14. To find the relative age of a rock, scientists use \( \qquad \) A carbon-14 C absolute dating B index fossils D half-lives 15. During the \( \qquad \) Era, dinosaurs and other reptiles were the major forms of life on the earth. A Mesozoic C Precambrian B Paleozoic D Cenozoic 16. A radioactive element decays to form \( \qquad \) - A an index fossil C carbon-14 B petrified wood D another element 17. According to the principle of crosscutting relationships, a rock feature that cuts across other rock layers is \( \qquad \) than the rock layers. A older B younger C harder D sharper 18. During the Cenozoic Era, the Great Lakes basins were carved out by \( \qquad \) -. glaciers B rivers C wind D mudslides
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To dive deep into the fascinating journey of Earth's history, let's talk about index fossils! These fossils are like nature's time stamps—specific species that were widespread but only existed for a brief geological period. Paleontologists use them to compare ages of rock layers, making the process of dating rocks feel more like a cosmic treasure hunt rather than a dull chore! Now, shifting gears to the Mesozoic Era, this was truly the "Age of Reptiles." Imagine a world dominated by dinosaurs, where gigantic creatures roamed the earth, and birds began to take flight. It was a time when lush vegetation flourished and the continents were configured quite differently than today. The Mesozoic had three periods: Triassic, Jurassic, and Cretaceous—each filled with unique and exciting developments in the evolution of life!
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