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Published byMargaretMargaret Sanders Modified over 9 years ago
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Vocab
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Fossil Remains, imprints, or traces of prehistoric organisms
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Permineralized Remains Fossils in which the spaces inside are filled with minerals from groundwater
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Carbon film A thin film of carbon residue that forms a silhouette of the original organism
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Mold A cavity in a rock left behind from a decaying organism
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Cast A copy of the original object formed by mineral-rich water or other sediment
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Index fossil Remains of species that existed on Earth for relatively short periods of time, were abundant, and were widespread geographically.
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Principle of Superposition The oldest rocks are on the bottom and the rocks become progressively younger toward the top
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Relative age An objects age in comparison to the ages of other things
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Unconformities A gap in a rock sequence
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Absolute age The age, in years, of a rock or other object
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Radioactive decay The process of breaking down
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Half-life The time it takes for half of the atoms in the isotope to decay
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Radiometric dating Calculating the absolute age of a rock by measuring the ratio of parent isotope to daughter product in a mineral and by knowing the half-life of the parent
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Uniformitarianism Principle that states that Earth’s processes occurring today are similar to those that occurred in the past
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Weathering The breaking down or disintegration of substances such as rocks and minerals by physical, chemical, or biological changes
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Erosion The movement of sediment or soil from one location to another by means of water, wind, or ice
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Deposition When particles carried by water, ice, or wind are deposited in another location
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Metamorphic rock Rocky material experiences intense heat and pressure in the crust of the earth.
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Igneous rock Formed when magma cools and makes crystals.
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Sedimentary rock Form at or near the earth's surface at relatively low temperatures and pressures primarily by: deposition by water, wind or ice
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