The most abundant element in both the Earth's inner core and outer core is iron. It makes up about 85% of the Earth's core composition.
Of the Earth, both the Inner Core and the Outer Core are believed to consist of a nickel iron mixture. The Inner Core is solid on account of the immense pressure. The Outer Core is a similar chemical composition, but with less pressure it behaves like a very viscous liquid. The Outer Core extends from about 1200 km to 3400km radius.
There are four main layers of the Earth: the crust, the mantle, the outer core, and the inner core. These layers differ in composition, temperature, and state of matter.
The Earth's core is the layer that is most similar in composition to an iron-nickel meteorite. The core is divided into an outer liquid layer and an inner solid layer, and both contain a high concentration of iron and nickel, similar to the composition of iron-nickel meteorites.
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the outer core
It is because the outer core is not under enough pressure to be solid, so it is liquid even though it has a composition similar to that of the inner core.
Dynamo theory is the idea that a magnetic field generator exists within the Earth's outer core. It is this generator that explains the difference between the inner and outer core.
Dynamo theory is the idea that a magnetic field generator exists within the Earth's outer core. It is this generator that explains the difference between the inner and outer core.
The Earth's interior has several layers in order from outer to inner: the crust, mantle, outer core, and inner core. These layers vary in composition, temperature, and physical properties.
The most abundant element in both the Earth's inner core and outer core is iron. It makes up about 85% of the Earth's core composition.
Of the Earth, both the Inner Core and the Outer Core are believed to consist of a nickel iron mixture. The Inner Core is solid on account of the immense pressure. The Outer Core is a similar chemical composition, but with less pressure it behaves like a very viscous liquid. The Outer Core extends from about 1200 km to 3400km radius.
The Earth's layers of rock are classified by their composition and physical properties. The main layers are the crust (continental and oceanic), mantle, and core (outer and inner). These layers are distinguished by differences in chemical composition, density, and temperature.
silicon, aluminum, calcium, sodium and potassium
The inner core appears to be solid, the outer core liquid. Composition is roughly the same nickel-iron mix. Pressure and temperature are greater in the inner core.The inner core is also beneath the mantke
The Earth's outer core is primarily composed of iron and nickel, with some smaller amounts of sulfur and oxygen. These elements are in a liquid state due to the high temperatures and pressures in the outer core. The composition is important for generating the Earth's magnetic field through the movement of the molten metal.