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Science · Grade 6 Science

Chapter 1: Earth, Sun, and Moon

Tides and the Moon's Pull

Two a day, and one of them on the wrong side.

Lesson
5
Time
About 25 minutes
0 of 10 done
Part 1 of 10Something to Notice
Practice
Developing and using models
Crosscutting concept
Cause and effect
Core idea
ESS1.B: Earth and the Solar System

Step 1: Something to Notice

Watch first. The explanation comes later.

Watch the idea first — 51 seconds. Then read on, and try it yourself in the next step.

A tide table for any coast shows high water roughly every 12 hours and 25 minutes — two high tides and two low tides each day, arriving about fifty minutes later each day.

If the Moon is only ever on one side of Earth at a time, why are there two high tides a day and not one?

Step 2: Find Out

Watch the red town go round once and read its tide off the curve underneath.

Step 1 — Predict

In one rotation of Earth, how many high tides will the town pass through?

Choose what you think will happen. You cannot see the experiment until you do — guessing first is what makes it worth watching.

Step 3: Find Out

The Sun raises tides too, at about 46% of the strength. Move it around and watch the range.

Step 1 — Predict

When the Sun and Moon are lined up, what happens to the difference between high and low tide?

Choose what you think will happen. You cannot see the experiment until you do — guessing first is what makes it worth watching.

Step 4: So Here Is Why

Now the explanation, after you have seen it happen.

Two bulges

There are two high tides and two low tides at most coasts each day, roughly 12 hours 25 minutes apart.

It is the difference that matters

A difference in pull

Gravity gets weaker with distance, so the Moon pulls the near water harder than it pulls the solid Earth, and the solid Earth harder than the far water. It is that difference across Earth's width — not the pull itself — that raises tides.

Tidal force The difference in gravitational pull across an object's width, which stretches it.

Stretched, not pulled

Stretched both ways

The result is that Earth is stretched along the line to the Moon, with a bulge of water at each end. The far bulge is water being left behind, not water being pushed.

Two bulges, one rotation

Earth turns under

The bulges stay lined up with the Moon while Earth turns underneath them. Any coast passes through both in one day, which is the two high tides.

The Sun helps

The Sun helps

The Sun raises tides too, at about 46% of the Moon's strength. Lined up with the Moon they add, giving the large spring tides at new and full moon. At right angles they partly cancel, giving the small neap tides at the quarters.

Spring tide The largest tides, when the Sun and Moon pull along the same line.

What this model leaves out

Real coasts differ

Real tides are also shaped by the ocean basin the water sloshes around in. That is why the Bay of Fundy has a range of fifty feet and parts of the Gulf of Mexico get only one tide a day. The two-bulge model explains the cause; the coastline explains the local details.

Two a day, and one on the wrong side

There is a tidal bulge facing the Moon and another on the opposite side. The near side is pulled hardest, the far side least, so the Earth is stretched — which produces two high tides daily.

The Sun matters too

When Sun and Moon line up, their effects add and tides are largest. When they are at right angles the tides are smallest. The pattern of spring and neap tides follows the Moon's phases.

Step 5: A Common Mistake

Lots of people think

The Moon pulls the ocean toward it, so there is one high tide — on the side of Earth facing the Moon.

Step 6: Why the Tide Is Later Each Day

The same idea somewhere new.

Earth takes 24 hours to spin once, but the Moon has moved about 13° further round its orbit in that time, so the town needs an extra 50 minutes to catch up with it. That is why high tide is roughly fifty minutes later each day, and why the tide table on a harbor wall is a list rather than a single time. The same arithmetic explains why the tidal day is 24 hours 50 minutes rather than 24.

Later each day

Step 7: Think It Through

Practice makes it stick.

The Tide Table

Problem 1 of 2

High tide today is at 6:00 in the morning. Tides run about 12 hours 25 minutes apart. To the nearest hour, what time is the next high tide? Give a 24-hour clock hour.

hundred hours

Catching Up

Problem 2 of 2

Earth spins once in 24 hours, but the Moon has moved on, so the town needs about 50 more minutes to line up with it again. How many minutes is a tidal day?

minutes

Bulges and Ranges

1 of 4

How many high tides does a coast get in one rotation of Earth?

2 of 4

What causes the bulge on the side facing away from the Moon?

3 of 4

At which two phases of the Moon do spring tides happen?

4 of 4

Match each arrangement to the tide it produces.

Tap a card on the left to start.

Step 8: Quick Check

Show what you know.

Question 1 of 1

Why are there two high tides a day rather than one?

Step 9: Explain It in Writing

Claim, evidence, then reasoning.

The question

A tide table shows two high tides a day. A classmate says this is impossible if the Moon pulls the water toward itself, because the Moon is only on one side. Using the model, explain what causes the second high tide.

Words to usetidal bulgerotationstretchfar sidepulldifference

Fill in all three boxes. The reasoning box is the one that matters most.

What You Found Out

  • Tides come from the difference in the Moon's pull across Earth, not from the pull itself.
  • Earth is stretched along the Moon line, so there is a bulge at each end.
  • One rotation past two bulges is two high tides a day.
  • Sun and Moon aligned gives spring tides; at right angles gives neap tides.