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Relative age of rocks https://www.youtube.com/watch?v=YgE-dSx-fPc&index=10&list=FLiMHnzsv_NuqhZrtgX5Rfxg.

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Presentation on theme: "Relative age of rocks https://www.youtube.com/watch?v=YgE-dSx-fPc&index=10&list=FLiMHnzsv_NuqhZrtgX5Rfxg."— Presentation transcript:

1 Relative age of rocks

2 Think pair share

3 Law of Superposition Top = youngest layer
In undisturbed sedimentary rock or lava flows In undisturbed sedimentary rock or lava Top = youngest layer Bottom = oldest layer The Law of Superposition is that an undeformed sedimentary rock layer is older than the layers above it and younger than the layers below it.

4 Law of Cross-Cutting Relationships
Any feature that cuts across a rock or layer of sediment is younger than the rock or layer it cuts youngest layer

5 Example of Cross-Cutting
Intrusion - igneous rock that forms when magma squeezes between existing rock and hardens Intrusion - igneous rock that forms when magma squeezes between existing rock and hardens

6 Example of Cross-cutting
Examples of Cross-Cutting Extrusion - igneous rock that forms when lava flows on Earth’s surface and hardens

7 Example of Cross-cutting Example of Cross-cutting
Inclusion - pieces of older rock trapped within younger rock

8 Examples of Cross-Cutting
Faults, joints, tilts, and veins also follow the law of cross--cutting relationships

9 Formation of an Unconformity

10 Formation of an Unconformity

11 Formation of an Unconformity

12 Formation of an Unconformity

13 Formation of an Unconformity

14 Picture of Unconformity


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