Here's why:
* The Lithosphere is broken: The lithosphere, the rigid outer layer of the Earth, is not a single solid piece. It's broken into large pieces called tectonic plates.
* Continents and Ocean Floors: These plates include both continents and the ocean floor.
* Constant Motion: The plates are constantly moving very slowly, driven by the convection currents in the Earth's mantle.
* Interlocking Pieces: As the plates move, they interact with each other at their boundaries, creating various geological phenomena. They collide, pull apart, or slide past each other, like pieces of a giant jigsaw puzzle.
Here are some examples of how this "jigsaw" works:
* Mountain Ranges: When plates collide, they can push up mountains, like the Himalayas.
* Earthquakes: Plates sliding past each other cause earthquakes, like the San Andreas Fault in California.
* Volcanoes: Where plates pull apart, magma from the Earth's mantle can rise to the surface, creating volcanoes.
* Ocean Trenches: At subduction zones, where one plate slides beneath another, deep ocean trenches can form.
So, while the Earth's lithosphere isn't literally a jigsaw puzzle, the way the plates fit together and move relative to each other creates a fascinating and complex system that has shaped our planet's surface over billions of years.