Section 4.2  The relative age of a rock is its age compared to the ages of other rocks.  Ex. Mrs. Herrscher is older than her sister and brother. 

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Section 4.2

 The relative age of a rock is its age compared to the ages of other rocks.  Ex. Mrs. Herrscher is older than her sister and brother.  The absolute age of a rock is the number of years that have passed since the rock formed.  Ex. Mrs. Herrscher is 33 years old.  It may be impossible to know a rock’s absolute age exactly, so geologists often use both absolute and relative ages. HOW OLD ARE ROCK LAYERS?

 According to the law of superposition, in undisturbed horizontal sedimentary rock layers, the oldest layer is at the bottom.  Each higher layer is younger than the layers below it.  The principle of original horizontality states that most sedimentary layers of rock are deposited in a horizontal position HOW OLD ARE ROCK LAYERS?

 Lava that hardens on the surface and forms igneous rock is called an extrusion.  An extrusion is always younger than the rocks below it.  When magma cools and hardens into a mass of igneous rock beneath the surface, it is called an intrusion.  An intrusion is always younger than the rock layers around and beneath it. CLUES FROM IGNEOUS ROCK

 A fault is a break in the Earth’s crust.  A fault is always younger than the rock it cuts through. Why?  An index fossil is a fossil that is widely distributed and represent an organism that only existed for a short period of time.  Index fossils are useful because they tell the relative ages of the rock layers in which they occur. CLUES FROM FOSSILS

CLUES WITH FOSSILS

 Gaps in the geologic record and folding can change the position in which rock layers appear.  An unconformity is a gap in the geologic record. It shows where rock layers have been lost doe to erosion. HOW CAN ROCK LAYERS CHANGE?