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Most of Earth's volume is contained in the mantle, which is the layer between the crust and the core. The mantle makes up about 84% of Earth's volume and is composed of solid rock that can flow slowly over long periods of time.
The Earth's volume is primarily composed of its layers: the inner core, outer core, mantle, and crust. These layers consist of different materials like iron, nickel, oxygen, silicon, and magnesium. The core is mostly made of iron and nickel, while the mantle is rich in silicate minerals.
The approximate percent of oxygen in Earth's lower atmosphere is around 20.95% by volume.
80%
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The mantle.
85%.
Most of earth's volume has been scientifically proved to be in the earth's mantle.
80 %
The Earth's mantle makes up about 84% of the planet's total volume.
Most of Earth's volume is contained in the mantle, which is the layer between the crust and the core. The mantle makes up about 84% of Earth's volume and is composed of solid rock that can flow slowly over long periods of time.
The mantle is 82% of Earth's volume. It is composed of ultramafic rock called peridotite, which is hot enough to flow.
It's the mantel.
mantle.
Less than 1%.
The Earth's volume is primarily composed of its layers: the inner core, outer core, mantle, and crust. These layers consist of different materials like iron, nickel, oxygen, silicon, and magnesium. The core is mostly made of iron and nickel, while the mantle is rich in silicate minerals.
The approximate percent of oxygen in Earth's lower atmosphere is around 20.95% by volume.