1. Earth’s History The Rock Cycle Complete on page 135

2. The study of the structure of planet Earth and the forces that make and shape Earth. ~James Hutton studied rocks and landscape around him and developed the principle of uniformitarianism. ~The principle of Uniformitarianism states that the geologic processes that operate today also operated in the past.

3. Fossils are preserved remains or traces of an organism that lived in the past. After a time, the sediments are compressed together to make sedimentary rock Index fossil: a fossil that is widely distributed and represents a type of organism that existed only briefly Index fossils help geologists match rock layers because they tell the relative ages of the rock layers in which they occur. A Plant Fossil!

4. Geologists classify rocks into three main groups: 1.Sedimentary rock: made of sediments that have been deposited and then pressed together to form solid rock. 2.Metamorphic rock: forms when an existing rock is changed by heat, pressure or chemical reactions. 3.Igneous rock: forms when molten material from beneath Earth’s surface cools and hardens.

5. The Rock Cycle is a series of processes on and beneath Earth’s surface that slowly change rocks from one kind of rock to another. Forces inside Earth and at the surface produce a rock cycle that builds, changes, and destroys rocks.

6. How does the rock cycle work?

7. How does the rock cycle work?

13. How does the rock cycle work?

14. Relative age: –The age compared to the ages of other rocks. –This does not give an exact age Absolute age: –The number of years since the rock formed

15. Law of superposition –When Geologist determine the relative ages of sedimentary rock layers –The oldest layer is at the bottom and each higher level is younger than the layers below it.

16. Radioactive dating: –The atoms of one element break down to form atoms of another –Used to determine the absolute age of rocks –Radioactive dating indicates that Earth is roughly 4.6 billion years old. –Half-life- the time it takes for half of the unstable atoms in a fossil sample to decay. Ranges from fractions of a second to billions of years.

17. You do not need to write this down! Atoms are tiny particles that make up matter. Some of them are unstable which means their insides cannot hold a the atom together. When atoms are unstable, they release some of their particles. This is called radioactive decay. All atoms decay at different speeds. When a atom is half decayed, the time it took to decay that far is its half-life. The ratio of unstable atoms to stable atoms helps scientists figure out an approximate age for the fossil and rock. This method of dating is called absolute dating.

18. Complete this drawing on p. 134 in your notebook