Another grouping on the basis of race stocks is frequently made beginning with the highest in culture, the Germanic; passing thence to the Romanic; concluding with the Slavonic, and the lands under the rule of the Turks, lowest in the scale, which are most closely connected with the Mongols of Asia. The Germanic, or Teutonic nations, include Great Britain; the German Empire; Austria-Hungary; Scandinavia (Norway, Sweden, Denmark); Holland, or the Netherlands; Switzerland, and Belgium. The Romanic nations include France; Italy; Spain; Portugal; Greece, and Roumania. The Slavonic nations, Russia in Europe; Servia, and Montenegro. The Turkish or Mongol nations, Turkey in Europe; Bulgaria.
For various reasons the first grouping is adopted in the pages following.
GREAT BRITAIN
The British Empire, Great Britain and England are often erroneously used in the popular mind for one and the same nation. In strict accuracy the British Empire consists of (1) The United Kingdom of Great Britain and Ireland; (2) India, and the British Colonies, Protectorates, and Dependencies. Great Britain proper includes only England, Scotland and Wales. What is really meant is the geographical group of the British Isles, including England, Scotland, Wales, Ireland and the adjacent islands. For here is the source of power and authority that holds together and controls this greatest of modern empires.
Geographical Features.—The British Isles belong distinctly to the mainland of Europe. If we imagine the sea level between England and Holland to fall sixty feet—the height of an ordinary house—the broad Dogger Bank, midway between England and Denmark, would begin to show its sands, and if a fall of two hundred feet took place one might walk dry shod across to the continent, to Belgium, Holland, or Denmark. From its shallows and banks, its stormy cross seas and frequent fogs, the navigation of the North Sea is dangerous; yet the traffic over it is enormous, for it is surrounded by countries, the inhabitants of which have been famous on the seas from the earliest times.
The great highways of commerce from it are Dover Strait, leading to the English Channel, in the south, and the stormy Pentland Firth, which separates Scotland from the Orkney Islands, in the north. The English Channel, though deeper than the North Sea, is also shallow; the enclosed Irish Sea, between England and Ireland, with St. George’s Channel and the North Channel leading out from it to the ocean, has been scoured deeper in its central lines; but there is a width of about fifty miles of shallow sea, or “soundings,” all round the islands, in the west, where they face the broad Atlantic.
Chief Islands and Divisions.—The main island of Great Britain, roughly triangular in shape, measures about six hundred miles in a straight line from its southwest corner, where the granite walls of Land’s End and the dark serpentine cliffs of the Lizard run out into the Atlantic, to the northern apex, the high red sandstone rocks of Dunnet Head, or its companion Duncansby Head, where John o’Groat’s House stood, on the beach of the Pentland Firth.
The base of the island, forming the north coast of the English Channel, measures only about half this distance, or three hundred and twenty miles; and the eastern side, from the chalk cliffs of the South Foreland, on the Strait of Dover, to the Pentland Firth, is about five hundred and forty miles long. No part of the interior of Great Britain is more distant than three or four days’ walk from the sea on one side or other. In the narrower parts of the north of Scotland, indeed, where the Moray Firth runs into the land, it is an easy day’s journey from the head of this inlet of the North Sea to that of one or other of the opposite sea lochs running in from the Atlantic.
The second island, Ireland, more rounded in general outline, measures three hundred miles from Malin Head, its northernmost point, to Mizen Head, its most southerly extremity, and two hundred miles from Carnsore Point, its southeastern corner nearest England, to Erris Head, its northwestern promontory on the Atlantic.