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  2. Parícutin - Wikipedia

    en.wikipedia.org/wiki/Parícutin

    Parícutin (or Volcán de Parícutin, also accented Paricutín) is a cinder cone volcano located in the Mexican state of Michoacán, near the city of Uruapan and about 322 kilometers (200 mi) west of Mexico City. The volcano surged suddenly from the cornfield of local farmer Dionisio Pulido in 1943, attracting both popular and scientific attention.

  3. List of cinder cones - Wikipedia

    en.wikipedia.org/wiki/List_of_cinder_cones

    Royal Society Volcano, Antarctica; Cerro Volcánico, Argentina; Mount Mayabobo, Philippines; Bombalai Hill (Sabah, Malaysia); Geghama mountains, Armenia; Chaîne des Puys, France (a chain of volcanoes including cinder cones)

  4. Volcanic cone - Wikipedia

    en.wikipedia.org/wiki/Volcanic_cone

    Cinder cones typically only erupt once like Parícutin. As a result, they are considered to be monogenetic volcanoes and most of them form monogenetic volcanic fields. Cinder cones are typically active for very brief periods of time before becoming inactive. Their eruptions range in duration from a few days to a few years. Of observed cinder ...

  5. Michoacán–Guanajuato volcanic field - Wikipedia

    en.wikipedia.org/wiki/Michoacán–Guanajuato...

    Other volcanoes in the field include Alberca de los Espinos in Michoacán and Cerro Culiacán in Guanajuato. [1] The cinder cones are randomly arranged and occur at low altitudes, usually, on alluvial plains or on the flanks of eroded shield volcanoes. There are an average of 2.5 cinder cones every 100 kilometres (62 mi) 2.

  6. Monogenetic volcanic field - Wikipedia

    en.wikipedia.org/wiki/Monogenetic_volcanic_field

    Many monogenetic volcanoes are cinder cones, often with lava flows, such as Parícutin in the Michoacán-Guanajuato volcanic field, which erupted from 1943 to 1952. Some monogenetic volcanoes are small lava shields, such as Rangitoto Island in the Auckland volcanic field. Other monogenetic volcanoes are tuff rings or maars. A monogenetic field ...

  7. Cinder cone - Wikipedia

    en.wikipedia.org/wiki/Cinder_cone

    Such cinder cones likely represent the final stages of activity of a mafic volcano. [11] However, most volcanic cones formed in Hawaiian-type eruptions are spatter cones rather than cinder cones, due to the fluid nature of the lava. [12] The most famous cinder cone, Paricutin, grew out of a corn field in Mexico in 1943 from a new vent. [3]

  8. List of inactive volcanoes in the Philippines - Wikipedia

    en.wikipedia.org/wiki/List_of_inactive_volcanoes...

    This is a list of inactive volcanoes in the Philippines. Volcanoes with no record of eruptions are considered as extinct or inactive. Their physical form since their last activity has been altered by agents of weathering and erosion with the formation of deep and long gullies. [1] Inactive does not necessarily indicate the volcano will not ...

  9. List of active volcanoes in the Philippines - Wikipedia

    en.wikipedia.org/wiki/List_of_active_volcanoes...

    Listed as Bud Dajo, a cinder cone on Jolo Island, in the PHIVOLCS list. Kanlaon: 2,435 7,989 Negros Occidental, Negros Oriental: 28 Eruptions were recorded from 1886 to 2006. On November 23, 2015 the volcano had a small, steam-driven explosion.