“On the other hand, the Icelanders consider themselves bound to pay $20,000 annually towards the general expenditure of the Danish state (Report of the Royal Commission Appointed to Inquire into the Financial Affairs of Iceland, 1861, as communicated in the Thjóðólfr newspaper, xvii., pp. 101, 107).”
SECTION IV.
POLITICAL GEOGRAPHY OF ICELAND.
§ 1. General Considerations.
Iceland, we have seen, is the largest island in the North Atlantic, and one of the most considerable known to the Old World. Lying 130 direct geographical miles east of Greenland, 500 north-west of Scotland, and 850 west of Norway; distant 1000 miles from Liverpool, 1300 from Copenhagen, and 3000 from Boston, it is claimed as an Eastern dependency of the American continent which the Icelander first colonised. It has also been called a “singular fragment of Scandinavian Europe.” Yet, geographically considered, it belongs neither to the Old nor to the New Hemisphere; it is a little continent of itself.
Formerly a considerable part of the island was made to enter the Polar circle, which, in some maps, passed through the northern third. On the other hand, the eastern coast was curtailed of its due proportions, being thrown too far west even in charts still used. Hooker, for instance, makes the longitude range from 10° to 12° west of Greenwich,—an extreme error of some two to three degrees.
Iceland extends from Portland, in N. lat. 63° 22´, to the North Cape, in N. lat. 66° 44´, covering 3° 22´ = 202 direct geographical miles of depth. The extreme longitudinal points are laid down between the north-eastern projection of Eskifjörð, in W. long. G. 13° 38´ (33´?), and the Point of Breiðavík, in 24° 40´ (36´?), or 11° 25´ of length, the degrees in this latitude being greatly reduced.[150] Thus the maximum depth would represent 186 geographical miles, which some writers increase to 190 and 192; and the length 308, which are again extended to 313. The circumference, measured from naze to naze, is variously given at 752 to 830 miles. The superficial area has also been variously calculated. Whilst Ólafsson gives 56,000 square geographical, and Egger 29,838 Danish, miles (15 = 1°), modern calculations have reduced it to 37,000, 37,388, and 40,000, the latter being generally assumed in round numbers.[151] Thus Iceland is about five times instead of double, as certain writers supposed, the size of Sicily (7700 sq. geog. miles); about one-sixth larger than Ireland (32,511); nearly equal to Portugal (37,900); approaching the state of New York (46,000); two-ninths the extent of Sweden, and one-fifth the size of France.
The parallel of N. lat. 65°, which, roughly speaking, bisects Iceland, would pass westwards through Southern Greenland, cross Davis Straits, Fox-land and Fox-channel; the northern apex of Southampton Island, the Back River, the Bear Lake, and entering Eskimo-land, formerly Russian America, would leave Norton Sound to the south, and Prince of Wales Cape a few miles to the north. Thence travelling over Behring’s Strait, it would enter Asia a little south of East Cape, cut the two Siberias, the Tobolsk River, the Urals, the White Sea, and the Bothnian Gulf, and issue from Europe about Vigten Island, somewhat north of mid-Norway. The antæcious oceans of the Old World contain no corresponding feature: the New Hemisphere shows immense uninhabited tracts—Graham’s Land, Enderby’s, Kemp’s, and the Antarctic continent, which are probably continuous; with, their outliers—South Shetlands, South Orkneys, and Sandwich Land.
The estimate of the habitable area was fixed at one-eighth by older writers.[152] It is now assumed, with Paijkull, at one-tenth (4000:40,000). Human life is confined to the larger islets, to the vicinity of the more important sub-maritime lakes, to the sheltered valleys and river courses, below the plateau, and to the false coast. The latter, eluvie mons deductus in æquor, is formed by the débris and alluvium of the mountain walls washed down by rains, torrents, débâcles, and glacier-exundations, and subsequently elevated by earthquakes, which are supposed to be still raising the southern coast.[153] According to Gunnlaugsson and Ólsen, one-third is green or agricultural; there is a similar proportion of Heiðiland; and the remainder is Úbygð (hod. Obygð) or desert—a chaos of sand-tracts and peat-swamps, lava-runs, and the huge masses of eternal congelation called Jökulls.[154]
The population was laid down by Barrow (1834) at 0·2 per whole area, and by Paijkull (1865) at 1·6: being now assumed at 70,000, it would be 1·75. Paijkull makes 6·2 head the average of habitable ground, and for the reclaimed tracts he gives 17·5. The latter figure exceeds the mean of Africa, which is 16 to the square mile (viz, 192,000,000 head to 11,556,000 square statute miles), and it is three times greater than in the whole Western Hemisphere.