It is called the shadow zone, an area at an angle of between 104° and 140° from the axis of the epicenter, where the earth's liquid outer core has refracted the P-waves away from the direct line of travel.
Stress waves
shadow zone
An area on Earth's surface where no direct seismic waves from a particular earthquake can be detected.
The shadow zone is an area on Earth's surface where no seismic waves are detected after an earthquake. This helps scientists understand the Earth's interior structure, as the absence of seismic waves in this zone indicates the presence of a liquid outer core that blocks the transmission of certain seismic waves.
If an area has a strong amount of seismic waves along, or around, you can predict if an area is active for earthquakes
If an area has a strong amount of seismic waves along, or around, you can predict if an area is active for earthquakes
If an area has a strong amount of seismic waves along, or around, you can predict if an area is active for earthquakes
If an area has a strong amount of seismic waves along, or around, you can predict if an area is active for earthquakes
they use vaginas
Shadow zone
mohorovicic discontinuity
S waves, or secondary waves, are a type of seismic wave that can only travel through solids. Since the Earth's outer core is liquid, S waves cannot pass through it, which creates an area on the opposite side of the Earth from an earthquake's epicenter where these waves are not detected. This results in an S-wave shadow zone, typically located between 103 and 180 degrees from the earthquake's source, where no S waves are recorded. Thus, their inability to traverse liquid prevents them from being detected everywhere on Earth after an earthquake.