no, the outer core flows
The inner core is solid, but the mantle is the only layer of Earth that flows in currents. These currents are caused by convection. If you don't know what convection is then you might as well look it up because I don't have a good definition.
None! Unless you mean the core. The outer core is liquid.
None! Unless you mean the core. The outer core is liquid.
The flow of the liquid iron in Earth's outer core is thought to be responsible for creating the Earth's magnetic field.
The inner core is solid, but the mantle is the only layer of Earth that flows in currents. These currents are caused by convection. If you don't know what convection is then you might as well look it up because I don't have a good definition.
The question is somewhat vague, in that there are multiple inner layers of the Earth.The mantle, though considered a solid, is of extremely high viscosity due to heat, and will move slowly over time. The outer core acts as a liquid and despite enormous pressures, does flow around the inner core, creating the magnetosphere. The inner core is thought to be a solid without flow characteristics.
crust = solid mantle = solid soft enough to flow though outer core = liquid iron inner core = solid iron
None! Unless you mean the core. The outer core is liquid.
of a planet; it has three layers, the crust,( the top) the mantle (the thickest part) and the core (the center) the outer core is just the outermost parts of the core, as opposed to the inner core
None! Unless you mean the core. The outer core is liquid.
None! Unless you mean the core. The outer core is liquid.
because they move with a flow. liquid flow down the ground, gases flow in currents
It does. We call this current, or currents, 'eddy currents', and they are minimised by using laminated cores.
The outer core of the mantle can be liquid.
the crust and the inner core
The Earth has a layered structure consisting of the inner core, outer core, mantle, and crust. The inner core is solid iron, the outer core is liquid iron, the mantle is mostly solid but can flow like a very thick liquid over long timescales, and the crust is the Earth's thin outer shell where we live. This structure is known as the "D-layered Earth model."