Phases of the MoonUnderstandabout 40 min
Reading the Moon: one angle explains everything
Elongation, lit fraction, rise times, the terminator and why one face always faces us
Turn the phase picture into a tool. Learn to go from the Sun-Earth-Moon angle to the shape, the fraction lit and the rise and set times; find out why craters show best at quarter moon, what earthshine is, and why the Moon keeps one face towards Earth.
In this part you’ll
- Define elongation and use it to work out the phase, the lit fraction and the rise and set times.
- Explain why the lit fraction grows unevenly through the month.
- Use the 15-degrees-per-hour rule to predict when a given phase is above the horizon.
- Explain the terminator, earthshine and why a full moon looks flat in binoculars.
- Explain synchronous rotation and distinguish the far side from the night side.
In Discover you met the idea: half the Moon is always lit, and the phase is how much of that lit half faces us.
That is the right picture, but it is not yet a tool. With it alone you cannot say what the Moon will look like on the 19th, or what time it will rise, or which craters will show up best in binoculars.
This layer turns the picture into a tool. It comes down to a single number — the angle between the Sun and the Moon as seen from Earth — and once you can read that angle, everything else follows: the shape, the name, the fraction lit, the rise time, the set time, and even which way up it looks.
Chapter 01
One angle runs everything: elongation
Stand on Earth. Point one arm at the Sun. Point the other arm at the Moon. The angle between your arms is called the elongation of the Moon.
That single angle decides the phase completely.
- Elongation 0 degrees: Sun and Moon in the same direction. Its lit half points away from you. New moon.
- Elongation 90 degrees: a right angle. You are looking at the lit half exactly side-on, so you see half of it. Quarter moon.
- Elongation 180 degrees: Sun and Moon in opposite directions, Earth in the middle. The lit half is aimed straight at you. Full moon.
Between those, the phase changes smoothly. Elongation does not jump; it grows steadily, day after day, from 0 all the way round to 360 — and 360 is the same as 0, so the cycle begins again.
| Elongation | Day of the month | Lit fraction | What you see |
|---|---|---|---|
| 0° | 0.00 | 0.0% | Nothing: new moon |
| 30° | 2.46 | 6.7% | A very thin crescent, hard to find |
| 45° | 3.69 | 14.6% | A clear crescent |
| 60° | 4.92 | 25.0% | A thick crescent |
| 90° | 7.38 | 50.0% | Exactly half: first quarter |
| 120° | 9.84 | 75.0% | Gibbous, clearly more than half |
| 135° | 11.07 | 85.4% | A fat gibbous |
| 150° | 12.30 | 93.3% | Almost full; a dark rim on one side |
| 180° | 14.77 | 100.0% | A complete bright disc: full moon |
Worked example
0 / 6 steps shownHow much of the Moon is lit 5 days after new moon?
The Moon is 5.0 days past new moon. Work out its elongation and the fraction of the disc that is lit, and name the phase.
Try it
Chapter 02
The eight phases, with numbers
Here is the whole month in one table. Every number in it was calculated from the elongation, not looked up.
Read it across: the phase, where the Moon is in its orbit as an angle, how many days into the month that is, and how much of the disc is bright.
| Phase | Elongation | Day | Lit | Bright side (from India) |
|---|---|---|---|---|
| New moon | 0° | 0.00 | 0.0% | — |
| Waxing crescent | 45° | 3.69 | 14.6% | Right |
| First quarter | 90° | 7.38 | 50.0% | Right |
| Waxing gibbous | 135° | 11.07 | 85.4% | Right |
| Full moon | 180° | 14.77 | 100.0% | All of it |
| Waning gibbous | 225° | 18.46 | 85.4% | Left |
| Last quarter | 270° | 22.15 | 50.0% | Left |
| Waning crescent | 315° | 25.84 | 14.6% | Left |
- Synodic month
- 29.531 dNew moon to new moon: 29 days, 12 hours, 44 minutes. The cycle of the phases.
