the epicenter
Earthquake waves travel outward in all directions from the point of seismic activity, which is known as the focus. The waves can move through the Earth's interior in various directions, including up towards the surface, causing shaking and potential damage.
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 source of an earthquake is called the "focus" or "hypocenter." It is the point within the Earth where the earthquake originates, and from there, energy is released and radiates outward in the form of seismic waves. The location directly above the focus on the Earth's surface is known as the "epicenter."
A spherical wave travels in all directions, expanding outward from its source like ripples on the surface of water.
The area beneath the Earth's surface where rock under stress breaks and triggers an earthquake is known as the focus or hypocenter. This point is typically located along a fault line, where tectonic plates interact. The seismic waves generated by the sudden release of energy at the focus propagate outward, causing the shaking felt during an earthquake. The point directly above the focus on the Earth's surface is called the epicenter.
Earthquake waves travel outward in all directions from the point of seismic activity, which is known as the focus. The waves can move through the Earth's interior in various directions, including up towards the surface, causing shaking and potential damage.
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 source of an earthquake is called the "focus" or "hypocenter." It is the point within the Earth where the earthquake originates, and from there, energy is released and radiates outward in the form of seismic waves. The location directly above the focus on the Earth's surface is known as the "epicenter."
The point on the earth's surface closest to the origin of an earthquake is called the epicenter. This is where the seismic waves generated by the earthquake first reach the surface.
Earthquake generated waves are called seismic waves. These are waves of energy that travel through the Earth's layers. Their velocity depends on the elasticity and density of the medium that they travel through.
The epicentre of an earthquake is the point on the Earth's surface directly above the point within the Earth where the earthquake actually occurred (known as the focus or hypocentre). From this point on the surface the waves of the earthquake radiate outward like the ripples in a pond when a stone is thrown in.
A spherical wave travels in all directions, expanding outward from its source like ripples on the surface of water.
These are known as seismic waves.
Convex surface. It is curved outward and acts as a reflector, spreading light in various directions. This type of surface is commonly used in mirrors and lenses to focus or diverge light rays.
The area beneath the Earth's surface where rock under stress breaks and triggers an earthquake is known as the focus or hypocenter. This point is typically located along a fault line, where tectonic plates interact. The seismic waves generated by the sudden release of energy at the focus propagate outward, causing the shaking felt during an earthquake. The point directly above the focus on the Earth's surface is called the epicenter.
A surface that curves outward is called a convex surface. It bulges or protrudes outward towards the exterior.
The epicentre of an earthquake is the central point on the Earth's surface directly above the point within the Earth where the earthquake actually occurred (known as the focus or hypocentre). From this point on the surface the waves of the earthquake propagate outward like the ripples on a pond when a stone is thrown in.