Arenal Volcano
Arenal
Stratovolcano · Costa Rica · 1670m
_(cropped).jpg?width=800)
- Type
- Stratovolcano
- Country
- Costa Rica
- Region
- Middle America-Caribbean Volcanic Regions / Central America Volcanic Arc
- Elevation
- 1670m
- Coordinates
- 10.463, -84.703
- Last eruption
- 2010
- Tectonic setting
- Subduction zone / Continental crust (> 25 km)
- Landform
- Composite
- Major rock type
- Andesite / Basaltic Andesite
Geological summary
Conical Volcán Arenal is the youngest stratovolcano in Costa Rica and one of its most active. The 1670-m-high andesitic volcano towers above the eastern shores of Lake Arenal, which has been enlarged by a hydroelectric project. Arenal lies along a volcanic chain that has migrated to the NW from the late-Pleistocene Los Perdidos lava domes through the Pleistocene-to-Holocene Chato volcano, which contains a 500-m-wide, lake-filled summit crater. The earliest known eruptions of Arenal took place about 7000 years ago, and it was active concurrently with Cerro Chato until the activity of Chato ended about 3500 years ago. Growth of Arenal has been characterized by periodic major explosive eruptions at several-hundred-year intervals and periods of lava effusion that armor the cone. An eruptive period that began with a major explosive eruption in 1968 ended in December 2010; continuous explosive activity accompanied by slow lava effusion and the occasional emission of pyroclastic flows characterized the eruption from vents at the summit and on the upper western flank.
From Wikipedia
Arenal Volcano is a recently active andesitic stratovolcano in north-western Costa Rica around 90 km (56 mi) northwest of San José, in the province of Alajuela, canton of San Carlos, and district of La Fortuna. The Arenal volcano stands 1,633 metres (5,358 ft) high. It is conically shaped with a crater 140 metres (460 ft) in diameter. Geologically, Arenal is considered a young volcano and it is estimated to be less than 7,500 years old. It is also known as "Pan de Azúcar", "Canaste", "Volcan Costa Rica", "Volcan Río Frío" or "Guatusos Peak".
Wikipedia · CC BY-SA · Read full article →
Eruption history
Detailed timeline
- 1968VEI 3Observed1968-07-29 – 2010-12-16W flank & summit
- 1922VEI 2Observed1922-10-05 – 1922-10-23
- 1915VEI 2Geological estimate1915-02-05 – Ongoing
- 1750 (±50 yrs)VEI 0Geological estimate1750 – OngoingSummit and NW flank (A2 lava flows)
- 1440VEI 2Geological estimate1440 – Ongoing
- 1400VEI 4Geological estimate1400 – Ongoing
- 1030VEI 4Geological estimate1030 – Ongoing
- 1020VEI 4Geological estimate1020 – Ongoing
- 750 (±50 yrs)VEI 4Geological estimate750 – Ongoing
- 700VEI 4Geological estimate700 – Ongoing
- 650 (±100 yrs)VEI 4Geological estimate650 – Ongoing
- 550VEI 4Geological estimate550 – Ongoing
- 400VEI 4Geological estimate400 – Ongoing
- 170 BCE (±200 yrs)VEI 4Geological estimateBCE 170 – Ongoing
- 270 BCEVEI 4Geological estimateBCE 270 – Ongoing
- 380 BCE (±200 yrs)VEI 4Geological estimateBCE 380 – Ongoing
- 830 BCE (±500 yrs)VEI 0Geological estimateBCE 830 – Ongoing
- 1250 BCE (±200 yrs)VEI 4Geological estimateBCE 1250 – Ongoing
- 1450 BCEVEI 4Geological estimateBCE 1450 – Ongoing
- 1650 BCEVEI 4Geological estimateBCE 1650 – Ongoing
- 1770 BCE (±100 yrs)VEI ?Geological estimateBCE 1770 – OngoingCerro Chato
- 2250 BCEVEI 4Geological estimateBCE 2250 – Ongoing
- 2800 BCEVEI 4Geological estimateBCE 2800 – Ongoing
- 3190 BCE (±100 yrs)VEI ?Geological estimateBCE 3190 – OngoingCerro Chato
- 3350 BCEVEI 4Geological estimateBCE 3350 – Ongoing
- 3900 BCEVEI 4Geological estimateBCE 3900 – Ongoing
- 4450 BCEVEI ?Geological estimateBCE 4450 – Ongoing
- 5060 BCE (±150 yrs)VEI 4Geological estimateBCE 5060 – Ongoing
External links
⚠ For reference only. Not for emergency response.