Quiz (Chapter 9) Flashcards
Numerical Dates
specify the number of years that have passed since an event occurred
specific and exact
Correlation within limited areas
- position of bed in a sequence
- matching of rocks of similar ages from different regions
- Fossils
Principal of Fossil succession
Fossils are arranged according to their age
Index fossils
widespread geographically and limited to a short period of geologic time
Fossil assemblage
group of fossils used to determine a rocks age
Environmental indicators of fossils
Fossils can be used to infer information about past environments
nucleus of an atom
protons +, neutrons 0
Electrons
negatively charged particles that orbit the nucleus
Atomic number
is told by the number of protons
The importance of a Time scale
-rocks record geologic and evolutionary changes throughout history
Principle of Superpostition
in sedimentary rocks, each bed is older than the above and younger than the one below
Principle of Original Horizontality
Layers of sediment are generally deposited in a horizontal position
Rocks layers that are flat have not been disturbed
Principle of Lateral Continuity
Beds originate as continuous layers that extend in all directions until they eventually thin out or grade into a different sediment
-continuous from side to side
Principle of Cross-Cutting
younger features cut across older features
Inclusions
fragments of one rock unit that are enclosed within another rock unit
-the rock containing the inclusion is younger