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The tectonic plate cycle involves six key steps:

  1. Mantle Convection: Heat from the Earth's core causes convection currents in the mantle, driving plate movements.
  2. Divergence: Plates move apart at mid-ocean ridges, creating new crust as magma rises to the surface.
  3. Subduction: One plate is forced beneath another at convergent boundaries, leading to the recycling of crust into the mantle.
  4. Collision: Two continental plates can collide, forming mountain ranges and causing seismic activity.
  5. Transform Boundaries: Plates slide past each other at transform faults, resulting in earthquakes.
  6. Plate Reconstruction: Over geological time, the cycle continues as plates reorganize, leading to changes in Earth's surface and new geological features.
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