Примери за използване на Seismic waves на Английски и техните преводи на Български
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On Seismic Waves".
Propagation of seismic waves.
Seismic waves reveal the depth of the plume.
The slurry-like composition slows the seismic waves.
Propagation of seismic waves through the Earth.
Seismic waves change depending on what they hit;
Many factors combine to make these seismic waves exceptional.
Typically, seismic waves would operate on several frequencies.
Each rock andeach mineral responded differently to seismic waves.
Seismic waves are studied by geophysicists called seismologists.
A depiction of different seismic waves propagating through the Earth.
The seismic waves of the‘ earthquake Heartbleed' even shake the network- ElMundo.
In this part,the velocity of seismic waves increases sharply.
This creates seismic waves and leads to the shaking or movement of the ground.
Fortunately for geoscientists,those blasts would have sent seismic waves through Earth.
The move sent seismic waves of shock and outrage around the globe.
Seismographs are devices used to measure seismic waves produced by earthquakes.
The seismic waves can be detected thousands of kilometers from the original earthquake.
There are certain areas in which the seismic waves tend to speed up without explanation.
The vibrations generated by the rhythmic movement of the crowd are transmitted as seismic waves.
Seismometer is an instrument used to measure seismic waves generated by earthquakes.
Furthermore, seismic waves will spread out radially from both the epicenter and the hypocenter.
Seismograph is the instrument used to record the seismic waves caused by earthquakes.
What's more, the lack of seismic waves means that the events can't be detected with seismometers.
Seismometers is the instrument used to measure the seismic waves produced by earthquakes.
But what if seismic waves could be deflected before they reach critical infrastructure?
We're thrilled that we're now in the best position to listen to all the seismic waves from below Mars' surface and from its deep interior.”.
So, looking at seismic waves inside our own planet doesn't tell us much about how it formed.
In the same way, that light waves can bounce(reflect) in a mirror or bend(refract)when they pass through a prism, seismic waves travel directly through homogeneous rocks but are reflected or refracted when finding limits or roughness.
By analyzing how seismic waves move through the orb, scientists can deduce depth and composition of its layers.