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Methods used to measure the age of Earth and its parts include radiometric dating, which uses the decay of radioactive isotopes to determine age, such as carbon dating for organic materials and uranium-lead dating for rocks. Other methods include stratigraphy, which analyzes the layering of rocks to establish a relative timeline, and dendrochronology, which uses tree rings to date events in the past. Additionally, paleomagnetism can help determine the age of rocks by analyzing changes in Earth's magnetic field recorded in the rocks.

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