Faults occur because the forces of plate motion push or pull the crust so much that the crust breaks.
The fault often occurs along plate boundaries because the pressure of the plates along the edges of the touching plates creates tremors. They can push each other up and possibly make mountains or subtract the others.
Yes, but not as often as earthquakes happen near plate boundaries
yes
Mountains are most often formed on faults. Because these faults occur due to the space between tectonic plates, these faults take the form of lines. Thus, the thin belts are along these long lines.
fault
Earthquakes infrequently occur away from plate boundaries. Most earthquakes occur at plate boundaries because of the stress caused by the interacting plates.
Earthquakes occur most often along the boundaries of tectonic plates.
Faults occur near plate boundaries because the earth is weaker there... The magma under the Earth's crust makes the plates move very slowly and sometimes two plates can crash into each other causing the ground to shake.
Earthquakes occur along faults, where two blocks for rock move against one another. The blocks snag on one another, build up stress, and then release it as an earthquake. Most active faults are found at or near plate boundaries, where two large segments of the crust move past each other. The relatively large amount of movement and stress compared to intraplate settings means there are more and larger faults, which leads to more frequent and stronger earthquakes.
Faults are breaks in the crust where the crust has moved. The types of dip-slip faults are normal and reverse faults. In both of these, the movement is along the slope of the fault. Sudden movements along these faults can produce fault scarps. Layers of rock being misaligned is evidence of fault movement. Fault creep is caused by slow movement along the fault.In a normal fault, the plates are moving away from each other. This is due to tension. When the fault moves, the footwall rises relative to the hanging wall. Normal faults occur at divergent boundaries, such as ocean ridges. Normal faults can produce fault-block mountains.In a reverse fault, the plates are moving towards each other. This is due to compression. Here, the footwall falls relative to the hanging wall. A thrust fault is a special type of reverse fault, where the angle is shallow. Reverse faults occur at convergent boundaries, like subduction zones.A strike-slip fault is where the two plates move horizontally past each other. The force between them is called shearing. This type of fault is often called a transform fault, because they occur at transform boundaries.
near the boundaries
Usually along convergent plate boundaries, but they can also occur at divergent plate boundaries and hotspots.
Volcanoes are most often found along plate boundaries. Here, conditions cause rocks in the upper mantle to melt, either by introducing volatiles or by reducing pressure.