What happens to the energy produced by blocks of Earth’s crust slipping past each other?(1 point) Responses It increases as it reaches the surface. It increases as it reaches the surface. It radiates outward in all directions. It radiates outward in all directions. It disappears at it moves through the crust. It disappears at it moves through the crust. It spreads out in random directions. It spreads out in random directions.
It radiates outward in all directions.
What happens to the energy produced by blocks of Earth’s crust slipping past each other?(1 point) Responses It increases as it reaches the surface. It increases as it reaches the surface. It radiates outward in all directions. It radiates outward in all directions. It disappears at it moves through the crust. It disappears at it moves through the crust. It spreads out in random directions. It spreads out in random directions.
It radiates outward in all directions.
The energy produced by blocks of Earth's crust slipping past each other radiates outward in all directions.
The correct answer is: "It radiates outward in all directions."
When two blocks of Earth's crust slip past each other, it results in an earthquake. During an earthquake, energy is released in various forms, such as seismic waves. Seismic waves carry the energy from the point of slip and radiate outward in all directions from the earthquake's epicenter. These waves can propagate through the Earth's interior, traveling through the crust, mantle, and even the core. As the waves move through the Earth, they gradually lose energy due to the resistance encountered by the rocks they pass through.
To determine the correct answer, one can understand earthquake mechanics and the behavior of seismic waves. Earthquakes occur due to the release of accumulated stress along faults, where blocks of Earth's crust slip past each other. As the crustal rocks deform and slip, they generate seismic energy, which then propagates as waves through the Earth's layers. This energy spreads out in all directions, leading to the shaking and vibrations felt during an earthquake.
By considering the nature of seismic waves and their behavior during an earthquake, we can conclude that the energy produced by blocks of Earth's crust slipping past each other radiates outward in all directions.