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  • Country
  • Subregion Name
  • Primary Volcano Type
  • Last Known Eruption
  • 14.33°N
  • 90.4°W

  • 1454 m
    4769 ft

  • 342111
  • Latitude
  • Longitude

  • Summit

  • Volcano

There are no activity reports for Cuilapa-Barbarena.

 Available Weekly Reports

There are no Weekly Reports available for Cuilapa-Barbarena.

There are no Holocene eruptions known for Cuilapa-Barbarena. If this volcano has had large eruptions prior to 10,000 years ago, information might be found in the LaMEVE (Large Magnitude Explosive Volcanic Eruptions) database, a part of the Volcano Global Risk Identification and Analysis Project (VOGRIPA).

The following references are the sources used for data regarding this volcano. References are linked directly to our volcano data file. Discussion of another volcano or eruption (sometimes far from the one that is the subject of the manuscript) may produce a citation that is not at all apparent from the title. Additional discussion of data sources can be found under Volcano Data Criteria.

Heiken G, Duffield W, 1990. An evaluation of the geothermal potential of the Tecuamburro volcano area of Guatemala. Central Amer Energy Resour Project, LA-11906-MS, Los Alamos Natl Lab, Los Alamos, NM 87545, 37 p.

IAVCEI, 1973-80. Post-Miocene Volcanoes of the World. IAVCEI Data Sheets, Rome: Internatl Assoc Volc Chemistry Earth's Interior..

Reynolds J H, 1987. Timing and sources of Neogene and Quaternary volcanism in south-central Guatemala. J Volc Geotherm Res, 33: 9-22.

Williams H, 1960. Volcanic history of the Guatemalan Highlands. Univ Calif Pub Geol Sci, 38: 1-86.

The Cuilapa-Barbarena volcanic field contains approximately 70 Quaternary cinder cones, generally less than 100 m high. Many of the mostly basaltic cones are located along the strike of the major regional Jalpatagua fault, which extends SE from Guatemala City, north of the chain of stratovolcanoes stretching across Guatemala. The cones were erupted from fracture systems related to the intersection of the Jalpatagua fault with the southern and western margins of the Miocene Santa Rosa de Lima caldera and overlie pyroclastic-flow deposits from Amatitlán caldera to the NW. The age of the most recent eruptions is not known, although the youngest cones post-date the last phase of eruptive activity at Tecuamburro volcano and could be of Holocene age (Reynolds, 1987). Williams (1960) considered the most recent eruptions from the Cuilapa-Barbarena volcanic field to have occurred within the last few thousand years.