Relative dating online activity

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Rock layers may have another rock cutting across them, like the igneous rock pictured below (Figure below). To determine this, we use the law of cross-cutting relationships.The cut rock layers are older than the rock that cuts across them.The unconformity was discovered by James Hutton in the 1700s.Hutton saw that the lower rock layers are very old. There are no layers in between the ancient and recent layers.What they could do was determine the ages of materials relative to each other. They could also determine when a process occurred relative to those rocks. The laws of stratigraphy can help scientists understand Earth’s past.Using sensible principles they could say whether one rock was older than another and when a process occurred relative to those rocks. The laws of stratigraphy are usually credited to a geologist from Denmark named Nicolas Steno. The laws are illustrated in the Figurebelow; refer to the figure as you read about Steno’s laws below. In most families a person’s age fits into his or her generation: Siblings are around the same age as are first cousins. The arid climate means that that the rocks are not covered by vegetation.But in some families, multiple marriages, delayed childbearing, extended childbearing or other variations mixes up generations so that Aunt Julia may be five years younger than her nephew. How do Steno’s laws help geologists to decipher the geological history of a region? In many places, especially the national parks, the formations are fantastic. The principles discussed below are easily seen around the Southwest.

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With rock units we use certain principles to tell their ages relative to each other. If they didn’t see it form, they couldn’t know if a rock was one hundred years or 100 million years old.

Early geologists had no way to determine the absolute age of a geological material. What they could do was determine the ages of materials relative to each other.

If they didn’t see it form, they couldn’t know if a rock was one hundred years or 100 million years old. Using sensible principles they could say whether one rock was older than another.

Remember Nicholas Steno, who determined that fossils represented parts of once-living organisms? Superposition refers to the position of rock layers and their relative ages (Figure below).

Steno also noticed that fossil seashells could be found in rocks and mountains far from any ocean. Steno proposed that if a rock contained the fossils of marine animals, the rock formed from sediments that were deposited on the seafloor. Relative age means age in comparison with other rocks, either younger or older.

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