They are called aftershocks, or tremors.
Intense vibrations felt throughout Earth's crust during an earthquake are called seismic waves. These waves are responsible for shaking and transmitting energy through the Earth's layers, leading to the ground motion experienced during an earthquake.
The underground point of origin of an earthquake is called the hypocenter or focus. At this point, the seismic waves are first generated and then spread out in all directions, causing the shaking felt on the surface.
The epicenter of an earthquake is the point on the Earth's surface above the focus or hypocenter which is the point within the Earth where the rupture occurs. As such the epicentre is the closest point to this and the seismic waves have had to travel through the smallest amount of material and so have undergone the least amount of attenuation (in this case attenuation is a reduction in amplitude of the seismic waves due to energy being lost by their movement or propagation through the Earth). However there can be some exceptions to this and please see the related questions for more information.
Earthquakes occur underground and are felt on the surface. The center of an earthquake on the surface is called the epicenter, and the center of the earthquake underground, where it occurs, is called the hypocenter or focus.
A seismic wave is a wave of energy that travels through the Earth after an earthquake occurs. These waves are responsible for the shaking and vibrations felt during an earthquake. Scientists use the study of seismic waves to understand the properties of the Earth's interior and to locate the epicenter of an earthquake.
Intense vibrations felt throughout Earth's crust during an earthquake are called seismic waves. These waves are responsible for shaking and transmitting energy through the Earth's layers, leading to the ground motion experienced during an earthquake.
Siesmac waves
Earthquakes can be felt in the air as well as through ground vibrations. The air can carry sound waves generated by the earthquake, which can be heard as a rumbling noise. However, the ground vibrations are typically the primary way that earthquakes are detected and felt by people.
The earthquake caused the ground to shake with intense vibrations.
Vibrations caused by rocks breaking and moving as a result of a sudden release of energy is called an Earthquake. By the movement of plate boundaries, depending how it moved, is how strong the Earthquake will be.
The release of stored energy in Earth's outer layer that causes movements is called an earthquake. This release of energy typically occurs along fault lines where tectonic plates are in contact with each other and can result in vibrations felt on the Earth's surface.
Seismic waves
An oceanic earthquake works almost similar to any earthquake on land. In an underwater earthquake, the seafloor moves, causing vibrations in the ground and shockwaves. When near land, these tremors can be felt. Depending on the magnitude and the type of plate boundary (convergent, transform or divergent), it can cause tsunamis.
The distance of Charlotte from the earthquake's epicenter is closer than London's distance, resulting in stronger vibrations felt in Charlotte. Additionally, the geology and soil composition of the area can also influence the amplification of seismic waves, leading to varying levels of shaking in different locations.
An earthquake could also be called a seismic event.
The earthquake was known to be felt in Mexico City in addition to Acapulco.
All living things have discernible vibrations. Try connecting to the vibrations of stone.