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  2. Submarine volcano - Wikipedia

    en.wikipedia.org/wiki/Submarine_volcano

    Submarine volcanoes are underwater vents or fissures in the Earth 's surface from which magma can erupt. Many submarine volcanoes are located near areas of tectonic plate formation, known as mid-ocean ridges. The volcanoes at mid-ocean ridges alone are estimated to account for 75% of the magma output on Earth. [1]

  3. Chaos Crags - Wikipedia

    en.wikipedia.org/wiki/Chaos_Crags

    Chaos Crags is the youngest group of lava domes in Lassen Volcanic National Park, California.They formed as six dacite domes 1,100-1,000 years ago, one dome collapsing during an explosive eruption about 70 years later.

  4. Magma chamber - Wikipedia

    en.wikipedia.org/wiki/Magma_chamber

    A magma chamber is a large pool of liquid rock beneath the surface of the Earth. The molten rock, or magma, in such a chamber is less dense than the surrounding country rock, which produces buoyant forces on the magma that tend to drive it upwards. [1] If the magma finds a path to the surface, then the result will be a volcanic eruption ...

  5. Drachenfels (Siebengebirge) - Wikipedia

    en.wikipedia.org/wiki/Drachenfels_(Siebengebirge)

    Coordinates: 50°39′55″N 7°12′35″E. Drachenfels, view from Mehlem. The Drachenfels ("Dragon's Rock", German pronunciation: [ˈdʁaxənˌfɛls]) is a hill (321 metres (1,053 ft)) in the Siebengebirge uplands between Königswinter and Bad Honnef in Germany. The hill was formed by rising magma that could not break through to the surface ...

  6. Mono–Inyo Craters - Wikipedia

    en.wikipedia.org/wiki/Mono–Inyo_Craters

    [28]: 55 In the past 6,000 years, approximately 0.19 cubic miles (0.8 km 3) of magma has been erupted from the Inyo part of the chain. [27]: 233 The last recorded volcanic activity in the chain was at Mono Lake between the years 1720 and 1850. [37] An intrusion of magma below the lake pushed lakebed sediments upward to form Paoha Island.

  7. Aira Caldera - Wikipedia

    en.wikipedia.org/wiki/Aira_Caldera

    A prime example is the Sakurajima eruption in 1914 (approximately 1.5 km 3 in volume), which caused the magma chamber to sink 60 cm. 58 people were killed in the eruption. [4] For this amount of magma to erupt, it would take approximately 130 years for the chamber to refill as according to Dr James Hickey and his co-authors.

  8. Magmatism - Wikipedia

    en.wikipedia.org/wiki/Magmatism

    Magmatism. Geological map showing the Gangdese batholith, which is a product of magmatic activity about 100 million years ago. Magmatism is the emplacement of magma within and at the surface of the outer layers of a terrestrial planet, which solidifies as igneous rocks. It does so through magmatic activity or igneous activity, the production ...

  9. Bathymetric chart - Wikipedia

    en.wikipedia.org/wiki/Bathymetric_chart

    A bathymetric chart is a type of isarithmic map that depicts the submerged bathymetry and physiographic features of ocean and sea bottoms. [1] Their primary purpose is to provide detailed depth contours of ocean topography as well as provide the size, shape and distribution of underwater features. Topographic maps display elevation above ground ...

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