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The Province of Georgia[ 1 ] (also Georgia Colony) was one of the Southern Colonies in colonial-era British America. In 1775 it was the last of the Thirteen Colonies to support the American Revolution. The original land grant of the Province of Georgia included a narrow strip of land that extended west to the Pacific Ocean.
Georgia was named after King George II, who approved the colony's charter in 1732. The conflict between Spain and England over control of Georgia began in earnest in about 1670, when the English colony of South Carolina was founded just north of the missionary provinces of Guale and Mocama, part of Spanish Florida.
Seafloor spreading. Age of oceanic lithosphere; youngest (light colour) is along spreading centers. Seafloor spreading, or seafloor spread, is a process that occurs at mid-ocean ridges, where new oceanic crust is formed through volcanic activity and then gradually moves away from the ridge.
James Oglethorpe. Lieutenant-General James Edward Oglethorpe (22 December 1696 [1] – 30 June 1785) was a British Army officer, Tory politician and colonial administrator best known for founding the Province of Georgia in British North America. As a social reformer, he hoped to resettle Britain's "worthy poor" in the New World, initially ...
The Province (and later State) of Georgia was a significant battleground in the American Revolution. Its population was at first divided about exactly how to respond to revolutionary activities and heightened tensions in other provinces. Georgia was the only colony not present in the First Continental Congress in 1774.
Mid-ocean ridge cross-section (cut-away view) A mid-ocean ridge (MOR) is a seafloor mountain system formed by plate tectonics. It typically has a depth of about 2,600 meters (8,500 ft) and rises about 2,000 meters (6,600 ft) above the deepest portion of an ocean basin. This feature is where seafloor spreading takes place along a divergent plate ...
Marine sediment. v. t. e. The seabed (also known as the seafloor, sea floor, ocean floor, and ocean bottom) is the bottom of the ocean. All floors of the ocean are known as 'seabeds'. The structure of the seabed of the global ocean is governed by plate tectonics. Most of the ocean is very deep, where the seabed is known as the abyssal plain.
Evidence for the earliest occupation of the territory of present-day Georgia goes back to c. 1.8 million years ago, as evident from the excavations of Dmanisi in the southeastern part of the country. This is the oldest evidence of humans anywhere in the world outside Africa. Later prehistoric remains (Acheulian, Mousterian, and the Upper ...