium. It is possible that Christopher Columbus visited in 1493 during his second voyage. In 1653, a fort was established by French colonists. Geography Grand-Bourg is located at the south-west of the island of Marie-Galante and is the location of the chief town. The co-ordinates are 15° 53'N and 61° 19'W. The major part of the commune consists of an undulating plateau. It is dominated by a broad littoral plain and mangrove forest in the north, with broad bea ...
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Petite-Anse, Les Saintes
Petite-Anse is a ''quartier'' of Terre-de-Bas Island, located in Îles des Saintes archipelago in the Caribbean. It is located in the western part of the island. The commercial activity of the island are focused on this village, shops, market, bakeries, groceries, restaurants, and bars. It hosts the majority of the administrative office of the island, the Post office, the community clinic, and the ''Mairie'' (City hall) of Terre-de-Bas Terre-de-Bas (; gcf, label=Antillean Creole, Tèdéba) is a commune in the French overseas department and region of Guadeloupe, in the Lesser Antilles. Terre-de-Bas is made up of Terre-de-Bas Island and several uninhabited islands and islets in .... Attractions *The square of ''9 août 1882'': The main place of the quartier, located in front the city hall. It is a lively and flowery place. *Saint-Nicholas' church: An ancient Roman Catholic church. The front of the church was rebuilt after its collapsing because of the earthquake of 21 November ...
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Terre-de-Bas
Terre-de-Bas (; gcf, label=Antillean Creole, Tèdéba) is a commune in the French overseas department and region of Guadeloupe, in the Lesser Antilles. Terre-de-Bas is made up of Terre-de-Bas Island and several uninhabited islands and islets in the group of Les Saintes islands, to the southwest of Guadeloupe's mainland. Education Public preschools and primary schools:LISTE DES ECOLES PUBLIQUES ET PRIVEES SOUS CONTRAT
" . Retrieved on 10 March 2018.
* Ecole primaire Petites Anses * Ecole maternelle Grande Anse


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