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  2. Types of volcanic eruptions - Wikipedia

    en.wikipedia.org/wiki/Types_of_volcanic_eruptions

    Volcanoes are not bound to one eruptive style, and frequently display many different types, both passive and explosive, even in the span of a single eruptive cycle. [3] Volcanoes do not always erupt vertically from a single crater near their peak, either. Some volcanoes exhibit lateral and fissure eruptions.

  3. Volcanology - Wikipedia

    en.wikipedia.org/wiki/Volcanology

    A volcanologist is a geologist who studies the eruptive activity and formation of volcanoes and their current and historic eruptions. Volcanologists frequently visit volcanoes, especially active ones, to observe volcanic eruptions, collect eruptive products including tephra (such as ash or pumice), rock and lava samples. One major focus of ...

  4. Volcanic plateau - Wikipedia

    en.wikipedia.org/wiki/Volcanic_plateau

    Satellite image of the Big Raven Plateau in British Columbia, Canada Rangipo Desert of the North Island Volcanic Plateau. Numerous tephra layers are visible. The Pajarito Plateau in New Mexico, United States is an example of a volcanic plateau. A volcanic plateau is a plateau produced by volcanic activity. There are two main types: lava ...

  5. Effusive eruption - Wikipedia

    en.wikipedia.org/wiki/Effusive_eruption

    A volcanic eruption is effusive when the erupting magma is volatile poor (water, carbon dioxide, sulfur dioxide, hydrogen chloride, and hydrogen fluoride), which suppresses fragmentation, creating an oozing magma which spills out of the volcanic vent and out into the surrounding area. [1]

  6. Flood basalt - Wikipedia

    en.wikipedia.org/wiki/Flood_basalt

    These are characterized by plateau landforms, so that flood basalts are also described as plateau basalts. Canyons cut into the flood basalts by erosion display stair-like slopes, with the lower parts of flows forming cliffs and the upper part of flows or interbedded layers of sediments forming slopes.

  7. Siberian Traps - Wikipedia

    en.wikipedia.org/wiki/Siberian_Traps

    The massive eruptive event that formed the traps is one of the largest known volcanic events in the last 500 million years. The eruptions continued for roughly two million years and spanned the Permian – Triassic boundary, or P–T boundary, which occurred around 251.9 million years ago.

  8. Monogenetic volcanic field - Wikipedia

    en.wikipedia.org/wiki/Monogenetic_volcanic_field

    A monogenetic volcanic field is a type of volcanic field consisting of a group of small monogenetic volcanoes, each of which erupts only once, as opposed to polygenetic volcanoes, which erupt repeatedly over a period of time. The small monogenetic volcanoes of these fields are the most common subaerial volcanic landform. [1]

  9. Category:Volcanic landforms - Wikipedia

    en.wikipedia.org/wiki/Category:Volcanic_landforms

    Volcanic landforms. Subcategories. This category has the following 33 subcategories, out of 33 total. C. Central volcanoes (1 C, 12 P) Cinder cones (6 C, 43 P)

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