There's the familiar thin crust of continents and ocean floors; the thick mantle of hot, semisolid rock; the molten
metal outer core; and the solid iron inner core.
Not exact matches
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Scientists had recently discovered that every 200,000 years, on average, churning in the hot liquid
metal of Earth's
outer core causes the planet's whole magnetic field to flip.
To obtain this result, they modeled Earth's
outer core using liquid sodium enclosed between two rotating concentric
metal spheres, a set - up they dubbed the Derviche Tourneur Sodium (DTS) experiment.1
This ocean of liquid
metal, the
outer core, surrounds the inner
core, which is made of solid
metal.
One of the analysis results concerning the internal structure of the Moon based upon the seismic data indicates that the satellite is considered to consist mainly of two parts: the «
core,» the inner portion made up of
metal, and the «mantle,» the
outer portion made up of rock.
The MESSENGER observations and data from the two earlier Mariner 10 flybys are consistent enough to describe a dipolar field with an active electrical dynamo in which the magnetic field is produced by electrical currents flowing in an
outer core of molten
metal (more discussion and images from MESSENGER's January 2008 flyby).