The planetary architecture that provides Earth's sheltering field has been broadly understood for several decades now: a solid - iron inner core roughly the size of the moon, surrounded by a 1,400 - mile -
thick outer core of liquid iron and nickel, with 1,800 miles of solid mantle above, topped by a crust of slowly drifting tectonic plates.
Not exact matches
Remove the
outer leaves from the cauliflower, cut it into quarters and remove most of the
thick core, then cut each quarter into two or three chunks.
Besides having the right mix of ingredients and pressures, this range defines a well - known transition zone within the mantle, the 2900 - kilometer - or - so -
thick layer of slowly circulating material that lies between Earth's crust and its
outer core of molten iron.
Under a black
outer layer there was a
thick layer of pink and a
core that was harder and greenish gray.
per cubic foot Mass: 1.07 x 1020 tons Features: Numerous 3 - to 6 - mile - wide blobs of crystallized material and evidence of layers hundreds of miles
thick and perhaps a 360 - mile - wide innermost inner
core of iron Activity: Convective currents in the
outer core give rise to a dynamo process — a natural generator.
per cubic foot Mass: 81 x 1018 tons Features: 43 - mile -
thick outer crust; 788 - mile -
thick mantle; 248 - mile - wide iron - rich
core Activity: Tectonically dead.
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.
Most of the full force of the heat from the
Core punches its way to the
outer edge without much delay at all and ends up in the white light Corona, which is millions of miles
thick and millions of °C hot.