Yes, but not as often as earthquakes happen near plate boundaries
yes
Earthquakes infrequently occur away from plate boundaries. Most earthquakes occur at plate boundaries because of the stress caused by the interacting plates.
Volcanoes and earthquakes are often found along tectonic plate boundaries where there are faults. In the case of volcanoes, they can form at subduction zones where one tectonic plate is being forced below another. Earthquakes occur along faults, which are fractures in the Earth's crust where tectonic plates move past each other.
Shallow-focus earthquakes occur within the upper 70 kilometers of the Earth's crust. These earthquakes are typically more destructive than deep-focus earthquakes because they are closer to the Earth's surface. Shallow-focus earthquakes are often associated with tectonic plate boundaries and faults.
Earthquakes occur more frequently near plate boundaries, where tectonic plates interact and create stress along faults. These interactions often result in sudden release of energy, causing earthquakes. In contrast, earthquakes far away from plate boundaries are less common but can still occur due to other geological processes like volcanic activity or human-induced activities.
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 most often along the boundaries of tectonic plates.
Not all they can occur inside plates due to slip on a fault or fracture, they can also occur after mass wasting events (landslides) and due to volcanic activity where as magma shifts underground it breaks up rocks causing small earthquakes often refered to as magmatic tremor.
Approximately 90% of earthquakes occur at or near tectonic plate boundaries. These boundaries are where the Earth's plates interact—diverging, converging, or sliding past one another—resulting in significant geological activity. The remaining earthquakes occur within tectonic plates, often referred to as intraplate earthquakes.
Earthquakes that occur away from plate boundaries are typically referred to as intraplate earthquakes. These seismic events can happen due to the reactivation of ancient faults or fractures within tectonic plates, often caused by tectonic stresses that build up over time. Additionally, they may result from human activities, such as mining or reservoir-induced seismicity. While less frequent than those at plate boundaries, intraplate earthquakes can still be damaging and pose significant risks to nearby populations.
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.
Earthquakes occur most often along tectonic plate boundaries, specifically at convergent boundaries where one plate sinks beneath another (subduction zones) or at transform boundaries where two plates slide past each other horizontally. Additionally, earthquakes can also occur within plates themselves due to intraplate stress and faulting.