test geologic time, met rocks Flashcards
Daughter product
The product of radioactive decay of a parent isotope
Absolute age
The actual age of a material in years
Parent isotope
An unstable isotope that will undergo radioactive decay
Half life
The amount of time required for half of the unstable parent substance to decay to the daughter product
HOW YOU FIND AGE OF ROCK
Radiometric dating
ratio between daughter and parent to find absolute age of rock
Radioactivity
Emission of high energy particles by unstable isotopes
geologic time scale
divides history of earth into time intervals
divisions of time
eon–> era—> period–> epoch–> year
age of earth
4.6 by
human existence vs. earth’s
humans= so small compared to earth’s like a sliver
uniformitarianism
present is key to the past
principle of original horizontality
sedimentary strata always form in horizontal layers
principle of original superposition
oldest layer of rock is on the bottom
law of cross cutting relationships
rock unit that crosses over another unit is always younger
principle of inclusions
inclusions are always older than the rock they are inside of
intrusions- young or old
always younger than rock they cut into
LOOK FOR FINGERS WHEN FINDING INTRUSIONS
disconformity
sed layers that have been eroded away, then covered by other depositing layers
nonconformity
erosional surface w igneous/metamorphic rock below, sed rock above
stratified rock rests on un stratified (igneous) rock
angular unconformity
angled or folded sed rocks are located below the erosional surface and horizontal layers of sed rocks are above
sed layers that have been tilted by force of tectonic plates then eroded
foliation
rock its layered, almost has skins peeling off, sheet like
when pressure squeezes flat minerals so they become aligned
protolith
first rock
regional metamorphism
large scale folding by compression at subduction zones
produces foliated rocks
contact metamorphism
when magma comes into contact with an already existing body of rock- usually sed
produces non foliated rocks
foliated rock
heat and pressure
subduction zones
regional metamorphism