1911 Encyclopædia Britannica, Volume 11… (1911)
“ The glaciers front, with a perpendicular ice-wall, a shore of debris on which a few low plants are found to grow—poppies, mosses and the like. The islands are volcanic, the main geological formation being Tertiary or Jurassic basalt, which occasionally protrudes through the ice-cap in high isolated blocks near the shore. A connecting island-chain between Franz Josef Land and Spitzbergen is probable. ”
