Doña Juana

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  • Colombia
  • Colombia
  • Stratovolcano
  • 1906 CE
  • Country
  • Subregion Name
  • Primary Volcano Type
  • Last Known Eruption
  • 1.47°N
  • 76.92°W

  • 4150 m
    13612 ft

  • 351070
  • Latitude
  • Longitude

  • Summit
    Elevation

  • Volcano
    Number

There are no activity reports for Doña Juana.



 Available Weekly Reports

There are no Weekly Reports available for Doña Juana.

Summary of eruption dates and Volcanic Explosivity Indices (VEI).

Start Date Stop Date Eruption Certainty VEI Evidence Activity Area or Unit
1897 Nov 1 1906 Confirmed 4 Historical Observations
2550 BCE ± 150 years Unknown Confirmed 4 Radiocarbon (uncorrected) Northeastern caldera

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.

Cuellar-Rodriguez J V, Ramirez-Lopez C, 1987. Descripcion de los volcanes Colombianos. Rev CIAF, Bogota, p 189-222.

Hantke G, Parodi I, 1966. Colombia, Ecuador and Peru. Catalog of Active Volcanoes of the World and Solfatara Fields, Rome: IAVCEI, 19: 1-73.

Mendez Fajury R A, 1989. Catalogo de los volcanes activos en Colombia. Bol Geol INGEOMINAS, Colombia, 30: 1-75.

Steimle U, 1989. The Dona Juana volcano, Departamento de Narino, southern Colombia. Unpublished MSci thesis, Eberhard Karls Univ, 97 p.

The forested Doña Juana stratovolcano contains two calderas, breached to the NE and SW. The summit of the andesitic-dacitic volcano is comprised of a series of post-caldera lava domes. The older caldera, open to the NE, formed during the mid-Holocene, accompanied by voluminous pyroclastic flows. The younger caldera contains the active central cone. The only historical activity of Doña Juana took place during a long-term eruption from 1897-1906, when growth of a summit lava dome was accompanied by major pyroclastic flows.