Use of the term
Tulane University professor Rosanne Adderly says:
The term "West Indies" was used by the British Europeans to describe the British West Indies their own acquired territories in the Americas... In the 1950s the British sought to unify all of its Anglo-caribbean colonies into one nation , the "West Indies" collective British Caribbean colonies which also includes Guyana and Belize which is geographically located in South America but is apart of the British West Indies, the British made their greatest political attempt to solidify the unification of their colonies into one independent nation in the 1950s with the creation of The West Indies Federation, the federation collapsed [in the early 1960s], however they decided to form CARICOM The Caribbean Community organisation or CC and the majority of the British colonies became independent except for four colonies and they all become apart of the British Commonwealth nations ... the West Indies continues to field a powerful cricket team for international competition.
The West Indies is a region of the North Atlantic Ocean and the Caribbean that includes the island countries and surrounding waters of three major archipelagos: the Greater Antilles, the Lesser Antilles, and the Lucayan Archipelago.
The region includes all the islands in or bordering the Caribbean Sea, plus The Bahamas and the Turks and Caicos Islands, which are in the Atlantic Ocean. The West Indies includes Anglophone nations of northern South America that share the history, demographic population and culture of the British West Indies islands.
Indigenous peoples were the first inhabitants of the West Indies. In 1492, Christopher Columbus became the first European to arrive at the islands, where he is believed by historians to have first set foot on land in the Bahamas. After the first of the voyages of Christopher Columbus to the Americas, Europeans began to use the term West Indies to distinguish the region from the East Indies of South Asia and Southeast Asia.
In the late sixteenth century, French, English and Dutch merchants and privateers began their operations in the Caribbean Sea, attacking Spanish and Portuguese shipping and coastal areas. They often took refuge and refitted their ships in the areas the Spanish could not conquer, including the islands of the Lesser Antilles, the northern coast of South America including the mouth of the Orinoco, and the Atlantic Coast of Central America. In the Lesser Antilles they managed to establish a foothold following the colonisation of St Kitts in 1624 and Barbados in 1626, and when the Sugar Revolution took off in the mid-seventeenth century, they brought in thousands of Africans to work the fields and mills as slave labourers. These Africans wrought a demographic revolution, replacing or joining with either the indigenous Caribs or the European settlers who were there as indentured servants.
The struggle between the northern Europeans and the Spanish spread southward in the mid to late seventeenth century, as English, Dutch, French and Spanish colonists, and in many cases their slaves from Africa first entered and then occupied the coast of The Guianas (which fell to the French, English and Dutch) and the Orinoco valley, which fell to the Spanish. The Dutch, allied with the Caribs of the Orinoco, would eventually carry the struggles deep into South America, first along the Orinoco and then along the northern reaches of the Amazon.
Since no European country had occupied much of Central America, gradually the English of Jamaica established alliances with the Miskito Kingdom of modern-day Nicaragua and Honduras, and then began logging on the coast of modern-day Belize. These interconnected commercial and diplomatic relations made up the Western Caribbean Zone which was in place in the early eighteenth century. In the Miskito Kingdom, the rise to power of the Miskito-Zambos, who originated in the survivors of a rebellion aboard a slave ship in the 1640s and the introduction of African slaves by British settlers within the Miskito area and in Belize, also transformed this area into one with a high percentage of persons of African descent as was found in most of the rest of the Caribbean.
From the 17th through the 19th century, the European colonial territories of the West Indies were the French West Indies, British West Indies, the Danish West Indies, the Netherlands Antilles (Dutch West Indies), and the Spanish West Indies.
In 1916, Denmark sold the Danish West Indies to the United States for US$25 million in gold, per the Treaty of the Danish West Indies. The Danish West Indies became an insular area of the U.S., called the United States Virgin Islands.
Between 1958 and 1962, the United Kingdom re-organised all their West Indies island territories (except the British Virgin Islands and the Bahamas) into the West Indies Federation. They hoped that the Federation would coalesce into a single, independent nation. However, the Federation had limited powers, numerous practical problems, consequently, it was dissolved by the British in 1963, with nine provinces eventually becoming independent sovereign states and four becoming current British Overseas Territories.
