What is the mass of Earth's mantle?
Earth's mantle has a mass of 5.972 × 10^24 kilograms. This mass represents 67% of the total mass of Earth.
Short answers, pulled from the story.
Earth's mantle has a mass of 5.972 × 10^24 kilograms. This mass represents 67% of the total mass of Earth.
The Mohorovičić discontinuity was first noted by Andrija Mohorovičić on the 19th of November 1909. This boundary marks the top of the mantle and is defined by a sudden increase in seismic velocity.
The lower mantle extends from approximately 660 kilometers to 2,885 kilometers deep. This region contains stable minerals such as bridgmanite and post-perovskite.
The transition zone is located between 410 kilometers and 660 kilometers deep within Earth's mantle. This zone is where wadsleyite and ringwoodite are stable minerals.
Project Mohole was abandoned in 1966 after repeated failures and cost over-runs. The deepest penetration achieved during this project was approximately 183 meters.
The transition zone may host a large quantity of water potentially containing more water than all the oceans combined. This water exists as hydroxyl groups bound within the crystal structure of minerals.