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  2. Types of volcanic eruptions - Wikipedia

    en.wikipedia.org/wiki/Types_of_volcanic_eruptions

    Pahoehoe lava is a relatively smooth lava flow that can be billowy or ropey. They can move as one sheet, by the advancement of "toes", or as a snaking lava column. [10] A'a lava flows are denser and more viscous than pahoehoe, and tend to move slower. Flows can measure 2 to 20 m (7 to 66 ft) thick.

  3. Tseax Cone - Wikipedia

    en.wikipedia.org/wiki/Tseax_Cone

    The fourth flow is the shortest and least voluminous of the four lava flows from Tseax Cone. It represents about 1% of the total lava volume and travelled Crater Creek for 5.3 kilometres (3.3 miles). These latter two lava flows consist of ʻaʻā [ d ] and are rich in phenocrysts.

  4. List of lava tubes - Wikipedia

    en.wikipedia.org/wiki/List_of_Lava_Tubes

    Leviathan Cave – At 12.5 kilometres, it is the longest lava tube in Africa. [3] Emuruangogolak Volcano caves [2] North Chyulu hills area – 20 caves are known [2] Hells Teeth [2] Kimakia Caves [2] Mathioni [2] Skull Caves [2] Kimakia Cave [2] Lake Tillam, near Korosi Volcano – several known lava tubes [2]

  5. Volcano - Wikipedia

    en.wikipedia.org/wiki/Volcano

    Augustine Volcano (Alaska) during its eruptive phase on January 24, 2006. A volcano is commonly defined as a vent or fissure in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface.

  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

    Eruptions continued for nine years, built the cone to a height of 424 meters (1,391 ft), and produced lava flows that covered 25 km 2 (9.7 sq mi). [3] The Earth's most historically active cinder cone is Cerro Negro in Nicaragua. [3] It is part of a group of four young cinder cones NW of Las Pilas volcano. Since its initial eruption in 1850, it ...

  8. Volcanic cone - Wikipedia

    en.wikipedia.org/wiki/Volcanic_cone

    A tuff cone, sometimes called an ash cone, is a small monogenetic volcanic cone produced by phreatic (hydrovolcanic) explosions directly associated with magma brought to the surface through a conduit from a deep-seated magma reservoir. They are characterized by high rims that have a maximum relief of 100–800 meters (330–2,620 ft) above the ...

  9. Tephra - Wikipedia

    en.wikipedia.org/wiki/Tephra

    The Waw an Namus volcano is surrounded by an apron of dark tephra, which has a notable color contrast to the surrounding Sahara Desert. Africa's volcanoes have had an impact on the fossil record. Geographically a part of Africa, El Hierro is a shield volcano and the youngest and smallest of the Canary Islands.