The geology of Turks and Caicos includes the Turks and Caicos Bank, which together with the Florida-Bahamas Platform is a section of continental crust rifted away from North America during the rifting open of the Atlantic Ocean. Triassic sedimentary and volcanic rocks are inferred based on similar rocks in the Bahamas, overlain by Jurassic, Cretaceous and Paleogene limestone. During a drop in sea level during the Pleistocene glaciations, limestone was exposed as plateaus as sand dunes accumulated atop them and a karst landscape developed with caves and blue holes. [1]
The Turks and Caicos Islands are a British Overseas Territory consisting of the larger Caicos Islands and smaller Turks Islands, two groups of tropical islands in the Lucayan Archipelago of the Atlantic Ocean and northern West Indies. They are known primarily for tourism and as an offshore financial centre. The resident population was 31,458 in 2012, of whom 23,769 lived on Providenciales in the Caicos Islands; July 2020 estimates put the population at 55,926. It is the third largest of the British overseas territories by population.
Before European colonization, the Turks and Caicos Islands were inhabited by Taino and Lucayan peoples. The first recorded European sighting of the islands now known as the Turks and Caicos occurred in 1512. In the subsequent centuries, the islands were claimed by several European powers with the British Empire eventually gaining control. For many years the islands were governed indirectly through Bermuda, the Bahamas, and Jamaica. When the Bahamas gained independence in 1973, the islands received their own governor, and have remained a separate autonomous British Overseas Territory since. In August 2009, the United Kingdom suspended the Turks and Caicos Islands' self-government following allegations of ministerial corruption. Home rule was restored in the islands after the November 2012 elections.
Grand Turk Island is an island in the Turks and Caicos Islands. It is the largest island in the Turks Islands with 18 km2 (6.9 sq mi). Grand Turk contains the territory's capital, Cockburn Town, and the JAGS McCartney International Airport. The island is the administrative, historic, cultural and financial center of the territory and has the second-largest population of the islands at approximately 4,831 people in 2012.
The Lucayan Archipelago, also known as the Bahama Archipelago, is an island group comprising the Commonwealth of The Bahamas and the British Overseas Territory of the Turks and Caicos Islands. The archipelago is in the western North Atlantic Ocean, north of Cuba and the other Antilles, and east and southeast of Florida.
Ripsaw is a musical genre which originated in the Turks and Caicos Islands, specifically in the Middle and North Caicos. A very closely related variant, rake-and-scrape, is played in the Bahamas. Its most distinctive characteristic is the use of the common handsaw as the primary instrument, along with various kinds of drums, box guitar, concertina, triangle and accordion.
The majority of the population of the Turks and Caicos Islands are Christian. They include Protestant 72.8%, Baptists 35.8%, Church of God 11.7%, Roman Catholics 11.4%, Anglicans 10%, Methodists 9.3%, Seventh-Day Adventists 6%, Jehovah's Witnesses 1.8%, and Other 14%
Drexel Wellington Gomez is a Bahamian Anglican bishop.
The Bahama Banks are the submerged carbonate platforms that make up much of the Bahama Archipelago. The term is usually applied in referring to either the Great Bahama Bank around Andros Island, or the Little Bahama Bank of Grand Bahama Island and Great Abaco, which are the largest of the platforms, and the Cay Sal Bank north of Cuba. The islands of these banks are politically part of the Bahamas. Other banks are the three banks of the Turks and Caicos Islands, namely the Caicos Bank of the Caicos Islands, the bank of the Turks Islands, and wholly submerged Mouchoir Bank. Farther southeast are the equally wholly submerged Silver Bank and Navidad Bank north of the Dominican Republic.
Mouchoir Bank, in Spanish also called Banco de Pañuelo Blanco, is a submerged bank disputed by the Turks and Caicos Islands and the Dominican Republic, claimed by both as part of their EEZ.
JAGS McCartney International Airport, also known as Grand Turk International Airport, is an airport located 1 mile (1.6 km) south of Cockburn Town on Grand Turk Island in the Turks and Caicos Islands, an overseas territory of the United Kingdom. It is the second largest airport in the Turks & Caicos, after Providenciales International Airport.
The West Indies are a subregion of North America, surrounded by the North Atlantic Ocean and the Caribbean Sea that includes 13 independent island countries and 18 dependencies and other territories in three major archipelagos: the Greater Antilles, the Lesser Antilles, and the Lucayan Archipelago.
The Caribbean bioregion is a biogeographic region that includes the islands of the Caribbean Sea and nearby Atlantic islands, which share a fauna, flora and mycobiota distinct from surrounding bioregions.
The Bahamian dry forests are a tropical and subtropical dry broadleaf forest ecoregion in the Bahamas and the Turks and Caicos Islands, covering an area of 4,800 km2 (1,900 sq mi). They are found on much of the northern Bahamas, including Andros, Abaco, and Grand Bahama, where they are known as coppices. Dry forests are distributed evenly throughout the Turks and Caicos.
Miss Turks and Caicos is a national Beauty pageant in Turks & Caicos.
Chilabothrus chrysogaster, commonly known as the Turks Island boa or the Southern Bahamas boa, is a species of snake found in the Southern Bahamas and the Turks and Caicos Islands. Local names include rainbow boa, Bahamas cat boa, rainbow snake, and fowl snake. Like all boids, it is not a venomous species.
This is a survey of the postage stamps and postal history of the Turks and Caicos Islands.
The Anglican Diocese of the Bahamas and the Turks and Caicos Islands was originally established in 1861 as the Diocese of Nassau. Retitled the Diocese of Nassau and The Bahamas in 1942, it is now known as the Diocese of The Bahamas and the Turks and Caicos Islands. It is a diocese of the Church in the Province of the West Indies, a constituent province of the Anglican Communion.
The Geology of Jamaica is formed of rocks of Cretaceous to Neogene age. The basement consists of Cretaceous island arc and back-arc basin sequences that formed above a subduction zone. The cover is of mainly Eocene to Miocene shallow water limestones, that have been uplifted due to the presence of a restraining bend along the major strike-slip faults that bound the southern edge of the Gonâve Microplate to the north of the island.
The geology of Tanzania began to form in the Precambrian, in the Archean and Proterozoic eons, in some cases more than 2.5 billion years ago. Igneous and metamorphic crystalline basement rock forms the Archean Tanzania Craton, which is surrounded by the Proterozoic Ubendian belt, Mozambique Belt and Karagwe-Ankole Belt. The region experienced downwarping of the crust during the Paleozoic and Mesozoic, as the massive Karoo Supergroup deposited. Within the past 100 million years, Tanzania has experienced marine sedimentary rock deposition along the coast and rift formation inland, which has produced large rift lakes. Tanzania has extensive, but poorly explored and exploited natural resources, including coal, gold, diamonds, graphite and clays.