Many cultures were indigenous to these islands, with evidence dating some of them back to the mid-6th millennium BCE.
In the late 16th century, French, English and Dutch merchants and privateers began 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 Saint Kitts in 1624 and Barbados in 1626, and when the Sugar Revolution took off in the mid-17th century, they brought in thousands of enslaved Africans to work the fields and mills as labourers. These enslaved 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, enslaved Africans 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 comprised the Western Caribbean Zone in place in the early-18th 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 enslaved Africans 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.
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. The Federation had limited powers, numerous practical problems, and a lack of popular support; consequently, it was dissolved by the British in 1963, with nine provinces eventually becoming independent sovereign states and four becoming current British Overseas Territories.
West Indian is the official term used by the U.S. government to refer to people of the West Indies.[14]
The term survives today mainly through the West Indies cricket team, representing all of the nations in the West Indian islands.
Geology
The West Indies are a geologically complex island system consisting of 7,000 islands and islets stretching over 3,000 km (2000 miles) from the Florida peninsula of North America south-southeast to the northern coast of Venezuela.[15] These islands include active volcanoes, low-lying atolls, raised limestone islands, and large fragments of continental crust containing tall mountains and insular rivers.[16] Each of the three archipelagos of the West Indies has a unique origin and geologic composition.
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.[19] 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.[20] 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.[21][19]
The oldest rocks in the Greater Antilles are located in Cuba. They consist of metamorphosedgraywacke, argillite, tuff, maficigneous extrusive flows, and carbonate rock.[22] It is estimated that nearly 70% of Cuba consists of karst limestone.[23] The Blue Mountains of Jamaica are a granite outcrop rising over 2,000 meters (6000'), while the rest of the island to the west consists mainly of karst limestone.[23] 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 arcterranes.[24] These terranes consist of oceanic crust, volcanic and plutonic rock.[24]
Lesser Antilles
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.[17] The volcanic activity that formed these islands began in the Paleogene, after a period of volcanism in the Greater Antilles ended, and continues today.[25] 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.[26]
Lucayan Archipelago
The Lucayan Archipelago includes The Bahamas and the 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.[16] 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.[16]
Countries and territories by subregion and archipelago
^ abGraham, Alan (2003). "Geohistory Models and Cenozoic Paleoenvironments of the Caribbean Region". Systematic Botany. 28 (2): 378–386. doi:10.1043/0363-6445-28.2.378 (inactive 1 November 2024). ISSN0363-6445. JSTOR3094007.{{cite journal}}: CS1 maint: DOI inactive as of November 2024 (link)
^Khudoley, K. M.; Meyerhoff, A. A. (1971), "Paleogeography and Geological History of Greater Antilles", Geological Society of America Memoirs, Geological Society of America, pp. 1–192, doi:10.1130/mem129-p1, ISBN978-0813711294
^ abMann, Paul; Draper, Grenville; Lewis, John F. (1991), "An overview of the geologic and tectonic development of Hispaniola", Geological Society of America Special Papers, Geological Society of America, pp. 1–28, doi:10.1130/spe262-p1, ISBN978-0813722627
^Santiago-Valentin, Eugenio; Olmstead, Richard G. (2004). "Historical Biogeography of Caribbean Plants: Introduction to Current Knowledge and Possibilities from a Phylogenetic Perspective". Taxon. 53 (2): 299–319. doi:10.2307/4135610. ISSN0040-0262. JSTOR4135610.
Wikimedia Commons has media related to West Indies.
Cave, Roderick, and R. Cave. 1978. "Early Printing and the Book Trade in the West Indies". Library Quarterly 48 (April): 163–92.
Cromwell, Jesse. "More than Slaves and Sugar: Recent Historiography of the Trans-imperial Caribbean and Its Sinew Populations". History Compass (2014) 12#10 pp 770–783.
Higman, Barry W. A Concise History of the Caribbean. (2011)
†Physiographically, these continental islands are not part of the volcanic Windward Islands arc, although sometimes grouped with them culturally and politically.
#Bermuda is an isolated North Atlanticoceanic island, physiographically not part of the Lucayan Archipelago, Antilles, Caribbean Sea nor North American continental nor South American continental islands. It is grouped with the Northern American region, but occasionally also with the Caribbean region culturally.