Puerto Rico Bank
The Puerto Rico Bank, also known as the Puerto Rican Bank, is a carbonate platform and insular shelf comprising the archipelagos of Puerto Rico and the Virgin Islands, located between the Greater Antilles and the Lesser Antilles in the northeastern Caribbean. Last subaerially exposed from the Last Glacial Maximum in the Last Glacial Period of the Late Pleistocene Age to the Northgrippian Age of the Holocene Epoch, the bank connected Puerto Rico and the Virgin Islands into a single landmass until Early Holocene [sea level rise|sea level rise] fragmented it into the present-day islands between 10,000 and 7,000 years Before Present. It is within the Puerto Rico–Virgin Islands microplate between the North American plate and Caribbean plate.
Name
Most commonly known as the Puerto Rico Bank and Puerto Rican Bank, the bank is named after the largest island within its limits, the eponymous main island of the archipelago of Puerto Rico. The part of the bank covering the Virgin Islands is occasionally referred to as the Virgin Bank.Location
Separated from the Greater Antilles by the Mona Passage and from the Lesser Antilles by the Anegada passage in the northeastern Caribbean Sea of the Atlantic Ocean, the Puerto Rico Bank compromises the main island of Puerto Rico, the Spanish Virgins Islands of Vieques and Culebra, the U.S. Virgin Islands of Saint Thomas and Saint John, and the British Virgin Islands of Jost Van Dyke, Tortola, Virgin Gorda, and Anegada. It includes all surrounding minor islands and cays of each one of the aforementioned major islands. The westernmost islands of Desecho, Mona, and Monito of Puerto Rico, and the southernmost island of Saint Croix of the U.S. Virgin Islands do not form part of the bank, as they lie on their own platforms.Extent
Including the island within the Puerto Rico Bank, it measures 350 km in length and in width. Around the main island of Puerto Rico, the bank is wide from the southeast to the southwest, over wide from the southwest to northwest, and less than wide from the northwest to the northeast. Around the archipelago of the Virgin Islands, the bank is wide.The Puerto Rico Bank is less than 79 m in depth, with the portion connecting all the islands being less than in depth. All islands and cays in the archipelago of Puerto Rico, including Vieques and Culebra, are connected less than. Similarly, the main islands of the U.S. Virgin Islands and the British Virgin Islands are connected by less than. The Spanish Virgin Islands of Vieques and Culebra and the American and British islands are separated by a narrow strait, the Virgin Passage, which is 16 km in length and in depth.
With an area of, it was last fully exposed during the Last Glacial Maximum when the sea level was lower than the present-day. The bank was inundated by sea level rise during the Late Pleistocene and Early Holocene, losing subaerial connection the main island of Puerto Rico and the Spanish Virgin Islands with the U.S. Virgin Islands and British Virgin Islands 10,000 to 8,000 years Before Present ago. The main island of Puerto Rico with Vieques, and the U.S. Virgin Islands and the British Virgin Islands with each other lost their land connection 7,000 years BP ago, while the main island of Puerto Rico with some of its minor islands, cays, and islets 3,000 BP years ago.