Stress due to the subduction of tectonic plates into Earth's mantle.
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.
Very little, as the earthquake occurs deep underground, hence the deep focus.
No, the absence of deep focus earthquakes along the oceanic ridge system is not inconsistent with the theory of plate tectonics. Deep focus earthquakes typically occur in subduction zones, where one tectonic plate is sinking beneath another. Oceanic ridges are areas where new oceanic crust is formed and plates are moving apart, which does not typically generate deep focus earthquakes.
Shallow focus earthquakes occur closer to the Earth's surface (up to 70 km deep) and typically have higher magnitudes due to proximity to the Earth's brittle crust. Deep focus earthquakes occur at depths of 300-700 km within the subducting slab in a subduction zone and are usually associated with more intense pressure and temperature conditions, resulting in unique seismic waves and less damage on the Earth's surface.
yes they do
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.
It depends, but 'shallow' (refering to the 'focus') earthquakes hit, usally, with a bigger force. This is because if the focus is closer to the surface of the earth (like in the Kobe earthquake) then the siesmic waves do not have as far to travel to reach the surface. But you can still have a deep focus with a big impact: if the siesmic waves are more powerful.
deep focus
Deep focus earthquakes are seismic events that occur at depths greater than 300 kilometers (approximately 186 miles) within the Earth's crust or upper mantle. They are typically associated with subduction zones, where one tectonic plate is forced beneath another. These earthquakes can release significant amounts of energy and are less common than shallow earthquakes, which occur at shallower depths. Due to their depth, deep focus earthquakes often produce less surface shaking compared to shallow ones, but they can still be felt over large distances.
what is the maximum depth of a deep-focus earthquake
Most deep-focus earthquakes occur in subduction zones, where one tectonic plate is being forced beneath another. These earthquakes typically occur at depths ranging from 300 to 700 kilometers below the Earth's surface. The deeper focus of these earthquakes is due to the intense pressure and high temperature conditions found at these depths in the Earth's mantle.
Deep-focus earthquakes are associated with convergent plate boundaries, where two tectonic plates collide and one is forced to subduct beneath the other into the Earth's mantle. As the subducted plate descends deeper into the mantle, it can generate earthquakes at depths exceeding 300 kilometers.