Lesser Antilles

The Lesser Antilles (also known as the Caribbees) is the name given to a group of islands in the Caribbean Sea. Most form a long, partly volcanic island arc between the Greater Antilles to the north-west and the continent of South America. The islands form the eastern boundary of the Caribbean Sea with the Atlantic Ocean. Together, the Lesser Antilles and the Greater Antilles compose the Antilles (or the Caribbean in its narrowest definition). When combined with the Lucayan Archipelago, all three are known as the West Indies.

Geography

The islands of the Lesser Antilles are divided into three groups. The two main groups are the Windward Islands in the south and the Leeward Islands in the north. The Windward Islands are so called because they were more windward to sailing ships arriving in the New World than the Leeward Islands, given that the prevailing trade winds blow east to west. The trans-Atlantic currents and winds that provided the fastest route across the ocean brought these ships to the rough dividing line between the Windward and Leeward Islands.

Greater Antilles

The Greater Antilles is a grouping of the larger islands in the Caribbean Sea; Cuba, Hispaniola (containing Haiti and the Dominican Republic), Puerto Rico, Jamaica, and the Cayman Islands. The Greater Antilles constitute over 90% of the land mass of the entire West Indies, as well as over 90% of its population, with the balance made of the archipelago of the Lesser Antilles which is a chain of islands to the east (running north-south and encompassing the eastern edge of the Caribbean Sea where it meets the Atlantic Ocean) and south (running east-west off the northern coast of South America).

The word Antilles originated in the period before the European conquest of the New World - Europeans used the term Antilia as one of the mysterious lands featured on medieval charts, sometimes as an archipelago, sometimes as continuous land of greater or lesser extent, its location fluctuating in mid-ocean between the Canary Islands and Eurasia.

Countries

See also

Puerto Rico

Coordinates: 18°12′N 66°30′W / 18.2°N 66.5°W / 18.2; -66.5

Puerto Rico (English /ˌpɔːrtə ˈriːkoʊ/ or /ˌpwɛərtə ˈriːkoʊ/;Spanish: [ˈpweɾto ˈriko], locally also [ˈpwelto ˈχiko; ˈʀ̥iko]), officially the Commonwealth of Puerto Rico (Spanish: Estado Libre Asociado de Puerto Rico, literally the "Free Associated State of Puerto Rico"), is a United States territory located in the northeastern Caribbean. Puerto Rico is an archipelago that includes the main island of Puerto Rico and a number of smaller islands. The capital and largest city is San Juan. The territory does not observe daylight saving time, and its official languages are Spanish, which is predominant, and English. The island's population is approximately 3.4 million.

Puerto Rico's rich history, tropical climate, diverse natural scenery, renowned traditional cuisine and attractive tax incentives make it a popular destination for visitors from around the world. Its location in the Caribbean, combined with centuries of colonization and subsequent migration, has made Puerto Rican culture a distinct melting pot of Amerindian, Spanish, African, and North American influences.

Flat Earth

The flat Earth model is an archaic conception of the Earth's shape as a plane or disk. Many ancient cultures subscribed to a flat Earth cosmography, including Greece until the classical period, the Bronze Age and Iron Age civilizations of the Near East until the Hellenistic period, India until the Gupta period (early centuries AD) and China until the 17th century. That paradigm was also typically held in the aboriginal cultures of the Americas, and the notion of a flat Earth domed by the firmament in the shape of an inverted bowl was common in pre-scientific societies.

The idea of a spherical Earth appeared in Greek philosophy with Pythagoras (6th century BC), although most Pre-Socratics retained the flat Earth model. Aristotle accepted the spherical shape of the Earth on empirical grounds around 330 BC, and knowledge of the spherical Earth gradually began to spread beyond the Hellenistic world from then on.

Historical development

Ancient Near East

In early Egyptian and Mesopotamian thought the world was portrayed as a flat disk floating in the ocean. A similar model is found in the Homeric account of the 8th century BC in which "Okeanos, the personified body of water surrounding the circular surface of the Earth, is the begetter of all life and possibly of all gods." The Israelites likely had a similar cosmology, with the earth as a flat disc floating on water beneath an arced firmament separating it from the heavens.

Modern flat Earth societies

Modern flat Earth hypotheses originated with the English writer Samuel Rowbotham (1816–1884). Based on his conclusions derived from the Bedford Level experiment, Rowbotham published a 16-page pamphlet, Zetetic Astronomy, which he later expanded into a 430-page book, Earth Not a Globe, in which the Earth is a flat disc centred at the North Pole and bounded along its southern edge by a wall of ice (Antarctica), with the Sun and Moon 3,000 miles (4,800 km) and the "cosmos" 3,100 miles (5,000 km) above Earth. He also published a leaflet entitled "The inconsistency of Modern Astronomy and its Opposition to the Scriptures!!", which argued that the "Bible, alongside our senses, supported the idea that the earth was flat and immovable and this essential truth should not be set aside for a system based solely on human conjecture".

Rowbotham and followers like William Carpenter, who continued the belief, gained attention by successful use of pseudoscience in public debates with leading scientists of the day. One such debate, involving Alfred Russel Wallace, concerned the Bedford Level experiment (and later led to several lawsuits for fraud and libel). Rowbotham created a Zetetic Society in England and New York, shipping over a thousand copies of Zetetic Astronomy.