1Metamorphic rocks
form when pre-existing rocks are exposed to increased pressure and/or temperature, causing solid-state recrystallization
2Protolith
the rock before
3Heat and pressure
Causes of Metamorphism (2)
4Recrystallization
Phase change
Neocrystallization
Pressure solution
Plastic deformation
Consequences of Metamorphism (5)
5Recrystallization
same mineral, new size and shape
6Phase change
same composition, new mineral
7Neocrystallization
growth of new mineral (chem and structure)
8Pressure solution
minerals smooshed together. Dissolution occurs at grain to grain contacts and new growth occurs in locations with less pressure
9Plastic deformation
changing shape without breaking under high pressure and temperature
10Porphyroblast
large crystal that grows within a finer-grained matrix during metamorphism
11Compression
squeezing a material
12Shear
moving part of a material sideways relative to another
13Dynamic (Regional) metamorphism
metamorphism with high pressure but relative low temperature that happens in subduction zones; happens over a large region
14Contact metamorphism
metamorphism where heat is transferred from melt to surrounding rock
15Burial metamorphism
metamorphism where, with depth, both pressure and temperature increase (but not extreme)
16Shock metamorphism
metamorphism with intense heat and pressure from shock wave pulse
17Foliation
planar rock fabric
18Uniformitarianism
the present is the key to the past
19Superposition
youngest on top
20Original horizontality
sediment layers are fairly horizontal when deposited and can be altered by deformation
21Lateral continuity
sediment generally deposited in continuous sheets. If later cut, you can assume once continuous
22Cross-cutting relationships
igneous intrusive must be younger than the rock it cuts across
23Baked contacts
heat transferred from igneous melt to surrounding rock. Evidence that surrounding rock existed prior to igneous rock
24Law of Inclusions
rock containing inclusion is younger than the inclusion
25Faunal succession
fossils that can be used for relative dating
26William “Strata” Smith
who realized that strata occurred in a predictable pattern and he could use fossils to trace rock layers. Made the first detailed nationwide geological map
27Angular unconformity
beds tilted and eroded prior to deposition of new horizontal bed on top. Forms between two strata not parallel to each other
28Radioactive decay
process by which the nucleus of an unstable atom loses energy by emitting radiation
29Nonconformity
igneous or metamorphic rock surface eroded and then sedimentary rock deposited on top. Forms between older metamorphic or igneous rocks and younger sediment strata deposited on top of them
30Disconformity
erosional surface between sedimentary rock layers where the older rock layer has been eroded but not tilted
Forms between parallel strata
31Electrons
Nuclear particles
Smaller nucleus
Electromagnetic radiation
Radiation can be one or more of the following (4)
32Isotope
same element (number of protons) but different number of neutrons
33Half-life
time required for one-half of parent to be converted into daughter
34Eon - Era - Period - Epoch - Age - Chron
Hierarchy of Geological Time