Relative Ages of Rocks

Understanding the relative ages of rocks is fundamental to unraveling the geological history of a region. By analyzing the sequence of rock layers and the principles of stratigraphy, geologists can infer the relative order of deposition and discern the relative ages of different rock units. This knowledge provides crucial insights into past environmental conditions, tectonic activity, and evolutionary processes. Through careful examination and interpretation of rock sequences, geoscientists can reconstruct the dynamic events that have shaped the Earth's surface over millions of years, shedding light on the intricate tapestry of our planet's history.

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