What do u know about structure of earth?
The interior of the Earth, similar to the other terrestrial planets, is chemically divided into layers. The Earth has an outer silicate solid crust, a highly viscous mantle, a liquid outer core that is much less viscous than the mantle, and a solid inner core. Many of the rocks now making up the Earth’s crust formed less than 100 million (1×108) years ago; however the oldest known mineral grains are 4.4 billion (4.4×109) years old, indicating that the Earth has had a solid crust for at least that long.[1] Much of what is known about the interior of the Earth has been inferred. The force exerted by Earth’s gravity is one measurement of its mass. After measuring the volume of the planet, its density can be calculated. Astronomers also have performed similar planetary measurements. Calculation of the mass and volume of the surface rocks and bodies of water allow estimation of the mass, volume and density of surface rocks. The mass which is not in the atmosphere, oceans, and surface rocks
Structure of the Earth The Earth is an oblate spheroid. It is composed of a number of different layers as determined by deep drilling and seismic evidence . These layers are: The core which is approximately 7000 kilometers in diameter (3500 kilometers in radius) and is located at the Earth’s center. The mantle which surrounds the core and has a thickness of 2900 kilometers. The crust floats on top of the mantle. It is composed of basalt rich oceanic crust and granitic rich continental crust. The core is a layer rich in iron and nickel that is composed of two layers: the inner and outer cores. The inner core is theorized to be solid with a density of about 13 grams per cubic centimeter and a radius of about 1220 kilometers. The outer core is liquid and has a density of about 11 grams per cubic centimeter. It surrounds the inner core and has an average thickness of about 2250 kilometers. The mantle is almost 2900 kilometers thick and comprises about 83% of the Earth’s volume. It is compo
