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The Cibao Valley (Dominican Republic) is the largest and the most important valley of the country. This long valley stretches from North Haiti, where is called Plaine du Nord , to Samaná Bay. It can be divided in two sections: the northwestern part is the Yaque del Norte Valley (or Línea Noroeste ) and the eastern Yuna Valley (or Vega Real ...
The provinces of the Dominican Republic Monte Cristi coastline. An enlargeable basic map of the Dominican Republic Boca Chica (in Santo Domingo Province), about 30km east of Santo Domingo. Santa Bárbara de Samaná, capital of Samaná Province. Provinces of the Dominican Republic – in alphabetical order: Distrito Azua; Distrito Baoruco
The Dominican Republic is divided into three macro-regions, which are in turn divided into ten regions. [ 1 ] [ 2 ] In 1858 the country was divided in 3 departments: Cibao (North), Ozama (Southwest), and Seybo (Southeast).
The Dominican Republic [a] is a North American country located on the island of Hispaniola in the Greater Antilles of the Caribbean Sea in the North Atlantic Ocean.It shares a maritime border with Puerto Rico to the east and a land border with Haiti to the west, occupying the eastern five-eighths of Hispaniola which, along with Saint Martin, is one of only two islands in the Caribbean shared ...
Provinces of the Dominican Republic map. The Dominican Republic is divided into thirty-one provincias (provinces; singular provincia), while the national capital, Santo Domingo, is contained within its own Distrito Nacional ("National District"; "D.N." on the map below).
Geography of the Dominican Republic by province (32 C). Geography of Santo Domingo (1 C, 8 P) * Dominican Republic geography-related lists (1 C, 13 P) B.
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Into the Paleogene at the start of the Cenozoic, volcanism, metamorphism and plutonism continued underwater until the Eocene, still largely below water.However, by the middle Eocene, the amalgamated island arcs collided with the southern margin of the North American Plate at the Florida-Bahama Platform, leading to the formation of extensive carbonates and the end of volcanism and plutonism.