convecting's Usage Examples:

to gravity that drives the convection or a larger distance through the convecting medium.

mechanical boundary layer that heats via conduction and the asthenosphere is a convecting adiabatic layer.

The dynamo theory describes the process through which a rotating, convecting, and electrically conducting fluid can maintain a magnetic field over.

unusual location and wide wind field, the system had a well-defined centre convecting around a warm core.

Overshoot is caused by the momentum of the convecting material, which carries the material beyond the unstable region.

a mobile, fractured lithosphere cyclically recycled into a vigorously convecting mantle, in a process commonly known as plate tectonics.

Transient uplift can occur over a thermal anomaly due to convecting anomalously hot mantle, and disappears when convection wanes.

interface between the cratonic continental lithosphere and the underlying convecting asthenospheric mantle.

observations, there are numerous surface features that indicate an actively convecting interior.

The presence of a stagnant lid above a convecting mantle was recognised as a possible stable regime for convection on Earth.

solid mantle to behave plastically, resulting in parts of the mantle convecting upward since it is lighter than the surrounding rock.

explained as different stages of the fractional crystallization of the convecting core of the parent body.

gravity that drives the convection, and/or a larger distance through the convecting medium.

of the planet, thought to be caused by a narrow stream of hot mantle convecting up from the mantle-core boundary called a mantle plume.

These are thought to be caused by a narrow stream of hot mantle convecting up from the Earth's core–mantle boundary called a mantle plume, although.

exist in large quantities in extraterrestrial environments as brine or convecting ice.

Heat flow from the core is necessary for maintaining the convecting outer core and the geodynamo and Earth's magnetic field; therefore primordial.

oceanic crust is "pulled" or sinks down into the mantle over the downward convecting limb of a mantle cell.

boundary layer of the convecting mantle.

This coupling between rigid plates moving on the surface of the Earth and the convecting mantle is called plate.

High resolution LORRI mosaic of a convecting region of Sputnik Planitia (context), up to its northwestern 'shoreline' (released 7 January 2016).

Synonyms:

circulate;

Antonyms:

stay in place;