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According to the geologic Law of Superposition, in undisturbed rock strata, the deepest rock layers are always the oldest. Accordingly, a fossil found in a lower layer of undisturbed rock would be the older.
Principle stating that older rock layers are beneath younger rock layers.
older because it is at the bottom and the ones on top are younger than the bottoms
The strata or rock layers of the grand canyon walls are undisturbed. As such, a layer of rock containing a fossil, that is below an overlying rock layer will be older.
There is no absolute trend, since geological faults can thrust older rocks above younger ones, and whole sequences can be turned upside down. However, more often than not, for a single location deeper strata are older.
the fissils in the upper strata are younger than thos in the lower strata.
According to the geologic Law of Superposition, older layers of undisturbed rock are found to be deeper than younger layers. The discovery of trace fossils (organisms that were abundant and rapidly evolving species) in sedimentary rock strata can indicate a relative age or timespan in which the sediments were laid down, based on their relative position in the dated rock strata.
The Law of Superposition states that underlying strata are older than overlying strata unless the layers have been disturbed by other processes. Hence the law would be most relevant when studying sedimentary rocks (but not excusively).
Superposition is the principle that states that, in undisturbed strata, newer layers will be deposited over older layers; thus, in a core sample, those samples of earth and rock nearest the surface will be newer in age than those beneath them.
The fossil on the bottom would be older because as time goes on rock builds up and buries fossils so the higher it is the more recent it is.
Superposition is the principle that states that, in undisturbed strata, newer layers will be deposited over older layers; thus, in a core sample, those samples of earth and rock nearest the surface will be newer in age than those beneath them.
because all the different types and weights of the sediments means that some fall through the water faster than others so when they compress into rock the heaviest sediments will be at the bottom etc.