Mexico · Volcanic field
San Martín Tuxtla
San Martin
- Type
- Volcanic field
- Elevation
- 1660m
- Last eruption
- 1796

- Type
- Volcanic field
- Country
- Mexico
- Region
- Middle America & Caribbean / Trans-Mexican Volcanic Arc
- Elevation
- 1660m
- Coordinates
- 18.561, -95.199
- Last eruption
- 1796
- Tectonic setting
- Subduction zone / Continental crust (> 25 km)
- Landform
- Composite
- Major rock type
- Trachybasalt / Tephrite basanite
Geological summary
Volcán de San Martín, part of the Tuxtla Volcanic Field, is a broad alkaline shield volcano that rises above the Gulf of Mexico. The massive volcano, also known as San Martín Tuxtla, is elongated NW-SE and is capped by a 1-km-wide summit crater. The upper part of the volcano is covered with dense tropical rain forests. The summit and flanks contain more than 250 pyroclastic cones and maars. Well-preserved cinder cones are abundant between the summit and Laguna Catemaco on the SE flank. Holocene cones in this area produced ash deposits that buried stone pyramids. The two largest recorded eruptions took place in 1664 and 1793. The 1793 eruption occurred from two cinder cones in the summit crater and produced widespread ashfall and lava flows that extended 3.5 km down the NE flank.
From Wikipedia
The isolated San Martin Tuxtla volcano is a shield volcano which rises above the Gulf of Mexico. It has had eruptions in historical times. It occurs in the Tuxtla volcanic field in Veracruz, Mexico. Lavas from San Martin vary between basanite and alkali basalt. Locally the volcano is also known as Tiltépetl.
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Eruption history
16 recordedGlossaryDetailed timeline
- 1932VEI ?Method not stated1932-12-31 – end unknown
- 1838VEI ?Method not stated1838-07-02 – end unknown
- 1797VEI 2Method not stated1797 – 1805-07-02
- 1794VEI 2Observed1794-05 – 1796
- 1793VEI 4Observed1793-03-02 – 1793-12Cinder cones in summit crater
- 1664VEI 3Observed1664-01-15 – end unknownSE flank
- 1534VEI ?Method not stated1534 – end unknown
- 890 (±40 yrs)VEI ?Geological estimate890 – end unknown
- 480 (±50 yrs)VEI ?Geological estimate480 – end unknown
- 380 (±75 yrs)VEI ?Geological estimate380 – end unknownSouth flank
- 120 (±200 yrs)VEI ?Geological estimate120 – end unknownSouth flank (Cerro Puntiagudo)
- 150 BCE (±300 yrs)VEI ?Geological estimate150 BCE – end unknownSouth flank
- 750 BCE (±40 yrs)VEI ?Geological estimate750 BCE – end unknown
- 1320 BCE (±300 yrs)VEI ?Geological estimate1320 BCE – end unknownSouth flank (Cerro Mono Blanco)
- 2130 BCE (±50 yrs)VEI ?Geological estimate2130 BCE – end unknown
- 3440 BCE (±50 yrs)VEI ?Geological estimate3440 BCE – end unknown
Nearby volcanoes
External links
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