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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 ...
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.
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 following is a list of ecoregions in the Dominican Republic, as identified by the World Wide Fund for Nature (WWF). Terrestrial ecoregions.
Location of the Dominican Republic – The Dominican Republic is located within the following regions or bodies of water: Northern Hemisphere and Western Hemisphere. North America (though not on the mainland) – Greater North America may be geographically subdivided into Northern America, Central America, and the Caribbean; Atlantic Ocean
Dominican Republic geography-related lists (1 C, 13 P) B. Borders of the Dominican Republic (4 C) E. Ecoregions of the Dominican Republic (1 C, 6 P) G.
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 ...
Location of the Sierra de Bahoruco mountain range. The mountain range is a massif of volcanic origin from the Cretaceous period (from 145 to 66 million years ago) and later covered by a layer of calcareous sediment of marine origin, this means that the entire mountain range was once submerged under the sea and in mostly inhabited by corals that left their sediments.