# Why does molten sand cool to form glass and not return to it's original yellow form?

I came across this website on the internet: http://www.explainthatstuff.com/glass.html. In this website, it is said that

When molten sand cools, it doesn't turn back into the gritty yellow stuff you started out with: it undergoes a complete transformation and gains an entirely different inner structure. But it doesn't matter how much you cool the sand, it never quite sets into a solid.

I asked myself, why is this so? Molten iron cools to form iron, back to how it was made. Same for many other materials, even plastics. However, the same does not apply to sand. Why doesn't molten sand cool to form the yellow, opaque sand it came from, but forms a transparent amorphous solid called glass?

Suppose you take iron filings, melt them, then let them solidify to a solid block of iron. This is obviously different to what you started with. Not chemically different but physically different.

The same is true of sand and glass. Sand is basically glass filings i.e. glass that the geological processes of erosion have broken down to a powder. When you melt then cool it the glass forms a solid block. Leave the block outside for a few million years and erosion will grind it back down to sand.

I suspect the bit about it never quite sets into a solid is referring to the myth that glass is a supercooled liquid. It is not. Glass is a solid like iron, however unlike iron it is an amorphous solid.

There is one last point to mention. Glass is silicon dioxide, $\mathrm{SiO}_2$, and silicon dioxide has both amorphous and crystalline forms. One common crystalline form is the mineral quartz, and some sand will be quartz not the glassy form - I confess I have no idea what percentage of sandy beaches are covered in quartz. In this case you would be melting the crystalline form, quartz, and cooling it to the amorphous form, glass, so there is a structural change in that sense. It is possible to cool molten silicon dioxide back to a crsytalline form but you have to cool it exceeding slowly as quartz crystals grow only very slowly from the melt.

A quick footnote: Pieter says in a comment that all (most?) sand is crystalline, and I'm happy to accept this as geology is not one of my strong points.

Another footnote following the edit to the question: it looks as if you are asking why cooling molten silicon dioxide forms an amorphous solid not a crystalline solid. This is addressed in the question Why do some things crystallize? (And others don't, for that matter.)

• The part you said about millions of years seems contradictory to what I've read up. I have read then even after millions of years, the piece of glass would have barely broken down. Furthermore, I we were to watch this process, then how? We see a transparent piece of glass disintegrating to tiny yellow grains! This doesn't seem possible. On what you said about iron fillings, I don't really understand your parallel drawn here. Iron fillings are bits of iron, but can you say the same for glass? Thanks for your answer anyways :) – QuIcKmAtHs Dec 30 '17 at 12:01
• Sand is quartz and crystalline. Except for lightning-strike channels, fulgurites. – Pieter Dec 30 '17 at 12:02
• @XcoderX where do you suppose the sand came from in the first place? Have you Googled formation of sand? It arises from weathering of rocks. – John Rennie Dec 30 '17 at 12:12
• Exactly my point. Why doesn't molten sand cool to rocks? – QuIcKmAtHs Dec 30 '17 at 12:15
• @XcoderX You're getting into geological territory here, which is far from my comfort zone, but I believe quartz is formed by crystallisation from silicic acid solution in superheated water deep in the Earth's crust, not from a melt. It is subsequently exposed by tectonic movements and erosion, then ground down to sand by erosion. If you melted the sand then cooled it very slowly it would reform a block of quartz. – John Rennie Dec 30 '17 at 12:20

sand consists of tiny fragments of quartz, mica, and feldspar. each grain of this mixture has sharp facets on its surface which reflect light. in the case of mica and quartz, the grains are transparent or nearly so, and refraction also occurs when light strikes those grains.

sand looks as it does because that refraction and reflection process randomly scatters incident light of all colors, making the sand look uniformly whitish. when you melt sand, all those tiny reflective and refractive interfaces between the air and the material comprising the grains disappear and you are eventually left with a big block of stuff that is semitransparent, and where the only reflection and refraction processes occur at the now-macroscopic interface between the lump and the air surrounding it.

If you then took that lump and began crushing it with a hammer into finer and finer fragments, eventually the pieces would stop looking transparent and begin looking white instead.

You can see the effect yourself by dropping a clear glass bottle on the pavement so it shatters. the tiniest sand-like fragments turn white while the larger pieces do not.