- Sidereal month
- 27.322 dOne full orbit against the stars: 27 days, 7 hours, 43 minutes. Shorter — and Go deeper explains why.
- Quarter to quarter
- 7.38 dA week and a fraction. Not exactly seven days, which is one reason the phases drift across our seven-day week.
- Daily elongation gain
- 12.19°How much the Moon pulls ahead of the Sun each day. In one day the shape changes visibly.
- Daily moonrise delay
- 49 min12.19° ÷ 15° per hour = 0.81 hours. Why the Moon is later every night.
- Moon's apparent size
- 0.52°About half a degree: your little fingernail at arm's length covers it easily. The same as the Sun's apparent size, near enough.
Lab
Match the Moon's position in its orbit to the shape you see, and test yourself on naming phases from either view.
Up in the sky: Rises around midday, so it is high in the sky all afternoon, in full daylight. Sets around midnight. Sets about 12:01 am.
The Sun lights exactly half the Moon, all month long. What changes is where we are standing to look at it. Day 7.4 means the Moon is 90.21° round its orbit from new moon.
Text version of this activity
Two linked panels. The space view looks down on Earth's orbit: the Sun far off to the left, Earth in the centre, the Moon on a circle around it. The sunlit half of Earth and of the Moon are shaded bright; the other halves are dark. The sky view shows the Moon as it would appear from India at that moment.
It opens at day 7.4, first quarter. In the space view the Moon is at a right angle: the Sun-Earth-Moon angle is 90°. In the sky view, exactly the right half is bright.
Drag the Moon round and watch: at 0° the lit half points away and the sky view is black; at 45° a crescent about 15% lit; at 135° a gibbous about 85%; at 180° a full disc.
Two things are worth checking as you drag. First, the Moon-ball is always exactly half bright in the space view — that never changes. Second, the terminator, the line between the bright and dark parts, is always a half-circle seen at an angle, which is why it looks straight at the quarters and curved everywhere else.
Eight quiz rounds then ask you to name a phase from the sky view, or to place the Moon in the space view given a phase name.
Chapter 03
Where in the sky, and at what time
Elongation tells you the shape. It also tells you where the Moon is in the sky, because elongation is literally the angle between the Sun and the Moon.
The sky turns 360° in 24 hours, which is 15° every hour. So if the Moon is 15° east of the Sun, it crosses the sky exactly one hour behind the Sun. If it is 90° east, it is four hours behind. If it is 180° away, it is twelve hours behind — which is why a full moon rises as the Sun sets.
That gives a rule you can do in your head:
Hours behind the Sun = elongation ÷ 15.
A waxing crescent at 45° elongation is 3 hours behind the Sun: it rises about 3 hours after sunrise, is highest about 3 hours after noon, and sets about 3 hours after sunset. That is exactly why a young crescent is an early-evening object that disappears before your bedtime.
| Phase | Elongation | Rises | Highest | Sets |
|---|---|---|---|---|
| New moon | 0° | 06:00 | 12:00 | 18:00 |
| Waxing crescent | 45° | 09:00 | 15:00 | 21:00 |
| First quarter | 90° | 12:00 | 18:00 | 00:00 |
| Waxing gibbous | 135° | 15:00 | 21:00 | 03:00 |
| Full moon | 180° | 18:00 | 00:00 | 06:00 |
| Waning gibbous | 225° | 21:00 | 03:00 | 09:00 |
| Last quarter | 270° | 00:00 | 06:00 | 12:00 |
| Waning crescent | 315° | 03:00 | 09:00 | 15:00 |
Worked example
0 / 6 steps shownWhat time does a waxing gibbous rise?
A Moon is a waxing gibbous at an elongation of 135°. Roughly what time does it rise, and is it a good target for a 9 pm look from a terrace?
Lab
Decide when each phase is best placed for observing, using its elongation and the 15-degrees-per-hour rule.
