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Snowflakes are known to form into pretty hexagonal structures. The image below shows a variety of such structures that are possible (although by all means not an exhaustive list):

enter image description here

What is the mechanism for snowflakes forming into these delightful symmetric hexagonal structures? Also what is the mechanism for the differing shapes in each of the different snow flakes?

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From wikipedia: "The initial symmetry can occur because the crystalline structure of ice is six-fold". What about this question is not already answered by the most obvious wikipedia page? – naught101 Apr 23 '14 at 5:31
@naught101, that portion of the article is brief and not really clear. Can you please elaborate on (a) why the crystalline structure ice is "six-fold" and what that means, and (b) how the crystalline structure give arise to the shape of the above crystals and why each crystal as a unique shape? The wikipedia article isn't really clear on these issues, but if you can interpret that page and post as an answer I will accept. – Geodude Apr 23 '14 at 5:35
a) b) I think that the paragraph I linked to is abundantly clear to anyone with a firm grasp of the English language and a junior highschool level of science education. Please re-read it, and specify which part of it is hard to understand. Responses like this really make you look incredibly lazy, if not wilfully ignorant. – naught101 Apr 23 '14 at 7:04
Note that such photos exhibit significant confirmation bias. Take 10,000 snowflake pictures and show the 12 that are most beautiful. Most snowflakes do not look as pretty as those. – gerrit Apr 23 '14 at 12:59
This is a terrific question, evidenced by the fact that the canonical explanation "the crystalline structure of ice is six-fold" does not address why refrigerator ice is not hexagonal. – dotancohen Apr 24 '14 at 6:21
up vote 30 down vote accepted

Ice grows in many forms. As mentioned in the other answer, all of the ice we are going to observe is Ice Ih, but there are many other forms. See this phase diagram of water:

Phase diagram of water
Image courtesy of Cmglee on wikipedia

The different ice regimes grow different crystalline shapes. Ice Ih grows hexagonal crystals and in certain regimes you can find triangular and cubic ice crystals. The hexagonal shape is a consequence of the bond angles within the water molecule as it forms into a solid crystal lattice.

This phase diagram says we'll experience Ice Ih between 0 C and -100 C and throughout tropospheric pressures. This ice crystal is hexagonal, but within this crystal form there are many ice habits of crystal growth.

ice habits
Image used from Weatherwise magazine, AMS

The axes of this plot are supersaturation with respect to ice ($e/e_{si} > 1$) and temperature. All of of these crystals are hexagonal but some are long skinny hexagonal prisms and some are very thin and wide hexagonal plates. The snowflake is a dendrite and these crystals grow between -10 and -22 C in and supersaturation with respect to liquid water.

What happens is that the hexagonal crystal has 6 vertices connecting its 6 edges. These vertices produce an increased gradient in vapor (indeed, the sharper the angle, the stronger the vapor gradient becomes). At high supersaturations vapor is quickly deposited in the areas of the enhanced vapor gradient and the arms of the dentrite form. The particular shape of the dendrite will depend strongly on the vapor gradient it is experiencing, which in turn is influenced strongly by its current shape and the environment it is growing in.


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H2O ice on Earth crystallizes with a structure called "Ice-Ih" which is hexagonal. The structure is dependent on the dipole properties of H2O-molecules. Similar to what water does with ions to bring them into solution, the crystal structure is dependent on the energetically favourable alignment of the dipoles. In Ice-Ih the most favourable alignment is a (more or less) plane hexagonal ring with the negative dipole (the oxygen) facing (more or less) inwards. Neighbouring rings in the same plane and rings in the above and below plane are held together by hydrogen bonds (the positive dipole the both hydrogens). (See

Snow flakes are all different, because crystal growth is very dynamic. While one crystal face grows another one can be susceptible to dissolution. While the snow flake is blown around through the air, temperature and humidity are always changing. This has the additional effect that sometimes crystal nucleation and sometimes crystal growth (which are energetically favourable at different temperatures) are active. While the snow flake descends the same dynamic continues. The crystal competes with liquid water and humidty for H2O-molecules. Even the crystal faces compete with each other leading to for example dissolution of molecules on the inside and crystallization on the outside. Because no snowflake experiences the same conditions in the same history, every one looks a little different (not surprising because actually there are also not two Zircon crystals that look alike, or two flowers that look alike, etc...).

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Is there any relationship between the fact that the angle between the 2 H-O bonds is 104.5 and the hexagonal symmetry in snowflakes? – Marco Apr 23 '14 at 11:21
@Marco There is, but I don't remember exactly why. – gerrit Apr 23 '14 at 13:01

To add to both Spießbürger's and casey's excellent answers, hydrogen bonds are the reason why some snowflakes are six-sided. His was alluded to, but I think it could use a bit more extrapolation.

Enter image description here

The image above shows an oxygen atom bonding with two hydrogen atoms (water). We can call these covalent bonds for our purposes, although hydrogen bonds tend, in some cases (and especially water) have special properties that make it unique from other covalent bonds. The result of this bond is a slightly negative charge near the oxygen atom and slightly positive near the hydrogens.

What happens next is that two water molecules will build up in a specific way, relating to their charge:

You see, as Spießbürger mentioned, the dipole of the water molecule allows the water molecules to build up in the shape pictured above, over and over and over. This happens naturally, since when water freezes, it forces the molecules to get closer together (but interestingly enough, the end result makes ice less dense than its liquid form). As these molecules build up, you start seeing a crystal lattice:

With each ring in the crystal lattice having six side. Each point is an oxygen atom. Each side is side is a hydrogen bonding with an oxygen. The snow flake, is just this bonding happening many many times.

So while it might not seem so obvious, we can explain the nature of the hexagonal structure with highschool/middle school level chemistry.

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This doesn't seem to answer the question. For example, graphite is also based on hexagonal structures at the atomic level but, at the macro level, graphite can be any shape. So why does the hexagonal arrangement at the molecular level of water cause snowflakes to be hexagonal at the macro level, when it doesn't cause ordinary water ice or graphite to be hexagonal at the macro level? – David Richerby Apr 24 '14 at 11:31

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