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The Rock Record

Students will identify terms relating to determing relative and absolute age and the fossil record.

AB
principle of uniformitarianismstates that all present geolgical processes are same processes as in past
James Huttontheorized that forces at work were the same as those in the past
stratalayers of rock
relative agetells age in relation to others around it
bedding planeboundary between two layers of rock
law of superpositionstates that undisturbed sedimentary rock is older than layers above and younger than those below
ripple markssmall waves in rock formed by wind and water
unconformityperiod in which deposition stopped and erosion started leaving a break in geologic record
nonconformityunconformity in which stratified rock sits upon unstratified
angular unconformityrock layers are folded or tilted and new layers deposited on top
disconformityhorizontal layers rest on top of eroded horizontal layers, leaving a gap in the rock record
law of crosscutting relationshipsstates that a fault or intrusion is youger than layers it cuts through
absolute ageactual age of a rock layer
varvesannual layers of sediment that form in lakes and can be counted to tell age of rock
radioactiveelements that emit particles and energy
radioactive decayprocess in which elements emit particles and change into different elements
Pb-206end product in the decay of U-238
parent elementthe element that starts radioactive decay
daughter elementthe final product of radioactive decay
half-lifetime it takes for half the mass of a given amount of an radioactive
Carbon-14decays into Nitrogen-14 and can be used to date anything once living
paleontologistsstudy fossils to learn about past
evolutionchange of living things over time
paleontologystudy of fossils
mummificationdrying of organisms to produce fossils
amberhardend tree sap
tar bedsthick accumulation of petroleum that traps and preserves organisms
freezingpreservation of organisms through low temperatures
petrificationprocess in which minerals replace organic material
trace fossilstracks, footprints, etc. in which only parts of organisms remains
imprintdisplays the surface features of organism
moldretains shape and surface markings of organism
castreplica of outer surface of organism
coprolitesfossilized fecal matter
gastrolithsstones that helped dinosaurs with digestion
index fossilfossil that is used to determine the age of a specific rock layer
ammonitemarine organism that serves as the index fossil for Jurassic/Cretaceous Periods
trilobitemarine fossils that serves as index fossil for Mesozoic Era


Teri Griffin

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