Here's a breakdown:
* Lithosphere: This is the rigid outermost layer of the Earth, composed of the crust and the uppermost part of the mantle. It's broken into large pieces called tectonic plates.
* Tectonic Plates: These plates are constantly moving, interacting with each other, and causing various geological phenomena like earthquakes, volcanoes, and mountain formation.
So, while the Earth's crust is where we see the direct evidence of plates (like continents and ocean floors), it's the lithosphere as a whole that contains these plates and allows them to move.
