Most earthquake energy is transported through the earth's crust in the form of seismic waves. These waves are vibrations that travel through the ground, and they can cause the ground to shake, rock, or roll. The energy of an earthquake is transported by these waves, and the intensity of the shaking depends on the magnitude of the earthquake and the distance from the epicenter.

There are two main types of seismic waves: body waves and surface waves. Body waves travel through the interior of the earth, while surface waves travel along the earth's surface. Body waves are faster than surface waves, so they are the first to arrive at a seismic station after an earthquake. Surface waves are slower, but they can cause more damage because they have a longer wavelength and can shake the ground more violently.

The energy of an earthquake is also transported through the earth's crust in the form of heat. This heat is generated by the friction between the rocks that move during an earthquake. The heat can cause the rocks to melt, and this molten rock can rise to the surface and form volcanoes.

The energy of an earthquake can also be transported through the earth's crust in the form of electrical energy. This electrical energy is generated by the movement of the rocks during an earthquake. The electrical energy can cause power outages, and it can also interfere with communications systems.

The energy of an earthquake can also be transported through the earth's crust in the form of sound waves. These sound waves are generated by the shaking of the ground, and they can travel for long distances. The sound waves can be heard by people, and they can also be used to detect earthquakes.