relative dating Flashcards
1
Q
What is the difference between relative dating and absolute dating?
A
Relative: when events occurred relative to one another. “which one came first”
Absolute: when events actually happened. “How old is it?”
2
Q
What different diagnostic methods are used to assess relative and absolute
geologic age?
A
- principles of superposition, original horizontiality, corss cutting relationships, inclusions, funal successions, and correlation
3
Q
Principle of Superposition
A
- Nicholas Steno, 1669
- in any undisturbed sedimentary rock, the oldest layer will always be at the bottom, successively
younger layers on top
4
Q
What are unconformities?
A
- a gap in the geological record; most often an erosion surface
5
Q
Principle of Original Horizontality
A
- Nicholas Steno
- beds of sediment laid down in water form horizontal layers on top
- original rocks started as horizontal; an event occurred which caused folding
6
Q
Principle of of Cross-Cutting Relationships
A
- Steno (1669), Hutton (1795), Lyell (1830)
- a geological feature that cuts across or perpendicular another body of rock much be younger than the rock mass penetrated
7
Q
Principle of Lateral Continuity
A
- Steno
- layers of rock care continuous until they encounter other solid bodies that block their deposition or until they are acted upon by agents that appear after deposition took place
8
Q
Principle of Inclusions
A
- Lyell, 1830
- fragments included in the host rock are older than the host rock
9
Q
Principle of Faunal successions
A
- Smith, 1800
- fossil species succeed one another in a recognizable order
- index fossils relate to specific time period
10
Q
Correlation
A
- determining time equivalency of rock units
- similarity in lithology and/or fossils
- 3 types: disconformity, angular unconformity, and nonconformaity
11
Q
Disconformity
A
- layers above and below the unconformity are parallel to eachother
12
Q
Angular Unconformity
A
- younger beds overlie tilted or folded beds
13
Q
nonconformity
A
- younger beds overlie much older metamorphic or plutonic rocks