| Have you ever wondered what happens
to slate if it is suddenly heated to very high temperatures? At the
solar furnace of Font-Romeu in the eastern Pyrenees of France, I
discovered it doesn't shatter or explode, but simply melts into a black,
obsidian-like glass. Which is not surprising, really, considering its
sedimentary origins before metamorphosis.
There is only a small exhibition hall here, below the 8-storey-high
furnace, but live demonstrations of high-temperature solar energy
effects are held nearby at the smaller experimental furnace of
Mont-Louis. This parabolic mirror is only about 20 feet in diameter, but
by focusing the mid-day sun, it can melt a 3-inch hole in a sheet of
steel in less than a minute, as well as melting roofing slates.

The eastern French Pyrenees are mostly mica schist, but inland
there are large granite formations, and pink marble is still quarried
for architectural purposes. Vast quantities of iron ore were extracted
here until the 1950s, not by open-cast methods but by tunnelling. The
village of Arles-sur-Tech has a small "Museum of Iron" but their mineral
specimens are deteriorating and sadly neglected.
This is in sharp contrast to an excellent museum of minerals and fossils
at Vernet-les-Bains, which is beautifully displayed by its founder and
curator, who collected most of the specimens himself.
The Mediterranean coastal sand here is surprisingly coarse, unlike the
sands at the western end of the Pyrenees which have been ground fine by
the more vigorous breakers of the Atlantic.
Inland, around Isle-sur-Tet a plain of sands and gravels came from a
mountain range, which aeons ago lay to the north of the present
Pyrenees. At Les Orgues the scarce rainfall has weathered this into
striking "Badlands" formations.

Perhaps WEGA could arrange a field trip to this fascinatingly
varied region.
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