The termWest India was the namesake of several companies of the 17th and 18th centuries, including the Danish West India Company, the Dutch West India Company, the French West India Company, and the Swedish West India Company.
The West Indies is a geologically complex island system consisting of 7,000 islands and islets stretching over 3,000 km from the Florida peninsula of North America south-southeast to the northern coast of Venezuela. These islands include active volcanoes, low-lying atolls, raised limestone islands, and large fragments of continental crust containing tall mountains and insular rivers. Each of the three archipelagos of the West Indies has a unique origin and geologic composition.
The Greater Antilles is geologically the oldest of the three archipelagos and includes both the largest islands (Cuba, Jamaica, Hispaniola, and Puerto Rico) and the tallest mountains (Pico Duarte, Blue Mountain, Pic la Selle, Pico Turquino) in the Caribbean. The islands of the Greater Antilles are composed of strata of different geological ages including Precambrian fragmented remains of the North American Plate (older than 541 million years), Jurassic aged limestone (201.3-145 million years ago), as well as island arc deposits and oceanic crust from the Cretaceous (145-66 million years ago).
The Greater Antilles originated near the Isthmian region of present day Central America in the Late Cretaceous (commonly referred to as the Proto-Antilles), then drifted eastward arriving in their current location when colliding with the Bahama Platform of the North American Plate ca. 56 million years ago in the late Paleocene. This collision caused subduction and volcanism in the Proto-Antillean area and likely resulted in continental uplift of the Bahama Platform and changes in sea level. The Greater Antilles have continuously been exposed since the start of the Paleocene or at least since the Middle Eocene (66-40 million years ago), but which areas were above sea level throughout the history of the islands remains unresolved.
The oldest rocks in the Greater Antilles are located in Cuba. They consist of metamorphosed graywacke, argillite, tuff, mafic igneous extrusive flows, and carbonate rock. It is estimated that nearly 70% of Cuba consists of karst limestone. The Blue Mountains of Jamaica are a granite outcrop rising over 2,000 meters, while the rest of the island to the west consists mainly of karst limestone. Much of Hispaniola, Puerto Rico, and the Virgin Islands were formed by the collision of the Caribbean Plate with the North American Plate and consist of 12 island arch terranes. These terranes consist of oceanic crust, volcanic and plutonic rock.
The Lesser Antilles is a volcanic island arc rising along the leading edge of the Caribbean Plate due to the subduction of the Atlantic seafloor of the North American and South American plates. Major islands of the Lesser Antilles likely emerged less than 20 Ma, during the Miocene. The volcanic activity that formed these islands began in the Paleogene, after a period of volcanism in the Greater Antilles ended, and continues today. The main arc of the Lesser Antilles runs north from the coast of Venezuela to the Anegada Passage, a strait separating them from the Greater Antilles, and includes 19 active volcanoes.
The Lucayan Archipelago includes the Bahamas and Turks and Caicos Islands, a chain of barrier reefs and low islands atop the Bahama Platform. The Bahama Platform is a carbonate block formed of marine sediments and fixed to the North American Plate. The emergent islands of the Bahamas and Turks and Caicos likely formed from accumulated deposits of wind-blown sediments during Pleistocene glacial periods of lower sea level.
Countries and territories by archipelago
- Anguilla (United Kingdom)
- Antigua and Barbuda
- Aruba (Netherlands)
- Bonaire (Netherlands)
- British Virgin Islands (United Kingdom)
- Curaçao (Netherlands)
- Guadeloupe (France)
- Martinique (France)
- Montserrat (United Kingdom)
- Nueva Esparta (Venezuela)
- Saba (Netherlands)
- Saint Barthélemy (France)
- Saint Kitts and Nevis
- Saint Lucia
- Saint-Martin (France)
- Saint Vincent and the Grenadines
- Sint Eustatius (Netherlands)
- Sint Maarten (Netherlands)
- Trinidad and Tobago
- United States Virgin Islands (United States)
- Federal Dependencies of Venezuela (Venezuela)
- Caribbean Basin Initiative
- Caribbean Basin Trade Partnership Act
- Caribbean Community
- History of the Caribbean
- History of the British West Indies
- Spanish colonization of the Americas
- West Indian
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