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Chapter 17: The Rock Record

AB
Age of the earth4.6 billion years old
James HuttonThe first to suggest the age of the earth
Principle of uniformitarianismstates that current geologic processes, such as volcanism and erosion, are some processes that were at work in the past
Stratalayers of rocks
Relative AgeIndicates that one layer is older or younger than another layer
Law of superpositionAttempting to determine the relative age of layer of sedimentary rock
Ripple marksSmall waves formed on the surface of the sand by the action of wind or water
UnconformityIndicates that for a period of time deposition stopped, rock was removed by erosion, and then deposition resumed.
StratifiedSedimentary rock
StratifiedDeposited in layers
Unstratifiedmetamorphic and igneous rock
Wnstratifieddeep
nonconformityan uncoformity in which stratified rock rests upon unstratified rock
Angular unconformityoccurs when rocks are deposited in horizontal layers are folded or tilted and then eroded
Discomformitylayers of rock are eroded, and a new layer of rock is placed on top of the eroded layer indicating a great lapse of time
law of crosscutting relationshipsstates that the fault or an intrusion is always younger than the rock layers it cuts through
Absolute agethe actual age of a rock layer
varvelayers of dark colored sediment and light colored sediment
Radioactive decaysome radioactive elements decay into other elements at a set and definite time
paleonologistsstudy fossils and learn about the earth's past
Evolutionthe change in living things over time
Paleontologythe study of fossils
mummificationpreservation of a dead organism by dying
amberpreservation in hardened tree sap
tar bedspreservation of an organism in thick petroleum oozing to the earth's surface
Freezingpreeservation of an organism in frozen soil and ice because not all bacteria can survive in those conditions
Petrificationthe process by which minerals solutions such as ground water remove the original organic materials and replace them with other minerals
Trace fossilstracks,footprints, borings, and burrows that are used to study the past
imprintscarbonized prints of leaves, stems, flowers, and fish made in clay or soft mud in clay sedimentary rock
moldsempty cavities where shells,trees, and other parts of organic material can collect; the mold retains the shape of the artifact
casta replica of the outer surface of the original organism
Coprolitesfertilized dung or waste materials from ancient animals
Gastrolithsstones found in the digestive tracts of some dinosaurs that were used to help grind food
Index Fossilsfossils that are found exclusively in rock layers of a particular geologic age


Katherine Ewing

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