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The Global Volcanism Program has no activity reports for Estelí.
The Global Volcanism Program has no Weekly Reports available for Estelí.
The Global Volcanism Program has no Bulletin Reports available for Estelí.
Fresh-looking, sparsely vegetated lava flows mostly erupted from fissure vents are located in valleys in the northern interior highlands between the town of Estelí and the border with Honduras. McBirney and Williams (1965) considered basaltic flows in this area to be certainly of Quaternary, and possibly of Holocene age. The lava flows near Estelí were faulted and slightly tilted during formation of the Estelí structural basin. Other youthful basaltic lava flows, one of which was erupted from the Bonete de Carrao cone, are located between Estelí and Jinotega. Well-preserved cones are also located in the area west and south of Ocotal. Some of the youthful lava flows in northern Nicaragua contain granitic xenoliths and xenocrysts of quartz.
The Global Volcanism Program is not aware of any Holocene eruptions from Estelí. If this volcano has had large eruptions (VEI >= 4) prior to 10,000 years ago, information might be found on the Estelí page in the LaMEVE (Large Magnitude Explosive Volcanic Eruptions) database, a part of the Volcano Global Risk Identification and Analysis Project (VOGRIPA).
This compilation of synonyms and subsidiary features may not be comprehensive. Features are organized into four major categories: Cones, Craters, Domes, and Thermal Features. Synonyms of features appear indented below the primary name. In some cases additional feature type, elevation, or location details are provided.
|Feature Name||Feature Type||Elevation||Latitude||Longitude|
|Bonete de Carrao||Cone|
|San Rafael, Cerro||Cinder cone||13° 5' 0" N||86° 23' 0" W|
|Vesubio, Cerro de||Cinder cone||13° 8' 0" N||86° 25' 0" W|
|Volcán, Cerro el||Cinder cone||13° 10' 0" N||86° 26' 0" W|
|The area NW of the town of Estelí (bottom-center) and east of the prominent fault-bound valley at the left contains sparsely vegetated lava flows of the Estelí volcanic field. The flows were mostly erupted from fissure vents located in valleys in the northern interior highlands of Nicaragua between the town of Estelí and the border with Honduras.
NASA Landsat7 image (worldwind.arc.nasa.gov)
The following references have all been used during the compilation of data for this volcano, it is not a comprehensive bibliography. 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.
Incer J, 1987. . (pers. comm.).
McBirney A R, Williams H, 1965. Volcanic history of Nicaragua. Univ Calif Pub Geol Sci, 55: 1-65.