Sort each Moon sighting by the time of day when it is easiest to see.
12 cards, 3 bins. Tap a card, then tap its bin. You can also drag, or press a bin’s number key.
Text version of this activity
Twelve sightings are sorted into three bins: best in the evening, best around midnight, best in the morning.
Evening: waxing crescent at 45°, first quarter at 90°, waxing gibbous at 135°, and the young Eid crescent — all of them Moons that are less than twelve hours behind the Sun.
Around midnight: full moon at 180°, waning gibbous at 225°, a Moon highest at 3 am, and Karva Chauth's Moon at about 222°.
Morning: last quarter at 270°, waning crescent at 315°, the old crescent before Amavasya, and a Moon high in the south at sunrise.
The rule underneath every card: hours behind the Sun = elongation ÷ 15. Small elongation means the Moon trails the Sun closely and is an evening object; large elongation means it trails by most of a day and is a morning object.
Try it
Chapter 04
Which way up? Waxing and waning revisited
In Discover you learned that from India a waxing Moon is bright on the right. Here is why — and why it is not true everywhere.
The Moon is always lit from the side the Sun is on. In the northern hemisphere, when you face the Moon in the evening, the Sun has just set to your right-hand side (to the west), so the bright edge faces right. Later in the month, when the Moon trails the Sun by more than half a day, you see it in the morning with the Sun rising on your left, and the bright edge faces left.
Three consequences, all worth knowing:
- In the southern hemisphere it is the other way round. In Australia, a waxing crescent is bright on the left, and the D-O-C trick becomes C-O-D. Same Moon, same phase, upside-down view.
- Near the equator the crescent lies on its back. From Kerala or Tamil Nadu, a young crescent often looks like a smile or a boat rather than a letter D, because the Sun sets almost straight down and the lit edge ends up along the bottom.
- The bright edge always points at the Sun. This is the single reliable rule for every place on Earth. Draw a line from the middle of the dark side through the middle of the bright side, keep going, and you are pointing at the Sun — even when the Sun is below the horizon.
| Phase | From Delhi (28°N) | From Kochi (10°N) | From Melbourne (38°S) |
|---|---|---|---|
| Waxing crescent | Bright edge on the right, tipped like a D | Horns pointing up: a bowl or boat | Bright edge on the left, like a C |
| First quarter | Right half bright, straight edge vertical | Bright half low, terminator tipped | Left half bright |
| Full moon | A full disc; the familiar 'rabbit' upright | A full disc, rabbit tilted | A full disc, rabbit upside down |
| Waning crescent | Bright edge on the left, like a C | Horns pointing up in the dawn sky | Bright edge on the right, like a D |
Try it
Chapter 05
The terminator, and where the craters hide
The curved line dividing the bright part of the Moon from the dark part has a name: the terminator. It is the Moon's sunrise-and-sunset line.
Along the terminator, the Sun is just on the horizon as seen from the lunar ground. That means shadows there are enormously long — the same way your own shadow stretches down the whole street at sunset. Every crater rim, every mountain, every ridge throws a black streak across the surface.
Move away from the terminator towards the middle of the bright part and the Sun climbs higher in the lunar sky. Shadows shorten. At full moon the Sun is almost directly overhead across the whole visible face, and there are hardly any shadows at all.
Which leads to an unexpected rule for anyone with binoculars:
The full moon is the worst night of the month to look at the Moon.
It is dazzlingly bright and almost completely flat, like a photograph taken with the flash on. The best views are around first quarter and last quarter, when the terminator runs straight down the middle of the disc and the craters along it stand out in three dimensions.
How to hunt craters with cheap binoculars
- Step 01Pick the right nightquarter moon
Look within two or three nights of first or last quarter. The terminator then runs down the middle of the disc, giving maximum shadow.
- Step 02Steady the binocularselbows down
Rest your elbows on a wall or a windowsill, or lie back on a chair. Unsteady hands blur far more detail than cheap optics do.
