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  2. Aguas Zarcas volcanic field - Wikipedia

    en.wikipedia.org/wiki/Aguas_Zarcas_volcanic_field

    Located in the North flank of the Platanar Volcano, it is composed of at least nine cones, of which one is recognized as a hill (cerro) and the remaining eight as hillocks (loma). [ 2 ] [ 3 ] The sides of the cones are slanted between 10 and 30 degrees, the cones have an elongated shape in the East to West direction and the complex runs in the ...

  3. Tortuguero National Park - Wikipedia

    en.wikipedia.org/wiki/Tortuguero_National_Park

    Tortuguero National Park is a national park in the Limón Province of Costa Rica. It is situated within the Tortuguero Conservation Area of the northeastern part of the country. [3] Despite its remote location, reachable only by airplane or boat, it is the third-most visited park in Costa Rica. [4]

  4. Irazú Volcano National Park - Wikipedia

    en.wikipedia.org/wiki/Irazú_Volcano_National_Park

    Irazú Volcano National Park, or in Spanish the Parque Nacional Volcán Irazú, is a National Park in the Central Conservation Area of Costa Rica that encompasses the area around the Irazú Volcano in Cartago Province which incorporates what used to be the Ruben Torres Rojas Forest Reserve now called the Prusia Forest Reserve. The volcano is ...

  5. Rincón de la Vieja National Park - Wikipedia

    en.wikipedia.org/wiki/Rincón_de_la_Vieja...

    Rincón de la Vieja National Park (Spanish: Parque Nacional Rincón de la Vieja), is a National Park in Guanacaste Province of the northwestern part of Costa Rica. It encompasses the Rincón de la Vieja and Santa María volcanoes, as well as the dormant Cerro Von Seebach. The last eruption here was by Rincón de la Vieja in 2017.

  6. Volcán Barú - Wikipedia

    en.wikipedia.org/wiki/Volcán_Barú

    The Volcán Barú (also Volcán de Chiriquí [1]) is an active stratovolcano and the tallest mountain in Panama, at 3,474 metres (11,398 ft) high.It lies about 35 km (22 mi) off the border of Costa Rica.

  7. Geology of Costa Rica - Wikipedia

    en.wikipedia.org/wiki/Geology_of_Costa_Rica

    The geology of Costa Rica is part of the Panama Microplate, which is slowly moving north relative to the stable Caribbean Plate. [1] [2] In the late Cretaceous , an oceanic trench or backarc system formed in connection with a subduction zone, situated where the Isthmus of Panama is now located.

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