Available Weekly Reports
- Volcano Info
- Search Database
- Info & Contacts
There are no activity reports for Los Atlixcos.
Available Weekly Reports
There are no Weekly Reports available for Los Atlixcos.
There are no Holocene eruptions known for Los Atlixcos. 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.
Ferrari L , Tagami T, Eguchi M, Orozco-Esquivel M T, Petrone C M, Jacobo-Albarran J, Lopez-Martinez M, 2005. Geology, geochronology and tectonic setting of late Cenozoic volcanism along the southwestern Gulf of Mexico: the Eastern Alkaline Province revisited. J Volc Geotherm Res, 146: 284-306.
Gomez-Tuena, LaGatta A B, Langmuir C H, Goldstein S L, Ortega-Gutierrez F, Carrasco-Nunez G, 2003. Temporal control of subduction magmatism in the eastern Trans-Mexican Volcanic Belt: mantle sources, slab contributions, and crustal contamination. Geochem Geophys Geosyst, 4(8): 1-33.
Negendank J F W, Emmermann R, Krawczyk R, Mooser F, Tobschall H, Werle D, 1985. Geological and geochemical investigations on the eastern Trans-Mexican Volcanic Belt. Geof Internac, 24: 477-575.
Los Atlixcos, also known as Cerro el Abra, consists of a shield volcano topped by two large pyroclastic cones and associated lava fields at the eastern end of the Mexican Volcanic Belt along the Gulf of Mexico about 80 km NW of the city of Veracruz. The two pyroclastic cones, both known as Cerro los Atlixcos, lie along an E-W line about 2 km apart; both cones are breached to the east. A broad apron of basaltic lava flows extends primarily to the north and east, reaching as far as the coast. The extent of the lava shield is defined by the Río Santa Ana on the NE and the Río El Tecuán on the south. The youthful morphology of the cones caused Negendank et al. (1985) to consider them to be of Holocene age. Other pyroclastic cones of Quaternary age are located to the NW, and a group of cones and silicic lava domes of Tertiary-to-Quaternary age were constructed along the coast to the SE.