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Geological Formation

Rincon de la Vieja

Volcanic Formations

Rincon de la Vieja rises in Guanacaste Province in northwestern Costa Rica, reaching an elevation of about 1,916 meters at its active Santa Maria crater, also known as the Von Seebach crater. It is a complex volcano made up of at least nine eruptive centers strung along a shared volcanic massif, built from andesitic lava flows and pyroclastic deposits, and its slopes host extensive hydrothermal features including fumaroles, boiling mud pots and hot springs. The volcano and its surrounding cloud forest are protected within Rincon de la Vieja National Park, and its active crater produces periodic phreatic and minor explosive eruptions. This entity documents Rincon de la Vieja specifically as a geological formation, a multi-vent complex volcano in Costa Rica noted for its extensive hydrothermal activity.

Facts
Classification
Protected Status
National Park or Reserve 1
Connections

Caused By

Volcanism, Processes
Source Rincón de la Vieja Volcano (Wikipedia)

In Discipline

Source Rincón de la Vieja Volcano (Wikipedia)
In the Other Atlases

Found In

Also in Geography Atlas: where this subject is found.

Sources
1. Rincón de la Vieja Volcano (Wikipedia)
  • Lead
    Rincón de la Vieja stands 1,916 metres (6,286 ft) above sea level, and its summit is the highest point in Rincón de la Vieja National Park.
  • In Discipline: Volcanology, Lead section (in-discipline Volcanology)
    Rincón de la Vieja is an active andesitic complex volcano in north-western Costa Rica, about 23 km (14 mi) from Liberia, in the province of Guanacaste.
  • Caused By: Volcanism, Lead section (caused-by Volcanism)
    Rincón de la Vieja is an active andesitic complex volcano in north-western Costa Rica, about 23 km (14 mi) from Liberia, in the province of Guanacaste.
View the Source
Wikidata: Rincon de la Vieja
Wikidata Q1122340, class allow-list match (w-wdresolver-0926)View the Source
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