How do moonquakes and earthquakes differ?

Moonquakes and earthquakes have fundamental differences in their characteristics and effects. The correct information highlights that moonquakes can affect the entire Moon, leading to broader vibrations compared to earthquakes, which are primarily localized phenomena.

Moonquakes occur due to the Moon’s unique geological processes, including tidal forces from Earth, which can cause the Moon’s crust to shift. As a result, the seismic waves generated by moonquakes can propagate throughout the Moon, resulting in vibrations that can be felt over large areas.

In contrast, earthquakes are typically caused by tectonic activity within Earth's crust and are usually focused around a fault line or specific region, resulting in localized shaking with varying intensities depending on the depth and magnitude of the quake.

This distinction emphasizes how the Moon's lack of tectonic plates and its different geological environment lead to various seismic activity patterns compared to Earth. Understanding these differences contributes to our knowledge of planetary geology and helps in comparing seismic activity across celestial bodies.