It seems like you have a school assignment to complete. I can help you with your research by providing information on the topics you mentioned. Here are five phrases from the introduction that you can use in your search for sources:
1. Earth’s early history
2. Estimate Earth’s age
3. First life appeared
4. Oldest rocks and fossils
5. Modern living things
Part 2:
According to scientific estimates, Earth is about 4.54 billion years old, plus or minus about 50 million years. Scientists have used radioactive dating techniques to determine the approximate ages of Earth’s oldest known rocks and minerals.
It is difficult to find the first rocks that formed on Earth because Earth’s oldest rocks have been recycled and destroyed by the process of plate tectonics. The rocks containing signs of early life have been deformed and metamorphosed by heat, stress, and hydrothermal alteration and then subject to billions of years of weathering processes such as erosion.
The oldest rocks on Earth are more than 4 billion years old and were formed during the Hadean Eon of Earth’s geological history. The Acasta Gneiss, found in northwestern Canada, is one of the oldest known rocks on Earth and has been dated at 4.03 billion years old. Even older than the Acasta Gneiss are individual zircons from the Jack Hills in Australia, dated to 4.4 billion years ago. Scientists determine the age of rocks using various dating techniques.
Scientists use various techniques to determine the age of rocks. One way is by determining the age of the group of rocks, or formation, that a rock is found in. The age of formations is marked on a geologic calendar known as the geologic time scale.
Another way scientists determine the age of rocks is by using radioactive dating techniques. This involves measuring the number of radioactive isotopes in a rock sample and using that information to calculate the age of the rock.
Radioactive dating techniques take advantage of the fact that certain isotopes of elements are unstable and undergo radioactive decay at a known rate. Scientists can measure the amount of a radioactive isotope and its decay products in a rock sample and use that information to calculate the age of the rock.
For example, uranium-lead dating involves measuring the amount of uranium and lead isotopes in a rock sample. Uranium isotopes decay into lead isotopes at a known rate, so by measuring the ratio of uranium to lead isotopes in a rock sample, scientists can determine how long it has been since the rock formed.