Florida SC.7.E.6.3

Science7th GradeEarth Structures

The Standard

Identify current methods for measuring the age of Earth and its parts, including the law of superposition and radioactive dating.

Florida Next Generation Sunshine State Standards for Science

Teacher's field guide

What This Standard Means

What Students Need to Do

Students compare relative dating with radiometric dating. They use rock layer position to order events and isotope decay data to estimate numerical ages.

What Mastery Looks Like

Given an undisturbed rock diagram, a student correctly identifies the oldest and youngest layers and explains why. Given half-life data, the student estimates a rock's age.

Common Misconceptions

Students may think deeper layers are always older, even when rocks have been folded, faulted, or overturned. They may think carbon-14 dates all rocks or that radiometric dates are guesses.

How to Assess It

Give students a four-layer rock diagram and a sample with two half-lives elapsed. Ask them to order the layers and calculate the sample's age.

Lesson moves

Ways to Teach It

  1. Stack colored clay layers, cut the stack, and have students label relative ages before and after tilting or faulting.

  2. Ask students to write: Why can radiometric dating give a numerical age while superposition usually cannot?

  3. Play a card sort matching rock diagrams, oldest-to-youngest sequences, isotope data, and calculated ages.

  4. Use simplified volcanic ash data to determine the age range of a fossil found between two dated ash layers.

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Printable SC.7.E.6.3 Worksheet

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