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The Cape of Good Hope (Afrikaans: Kaap die Goeie Hoop [ˌkɑːp di ˌχujə ˈɦuəp]) [a] is a rocky headland on the Atlantic coast of the Cape Peninsula in South Africa. A common misconception is that the Cape of Good Hope is the southern tip of Africa, based on the misbelief that the Cape was the dividing point between the Atlantic and ...
Bartolomeu Dias [a] (c. 1450 – 29 May 1500) was a Portuguese mariner and explorer. In 1488, he became the first European navigator to round the southern tip of Africa and to demonstrate that the most effective southward route for ships lies in the open ocean, well to the west of the African coast.
The Gonâve microplate, showing the main fault zones that bound it. The island of Jamaica lies on the boundary between the Caribbean plate and the Gonâve microplate.The Gonâve microplate is a 1,100 km (680 mi) long strip of mainly oceanic crust formed by the Cayman spreading ridge within a strike-slip pull-apart basin on the northern transform margin of the Caribbean plate with the North ...
However, production from the Caribbean and North American colonies deflated the price resulting in an 18-month moratorium on St. Kitts tobacco farming in 1639. This prompted the production of sugar from sugar cane on St. Kitts in 1643, and on Nevis in 1648. Windmills were built to crush the canes and extract the juice.
[127] [128] The expedition reached a cape extending north to south which they called Cape of "Santa Maria" (Punta del Este, keeping the name the Cape nearby); and after 40°S they found a "Cape" or "a point or place extending into the sea", and a "Gulf" (in June and July). After they had navigated for nearly 300 km (186 mi) to round the cape ...
Drive to hegemony: the United States in the Caribbean, 1898-1917 (1988). Higman, Barry W. A concise history of the Caribbean. Cambridge University Press, 2010. Hoffman, Paul E. The Spanish Crown and the Defense of the Caribbean, 1535-1585: Precedent, Patrimonialism, and Royal Parsimony. Baton Rouge: LSU Press 1980. Jackson, Ashley.
For decades, scientists have warned about the potential of the Cascadia Subduction Zone, a megathrust fault that runs offshore along the coast from northern Vancouver Island to Cape Mendocino ...
The source of the earthquake is located in the Anegada Passage. [7] The Reid Fault located 17 km (11 mi) south of Saint Thomas on the northern scarp of the Anegada Trough runs for seven tens of kilometers may have ruptured and produced slip no greater than ten meter. [19] The rupture may have initiated at a depth of 3 km along this thrust fault.