levykiteitä
Levykiteitä, often translated as "plate tectonics" in English, is a scientific theory that describes the large-scale motion of the Earth's lithosphere. The lithosphere, the rigid outer shell of the planet, is broken into numerous pieces called tectonic plates. These plates float on the semi-fluid asthenosphere beneath them, which is part of the upper mantle.
The movement of these plates is driven by convection currents within the Earth's mantle. Hotter, less dense
The interactions at these plate boundaries are responsible for many of Earth's major geological features and
The theory of levykiteit provides a unifying framework for understanding earthquakes, volcanic activity, mountain building, and