Cerro Cinotepeque

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  • Country
  • Subregion Name
  • Primary Volcano Type
  • Last Known Eruption
  • 14.02°N
  • 89.25°W

  • 665 m
    2181 ft

  • 343051
  • Latitude
  • Longitude

  • Summit

  • Volcano

There are no activity reports for Cerro Cinotepeque.

 Available Weekly Reports

There are no Weekly Reports available for Cerro Cinotepeque.

There are no Holocene eruptions known for Cerro Cinotepeque. 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.

Weber H S, Wiesemann G, 1978. Mapa Geologico de la Republica de El Salvador/America Central. Bundesanstalt fur Geowissenschaften und Rohstoffe, Hannover, Germany, 1:100,000 scale geologic map in 6 sheets.

Cerro Cinotepeque is the largest and most prominent of a group of four pyroclastic cones of Holocene age mapped by Weber and Weismann (1978) in low-lying areas on either side of the Río Lempa, about 40 km north of San Salvador. Cerro Cinotepeque (also spelled Cinotepec) lies south of the river; two other cones, Cerro Santiago and Cerro Mosquito, lie immediately north of the river. A fourth cone is located along the Río Gualchayo about 10 km farther north. A large group of small Pleistocene stratovolcanoes and pyroclastic cones constructed along NW-SE-trending faults is located west and south of Cerro Cinotepeque and west of Guazapa volcano.