The Old Red Sandstone; or, New Walks in an Old Field
John Stuart Mill · en
largely impregnated with the peculiar ingredients of the formation,
the famous medicinal springs of the Strath have their rise. They
contain, as shown by chemical analysis, the sulphates of soda, of
lime, of magnesia, common salt, and, above all, sulphuretted hydrogen
gas--elements which masses of sea-mud, charged with animal matter,
would yield as readily to the chemist as the medicinal springs of
Strathpeffer. Is it not a curious reflection, that the commercial
greatness of Britain, in the present day, should be closely connected
with the towering and thickly spread forests of arboraceous ferns and
gigantic reeds--vegetables of strange form and uncouth names--which
flourished and decayed on its surface, age after age, during the
vastly extended term of the carboniferous period, ere the mountains
were yet upheaved, and when there was as yet no man to till the
ground? Is it not a reflection equally curious, that the invalids of
the present summer should be drinking health, amid the recesses of
Strathpeffer, from the still more ancient mineral and animal debris
of the lower ocean of the Old Red Sandstone, strangely elaborated
for vast but unreckoned periods in the bowels of the earth? The fact
may remind us of one of the specifics of a now obsolete school of
medicine, which flourished in this country about two centuries ago,
and which included in its _materia medica_ portions of the human
frame. Among these was the flesh of Egyptian mummies, impregnated
with the embalming drugs--the dried muscles and sinews of human
creatures who had walked in the streets of Thebes or of Luxor three
thousand years ago.
[Footnote AV: "In the slaty schists of Seefeld, in the Tyrol,"
say Messrs. Sedgwick and Murchison, "there is such an abundance
of a similar bitumen, that it is largely extracted for medicinal
purposes."--(_Geol. Trans. for 1829_, p. 134.)]