NGSS HS-ESS1-5

ScienceGrades 9–12Earth's Place in the Universe

The Standard

Evaluate evidence of the past and current movements of continental and oceanic crust and the theory of plate tectonics to explain the ages of crustal rocks.

Next Generation Science Standards

Teacher's field guide

What This Standard Means

What Students Need to Do

Students read rock-age maps, sample tables, and distance data to find age patterns across oceanic and continental crust. They use those patterns to judge how well plate movement explains where younger and older rocks occur.

What Mastery Looks Like

Students identify that ocean crust gets older away from spreading ridges and continental crust often gets older toward ancient cores. They cite mapped ages or sample data to support a plate movement explanation.

Common Misconceptions

Students may think ocean crust is oldest near a ridge because the ridge formed first. They may also confuse rock age with Earth’s age or assume continental crust gets younger toward its ancient core.

How to Assess It

Give students these data: ocean crust at 0, 400, and 800 km from a ridge is 2, 22, and 43 million years old. Ask them to explain the pattern, name the plate process, and cite two data points.

Lesson moves

Ways to Teach It

  1. Build a paper seafloor model by pulling colored age bands apart from a central slit, then label the youngest and oldest crust.

  2. Write a claim explaining why Atlantic crust ages form matching bands on both sides of the Mid-Atlantic Ridge, using map evidence.

  3. Sort cards showing rock ages, locations, and plate settings, then match each set with spreading, collision, or continental growth.

  4. Use an ocean-floor age map to choose two possible drilling sites for young and old crust, then defend each choice.

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Printable HS-ESS1-5 Worksheet

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Learning progression

Where This Standard Sits

See the whole path on the Earth & Space Science progression map.

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