Something something in a subduction zone
Yes, shallow earthquakes are common in regions near transform plate boundaries and divergent plate boundaries. These boundaries are characterized by horizontal slipping and pulling apart of tectonic plates, respectively, which can generate shallow-focus earthquakes.
All three type of Earthquakes (Shallow-seated, Medium-seated and Deep-seated) occur only at the Convergent plate boundary. At divergent plate boundary we find mostly Shallow-seated Earthquakes only.
the answer to this question is a transform boundary. At a transform boundary plates slide past one another. Because tectonic plates have irregular edges, they grind and jerk as they slide, which produces earthquakes.
Shallow focus earthquakes are associated with divergent and transform plate boundaries. These earthquakes typically occur within the top 70 kilometers of the Earth's crust and are caused by the movement of tectonic plates against each other.
Shallow earthquakes occur within the top 70 kilometers of the Earth's crust, known as the seismogenic zone. These earthquakes are typically associated with transform plate boundaries, divergent plate boundaries, and some convergent plate boundaries, where tectonic plates interact and generate seismic activity.
Shallow earthquakes typically occur at divergent plate boundaries, where two tectonic plates are moving away from each other, or at transform boundaries, where two plates slide past each other horizontally. These earthquakes are typically found at depths ranging from 0 to 70 km below the surface.
Shallow earthquakes do not often occur along the boundary of the Nazca Plate because the movement and interaction of plates at that depth do not create the conditions necessary for earthquakes to happen. Instead, deeper earthquakes occur within the subducting Nazca Plate, where there is more stress and pressure buildup due to the plate's movement beneath the South American Plate.
Earthquakes that happen in shallow water cause tsunami and other side affects like landslides.
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.
Shallow-focus earthquakes cause more damage than deep-focus earthquakes. This is because shallow-focus earthquakes originate closer to the Earth's surface, which allows the energy to be more concentrated and lead to stronger shaking and more destruction of structures. Deep-focus earthquakes, occurring deeper underground, tend to have their energy dissipate before reaching the surface.
Frequent shallow earthquakes
At divergent and transform boundaries.