Vulcano Arenal
Arenal
Stratovulcano · Costa Rica · 1670 m
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- Tipo
- Stratovulcano
- Paese
- Costa Rica
- Regione
- Middle America-Caribbean Volcanic Regions / Central America Volcanic Arc
- Altitudine
- 1670 m
- Coordinate
- 10.463, -84.703
- Ultima eruzione
- 2010
- Contesto tettonico
- Subduction zone / Continental crust (> 25 km)
- Forma vulcanica
- Composite
- Roccia principale
- Andesite / Basaltic Andesite
Sintesi geologica
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.
Sintesi da Wikipedia
Riassunto in ingleseArenal 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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Storia delle eruzioni
Cronologia dettagliata
- 1968VEI 3Osservata1968-07-29 – 2010-12-16W flank & summit
- 1922VEI 2Osservata1922-10-05 – 1922-10-23
- 1915VEI 2Stima geologica1915-02-05 – In corso
- 1750 (±50 anni)VEI 0Stima geologica1750 – In corsoSummit and NW flank (A2 lava flows)
- 1440VEI 2Stima geologica1440 – In corso
- 1400VEI 4Stima geologica1400 – In corso
- 1030VEI 4Stima geologica1030 – In corso
- 1020VEI 4Stima geologica1020 – In corso
- 750 (±50 anni)VEI 4Stima geologica750 – In corso
- 700VEI 4Stima geologica700 – In corso
- 650 (±100 anni)VEI 4Stima geologica650 – In corso
- 550VEI 4Stima geologica550 – In corso
- 400VEI 4Stima geologica400 – In corso
- 170 a.C. (±200 anni)VEI 4Stima geologicaBCE 170 – In corso
- 270 a.C.VEI 4Stima geologicaBCE 270 – In corso
- 380 a.C. (±200 anni)VEI 4Stima geologicaBCE 380 – In corso
- 830 a.C. (±500 anni)VEI 0Stima geologicaBCE 830 – In corso
- 1250 a.C. (±200 anni)VEI 4Stima geologicaBCE 1250 – In corso
- 1450 a.C.VEI 4Stima geologicaBCE 1450 – In corso
- 1650 a.C.VEI 4Stima geologicaBCE 1650 – In corso
- 1770 a.C. (±100 anni)VEI ?Stima geologicaBCE 1770 – In corsoCerro Chato
- 2250 a.C.VEI 4Stima geologicaBCE 2250 – In corso
- 2800 a.C.VEI 4Stima geologicaBCE 2800 – In corso
- 3190 a.C. (±100 anni)VEI ?Stima geologicaBCE 3190 – In corsoCerro Chato
- 3350 a.C.VEI 4Stima geologicaBCE 3350 – In corso
- 3900 a.C.VEI 4Stima geologicaBCE 3900 – In corso
- 4450 a.C.VEI ?Stima geologicaBCE 4450 – In corso
- 5060 a.C. (±150 anni)VEI 4Stima geologicaBCE 5060 – In corso
Link esterni
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