Comp Sci 2 Unit 1 Earth Structures (Lesson 4)

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1.
The process where rocks break and move along a fracture or crack in Earth’s crust, often caused by tectonic forces and associated with earthquakes.
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The bending of rock layers due to pressure and stress, usually from tectonic forces, without the rocks breaking. This creates features like anticlines (upward folds) and synclines (downward folds).
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Record, The collection of all known fossils and their placement in rock formations and layers, used to study the history of life on Earth.
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Column, An ideal, ordered arrangement of rock layers (strata) that represents the chronological sequence of Earth's geological history.
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Intrusion, Molten rock (magma) that pushes into existing rock layers and solidifies beneath Earth’s surface, often cutting across older layers.
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of Superposition, A principle stating that in undisturbed sedimentary rock layers, the oldest layers are at the bottom and the youngest are at the top.
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Dating, A method of determining the actual age of a rock, fossil, or geologic event in years, often using radioactive decay.
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Dating, A technique for determining the age of materials by measuring the amount of a radioactive isotope and its decay products.
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Decay, The process by which an unstable atomic nucleus loses energy by emitting radiation, changing into a different element over time.
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Elements, Unstable elements that naturally break down (decay) over time, releasing radiation; commonly used in dating rocks (e.g., uranium, carbon-14).