Parícutin volcano is currently classified as dormant and is not active; its only eruption occurred from 1943 to 1952, and it has shown no signs of substantial volcanic activity since then.
Geological Status
Parícutin is a monogenetic cinder cone volcano, meaning it typically erupts only once during its lifetime. After its nine-year eruption ended in 1952, Parícutin became dormant, with no further lava or ash emissions observed since that time. The only occasional activity is mild release of warm acidic water vapor from fumarole vents near the cone rim, but this does not constitute an active eruption.
Recent Activity and Scientific Consensus
- Parícutin has not erupted in over 70 years, and there are no indications of renewed activity.
- As a monogenetic volcano, Parícutin is not expected to erupt again based on scientific understanding of this volcano type.
- The surrounding Michoacán-Guanajuato Volcanic Field remains active as a region, but Parícutin itself stands as a dormant geological monument.
Implications for Visitors
- The volcano is safe for hiking and tourism, making it a popular destination for geologists and visitors interested in witnessing a site of relatively recent volcanic birth.
- Any observed activity is limited to gentle fumarole emissions, posing no threat to visitors.
Summary Table
| Volcano | Latest Eruption | Current Status | Expected Future Eruptions |
| Parícutin | 1952 | Dormant | Not expected |
Parícutin volcano is dormant and poses no volcanic hazard in the present day.
