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Land use map of Nicaragua, 1979 Topography of Nicaragua Nicaragua map of Köppen climate classification zones. Nicaragua (officially the Republic of Nicaragua Spanish: República de Nicaragua [reˈpuβlika ðe nikaˈɾaɣwa] ⓘ) is a country in Central America, bordering both the Caribbean Sea and the North Pacific Ocean, between Costa Rica and Honduras.
Nicaragua, [d] officially the Republic of Nicaragua, [e] is the geographically largest country in Central America, comprising 130,370 km 2 (50,340 sq mi). With a population of 7,142,529 as of 2024, [ 16 ] it is the third-most populous country in Central America after Guatemala and Honduras .
The history of Nicaragua remained relatively static for three hundred years following the conquest. There were minor civil wars and rebellions, but they were quickly suppressed. The region was subject to frequent raids by Dutch , French and British pirates, with the city of Granada being invaded twice, in 1658 and 1660.
The Mosquito Coast (also known as the Mosquitia or Mosquito Shore) is an area along the eastern coast of present-day Nicaragua and Honduras.It was named after the local Miskito Nation and was long dominated by British interests and known as the Mosquito Kingdom.
An enlargeable topographic map of Nicaragua. Geography of Nicaragua. Nicaragua is: a country; Location: Northern Hemisphere and Western Hemisphere. Americas. North America. Middle America. Central America; Time zone: Central Standard Time ; Extreme points of Nicaragua High: Mogoton 2,107 m (6,913 ft) Low: North Pacific Ocean and Caribbean Sea 0 m
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Settlement of English people along the Caribbean Coast, or Miskito Coast, of Nicaragua began in 1633. The area was controlled by Britain until 1860, and eventually integrated into Nicaragua by 1894. The Miskito Coast region divided into two autonomous regions within Nicaragua after 1987. [citation needed]
The geology of Nicaragua includes Paleozoic crystalline basement rocks, Mesozoic intrusive igneous rocks and sedimentary rocks spanning the Cretaceous to the Pleistocene. Volcanoes erupted in the Paleogene and within the last 2.5 million years of the Quaternary , due to the subduction of the Cocos Plate, which drives melting and magma creation.