- Step 03Find the terminatorthe ragged edge
Look for the boundary between bright and dark. At a quarter Moon it looks visibly rough and bitten, not smooth — those bites are crater rims catching the low Sun.
- Step 04Look for black ovalslong shadows
Craters near the terminator show a bright rim on the sunward side and a long black shadow pooled inside. Watch the same crater on the next night and the shadow will have shrunk.
- Step 05Find the dark seasmaria
The large smooth grey patches are maria, ancient lava plains. They have fewer craters because the lava flooded the old ones.
- Step 06Come back at full mooncompare
Look at the same region at full moon and notice that the craters have almost vanished, while bright streaks called rays now dominate. Same rocks, different lighting.
Chapter 06
Earthshine: the old Moon in the new Moon's arms
Find a crescent Moon three or four days after new moon, on a clear evening, once the sky has properly darkened. Look at the part that should be black.
It is not black. There is a faint, ghostly grey glow filling the whole unlit disc, so that you can see the Moon's complete round outline with a bright crescent stuck on one edge. Sailors and poets called it the old Moon in the new Moon's arms.
The explanation is lovely, and it is the same idea as the whole lesson, run one step further.
You are looking at the Moon's night side. There is no sunlight there. But there is light: light from Earth. At that moment, an astronaut standing on that dark lunar ground would look up and see a huge, brilliant, nearly full Earth in the sky — four times wider than the Moon looks to us and dozens of times brighter, because Earth's clouds and oceans reflect far more sunlight than grey Moon rock.
That Earthlight falls on the lunar night side, bounces off, and comes back to your eye. It has made a round trip: Sun → Earth → Moon → you.
Chapter 07
Why we always see the same face
Look at the full moon and you will see dark patches that people all over the world have turned into pictures: a rabbit, a man's face, a woman carrying a bundle of sticks, a buffalo.
Now here is the strange part. Your grandparents saw exactly the same patches. So did everyone who has ever lived. The Moon keeps one face permanently turned towards Earth. The other half has never been visible from the ground, from anywhere, at any time in human history.
The usual guess is that the Moon does not spin. That guess is wrong, and the truth is more interesting: the Moon spins exactly once for every orbit it makes. One rotation takes 27.32 days; one orbit takes 27.32 days. The two are locked together, which is why the same side always points our way.
This is called synchronous rotation, or tidal locking, and it is not a coincidence. Earth's gravity pulls slightly harder on the near side of the Moon than on the far side, which stretches it very slightly into a non-spherical shape. Over billions of years, the friction of that stretching acted like a brake on the Moon's spin, slowing it until it settled into the one rate where the stretch stops fighting the rotation: exactly once per orbit.
Helps you understand
TidesThe same tidal stretching that raises the oceans on Earth is what slowed the Moon's spin until it matched its orbit. Tides and tidal locking are the same physics.
Predict first
Chapter 08
Four mix-ups worth clearing up
Try it
Chapter 09
The vocabulary, gathered
Words to know
All maths vocabulary →The words you now own
- Elongation
- The angle at Earth between the direction of the Sun and the direction of the Moon. It sets the phase completely.
- Example: Elongation 90° means a quarter moon, half the disc lit.
- Lit fraction
- The share of the Moon's visible disc that is sunlit, from 0 at new moon to 1 at full moon.
- Example: At 45° elongation the lit fraction is about 0.15.
- Synodic month
- New moon to new moon: 29.53 days. The cycle of the phases.
- Example: 29 days, 12 hours, 44 minutes.
- Sidereal month
- One orbit measured against the distant stars: 27.32 days. Shorter than the synodic month.
- Example: Also the Moon's rotation period, which is why we see one face.
- Terminator
- The sunrise-sunset line on a world: the boundary between its lit and unlit halves.
- Example: Craters show best along the Moon's terminator.
- Maria
- The large dark smooth plains on the Moon, made of ancient hardened lava. Latin for 'seas'.
