The Fundamental Principles of Geology (1.3.2) Flashcards
1
Q
Methods of dating geological materials: Relative Ages
A
- Brought together concepts developed hundreds of years ago.
- Based on order of formation of features.
- Qualitative method.
- Assigns a relative order to events.
2
Q
Methods of dating geological materials: Absolute Ages
A
- Quantitative methods developed recently.
- Age is given as a number.
- Assign absolute dates to events.
3
Q
What is superposition?
A
- Rock layers laid down on top of another.
- Oldest layers at bottom, youngest at top.
- Determine relative ages of rock strata.
4
Q
What is origin horizontality?
A
- Sediments settle out of fluid by gravity.
- Causes sediment to accumulate horizontally.
- Sediment accumulation not favoured on slopes.
- Tilted sedimentary rocks likely to have been deformed.
5
Q
What is lateral continuity?
A
- Strata often form laterally extensive horizontal sheets.
- Spatially isolated.
6
Q
What are cross-cutting relations?
A
- Younger features truncate (cut across) older features.
- Faults, dykes, erosion etc must be younger than material that is faulting, intruded, or eroded.
- Volcano can’t intrude rocks that aren’t there.
7
Q
What are baked contacts?
A
- Igneous intrusions cooks invaded country rock.
- Baked rock must have been there first.
- Chilled margin formed (in younger, intrusive rock) at the contact, from rapid cooling.
8
Q
What are inclusions (rock fragment with another)?
A
- Weathering rubble must have come from older rock.
- Fragments (xenoliths) and igneous intrusions are older.
- Inclusions always older than enclosing material.
9
Q
What are uncomformities?
A
- Represent a time gap in rock record as result of non-deposition and erosion.
- Three types: Unconformity, nonconformity, disconformity.
10
Q
What are nonconformities?
A
- Igneous/metamorphic capped by sedimentary rocks.
- Crystalline igneous/metamorphic rocks exposed by erosion, sediment was deposited eroded on surface.
11
Q
What are disconformities?
A
- Parallel strata bounding non-deposition due to an interruption in sedimentation (pause in deposition, sea level falls, rises, erosion).
- May be hard to detect, sometimes detects from fossils.
12
Q
What is fossil succession?
A
- First appearance, range, and extinction used for dating.
- Fossils succeed one another in known order.
- Index fossils are diagnostic of particular geological time period.
- Fossils correlate strata locally, regionally, and globally.