Geology Principles of Relative Dating

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Questions and Answers

What does the Principle of Original Horizontality state?

  • Rock fragments within another rock are younger.
  • Sedimentary layers are deposited in horizontal layers. (correct)
  • Fossils appear in a recognizable order over time.
  • The oldest layer is always on top.

Which type of unconformity involves older sedimentary layers being tilted or folded?

  • Disconformity
  • Nonconformity
  • Angular Unconformity (correct)
  • Paraconformity

What does radiometric dating primarily measure?

  • The sequence of rock layers
  • The decay of radioactive isotopes (correct)
  • The position of fossils in layers
  • The thickness of sedimentary rocks

In the Principle of Faunal Succession, what is the significance of fossil organisms?

<p>They allow for the correlation of rock layers over distance. (D)</p> Signup and view all the answers

Which method is suitable for dating very old rocks using radiometric principles?

<p>Uranium-Lead Dating (C)</p> Signup and view all the answers

What is a characteristic of a disconformity?

<p>It indicates significant erosion or non-deposition. (A)</p> Signup and view all the answers

What is a half-life in the context of radiometric dating?

<p>The time required for half of a radioactive isotope to decay (D)</p> Signup and view all the answers

Which principle suggests that a geological feature cutting through another must be younger?

<p>Principle of Cross-Cutting Relationships (D)</p> Signup and view all the answers

Flashcards

Principle of Superposition

In undisturbed sedimentary rock layers, the oldest is at the bottom.

Principle of Original Horizontality

Sedimentary layers are deposited horizontally; tilting happens later.

Principle of Cross-Cutting Relationships

Features that cut through layers are younger than the layers they cut.

Principle of Inclusions

Rock fragments found in another rock must be older than that rock.

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Disconformity

A gap between parallel sedimentary layers due to erosion or non-deposition.

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Nonconformity

Sedimentary rocks on eroded igneous or metamorphic rocks, indicating a gap.

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Half-Life

The time it takes for half of a radioactive isotope to decay.

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Carbon-14 Dating

A method to date organic materials up to about 50,000 years old.

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Study Notes

Relative Dating Principles

  • Superposition: In undisturbed sedimentary rock layers, the oldest layer is at the bottom, and the youngest at the top.
  • Original Horizontality: Sedimentary layers are originally deposited horizontally. Tilting or folding indicates later events.
  • Cross-Cutting Relationships: A geological feature (fault, intrusion) that cuts across existing layers is younger than the layers it cuts through.
  • Inclusions: Rock fragments (inclusions) within a rock are older than the rock they are included in.
  • Faunal Succession: Fossil organisms appear and disappear in a specific, recognizable order, used to correlate rock layers across different locations.

Unconformities

  • Disconformity: A gap in the rock record between parallel layers of sedimentary rock, often subtle due to erosion or non-deposition.
  • Angular Unconformity: Older tilted or folded rock layers are eroded, and younger horizontal layers are deposited on top.
  • Nonconformity: Sedimentary rocks rest on eroded igneous or metamorphic rocks, indicating a long period of erosion or missing time.
  • Paraconformity: A type of disconformity where there are no visible signs of erosion but a period of missing time exists in the rock record.

Radiometric Dating

  • Radiometric Dating: Measures radioactive isotope decay to determine absolute ages of rocks and minerals.
    • Parent Isotope: The original radioactive isotope.
    • Daughter Isotope: The stable product resulting from decay.
    • Half-Life: The time it takes for half of a radioactive isotope to decay.
  • Common Methods:
    • Carbon-14 Dating: Used for organic materials up to ~50,000 years old.
    • Uranium-Lead Dating: Used for very old rocks (millions to billions of years).
    • Potassium-Argon Dating: Used for volcanic rocks (useful in archaeology and geology).
    • Rubidium-Strontium Dating: Used for very old rocks & minerals.
  • Complement to Relative Dating: Radiometric techniques provide absolute age data, complementing the relative age information from stratigraphy.

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