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Fossils and rock layers

Review your understanding of fossils and rock layers with this free article aligned to NGSS standards.

Key points:

  • Sedimentary rocks typically occur in horizontal layers called strata.
  • In undisturbed strata, younger layers sit on top of older ones. This is known as the law of superposition.
  • Strata can be cut by other geologic features, such as faults or intrusions. A fault is a crack in Earth’s crust. An intrusion is a body of igneous rock formed within Earth’s crust.
  • When two features intersect, the one that cuts through the other is younger. This is known as the law of crosscutting relationships.
  • Some strata contain index fossils, or fossils associated with a specific time in Earth’s history. If the same index fossil is found in different strata far apart, the layers likely formed around the same time.
  • By studying strata, geologists have determined the relative order of major events in Earth’s history. The timeline of these events is called the geologic time scale.
Layers of sedimentary rock.
Sedimentary rock strata in the western United States. Image credit: “Folded layers” by arbyreed, CC BY-NC-SA 2.0.

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