Stratovolcanoes

Arenal

Arenal (Costa Rica) is a stratovolcano. It rises to 1,670 m above sea level. The GVP records 27 confirmed eruptions in the Holocene, the latest in 2010.

Elevation
1,670 m
Last eruption
2010
Confirmed eruptions
27
Max VEI
4
Country
Costa Rica
Location
10.46° N, 84.70° W
Region (GVP)
Central America Volcanic Arc
GVP type
Stratovolcano
Tectonic setting
Subduction zone / Continental crust (> 25 km)
Main rock type
Andesite / Basaltic Andesite

Show on the timeline GVP entry ↗

Other volcanoes and strong earthquakes within 300 km

Eruption history

VEI – Volcanic Explosivity Index: 0 = lava outpouring, 4 = like Eyjafjallajökull 2010, 6 = like Pinatubo 1991, 7 = like Tambora 1815. The scale is logarithmic – each step is about 10 times more material.

StartEndVEIVent and dating
29 July 1968 16 December 2010 3 W flank & summit · Observations: Reported
5 October 1922 23 October 1922 2 Observations: Reported
1750 ± 50 years — 0 Summit and NW flank (A2 lava flows) · Correlation: Tephrochronology
c. 1440 — 2 Isotopic: 14C (uncalibrated)
c. 1400 — 4 Isotopic: 14C (uncalibrated)
c. 1030 — 4 Correlation: Tephrochronology
c. 1020 — 4 Correlation: Tephrochronology
750 ± 50 years — 4 Correlation: Anthropology
c. 700 — 4 Correlation: Tephrochronology
650 ± 100 years — 4 Isotopic: 14C (calibrated)
c. 550 — 4 Correlation: Tephrochronology
c. 400 — 4 Correlation: Anthropology
170 BCE ± 200 years — 4 Isotopic: 14C (calibrated)
c. 270 BCE — 4 Correlation: Tephrochronology
380 BCE ± 200 years — 4 Isotopic: 14C (calibrated)
830 BCE ± 500 years — 0 Correlation: Tephrochronology
1,250 BCE ± 200 years — 4 Isotopic: 14C (calibrated)
c. 1,450 BCE — 4 Correlation: Tephrochronology
c. 1,650 BCE — 4 Correlation: Tephrochronology
1,770 BCE ± 100 years — ? Cerro Chato · Isotopic: 14C (calibrated)
c. 2,250 BCE — 4 Correlation: Tephrochronology
c. 2,800 BCE — 4 Correlation: Tephrochronology
3,190 BCE ± 100 years — ? Cerro Chato · Isotopic: 14C (uncalibrated)
c. 3,350 BCE — 4 Correlation: Tephrochronology
c. 3,900 BCE — 4 Correlation: Tephrochronology
c. 4,450 BCE — ? Correlation: Tephrochronology
5,060 BCE ± 150 years — 4 Isotopic: 14C (calibrated)

Data: Global Volcanism Program, Smithsonian Institution (#345033)