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  2. Middle latitudes - Wikipedia

    en.wikipedia.org/wiki/Middle_latitudes

    World map with the middle latitudes highlighted in red Extratropical cyclone formation areas. The middle latitudes, also called the mid-latitudes (sometimes spelled midlatitudes) or moderate latitudes, are spatial regions on either hemisphere of Earth, located between the Tropic of Cancer (latitude 23°26′09.7″) and the Arctic Circle (66°33′50.3″) in the northern hemisphere and ...

  3. Geology of the Canary Islands - Wikipedia

    en.wikipedia.org/wiki/Geology_of_the_Canary_Islands

    La Palma's shield-building stage began at 1.77 Ma - the Garafía shield volcano grew, on top of the seamount, between 1.77 Ma and 1.20 Ma (forming the present-day northern part of La Palma), with the oldest subaerial lavas dated to 1.7 Ma. This shield volcano grew quickly to a height of about 3,000 m (9,800 ft) and a diameter of about 23 km (14 ...

  4. Midcontinent Rift System - Wikipedia

    en.wikipedia.org/wiki/Midcontinent_Rift_System

    The Midcontinent Rift appears to have progressed almost to the point where the ocean intruded. [7] But after about 15–22 million years the rift failed. [6] [8] The Midcontinent Rift is the deepest closed or healed rift yet discovered; no known deeper rift ever failed to become an ocean. [7]

  5. Types of volcanic eruptions - Wikipedia

    en.wikipedia.org/wiki/Types_of_volcanic_eruptions

    Volcanoes known to have Surtseyan activity include: Surtsey, Iceland. The volcano built itself up from depth and emerged above the Atlantic Ocean off the coast of Iceland in 1963. Initial hydrovolcanics were highly explosive, but as the volcano grew, rising lava interacted less with water and more with air, until finally Surtseyan activity ...

  6. Hotspot (geology) - Wikipedia

    en.wikipedia.org/wiki/Hotspot_(geology)

    The volcano erupted from 1983 to 2018 and is part of the Hawaiian–Emperor seamount chain. Mauna Loa is a large shield volcano. Its last eruption was in 2022 and it is part of the Hawaiian–Emperor seamount chain. Bowie Seamount is a dormant submarine volcano and part of the Kodiak-Bowie Seamount chain.

  7. Trans-Mexican Volcanic Belt - Wikipedia

    en.wikipedia.org/wiki/Trans-Mexican_Volcanic_Belt

    The Trans-Mexican Volcanic Belt (Spanish: Eje Volcánico Transversal), also known as the Transvolcanic Belt and locally as the Sierra Nevada (Snowy Mountain Range), [4] is an active volcanic belt that covers central-southern Mexico. Several of its highest peaks have snow all year long, and during clear weather, they are visible to a large ...

  8. Volcanism of Iceland - Wikipedia

    en.wikipedia.org/wiki/Volcanism_of_Iceland

    Over the past 500 years, Iceland's volcanoes have produced a third of the total global lava output. [7] Current productivity, which is known to be cyclical, has been estimated to be between 0.05–0.08 km 3 (0.012–0.019 cu mi) per year which is higher than the output rate of the Hawaiian volcanoes, and would be double or even triple this ...

  9. Soufrière Hills - Wikipedia

    en.wikipedia.org/wiki/Soufrière_Hills

    The 9 October 2008 issue of the journal Science suggested that two interconnected magma chambers lie beneath the surface of the volcano on Montserrat – one six kilometres below the surface and the other 12 kilometres (7.5 mi) below the surface. The journal also showed a link between surface behaviour and the size of the deeper magma chamber.

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