Mount Santa Maria in Guatemala has experienced both effusive and explosive eruptions in its history. The 1902 eruption was explosive, causing catastrophic destruction, while subsequent eruptions have been effusive with lava flows.
Like many other stratovolcanoes, Mount Vesuvius varies in its type of eruptions. Some eruptions are explosive, producing clouds of ash. Others are are effusive, producing lava flows. The famous eruption that buried Pompeii in the year 79 was a highly explosive Plinian eruption.
Eruptions at Mount Etna can be explosive or effusive, with lava flows being the most common form of eruption. Explosive eruptions can generate ash plumes, pyroclastic flows, and lahars. Effusive eruptions produce lava flows that can flow for long distances and can pose a hazard to nearby communities.
Like most stratovolcanoes, Mount St Helens alternates between explosive and effusive eruptions.
Principal eruptions list 79 explosive Ash-fall, pomices and lahars472 effusive-explosive Lava flow and lahars to north-western flank51226 February 685 effusive Imposing lava flow787 effusive-explosive Lahars and imposing lava flow968 Lava flow to sea27 January 1037 Lava flow to sea29 May 1139 explosive Ash-fall1500 explosive Ash-fall16 December 1631 effusive-explosive Cone collapse; lava flow to sea3 July 1660 explosive Ash-fall to north-east flank13 April 1694 effusive Lava toward Torre del Greco25 May 1698 effusive-explosive Damage by ash-fall to south-east flank28 July 1707 effusive-explosive20 May 1737 effusive-explosive A lava flow invades T. del Greco; ash-fall and lahars23 December 1760 effusive-explosive Opening of lateral vents on southern flank (150 m asl)19 October 1767 effusive-explosive Two lava flows toward T.Annunziata. and S. Giorgio a Cremano8 August 1779 explosive Ash and bombs over Ottaviano15 June 1794 effusive-explosive Opening of lateral vents on south-western flank (470 m asl)22 October 1822 effusive-explosive Two lava flows toward T. del Greco and Boscotrecase23 August 1834 effusive-explosive A lava flow toward Poggiomarino6 February 1850 effusive-explosive1 May 1855 effusive A lava flow invades Massa and S.Sebastiano8 December 1861 effusive-explosive Opening of lateral vents on south-western flank (290 m asl)15 November 1868 effusive24 April 1872 effusive-explosive A lava flow invades Massa and S.Sebastiano4 April 1906 effusive-explosive A lava flow toward T.Annunziata, strong explosive activity3 June 1929 effusive-explosive A lava flow toward Terzigno18 March 1944 effusive-explosive A lava flow invades Massa and S.Sebastianosource:http://www.vesuvioinrete.it/e_storia.htm
No. Kilauea generally produces effusive eruptions. Explosive eruptions are rare.
There are effusive eruptions and explosive eruptions.
Generally not. Explosive eruptions may happen occasionally, but most eruptions are effusive.
Mount Santa Maria in Guatemala has experienced both effusive and explosive eruptions in its history. The 1902 eruption was explosive, causing catastrophic destruction, while subsequent eruptions have been effusive with lava flows.
Generally not. Most eruptions in Hawaii are effusive.
Like many other stratovolcanoes, Mount Vesuvius varies in its type of eruptions. Some eruptions are explosive, producing clouds of ash. Others are are effusive, producing lava flows. The famous eruption that buried Pompeii in the year 79 was a highly explosive Plinian eruption.
Eruptions at Mount Etna can be explosive or effusive, with lava flows being the most common form of eruption. Explosive eruptions can generate ash plumes, pyroclastic flows, and lahars. Effusive eruptions produce lava flows that can flow for long distances and can pose a hazard to nearby communities.
Yes. The Yellowstone volcano has produced several VEI-8 eruptions, the most explosive level of eruption possible.
Like most stratovolcanoes, Mount St Helens alternates between explosive and effusive eruptions.
Galeras volcano is known to have had both explosive and effusive eruptions in the past. It has been classified as a stratovolcano, which means it can exhibit a range of eruption types, including explosive eruptions with ash and pyroclastic flows, as well as effusive eruptions with lava flows.
Principal eruptions list 79 explosive Ash-fall, pomices and lahars472 effusive-explosive Lava flow and lahars to north-western flank51226 February 685 effusive Imposing lava flow787 effusive-explosive Lahars and imposing lava flow968 Lava flow to sea27 January 1037 Lava flow to sea29 May 1139 explosive Ash-fall1500 explosive Ash-fall16 December 1631 effusive-explosive Cone collapse; lava flow to sea3 July 1660 explosive Ash-fall to north-east flank13 April 1694 effusive Lava toward Torre del Greco25 May 1698 effusive-explosive Damage by ash-fall to south-east flank28 July 1707 effusive-explosive20 May 1737 effusive-explosive A lava flow invades T. del Greco; ash-fall and lahars23 December 1760 effusive-explosive Opening of lateral vents on southern flank (150 m asl)19 October 1767 effusive-explosive Two lava flows toward T.Annunziata. and S. Giorgio a Cremano8 August 1779 explosive Ash and bombs over Ottaviano15 June 1794 effusive-explosive Opening of lateral vents on south-western flank (470 m asl)22 October 1822 effusive-explosive Two lava flows toward T. del Greco and Boscotrecase23 August 1834 effusive-explosive A lava flow toward Poggiomarino6 February 1850 effusive-explosive1 May 1855 effusive A lava flow invades Massa and S.Sebastiano8 December 1861 effusive-explosive Opening of lateral vents on south-western flank (290 m asl)15 November 1868 effusive24 April 1872 effusive-explosive A lava flow invades Massa and S.Sebastiano4 April 1906 effusive-explosive A lava flow toward T.Annunziata, strong explosive activity3 June 1929 effusive-explosive A lava flow toward Terzigno18 March 1944 effusive-explosive A lava flow invades Massa and S.Sebastianosource:http://www.vesuvioinrete.it/e_storia.htm
Mount Shasta is considered a potentially explosive stratovolcano due to its composition of andesite and dacite lava which can lead to explosive eruptions. However, its most recent eruptions have been relatively non-explosive with mainly effusive lava flows.