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transform plate boundary

geology
Also known as: side-slipping plate boundary, strike-slip plate boundary(Show More)

Quick Summary

A transform plate boundary is a geological feature where two tectonic plates slide past each other horizontally. This movement occurs along large fractures in the Earth's crust known as transform faults. These boundaries are considered "conservative" because they neither create nor destroy crustal material.12

The interaction along transform faults can cause stress to build up when the plates lock. This stored energy can be suddenly released, resulting in earthquakes. Famous examples of transform faults include the San Andreas Fault in California and the North Anatolian fault system in Turkey. These boundaries are crucial in understanding the dynamics of plate tectonics and seismic activity on Earth.134

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