Narrative of the Circumnavigation of the Globe by the Austrian Frigate Novara, Volume I: (Commodore B. Von Wullerstorf-Urbair,) Undertaken by Order of the Imperial Government in the Years 1857, 1858, & 1859, Under the Immediate Auspices of His I. and R. Highness the Archduke Ferdinand Maximilian, Commander-In-Chief of the; Austrian Navy.Scherzer, Karl, Ritter von
History
Narrative of the Circumnavigation of the Globe by the Austrian Frigate Novara, Volume I: (Commodore B. Von Wullerstorf-Urbair,) Undertaken by Order of the Imperial Government in the Years 1857, 1858, & 1859, Under the Immediate Auspices of His I. and R. Highness the Archduke Ferdinand Maximilian, Commander-In-Chief of the; Austrian Navy.
Scherzer, Karl, Ritter von
Novara Expedition (1857-1859); Voyages around the world -- History -- 19th century
The exhibition of comprehensive volcanic collections brings to light the
strong analogy subsisting between the trachytes belonging to volcanoes,
far distant from one another, while it indicates the existence of great
differences in the mineralogical composition of volcanoes situated very
near each other. My most excellent friend and fellow-traveller in Siberia,
Professor Gustavus Rose, recently subjected the trachytes of the Berlin
Museum, the greater number of which were collected by myself, to careful
crystallographical and chemical investigation. He found oligoclase and
pyroxene on the trachytes of Chimborazo, Popocatepetl, Colima,
Tunguragua, Puracé, Paramo de Ruiz, and the Peak of Teneriffe, which has
recently been accurately examined by Mr. Charles Deville. The trachytes of
Toluca, Orizaba, Gunung Barang, and Burung Agung, on the Island of Java,
Argæus, in Asia Minor, Cuneguilla, south of Sta. Fé de Nuevo-Mexico, the
Sièrra de San Francisco, west of the Rocky Mountains and Pueblo Zuni,
consist of hornblende, oligoclase, and brown mica. The trachytes of
Stromboli and Etna, those of the Siebengebirge (Drachenfels), and of Kara
Hissar in Phrygia, consist of large crystals of glassy felspar, with
numerous smaller crystals of oligoclase, some hornblende and mica.
Oligoclase, having been mistaken for albite, led to the fantastic idea of
a peculiar rock, the _Andesite_, prevailing in the Andes, and even led our
great master, Leopold von Buch, to make some curious distinctions,
(Déscription des Iles Canaries, 1836, pp. 186-87.)
To ascertain the average height above the level of the sea, I propose that
furrows should be cut in the rocks of the different regions along with
inscriptions, which might carry information to unborn ages, as has been
done, on my suggestion, now some 25 years ago, by the Academy of Science
at St. Petersburg, on the Caspian Sea, while Sir James Ross, in his
"Voyage of Discovery in the Southern and Antarctic Regions," 1839-43, Vol.
II. p. 23, regrets not having done so, or, at least, of having only once
adopted this plan.
Public-domain text, read in full here on John Shaqi.
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