Reverse faults, in contrast, form in regions where the crust is being compressed. These compressional forces cause the hanging wall to move upward relative to the footwall.

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Reverse faults are the opposite: plates push together, and the resting side is shoved up and over. There are other types and subtypes of faults represented around the world, ...

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The earthquake was a reverse fault type, where the active fault directly beneath the northern part of the Noto Peninsula moved vertically.

The second is a reverse fault, where plates pushing against each other build compressional stress. This forces one plate to rise overtop of the other and the area is shortened.

The earthquake resulted from a geological phenomenon called a “reverse fault”. This occurs when tectonic plates collide, causing the Earth’s crust to thicken.

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Thrust, or reverse, faults are features in the Earth’s crust that occur when a massive slab of rock moves up and over a lower block of rock, which moves deeper into the Earth, Aron explained.

What caused the earthquake? So far, the explanation is that the quake happened when a reverse fault – where the edge of the rock on one side of a fault slips under the other – occurred between ...

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