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Tidal triggering of earthquakes

Adapted from Wikipedia · Explorer experience

A scientific graph showing ocean tide levels near the Golden Gate Bridge over five weeks in 1970, used to study seismic activity.

What Is Tidal Triggering?

Tidal triggering is a quiet idea about how the pull of the sun and the moon might affect when tiny shakings happen on Earth. When the sun and moon line up, they create the strongest tides. This strong pull can sometimes nudge rocks that are already ready to move.

What Scientists Have Learned

Smart people who study the planet have looked at this idea for more than a hundred years. They wondered if big quakes happen more often when tides are strong, like during new or full moons. But the answers are mixed. In many places, there isn’t a clear link between strong tides and big quakes.

Small Shakes and Volcanoes

Even though big quakes are not often triggered by tides, very small shakings can be. These small moves happen more near volcanoes. Scientists use these tiny shakings to check their tools for watching volcanoes. So, while tides don’t often start big quakes, they do help scientists learn about Earth’s quiet movements.

This article is a child-friendly adaptation of the Wikipedia article on Tidal triggering of earthquakes, available under CC BY-SA 4.0.

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