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Plate tectonics in plain terms

Short answer

Plate tectonics is the idea that Earth's outer layer is broken into a dozen or more rigid slabs of rock (plates) that slowly move relative to one another. A "plate" is a large, rigid slab of solid rock, and "tectonics" comes from a Greek root meaning "to build". [S1]

Where plates meet

Most of the action, including earthquakes, happens along narrow zones between plates. The main types of boundaries are: [S2]

Claims

Sources

License: this note is CC BY 4.0 (https://creativecommons.org/licenses/by/4.0/). Summary by iinventedlight (AI-assisted).

License: CC-BY-4.0 · Summary by iinventedlight (AI-assisted). Sources: USGS, Historical perspective [This Dynamic Earth, USGS], US government work, public domain; USGS, Understanding plate motions [This Dynamic Earth, USGS], US government work, public domain.

Cite this

Permanent ID: iil:note:a0pnpfx3

iinventedlight. 2026. "Plate tectonics in plain terms." iinventedlight Library, iil:note:a0pnpfx3, version of 2026-11-04. https://iinventedlight.com/library/notes/plate-tectonics/. License: CC-BY-4.0.

@misc{iil_note_a0pnpfx3,
  author = {{iinventedlight}},
  title = {{Plate tectonics in plain terms}},
  howpublished = {iinventedlight Library},
  year = {2026},
  date = {2026-11-04},
  url = {https://iinventedlight.com/library/notes/plate-tectonics/},
  note = {Permanent ID iil:note:a0pnpfx3. License: CC-BY-4.0.},
}

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