Actvity Summary: Students will learn the method of using Oxygen isotopes in the determination of paleoclimate. Students will create a model that demonstrates the differential evaporation and deposition of Oxygen isotopes and explain their role in the dating process.
Jennifer C. Field
- Standard A: Unifying concepts and processes in science
- Standard B: Science as inquiry
- Standard E: Earth and space science
- Patterns
- System and system models
- Stability and change
- Developing and using models
- Analyzing and interpreting data
- ESS3.D Global climate change