The secondary wave breaks up.
the secondary wave breaks up
the secondary wave breaks up
the secondary wave break up
The difference between the arrival times increases as the distance from an earthquake epicentre increases as S-waves travel more slowly than P-waves so the greater the distance the further they lag behind.
A voltage appears between the terminal points of the secondary winding
Nothing happens. Distance between crests is a measure of frequency; amplitude is a measure of the strength, the height of the wave, or auditory volume of the signal.
During flexion, the distance between the spinous processes is increased.
The difference between what one expects to happen and what actually happens is simple. It is most often called reality.
Nothing.
Reality.
the gravitational force between them decreases.
the force of attraction get weaker the more the distance grows between magnetic fields