• Shuffle
    Toggle On
    Toggle Off
  • Alphabetize
    Toggle On
    Toggle Off
  • Front First
    Toggle On
    Toggle Off
  • Both Sides
    Toggle On
    Toggle Off
  • Read
    Toggle On
    Toggle Off
Reading...
Front

Card Range To Study

through

image

Play button

image

Play button

image

Progress

1/18

Click to flip

Use LEFT and RIGHT arrow keys to navigate between flashcards;

Use UP and DOWN arrow keys to flip the card;

H to show hint;

A reads text to speech;

18 Cards in this Set

  • Front
  • Back
Correlation
Establishing the equivalence of rocks of similar age in different areas
law of superposition
this law states thati n an undeformed sequence of sedimentary rocks, each bed is older than the one above it and younger than the one below it
unconformity
represents along period during which deposition stopped erosion, removed previously formed rocks, and then deposition resumed. It is a surface that represents a break in the rock record, caused by erosion resumed.
relative dating
to identify which rock units formed first, second, third, and so on. It also tells us the sequence in which events occurred, not how long they occurred
uniformitarianism
simply states that the physical, chemical, and biological laws that operate today have laos operated in the geologic past. It means that the forces and processes that we observe today have been at work for a very long time
fossil
the remains or traces of prehistoric life. They are important components of sediment and sedimentary rocks
index fossil
a fossil that is associated wit ha particular span of geologic time
half-life
a common way of expressing the rate of radioactive decay. It is the amount of time necessary for one half of the nuclei in a sample to decay to its stable isotope
radioactivity
when nuclei are unstable, and they spontaneously break apart or decay
radiometric dating
the procedure of calculating the absolute ages of rocks and minerals that contain radioactive isotopes
radiocarbon dating
method for determining age by comparing the amount of carbon-14 to the amount of carbon-12 in a sample
geologic time scale
the divisions of earth's history in the blocks of time-eons, eras, periods, and epochs; the time scale was created using relative dating principles
eon
the largest time unit on geologic time scale, next in order of magnitude above era
era
a major division on the geologic time scale; eras are divided into shorter units called periods
period
a basic unit of the geologic time scale that is a subdivision of an era; it may be divided into smaller units called epochs
epoch
a unit of the geologic time scale that is a subdivision of a period
principle of horizontality
this is another one of stends observation that means that the layers of sediment are generally deposited in a horizontal position
principle of cross-cutting relationships
this relationship is an important principle used in relative dating. An intrusive rock body is younger than the rocks it intrudes. A fault is younger than the rock layers it cuts. This states that when a fault cuts through, or when magma intrudes other rocks and crystallizes we can assume that the fault or intrusion is younger than the rocks affected