The fastest earthquake wave, which travels by compression and expansion of the medium.
Reference:
Tarbouk, E.J. & F.K. Lutgens, (2006), EARTH, 8th edition, Pearson Education International.
The natural remnant magnetism in rock bodies. The permanent magnetization acquired by rock that can be used to determine the location of the magnetic poles and the latitude of the rock at the time it became magnetized.
Reference:
Tarbouk, E.J. & F.K. Lutgens, (2006), EARTH, 8th edition, Pearson Education International.
The study of ancient magnetic fields, which are preserved in the magnetic properties of rocks. ie. studying the changes in position of the magnetic poles, as well as reversals of poles in the geological past.
The systematic study of fossils and the history of life on Earth.
Reference:
Tarbouk, E.J. & F.K. Lutgens, (2006), EARTH, 8th edition, Pearson Education International.
An era of geologic time, from the end of the Precambrian to the beginning of the Mesozoic (about 590-248 million years ago). Termed as the era of ancient life.