Comondú-La Purísima

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  • Mexico
  • Mexico
  • Volcanic field
  • Unknown
  • Country
  • Subregion Name
  • Primary Volcano Type
  • Last Known Eruption
  • 26°N
  • 111.92°W

  • 780 m
    2558 ft

  • 341012
  • Latitude
  • Longitude

  • Summit
    Elevation

  • Volcano
    Number

There are no activity reports for Comondú-La Purísima.



 Available Weekly Reports

There are no Weekly Reports available for Comondú-La Purísima.

There are no Holocene eruptions known for Comondú-La Purísima. 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.

Bellon H, Aguillon-Robles A, Calmus T, Maury R C, Bourgois J, Cotten J, 2006. La Purisima volcanic field, Baja California Sur (Mexico): Miocene to Quaternary volcanism related to subduction and opening of an asthenospheric window. J Volc Geotherm Res, 152: 253-272.

Calmus T, Aguillon-Robles A, Maury R C, Bellon H, Benoit M, Cotten J, Bourgois J, Michaud F, 2003. Spatial and temporal evolution of basalts and magnesian andesites ("bajaites") from Baja California, Mexico: the role of slab melts. Lithos, 66: 77-105.

Haukwa C, Bodvarsson G S, Lippmann M J, Mainieri A, 1992. Preliminary reservoir engineering studies of the Miravalles geothermal field, Costa Rica. Proc 17th Stanford Geotherm Workshop, p 127-137.

Hausback B P, 1984. Cenozoic volcanic and tectonic evolution of Baja California Sur, Mexico. In: Frizzell V A Jr (ed) {Geology of the Baja California Peninsula}, SEPM, 39: 219-236.

Saunders A D, Rogers G, Marriner G F, Terrell D J, Verma S P, 1987. Geochemistry of Cenozoic volcanic rocks, Baja California, Mexico: implications for the petrogenesis of post-subduction magmas. J Volc Geotherm Res, 32: 223-245.

Sawlan M G, 1991. Magmatic evolution of the Gulf of California rift. In: Dauphin J P and Simoneit B A (eds) {The Gulf and Peninsular Province of the Californias}, Amer Assoc Petrol Geol Mem, 47: 301-369.

The Comondú-La Purísima volcanic field, located in southern Baja California, west of the Sierra de la Giganta, dates back to the Miocene. However, the youthful morphology of some cinder cones suggested possible Holocene ages (Sawlan, 1991). The youngest lavas form blocky flows with flow ridges and are mostly located in the area between Comondú and the La Purísima river. Vents usually occur along NNW-trending faults, and many lava flows are offset, sometimes repeatedly, along grabens. Both basaltic and andesitic lava flows are present. The former are typically 5-10 m thick, and the latter are up to 60-80 m thick and form dense, glassy flows with subhorizontal fractures.