- Example: The rabbit and the man in the Moon are patterns of maria.
- Highlands
- The pale, heavily cratered older regions of the Moon, standing above the maria.
- Example: Brighter because the rock is more reflective.
- Earthshine
- Faint light on the Moon's night side, reflected from Earth.
- Example: 'The old Moon in the new Moon's arms', best seen near a crescent.
- Synchronous rotation
- Spinning exactly once per orbit, so the same face always points at the partner body.
- Example: The Moon spins once every 27.32 days and orbits in 27.32 days.
- Tidal locking
- The process by which gravity's uneven pull slowly brakes a moon's spin until it becomes synchronous.
- Example: It is why the Moon keeps one face towards Earth.
- Far side
- The hemisphere of the Moon permanently turned away from Earth. Not the same as the dark side.
- Example: First photographed by Luna 3 in October 1959.
- Near side
- The hemisphere permanently facing Earth, dominated by dark maria.
- Example: Every crater you can see from the ground is on the near side.
- Waxing
- Growing brighter night by night, from new moon to full moon.
- Example: Shukla paksha, the bright fortnight.
- Waning
- Shrinking night by night, from full moon to new moon.
- Example: Krishna paksha, the dark fortnight.
- Lunar eclipse
- Earth's shadow genuinely falling on the Moon. Only possible at full moon, and rare.
- Example: Quite different from a phase.
Lab
See why the shadow explanation of phases fails, by finding how rarely the three bodies really line up.
34,171 km off the plane is 2.7 whole Earths' worth of miss. The shadow sails harmlessly over the top (or under the bottom) of us. Only within about 17° of a node is the line-up good enough — which happens in two short "eclipse seasons" a year, not every month.
The Moon's orbit is tilted 5.1° against the flat plane Earth goes round the Sun in. Two tilted circles can only cross at two points, and those two points are called the nodes. An eclipse needs a new or full moon to land almost exactly on a node.
Sizes on the picture: the Sun is 6,96,000 km in radius and 150 million km away, the Moon 1,737 km and about 3,84,400 km away. Their apparent sizes agree to within a few per cent — 0.52° against 0.53° — which is a coincidence, and the reason total solar eclipses exist at all.
Text version of this activity
This lab shows the Sun, Earth and Moon from the side, with Earth's shadow drawn as a long dark cone stretching away from the Sun, and the Moon's orbit drawn as a ring tilted at 5.1° to Earth's orbit around the Sun.
Step the Moon through a month and watch the shadow cone. At most full moons the Moon passes above or below the cone, missing it completely — often by several times the Moon's own width. Only when the Moon happens to be crossing the flat plane of Earth's orbit at the same moment as full moon does it slide into the shadow, and an eclipse happens.
Set the tilt slider to 0° and everything changes: now the Moon crosses the shadow at every single full moon, and passes exactly in front of the Sun at every new moon. You would get a lunar eclipse and a solar eclipse every month.
The 5.1° tilt is the reason eclipses are special, and it is also a second proof that phases are not shadows: if phases were caused by the shadow, they would stop happening whenever the Moon misses the cone — which is most months.
Helps you understand
EclipsesKnowing the phase tells you when an eclipse is even possible: solar eclipses only at new moon, lunar eclipses only at full moon.
Helps you understand
LightEvery phase is a story about light travelling in straight lines and bouncing off a rough grey surface.
Reflect
This stays on this page only. It isn’t saved or sent anywhere.
Quick check
Check yourself
10 questions · answer what you can, then check. Getting one wrong is useful.
Keep this
Cheat sheet
- Elongation is the Sun-Earth-Moon angle, and it sets everything: 0° new, 90° quarter, 180° full.
- elongation = 360 x day ÷ 29.53, and lit fraction = (1 − cos e) ÷ 2.
- Lit fraction is not proportional to angle. 45° gives only about 15%; the Moon fattens slowly, then quickly, then slowly again.
