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All 30 terms

TermDefinition
Relative Datingmethod for determining if an event or rock is younger or older than others.
Principle of Original Horizontalitylayers of sediment that are generally deposited in a horizontal or nearly horizontal position
Law of SuperpositionThe geologic principle that states that in horizontal layers of sedimentary rock, each layer is older than the layer above it and younger than the layer below it.
Principle of Cross Cutting RelationshipsPrinciple that a fault or intrusion is younger than the rock layers affected by it
StrataDistinct layers of rock
Igneous Intrusionalways younger than the rock it has intruded, cross cuts
Unconformitya place where an old, eroded rock surface is in contact with a newer rock layer
Unformitarianisma principle that states that geologic process that occured in the past can be explained by current geological process
Correlationestablishing the equivalence of rocks of similar age in different areas
Fossilthe remains (or an impression) of a plant or animal that existed in a past geological age and that has been excavated from the soil
Index Fossila fossil known to have lived in a particular geologic age that can be used to date the rock layer in which it is found
Absolute Age Datinguses radioactive decay to determine an exact age
Half-Lifethe time required for something to fall to half its initial value (in particular, the time for half the atoms in a radioactive substance to disintegrate)
Radiometric Datingthe procedure of calculating the absolute ages of rocks and minerals that contain radioactive isotopes
Radiocarbon Datingmethod measuring the decay rate of carbon isotopes in organic matter to provide dates for organic materials like wood or fiber
Isotopeone of two or more atoms with the same atomic number but with different numbers of neutrons
Parent Isotopean unstable radioactive isotope
Daughter productradioactive decay resulting from the parent isotope
RadioactivitySpontaneous emission of radiation by some elements
Geologic Time Scalethe division of Earth history into blocks of time--eons, eras, periods, and epochs. The time scale was created using relative dating principles.
Principle of InclusionStates that the pebbles cemented into a sediment matrix are older than the matrix itself
Faunal SuccessionThat certain fossils will never be found together. You can identify a strata of rock by its fossils
Shieldsexpansive, flat regions composed of deformed crystalline rock found within the stable interiors of continents, made by erosion of ancient mountain systems, ex: Canadian Shield in northeast North America
Stromatolitesfossilized bacteria grew like stacks of pancakes, estimated at 3 billion years old, one of the oldest living things found on Earth
Gondwanalate Paleozoic continent that formed the southern portion of Pangaea, consisting of all or parts of present-day South America, Africa, Australia, India, and Antarctica
LaurasiaLate Paleozoic, Northern Hemisphere continent composed of the present-day continents of North America, Greenland, Europe, and Asia
Dinosaurany of numerous extinct terrestrial reptiles of the Mesozoic era
Gymnospermplant that produces seed that are not enclosed by a protective fruit
Mammala warm-blooded vertebrate with hair or fur and females produce milk to feed their young
Angiospermflowering plant; bears its seeds within a layer of tissue that protects the seed
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Terms 30
Creator Urchin123
Created October 8, 2009
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