Plate tectonics is the scientific theory explaining the movement of Earth's lithospheric plates, which shapes continents, forms mountains, and triggers earthquakes. The rock cycle describes how rocks transform between igneous, sedimentary, and metamorphic forms through processes like melting, cooling, erosion, and pressure. Together, plate tectonics and the rock cycle illustrate how Earth's surface continuously changes, recycling materials and driving geological activity over millions of years.
Plate tectonics is the scientific theory explaining the movement of Earth's lithospheric plates, which shapes continents, forms mountains, and triggers earthquakes. The rock cycle describes how rocks transform between igneous, sedimentary, and metamorphic forms through processes like melting, cooling, erosion, and pressure. Together, plate tectonics and the rock cycle illustrate how Earth's surface continuously changes, recycling materials and driving geological activity over millions of years.
What is plate tectonics?
Plate tectonics is the theory that Earth's lithosphere is divided into moving plates that drift over the mantle. Their interactions shape continents and mountains and cause earthquakes and volcanoes.
What are the main plate boundary types and their features?
Divergent boundaries push plates apart (mid‑ocean ridges), convergent boundaries collide (subduction zones and mountain belts), and transform boundaries slide plates past each other (fault lines). Each type yields different geologic activity.
How do plate motions create mountains and earthquakes?
Collisions and interactions at boundaries uplift crust to form mountains; rocks store energy and rupture at faults, causing earthquakes. Subduction can also drive volcanic activity.
What is the rock cycle and its three main rock types?
The rock cycle describes rocks transforming among igneous, sedimentary, and metamorphic forms through melting, cooling, weathering/erosion, deposition, burial, and metamorphism.