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Fossils
are the preserved remains or traces of living things; they provided evidence of how life has
changed over time
paleontologist
scientist that studies, collects & classifies fossils
fossil record
all the information that paleontologists have collected about past life
evolution
the gradual change in living things over long periods of time
extinct
an organism no longer exists & will never again live on Earth
The Relative Age of Rocks
the rock's age compared with the ages of other rocks
absolute age
the number of years since a rock formed
index fossils
a fossil that is widely distributed & represents a type of organism that existed only briefly
Law of superposition
in horizontal sedimentary rock layers the oldest layer is at the bottom
cross-cutting relationships
study extrusions & intrusions of igneous rock
study of faults
a fault is always younger than the rocks it cuts through
study of unconformity
a gap in the geologic record that shows where some rock layers have been lost because of erosion
Radioactive Dating of Rocks
the process of using radioactive rocks to determine the numerical age of a rock
Planetary Differentiation
where a planetary body develops into compositionally distinct layers, the denser materials sink to the center, while the less dense materials rise tot he surface
Geologic Time Scale
a record of the life forms and geologic events in Earth's history, it is used to show Earth's history
Molds and Casts
most common fossils; are a hollow area in sediment in the shape of an
organism or part of it; forms when dissolved minerals in water seep into the empty space of a hollow area in sediment in the shape of the organism
Petrified Fossils
minerals replace all or part of an organism
Carbon Films
an extremely thin coating of carbon on rock
Trace Fossils
these provide evidence of the activities of ancient organisms
Preserved Fossils
Tar, Amber, & Ice
Law of Original Horizontality
rocks & sediment are always deposited in horizontal layer
half-life
the amount of time that it takes for 1/2 of a portion of radioactive material to break down into a new stable element
Eon
88% of Earth's history; ended 544 million yrs. ago
Era
the three largest divisions of geologic time after the Precambrian.
Period
subdivisions of each of the 3 Eras - are named after places in the world where geologists first discovered the rocks and fossils of each period