When two plates move apart it forms a hole but new crust is formed.
When an earthquake occurs, lithospheric plates either slide past each other, collide, or move apart along their boundaries. The stress accumulated along the plate boundaries is released suddenly, causing the plates to deform and generate seismic waves that we feel as an earthquake.
boundaries. There are three main types of plate boundaries: divergent, where plates move apart; convergent, where plates move towards each other; and transform, where plates slide past each other horizontally. These interactions can create earthquakes, volcanic activity, and mountain formation.
Tectonic plates typically interact at their boundaries, leading to different geological phenomena such as earthquakes, volcanic activity, and the formation of mountain ranges. These interactions occur due to the movement of the plates, where they can collide, move apart, or slide against each other.
The three main plate movements are: 1) Divergent boundary, where plates move away from each other; 2) Convergent boundary, where plates move towards each other; and 3) Transform boundary, where plates slide past each other horizontally.
"Collide divide slide" is a phrase used to describe the three main types of plate boundaries: convergent (collide), divergent (divide), and transform (slide). Convergent boundaries are where plates come together, divergent boundaries are where plates move apart, and transform boundaries are where plates slide past each other.
there is faulting
Plates either move towards each other (convergent plates), away from each other (divergent plates) or slide next to each other (transform plates).
When an earthquake occurs, lithospheric plates either slide past each other, collide, or move apart along their boundaries. The stress accumulated along the plate boundaries is released suddenly, causing the plates to deform and generate seismic waves that we feel as an earthquake.
earthquake.
collide
tectonic movement can cause tectonic plates to collide, drift apart, or slide across one another
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boundaries. There are three main types of plate boundaries: divergent, where plates move apart; convergent, where plates move towards each other; and transform, where plates slide past each other horizontally. These interactions can create earthquakes, volcanic activity, and mountain formation.
Tectonic plates typically interact at their boundaries, leading to different geological phenomena such as earthquakes, volcanic activity, and the formation of mountain ranges. These interactions occur due to the movement of the plates, where they can collide, move apart, or slide against each other.
The three main plate movements are: 1) Divergent boundary, where plates move away from each other; 2) Convergent boundary, where plates move towards each other; and 3) Transform boundary, where plates slide past each other horizontally.
"Collide divide slide" is a phrase used to describe the three main types of plate boundaries: convergent (collide), divergent (divide), and transform (slide). Convergent boundaries are where plates come together, divergent boundaries are where plates move apart, and transform boundaries are where plates slide past each other.
It happens when two stressed plates slide pass each other