Note 77 — Chapter XII
Reading edition
The highest points of New Zealand, nearly 10,000 feet above the sea, are said to be clothed for two-thirds of their height with ice and snow. If, therefore, during Carboniferous times, there existed somewhere to the west of what is now central Scotland, a chain cf hills 5000 or 6000 feet high, their summits might perhaps have been as wintry us that of Mont Blanc.