The crust is the least dense. The inner core is the most dense. So from the middle outwards the layers get less and less dense
The inner core is the least dense out of the inner core, outer core, mantle, and crust. It is composed mostly of iron and nickel, making it very dense despite being solid.
It is neither. The densest layer is the inner core. The least dense layer is the crust.
The Earth's compositional layers in order of increasing density are the crust, mantle, outer core, and inner core. The crust is the least dense layer, while the inner core is the most dense layer.
The Earth's layers, from least dense to most dense, are the crust, mantle, outer core, and inner core. The crust is the thinnest and least dense layer, primarily composed of silicate rocks. Beneath it, the mantle is denser and made up of semi-solid silicate materials. The outer core, consisting of liquid iron and nickel, is denser than the mantle, and the inner core, a solid sphere of iron and nickel, is the densest layer.
The least dense layer of the earth is the Crust , the mantle is second densest , whereas the core is the most dense layer of the earth
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The outer core, inner core, mantle, crust, water, atmosphere. This is the order from densest to least dense.
The inner core is the least dense out of the inner core, outer core, mantle, and crust. It is composed mostly of iron and nickel, making it very dense despite being solid.
inner core outter core mantle and crust
inner core outter core mantle and crust
It is neither. The densest layer is the inner core. The least dense layer is the crust.
The Earth's compositional layers in order of increasing density are the crust, mantle, outer core, and inner core. The crust is the least dense layer, while the inner core is the most dense layer.
The outer core, inner core, mantle, crust, water, atmosphere. This is the order from densest to least dense.
The Earth's layers, from least dense to most dense, are the crust, mantle, outer core, and inner core. The crust is the thinnest and least dense layer, primarily composed of silicate rocks. Beneath it, the mantle is denser and made up of semi-solid silicate materials. The outer core, consisting of liquid iron and nickel, is denser than the mantle, and the inner core, a solid sphere of iron and nickel, is the densest layer.
The least dense layer of the earth is the Crust , the mantle is second densest , whereas the core is the most dense layer of the earth
No. The crust is the least dense of Earth's layers. The inner core is the densest player.
Inner core: 2450 km thick Outer core: 2300 km thick Lower mantle: 2500 km thick Upper Mantle: 400 km thick continental crust: 30-70 km thick Oceanic Crust: 6 km thick