Earth’s History Test: Monday, February 13, 2017 The Rock Cycle Why is it called a cycle? Does it always start/end in the same place? Types of rock. How does each form? (Sedimentary, Igneous, Metamorphic) Fossils: (Study the “Getting Into the Fossil Record” online activity!) Form in what type of rock? How do they form? How can we use fossil data to predict past environments? Besides in rock, what other substances can fossils form in? (There are 4 more besides rock) Who studies them? The fossil record- How do we use it? What does it tell us? Body vs. Trace Fossils examples and definitions! Using ice core data and tree rings Explain WHY a turtle would fossilize better than a caterpillar Relative age of rocks/fossils (based on layers) Relative Dating- put layers/rock in order from oldest to youngest o Pictures with: igneous intrusions, faulting, folding, tilting, erosion, uplifting, unconformities Law of Superposition Principle of Original Horizontality Principle of Cross-Cutting Relationships Absolute age of rocks/fossils (based on radiometric dating) Absolute Age- what does this mean? Radiometric dating and decay: How is it used? Different methods? Bracketing (on the “Radiometric Dating Information: notes) o If a layer of sedimentary rock sits between igneous rock layers that we can determine the age of, we can estimate the age of the sedimentary rock What is a half-life? What are index fossils and how are they used? Correlation of rock layers There is a Study Island practice quiz that you can take to help you study!! Due by 10:00 PM Sunday, February 12 for EXTRA CREDIT! (extra credit based on the score you earn) Sedimentary rock Metamorphic rock Igneous rock Magma vs. Lava Uniformitarianism Fossil Paleontologist Trace Fossil Body Fossil Ice core Tree ring Relative Age Relative Dating Law of Superposition Unconformity Principle of Original Horizontality Principle of Crossing Cutting Relationships Tilting Erosion Faulting Folding Absolute Age Absolute Dating Radioactive Decay Half-life Radiometric-dating Index Fossil
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