Examples of using Outer core in English and their translations into Indonesian
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Colloquial
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Ecclesiastic
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Computer
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Ecclesiastic
is not entirely understood, but its almost certainly made within the outer core layer of countries around the world,
It is normally believed that convection in the outer core, combined with stirring brought on by the Earth's rotation gives rise to the Earth's magnetic field by way of a process described by the dynamo theory.
(2) A complete numerical simulation of the motions taking place in the outer core would make it necessary to cover a wide range of scales with a very small time step, which is out of reach with current capabilities.
It is generally believed that convection in the outer core, combined with stirring brought on by the Earth's rotation provides rise to the Earth's magnetic field by way of a method described by the dynamo theory.
a solid inner core surrounded by a liquid outer core, separated by what has come to be called the Lehmann Discontinuity.
impacts the liquid outer core on which the tectonic plates that form the Earth's crust rest.
mantle, outer core and inner core, and then get recorded on seismograms all over the world.
the Pacific where the lowermost mantle is hotter than average, the outer core below those areas can become hot enough to start melting the inner core. .
mantle, outer core and inner core, and then get recorded on seismograms all over the world.
a radius of~1,220 km[2] and a liquid outer core extending beyond it to a radius of~3,400 km.
and a fluid outer core primarily made of liquid iron with a radius of roughly 300 kilometres 190 mi.
Using computer models of convection in the outer core in conjunction with seismology data,
that an inner core exists that has physical properties different from those in the outer core.
which has physical properties that are different from those in the outer core.
This occurs mostly because it cannot dissolve the same amount of light elements as the outer core, and therefore freezing at the inner core boundary produces a residual liquid that contains more light elements than the overlying liquid.
The net flow of heat from core to mantle ensures that there's still overall freezing of outer core material and it's still growing over time,
The primary seismic waves are refracted by the liquid outer core of the Earth and are not detected between 104°
since it is processes in the inner and outer core that form the Earth's geomagnetic field.
First is the outer core.
Lehman discontinuity separates inner core and outer core.