Answer:
Surface waves have a longer duration and higher amplitude than body waves.
Explanation:
The stark difference between an earthquake body and surface waves is such that they have longer duration and a higher amplitude compared to body waves.
There are two categories of seismic waves that usually accompanies an earthquake:
- body waves are faster and perpetuate in the subsurface. They reach the seismic station first and are discovered faster.
- surface waves arrives later and they cause the damage produced by most earthquake waves. They perpetuate on the surface.
- surface waves are the love and Rayleigh waves
- body waves are the primary and secondary waves.
Explanation:
Coriolis force -
It helps to determine the turn of the wind to the right in the Northern Hemisphere due to the rotation of the Earth .
This effect does not impact the speed of the wind , it only affect the direction of the wind .
<u>The impact of the Coriolis force of the wind direction is as follows -</u>
From the north pole , the earth rotates at higher speed in the counter - clockwise direction , then the object will appear to deflect to the right of its intended path , due to the Earth's rotation .
1 High
2 <span> northeast of Los Angeles over the Great Basin
Hope this helps!!</span>
Answer:
This is a cycle because it continues forever. Cycles like for example, a human. A human starts off as a baby, becomes a toddler., then ages into a kid then a teenager, afterwards an adult. And this cycle continues. It happens everywhere in nature and everywhere in the world today with living things including: Plants, Humans, and animals. I hope this helps It might be wrong and I'm sorry if it is:(
Answer:
Intensity depends on the distance form the ground and source of energy.
Explanation:
- Earth quake that has an intensity of 1.5 on the Richter scale can be detected only through the seismograph. The earthquake with an intensity of 0 levels on the Richter scale that is below micro will not be felt or rarely felt in scale.
- This can be defied by the Richter scale formula of R=log(IcIn), Ic is the intensity and In is the intensity if the standards earthquake. Hence the difference will be R2−R1=log(I2I1)
