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Name Elevation Location Last eruption meters feet Coordinates; Apaneca Range: 2036: 6680: Holocene Apastepeque Volcanic Field: 700: 2297: Holocene Chingo [1]: 1775: 5823
The total land area of El Salvador is 23,041 km 2, with 20,721 km 2 of land and 320 km 2 of water. El Salvador is about the size of Israel and the U.S states of New Jersey and Vermont, but has the population size of Libya and Lebanon. El Salvador has 590 km of borders, including 391 km of borders with Honduras and 199 km with Guatemala. El ...
El Boquerón National Park. The San Salvador Volcano (also known as Quezaltepeque or El Boquerón) is a stratovolcano situated northwest to the city of San Salvador. The crater has been nearly filled with a relatively newer edifice, the Boquerón volcano. San Salvador is adjacent to the volcano and the western section of the city actually lies ...
The Central American Volcanic Arc (often abbreviated to CAVA) is a chain of volcanoes which extends parallel to the Pacific coastline of the Central American Isthmus, from Mexico to Panama. This volcanic arc, which has a length of 1,100 kilometers (680 mi) [1][2] is formed by an active subduction zone, with the Cocos Plate subducting underneath ...
Ring of Fire. The Ring of Fire (also known as the Pacific Ring of Fire, the Rim of Fire, the Girdle of Fire or the Circum-Pacific belt) [note 1] is a tectonic belt of volcanoes and earthquakes. It is about 40,000 km (25,000 mi) long [1] and up to about 500 km (310 mi) wide, [2] and surrounds most of the Pacific Ocean.
Download as PDF; Printable version; ... Stratovolcanoes of El Salvador (15 P) Pages in category "Volcanoes of El Salvador"
Izalco. Izalco is an active stratovolcano [2] on the side of the Santa Ana Volcano, which is located in western El Salvador. It is situated on the southern flank of the Santa Ana volcano. Izalco erupted almost continuously from 1770 (when it formed) to 1958 [3] earning it the nickname of "Lighthouse of the Pacific", and experienced a flank ...
Coatepeque Caldera (Nawat: cōātepēc, "at the snake hill") is a volcanic caldera in El Salvador in Central America. The caldera was formed during a series of rhyolitic explosive eruptions from a group of stratovolcanoes between about 72,000 and 57,000 years ago. Since then, basaltic cinder cones and lava flows formed near the west edge of the ...