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The Geological Time Scale. Geological Time Scale. The Earth is about 4.6 billion years old Since then Earth has experienced continuous change
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Geological Time Scale • The Earth is about 4.6 billion years old • Since then Earth has experienced continuous change • Some changes occur quickly, like volcanoes, earthquakes and floods, while others occur so slowly we can barely notice them, like erosion, and moving continents.
Geological Time Scale • To make the age of the Earth more understandable geologists have designed the Geological Time Scale, which breaks the 4.6 billion years into smaller portions.
Geological Time Scale • As the Earth changes so do the organisms that live on it. • Species have developed through time and changed as their environment changed. • Others have dominated the planet for millions of years only to be replaced by other species better adapted to changing conditions.
Geological Time Scale • Mass extinctions have occurred several times in Earth’s history • Dinosaurs died about 65 mya • 250 mya 96% of marine animals and 75% of land animals were wiped out • After every major extinction there is an opportunity for different species to become dominant
The Principle of Faunal Succession • This principle states that species change in form through time. • Each form is different from those that come before and after • From the fossils they find geologists use this principle to tell the order of layers in a rock sequence
Index Fossils • These are fossils that can help tell the age of the rock layer it is found in.
Index Fossils • These are fossils that can help tell the age of the rock layer it is found in. The Three Characteristics of an Index Fossil
Index Fossils • These are fossils that can help tell the age of the rock layer it is found in. The Three Characteristics of an Index Fossil • It’s easy to recognize • It was only in existence for a short period of time • It is found in many locations around the world