A thermocline is the transition layer between the warmer mixed water at the surface and the cooler deep water below. It is relatively easy to tell when you have reached the thermocline in a body of water because there is a sudden change in temperature.
hope it helps...!!!!
Answer:
By using seismic waves and seeing where they are reflected off of a fault a geologist can map.
did that help?
Explanation:
C maybe she wanted to keep them safe
Rossby waves occur at the equatorial. Regions only
