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Earth Science · Geology · Earth Interior

Relative ages of rock layers

Overlapping layers and cross-cutting structures reveal the relative order of geological events. Relative order must be distinguished from absolute age.

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Relative ages of rock layers
Relative ages of rock layers: simulation view →

Meaning and mechanism

When dealing with non-inverted sedimentary layers, the “superposition principle” can be applied, stating that the lower layer was deposited before the upper layer. It is essential to first verify the original depositional state.

The fault cutting into an intruded rock or layer was formed after the intrusion. By connecting multiple relationships, it is possible to establish the sequence of deposition, intrusion, and fault events.

Relationships and conditions

Discordance refers to the gap between observed data and expected values, which arises when erosion ceases or when an existing stratum has been eroded over a period of time. The fact that there is a gap, and the length of that period, are separate pieces of information.

When dealing with layers overturned by drainage or with deposited materials, a simple “up and down” assessment cannot be applied directly. In absolute dating, separate dating measurement data is required.

What to observe in the simulation

The order is determined by the law of superposition, law of penetration, and law of cutting. The unconformity represents time of loss of deposition and erosion.

It covers only the two sedimentary layers that have not been overturned and designated faulting, intrusion, and erosion events. Absolute age and duration of unconformity are not calculated. Tilt and displacement are for explanatory purposes only and do not restore the actual geological structure.

Key relationships and symbols

The cutting incident is younger than the cutting subject.

Symbols and units used in the formulas
SymbolMeaningUnit
SuperpositionLower layers form first in an undisturbed sedimentary sequenceOrdering relationship
Cross-cuttingA cross-cutting event is younger than what it cutsOrdering relationship

Worked example

What if a fault cuts the intrusive rock that cuts both A below and B above?

According to the law of superposition, B is younger than A, and according to the law of penetration and cutting, the cutting event is younger than the cut object.

Common misconceptions

  • It is not possible to directly calculate the age of each layer simply by knowing the relative order.

Explore this concept through experiments

References

BCcampus · Physical Geology (English)