unit 2 (dating)
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Catastrophism
Earth’s physical features were formed by sudden unexplainable events
Uniformitarianism
the geologic processes at work today were also active in the past
relative dating
places events in a sequence of events, cannot tell us how long ago something happened, only that it followed one event and preceded another
absolute dating
identifies the actual date of an event
superposition
in any undisturbed sequence of sedimentary rocks, a sedimentary layer is older than the layers above it and younger than the ones below it
horizontality
most layers of sediment are deposited in a horizontal position, and if they aren’t, they were moved into that position later
cross-cutting
igneous rock is younger than the rocks it has cut across
included fragments
pieces of one rock found in another rock must be older than the rock in which they are found
fossil succession
in a stratigraphic sequence, different fossils appear in a definite order. Once a species disappears it will never reappear higher in the sequence
unconformites
buried eroded surfaces which represent gaps in geologic time.
angular unconformity
compressional forces cause layers to fold as they uplift
disconformity
rock layers above and below the eroded surface area parallel
nonconformity
eroded surface of metamorphic or igneous layers are buried by younger sedimentary layers
folding
when sedimentary rocks are compressed and bend into wave like patterns
faulting
crack in the Earth’s surface along which movement occurs
contact metamorphism
when molten rock comes into contact with older rock the heat causes a kind of baking that changes the older rock
radioactive dating
a radioactive sample is the parent material, and the decayed product is called the daughter material.
isotope
chemical element
what is a fossil
remains of organisms found in sedimentary rocks
half life
the rate at which a radioactive element decays
what do fossils indicate
age of rocks and the environment in which rocks are formed
carbonization
fine sediment encloses delicate matter in an oxygen poor environment. Over time, pressure squeezes out remnants,leaving behind a thin residue of carbon
what conditions are necessary for fossils to form
rapid burial (scavengers/decomp by bacteria) presense of hard body parts low oxygen environment (decomp is slower)
mould
organisms buried in sediment then dissolved, leaving an impression