The shadow zone
They go faster through the inner core than the liquid outer core.
S-waves (or Secondary waves) and Love waves are both transverse seismic waves.
A seismograph is an instrument that measures the seismic wave activity in an area. According to Wikipedia, Seismometersare instruments that measure and record motions of the ground, including those of seismic waves generated by earthquakes, nuclear explosions, and other seismic sources. Records of seismic waves allow seismologists to map the interior of the Earth, and locate and measure the size of these different sources. A seismic wave, according to wikipedia is, "Seismic waves are waves of force that travel through the Earth or other elastic body, for example as the result of an earthquake, explosion, or some other process that imparts forces to the body. Seismic waves are also continually excited on Earth by the incessant pounding of ocean waves (referred to as the microseism) and the wind."Seismograph is another Greek term from seismós and γράφω, gráphō, to draw. It is often used to mean seismometer, though it is more applicable to the older instruments in which the measuring and recording of ground motion were combined than to modern systems, in which these functions are separated. Both types provide a continuous record of ground motion; this distinguishes them from seismoscopes, which merely indicate that motion has occurred, perhaps with some simple measure of how large it was.
Firstly, there are 3 types of seismic waves. Long Waves, Primary Waves(Longitudinal) and Secondary Waves(Transverse). Long Waves travel quickly along the Earth's crust, the thin outer layer. Primary Waves are longitudinal waves, they can travel both through solids andliquids, so they travel through the crust, the mantle, and the outer core (note that they refract through each layer, as each layer has a different density. Secondary Waves are transverse waves, they can only travel through solids, so they go through the inner and outer mantles, and curve away from the cores.
The shadow zone
The shadow zone
none, p-waves can travel anywhere
The shadow zone, located at a distance of 103 to 143 degrees from the earthquake epicenter, is the area on Earth's surface where both P and S waves are completely absorbed and do not arrive due to the core's properties.
The liquid outer core of the Earth's interior refracts p-waves at the boundary with the mantle, and does not carry s-waves.
Primary waves (P-waves) and secondary waves (S-waves) are both types of seismic waves that travel through the Earth's interior during an earthquake. They are both body waves that move through the Earth's interior. Additionally, both P-waves and S-waves play a crucial role in helping seismologists understand the structure of the Earth's interior.
Vertical and horizontal surface waves are both types of seismic waves that travel along the Earth's surface. They are both considered to be surface waves, which means they do not penetrate deep into the Earth like body waves. These waves are typically the most destructive during an earthquake due to their ability to cause significant ground shaking and damage.
When part of the Earth's crust breaks, seismic waves pass through the Earth. These waves include primary (P) waves, secondary (S) waves, and surface waves. P waves are the fastest and can travel through both solids and liquids, while S waves are slower and can only travel through solids. Surface waves cause the most damage during an earthquake.
Primary and surface waves are both types of seismic waves that travel through the Earth's interior during an earthquake. They both cause ground shaking, but primary waves (P-waves) are faster and travel through solids, liquids, and gases, while surface waves travel only along the Earth's surface and are responsible for the most damage during an earthquake.
P waves are seismic body waves that can penetrate the Earth's core. They are the fastest seismic waves and can travel through both solid and liquid materials, allowing them to pass through the Earth's core.
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.
No. Surface waves are slower than both P and S-waves.