The magnetic field is extremely important to sustaining life on Earth. Without it, we would be exposed to high amounts of radiation from the Sun and our atmosphere would be free to leak into space.
NASA will land the first woman on the Moon, using innovative technologies to explore more of the lunar surface than ever before establishing the first long-term presence on the Moon. Then, learnings and discoveries around the Moon will be used in the next giant leap: sending the first astronauts to Mars.
NASA's Perseverance Mars rover landed on the Red Planet on Feb. 18, 2021. Perseverance's mission on Mars is astrobiology, the search for signs of ancient microbial life. The rover will characterize the planet's geology and past climate, pave the way for human exploration of the Red Planet, and be the first mission to collect Martianrock.
Lies beneath the crust and extends to a depth of 2,900 km, made up of very hot and dense rocks which flow due to great differences in temperature moving from the bottom to the top, called convection currents
Divided into a solid inner core and a liquid outer core
Inner core is an extremely dense, solid metal ball with a radius of 1,220 km, made mostly of iron and nickel
Outer core is made from iron and nickel, in liquid form, sitting 5,180 to 2,880 km below the surface, heated largely by the radioactive decay of uranium and thorium
Earth's magnetic field is caused by a dynamo effect. The earth's liquid outer core motion generates electrical currents that generates the earth's magnetic field.
The same process as a dynamo light on a bicycle, where magnets in the dynamo start spinning when the bicycle is pedaled, creating an electric current which is then used to turn on the light. This process also works in reverse, where a rotating electric current will create a magnetic field.
Mars doesn't have flowing liquid metal in its core, it doesn't produce the same dynamo effect. The red planet has a very weak magnetic field, allowing for its atmosphere to be stripped away by solar winds, leaving it uninhabitable.
The inner core spins a bit faster than the rest of the planet. It's also intensely hot: Temperatures sizzle at 5,400° C (9,800° F) almost as hot as the surface of the sun, 3 million times greater than on Earth's surface.
Scientists know a great deal about Earth's inner structure by studying how earthquake waves travel through the planet. The speed and behavior of these waves change as they encounter layers of different densities. They have also learned about the core and mantle from calculations of Earth's total density, gravitational pull and magnetic field.
The mass of air surrounding our planet, subdivided into different layers of different densities
Most of the gas is nitrogen (78%) or oxygen (21%), with the remaining 1% a mixture of other gases
The "thickest" air is right above Earth's surface, becoming increasingly thinner with increasing altitude due to gravity pulling the air molecules down
If you squeeze a quartz crystal, it generates a tiny electric voltage. The opposite is also true: if you apply a voltage to a piece of quartz, it vibrates at a precise frequency. This ability is called "Piezoelectric effect"
When an irritant works its way into a particular species of oyster, mussel, or clam, the mollusk secretes a fluid to coat the irritant. Layer upon layer of this coating is deposited on the irritant until a lustrous pearl is formed.
Flat surfaces that are formed from breakage are called cleavage. Minerals that do not exhibit cleavage planes have strong chemical bonds between atoms.