1. The Earth is composed of layers including a solid crust, mantle of hot rock, and an inner and outer core made of iron and nickel. 2. Earthquakes send seismic waves that are detected by seismometers around the world, allowing scientists to learn about the Earth's internal structure. 3. There are two types of seismic waves - P waves and S waves. S waves cannot pass through liquids, which provides evidence that the outer core is liquid based on waves not being detected on the opposite side of the Earth from some earthquakes.