jarðskorpuhreyfinga
Jarðskorpuhreyfinga, or tectonic plate movement, refers to the gradual movement of the Earth's lithosphere, which is divided into several large and small plates. These plates float on the semi-fluid asthenosphere beneath them and interact at their boundaries, leading to various geological phenomena. There are three main types of plate boundaries: divergent, convergent, and transform.
At divergent boundaries, plates move apart, allowing magma from the mantle to rise and form new crust.
The movement of tectonic plates is driven by convection currents in the mantle, which are caused by
Jarðskorpuhreyfinga plays a crucial role in the Earth's geological processes and has significant implications for human