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'''Volcán Ipala''' is a [[stratovolcano]] in south-eastern [[Guatemala]]. It has a {{Convert|1000|m|ft|-2}} wide [[summit crater]] which contains a [[crater lake]] ([[Lake Ipala]]), whose surface lies about {{Convert|150|m|ft|-2|abbr=on|abbr=on}} below the crater rim. Volcán Ipala is part of a cluster of small stratovolcanoes and cinder cone fields in south-eastern Guatemala.
'''Volcán Ipala''' is a [[stratovolcano]] in south-eastern [[Guatemala]]. It has a {{Convert|1000|m|ft|-2}} wide [[summit crater]] which contains a [[crater lake]] ([[Lake Ipala]]), whose surface lies about {{Convert|150|m|ft|-2|abbr=on}} below the crater rim. Volcán Ipala is part of a cluster of small stratovolcanoes and cinder cone fields in south-eastern Guatemala.


==See also==
==See also==

Revision as of 16:55, 23 December 2014

Volcán Ipala
Highest point
Elevation1,650 m (5,410 ft)
Geography
Volcán Ipala is located in Guatemala
Volcán Ipala
Volcán Ipala
Geology
Mountain typeStratovolcano
Last eruptionUnknown

Volcán Ipala is a stratovolcano in south-eastern Guatemala. It has a 1,000 metres (3,300 ft) wide summit crater which contains a crater lake (Lake Ipala), whose surface lies about 150 m (500 ft) below the crater rim. Volcán Ipala is part of a cluster of small stratovolcanoes and cinder cone fields in south-eastern Guatemala.

See also

References

  • "Ipala". Global Volcanism Program. Smithsonian Institution.