The Life of Sir Humphry Davy, Bart. LL.D., Volume 2 (of 2)Paris, John Ayrton
History
The Life of Sir Humphry Davy, Bart. LL.D., Volume 2 (of 2)
Paris, John Ayrton
Chemists -- England -- Biography; Davy, Humphry, Sir, 1778-1829
"It is amongst extinct volcanoes, the surfaces of which have been
removed by the action of air and water, and in which the interior
parts of strata of lavas are exposed, that the most instructive
examples of the operation of slow cooling upon heated masses are to
be found. It is difficult to conceive that water could have been
the solvent of the different granitic and porphyritic formations;
for, in that case, some combinations of water with the pure earths
ought to be found in them. Quartz ought to exist in a state of
_hydrate_, and Wavellite, not Corundum, ought to be the state of
alumina in granite.
"To suppose the primary rocks, in general, to have been produced
by the slow cooling of a mass formed by the combustion of the
metallic bases of the earths, appears to me the most reasonable
hypothesis; yet aqueous agency must not be entirely excluded from
our geological views. In many cases of crystallization, even in
volcanic countries, this cause operates; thus in Ischia, siliceous
_tufas_ are formed from hot springs; and in the lake Albula, or
the lake of Solfaterra, near Tivoli, crystals of calcareous spar
and of sulphur separate from water impregnated with carbonic acid
and hepatic gas; and large strata of calcareous rocks, formed
evidently in late times by water impregnated with carbonic acid,
exist in various parts of Europe. The Travertine marble (_Marmor
Tiburtinum_) is a production of this kind; and it is of this
species of stone that the Colosseum at Rome, and the cathedral of
St. Peter, are built. It is likewise employed in the ancient temple
of Pæstum, and it rivals in durability, if not in beauty, the
primary marble of Paris and Carrara."
CHAPTER XII.
Sir Humphry Davy suggests a chemical method for unrolling
the ancient Papyri.--He is encouraged by the Government
to proceed to Naples for that purpose.--He embarks at
Dover.--His experiments on the Rhine, the Danube, the Raab,
the Save, the Ironzo, the Po, and the Tiber, in order to
explain the formation of mists on rivers and lakes.--His
arrival and reception at Naples.--He visits the excavations
at Herculaneum.--He concludes that it was overwhelmed by
sand and ashes, but had never been exposed to burning
matter.--He commences his attempt of unrolling the Papyri.--His
failure.--He complains of the persons at the head of the
department in the Museum.--He analyses the waters of the
Baths of Lucca.--His return to England.--Death of Sir Joseph
Banks.--He is elected President of the Royal Society.--Some
remarks on that event.--He visits Penzance.--Is honoured by
a public dinner.--Electro-magnetic discoveries of Oersted
extended by Davy.--He examines Electrical Phenomena in
vacuo.--The results of his experiments questioned.--He enquires
into the state of the water, and aëriform matter in the
cavities of crystals.--The interesting results of his enquiry
confirm the views of the Plutonists.
Public-domain text, read in full here on John Shaqi.
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