the zone of subduction
The place where an earthquake starts is called the hypocenter, also known as the focus. This is the point within the Earth where the seismic energy is first released, leading to the generation of seismic waves. The hypocenter is typically located beneath the Earth's surface along the fault line where the stress is released, causing the rocks to break and slip, resulting in an earthquake.
The place where slipping begins on an earthquake is called the hypocenter or focus. This is the point within the Earth's crust where the seismic waves originate and energy is released.
The place along the fault where the earthquake starts is called the hypocenter, or focus. This is the point within the Earth's crust where the energy is first released, generating seismic waves that cause the shaking felt at the surface.
The place beneath the ground where an earthquake starts is called the "hypocenter" or "focus." This is the point within the Earth where the seismic energy is released, generating seismic waves that cause the ground shaking experienced during an earthquake.
A place where an earthquake has occurred in the past but not recently is known as a seismic gap.
The place where an earthquake starts is called the hypocenter, also known as the focus. This is the point within the Earth where the seismic energy is first released, leading to the generation of seismic waves. The hypocenter is typically located beneath the Earth's surface along the fault line where the stress is released, causing the rocks to break and slip, resulting in an earthquake.
The place where an earthquake's slipping motion begins is called the focus or hypocenter. It is the exact point underground where the seismic energy is released.
The place where slipping begins on an earthquake is called the hypocenter or focus. This is the point within the Earth's crust where the seismic waves originate and energy is released.
An earthquake originates at a point underground called the hypocenter or focus. This is where the seismic energy is released, causing the ground to shake. The point on the Earth's surface directly above the hypocenter is called the epicenter.
They are quite common; they are called aftershocks. An earthquake redistributes the stress that creates the quake across the fault line, which then creates new points of stress, which result in additional earthquakes, which further redistribute the stress again, and so on and so forth until all the energy is spent.
The place along the fault where the earthquake starts is called the hypocenter, or focus. This is the point within the Earth's crust where the energy is first released, generating seismic waves that cause the shaking felt at the surface.
The place along a fault where the slipping that causes an earthquake begins is called the "focus" or "hypocenter." This is the point within the Earth where the energy is released, initiating the seismic activity that generates an earthquake.
The place inside Earth where an earthquake starts is called the "focus" or hypocenter. This is the point beneath the Earth's surface where the seismic energy is released, generating seismic waves that cause the ground to shake.
Within the Earth, the focal point of the energy released in an earthquake is called the hypocentre or focus. This is where an earthquake actually begins. The place on the Earth's surface directly above this point is known as the epicentre.
Epicenter
epicentre
The place beneath the ground where an earthquake starts is called the "hypocenter" or "focus." This is the point within the Earth where the seismic energy is released, generating seismic waves that cause the ground shaking experienced during an earthquake.