Chapter 13--Clues to Earth's Past

absolute age

The calculated age of an artifact from a specific dating method that is used to determine when the artifact was made

carbon film

a type of fossil consisting of an extremely thin coating of carbon on rock

cast

mineral-rich water or other sediment fills a cavity and forms new rock which produces a copy of the original object

fossil

the remains, imprints, or traces of a plant or animal that existed in a past geological age

half-life

length of time required for half of the radioactive atoms in a sample to decay

index fossil

a fossil known to have lived in a particular geologic age that can be used to date the rock layer in which it is found

mold

a cavity into which liquid is poured to create a given shape when it hardens

permineralized remains

fossils in which the spaces inside are filled with minerals from groundwater

principle of superposition

the principle that in a series of stratified sedimentary rocks the lowest stratum is the oldest

radioactive decay

the process in which a radioactive isotope tends to break down into a stable isotope of the same element or another element.

radiometric dating

A method paleontologists use for determining the ages of rocks and fossils on a scale of absolute time, based on the half-life of radioactive isotopes.

relative age

the age of an object in relation to the ages of other objects

unconformity

a break in the geologic record created when rock layers are eroded or when sediment is not deposited for a long period of time

uniformitarianism

principle that Earth's processes occurring today are similar to those that occurred in the past