As geologists continue to study the Earth, they have found that it is older than previously thought
Some 300 years ago, geologists thought that the Earth was about 6 000 years old
Later, they discovered rocks that were formed 40 million years ago
Today, scientists claim that the Earth is between 4 and 5 billion years old
How scientists determined the Earth's age
1. Study of rocks
2. Changes in rocks occur slowly
3. Can tell time involved in formation of rocks
4. Can tell how long it has taken rocks to be worn away by erosion
5. Size and position of rock layers tell about changes that have occurred
Law of Superposition
In undisturbed sedimentary rocks, each layer is younger than the layer below it and older than the layer above it
Presence of igneous or volcanic rocks makes it more difficult to determine the age of rocks
Radioactive dating
Method to determine the Earth's age by measuring the amounts of uranium and lead present in rock samples
Some rocks have been found to be 5 billion years old using radioactive dating
Fossils
Hardened remains or imprints of organisms that lived a very long time ago
Fossils
They provide records of the past
They show when glaciers or seas covered the land, when volcanoes erupted, when mountains were pushed up, and the kinds of living things that existed millions of years ago
Types of fossils
Footprints
Impressions of leaves or plants
Petrified or changed into rock
Whole bodies or skeletons of animals
Ice and amber are materials that can prevent decay and preserve fossils
Fossils reveal the sizes, shapes, appearances, habits, and habitats of living things from long ago
Geologic time scale
The story of living creatures divided into chapters showing the dominant families of living creatures that existed
Eras of the geologic time scale
Precambrian
Paleozoic
Mesozoic
Cenozoic
Precambrian era
Lasted from the beginning of the Earth to about 600 million years ago
Rocks were almost devoid of fossils
Primitive organisms like algae, sponges, and worms did exist
Paleozoic era
Many fossils of marine invertebrates like trilobites and brachiopods
Development of shells, limestone, and coral reefs
First animals to adapt to breathe air were amphibians
Land plants and animals developed
Mesozoic era
Formation of several continents
Great changes in plant and animal life
Dinosaurs were the largest creatures, some were carnivores and some were herbivores
Cenozoic era
Warm-blooded animals like marsupials and primitive mammals appeared
Development of modern life forms like horses, birds, and deciduous trees
Start of the Pleistocene Ice Age
Cold-blooded animals
Animals not capable of regulating their body temperature
Warm-blooded animals
Animals capable of maintaining a nearly constant body temperature