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List Of Volcanoes In Dominica
Dominica is an island-nation in the Caribbean that is part of the Lesser Antilles chain of islands. The island has active and extinct volcanoes. References {{Global Volcanism Program Dominica Volcanoes A volcano is a rupture in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface. On Earth, volcanoes are most often found where tectonic plates a ... Dominica ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dominica
Dominica ( or ; Kalinago: ; french: Dominique; Dominican Creole French: ), officially the Commonwealth of Dominica, is an island country in the Caribbean. The capital, Roseau, is located on the western side of the island. It is geographically situated as part of the Windward Islands chain in the Lesser Antilles archipelago in the Caribbean Sea. Dominica's closest neighbours are two constituent territories of the European Union, the overseas departments of France, Guadeloupe to the northwest and Martinique to the south-southeast. Dominica comprises a land area of , and the highest point is Morne Diablotins, at in elevation. The population was 71,293 at the 2011 census. The island was settled by the Arawak arriving from South America in the fifth century. The Kalinago displaced the Arawak by the 15th century. Columbus is said to have passed the island on Sunday, 3 November 1493. It was later colonised by Europeans, predominantly by the French from the 1690s to 1763. The Frenc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Caribbean
The Caribbean (, ) ( es, El Caribe; french: la Caraïbe; ht, Karayib; nl, De Caraïben) is a region of the Americas that consists of the Caribbean Sea, its islands (some surrounded by the Caribbean Sea and some bordering both the Caribbean Sea and the North Atlantic Ocean) and the surrounding coasts. The region is southeast of the Gulf of Mexico and the North American mainland, east of Central America, and north of South America. Situated largely on the Caribbean Plate, the region has more than 700 islands, islets, reefs and cays (see the list of Caribbean islands). Island arcs delineate the eastern and northern edges of the Caribbean Sea: The Greater Antilles and the Lucayan Archipelago on the north and the Lesser Antilles and the on the south and east (which includes the Leeward Antilles). They form the West Indies with the nearby Lucayan Archipelago (the Bahamas and Turks and Caicos Islands), which are considered to be part of the Caribbean despite not bordering the Caribbe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lesser Antilles
The Lesser Antilles ( es, link=no, Antillas Menores; french: link=no, Petites Antilles; pap, Antias Menor; nl, Kleine Antillen) are a group of islands in the Caribbean Sea. Most of them are part of a long, partially volcanic island arc between the Greater Antilles to the north-west and the continent of South America."West Indies." ''Merriam-Webster's Geographical Dictionary'', 3rd ed. 2001. () Springfield, MA: Merriam-Webster Inc., p. 1298. The islands of the Lesser Antilles form the eastern boundary of the Caribbean Sea where it meets the Atlantic Ocean. Together, the Lesser Antilles and the Greater Antilles make up the Antilles. (Somewhat confusingly, the word Caribbean is sometimes used to refer only to the Antilles, and sometimes used to refer to a much larger region.) The Lesser and Greater Antilles, together with the Lucayan Archipelago, are collectively known as the West Indies. History after European arrival The Spanish were the first Europeans to arrive on the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Volcanoes
A volcano is a rupture in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface. On Earth, volcanoes are most often found where tectonic plates are diverging or converging, and most are found underwater. For example, a mid-ocean ridge, such as the Mid-Atlantic Ridge, has volcanoes caused by divergent tectonic plates whereas the Pacific Ring of Fire has volcanoes caused by convergent tectonic plates. Volcanoes can also form where there is stretching and thinning of the crust's plates, such as in the East African Rift and the Wells Gray-Clearwater volcanic field and Rio Grande rift in North America. Volcanism away from plate boundaries has been postulated to arise from upwelling diapirs from the core–mantle boundary, deep in the Earth. This results in hotspot volcanism, of which the Hawaiian hotspot is an example. Volcanoes are usually not created where two tectonic plates slide pa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geographic Coordinates
The geographic coordinate system (GCS) is a spherical or ellipsoidal coordinate system for measuring and communicating positions directly on the Earth as latitude and longitude. It is the simplest, oldest and most widely used of the various spatial reference systems that are in use, and forms the basis for most others. Although latitude and longitude form a coordinate tuple like a cartesian coordinate system, the geographic coordinate system is not cartesian because the measurements are angles and are not on a planar surface. A full GCS specification, such as those listed in the EPSG and ISO 19111 standards, also includes a choice of geodetic datum (including an Earth ellipsoid), as different datums will yield different latitude and longitude values for the same location. History The invention of a geographic coordinate system is generally credited to Eratosthenes of Cyrene, who composed his now-lost ''Geography'' at the Library of Alexandria in the 3rd century ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Morne Aux Diables
Morne aux Diables, also known as Devil's Peak, is a volcano on the island of Dominica and the volcanic formation is the northernmost peak on the island. The volcano is considered dormant, with no unusual volcanic activity reported aside from a swarm of small earthquakes detected in 2009–2010. Sulfur springs are present near the volcano. See also * List of mountains of Dominica * List of volcanoes in Dominica References Mountains of Dominica Volcanoes of Dominica Inactive volcanoes Stratovolcanoes of North America {{Dominica-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Holocene
