EXPLAIN EXTENDED

This winter is anomalously warm in Europe, there is no snow and no New Year mood. So today we will be drawing a snowflake in PostgreSQL.

#1. A little theory

Core of a snowflake is six large symmetrical ice crystals growing from the common center. Out of these larger crystals other, smaller, crystals grow.

The overall shape of the snowflake is defined by how large do crystals grow and where exactly are they attached to each other.

These things are defined by fluctuations in air and temperature conditions around the snowflake. Because the flake itself is very small, in any given moment the conditions are nearly identical around each crystal, that's why the offspring crystals pop up in almost same places and grow to almost same lengths. Different flakes, though, constantly move to and from each other and are subject to very different fluctuations, and that's why they grow so unique.

Except for the root crystals (of which there are six), the child icicles grow in symmetrical pairs. More than that, each branch grows their own children (also in pairs), so on each step there are twice as many crystals, but they all share almost same length and angle. This gives the snowflake its symmetrical look.

So we can easily see that, despite the fact there may be many child crystals, the shape of a snowflake is defined by a relatively small number of parameters: how many children each crystal produces, where are they attached to it, at which angle they grow and to which length.

Now, let's try to model it.
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