about 2,300 km
about 2,300 km
The density of the outer core is between the 10g/cm³ and 12,3g/cm³.
iner core outer core
There are differences in chemistry (the mantle is mainly ultramafic rock--the outer core is metallic), in phase (the mantle is predominately solid--the outer core is liquid), in depth (the outer core is closer to the center of the Earth), and in density (the outer core is more dense).
The inner core was discovered in 1936 by Inge Lehmann and is generally believed to be composed primarily of iron and some nickel. Its estimated density is between 12.6 to 13.0 grams to cubic centimeters.
about 2,300 km
about 2,300 km
The density of the outer core is between the 10g/cm³ and 12,3g/cm³.
iner core outer core
9.9-12.2
9.9-12.2
the muppets
There are differences in chemistry (the mantle is mainly ultramafic rock--the outer core is metallic), in phase (the mantle is predominately solid--the outer core is liquid), in depth (the outer core is closer to the center of the Earth), and in density (the outer core is more dense).
The inner core was discovered in 1936 by Inge Lehmann and is generally believed to be composed primarily of iron and some nickel. Its estimated density is between 12.6 to 13.0 grams to cubic centimeters.
its between 9.9- 12.2 g/cm3
The density of the outer core is calculated to be 10 g/cm3 and a volume of 1.719 *10 to the 20 cubic meters.
liquid