Knowledge

Ceboruco

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flows preserved around the volcano keep a record of the recent eruptions. Before the Jala eruption, there is record of one major lava flow, called the Destiladero flow. During the 500 years after the Jala eruption, the volcano was at its most active, leaving record of six major lava flows: the
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Copales, El Cajón, Coapan I, Coapan II, El Norte, and Ceboruco flows, all before the Spanish arrived in 1521. The volcano remained active until the next major eruption in 1870, however volcanism was, for the most part, constrained within the calderas.
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Sieron, K.; Siebe, C. (2008). "Revised stratigraphy and eruption rates of Ceboruco stratovolcano and surrounding monogenetic vents (Nayarit, Mexico) from historical documents and new radiocarbon dates".
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nested inside that formed when the Dos Equis lava dome collapsed during the Coapales eruption around 1100 AD. Within both of these craters, are several explosive volcanic features, including
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Chertkoff, D.G.; Gardner, J.E. (2003). "Nature and timing of magma interactions before, during and after the caldera-forming eruption of Volcan Ceboruco, Mexico".
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activity lasting well into the 20th century. The mountain features one large
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Index


Elevation
Listing
Coordinates
21°7′30″N 104°30′30″W / 21.12500°N 104.50833°W / 21.12500; -104.50833
Ceboruco is located in Nayarit
Jala
Nayarit
Ceboruco is located in Mexico
Mountain type
Stratovolcano
Volcanic belt
Trans-Mexican Volcanic Belt
Last eruption
dacitic
stratovolcano
Nayarit
Trans-Mexican Volcanic Belt
Plinian eruption
VEI
tephra
fumarole
caldera
crater
scoria
lava domes
pyroclastic
cinder cone
lava
trachydacite

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