The History of the Decline and Fall of the Roman Empire - Edward Gibbon [176]
These three were the principal races which inhabited Germany; they moved from east to west, and are the parent stem of the modern natives. But northern Europe, according to Schlozer, was not peopled by them alone; other races, of different origin, and speaking different languages, have inhabited and left descendants in these countries.
The German tribes called themselves, from very remote times, by the generic name of Teutons, (Teuten, Deutschen,) which Tacitus derives from that of one of their gods, Tuisco. It appears more probable that it means merely men, people. Many savage nations have given themselves no other name. Thus the Laplanders call themselves Almag, people; the Samoiedes Nilletz, Nissetsch, men, &c. As to the name of Germans, (Germani,) Caesar found it in use in Gaul, and adopted it as a word already known to the Romans. Many of the learned (from a passage of Tacitus, de Mor Germ. c. 2) have supposed that it was only applied to the Teutons after Caesar's time; but Adelung has triumphantly refuted this opinion. The name of Germans is found in the Fasti Capitolini. See Gruter, Iscrip. 2899, in which the consul Marcellus, in the year of Rome 531, is said to have defeated the Gauls, the Insubrians, and the Germans, commanded by Virdomar. See Adelung, Aelt. Geschichte der Deutsch, p. 102. - Compressed from G.]
[Footnote 1: The modern philosophers of Sweden seem agreed that the waters of the Baltic gradually sink in a regular proportion, which they have ventured to estimate at half an inch every year. Twenty centuries ago the flat country of Scandinavia must have been covered by the sea; while the high lands rose above the waters, as so many islands of various forms and dimensions. Such, indeed, is the notion given us by Mela, Pliny, and Tacitus, of the vast countries round the Baltic. See in the Bibliotheque Raisonnee, tom. xl. and xlv. a large abstract of Dalin's History of Sweden, composed in the Swedish language.
Note: Modern geologists have rejected this theory of the depression of the Baltic, as inconsistent with recent observation. The considerable changes which have taken place on its shores, Mr. Lyell, from actual observation now decidedly attributes to the regular and uniform elevation of the land. - Lyell's Geology, b. ii. c. 17 - M.]
Some ingenious writers ^2 have suspected that Europe was much colder formerly than it is at present; and the most ancient descriptions of the climate of Germany tend exceedingly to confirm their theory. The general complaints of intense frost and eternal winter, are perhaps little