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The Dominican Republic (Spanish: República Dominicana) is a country in the West Indies that occupies the eastern five-eighths of Hispaniola. It has an area of 48,670 km 2 , including offshore islands.
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
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 ...
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).
According to statistical data, Pedernales is the least densely populated province in the Dominican Republic [citation needed]. For 2010, the total population reached 31,587 people: 16,895 men and 14,692 women, with a density of 15.7 inhabitants / km 2 (inhabitants per square kilometer). The predominant ethnic groups are 78% mulatto or mestizo ...
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The Dominican Republic 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 by ...
Within the Dominican Republic, the central Cordillera Septentrional spans the strike-slip fault boundary between the North American and Caribbean plates. Faults and folds from the Paleocene to the Pliocene in marine sedimentary rocks indicate its history of uplift, beginning in Eocene pelagic carbonates.