The Holocene ( ) is the current geological epoch. It began approximately 11,650 cal years Before Present (), after the Last Glacial Period, which concluded with the Holocene glacial retreat. The Holocene and the preceding Pleistocene together form the Quaternary period. The Holocene has been identified with the current warm period, known as MIS 1. It is considered by some to be an interglacial period within the Pleistocene Epoch, called the Flandrian interglacial.Oxford University Press – Why Geography Matters: More Than Ever (book) – "Holocene Humanity" section https://books.google.com/books?id=7P0_sWIcBNsC The Holocene corresponds with the rapid proliferation, growth and impacts of the human species worldwide, including all of its written history, technological revolutions, development of major civilizations, and overall significant transition towards urban living in the present. The human impact on modern-era Earth and its ecosystems may be considered of global si ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Morne Diablotins
Morne Diablotins is the highest mountain in Dominica, an island-nation in the Caribbean Lesser Antilles. It is the second highest mountain in the Lesser Antilles, after La Grande Soufrière in Guadeloupe. Morne Diablotins is located in the northern interior of the island, about north of Dominica's capital Roseau and about southeast of Portsmouth, the island's second-largest town. It is located within Morne Diablotin National Park. The mountain is volcanic, and last erupted c. 30,000 years ago. There are no known historical eruptions. The source of the Toulaman River lies in the mountain area. Morne Diablotins shares its name with the local term for the rare black-capped petrel (''Pterodroma hasitata''). See also * List of mountains of Dominica * List of volcanoes in Dominica Dominica is an island-nation in the Caribbean that is part of the Lesser Antilles chain of islands. The island has active and extinct volcanoes. References {{Global Volcanism Program ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Morne Plat Pays
Morne Plat Pays is a volcano on the island of Dominica. Located on the southern region of the island, the volcano last erupted around the year 1270 AD. Since the mid-18th century, a number of earthquake swarms have occurred near the mountain, but these are not related to Morne Plat Pays' eruptive activity. See also * List of mountains of Dominica * List of volcanoes in Dominica Dominica is an island-nation in the Caribbean that is part of the Lesser Antilles chain of islands. The island has active and extinct volcanoes. References {{Global Volcanism Program Dominica Volcanoes A volcano is a rupture in t ... References External links * Mountains of Dominica Volcanoes of Dominica Inactive volcanoes Stratovolcanoes of North America {{Dominica-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Morne Trois Pitons
Morne is an Old-French word for a small mountain. It may refer to: * Morne a Chandelle, a village in the Sud-Est department of Haiti * Morne-à-l'Eau, a commune in Guadeloupe * Morne Bois-Pin, the fourth highest mountain in Haiti * Morne la Vigie, hill and extinct cinder cone in Haiti * Morne Ciseaux, a town on the island of Saint Lucia * Morne Criquet, a quartier of Saint Barthélemy * Morne de Dépoudré, a quartier of Saint Barthélemy in the Caribbean * Morne de la Grande Montagne, the highest point of Saint Pierre and Miquelon * Morne Diablotins, the highest mountain in Dominica * Morne du Cibao, the third highest mountain in Haiti * Morne du Vitet, the highest point of Saint Barthélemy * Morne Docteur, a town in Saint George Parish, Grenada * Morne Fendue, a town in Saint Patrick Parish, Grenada * Morne Fortune, a hill and residential area located south of Castries, Saint Lucia * Morne Jaloux, a town in Saint George Parish, Grenada * Morne Jaloux Ridge, a town in S ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Morne Watt
Morne Watt or Watt Mountain is a mountain consisting of one or more stratovolcanoes at the south end of Dominica in the eastern Caribbean Sea. With an elevation of , it is the third highest mountain in Dominica after Morne Diablotins and Morne Trois Pitons. The mountain is home to the Boiling Lake and Valley of Desolation thermal areas, both of which are the best-known volcanic features in Dominica and major tourist attractions in Morne Trois Pitons National Park. Morne Watt was the source of a major eruption about 1,300 years ago that produced pyroclastic flows. A VEI-2 phreatic eruption occurred at the Valley of Desolation thermal area in 1880, which deposited ash away from the mountain. This was followed by a smaller VEI-1 phreatic eruption in July 1997. The 1880 and 1997 explosions are the only historically confirmed Dominican eruptions. See also *List of volcanoes in Dominica Dominica is an island-nation in the Caribbean that is part of the Lesser Antilles chain o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Volcanoes Of Dominica
A volcano is a rupture in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface. On Earth, volcanoes are most often found where tectonic plates are diverging or converging, and most are found underwater. For example, a mid-ocean ridge, such as the Mid-Atlantic Ridge, has volcanoes caused by divergent tectonic plates whereas the Pacific Ring of Fire has volcanoes caused by convergent tectonic plates. Volcanoes can also form where there is stretching and thinning of the crust's plates, such as in the East African Rift and the Wells Gray-Clearwater volcanic field and Rio Grande rift in North America. Volcanism away from plate boundaries has been postulated to arise from upwelling diapirs from the core–mantle boundary, deep in the Earth. This results in hotspot volcanism, of which the Hawaiian hotspot is an example. Volcanoes are usually not created where two tectonic plates slide ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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