- hours behind the Sun = elongation ÷ 15, because the sky turns 15° every hour.
- Full moon rises at sunset, first quarter is high in the south at sunset, last quarter is high in the south at sunrise.
- Moonrise slips about 49 minutes later each day, because the Moon gains 12.19° of elongation daily.
- The bright edge always points at the Sun — the one orientation rule that works at every latitude.
- Left/right flips in the southern hemisphere; near the equator the crescent lies on its back like a boat.
- The terminator is the Moon's sunrise line. Craters show best along it, which is why quarter moons beat full moons in binoculars.
- Earthshine is sunlight bounced off Earth onto the Moon's night side: Sun → Earth → Moon → you.
- The Moon spins once per orbit (27.32 days), which is why one face always points at us. That is tidal locking, not a lack of rotation.
- Far side is not dark side. At new moon the far side is in full sunlight and the near side is in night.
- Everyone on Earth sees the same phase at the same moment; only the orientation and the clock differ.
- Phases are a viewing angle. Eclipses are a shadow. Do not mix them up.
Where this comes from
Sources
Moon Phases (opens another website) — NASA Scienceawaiting check
Supports the eight named phases in order, phases being caused by the changing view of the Sun-lit half rather than by Earth's shadow, the 29.5-day cycle, waxing and waning, and the fact that half the Moon is always lit.
Moon Facts: Earth's Natural Satellite (opens another website) — NASA Scienceawaiting check
Supports the Moon's diameter of about 3,475 km, its mean distance of about 384,400 km, synchronous rotation (the same face always turned to Earth), and the 27.3-day sidereal period.
Lunar phase (opens another website) — Wikipediaawaiting check
Supports the illuminated-fraction formula, the synodic month of 29.53 days versus the sidereal month of 27.32 days, phase rise and set times, earthshine and the terminator.
Tidal locking (opens another website) — Wikipediaawaiting check
Supports synchronous rotation, how tidal friction slowed the Moon's spin until it matched its orbit, and the link between the same-face effect and the Moon's slow recession.
Moon: Earth's natural satellite (opens another website) — Encyclopaedia Britannicaawaiting check
Supports general lunar description: maria and highlands, cratering, the difference between near side and far side, and the Moon's albedo and brightness.
Moon Phase and Libration visualisations (opens another website) — NASA Scientific Visualization Studioawaiting check
Supports libration in longitude and latitude, the resulting visibility of about 59% of the lunar surface over time, and the hour-by-hour appearance of the Moon through a month.
Moon phases and moonrise times for New Delhi (opens another website) — timeanddate.comawaiting check
Supports checking real moonrise, moonset and phase times for Indian cities, used for the moon diary and the Karva Chauth moonrise prediction exercise.
End of Understand
What you just read
- Define elongation and use it to work out the phase, the lit fraction and the rise and set times.
- Explain why the lit fraction grows unevenly through the month.
- Use the 15-degrees-per-hour rule to predict when a given phase is above the horizon.
- Explain the terminator, earthshine and why a full moon looks flat in binoculars.
- Explain synchronous rotation and distinguish the far side from the night side.
- Next depthGo deeper: InvestigateChange conditions, predict, compare evidence and test.
- Practise75 questionsHints and a worked solution for every question — or play a 10-question round.
- Step backDiscoverGo back over the ground before this one — you can move up and down as often as you like.
- TopicAll of phases of the moonThe whole ladder, the connections and the words to know, on one page.
The web
Explore a connection
Builds onanother area
LightThe Moon has no light of its own: we see the half of it the Sun is lighting.
Builds onanother area
GravityGravity is what keeps the Moon in the orbit that produces the monthly cycle of phases.
Helps you understand
EclipsesEclipses can only happen at new moon or full moon — the two phases where the three bodies line up.
Want to save topics or ask for new ones? Invited families can connect a learning device. Everything here stays free to read without signing in.
Revision 1 · release preview-7e1cbbcc4f · accepted 20/09/2026