Overview
Geochronological techniques are essential for understanding the age and timing of geological events. By employing methods such as radiometric dating, stratigraphy, and paleomagnetism, geologists can piece together the history of the Earth and its processes. These techniques not only help in dating r...
Key Terms
Example: Geochronology helps us understand the timeline of Earth's history.
Example: Carbon-14 dating is a common radiometric dating technique.
Example: Stratigraphy is used to understand the sequence of geological events.
Example: Paleomagnetism can reveal past movements of tectonic plates.
Example: Trilobites are often used as index fossils.
Example: The half-life of Carbon-14 is about 5,730 years.