kaleidoscopedoodle

WHAT THE PHYSICS SAYS

Nature's own
kaleidoscope.

A snow crystal repeats one pattern six times.

Check a cloud
A single six-armed snow crystal resting on dark blue wool, magnified so every branch is sharp
AI-generated image, not a photograph of a real person or place.

SIX ARMSone journey

  • Hexagons from the start
  • Same path, same arms
  • Temperature sets the shape
  • Order and chaos in every flake

No blueprint tells it to. The six-fold shape comes from how water molecules line up in ice, and the matching arms come from a shared journey through the cloud, where every change in temperature and humidity reaches all six arms at once.

Updated

THE SHORT ANSWER

Six from the molecules,
symmetry from the sky.

Two separate questions with two answers:
why six, and why the arms match.

WHY SIX

Hexagons all the way down

In a snow crystal the water molecules sit in a precise hexagonal array. Crystals start as tiny six-sided prisms, and arms sprout from the six corners.

How it grows

WHY THEY MATCH

One path through the cloud

The arms do not communicate. They match because all six took the same path and met the same changes at the same times.

Check a cloud

PAPER SNOWFLAKES

An old craft with real roots

An 1864 snowflake album was made by cutting paper copies of crystals as they landed on a windowsill, a craft now practised by millions of schoolchildren.

See the numbers

A QUICK CLOUD CHECK

What grows at
this temperature?

Pick the conditions in the cloud to see which snow crystals tend to form there. The bar shows how likely you are to find the classic large six-armed star.

Based on the snow crystal morphology diagram as explained by SnowCrystals.com. These are temperatures in the cloud; it is often much warmer on the ground.

Cloud check

Choose the cloud conditions
Near −2 °CSmall thin plates

Plate-like crystals grow here, but they are smaller and prone to melting because the temperature is so close to freezing point.

Near −6 °CColumns and needles

Slender columns and needles grow best around this temperature. A column carried into colder air can grow plates on its ends, making a capped column.

Near −15 °CLarge stellar plates

The largest, most photogenic stellar crystals only grow in a narrow range around −15 °C, especially when the air is humid.

Colder stillPlates or columns

At lower temperatures either plates or columns can be found.

Any temperature, dry airSimple prisms

Low humidity means slow growth and simple hexagonal prisms. Branched, ornate forms need high humidity and rapid growth.

Source: SnowCrystals.com, Guide to Snowflakes and Snowflake Science (snow crystal morphology diagram, first worked out in a cold laboratory in the 1930s).

TWO NUMBERS WORTH KNOWING

Small crystals,
rare in Britain.

One figure on how big a single crystal gets,
one on how often snow settles in the UK.

10 mm

Largest snow crystal ever photographed

It measured 10 mm (0.4 inches) from tip to tip. The smallest crystals, called diamond dust, can be as small as the diameter of a human hair.

SIZE · SNOWCRYSTALS.COM

13 days

Days of lying snow a year, UK average

The UK averages 13.0 days of lying snow a year (1991 to 2020). Scotland sees the most, with 23.0 days on average.

UK SNOW · MET OFFICE

Perfectly symmetrical crystals are the exception. SnowCrystals.com notes that irregular crystals are by far the most common type; near-perfect ones are sought after by photographers but not common.

Hands holding small scissors and a folded square of white paper, with finished paper snowflakes on a wooden table
AI-generated image, not a photograph of a real person or place.

FOUR WAYS TO SEE IT

Catch a crystal
before it melts.

You do not need a lab. These tips follow from what the snow crystal research and the Met Office say about how snow forms and falls.

  1. Pick a cold, dry snowfall

    Near 0 °C flakes melt at the edges and clump into big wet flakes. Cold, dry air gives small, powdery flakes that do not stick together.

  2. Hope for real cold

    Large plate-like crystals are most likely when it is cold, near −15 °C. Plates near −2 °C are smaller and melt easily.

  3. Look for the hexagon

    The simplest crystals are six-sided prisms: thin flat plates, slender columns or anything in between.

  4. Expect imperfection

    Most crystals are irregular. Finding a near-perfect star is a lucky catch, not the norm.

FROM VAPOUR TO STAR

No blueprint,
just growth.

A snow crystal forms when water vapour turns straight into ice without becoming liquid first. Faceting builds flat, orderly faces, while branching sends arms and side-branches out into the air.

The Met Office explains that snowflakes, as most people know them, are often many crystals stuck together, and that the heaviest UK snowfalls tend to come when the air is between 0 and 2 °C.

Snow falling softly over a quiet village lane with stone walls and bare trees on a grey winter afternoon
AI-generated image, not a photograph of a real person or place.

Questions

Questions people ask

Why do snowflakes have six sides?

Because of the way water molecules arrange themselves in ice. In a snow crystal they sit in a precise hexagonal array, so the crystal starts as a six-sided prism and its arms grow from the six corners.

Is it true that no two snowflakes are alike?

Each crystal's final shape depends on its exact path through the clouds, and no two follow exactly the same path, so no two look exactly alike. In a lab, crystals grown side by side under the same conditions have come out nearly, but not precisely, identical.

How do the six arms know to grow the same way?

They do not. Each arm grows independently, but all six meet the same changes in temperature and humidity at the same time, so they change in step.

What is the difference between a snowflake and a snow crystal?

A snow crystal is a single crystal of ice. A snowflake can mean one crystal or a clump of hundreds or thousands of crystals that collided and stuck together as they fell.

Does it have to be below 0 °C to snow?

No. The Met Office says precipitation falls as snow when the air is below 2 °C, and that the heaviest UK snowfalls tend to happen between 0 and 2 °C.

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