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A dive center in Playa Kalki is available. Westpunt is famous for the two currents that meet in-front of Cliff Villa Peninsula stirring up the nutrients in the water making it the premium diving location on the island. The dive area is called Watamula which is a corruption of the Dutch word for “water mill”. [11]
Aerial view of the coast of Curaçao Enlargeable, detailed map of Curaçao Green Iguana from Curaçao. Curaçao, as well as the rest of the ABC islands and Trinidad and Tobago, lies on the continental shelf of South America. It is a thin island with a generally hilly topography; the highest point is Christoffelberg 372 m (1,220 ft) in the ...
Playa Kalki is a beach on the Caribbean island of Curaçao, also known as Alice in Wonderland due to mushroom-shaped coral formations. [1] The name Kalki is unrelated to the Avatar Kalki, but comes from the local Papiamentu word for the white coral rock and limestone, which is abundant on the beach and surrounding cliffs.
Curaçao, [a] officially the Country of Curaçao (Dutch: Land Curaçao; [10] Papiamentu: Pais Kòrsou), [11] [12] is a constituent island country within the Kingdom of the Netherlands in the southern Caribbean Sea, specifically the Dutch Caribbean region, about 65 km (40 mi) north of Venezuela.
Boesmansgat – Sinkhole and dive site in South Africa; Bohol Sea – Marginal sea between the Visayas and Mindanao in the Philippines; Booya – Schooner wrecked in Darwin, Australia; BOS 400 – Recent wreck and dive site at Duiker Point on the Cape Peninsula west coast; Bottle Island – One of the Summer Isles in Loch Broom, Scotland
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The shaded relief map of the Caribbean Sea and the Gulf of Mexico area [8] [9] The geological age of the Caribbean Sea is estimated to be between 160 and 180 million years and was formed by a horizontal fracture that split the supercontinent called Pangea in the Mesozoic Era. [10]
The island of Curaçao began to form within the past 145 million years, beginning in the Cretaceous, as part of the Lesser Antilles island arc.Because the island was submerged for large parts of its history, reef environments formed atop thick layers of mafic volcanic rock, producing carbonate sedimentary rocks.
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