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Velocity of the Earth's core
What is the core's approximate velocity?
What is the core's approximate velocity?
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Deep within our planet, the Earth's inner core is also spinning -- only it's moving faster than the surface. Every 400 years or so, it will overtake those of us riding on the outside.
This startling discovery was made when two NSF-funded seismologists working at the Lamont-Doherty Earth Observatory at Columbia University took on the challenge of investigating an unproven theory. The theory states that the inner core rotates separately from the rest of the planet, as predicted by an unproven model of the Earth's magnetic field.
Researchers Xiaodong Song and Paul Richards used seismic wave readings from 38 earthquakes between 1967 and 1995. They tracked waves that moved from the south Atlantic, through the inner core, to College, Alaska. They found that the waves in the 1990s were 0.3 seconds faster than those in the 1960s.
The Earth's core is primarily made up of iron and nickel, with smaller amounts of other elements such as sulfur and oxygen.
The temperature of the Earth's core is estimated to be between 4,000 to 5,000 degrees Celsius (7,200 to 9,000 degrees Fahrenheit).
The inner core is solid and composed mostly of iron, while the outer core is liquid due to the intense heat and pressure. The outer core is also responsible for creating the Earth's magnetic field.
Scientists use a variety of techniques, such as seismology and studying the Earth's magnetic field, to gather data and make observations about the Earth's core.
No, it is currently not possible to access the Earth's core. The deepest humans have ever drilled is only about 12 kilometers (7.5 miles) into the Earth's crust.