Nicolas steno relative dating dating spode

10-Jul-2020 23:15

Plus, get practice tests, quizzes, and personalized coaching to help you succeed.

The four laws are the law of superposition, law of original horizontality, law of cross-cutting relationships, and law of lateral continuity.An example would be that the silt back-fill of an underground drain would form some time after the ground immediately above it.Other examples of non vertical superposition would be modifications to standing structures such as the creation of new doors and windows in a wall.It sounds like common sense to you and me, but geologists have to define the Principle of Original Horizontality in order to make assumptions about the relative ages of sedimentary rocks. Say you have a layer of mud accumulating at the bottom of a lake. More sediment accumulates from the leaf litter and waste of the forest, until you have a second layer.

Once we assume that all rock layers were originally horizontal, we can make another assumption: that the oldest rock layers are furthest toward the bottom, and the youngest rock layers are closest to the top. The forest layer is younger than the mud layer, right? When scientists look at sedimentary rock strata, they essentially see a timeline stretching backwards through history.Now imagine that you come upon a formation like this: What do you think of it? How can you make any conclusions about rock layers that make such a crazy arrangement?