Earth's core
The Earth's core is the central part of our planet, divided into a solid Inner core and a liquid Outer core, made up of Iron and Nickel and reaching temperatures of up to 6,000 degrees Celsius. The core is responsible for generating the Earth's Magnetic field, which protects the planet from harmful Solar wind and Cosmos radiation. The Earth's core is also believed to play a crucial role in the planet's Geodynamics, including the movement of Tectonic plates and the creation of Earthquakes. Scientists study the Earth's core using Seismology and Gravity measurements, which help us understand the core's composition, temperature, and movement. The Earth's core is a complex and fascinating topic, closely related to the study of Geophysics and the Earth as a whole.