Mississippi Science MAQ.3.4

ScienceGrades 9–12Marine and Aquatic Science I & II

The Standard

MAQ.3
Students will understand the principles of plate tectonics, sea floor spreading, and physical features of oceanic zones.
Classify zones of freshwater sources based on the velocity of current, depth, and temperature.

2026 Mississippi College- and Career-Readiness Standards for Science · Geological Features

Teacher's field guide

What This Standard Means

What Students Need to Do

Students use current speed, depth, and temperature readings to sort parts of streams and lakes into zones. They explain which readings support each choice.

What Mastery Looks Like

Given measurements from a stream, a student identifies fast, shallow riffles and slow, deep pools. Given summer lake readings, they distinguish warmer surface water from colder deep water.

Common Misconceptions

Students may call any slow stream water a pool, even when it is shallow. They may assume a lake has the same temperature from top to bottom, or that deep water stays cold in every season.

How to Assess It

Exit ticket: Label two stream sites, A (0.2 m deep, 0.8 m/s) and B (2 m deep, 0.05 m/s), as riffle or pool, with one reason each. On a summer day, which lake sample likely came from deeper water, 24°C or 9°C?

Lesson moves

Ways to Teach It

  1. Build a stream tray with gravel; time floating corks across shallow and deep sections, then measure depth and temperature at each spot.

  2. Ask: Why might a deep pool stay cooler than a shallow riffle on a sunny afternoon? Write a claim using two measurements.

  3. Give pairs six site cards with speed, depth, and temperature readings; have them sort riffles, pools, lake surface water, and lake deep water.

  4. Give students a river map with depth, speed, and temperature readings; have them mark where to avoid strong current while wading.

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Printable MAQ.3.4 Worksheet

Preview of the MAQ.3.4 printable worksheet

A ready-to-print activity worksheet aligned to MAQ.3.4, with an answer key for the teacher on its own page. No account needed.

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