n.
(geology) the principle that in a series of stratified sedimentary rocks the lowest stratum is the oldest
the displacement of any point due to the superposition of wave systems is equal to the sum of the displacements of the individual waves at that point
Copyright: Proverb ©
Our website is made possible by displaying online advertisements to our visitors.
Please consider supporting us by disabling your ad blocker.
I turned off Adblock