Fagradalsfjall volcano floods the Meradalir Valley with lava flows.
Fagradalsfjall volcano mountain is a tuya that erupted during the last glaciation under the ice shield. The broader Fagradalsfjall volcanic system comprises an area of eruptive fissures (fissure swarm), cones and lava fields in the southern part of the Reykjanes peninsula.
A strong seismic crisis began in the area near Fagradalsfjall since late Feb 2021, interpreted as intrusion of magma at shallow depth. This led to the first historic eruption of the volcano on 19 March 2021.
Fagradalsfjall (Icelandic pronunciation: [ˈfaɣraˌtalsˌfjatl̥]) is a tuya volcano formed in the Last Glacial Period on the Reykjanes Peninsula, around 40 kilometres (25 mi) from Reykjavík, Iceland. Fagradalsfjall is also the name for the wider volcanic system covering an area 5 kilometres (3 mi) wide and 15 kilometres (9 mi) long between the Svartsengi and Krýsuvík systems.The highest summit in this area is Langhóll (385 m (1,263 ft)). No volcanic eruption had occurred for 800 years on the Reykjanes Peninsula until 19 March 2021 when a fissure vent appeared in Geldingadalir to the south of Fagradalsfjall mountain.The eruption is effusive and still emitting fresh lava as of 20 July 2021. The eruption is unique among the volcanoes monitored in Iceland so far and is expected to develop into a shield volcano.Due to its relative ease of access from Reykjavík, the volcano has become an attraction for local people and foreign tourists alike.
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