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Updated: April 30, 2025
Nay, even in glacier-clad Spitzbergen itself, where the character of the flora already begins to show signs of incipient chilling, we nevertheless see among the Eocene types such plants as the swamp-cyprus of the Carolinas and the wellingtonias of the Far West, together with a rich forest vegetation of poplars, birches, oaks, planes, hazels, walnuts, water-lilies, and irises.
The scene shifts to a land afar off toward the north, Norway away up into one of its mountain meadows. The landscape is a mixture of grandeur and beauty. Hills upon hills, covered with pine and fir, stretch away from the lowlands to the distant glacier-clad mountains, and patches of green meadow gleam through the dark pine depths. The clear blue sky changes to a faint haze in the hilly distance.
Behind these first massive walls, everywhere unscalable, and rising in separate promontories to altitudes of, perhaps, four hundred feet, an inner fortification of precipitous mountains flung their glacier-clad peaks heavenward to immense heights, heights which, in that region, soared far above the snow-line.
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