Costa Rica · Stratovolcano
Arenal Volcano
Arenal
- Type
- Stratovolcano
- Elevation
- 1670m
- Last eruption
- 2010
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- Type
- Stratovolcano
- Country
- Costa Rica
- Region
- Middle America & Caribbean / 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".
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Eruption history
28 recordedGlossaryDetailed timeline
- 1968VEI 3Observed1968-07-29 – 2010-12-16W flank & summit
- 1922VEI 2Observed1922-10-05 – 1922-10-23
- 1915VEI 2Method not stated1915-02-05 – end unknown
- 1750 (±50 yrs)VEI 0Geological estimate1750 – end unknownSummit and NW flank (A2 lava flows)
- 1440VEI 2Geological estimate1440 – end unknown
- 1400VEI 4Geological estimate1400 – end unknown
- 1030VEI 4Geological estimate1030 – end unknown
- 1020VEI 4Geological estimate1020 – end unknown
- 750 (±50 yrs)VEI 4Geological estimate750 – end unknown
- 700VEI 4Geological estimate700 – end unknown
- 650 (±100 yrs)VEI 4Geological estimate650 – end unknown
- 550VEI 4Geological estimate550 – end unknown
- 400VEI 4Geological estimate400 – end unknown
- 170 BCE (±200 yrs)VEI 4Geological estimate170 BCE – end unknown
- 270 BCEVEI 4Geological estimate270 BCE – end unknown
- 380 BCE (±200 yrs)VEI 4Geological estimate380 BCE – end unknown
- 830 BCE (±500 yrs)VEI 0Geological estimate830 BCE – end unknown
- 1250 BCE (±200 yrs)VEI 4Geological estimate1250 BCE – end unknown
- 1450 BCEVEI 4Geological estimate1450 BCE – end unknown
- 1650 BCEVEI 4Geological estimate1650 BCE – end unknown
- 1770 BCE (±100 yrs)VEI ?Geological estimate1770 BCE – end unknownCerro Chato
- 2250 BCEVEI 4Geological estimate2250 BCE – end unknown
- 2800 BCEVEI 4Geological estimate2800 BCE – end unknown
- 3190 BCE (±100 yrs)VEI ?Geological estimate3190 BCE – end unknownCerro Chato
- 3350 BCEVEI 4Geological estimate3350 BCE – end unknown
- 3900 BCEVEI 4Geological estimate3900 BCE – end unknown
- 4450 BCEVEI ?Geological estimate4450 BCE – end unknown
- 5060 BCE (±150 yrs)VEI 4Geological estimate5060 BCE – end unknown
Nearby volcanoes
External links
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