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  2. Dynamo theory - Wikipedia

    en.wikipedia.org/wiki/Dynamo_theory

    This has to be non-negative at least in part of the volume, for the dynamo to produce magnetic field. [19] From the diagram above, it is not clear why this term should be positive. A simple argument can be based on consideration of net effects. To create the magnetic field, the net electric current must wrap around the axis of rotation of the ...

  3. Convection - Wikipedia

    en.wikipedia.org/wiki/Convection

    Convection is also seen in the rising plume of hot air from fire, plate tectonics, oceanic currents (thermohaline circulation) and sea-wind formation (where upward convection is also modified by Coriolis forces). In engineering applications, convection is commonly visualized in the formation of microstructures during the cooling of molten ...

  4. Slab suction - Wikipedia

    en.wikipedia.org/wiki/Slab_suction

    This is how throughout the Earth's history there has been the ability to create super continents where all of the land mass has converged into one (for example, Pangaea). Slab suction occurs when a subducting slab drives flow in the lower mantle by exerting additional force down in the direction of the mantle's convection currents.

  5. Mantle convection - Wikipedia

    en.wikipedia.org/wiki/Mantle_convection

    Mantle convection is the very slow creep of Earth's solid silicate mantle as convection currents carry heat from the interior to the planet's surface. [2] [3] Mantle convection causes tectonic plates to move around the Earth's surface. [4] The Earth's lithosphere rides atop the asthenosphere, and the two form the components of the upper mantle ...

  6. Outline of plate tectonics - Wikipedia

    en.wikipedia.org/wiki/Outline_of_plate_tectonics

    Lateral density variations in the mantle result in convection currents, the slow creeping motion of Earth's solid mantle. At a seafloor spreading ridge , plates move away from the ridge, which is a topographic high, and the newly formed crust cools as it moves away, increasing its density and contributing to the motion.

  7. Plate tectonics - Wikipedia

    en.wikipedia.org/wiki/Plate_tectonics

    Lateral density variations in the mantle result in convection currents, the slow creeping motion of Earth's solid mantle. At a seafloor spreading ridge , plates move away from the ridge, which is a topographic high, and the newly formed crust cools as it moves away, increasing its density and contributing to the motion.

  8. Geophysics - Wikipedia

    en.wikipedia.org/wiki/Geophysics

    Relative to the solid Earth, the ionization of the planet's atmosphere is a result of the galactic cosmic rays penetrating it, which leaves it with a net positive charge. [22] A current of about 1800 amperes flows in the global circuit. [21] It flows downward from the ionosphere over most of the Earth and back upwards through thunderstorms.

  9. Earth's inner core - Wikipedia

    en.wikipedia.org/wiki/Earth's_inner_core

    This process creates convection currents in the outer core, which are thought to be the prime driver for the currents that create the Earth's magnetic field. [5] The existence of the inner core also affects the dynamic motions of liquid in the outer core, and thus may help fix the magnetic field. [citation needed]