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Guyot. In marine geology, a guyot ( / ˈɡiː.oʊ, ɡiːˈoʊ / ), [ 1][ 2] also called a tablemount, is an isolated underwater volcanic mountain ( seamount) with a flat top more than 200 m (660 ft) below the surface of the sea. [ 3] The diameters of these flat summits can exceed 10 km (6 mi). [ 3] Guyots are most commonly found in the Pacific ...
Mount Mazama ( Tum-sum-ne in the Native American language Klamath [ 5]) is a complex volcano in the western U.S. state of Oregon, in a segment of the Cascade Volcanic Arc and Cascade Range. A volcanic peak once existed, but it collapsed following a major eruption approximately 7,700 years ago, to be replaced by a caldera.
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 ...
Magma. Magma can be found in the mantle or molten crust. Magma (from Ancient Greek μάγμα (mágma) 'thick unguent ') [ 1] is the molten or semi-molten natural material from which all igneous rocks are formed. [ 2]
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 ...
Phreatic eruption at the summit of Mount St. Helens, Washington, in the spring of 1980. A phreatic eruption, also called a phreatic explosion, ultravulcanian eruption or steam-blast eruption, [ 1] occurs when magma heats ground water or surface water. The extreme temperature of the magma (anywhere from 500 to 1,170 °C (930 to 2,100 °F ...
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