Seismic waves are generated by the sudden release of energy in the Earth's crust, typically from earthquakes or volcanic activity. These waves travel through the Earth, carrying information about the Earth's interior and helping scientists study its structure.
During an earthquake, seismic waves are released. These waves travel through the Earth and can be detected by seismographs. The main types of seismic waves are P-waves (primary waves), S-waves (secondary waves), and surface waves.
Waves are the carriers of both sound energy and seismic energy. In the case of sound energy, it is carried through compressional waves in the air or other mediums. For seismic energy, it is transmitted through elastic waves in the Earth's crust. In both cases, the energy is transferred through the vibration of particles.
seismic waves
Light waves are electromagnetic waves that can travel through a vacuum, while seismic waves are mechanical waves that require a medium, such as rocks or soil, to propagate. Light waves travel at the speed of light (about 300,000 km/s), while seismic waves travel at much slower speeds (a few km/s to several km/s). Light waves exhibit characteristics such as reflection and refraction, while seismic waves can produce earthquakes and reveal information about the Earth's interior.
Examples of longitudinal waves include sound waves, seismic waves, and sound waves in solids (such as ultrasound waves). These waves propagate by compressing and rarefying the medium in the direction of wave motion.
The point of origin of seismic waves during an earthquake is called the "focus" or "hypocenter." This is the location within the Earth where the seismic energy is released. The point directly above the focus on the Earth's surface is known as the "epicenter."
Seismic waves travel outward in all directions from their point of origin, which is the focus of an earthquake. The waves propagate through the Earth's interior in various patterns and speeds, with different types of waves exhibiting different behaviors.
P-waves are the first to arrive at a seismic station. There are two major types of waves: Body waves and surface waves. P-waves and S-waves come under Body waves while Love and Rayleigh waves come under surface waves. Body waves are much faster than the Surface waves. Waves are detected in the following order: P, S, Love and Rayleigh
Seismic Waves
Seismic Waves
The vibrations that move away from an earthquake's origin are known as seismic waves. There are two main types of seismic waves: primary (P) waves, which are compressional waves that travel fastest through the Earth's interior, and secondary (S) waves, which are shear waves that move more slowly and can only travel through solids. Both types of waves propagate outward from the earthquake's focus, causing the ground shaking associated with seismic events.
An earthquake deep underground releases seismic energy in the form of seismic waves. These waves carry energy from the point of the earthquake's origin (the focus) and cause the ground to shake as they propagate through the Earth's crust.
Seismic waves are any waves that travel through the Earth. As such all earthquake waves are seismic waves, however not all seismic waves are caused by earthquakes.
(not seismic, seismic wave)Seismic waves are waves of energy that travel through the earth.
Seismic wave is mostly referred to earthquake impact ,so the word epicentre can be applied to its origin or point of impact.
Seismic waves.
seismic waves actually the correct answer is S waves. trust me if you put seismic waves it will be wrong