p waves help geologist by telling them if a earthquake is coming
Yes, geologists determined that the outer core is liquid because P-waves cannot travel through it and instead undergo a shadow zone. P-waves can only pass through solid material, so the inability for P-waves to travel through the outer core indicates that it is in a liquid state.
the distance to the earthquake's epicenter. P waves, or primary waves, travel faster than S waves, or secondary waves, so the interval between their arrival times can be used to calculate the distance the seismic waves have traveled. By measuring this time difference at different seismograph stations, geologists can triangulate the epicenter of the earthquake.
Geologists learn about Earth's interior using indirect evidence from seismic waves, magnetic field data, and rock samples from volcanoes and deep drilling. These methods help provide insights into the composition, structure, and properties of Earth's interior layers.
We know the discontinuity exists because of different types of seismic waves; certain waves can penertrate to different depths. Seismic waves are refracted at the Gutenburg discontinuity, which marks the upper boundary of the earth's core
Geologists locate the epicenter of an earthquake by analyzing the arrival times of seismic waves from the earthquake recorded by seismographs at different locations. By triangulating the arrival times from at least three stations, they can pinpoint the epicenter where the waves intersect.
Yes, geologists determined that the outer core is liquid because P-waves cannot travel through it and instead undergo a shadow zone. P-waves can only pass through solid material, so the inability for P-waves to travel through the outer core indicates that it is in a liquid state.
the distance to the earthquake's epicenter. P waves, or primary waves, travel faster than S waves, or secondary waves, so the interval between their arrival times can be used to calculate the distance the seismic waves have traveled. By measuring this time difference at different seismograph stations, geologists can triangulate the epicenter of the earthquake.
The factors that help geologists determine for earthquake risk for religion are the movement of seismic waves along faults and friction.Hope this helped!
could you help me in my homework? the question is list 5 examples of p waves and s waves
No. Seismologists (a type of geophysicist) use the difference in the arrival time of P and S waves to estimate the distance from the seismometer station to the epicentre of the earthquake.
because the waves travel through the solid crust and simisolid mantle they help see where the epicenter from an earthquake is
could you help me in my homework? the question is list 5 examples of p waves and s waves
Geologists use evidence from seismic waves to learn about earth's interior. Geologists record the seismic waves and study how they travel through earth. By Brianna.
distance to the epicenter of an earthquake. [:
Seismic waves
The abbreviation for primary waves is P-waves.
The factors that help geologists determine for earthquake risk for religion are the movement of seismic waves along faults and friction.Hope this helped!