Thrust or compressive motion.
No, divergent motion does not create reverse faults. Reverse faults are created by compressional forces that cause the rock layers to be pushed together, leading to an upward movement on one side of the fault. Divergent motion, on the other hand, occurs when two tectonic plates move away from each other, creating rift zones and normal faults.
The plates of the lithosphere are in constant slow motion due to convection currents in the Earth's mantle. Heat from the Earth's core causes magma to rise, cool, and sink, creating a circular motion that moves the plates. This process is known as plate tectonics.
One of the three types of plates are the transform plates slip past each other. The convergent plates push together. The divergent plates pull away from each other.
One of the three types of plates are the transform plates slip past each other. The convergent plates push together. The divergent plates pull away from each other.
A convergent boundary can form between two plates and a divergent boundary can be created between two plates, then two plates rubbing together create earthquakes, many are very minor. A convergent boundary is two plates pushing together to form a mountain, hill, or volcano. Divergent plates move apart and create canyons and stuff.
They can move apart or in some rare cases together.
Two plates are being smashed together creating the Himalayas.
When two plates move towards each other, it is called convergence. The motion during convergence is usually called subduction if one plate is forced beneath the other, or collision if the two plates collide and form mountain ranges.
Yes, convergent motion occurs where two tectonic plates push together. This movement leads to the formation of features such as mountains, volcanoes, and deep ocean trenches due to the intense pressure and geological activity at the plate boundaries.
The motion of the continental plates on Earth is primarily driven by the process of mantle convection. Heat from Earth's core causes the rock in the mantle to slowly move, creating convection currents that push and pull the plates along with them. This movement leads to the drifting and collision of the plates, shaping the Earth's surface over millions of years.
Continental drift is the theory that "plates" on the Earth are constantly in motion and have been for millions of years. Tectonic plates are the actual moving plates.
A deep ocean trench is likely to form where two oceanic plates push together in a convergent boundary. This is because one of the plates subducts beneath the other, creating a deep trench.