Its immense length of 625 miles takes the Loire through ten
departments, but the changes of scenery are not so remarkable as those
of the Rhone. The source is in the Cevennes, about 4500 feet above
sea-level, on the east side of the Gerbier de Jonc, and almost in
sight of the Rhone. Through Haute Loire in the marvellously
picturesque region of dead volcanoes near Le Puy-en-Velay it takes its
course northwards, flowing at the foot of basaltic cliffs and
chestnut-clad slopes. On commanding spurs ruined castles are perched
in most romantic fashion, and if it were not for their painful
inaccessibility, the demand among the wealthy for these little
strongholds of the Middle Ages would run up their value to astonishing
figures.
The action of water in the past has been vastly more energetic in the
Auvergnes and the Cevennes in the ages since their masses of plutonic
rock were produced than at the present day, for the scoria and the
general debris of seismic disturbance has been so much eroded that the
throats of volcanoes filled with the last product of the immense heat
below here and there stand out stripped of their cones. One of the
most remarkable of these phenomena is to be seen at Le Puy. This
strange _aiguille_ has been crowned with a beautiful Romanesque chapel
for some nine centuries, and it is just possible that a Roman temple
stood there at an earlier date.
In the neighbourhood of St. Etienne the Loire is considered to be
navigable. It traverses the alluvial plain of Forez, the mountains of
that name to the west separating it from the basin of its great
tributary the Allier, which takes a roughly parallel course and joins
it just below Nevers. If rivers could express their feeling by other
means than overproduction and strikes, the Allier would no doubt say
something forcible as to the ascendency of its neighbour, whose claims
to be the parent stream are open to question.
Public-domain text, read in full here on John Shaqi.
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