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  2. 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 ...

  3. 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.

  4. Lake Toba - Wikipedia

    en.wikipedia.org/wiki/Lake_Toba

    In 2016, a study revealed that the Toba Supervolcano has a magma chamber containing 50,000 cubic kilometres (12,000 cu mi) of eruptible magma, about 30–50 kilometres (19–31 mi) underground. [30] This makes the supervolcano's magma chamber more than four times larger than the volume of Lake Superior in North America, and also larger than the ...

  5. Hydrothermal circulation - Wikipedia

    en.wikipedia.org/wiki/Hydrothermal_circulation

    Hydrothermal also refers to the transport and circulation of water within the deep crust, in general from areas of hot rocks to areas of cooler rocks. The causes for this convection can be: Intrusion of magma into the crust. Radioactive heat generated by cooled masses of granite. Heat from the mantle. Hydraulic head from mountain ranges, for ...

  6. Caldera - Wikipedia

    en.wikipedia.org/wiki/Caldera

    Caldera. A caldera (/ kɔːlˈdɛrə, kæl -/ [1] kawl-DERR-ə, kal-) is a large cauldron -like hollow that forms shortly after the emptying of a magma chamber in a volcanic eruption. An eruption that ejects large volumes of magma over a short period of time can cause significant detriment to the structural integrity of such a chamber, greatly ...

  7. Geothermal areas of Yellowstone - Wikipedia

    en.wikipedia.org/wiki/Geothermal_areas_of...

    This in turn released the enclosed magma as lava and caused the surface above the emptied magma chamber to collapse. [20] Water later filled the collapsed area of the caldera, forming an extension of Yellowstone Lake. This created the source of heat and water that feed the West Thumb Geyser Basin today. Geyser cone under water at West Thumb ...

  8. Volcanic and igneous plumbing systems - Wikipedia

    en.wikipedia.org/wiki/Volcanic_and_igneous...

    Volcanic and igneous plumbing systems (VIPS) consist of interconnected magma channels and chambers through which magma flows and is stored within Earth's crust. [ 1] Volcanic plumbing systems can be found in all active tectonic settings, such as mid-oceanic ridges, subduction zones, and mantle plumes, when magmas generated in continental ...

  9. Ancient ocean of magma found on Moon south pole

    www.aol.com/ancient-ocean-magma-found-moon...

    The Moon’s south pole was once covered in an ocean of liquid molten rock, according to scientists. The findings back up a theory that magma formed the Moon's surface around 4.5 billion years ago.