S waves move perpendicular to the direction of wave propagation. This means that S waves move in a side-to-side or horizontal motion as they travel through the Earth's crust and mantle.
The three types of seismic waves are:P waves, S waves, and Surface waves
Seismic waves, specifically Love waves, move like an inchworm. Love waves are surface seismic waves that move in a horizontal, side-to-side motion, causing the ground to shake horizontally. This motion resembles the movement of an inchworm as it travels along a surface.
Transverse waves move perpendicular to the direction of the wave's motion. As the wave travels, the particles in the medium oscillate up and down or side to side. Examples of transverse waves include light waves, water waves, and seismic S-waves.
If you throw ball at an angle above horizontal, you will see the path of the ball looks like an inverted parabola. This is result of the fact that the ball's initial velocity has a horizontal and vertical component. If we neglect the effect of air resistance, the horizontal component is constant. But the vertical component is always decreasing at the rate of 9.8 m/s each second. To illustrate this, let the initial velocity be 49 m/s and the initial angle be 30˚. Horizontal component = 49 * cos 30, Vertical = 49 * sin 30 = 24.5 m/s As the ball rises from the ground to its maximum height, its vertical velocity decreases from 24.5 m/s to 0 m/s. As the ball falls from its maximum height to the ground, its vertical velocity decreases from 0 m/s to -24.5 m/s. Since the distance it rises is equal to the distance it falls, the time that it is rising is equal to the time it is falling. This means the total time is equal to twice the time it is falling. This is the reason that the shape of the ball's path is an inverted parabola. At the maximum height, the ball is moving horizontally. If you do a web search for projectile motion, you will see graphs illustrating this.
The subtypes of secondary waves (S-waves) are Love waves and Rayleigh waves. Love waves cause horizontal movement, while Rayleigh waves cause both horizontal and vertical movement. Both types of waves are surface waves that move along the Earth's crust.
S waves move perpendicular to the direction of wave propagation. This means that S waves move in a side-to-side or horizontal motion as they travel through the Earth's crust and mantle.
Love waves are horizontally polarized and move in a shearing motion, while Rayleigh waves move in an elliptical motion that combines vertical and horizontal displacements. Rayleigh waves are slower than Love waves and cause more vertical motion, resulting in more damage during an earthquake. Love waves, on the other hand, cause more horizontal motion and can be more damaging to structures parallel to their direction of propagation.
body waves and surface waves
False. S waves (secondary waves) move through the ground by shearing the rock particles side to side, creating a horizontal motion that is perpendicular to their direction of travel. This shearing motion can cause the ground to move in a wave-like pattern, but not compress and then expand as with compressional waves (P waves).
The three types of seismic waves are:P waves, S waves, and Surface waves
L waves, also known as Love waves, are a type of surface wave that move in a horizontal, side-to-side motion. They travel along the Earth's outer layer and can cause significant shaking and damage during earthquakes due to their long wavelengths and high amplitudes. L waves move slower than P and S waves but are responsible for the most long-lasting and destructive effects of an earthquake.
Surface waves are slower than body waves like P-waves and S-waves because they travel along the Earth's surface instead of through the interior. Surface waves typically cause the most damage during an earthquake due to their combination of horizontal and vertical motion.
S-waves are slower than P-waves, which are the fastest seismic waves. S-waves are shear waves that move in a back-and-forth motion, causing particles to move perpendicular to the direction of wave propagation.
L waves, also known as Love waves, are a type of seismic wave that travels on the surface of the Earth and causes horizontal shifting of the ground during an earthquake. They move slower than P and S waves but are responsible for the majority of the damage done during an earthquake. Their movement creates a side-to-side or horizontal motion that can be particularly destructive to buildings and structures.
Seismic waves, specifically Love waves, move like an inchworm. Love waves are surface seismic waves that move in a horizontal, side-to-side motion, causing the ground to shake horizontally. This motion resembles the movement of an inchworm as it travels along a surface.
Seismic waves that move rocks up and down like a wave in a rope are called vertical or P-waves. These waves cause particles to vibrate in the direction of wave propagation, creating compression and expansion as the wave passes through the material. P-waves are the fastest seismic waves and can travel through both solids and liquids.