0
Mohorovicic Discontinuity. A+
Good luck! ~K
What else can I help you with?
In which area do seismic waves change dramatically?
they use vaginas
In which area do seismic waves change dramatically in speedanswer?
mohorovicic discontinuity
In which area do seismic waves change dramatically in speed?
they use vaginas
The speed at which seismic waves travel through Earth's layers depends upon the of those layers. temperature density shape area?
The speed of the waves depends on the density of the material.
How do the data from movements of seismic waves help geologist determine the risk from an area?
If an area has a strong amount of seismic waves along, or around, you can predict if an area is active for earthquakes
How do the data from movements of seismic waves help geologist determine the risk for an area?
If an area has a strong amount of seismic waves along, or around, you can predict if an area is active for earthquakes
How do the data from the movement of seismic waves help determine the earthquake risk for an area?
If an area has a strong amount of seismic waves along, or around, you can predict if an area is active for earthquakes
What area do seismic wave change dramatically?
Seismic waves can dramatically change in velocity and direction when they encounter boundaries between different types of rock or geological formations. These changes, known as refraction and reflection, occur at interfaces with contrasting physical properties, leading to the bending or bouncing of seismic waves. The behavior of seismic waves at these boundaries provides valuable information about the Earth's interior structure.
How do the data from the movement of seismic waves help geologist determine the earthquakes risk an area?
If an area has a strong amount of seismic waves along, or around, you can predict if an area is active for earthquakes
What is in the area where no seismic wave are detected?
Stress waves
In which area do seismic waves change dramaticaly?
Seismic waves can change dramatically when they encounter boundaries between different geological materials with contrasting densities and elastic properties, such as the crust-mantle boundary or the core-mantle boundary. These changes in seismic wave behavior are key in helping scientists study the internal structure of the Earth.
An area where no direct seismic waves from a particular earthquake can be detected?
shadow zone
